{"text_format":"dbase-jsonl-2026-09-30","columns":[{"name":"line_type","type":"character","width":80},{"name":"anlys_id","type":"number","width":24,"decimals":15},{"name":"glac_id","type":"character","width":80},{"name":"anlys_time","type":"character","width":80},{"name":"area","type":"number","width":24,"decimals":15},{"name":"db_area","type":"number","width":24,"decimals":15},{"name":"width","type":"number","width":24,"decimals":15},{"name":"length","type":"number","width":24,"decimals":15},{"name":"primeclass","type":"number","width":24,"decimals":15},{"name":"min_elev","type":"number","width":24,"decimals":15},{"name":"mean_elev","type":"number","width":24,"decimals":15},{"name":"max_elev","type":"number","width":24,"decimals":15},{"name":"src_date","type":"character","width":80},{"name":"rec_status","type":"character","width":80},{"name":"glac_name","type":"character","width":80},{"name":"wgms_id","type":"character","width":80},{"name":"local_id","type":"character","width":80},{"name":"glac_stat","type":"character","width":80},{"name":"subm_id","type":"number","width":24,"decimals":15},{"name":"release_dt","type":"character","width":80},{"name":"proc_desc","type":"character","width":254},{"name":"rc_id","type":"number","width":24,"decimals":15},{"name":"geog_area","type":"character","width":80},{"name":"chief_affl","type":"character","width":80},{"name":"conn_lvl","type":"number","width":24,"decimals":15},{"name":"loc_unc_x","type":"number","width":18,"decimals":0},{"name":"loc_unc_y","type":"number","width":18,"decimals":0},{"name":"glob_unc_x","type":"number","width":18,"decimals":0},{"name":"glob_unc_y","type":"number","width":18,"decimals":0},{"name":"submitters","type":"character","width":80},{"name":"analysts","type":"character","width":80},{"name":"CenLon","type":"number","width":24,"decimals":15},{"name":"CenLat","type":"number","width":24,"decimals":15}],"n_rows":5099,"rows_kept":5099,"cut":false,"deleted_skipped":0,"read_ended":"whole","bounds":"16MiB/16384/4096/first_that_fit","version":"dbase_level_three","encoding_class":"enc_absent","reader":"statdb_count/12"}
["glac_bound",374783.000000000000000,"G226900E58234N","2008-05-01T00:00:00",2061163.401426981901750,2.061160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226900E58234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.103029199090429,58.235690500000004]
["glac_bound",374789.000000000000000,"G229576E56186N","2008-05-01T00:00:00",1128983.530003267573193,1.128980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229576E56186N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.414008665898223,56.173901000000001]
["glac_bound",374791.000000000000000,"G229517E56978N","2008-05-01T00:00:00",2008679.050152268493548,2.008680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229517E56978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.485488646775138,56.979629500000001]
["glac_bound",374795.000000000000000,"G230287E57003N","2008-05-01T00:00:00",737074.564210964017548,0.737075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230287E57003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.712610143294057,57.003451499999997]
["glac_bound",374796.000000000000000,"G230441E54750N","2008-05-01T00:00:00",1524118.247655688552186,1.524120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230441E54750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.559634625756900,54.751878000000005]
["glac_bound",374797.000000000000000,"G230479E55941N","2008-05-01T00:00:00",370736.213340389134828,0.370736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230479E55941N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.525432801700674,55.938820499999999]
["glac_bound",374804.000000000000000,"G227745E57200N","2008-05-01T00:00:00",27382.229310162711045,0.027382000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227745E57200N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.254956902721119,57.200229999999998]
["glac_bound",374806.000000000000000,"G230064E55621N","2008-05-01T00:00:00",505677.751291834749281,0.505678000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230064E55621N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.935521537955424,55.621338000000002]
["glac_bound",374811.000000000000000,"G229297E57362N","2008-05-01T00:00:00",252273.308568746550009,0.252273000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229297E57362N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.700783639216894,57.362959500000002]
["glac_bound",374812.000000000000000,"G229351E56990N","2008-05-01T00:00:00",428733.309735420334619,0.428733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229351E56990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.647603059144359,56.993068500000000]
["glac_bound",374816.000000000000000,"G226105E58968N","2008-05-01T00:00:00",2588203.677004551980644,2.588200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226105E58968N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.890786620651681,58.970509499999999]
["glac_bound",374817.000000000000000,"G224825E59924N","2008-05-01T00:00:00",174577.010859433357837,0.174577000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224825E59924N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.175757997358886,59.924349500000005]
["glac_bound",374821.000000000000000,"G228544E56626N","2008-05-01T00:00:00",120791.141030747632612,0.120791000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228544E56626N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.455747385539212,56.625570499999995]
["glac_bound",374822.000000000000000,"G229502E57026N","2008-05-01T00:00:00",122236.229044389881892,0.122236000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229502E57026N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.499116962015762,57.026436000000004]
["glac_bound",374829.000000000000000,"G222760E59334N","2008-05-01T00:00:00",254532.079921891447157,0.254532000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222760E59334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.239992958128084,59.333723000000006]
["glac_bound",374830.000000000000000,"G227906E57632N","2008-05-01T00:00:00",400674.585339907847811,0.400675000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227906E57632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.094668835684473,57.633678500000002]
["glac_bound",374843.000000000000000,"G230651E56821N","2008-05-01T00:00:00",2888625.741847810801119,2.888630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230651E56821N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351131379733772,56.820169000000000]
["glac_bound",374852.000000000000000,"G225824E59206N","2008-05-01T00:00:00",2341315.826267309952527,2.341320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225824E59206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.184145807056268,59.205759999999998]
["glac_bound",374853.000000000000000,"G230813E56481N","2008-05-01T00:00:00",153814.312581014935859,0.153814000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230813E56481N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.187140491700347,56.482059499999998]
["glac_bound",374855.000000000000000,"G230127E57342N","2008-05-01T00:00:00",72751.775156686286209,0.072752000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230127E57342N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.873336454751126,57.342039499999998]
["glac_bound",374856.000000000000000,"G230125E55615N","2008-05-01T00:00:00",205600.158553433167981,0.205600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230125E55615N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.871794563249750,55.614753000000000]
["glac_bound",374860.000000000000000,"G229010E56815N","2008-05-01T00:00:00",188892.132675582077354,0.188892000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229010E56815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.988000762809463,56.816645999999999]
["glac_bound",374862.000000000000000,"G230104E56487N","2008-05-01T00:00:00",215999.105632783932379,0.215999000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230104E56487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.896226572368391,56.487251000000001]
["glac_bound",374868.000000000000000,"G230053E55368N","2008-05-01T00:00:00",85533.038768272745074,0.085533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230053E55368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.947530593033832,55.367695499999996]
["glac_bound",374872.000000000000000,"G228269E57265N","2008-05-01T00:00:00",463038.793428578122985,0.463039000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228269E57265N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.725648950351285,57.265422999999998]
["glac_bound",374883.000000000000000,"G227854E57434N","2008-05-01T00:00:00",218224.066074471251341,0.218224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227854E57434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.145525322701303,57.434474999999999]
["glac_bound",374890.000000000000000,"G227813E57729N","2008-05-01T00:00:00",280394.334987059759442,0.280394000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227813E57729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.185471672177187,57.728947000000005]
["glac_bound",374893.000000000000000,"G230262E54569N","2008-05-01T00:00:00",287705.567789497552440,0.287706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230262E54569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.733629549439684,54.572283999999996]
["glac_bound",374896.000000000000000,"G230518E55323N","2008-05-01T00:00:00",2703382.713950876146555,2.703380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230518E55323N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.486777046879212,55.327364500000002]
["glac_bound",374897.000000000000000,"G228836E56453N","2008-05-01T00:00:00",2166947.047420974355191,2.166950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228836E56453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.158863395488197,56.458269500000000]
["glac_bound",374898.000000000000000,"G230534E54915N","2008-05-01T00:00:00",378541.713529478234705,0.378542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230534E54915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464227774937342,54.914891499999996]
["glac_bound",374904.000000000000000,"G222309E59340N","2008-05-01T00:00:00",9667242.157782474532723,9.667240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222309E59340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.694070793722631,59.359493999999998]
["glac_bound",374905.000000000000000,"G225128E59477N","2008-05-01T00:00:00",141918.791235358134145,0.141919000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225128E59477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.871267167075388,59.476463500000001]
["glac_bound",374933.000000000000000,"G229399E57744N","2008-05-01T00:00:00",771986.965426442795433,0.771987000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229399E57744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.600024985094848,57.744700999999999]
["glac_bound",374940.000000000000000,"G223099E59514N","2008-05-01T00:00:00",584156.855126930051483,0.584157000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223099E59514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.901802325937496,59.515433500000000]
["glac_bound",374942.000000000000000,"G227238E58198N","2008-05-01T00:00:00",1693229.971040986711159,1.693230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227238E58198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.758735510361873,58.204600999999997]
["glac_bound",374944.000000000000000,"G230713E55289N","2008-05-01T00:00:00",175182.361612876469735,0.175182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230713E55289N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.287958097796150,55.289276999999998]
["glac_bound",374945.000000000000000,"G227533E57982N","2008-05-01T00:00:00",1138116.665519190719351,1.138120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227533E57982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.469568908358667,57.990188000000003]
["glac_bound",374947.000000000000000,"G229132E57080N","2008-05-01T00:00:00",72585.468384251857060,0.072585000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229132E57080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.866738174974472,57.080295499999998]
["glac_bound",374948.000000000000000,"G228732E57077N","2008-05-01T00:00:00",4403670.151959246024489,4.403670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228732E57077N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.281656865568692,57.072456500000001]
["glac_bound",374953.000000000000000,"G230438E57102N","2008-05-01T00:00:00",357577.467913453467190,0.357577000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230438E57102N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.562185078947351,57.103021499999997]
["glac_bound",374961.000000000000000,"G223226E59501N","2008-05-01T00:00:00",414031.374476691358723,0.414031000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223226E59501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.775024185240966,59.500316499999997]
["glac_bound",374968.000000000000000,"G222787E59287N","2008-05-01T00:00:00",347197.476897030312102,0.347197000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222787E59287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.212745980483533,59.287277500000002]
["glac_bound",374969.000000000000000,"G228753E57555N","2008-05-01T00:00:00",351311.545822299027350,0.351312000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228753E57555N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.250411559620943,57.555843500000002]
["glac_bound",374974.000000000000000,"G226302E58747N","2008-05-01T00:00:00",188738.195863367960555,0.188738000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226302E58747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.698308857326083,58.746963500000007]
["glac_bound",374977.000000000000000,"G230922E56436N","2008-05-01T00:00:00",303200.114705483720172,0.303200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230922E56436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.077090434646124,56.435462999999999]
["glac_bound",374979.000000000000000,"G224548E59795N","2008-05-01T00:00:00",94922.239922989901970,0.094922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224548E59795N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.452808172283937,59.794557999999995]
["glac_bound",374986.000000000000000,"G230620E57157N","2008-05-01T00:00:00",499797.179086126096081,0.499797000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230620E57157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.380676408273359,57.159749500000004]
["glac_bound",374998.000000000000000,"G229411E56885N","2008-05-01T00:00:00",222959.377124694176018,0.222959000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229411E56885N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.587708188463751,56.885200499999996]
["glac_bound",375000.000000000000000,"G225275E59334N","2008-05-01T00:00:00",2275782.554758794605732,2.275780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225275E59334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.729027735373421,59.332301999999999]
["glac_bound",375001.000000000000000,"G229379E56365N","2008-05-01T00:00:00",696802.693787930300459,0.696803000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229379E56365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.625183029600635,56.365931000000003]
["glac_bound",375003.000000000000000,"G225091E59654N","2008-05-01T00:00:00",1303525.279615829698741,1.303530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225091E59654N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.906080181971959,59.656557500000005]
["glac_bound",375004.000000000000000,"G228564E57106N","2008-05-01T00:00:00",446442.710838273167610,0.446443000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228564E57106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.433656055475524,57.104485499999996]
["glac_bound",375011.000000000000000,"G227497E58364N","2008-05-01T00:00:00",383667.710876010707580,0.383668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227497E58364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.504097199821729,58.365243000000000]
["glac_bound",375012.000000000000000,"G226112E58800N","2008-05-01T00:00:00",301669.095681473729201,0.301669000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226112E58800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.884488806996558,58.799334000000002]
["glac_bound",375014.000000000000000,"G225007E59933N","2008-05-01T00:00:00",120553.419733023794834,0.120553000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225007E59933N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.989110647447319,59.932838500000003]
["glac_bound",375020.000000000000000,"G224054E59945N","2008-05-01T00:00:00",274572.949727286642883,0.274573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224054E59945N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.948181572064072,59.945236500000000]
["glac_bound",375023.000000000000000,"G228004E57979N","2008-05-01T00:00:00",4468792.037769521586597,4.468790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228004E57979N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.997718335705855,57.985680000000002]
["glac_bound",375026.000000000000000,"G231110E55257N","2008-05-01T00:00:00",217277.258893740712665,0.217277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231110E55257N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.893873136918842,55.259306500000001]
["glac_bound",375028.000000000000000,"G227347E57892N","2008-05-01T00:00:00",148823.370306449622149,0.148823000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227347E57892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.651092783389004,57.894694999999999]
["glac_bound",375030.000000000000000,"G228687E56955N","2008-05-01T00:00:00",394910.484463862085249,0.394910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228687E56955N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.310577393589369,56.954544999999996]
["glac_bound",375031.000000000000000,"G228818E56543N","2008-05-01T00:00:00",237198.741461711324519,0.237199000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228818E56543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.182420162526796,56.543875000000000]
["glac_bound",375032.000000000000000,"G227261E58545N","2008-05-01T00:00:00",61003.420973494910868,0.061003000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227261E58545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.739879427807296,58.545494500000004]
["glac_bound",375033.000000000000000,"G230871E56509N","2008-05-01T00:00:00",168228.742200475622667,0.168229000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230871E56509N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.130067623559512,56.509094500000003]
["glac_bound",375034.000000000000000,"G225715E59274N","2008-05-01T00:00:00",282164.877015980542637,0.282165000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225715E59274N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.285931666158547,59.274529999999999]
["glac_bound",375036.000000000000000,"G230999E56484N","2008-05-01T00:00:00",621630.267322140163742,0.621630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230999E56484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.999433214372885,56.484364499999998]
["glac_bound",375039.000000000000000,"G230847E55101N","2008-05-01T00:00:00",181142.240547554130899,0.181142000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230847E55101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.154501328441484,55.100182500000003]
["glac_bound",375048.000000000000000,"G225121E59474N","2008-05-01T00:00:00",192529.447416494600475,0.192529000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225121E59474N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.880761800410141,59.474094500000000]
["glac_bound",375051.000000000000000,"G224967E59573N","2008-05-01T00:00:00",502675.305072870978620,0.502675000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224967E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.029696971917815,59.573369000000000]
["glac_bound",375052.000000000000000,"G222224E59573N","2008-05-01T00:00:00",131656.740095431392547,0.131657000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222224E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.775521251215793,59.572675500000003]
["glac_bound",375054.000000000000000,"G225572E59334N","2008-05-01T00:00:00",708651.474590959609486,0.708651000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225572E59334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.428364989729232,59.334918000000002]
["glac_bound",375057.000000000000000,"G224129E59836N","2008-05-01T00:00:00",10736213.731615651398897,10.736200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224129E59836N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.863145651575849,59.838722500000003]
["glac_bound",375059.000000000000000,"G222222E59694N","2008-05-01T00:00:00",23645193.122389346361160,23.645199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222222E59694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.816608936536795,59.688193499999997]
["glac_bound",375064.000000000000000,"G227323E57633N","2008-05-01T00:00:00",208769.200425035844091,0.208769000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-11T00:00:00","okay","None","None","08BC227323E57633N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.675840592297675,57.632527500000002]
["glac_bound",375065.000000000000000,"G225697E59388N","2008-05-01T00:00:00",491051.287761691724882,0.491051000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225697E59388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.304028786458332,59.388512499999997]
["glac_bound",375068.000000000000000,"G230362E56315N","2008-05-01T00:00:00",166395.314219742227579,0.166395000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230362E56315N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.638714368995977,56.314978999999994]
["glac_bound",375072.000000000000000,"G227549E58202N","2008-05-01T00:00:00",1907942.486631609732285,1.907940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227549E58202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.452734977518105,58.201564000000005]
["glac_bound",375075.000000000000000,"G227871E57803N","2008-05-01T00:00:00",467542.271122731326614,0.467542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227871E57803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.127679192307681,57.803393000000000]
["glac_bound",375079.000000000000000,"G229575E56432N","2008-05-01T00:00:00",923179.044145354069769,0.923179000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229575E56432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.424666645764773,56.431998000000000]
["glac_bound",375084.000000000000000,"G224344E59838N","2008-05-01T00:00:00",4336484.523918274790049,4.336480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224344E59838N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.656746325096549,59.847954999999999]
["glac_bound",375089.000000000000000,"G230342E56204N","2008-05-01T00:00:00",4115109.845294278580695,4.115110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230342E56204N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.660552787352970,56.201253000000001]
["glac_bound",375090.000000000000000,"G225020E59611N","2008-05-01T00:00:00",1260509.909799611428753,1.260510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225020E59611N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.982302356548729,59.611420000000003]
["glac_bound",375097.000000000000000,"G226215E58958N","2008-05-01T00:00:00",5956594.289110695011914,5.956590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226215E58958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.782562775995956,58.956712500000002]
["glac_bound",375102.000000000000000,"G222819E59250N","2008-05-01T00:00:00",2879750.591894361656159,2.879750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222819E59250N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.185172350097673,59.251868500000000]
["glac_bound",375103.000000000000000,"G225683E59381N","2008-05-01T00:00:00",109752.526892423295067,0.109753000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225683E59381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.317482574909064,59.381451999999996]
["glac_bound",375104.000000000000000,"G227915E57631N","2008-05-01T00:00:00",174231.469752208184218,0.174231000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227915E57631N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.086144657114630,57.631161500000005]
["glac_bound",375108.000000000000000,"G223681E59571N","2008-05-01T00:00:00",102566.133694508913322,0.102566000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223681E59571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.320083005754668,59.570514000000003]
["glac_bound",375114.000000000000000,"G228640E57477N","2008-05-01T00:00:00",84802.933527187138679,0.084803000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228640E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.359761950980413,57.476316999999995]
["glac_bound",375115.000000000000000,"G230294E57201N","2008-05-01T00:00:00",79780.679119640335557,0.079781000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230294E57201N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.705799267191992,57.200809000000000]
["glac_bound",375116.000000000000000,"G230211E54438N","2008-05-01T00:00:00",1643536.863331638043746,1.643540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230211E54438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.780446063976058,54.440634500000002]
["glac_bound",375126.000000000000000,"G226281E58845N","2008-05-01T00:00:00",1345302.438697653124109,1.345300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226281E58845N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.722069495499312,58.845442000000006]
["glac_bound",375127.000000000000000,"G228392E57376N","2008-05-01T00:00:00",1020753.973281986196525,1.020750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228392E57376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.604025348512778,57.376136500000001]
["glac_bound",375129.000000000000000,"G223392E59940N","2008-05-01T00:00:00",152623.936742920865072,0.152624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223392E59940N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.608087538135266,59.940198499999994]
["glac_bound",375137.000000000000000,"G228098E56761N","2008-05-01T00:00:00",1046610.315705909859389,1.046610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228098E56761N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.903545841740538,56.761313000000001]
["glac_bound",375139.000000000000000,"G224299E59983N","2008-05-01T00:00:00",59227.267865521847853,0.059227000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224299E59983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.703993568243845,59.983843999999998]
["glac_bound",375140.000000000000000,"G229740E56792N","2008-05-01T00:00:00",379565.475016863259953,0.379565000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229740E56792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.262855748576840,56.794299500000001]
["glac_bound",375142.000000000000000,"G222429E59996N","2008-05-01T00:00:00",7246584.440477908588946,7.246580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222429E59996N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.469772722240151,59.994702500000002]
["glac_bound",375143.000000000000000,"G227503E57708N","2008-05-01T00:00:00",10590868.986004156991839,10.590900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227503E57708N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.504190177175531,57.712325999999997]
["glac_bound",375146.000000000000000,"G230390E56127N","2008-05-01T00:00:00",2430089.769792848266661,2.430090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230390E56127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.591648625239827,56.133678000000003]
["glac_bound",375147.000000000000000,"G230161E54815N","2008-05-01T00:00:00",55907.422224175032170,0.055907000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230161E54815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.839061118938162,54.814877500000001]
["glac_bound",375152.000000000000000,"G229325E57228N","2008-05-01T00:00:00",291940.611027021019254,0.291941000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229325E57228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.678144107339506,57.229634000000004]
["glac_bound",375171.000000000000000,"G222072E59534N","2008-05-01T00:00:00",287996.787269340304192,0.287997000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222072E59534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.928850149999988,59.534594999999996]
["glac_bound",375173.000000000000000,"G226762E58577N","2008-05-01T00:00:00",683841.583187808399089,0.683842000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226762E58577N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.238856289646094,58.575561500000006]
["glac_bound",375179.000000000000000,"G226640E58326N","2008-05-01T00:00:00",389103.062406888813712,0.389103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226640E58326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.361695052698309,58.327446000000002]
["glac_bound",375182.000000000000000,"G230011E56302N","2008-05-01T00:00:00",202846.900122746592388,0.202847000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230011E56302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.989323660688115,56.301561999999997]
["glac_bound",375186.000000000000000,"G223256E59365N","2008-05-01T00:00:00",462134.454227816255298,0.462134000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223256E59365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.742306818155555,59.363978000000003]
["glac_bound",375188.000000000000000,"G228397E57456N","2008-05-01T00:00:00",6843845.161128868348897,6.843850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228397E57456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.598824479743598,57.458227500000007]
["glac_bound",375192.000000000000000,"G229968E56437N","2008-05-01T00:00:00",104185372.33363793790340,104.185000000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229968E56437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.001915579099091,56.473250000000000]
["glac_bound",375193.000000000000000,"G230128E56431N","2008-05-01T00:00:00",272026.746130437357351,0.272027000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230128E56431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.867933466217323,56.429271000000000]
["glac_bound",375196.000000000000000,"G222606E59347N","2008-05-01T00:00:00",1671576.540585188427940,1.671580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222606E59347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.396473381879588,59.346452499999998]
["glac_bound",375199.000000000000000,"G228037E57385N","2008-05-01T00:00:00",363137.957096289494075,0.363138000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228037E57385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.968891507974149,57.386381499999999]
["glac_bound",375201.000000000000000,"G223046E59523N","2008-05-01T00:00:00",1274078.631927865790203,1.274080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223046E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.957677013746547,59.523943000000003]
["glac_bound",375202.000000000000000,"G229141E57048N","2008-05-01T00:00:00",1117658.806670053163543,1.117660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229141E57048N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.856135706231441,57.048439500000001]
["glac_bound",375210.000000000000000,"G225315E59267N","2008-05-01T00:00:00",17977391.781631283462048,17.977399999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225315E59267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.718101866642854,59.256366000000000]
["glac_bound",375215.000000000000000,"G228414E57467N","2008-05-01T00:00:00",172926.636065571074141,0.172927000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228414E57467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584574995133721,57.468344500000001]
["glac_bound",375218.000000000000000,"G223257E59551N","2008-05-01T00:00:00",350996.670639497519005,0.350997000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223257E59551N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.745866321896358,59.549678999999998]
["glac_bound",375219.000000000000000,"G229396E57367N","2008-05-01T00:00:00",391057.714520513662137,0.391058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229396E57367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.605093972823056,57.369061000000002]
["glac_bound",375224.000000000000000,"G230488E57085N","2008-05-01T00:00:00",1015919.335171441431157,1.015920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230488E57085N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.513833223622441,57.085724999999996]
["glac_bound",375225.000000000000000,"G225915E58812N","2008-05-01T00:00:00",11072109.783192614093423,11.072100000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB225915E58812N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.091676768457603,58.812760499999996]
["glac_bound",375230.000000000000000,"G230011E55612N","2008-05-01T00:00:00",113659.202174774734885,0.113659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230011E55612N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.988838617707472,55.612355500000007]
["glac_bound",375233.000000000000000,"G226217E58992N","2008-05-01T00:00:00",2503405.395848855841905,2.503410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226217E58992N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.784506318420370,58.993499999999997]
["glac_bound",375238.000000000000000,"G225567E59504N","2008-05-01T00:00:00",169064.203609221032821,0.169064000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225567E59504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.432268391964271,59.504246500000001]
["glac_bound",375239.000000000000000,"G229411E56918N","2008-05-01T00:00:00",1743791.135964836226776,1.743790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229411E56918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.584364840462428,56.917831499999998]
["glac_bound",375242.000000000000000,"G225590E59262N","2008-05-01T00:00:00",637939.337527445284650,0.637939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225590E59262N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.412588633268570,59.263271000000003]
["glac_bound",375243.000000000000000,"G227198E58334N","2008-05-01T00:00:00",1802440.751062500989065,1.802440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227198E58334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.807159290958850,58.332966499999998]
["glac_bound",375246.000000000000000,"G228148E57156N","2008-05-01T00:00:00",603825.518434398225509,0.603826000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228148E57156N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.850623107713773,57.155754999999999]
["glac_bound",375247.000000000000000,"G224577E59919N","2008-05-01T00:00:00",576009.851061607128941,0.576010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224577E59919N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.422627422849388,59.919386000000003]
["glac_bound",375248.000000000000000,"G227117E58514N","2008-05-01T00:00:00",368092.738210083683953,0.368093000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227117E58514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.884569304802966,58.513021999999999]
["glac_bound",375250.000000000000000,"G230369E56218N","2008-05-01T00:00:00",4087671.781892397440970,4.087670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230369E56218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.643518389758185,56.223039000000000]
["glac_bound",375251.000000000000000,"G224799E59818N","2008-05-01T00:00:00",173572.142137308837846,0.173572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224799E59818N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.201374932229498,59.818302000000003]
["glac_bound",375258.000000000000000,"G229309E56536N","2008-05-01T00:00:00",150160.657007607951527,0.150161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229309E56536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.690769477517989,56.536420000000000]
["glac_bound",375261.000000000000000,"G228077E57830N","2008-05-01T00:00:00",117166.626772287127096,0.117167000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228077E57830N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.924251301125082,57.829661500000000]
["glac_bound",375262.000000000000000,"G222447E59515N","2008-05-01T00:00:00",1377697.921513156266883,1.377700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222447E59515N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.553326791713005,59.515744999999995]
["glac_bound",375270.000000000000000,"G230269E55913N","2008-05-01T00:00:00",261744.797635004273616,0.261745000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230269E55913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.731363520000002,55.912575000000004]
["glac_bound",375275.000000000000000,"G230028E57032N","2008-05-01T00:00:00",252103.689414833497722,0.252104000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230028E57032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.969350073867730,57.033872000000002]
["glac_bound",375284.000000000000000,"G227448E58093N","2008-05-01T00:00:00",10600222.930917849764228,10.600199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227448E58093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.526937470491816,58.115050500000002]
["glac_bound",375289.000000000000000,"G228511E57078N","2008-05-01T00:00:00",140739.701650138682453,0.140740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228511E57078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.486539206553743,57.077596499999999]
["glac_bound",375290.000000000000000,"G229537E56279N","2008-05-01T00:00:00",9727667.422260552644730,9.727670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229537E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.448777262743761,56.293374000000000]
["glac_bound",375294.000000000000000,"G229295E56578N","2008-05-01T00:00:00",751879.582760752644390,0.751880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229295E56578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.702655728074603,56.581710999999999]
["glac_bound",375299.000000000000000,"G228040E56849N","2008-05-01T00:00:00",90435.800765489679179,0.090436000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228040E56849N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.958800115876102,56.850909999999999]
["glac_bound",375305.000000000000000,"G224260E59816N","2008-05-01T00:00:00",2213623.571291403844953,2.213620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224260E59816N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.748824297348960,59.815232999999999]
["glac_bound",375307.000000000000000,"G226746E58256N","2008-05-01T00:00:00",380134.245985058776569,0.380134000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226746E58256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.254715420950674,58.255793499999996]
["glac_bound",375308.000000000000000,"G229361E56561N","2008-05-01T00:00:00",447250.679704528709408,0.447251000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229361E56561N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.634693914721765,56.563483500000004]
["glac_bound",375311.000000000000000,"G226938E58299N","2008-05-01T00:00:00",762126.284965984523296,0.762126000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226938E58299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.065097810442808,58.297201999999999]
["glac_bound",375316.000000000000000,"G227402E58101N","2008-05-01T00:00:00",547570.443073450820521,0.547570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227402E58101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.597474315789469,58.101614999999995]
["glac_bound",375323.000000000000000,"G230295E55709N","2008-05-01T00:00:00",6837130.061956075951457,6.837130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230295E55709N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.685985963322764,55.715015500000000]
["glac_bound",375324.000000000000000,"G227844E57414N","2008-05-01T00:00:00",263523.514608582248911,0.263524000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227844E57414N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.156294784194301,57.413978999999998]
["glac_bound",375327.000000000000000,"G231118E57370N","2008-05-01T00:00:00",131833.970966321503511,0.131834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231118E57370N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.882717674251154,57.370238499999999]
["glac_bound",375330.000000000000000,"G222377E59535N","2008-05-01T00:00:00",3248853.006618563085794,3.248850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222377E59535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.636660026994150,59.540706000000000]
["glac_bound",375334.000000000000000,"G229216E57210N","2008-05-01T00:00:00",279883.030237019644119,0.279883000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229216E57210N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.788961017192122,57.210559000000003]
["glac_bound",375335.000000000000000,"G227165E58232N","2008-05-01T00:00:00",1731679.473981196526438,1.731680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227165E58232N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.834931965049748,58.228779000000003]
["glac_bound",375337.000000000000000,"G225667E59378N","2008-05-01T00:00:00",307656.087002443964593,0.307656000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225667E59378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.332916490331513,59.378596000000002]
["glac_bound",375339.000000000000000,"G229774E56553N","2008-05-01T00:00:00",1572773.185459405416623,1.572770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229774E56553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.226149792678342,56.552080000000004]
["glac_bound",375345.000000000000000,"G228300E57217N","2008-05-01T00:00:00",743619.315814093104564,0.743619000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228300E57217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.698444035490240,57.217151500000000]
["glac_bound",375346.000000000000000,"G223714E59867N","2008-05-01T00:00:00",1582752.376747385598719,1.582750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223714E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.285951655620238,59.867442499999996]
["glac_bound",375350.000000000000000,"G228512E57578N","2008-05-01T00:00:00",70537.718726559673087,0.070538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228512E57578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.487915019230769,57.578564499999999]
["glac_bound",375354.000000000000000,"G228512E57320N","2008-05-01T00:00:00",8605525.408173114061356,8.605530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228512E57320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.490059222894786,57.328946000000002]
["glac_bound",375356.000000000000000,"G227502E58192N","2008-05-01T00:00:00",1417856.442034038249403,1.417860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227502E58192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.494546531657363,58.191579500000003]
["glac_bound",375359.000000000000000,"G224598E59912N","2008-05-01T00:00:00",114016.205972737414413,0.114016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224598E59912N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.401747385675804,59.912213500000000]
["glac_bound",375360.000000000000000,"G222764E59113N","2008-05-01T00:00:00",297484.456970736617222,0.297484000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222765E59114N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.235982741055068,59.114159500000000]
["glac_bound",375369.000000000000000,"G228148E57412N","2008-05-01T00:00:00",55648.626073195853678,0.055649000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228148E57412N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.851529391842689,57.411586999999997]
["glac_bound",375370.000000000000000,"G222300E59836N","2008-05-01T00:00:00",541882.022264368250035,0.541882000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222300E59836N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.698942720973776,59.835642499999999]
["glac_bound",375378.000000000000000,"G230610E56826N","2008-05-01T00:00:00",111618.534204894283903,0.111619000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230610E56826N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.390349685642349,56.826079499999999]
["glac_bound",375381.000000000000000,"G230108E55603N","2008-05-01T00:00:00",826906.174343204475008,0.826906000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230108E55603N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.893194141275984,55.603775999999996]
["glac_bound",375383.000000000000000,"G225326E59702N","2008-05-01T00:00:00",133850.637936561019160,0.133851000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225326E59702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.674164390229890,59.702473499999996]
["glac_bound",375388.000000000000000,"G229144E57041N","2008-05-01T00:00:00",51407.164729329742840,0.051407000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229144E57041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.855895858695646,57.041258499999998]
["glac_bound",375392.000000000000000,"G225111E59588N","2008-05-01T00:00:00",325693.516850485175382,0.325694000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225111E59588N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.885080185701867,59.588746499999999]
["glac_bound",375395.000000000000000,"G227294E58291N","2008-05-01T00:00:00",305545.536690832057502,0.305546000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227294E58291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.702923457054652,58.289940999999999]
["glac_bound",375401.000000000000000,"G225299E59531N","2008-05-01T00:00:00",765774.415909831994213,0.765774000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225299E59531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.703373785570278,59.536124000000001]
["glac_bound",375402.000000000000000,"G228982E56411N","2008-05-01T00:00:00",5154461.503141649067402,5.154460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD228982E56411N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.025756253683994,56.419564000000001]
["glac_bound",375403.000000000000000,"G230536E57038N","2008-05-01T00:00:00",265049.745110739022493,0.265050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230536E57038N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464060022257399,57.038186500000002]
["glac_bound",375408.000000000000000,"G231168E57516N","2008-05-01T00:00:00",284725.842391100071836,0.284726000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231168E57516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.832031181920456,57.516452000000001]
["glac_bound",375413.000000000000000,"G223435E59904N","2008-05-01T00:00:00",151469.329882549936883,0.151469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223435E59904N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.564576522258051,59.904071500000001]
["glac_bound",375415.000000000000000,"G228575E56854N","2008-05-01T00:00:00",39983936.497018240392208,39.983899999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228575E56854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.428888458715903,56.825760500000001]
["glac_bound",375421.000000000000000,"G226867E58634N","2008-05-01T00:00:00",401015.411748159269337,0.401015000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226867E58634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.136295546793463,58.635455499999999]
["glac_bound",375426.000000000000000,"G222831E59028N","2008-05-01T00:00:00",923850.435375676839612,0.923850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222831E59028N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.166671086447707,59.025292499999999]
["glac_bound",375432.000000000000000,"G228454E56762N","2008-05-01T00:00:00",89344.835512330479105,0.089345000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228454E56762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.545339534755101,56.762921000000006]
["glac_bound",375434.000000000000000,"G229381E56316N","2008-05-01T00:00:00",634544.740398539928719,0.634545000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229381E56316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.617874944690612,56.315466499999999]
["glac_bound",375435.000000000000000,"G228338E57413N","2008-05-01T00:00:00",1763168.584899229463190,1.763170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228338E57413N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.663548014473236,57.416027000000000]
["glac_bound",375437.000000000000000,"G225948E59133N","2008-05-01T00:00:00",155547.740028750209603,0.155548000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225948E59133N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.052113784105984,59.133420000000001]
["glac_bound",375439.000000000000000,"G226418E58467N","2008-05-01T00:00:00",12612.105878749503972,0.012612000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BD226418E58467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.582526615079360,58.467008500000006]
["glac_bound",375447.000000000000000,"G230811E55027N","2008-05-01T00:00:00",2219189.180147909093648,2.219190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230811E55027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.189450321321715,55.027408500000000]
["glac_bound",375450.000000000000000,"G227516E57861N","2008-05-01T00:00:00",1393927.326925353147089,1.393930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227516E57861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.477849794241592,57.861610499999998]
["glac_bound",375452.000000000000000,"G229155E56458N","2008-05-01T00:00:00",165465.522781798557844,0.165466000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229155E56458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.843259892810863,56.457695500000000]
["glac_bound",375453.000000000000000,"G228038E57776N","2008-05-01T00:00:00",569575.410668929223903,0.569575000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228038E57776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.962584866228099,57.777209499999998]
["glac_bound",375455.000000000000000,"G230446E55931N","2008-05-01T00:00:00",19550879.925462529063225,19.550899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230446E55931N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.594129932100657,55.958089500000000]
["glac_bound",375456.000000000000000,"G228312E57422N","2008-05-01T00:00:00",129501.525923725290340,0.129502000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228312E57422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.688148473435319,57.421799000000000]
["glac_bound",375463.000000000000000,"G227442E58365N","2008-05-01T00:00:00",1871302.588059446541592,1.871300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227442E58365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.556597186385318,58.364910999999999]
["glac_bound",375464.000000000000000,"G227991E57108N","2008-05-01T00:00:00",704256.014053579536267,0.704256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227991E57108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.007388820123765,57.106712000000002]
["glac_bound",375466.000000000000000,"G228754E57477N","2008-05-01T00:00:00",204001.492459500936093,0.204001000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228754E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.241108520607526,57.476670499999997]
["glac_bound",375469.000000000000000,"G222591E59367N","2008-05-01T00:00:00",97592.141259892203379,0.097592000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222591E59367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.410228884529175,59.366245500000005]
["glac_bound",375474.000000000000000,"G230655E55370N","2008-05-01T00:00:00",281732.745460731268395,0.281733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230655E55370N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.345611022757794,55.370920999999996]
["glac_bound",375475.000000000000000,"G230177E55766N","2008-05-01T00:00:00",1982692.972980437101796,1.982690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230177E55766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.826996952154047,55.764740500000002]
["glac_bound",375476.000000000000000,"G225751E59326N","2008-05-01T00:00:00",344814.392510231584311,0.344814000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225751E59326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.246193284235289,59.326532000000000]
["glac_bound",375477.000000000000000,"G228526E57351N","2008-05-01T00:00:00",203805.866144860658096,0.203806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228526E57351N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.474720694187340,57.351294499999995]
["glac_bound",375479.000000000000000,"G230387E55659N","2008-05-01T00:00:00",302547.979221301502548,0.302548000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230387E55659N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.612393587365602,55.658598499999997]
["glac_bound",375485.000000000000000,"G227390E57833N","2008-05-01T00:00:00",224608.674993196589639,0.224609000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227390E57833N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.609150981343305,57.832403999999997]
["glac_bound",375489.000000000000000,"G230403E56128N","2008-05-01T00:00:00",572477.406628926284611,0.572477000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230403E56128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.596430767372624,56.126891000000001]
["glac_bound",375491.000000000000000,"G223521E59470N","2008-05-01T00:00:00",236921.498315572593128,0.236922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223521E59470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.479742442040504,59.469362500000003]
["glac_bound",375494.000000000000000,"G224119E59861N","2008-05-01T00:00:00",421697.161200312082656,0.421697000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224119E59861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.882391221578928,59.860962000000001]
["glac_bound",375496.000000000000000,"G227787E57909N","2008-05-01T00:00:00",2288182.213942207396030,2.288180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227787E57909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.223533315995098,57.910165000000006]
["glac_bound",375497.000000000000000,"G223418E59529N","2008-05-01T00:00:00",290415.372614915017039,0.290415000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223418E59529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.583148106107217,59.528691000000002]
["glac_bound",375499.000000000000000,"G227806E57494N","2008-05-01T00:00:00",689473.879348873975687,0.689474000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227806E57494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.191255163083014,57.494568999999998]
["glac_bound",375504.000000000000000,"G221712E59917N","2008-05-01T00:00:00",2198836.130055213812739,2.198840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221712E59917N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.292438609631290,59.917800499999998]
["glac_bound",375506.000000000000000,"G225075E59593N","2008-05-01T00:00:00",83233.443113388741040,0.083233000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225075E59593N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.926231240814587,59.593779999999995]
["glac_bound",375507.000000000000000,"G228930E57098N","2008-05-01T00:00:00",4706669.336730983108282,4.706670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228930E57098N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.068133974386114,57.107084999999998]
["glac_bound",375509.000000000000000,"G228991E56810N","2008-05-01T00:00:00",3758575.388592458795756,3.758580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228991E56810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.020855843114305,56.816046999999998]
["glac_bound",375520.000000000000000,"G228736E57458N","2008-05-01T00:00:00",1752180.447435343870893,1.752180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228736E57458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.269442948904782,57.456135500000002]
["glac_bound",375522.000000000000000,"G231009E57143N","2008-05-01T00:00:00",160401.807933824165957,0.160402000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA231009E57143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.994516550061292,57.143282499999998]
["glac_bound",375524.000000000000000,"G229877E56380N","2008-05-01T00:00:00",29057879.707520440220833,29.057900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229877E56380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.139829720670377,56.403255000000001]
["glac_bound",375526.000000000000000,"G228861E57736N","2008-05-01T00:00:00",339209.741391554765869,0.339210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228861E57736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.137464645059936,57.735875999999998]
["glac_bound",375528.000000000000000,"G230545E54811N","2008-05-01T00:00:00",1330181.657767015974969,1.330180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230545E54811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.453331938746487,54.809958500000000]
["glac_bound",375530.000000000000000,"G223253E59708N","2008-05-01T00:00:00",1446565.513004456413910,1.446570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223253E59708N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.739011217110004,59.707037499999998]
["glac_bound",375532.000000000000000,"G229652E56313N","2008-05-01T00:00:00",826802.193399196141399,0.826802000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229652E56313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.349242272740327,56.313612500000005]
["glac_bound",375533.000000000000000,"G226572E58569N","2008-05-01T00:00:00",87528.082251440107939,0.087528000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226572E58569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.427031087149487,58.569959499999996]
["glac_bound",375541.000000000000000,"G230611E55200N","2008-05-01T00:00:00",154145.316426949255401,0.154145000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230611E55200N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.389762146120404,55.200088000000001]
["glac_bound",375556.000000000000000,"G230506E54646N","2008-05-01T00:00:00",249144.320238824293483,0.249144000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230506E54646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.494268315838156,54.646577000000001]
["glac_bound",375560.000000000000000,"G230154E55840N","2008-05-01T00:00:00",16732073.695910669863224,16.732099999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230154E55840N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.847502904073622,55.860771000000000]
["glac_bound",375561.000000000000000,"G230569E56774N","2008-05-01T00:00:00",338588.497825645667035,0.338589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230569E56774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.437355748851644,56.772894000000001]
["glac_bound",375562.000000000000000,"G226888E58312N","2008-05-01T00:00:00",344777.668520453677047,0.344778000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226888E58312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.115205196309887,58.310502499999998]
["glac_bound",375563.000000000000000,"G227926E56863N","2008-05-01T00:00:00",325692.210086669656448,0.325692000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227926E56863N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.073212861580998,56.862976000000003]
["glac_bound",375567.000000000000000,"G228710E56775N","2008-05-01T00:00:00",9285570.357734810560942,9.285570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228710E56775N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.285581414835178,56.773047000000005]
["glac_bound",375570.000000000000000,"G223566E59670N","2008-05-01T00:00:00",265559.916169153468218,0.265560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223566E59670N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.434213867030536,59.670221999999995]
["glac_bound",375575.000000000000000,"G230747E56485N","2008-05-01T00:00:00",1164362.910821395227686,1.164360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230747E56485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.255212318416113,56.485216000000001]
["glac_bound",375584.000000000000000,"G222954E59465N","2008-05-01T00:00:00",73471.952380816059303,0.073472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222954E59465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.046051076045785,59.463834000000006]
["glac_bound",375587.000000000000000,"G229337E57728N","2008-05-01T00:00:00",1862740.434667776571587,1.862740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229337E57728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.678877940226471,57.730755000000002]
["glac_bound",375588.000000000000000,"G230300E57302N","2008-05-01T00:00:00",250464.099223226046888,0.250464000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230300E57302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.701741954922227,57.301801999999995]
["glac_bound",375590.000000000000000,"G222753E59448N","2008-05-01T00:00:00",1437476.801265725400299,1.437480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222753E59448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.247027858878909,59.450495000000004]
["glac_bound",375592.000000000000000,"G231213E57072N","2008-05-01T00:00:00",483162.169656152313109,0.483162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231213E57072N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.787268835211876,57.072492499999996]
["glac_bound",375593.000000000000000,"G228931E56407N","2008-05-01T00:00:00",6924360.083877788856626,6.924360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228931E56407N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.064093666287590,56.419998000000000]
["glac_bound",375594.000000000000000,"G222645E59059N","2008-05-01T00:00:00",918074.147618389572017,0.918074000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222646E59059N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.353905432113834,59.059547999999999]
["glac_bound",375595.000000000000000,"G228928E57205N","2008-05-01T00:00:00",6886729.453345077112317,6.886730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228928E57205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.046909345500012,57.214786500000002]
["glac_bound",375596.000000000000000,"G222667E59669N","2008-05-01T00:00:00",1444014.757516596931964,1.444010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222667E59669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.330188162049865,59.669546499999996]
["glac_bound",375597.000000000000000,"G231684E56252N","2008-05-01T00:00:00",125372.935555288640899,0.125373000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231684E56252N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.316816299594734,56.252116999999998]
["glac_bound",375598.000000000000000,"G226882E58287N","2008-05-01T00:00:00",51532.949108297296334,0.051533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226882E58287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.117650399765523,58.286970500000002]
["glac_bound",375599.000000000000000,"G227221E58044N","2008-05-01T00:00:00",454936.924734690517653,0.454937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227221E58044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.778567963756814,58.043282500000004]
["glac_bound",375602.000000000000000,"G226320E58900N","2008-05-01T00:00:00",210105.779909671051428,0.210106000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226320E58900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.680232772641091,58.901687499999994]
["glac_bound",375603.000000000000000,"G229031E56860N","2008-05-01T00:00:00",1137396.409707891056314,1.137400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229031E56860N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.963128156934317,56.858682000000002]
["glac_bound",375605.000000000000000,"G230641E55369N","2008-05-01T00:00:00",378744.891716316342354,0.378745000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230641E55369N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.356657348050646,55.370234499999995]
["glac_bound",375607.000000000000000,"G231040E57139N","2008-05-01T00:00:00",89439.577958365858649,0.089440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231040E57139N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.960980977560126,57.139324000000002]
["glac_bound",375608.000000000000000,"G228742E57424N","2008-05-01T00:00:00",122942.137215514696436,0.122942000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228742E57424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.256015776190395,57.424299000000005]
["glac_bound",375609.000000000000000,"G224327E59744N","2008-05-01T00:00:00",89813.865466969713452,0.089814000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224327E59744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.674268512940330,59.744912499999998]
["glac_bound",375610.000000000000000,"G225649E59161N","2008-05-01T00:00:00",586453.976587570388801,0.586454000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225649E59161N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.353758135069825,59.161468499999998]
["glac_bound",375611.000000000000000,"G225929E59222N","2008-05-01T00:00:00",92239.838971104545635,0.092240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225929E59222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.070902853389839,59.221297000000000]
["glac_bound",375617.000000000000000,"G224637E59966N","2008-05-01T00:00:00",128325.403213781872182,0.128325000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224637E59966N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.364161180408956,59.966759499999995]
["glac_bound",375623.000000000000000,"G222242E59369N","2008-05-01T00:00:00",1020469.657421240815893,1.020470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222242E59369N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.760890094539093,59.367770999999998]
["glac_bound",375626.000000000000000,"G228502E57410N","2008-05-01T00:00:00",170981.113524304382736,0.170981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228502E57410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.499981945887072,57.412644000000000]
["glac_bound",375627.000000000000000,"G221713E59892N","2008-05-01T00:00:00",930489.671161450212821,0.930490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221713E59892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.282802618837195,59.889515000000003]
["glac_bound",375630.000000000000000,"G222977E59449N","2008-05-01T00:00:00",441068.195172038918827,0.441068000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222977E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.022180282627062,59.449026500000002]
["glac_bound",375645.000000000000000,"G228961E56619N","2008-05-01T00:00:00",1502869.920702645089477,1.502870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228961E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.036868745433196,56.620194999999995]
["glac_bound",375646.000000000000000,"G226822E58483N","2008-05-01T00:00:00",1743704.262691535986960,1.743700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226822E58483N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.178150403169013,58.485234499999997]
["glac_bound",375650.000000000000000,"G223566E59832N","2008-05-01T00:00:00",90507.641626274562441,0.090508000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223566E59832N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.432826640961537,59.832611999999997]
["glac_bound",375658.000000000000000,"G229106E56983N","2008-05-01T00:00:00",679539.472739038988948,0.679540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229106E56983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.897088461703731,56.982867499999998]
["glac_bound",375659.000000000000000,"G221885E59560N","2008-05-01T00:00:00",8846648.551000546664000,8.846650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221885E59560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.108001571981418,59.573584499999996]
["glac_bound",375664.000000000000000,"G230054E56320N","2008-05-01T00:00:00",4048884.852281954139471,4.048880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230054E56320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.946154161045968,56.323753500000002]
["glac_bound",375666.000000000000000,"G228610E57058N","2008-05-01T00:00:00",54896.577150283483206,0.054897000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228610E57058N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.389702054408104,57.058158499999998]
["glac_bound",375671.000000000000000,"G223466E59472N","2008-05-01T00:00:00",96806.409070184046868,0.096806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223466E59472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.533562129968402,59.472120500000003]
["glac_bound",375677.000000000000000,"G228955E57024N","2008-05-01T00:00:00",63729.773970970585651,0.063730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228955E57024N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.042596254700470,57.023389000000002]
["glac_bound",375678.000000000000000,"G227861E57184N","2008-05-01T00:00:00",3557838.065555117093027,3.557840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227861E57184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.143882862161092,57.182502999999997]
["glac_bound",375679.000000000000000,"G230093E55780N","2008-05-01T00:00:00",156908.005130433855811,0.156908000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230093E55780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.906711061562788,55.780686000000003]
["glac_bound",375685.000000000000000,"G230503E54682N","2008-05-01T00:00:00",147673.526607334904838,0.147674000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230503E54682N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.497423859464504,54.682006999999999]
["glac_bound",375688.000000000000000,"G227251E57998N","2008-05-01T00:00:00",1053052.882088673068210,1.053050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227251E57998N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.752152907418690,58.000513499999997]
["glac_bound",375695.000000000000000,"G229381E56647N","2008-05-01T00:00:00",861509.363129628705792,0.861509000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229381E56647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.621685895038155,56.649332500000000]
["glac_bound",375696.000000000000000,"G230477E56070N","2008-05-01T00:00:00",135868.582638731750194,0.135869000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230477E56070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522152731277515,56.069288000000000]
["glac_bound",375699.000000000000000,"G229268E57379N","2008-05-01T00:00:00",763218.198056596680544,0.763218000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229268E57379N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.733483607177504,57.378748999999999]
["glac_bound",375703.000000000000000,"G225571E59239N","2008-05-01T00:00:00",2800557.203552708029747,2.800560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225571E59239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.435554791281845,59.243894499999996]
["glac_bound",375705.000000000000000,"G230711E56764N","2008-05-01T00:00:00",311766.365448564407416,0.311766000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230711E56764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.289246598075636,56.764517499999997]
["glac_bound",375707.000000000000000,"G230515E55894N","2008-05-01T00:00:00",81775.980205661253422,0.081776000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230515E55894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.484927662808445,55.893650500000000]
["glac_bound",375713.000000000000000,"G223528E59870N","2008-05-01T00:00:00",606914.766164303990081,0.606915000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223528E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.472738036516830,59.869676999999996]
["glac_bound",375715.000000000000000,"G229331E57479N","2008-05-01T00:00:00",76107.418168336225790,0.076107000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229331E57479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.668776653504892,57.479164499999996]
["glac_bound",375716.000000000000000,"G225998E59019N","2008-05-01T00:00:00",2144926.116503078490496,2.144930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225998E59019N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.988931150084113,59.023047500000004]
["glac_bound",375718.000000000000000,"G224431E59811N","2008-05-01T00:00:00",2794064.733922833111137,2.794060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224431E59811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.577180944437430,59.809965500000004]
["glac_bound",375723.000000000000000,"G230429E55492N","2008-05-01T00:00:00",184009.240569354384206,0.184009000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230429E55492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.568919516409380,55.491619999999998]
["glac_bound",375724.000000000000000,"G230056E55906N","2008-05-01T00:00:00",245938.664619645860512,0.245939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230056E55906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.944110009728320,55.906374000000000]
["glac_bound",375730.000000000000000,"G228026E57198N","2008-05-01T00:00:00",1688020.717949957121164,1.688020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228026E57198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.979403715055412,57.198307499999999]
["glac_bound",375731.000000000000000,"G230071E55927N","2008-05-01T00:00:00",456805.405486554431263,0.456805000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230071E55927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.930412121526899,55.927424500000001]
["glac_bound",375734.000000000000000,"G230861E56506N","2008-05-01T00:00:00",104487.916173381949193,0.104488000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230861E56506N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.140561282857163,56.507755000000003]
["glac_bound",375735.000000000000000,"G230562E54976N","2008-05-01T00:00:00",79838.165627056107041,0.079838000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230562E54976N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.436834484446990,54.975731499999995]
["glac_bound",375739.000000000000000,"G227918E57949N","2008-05-01T00:00:00",1032214.984503359999508,1.032210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227918E57949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.092168794391455,57.953693000000001]
["glac_bound",375740.000000000000000,"G230373E55666N","2008-05-01T00:00:00",663085.250260196626186,0.663085000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230373E55666N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.625428851212149,55.665887499999997]
["glac_bound",375745.000000000000000,"G228635E56640N","2008-05-01T00:00:00",361978.148008387710433,0.361978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228635E56640N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.365634912921337,56.643810999999999]
["glac_bound",375747.000000000000000,"G229915E56805N","2008-05-01T00:00:00",427588.578942740976345,0.427589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229915E56805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.089230113475196,56.803454000000002]
["glac_bound",375749.000000000000000,"G223027E59556N","2008-05-01T00:00:00",1713684.234957670792937,1.713680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223027E59556N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.973313174776308,59.562964500000000]
["glac_bound",375751.000000000000000,"G229007E56890N","2008-05-01T00:00:00",390250.107537478208542,0.390250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229007E56890N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.995534963636374,56.892688000000000]
["glac_bound",375752.000000000000000,"G230007E56292N","2008-05-01T00:00:00",3442416.349236003588885,3.442420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230007E56292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.975975741584705,56.290360999999997]
["glac_bound",375754.000000000000000,"G230658E55600N","2008-05-01T00:00:00",309370.582506779581308,0.309371000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230658E55600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.342719125641281,55.599954499999996]
["glac_bound",375757.000000000000000,"G228368E56680N","2008-05-01T00:00:00",327854.416569312277716,0.327854000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228368E56680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.630593657273380,56.679794999999999]
["glac_bound",375763.000000000000000,"G222401E59320N","2008-05-01T00:00:00",788952.916948022204451,0.788953000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222401E59320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.599047469926745,59.321811999999994]
["glac_bound",375769.000000000000000,"G229064E56614N","2008-05-01T00:00:00",497458.779945482092444,0.497459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229064E56614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.941210784282077,56.617045000000005]
["glac_bound",375775.000000000000000,"G229020E57256N","2008-05-01T00:00:00",466206.106077119999100,0.466206000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229020E57256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.985132152953042,57.255325999999997]
["glac_bound",375777.000000000000000,"G230169E57016N","2008-05-01T00:00:00",75311.131748113519279,0.075311000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230169E57016N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.831330507448797,57.016232000000002]
["glac_bound",375789.000000000000000,"G229399E57709N","2008-05-01T00:00:00",596294.935166766401380,0.596295000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229399E57709N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.602132489702001,57.709469499999997]
["glac_bound",375796.000000000000000,"G230444E54676N","2008-05-01T00:00:00",1020413.807875540223904,1.020410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230444E54676N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.559658674873958,54.678973999999997]
["glac_bound",375798.000000000000000,"G229165E57087N","2008-05-01T00:00:00",4028581.313692405354232,4.028580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229165E57087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.828860825010622,57.094122499999997]
["glac_bound",375802.000000000000000,"G230001E56248N","2008-05-01T00:00:00",1489567.445988044841215,4.040610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230001E56248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.005892000000017,56.248394500000003]
["glac_bound",375802.000000000000000,"G230001E56248N","2008-05-01T00:00:00",2551044.144610883668065,4.040610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230001E56248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.995385290763124,56.261254500000007]
["glac_bound",375806.000000000000000,"G230749E55307N","2008-05-01T00:00:00",54062.951121783036797,0.054063000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230749E55307N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.250337759264426,55.307091499999999]
["glac_bound",375813.000000000000000,"G230448E56635N","2008-05-01T00:00:00",2828300.656659560743719,2.828300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230448E56635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.546707994664331,56.634874500000002]
["glac_bound",375815.000000000000000,"G229325E56546N","2008-05-01T00:00:00",508626.916051897394937,0.508627000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229325E56546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.675405341147979,56.545086499999996]
["glac_bound",375820.000000000000000,"G230355E54900N","2008-05-01T00:00:00",133396.187317833100678,0.133396000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230355E54900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.643261215663586,54.900297999999999]
["glac_bound",375830.000000000000000,"G222178E59613N","2008-05-01T00:00:00",389085.984651709964965,0.389086000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222178E59613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.818700695606879,59.611611499999995]
["glac_bound",375832.000000000000000,"G228047E57290N","2008-05-01T00:00:00",2056987.418578786076978,2.056990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228047E57290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.955347537745268,57.292528000000004]
["glac_bound",375835.000000000000000,"G225381E59526N","2008-05-01T00:00:00",980962.701270637451671,0.980963000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225381E59526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.619295729376972,59.525580000000005]
["glac_bound",375837.000000000000000,"G228453E57110N","2008-05-01T00:00:00",294089.290141563280486,0.294089000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228453E57110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.546987108057294,57.110337000000001]
["glac_bound",375842.000000000000000,"G229615E57388N","2008-05-01T00:00:00",407151.205409198824782,0.407151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229615E57388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.382575370415651,57.388138499999997]
["glac_bound",375850.000000000000000,"G223291E59600N","2008-05-01T00:00:00",256186.239875368017238,0.256186000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223291E59600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.708054898613057,59.599552500000001]
["glac_bound",375853.000000000000000,"G230124E55619N","2008-05-01T00:00:00",132757.555796582717448,0.132758000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230124E55619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.875765774521682,55.618621000000005]
["glac_bound",375858.000000000000000,"G229489E56302N","2008-05-01T00:00:00",213686.477315879979869,0.213686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229489E56302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.510959220553815,56.301969499999998]
["glac_bound",375866.000000000000000,"G222037E59531N","2008-05-01T00:00:00",211454.062892714660848,0.211454000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222037E59531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.964526831455146,59.530502999999996]
["glac_bound",375868.000000000000000,"G228504E57453N","2008-05-01T00:00:00",85135.428990576212527,0.085135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228504E57453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.494170646551737,57.452750999999999]
["glac_bound",375873.000000000000000,"G223346E59283N","2008-05-01T00:00:00",62265.435015371389454,0.062265000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223346E59283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.652603916341462,59.283836000000001]
["glac_bound",375877.000000000000000,"G229139E56458N","2008-05-01T00:00:00",506064.428664331906475,0.506064000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229139E56458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.863567267576798,56.463870999999997]
["glac_bound",375879.000000000000000,"G230370E54908N","2008-05-01T00:00:00",63714.557098870100162,0.063715000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230370E54908N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.630639142999541,54.908064000000003]
["glac_bound",375883.000000000000000,"G230394E56041N","2008-05-01T00:00:00",6801445.439190645702183,6.801450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230394E56041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.596879744087488,56.052756000000002]
["glac_bound",375884.000000000000000,"G223323E59905N","2008-05-01T00:00:00",218904.499211236863630,0.218904000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223323E59905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.680620083045483,59.906628999999995]
["glac_bound",375885.000000000000000,"G227112E58359N","2008-05-01T00:00:00",3774646.362318668514490,3.774650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227112E58359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.879724985839118,58.368067999999994]
["glac_bound",375886.000000000000000,"G224958E59338N","2008-05-01T00:00:00",356232.961822043231223,0.356233000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224958E59338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.041267888006871,59.339726999999996]
["glac_bound",375888.000000000000000,"G228470E56766N","2008-05-01T00:00:00",452459.622166210610885,0.452460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228470E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.523342315609455,56.765284500000000]
["glac_bound",375892.000000000000000,"G222056E59952N","2008-05-01T00:00:00",1199219.382422089576721,1.199220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222056E59952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.943848770270279,59.951698000000000]
["glac_bound",375893.000000000000000,"G227643E57506N","2008-05-01T00:00:00",23698508.497538134455681,23.698499999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227643E57506N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.379897985478294,57.536523500000001]
["glac_bound",375895.000000000000000,"G225498E59285N","2008-05-01T00:00:00",2357515.147610643878579,2.357520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225498E59285N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.505636327681941,59.285623999999999]
["glac_bound",375897.000000000000000,"G228405E56885N","2008-05-01T00:00:00",11373598.821581771597266,11.373600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228405E56885N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.563921286639697,56.893943000000000]
["glac_bound",375901.000000000000000,"G230592E57032N","2008-05-01T00:00:00",1728488.919674990233034,1.728490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230592E57032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.402501256297711,57.033087999999999]
["glac_bound",375903.000000000000000,"G228478E57358N","2008-05-01T00:00:00",93643.512212258690852,0.093644000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228478E57358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.520774158006645,57.357555500000004]
["glac_bound",375909.000000000000000,"G230576E56707N","2008-05-01T00:00:00",123498.937576528231148,0.123499000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230576E56707N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.425256566877607,56.706203000000002]
["glac_bound",375916.000000000000000,"G226864E58404N","2008-05-01T00:00:00",128953.774968601646833,0.128954000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226864E58404N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.137021444794101,58.404717500000004]
["glac_bound",375917.000000000000000,"G227909E57212N","2008-05-01T00:00:00",2300663.819515576120466,2.300660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227909E57212N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.097475991038635,57.209284999999994]
["glac_bound",375919.000000000000000,"G225436E59349N","2008-05-01T00:00:00",435770.452991838625167,0.435770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225436E59349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.564382224706094,59.348657500000002]
["glac_bound",375924.000000000000000,"G226273E59018N","2008-05-01T00:00:00",525649.170265462831594,0.525649000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226273E59018N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.726421112873140,59.018225999999999]
["glac_bound",375927.000000000000000,"G224963E59359N","2008-05-01T00:00:00",268207.011124796175864,0.268207000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224963E59359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.035240564605033,59.360135499999998]
["glac_bound",375928.000000000000000,"G222423E59696N","2008-05-01T00:00:00",342936.737936019839253,0.342937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222423E59696N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.576465893280556,59.695689500000000]
["glac_bound",375930.000000000000000,"G226817E58519N","2008-05-01T00:00:00",1912544.005058152601123,1.912540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226817E58519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.183635533103143,58.526800999999999]
["glac_bound",375933.000000000000000,"G228896E57359N","2008-05-01T00:00:00",659581.918056591181085,0.659582000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228896E57359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.105255518163915,57.358727999999999]
["glac_bound",375935.000000000000000,"G224677E59871N","2008-05-01T00:00:00",126796.478510470973561,0.126796000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224677E59871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.321591203103225,59.871030500000003]
["glac_bound",375940.000000000000000,"G230877E54949N","2008-05-01T00:00:00",877397.258718744269572,0.877397000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230877E54949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.124056252164223,54.950632499999998]
["glac_bound",375943.000000000000000,"G229325E56930N","2008-05-01T00:00:00",110190.790578524043667,0.110191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229325E56930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.673152279954593,56.930833999999997]
["glac_bound",375948.000000000000000,"G228634E56533N","2008-05-01T00:00:00",288950.907741930917837,0.288951000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228634E56533N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.366408586734678,56.533979000000002]
["glac_bound",375954.000000000000000,"G230004E56727N","2008-05-01T00:00:00",793934.018924289382994,0.793934000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230004E56727N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.998080669586699,56.727524000000003]
["glac_bound",375955.000000000000000,"G230293E54747N","2008-05-01T00:00:00",176496.241313914710190,0.176496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230293E54747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.706432817159538,54.746442999999999]
["glac_bound",375957.000000000000000,"G228616E56541N","2008-05-01T00:00:00",2996821.299226434435695,2.996820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228616E56541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.388327211904652,56.544414000000003]
["glac_bound",375960.000000000000000,"G230094E55913N","2008-05-01T00:00:00",70527.603097319341032,0.070528000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230094E55913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.904767115160439,55.913276999999994]
["glac_bound",375968.000000000000000,"G222713E59645N","2008-05-01T00:00:00",658690.517331769107841,0.658691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222713E59645N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.289031922183511,59.646474499999997]
["glac_bound",375969.000000000000000,"G231156E55294N","2008-05-01T00:00:00",79182.008483881916618,0.079182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231156E55294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.844103601907193,55.293778000000003]
["glac_bound",375980.000000000000000,"G230102E57442N","2008-05-01T00:00:00",59393.134053561007022,0.059393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230102E57442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.898603410457213,57.441637499999999]
["glac_bound",375983.000000000000000,"G227916E57502N","2008-05-01T00:00:00",460413.737603990070056,0.460414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227916E57502N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.082579322809181,57.502742499999997]
["glac_bound",375986.000000000000000,"G229400E56376N","2008-05-01T00:00:00",3658178.847674110438675,3.658180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229400E56376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.584573326394406,56.382361500000002]
["glac_bound",375990.000000000000000,"G225688E59122N","2008-05-01T00:00:00",19205736.596006128937006,19.205700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225688E59122N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.317352477471303,59.117091500000001]
["glac_bound",375991.000000000000000,"G228340E57408N","2008-05-01T00:00:00",100436.542782472315594,0.100437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228340E57408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.660693249697943,57.408282499999999]
["glac_bound",376001.000000000000000,"G223847E59914N","2008-05-01T00:00:00",1640641.280635080765933,1.640640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223847E59914N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.151728574940051,59.915838000000001]
["glac_bound",376014.000000000000000,"G229562E56315N","2008-05-01T00:00:00",1402217.604380844160914,1.402220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229562E56315N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.437545620967740,56.314159000000004]
["glac_bound",376017.000000000000000,"G228528E57178N","2008-05-01T00:00:00",819589.032302223495208,0.819589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228528E57178N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.475023735799994,57.179181999999997]
["glac_bound",376020.000000000000000,"G228803E56490N","2008-05-01T00:00:00",122715.515208528231597,0.122716000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228803E56490N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.196870561418450,56.489356999999998]
["glac_bound",376034.000000000000000,"G227879E57073N","2008-05-01T00:00:00",56097.348934969530092,0.056097000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227879E57073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.120622436254962,57.072965499999995]
["glac_bound",376039.000000000000000,"G223020E59332N","2008-05-01T00:00:00",172973.820446804485982,0.172974000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223020E59332N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.980240442918927,59.332311500000003]
["glac_bound",376042.000000000000000,"G228578E57551N","2008-05-01T00:00:00",168201.705186357896309,0.168202000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228578E57551N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.421831648106490,57.551076999999999]
["glac_bound",376049.000000000000000,"G223240E59571N","2008-05-01T00:00:00",245365.638808887684718,0.245366000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223240E59571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.760099914044076,59.571606500000001]
["glac_bound",376052.000000000000000,"G226633E58473N","2008-05-01T00:00:00",362380.153838223137427,0.362380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226633E58473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.369638066241492,58.472352000000001]
["glac_bound",376057.000000000000000,"G224750E59783N","2008-05-01T00:00:00",995705.111751092714258,0.995705000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224750E59783N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.253488136363615,59.785201999999998]
["glac_bound",376058.000000000000000,"G229134E56516N","2008-05-01T00:00:00",10326725.798237673938274,10.326700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229134E56516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.899383747027798,56.524484999999999]
["glac_bound",376059.000000000000000,"G225781E58984N","2008-05-01T00:00:00",439422239.78801137208938,439.422000000000025,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Llewellyn Glacier","None","09AA225781E58984N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.120492580742138,58.999763999999999]
["glac_bound",376061.000000000000000,"G230530E57055N","2008-05-01T00:00:00",269000.536363422812428,0.269001000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230530E57055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.469176863382899,57.054910000000000]
["glac_bound",376064.000000000000000,"G227098E58292N","2008-05-01T00:00:00",575065.045490209478885,0.575065000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227098E58292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.902513941242347,58.298220999999998]
["glac_bound",376065.000000000000000,"G230634E55626N","2008-05-01T00:00:00",459988.143741064355709,0.459988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230634E55626N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.365252346663510,55.626854999999999]
["glac_bound",376066.000000000000000,"G229927E57017N","2008-05-01T00:00:00",438380.290038347535301,0.438380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229927E57017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.072386025316462,57.016979500000005]
["glac_bound",376068.000000000000000,"G229929E57011N","2008-05-01T00:00:00",67305.179153414021130,0.067305000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229929E57011N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.071364835422941,57.010482499999995]
["glac_bound",376071.000000000000000,"G227751E57783N","2008-05-01T00:00:00",361539.366083481581882,0.361539000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227751E57783N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.249938659405245,57.783562500000002]
["glac_bound",376073.000000000000000,"G224024E59994N","2008-05-01T00:00:00",269530.075978257285897,0.269530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224024E59994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.975773042768964,59.994013499999994]
["glac_bound",376074.000000000000000,"G230269E56214N","2008-05-01T00:00:00",635757.908876900211908,0.635758000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230269E56214N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.730427858934632,56.212401000000000]
["glac_bound",376076.000000000000000,"G229831E56609N","2008-05-01T00:00:00",1462072.729755404870957,1.462070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229831E56609N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.159364559587175,56.607855000000001]
["glac_bound",376078.000000000000000,"G226208E58672N","2008-05-01T00:00:00",81351.685207925926079,0.081352000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226208E58672N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.791416861880407,58.671394500000005]
["glac_bound",376081.000000000000000,"G227911E57050N","2008-05-01T00:00:00",25027.090675833227579,0.025027000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227911E57050N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.088499605351387,57.049191999999998]
["glac_bound",376085.000000000000000,"G228922E57197N","2008-05-01T00:00:00",224334.979934080241947,0.224335000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228922E57197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.079146478202432,57.197277000000000]
["glac_bound",376089.000000000000000,"G230594E56733N","2008-05-01T00:00:00",872563.960232782759704,0.872564000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230594E56733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.404358790021888,56.735629500000002]
["glac_bound",376090.000000000000000,"G229988E56154N","2008-05-01T00:00:00",1204447.208510741824284,1.204450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229988E56154N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.010777816746781,56.159111500000002]
["glac_bound",376100.000000000000000,"G228082E58055N","2008-05-01T00:00:00",129286.409202781738713,0.129286000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228082E58055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.918565951252219,58.054689499999995]
["glac_bound",376101.000000000000000,"G227816E57527N","2008-05-01T00:00:00",718473.089632436749525,0.718473000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227816E57527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.185409419329062,57.526194500000003]
["glac_bound",376104.000000000000000,"G222826E59510N","2008-05-01T00:00:00",380571.003923871496227,0.380571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222826E59510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.175979783707021,59.509301500000007]
["glac_bound",376105.000000000000000,"G228797E57019N","2008-05-01T00:00:00",71035.765125020872802,0.071036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228797E57019N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.203557243243267,57.018778499999996]
["glac_bound",376106.000000000000000,"G227002E57897N","2008-05-01T00:00:00",116006.727012880190159,0.116007000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227002E57897N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.998243581341626,57.895851000000000]
["glac_bound",376109.000000000000000,"G227971E57365N","2008-05-01T00:00:00",167988.463349160971120,0.167988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227971E57365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.029339899629747,57.369176499999995]
["glac_bound",376112.000000000000000,"G226306E58741N","2008-05-01T00:00:00",372441.649782473454252,0.372442000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226306E58741N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.692647420169834,58.741502500000003]
["glac_bound",376119.000000000000000,"G230467E57069N","2008-05-01T00:00:00",345532.887212632515002,0.345533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230467E57069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.531336441770350,57.068486000000000]
["glac_bound",376120.000000000000000,"G229763E56419N","2008-05-01T00:00:00",254835.599389662500471,0.254836000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229763E56419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.244233087797852,56.418553500000002]
["glac_bound",376124.000000000000000,"G229378E57444N","2008-05-01T00:00:00",139850.334512476489181,0.139850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229378E57444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.621935525897300,57.443632000000001]
["glac_bound",376126.000000000000000,"G227851E57403N","2008-05-01T00:00:00",95633.890875735742156,0.095634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227851E57403N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.150270807692323,57.402339999999995]
["glac_bound",376127.000000000000000,"G226779E58218N","2008-05-01T00:00:00",692625.718552016187459,0.692626000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226779E58218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.221529550291052,58.218229000000001]
["glac_bound",376128.000000000000000,"G229250E56524N","2008-05-01T00:00:00",85708.534378778655082,0.085709000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229250E56524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.750954429386070,56.522447499999998]
["glac_bound",376129.000000000000000,"G222202E59668N","2008-05-01T00:00:00",114731.400774895519135,0.114731000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222202E59668N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.797578105056033,59.668670499999998]
["glac_bound",376130.000000000000000,"G230540E54909N","2008-05-01T00:00:00",134536.427633988932939,0.134536000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230540E54909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.460083448912229,54.909151000000001]
["glac_bound",376134.000000000000000,"G222703E59456N","2008-05-01T00:00:00",1002352.332189489272423,1.002350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222703E59456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.294489111111091,59.455090499999997]
["glac_bound",376141.000000000000000,"G228487E57433N","2008-05-01T00:00:00",2749796.207127826288342,2.749800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228487E57433N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.516430126343494,57.437114500000000]
["glac_bound",376142.000000000000000,"G230051E56128N","2008-05-01T00:00:00",482602.682191523141228,0.482603000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230051E56128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.949217173759592,56.127616000000003]
["glac_bound",376149.000000000000000,"G230680E55638N","2008-05-01T00:00:00",1132563.731247775489464,1.132560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230680E55638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.326198845000192,55.640686500000001]
["glac_bound",376155.000000000000000,"G224270E59854N","2008-05-01T00:00:00",188887.307078341284068,0.188887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224270E59854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.729312734247969,59.854335500000005]
["glac_bound",376161.000000000000000,"G222709E58921N","2008-05-01T00:00:00",1365943.098049123072997,113.760999999999996,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Margerie Glacier","None","08BF222811E59020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.188266971358075,59.021019500000001]
["glac_bound",376161.000000000000000,"G222709E58921N","2008-05-01T00:00:00",112395490.09958156943321,113.760999999999996,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Margerie Glacier","None","08BF222811E59020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.133992614079204,58.962247000000005]
["glac_bound",376167.000000000000000,"G227324E58430N","2008-05-01T00:00:00",727345.810784666682594,0.727346000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227324E58430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.680297713878986,58.432345499999997]
["glac_bound",376169.000000000000000,"G228729E57208N","2008-05-01T00:00:00",760169.228948127711192,0.760169000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228729E57208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.271325518358481,57.208694500000000]
["glac_bound",376176.000000000000000,"G228690E57075N","2008-05-01T00:00:00",698001.242370814317837,0.698001000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228690E57075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.309216949660765,57.073325499999996]
["glac_bound",376186.000000000000000,"G230147E56203N","2008-05-01T00:00:00",109766.911630117290770,0.109767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230147E56203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.853096718135134,56.202128999999999]
["glac_bound",376192.000000000000000,"G230851E57267N","2008-05-01T00:00:00",660911.746805742499419,0.660912000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230851E57267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.149985882818441,57.266501500000004]
["glac_bound",376196.000000000000000,"G230065E56448N","2008-05-01T00:00:00",290541.074412746645976,0.290541000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230065E56448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.934934867647058,56.447499000000001]
["glac_bound",376197.000000000000000,"G222235E59922N","2008-05-01T00:00:00",1536151.608856706647202,1.536150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222235E59922N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.767790914149884,59.923067000000003]
["glac_bound",376198.000000000000000,"G225295E59405N","2008-05-01T00:00:00",281751.551289318769705,0.281752000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225295E59405N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.701792860114779,59.404618999999997]
["glac_bound",376199.000000000000000,"G222638E59655N","2008-05-01T00:00:00",3042286.912180254701525,3.042290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222638E59655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.364239459049202,59.662072500000001]
["glac_bound",376205.000000000000000,"G230156E56628N","2008-05-01T00:00:00",77966.687648702732986,0.077967000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230156E56628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.842989181093884,56.628056500000000]
["glac_bound",376206.000000000000000,"G225813E59124N","2008-05-01T00:00:00",300572.047516552207526,0.300572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225813E59124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.187984444962808,59.125085999999996]
["glac_bound",376208.000000000000000,"G229828E56836N","2008-05-01T00:00:00",694867.654627250740305,0.694868000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229828E56836N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.170654057522768,56.836623500000002]
["glac_bound",376209.000000000000000,"G227122E58313N","2008-05-01T00:00:00",691382.761005410458893,0.691383000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227122E58313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.885777961423827,58.316122500000006]
["glac_bound",376215.000000000000000,"G228139E56901N","2008-05-01T00:00:00",51382.758930329458963,0.051383000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228139E56901N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.863228022025339,56.902259500000000]
["glac_bound",376216.000000000000000,"G229432E57199N","2008-05-01T00:00:00",639813.014067279407755,0.639813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229432E57199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.567331269321471,57.202711499999999]
["glac_bound",376243.000000000000000,"G228315E57199N","2008-05-01T00:00:00",102559.886821459804196,0.102560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228315E57199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.685106657894721,57.199432500000000]
["glac_bound",376252.000000000000000,"G229304E57361N","2008-05-01T00:00:00",115900.434872233105125,0.115900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229304E57361N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.696510254401858,57.360473499999998]
["glac_bound",376258.000000000000000,"G229400E56298N","2008-05-01T00:00:00",682793.136534507269971,0.682793000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229400E56298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.597055030000007,56.298575999999997]
["glac_bound",376259.000000000000000,"G225543E59225N","2008-05-01T00:00:00",56390.118348195348517,0.056390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225543E59225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.458365191752705,59.224870499999994]
["glac_bound",376266.000000000000000,"G229812E57779N","2008-05-01T00:00:00",170701.078058784012683,0.170701000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229812E57779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.188434704183265,57.779508000000000]
["glac_bound",376267.000000000000000,"G225583E59376N","2008-05-01T00:00:00",1030660.454999950714409,1.030660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225583E59376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.411544651119414,59.374344999999998]
["glac_bound",376274.000000000000000,"G227495E58181N","2008-05-01T00:00:00",752121.026293566799723,0.752121000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227495E58181N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.500539882840229,58.180191500000006]
["glac_bound",376277.000000000000000,"G225431E59453N","2008-05-01T00:00:00",76340.627546839983552,0.076341000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225431E59453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.569166952283950,59.453767999999997]
["glac_bound",376289.000000000000000,"G229976E56205N","2008-05-01T00:00:00",195885.091878624283709,0.195885000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229976E56205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.025641110132142,56.206522000000000]
["glac_bound",376292.000000000000000,"G230675E56828N","2008-05-01T00:00:00",438266.341509759600740,0.438266000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230675E56828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.325278659377517,56.828609999999998]
["glac_bound",376295.000000000000000,"G230714E56463N","2008-05-01T00:00:00",277562.400573434191756,0.277562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230714E56463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.285119498680729,56.463306000000003]
["glac_bound",376306.000000000000000,"G230698E54885N","2008-05-01T00:00:00",4508456.893628476187587,4.508460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230698E54885N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.316773369323414,54.889180499999995]
["glac_bound",376307.000000000000000,"G227107E58321N","2008-05-01T00:00:00",325475.948571068234742,0.325476000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227107E58321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.891740527146908,58.319948500000002]
["glac_bound",376308.000000000000000,"G222925E59313N","2008-05-01T00:00:00",55579.241590413839731,0.055579000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222925E59313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.075540904424543,59.312854500000000]
["glac_bound",376309.000000000000000,"G230451E57106N","2008-05-01T00:00:00",611566.813574219238944,0.611567000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230451E57106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.550066052490934,57.106040499999999]
["glac_bound",376310.000000000000000,"G226888E58308N","2008-05-01T00:00:00",224494.148765946069034,0.224494000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226888E58308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.112442885191456,58.307372500000000]
["glac_bound",376314.000000000000000,"G223259E59474N","2008-05-01T00:00:00",530016.098425169126131,0.530016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223259E59474N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.740558907600501,59.478628999999998]
["glac_bound",376315.000000000000000,"G229454E56381N","2008-05-01T00:00:00",1504874.613828520057723,1.504870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229454E56381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.546901932523667,56.383877499999997]
["glac_bound",376317.000000000000000,"G227302E58091N","2008-05-01T00:00:00",4285226.358382759615779,4.285230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227302E58091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.682390176769786,58.093719000000000]
["glac_bound",376321.000000000000000,"G227361E58140N","2008-05-01T00:00:00",272113.952780632243957,0.272114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227361E58140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.637183010997660,58.140941999999995]
["glac_bound",376330.000000000000000,"G221634E59954N","2008-05-01T00:00:00",1109043.720661750528961,1.109040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221634E59954N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.367147312500009,59.955084499999998]
["glac_bound",376342.000000000000000,"G225526E59568N","2008-05-01T00:00:00",88406.684430618057377,0.088407000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225526E59568N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.470664987722301,59.566214000000002]
["glac_bound",376343.000000000000000,"G231237E57532N","2008-05-01T00:00:00",1174446.748834720347077,1.174450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231237E57532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.763096567058653,57.531300500000000]
["glac_bound",376345.000000000000000,"G223323E59590N","2008-05-01T00:00:00",203255.733325292996597,0.203256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223323E59590N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.674401019807192,59.591457500000004]
["glac_bound",376347.000000000000000,"G225349E59867N","2008-05-01T00:00:00",54338.648807938669052,0.054339000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225349E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.650707395217353,59.866888500000002]
["glac_bound",376362.000000000000000,"G230434E56275N","2008-05-01T00:00:00",220806.866663903492736,0.220807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230434E56275N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.566744536140959,56.274580499999999]
["glac_bound",376367.000000000000000,"G228733E57486N","2008-05-01T00:00:00",312750.838964043592568,0.312751000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228733E57486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.266638188490788,57.485951999999997]
["glac_bound",376371.000000000000000,"G226996E58415N","2008-05-01T00:00:00",624855.327011440414935,0.624855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226996E58415N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.001696808685438,58.414284500000001]
["glac_bound",376372.000000000000000,"G228968E57197N","2008-05-01T00:00:00",4567558.754366473294795,4.567560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228968E57197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.037179009823518,57.199346000000006]
["glac_bound",376373.000000000000000,"G226313E59013N","2008-05-01T00:00:00",241237.281922903028317,0.241237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226313E59013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.687184055532100,59.014251500000000]
["glac_bound",376378.000000000000000,"G230548E56253N","2008-05-01T00:00:00",213861.137379273917759,0.213861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230548E56253N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.453313326268017,56.254214500000003]
["glac_bound",376381.000000000000000,"G222693E58950N","2008-05-01T00:00:00",38620.209955670296040,0.038620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222693E58950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.306467417220404,58.950558500000000]
["glac_bound",376383.000000000000000,"G221438E59744N","2008-05-01T00:00:00",2668012.955914173740894,2.668010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221438E59744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.558037048860967,59.740731500000003]
["glac_bound",376396.000000000000000,"G222864E59373N","2008-05-01T00:00:00",53124.865148075397883,0.053125000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222864E59373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.136518683365296,59.373060500000001]
["glac_bound",376397.000000000000000,"G222395E59746N","2008-05-01T00:00:00",925309.253219947800972,0.925309000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222395E59746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.606118690513199,59.749987500000003]
["glac_bound",376400.000000000000000,"G230566E57065N","2008-05-01T00:00:00",2069137.347981681115925,2.069140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230566E57065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.437800318784156,57.063508499999998]
["glac_bound",376404.000000000000000,"G223879E59748N","2008-05-01T00:00:00",308043.990034959279001,0.308044000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223879E59748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.116665255668067,59.747800499999997]
["glac_bound",376405.000000000000000,"G223300E59710N","2008-05-01T00:00:00",4814394.130988564342260,4.814390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223300E59710N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.706775966441967,59.712182499999997]
["glac_bound",376417.000000000000000,"G228349E57218N","2008-05-01T00:00:00",202411.958052292582579,0.202412000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228349E57218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.650933150565407,57.217888500000001]
["glac_bound",376418.000000000000000,"G229668E56277N","2008-05-01T00:00:00",10630403.254205156117678,10.630400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229668E56277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.328228458333342,56.288086499999999]
["glac_bound",376422.000000000000000,"G227279E58424N","2008-05-01T00:00:00",217932.059654563869117,0.217932000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227279E58424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.721691115548026,58.424953000000002]
["glac_bound",376425.000000000000000,"G230309E56044N","2008-05-01T00:00:00",35625416.073133200407028,35.625399999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230309E56044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.687940275754272,56.056752500000002]
["glac_bound",376426.000000000000000,"G227398E57793N","2008-05-01T00:00:00",179671.379094303527381,0.179671000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227398E57793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.602392284130275,57.793765000000000]
["glac_bound",376429.000000000000000,"G230515E56013N","2008-05-01T00:00:00",89174.433703194081318,0.089174000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230515E56013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.486237425512115,56.012595500000003]
["glac_bound",376435.000000000000000,"G229578E57197N","2008-05-01T00:00:00",389844.517026673071086,0.389845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229578E57197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.423225921787719,57.197080999999997]
["glac_bound",376437.000000000000000,"G223141E59455N","2008-05-01T00:00:00",221214.580741262965603,0.221215000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223141E59455N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.859658424578868,59.455182499999999]
["glac_bound",376438.000000000000000,"G230204E56235N","2008-05-01T00:00:00",485700.808319480682258,0.485701000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230204E56235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.800301920391064,56.239986000000002]
["glac_bound",376442.000000000000000,"G225693E59282N","2008-05-01T00:00:00",63372.090543572769093,0.063372000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225693E59282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.308274758272034,59.282416499999997]
["glac_bound",376445.000000000000000,"G230056E56081N","2008-05-01T00:00:00",215211.931683138100198,0.215212000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230056E56081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.946242887341782,56.081980000000001]
["glac_bound",376446.000000000000000,"G227448E58309N","2008-05-01T00:00:00",3309121.433515956625342,3.306220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227448E58309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.545541159556763,58.320054499999998]
["glac_bound",376448.000000000000000,"G227738E57739N","2008-05-01T00:00:00",145976.455463324877201,0.145976000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227738E57739N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.258881951648334,57.739339999999999]
["glac_bound",376459.000000000000000,"G229295E56467N","2008-05-01T00:00:00",88301.729384165257215,0.088302000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229295E56467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.703000408130379,56.464910500000002]
["glac_bound",376460.000000000000000,"G226640E58549N","2008-05-01T00:00:00",940247.523556884611025,0.940248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226640E58549N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.354573552861382,58.552847499999999]
["glac_bound",376461.000000000000000,"G227954E57970N","2008-05-01T00:00:00",2881902.227136086672544,2.881900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227954E57970N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.035914473812738,57.973584500000001]
["glac_bound",376462.000000000000000,"G227436E58284N","2008-05-01T00:00:00",191291.435962193470914,0.191291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227436E58284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.565027302816901,58.283069999999995]
["glac_bound",376465.000000000000000,"G230416E55554N","2008-05-01T00:00:00",110814.053365193714853,0.110814000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230416E55554N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.585776856617656,55.552902500000002]
["glac_bound",376468.000000000000000,"G225353E59325N","2008-05-01T00:00:00",88204.197520844725659,0.088204000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225353E59325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.648930205390712,59.325542499999997]
["glac_bound",376469.000000000000000,"G230534E55916N","2008-05-01T00:00:00",88586.646412257134216,0.088587000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230534E55916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.465355976745570,55.915827000000000]
["glac_bound",376471.000000000000000,"G227472E58364N","2008-05-01T00:00:00",1354280.234354967484251,1.354280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227472E58364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.536903956468052,58.369565500000000]
["glac_bound",376472.000000000000000,"G230093E55823N","2008-05-01T00:00:00",1039884.848134901956655,1.039880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230093E55823N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.917515124927775,55.825094499999999]
["glac_bound",376478.000000000000000,"G225127E59465N","2008-05-01T00:00:00",173581.383329622243764,0.173581000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225127E59465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.873489984353967,59.464682499999995]
["glac_bound",376484.000000000000000,"G222178E59397N","2008-05-01T00:00:00",603380.805403899983503,0.603381000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222178E59397N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.823028945092801,59.397408999999996]
["glac_bound",376486.000000000000000,"G223694E59581N","2008-05-01T00:00:00",183193.968285076698521,0.183194000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223694E59581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.307215883946668,59.581267500000003]
["glac_bound",376497.000000000000000,"G223642E59745N","2008-05-01T00:00:00",1605324.324626070214435,1.605320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223642E59745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.360969632401407,59.745801000000000]
["glac_bound",376499.000000000000000,"G230033E55799N","2008-05-01T00:00:00",304702.280214618658647,0.304702000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230033E55799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.964118550842670,55.802591500000005]
["glac_bound",376506.000000000000000,"G225101E59596N","2008-05-01T00:00:00",328979.300733662676066,0.328979000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225101E59596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.900602438136843,59.596758000000001]
["glac_bound",376507.000000000000000,"G224976E59572N","2008-05-01T00:00:00",843972.666322410455905,0.843973000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224976E59572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.023335343172505,59.572657500000005]
["glac_bound",376521.000000000000000,"G229665E56575N","2008-05-01T00:00:00",292492.875539937173016,0.292493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229665E56575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.333751176863359,56.575274499999999]
["glac_bound",376524.000000000000000,"G228097E57103N","2008-05-01T00:00:00",676368.987828438170254,0.676369000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228097E57103N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.904603817763729,57.103546499999993]
["glac_bound",376525.000000000000000,"G222002E59536N","2008-05-01T00:00:00",2531825.030306408647448,2.531830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222002E59536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.002681745842779,59.534583999999995]
["glac_bound",376526.000000000000000,"G230294E56296N","2008-05-01T00:00:00",62273.027277058674372,0.062273000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230294E56296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.706902714078637,56.296158500000004]
["glac_bound",376529.000000000000000,"G230418E56652N","2008-05-01T00:00:00",319159.663436161936261,0.319160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230418E56652N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.587136184993824,56.654099500000001]
["glac_bound",376530.000000000000000,"G227435E57842N","2008-05-01T00:00:00",50980.928310288436478,0.050981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227435E57842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.565705472742422,57.842165000000001]
["glac_bound",376531.000000000000000,"G228470E57322N","2008-05-01T00:00:00",196828.403112366766436,0.196828000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228470E57322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.530093988472629,57.322342499999998]
["glac_bound",376532.000000000000000,"G229015E57141N","2008-05-01T00:00:00",11251553.736289022490382,11.251600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229015E57141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.969817567242103,57.155738499999998]
["glac_bound",376535.000000000000000,"G230107E57442N","2008-05-01T00:00:00",127551.955948338465532,0.127552000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230107E57442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.892813124302961,57.442815499999995]
["glac_bound",376536.000000000000000,"G230350E56682N","2008-05-01T00:00:00",85276.803568926159642,0.085277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230350E56682N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.652241998440616,56.682769499999999]
["glac_bound",376539.000000000000000,"G230665E55594N","2008-05-01T00:00:00",654699.719835598254576,0.654700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230665E55594N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.334186263855003,55.594088499999998]
["glac_bound",376546.000000000000000,"G230477E56375N","2008-05-01T00:00:00",379341.805989353510085,0.379342000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230477E56375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.525297310140644,56.376131500000000]
["glac_bound",376552.000000000000000,"G226875E58489N","2008-05-01T00:00:00",161631.189610368222930,0.161631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226875E58489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.123541576446286,58.488703999999998]
["glac_bound",376555.000000000000000,"G230432E56374N","2008-05-01T00:00:00",807448.683917047572322,0.807449000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230432E56374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.572719570981690,56.377403999999999]
["glac_bound",376557.000000000000000,"G228041E56981N","2008-05-01T00:00:00",39796616.873969785869122,39.796599999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228041E56981N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.911737505076815,57.007818000000000]
["glac_bound",376558.000000000000000,"G230117E56435N","2008-05-01T00:00:00",67125.463298281058087,0.067126000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230117E56435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.882837092917498,56.435193499999997]
["glac_bound",376561.000000000000000,"G230825E57116N","2008-05-01T00:00:00",1557283.698474698001519,1.557280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230825E57116N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.182257770719616,57.118053000000003]
["glac_bound",376562.000000000000000,"G229582E57187N","2008-05-01T00:00:00",1048717.874247677158564,1.048720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229582E57187N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.421108994496194,57.186218499999995]
["glac_bound",376567.000000000000000,"G228310E57474N","2008-05-01T00:00:00",108920.345304409667733,0.108920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228310E57474N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.691096549881138,57.474761500000000]
["glac_bound",376581.000000000000000,"G222710E59107N","2008-05-01T00:00:00",247272.887421521794749,0.247273000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222710E59107N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.290315334312652,59.106009499999999]
["glac_bound",376582.000000000000000,"G228798E57394N","2008-05-01T00:00:00",85554.791093707157415,0.085555000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228798E57394N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.202783353625534,57.394084499999998]
["glac_bound",376591.000000000000000,"G231218E57373N","2008-05-01T00:00:00",136371.570730768493377,0.136372000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231218E57373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.781878376752559,57.372692499999999]
["glac_bound",376592.000000000000000,"G228768E57345N","2008-05-01T00:00:00",65760.790237783978228,0.065761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228768E57345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.229641259848478,57.345596499999999]
["glac_bound",376593.000000000000000,"G226571E58378N","2008-05-01T00:00:00",544301.204911262146197,0.544301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226571E58378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.428671822974536,58.377704000000001]
["glac_bound",376596.000000000000000,"G228333E56780N","2008-05-01T00:00:00",114567.589191568593378,0.114568000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228333E56780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.664730158669272,56.779462000000002]
["glac_bound",376597.000000000000000,"G229817E56590N","2008-05-01T00:00:00",1323876.864939416293055,1.323880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229817E56590N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.188065991992801,56.587493499999994]
["glac_bound",376604.000000000000000,"G229230E57041N","2008-05-01T00:00:00",2686859.360545148141682,2.686860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229230E57041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.766266759040946,57.046396000000001]
["glac_bound",376606.000000000000000,"G230322E56484N","2008-05-01T00:00:00",846755.748724561068229,0.846756000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230322E56484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.674251104580208,56.483749000000003]
["glac_bound",376610.000000000000000,"G225536E59250N","2008-05-01T00:00:00",3971477.599447765853256,3.971480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225536E59250N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.469623000000013,59.255240000000001]
["glac_bound",376611.000000000000000,"G229406E57477N","2008-05-01T00:00:00",165445.889319440640975,0.165446000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229406E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.593589745972167,57.476579000000001]
["glac_bound",376615.000000000000000,"G228381E57372N","2008-05-01T00:00:00",255468.113360793184256,0.255468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228381E57372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.619128504901994,57.371007000000006]
["glac_bound",376617.000000000000000,"G226677E58330N","2008-05-01T00:00:00",18277933.102643925696611,18.277899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Speel Glacier","None","08BC226677E58330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.318198470762525,58.334045500000002]
["glac_bound",376619.000000000000000,"G229848E56305N","2008-05-01T00:00:00",269392.892795499879867,0.269393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229848E56305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.153332125873106,56.305953500000001]
["glac_bound",376621.000000000000000,"G228722E56653N","2008-05-01T00:00:00",170254.447783470386639,0.170254000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228722E56653N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.277011354041520,56.653503999999998]
["glac_bound",376624.000000000000000,"G222355E59512N","2008-05-01T00:00:00",5346870.513024289160967,5.346870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222355E59512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.652863119034009,59.522453999999996]
["glac_bound",376635.000000000000000,"G227188E58244N","2008-05-01T00:00:00",309901.037074581254274,0.309901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227188E58244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.812721427647546,58.242407000000000]
["glac_bound",376636.000000000000000,"G226553E58567N","2008-05-01T00:00:00",3066953.480953525751829,3.066950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226553E58567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.442427890305453,58.573887999999997]
["glac_bound",376639.000000000000000,"G230417E55675N","2008-05-01T00:00:00",1409258.368493658956140,1.409260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230417E55675N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.583215190979672,55.674677000000003]
["glac_bound",376643.000000000000000,"G228838E57361N","2008-05-01T00:00:00",98074.473061931712436,0.098074000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228838E57361N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.162674643745135,57.360495000000000]
["glac_bound",376646.000000000000000,"G225256E59475N","2008-05-01T00:00:00",91702.951542524373508,0.091703000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225256E59475N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.743544418381475,59.475061999999994]
["glac_bound",376648.000000000000000,"G230230E57303N","2008-05-01T00:00:00",212898.693468145094812,0.212899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230230E57303N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.773599087287209,57.303446500000000]
["glac_bound",376653.000000000000000,"G230401E57324N","2008-05-01T00:00:00",112033.675035860986100,0.112034000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230401E57324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.599492915601502,57.323952500000004]
["glac_bound",376654.000000000000000,"G230523E54649N","2008-05-01T00:00:00",1518852.016235038405284,1.518850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230523E54649N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.479191302351609,54.647428000000005]
["glac_bound",376658.000000000000000,"G230460E55941N","2008-05-01T00:00:00",58589.534284186309378,0.058590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230460E55941N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.539745076597967,55.941212499999999]
["glac_bound",376663.000000000000000,"G227165E58534N","2008-05-01T00:00:00",126538.712667432933813,0.126539000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227165E58534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.835055218164769,58.534886999999998]
["glac_bound",376671.000000000000000,"G222875E59420N","2008-05-01T00:00:00",13727193.721527131274343,13.727200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222875E59420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.128251919621704,59.425680499999999]
["glac_bound",376673.000000000000000,"G227514E58198N","2008-05-01T00:00:00",317009.908697027422022,0.317010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227514E58198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.485371623463521,58.197963000000001]
["glac_bound",376677.000000000000000,"G229040E57331N","2008-05-01T00:00:00",457021.518767407920677,0.457022000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229040E57331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.959808545220483,57.331078000000005]
["glac_bound",376679.000000000000000,"G230585E55627N","2008-05-01T00:00:00",1736957.296818826347589,1.736960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230585E55627N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.411969383539201,55.634582500000000]
["glac_bound",376680.000000000000000,"G230353E57308N","2008-05-01T00:00:00",186672.746626812353497,0.186673000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230353E57308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.646396126393256,57.308529000000000]
["glac_bound",376686.000000000000000,"G229163E57050N","2008-05-01T00:00:00",2278799.481269985903054,2.278800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229163E57050N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.840854362979201,57.050107999999994]
["glac_bound",376687.000000000000000,"G222557E59014N","2008-05-01T00:00:00",275170.062237493635621,0.275170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222557E59014N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.438749844866095,59.014180500000002]
["glac_bound",376690.000000000000000,"G230600E57159N","2008-05-01T00:00:00",299232.400946472072974,0.299232000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230600E57159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.397176651266648,57.158821500000002]
["glac_bound",376695.000000000000000,"G228398E56629N","2008-05-01T00:00:00",244838.917472310015000,0.244839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228398E56629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.602799131126773,56.630159499999998]
["glac_bound",376698.000000000000000,"G224291E59973N","2008-05-01T00:00:00",67753.303257698164089,0.067753000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224291E59973N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.707300680850778,59.973607000000001]
["glac_bound",376699.000000000000000,"G228662E57013N","2008-05-01T00:00:00",424671.964248789416160,0.424672000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228662E57013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.337531793689323,57.012568000000002]
["glac_bound",376707.000000000000000,"G229055E56421N","2008-05-01T00:00:00",162466.314173364226008,0.162466000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229055E56421N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.945243398559285,56.420618500000003]
["glac_bound",376710.000000000000000,"G223314E59760N","2008-05-01T00:00:00",427597.556637004250661,0.427598000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223314E59760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.686951873749535,59.760460500000001]
["glac_bound",376712.000000000000000,"G230377E55519N","2008-05-01T00:00:00",56421.563307363969216,0.056422000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230377E55519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.624214895177289,55.520571000000004]
["glac_bound",376714.000000000000000,"G227814E57900N","2008-05-01T00:00:00",2437197.027955307625234,2.437200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227814E57900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.184495203459107,57.899925500000002]
["glac_bound",376717.000000000000000,"G230464E56763N","2008-05-01T00:00:00",205200.049228548945393,0.205200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230464E56763N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.537221483507352,56.764253499999995]
["glac_bound",376720.000000000000000,"G230467E56211N","2008-05-01T00:00:00",1416205.849690189817920,1.416210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230467E56211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.524489359539956,56.212670000000003]
["glac_bound",376721.000000000000000,"G225638E59345N","2008-05-01T00:00:00",889921.864322345820256,0.889922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225638E59345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.367873902284714,59.348715499999997]
["glac_bound",376722.000000000000000,"G230535E54658N","2008-05-01T00:00:00",1671911.161992769921198,1.671910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230535E54658N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.465931405064794,54.659616000000000]
["glac_bound",376727.000000000000000,"G228015E57363N","2008-05-01T00:00:00",673585.029491112800315,0.673585000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228015E57363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.985733772057301,57.362285999999997]
["glac_bound",376731.000000000000000,"G229345E56544N","2008-05-01T00:00:00",5103616.161190192215145,5.103620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229345E56544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.655448699405667,56.542799000000002]
["glac_bound",376732.000000000000000,"G226296E58745N","2008-05-01T00:00:00",64722.226890804158757,0.064722000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226296E58745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.704308944360406,58.744919499999995]
["glac_bound",376733.000000000000000,"G229905E57799N","2008-05-01T00:00:00",165529.996317436394747,0.165530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229905E57799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.093546937100797,57.800706500000004]
["glac_bound",376734.000000000000000,"G230053E56166N","2008-05-01T00:00:00",136288.900893354788423,0.136289000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230053E56166N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.949026407412958,56.167871500000004]
["glac_bound",376735.000000000000000,"G222690E59659N","2008-05-01T00:00:00",5160931.891788529232144,5.160930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222690E59659N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.309488456533074,59.663076000000004]
["glac_bound",376737.000000000000000,"G229747E56802N","2008-05-01T00:00:00",246956.946265695674811,0.246957000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229747E56802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.249027349017297,56.803511000000000]
["glac_bound",376739.000000000000000,"G224178E59774N","2008-05-01T00:00:00",1437397.620590940816328,1.437400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224178E59774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.821816397315274,59.776700500000004]
["glac_bound",376744.000000000000000,"G223233E59772N","2008-05-01T00:00:00",918959.921886577620171,0.918960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223233E59772N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.765366027984044,59.772637500000002]
["glac_bound",376745.000000000000000,"G228904E56800N","2008-05-01T00:00:00",55649.956337823838112,0.055650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228904E56800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.095317189655191,56.799685500000002]
["glac_bound",376751.000000000000000,"G228075E57221N","2008-05-01T00:00:00",454858.317494765564334,0.454858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228075E57221N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.926099939228521,57.220240000000004]
["glac_bound",376753.000000000000000,"G230590E54974N","2008-05-01T00:00:00",1780490.348852753406391,1.780490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230590E54974N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.400388488636338,54.977654500000000]
["glac_bound",376755.000000000000000,"G230262E55706N","2008-05-01T00:00:00",528748.218790440238081,0.528748000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230262E55706N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.738748904831709,55.710966999999997]
["glac_bound",376765.000000000000000,"G222670E59065N","2008-05-01T00:00:00",823872.098821222083643,0.823872000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222669E59066N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.327638391903179,59.064959999999999]
["glac_bound",376766.000000000000000,"G225975E59236N","2008-05-01T00:00:00",58819.136636825714959,0.058819000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225975E59236N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.026235945329972,59.236164500000001]
["glac_bound",376772.000000000000000,"G226458E58856N","2008-05-01T00:00:00",234635.254867885523709,0.234635000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226458E58856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.539361254197331,58.857297000000003]
["glac_bound",376778.000000000000000,"G227613E58149N","2008-05-01T00:00:00",680990.452653006417677,0.680990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227613E58149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.388195771121502,58.149710499999998]
["glac_bound",376781.000000000000000,"G224893E59406N","2008-05-01T00:00:00",439719.280407980782911,0.439719000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224893E59406N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.108905886953949,59.409072000000002]
["glac_bound",376784.000000000000000,"G229616E56456N","2008-05-01T00:00:00",154832.912265175575158,0.154833000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229616E56456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.382119435993957,56.456779499999996]
["glac_bound",376786.000000000000000,"G224568E59805N","2008-05-01T00:00:00",215379.770674899744336,0.215380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224568E59805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.432851967701936,59.804163500000001]
["glac_bound",376790.000000000000000,"G228413E57368N","2008-05-01T00:00:00",1279218.395172140561044,1.279220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228413E57368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584798776934093,57.368359999999996]
["glac_bound",376794.000000000000000,"G227274E58541N","2008-05-01T00:00:00",374155.306621794123203,0.374155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227274E58541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.726024317758515,58.542259000000001]
["glac_bound",376799.000000000000000,"G229974E57103N","2008-05-01T00:00:00",3139956.303494963329285,3.139960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229974E57103N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.023429350450954,57.103730999999996]
["glac_bound",376809.000000000000000,"G226367E58929N","2008-05-01T00:00:00",5317553.209391104988754,5.306330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226367E58929N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.611084000000005,58.923454000000000]
["glac_bound",376810.000000000000000,"G230005E56241N","2008-05-01T00:00:00",360272.050804087775759,0.360272000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230005E56241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.992721372656234,56.244163000000000]
["glac_bound",376813.000000000000000,"G222289E59930N","2008-05-01T00:00:00",604209.704891242668964,0.604210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222289E59930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.715176614420642,59.929118500000001]
["glac_bound",376814.000000000000000,"G228969E56957N","2008-05-01T00:00:00",91431105.962276801466942,91.431100000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Andrei Glacier","None","08CG228969E56957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.076392098717236,56.958255999999999]
["glac_bound",376815.000000000000000,"G228884E56428N","2008-05-01T00:00:00",7110245.678558875806630,7.110250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228884E56428N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.120778397489062,56.430812000000003]
["glac_bound",376822.000000000000000,"G230759E57101N","2008-05-01T00:00:00",1220206.983042399631813,1.220210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230759E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.242792732144977,57.103568500000002]
["glac_bound",376823.000000000000000,"G222563E59600N","2008-05-01T00:00:00",973160.536289071198553,0.973161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222563E59600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.439413687580469,59.598631499999996]
["glac_bound",376825.000000000000000,"G227605E57570N","2008-05-01T00:00:00",646918.283174072625116,0.646918000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227605E57570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.396202647847645,57.569613500000003]
["glac_bound",376827.000000000000000,"G222635E59331N","2008-05-01T00:00:00",1213989.395650291815400,1.213990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222635E59331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.366737488712829,59.331946000000002]
["glac_bound",376829.000000000000000,"G226716E58632N","2008-05-01T00:00:00",848741.679573942325078,0.848742000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226716E58632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.284310726426781,58.631161500000005]
["glac_bound",376837.000000000000000,"G227674E57416N","2008-05-01T00:00:00",52111.671901029098080,0.052112000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227674E57416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.325851212865473,57.416057500000001]
["glac_bound",376841.000000000000000,"G221662E59995N","2008-05-01T00:00:00",531444.246584307402372,0.531444000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221662E59995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.336991800391928,59.995704000000003]
["glac_bound",376844.000000000000000,"G226651E58284N","2008-05-01T00:00:00",333002.775265311240219,0.333003000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226651E58284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.349181579250796,58.282230999999996]
["glac_bound",376845.000000000000000,"G229967E56985N","2008-05-01T00:00:00",99184.537982079244102,0.099184000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229967E56985N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.032688836242301,56.984918000000000]
["glac_bound",376846.000000000000000,"G230537E56732N","2008-05-01T00:00:00",395943.634462539921515,0.395944000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230537E56732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463407453778473,56.731347999999997]
["glac_bound",376849.000000000000000,"G229591E56557N","2008-05-01T00:00:00",85142.366973733252962,0.085142000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229591E56557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.410985754180160,56.557424499999996]
["glac_bound",376851.000000000000000,"G227737E58444N","2008-05-01T00:00:00",691855.663424720638432,0.691856000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227737E58444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.267469861755160,58.443563999999995]
["glac_bound",376854.000000000000000,"G230140E56228N","2008-05-01T00:00:00",657330.216335402219556,0.657330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230140E56228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.854691454115368,56.229589000000004]
["glac_bound",376855.000000000000000,"G231009E56480N","2008-05-01T00:00:00",143535.122127165610436,0.143535000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA231009E56480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.990996286360257,56.480305500000000]
["glac_bound",376856.000000000000000,"G230621E54931N","2008-05-01T00:00:00",490272.559454054571688,0.490273000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230621E54931N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.380224671909019,54.932636500000001]
["glac_bound",376858.000000000000000,"G230416E57430N","2008-05-01T00:00:00",559541.216629786998965,0.559541000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230416E57430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.583723296372341,57.430217999999996]
["glac_bound",376859.000000000000000,"G226462E58938N","2008-05-01T00:00:00",201048.302055872016354,0.201048000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226462E58938N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.537936798074696,58.937281999999996]
["glac_bound",376860.000000000000000,"G222730E59071N","2008-05-01T00:00:00",702182.055323069682345,0.702182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222730E59071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.270819839547187,59.072020500000001]
["glac_bound",376866.000000000000000,"G230146E56275N","2008-05-01T00:00:00",568567.991698648547754,0.568568000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230146E56275N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.858865103532594,56.275545500000000]
["glac_bound",376867.000000000000000,"G227999E57413N","2008-05-01T00:00:00",168574.113099328096723,0.168574000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227999E57413N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.999778134946951,57.413567999999998]
["glac_bound",376868.000000000000000,"G224018E59983N","2008-05-01T00:00:00",219460.166276256961282,0.219460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224018E59983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.983982134920666,59.982596500000000]
["glac_bound",376872.000000000000000,"G230296E55595N","2008-05-01T00:00:00",161053.593218227004400,0.161054000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230296E55595N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.700921999999991,55.595787500000000]
["glac_bound",376877.000000000000000,"G227413E57797N","2008-05-01T00:00:00",1251764.038089194335043,1.251760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227413E57797N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.593340745649272,57.798859499999999]
["glac_bound",376879.000000000000000,"G223321E59555N","2008-05-01T00:00:00",1113477.906755326315761,1.113480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223321E59555N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.675674967795658,59.554051999999999]
["glac_bound",376887.000000000000000,"G228008E57781N","2008-05-01T00:00:00",1351511.047421263298020,1.351510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228008E57781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.988561184545802,57.779425500000002]
["glac_bound",376892.000000000000000,"G228486E57380N","2008-05-01T00:00:00",253351.873143189237453,0.253352000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228486E57380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.515393504291694,57.381895000000000]
["glac_bound",376894.000000000000000,"G230161E56440N","2008-05-01T00:00:00",1455752.446538711898029,1.455750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230161E56440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.841679504909763,56.443956499999999]
["glac_bound",376899.000000000000000,"G225469E59330N","2008-05-01T00:00:00",1970573.783492105081677,1.970570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225469E59330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.533975141141696,59.331307500000001]
["glac_bound",376902.000000000000000,"G226223E58740N","2008-05-01T00:00:00",6143908.619965807534754,6.143910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226223E58740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.769901623137685,58.754061000000000]
["glac_bound",376904.000000000000000,"G229018E56542N","2008-05-01T00:00:00",1227940.689592086942866,1.227940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229018E56542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.975319313929333,56.542581999999996]
["glac_bound",376907.000000000000000,"G226839E58334N","2008-05-01T00:00:00",25672680.354513406753540,25.672699999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226839E58334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.158186670160376,58.349836999999994]
["glac_bound",376909.000000000000000,"G230428E55997N","2008-05-01T00:00:00",4193977.259278792422265,4.193980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230428E55997N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.595517488995654,56.000032500000003]
["glac_bound",376911.000000000000000,"G229962E56979N","2008-05-01T00:00:00",195481.892776376043912,0.195482000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229962E56979N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.035613184985550,56.976689999999998]
["glac_bound",376914.000000000000000,"G226186E58734N","2008-05-01T00:00:00",9778278.490457588806748,9.778280000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226186E58734N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.835537433367051,58.753753000000003]
["glac_bound",376925.000000000000000,"G222315E59649N","2008-05-01T00:00:00",311791.581005838175770,0.311792000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222315E59649N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.685876578783422,59.648940499999995]
["glac_bound",376927.000000000000000,"G229412E56894N","2008-05-01T00:00:00",2450764.058560048229992,2.450760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229412E56894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.582412543680306,56.896655499999994]
["glac_bound",376932.000000000000000,"G229060E56875N","2008-05-01T00:00:00",3949589.283237837255001,3.949590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229060E56875N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.952601836264648,56.872936500000002]
["glac_bound",376942.000000000000000,"G230805E57310N","2008-05-01T00:00:00",835360.278832509880885,0.835360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230805E57310N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.197643813764046,57.307001499999998]
["glac_bound",376944.000000000000000,"G228533E57489N","2008-05-01T00:00:00",6084905.195558099076152,6.084910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228533E57489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.467404772347550,57.495210999999998]
["glac_bound",376945.000000000000000,"G229512E57033N","2008-05-01T00:00:00",77380.698276578783407,0.077381000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229512E57033N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.486277246238330,57.032950499999998]
["glac_bound",376953.000000000000000,"G225937E59217N","2008-05-01T00:00:00",159000.357188722147839,0.159000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225937E59217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.063515091100356,59.217261499999999]
["glac_bound",376966.000000000000000,"G229258E56766N","2008-05-01T00:00:00",1650457.065072782803327,1.650460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229258E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.744566774353473,56.765561500000004]
["glac_bound",376968.000000000000000,"G226704E58624N","2008-05-01T00:00:00",910077.331787014147267,0.910077000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226704E58624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.294132353218686,58.623826500000000]
["glac_bound",376970.000000000000000,"G227596E58369N","2008-05-01T00:00:00",387642.428944236831740,0.387642000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227596E58369N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.404379824633509,58.368650500000001]
["glac_bound",376972.000000000000000,"G229608E56424N","2008-05-01T00:00:00",498828.909104457590729,0.498829000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229608E56424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.392167508550472,56.424262999999996]
["glac_bound",376974.000000000000000,"G227400E58263N","2008-05-01T00:00:00",1562630.918443305417895,1.562630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227400E58263N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.599865070261075,58.263710000000003]
["glac_bound",376979.000000000000000,"G228950E56471N","2008-05-01T00:00:00",1012111.285220696707256,1.012110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228950E56471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.056853785342895,56.475209000000000]
["glac_bound",376980.000000000000000,"G230399E55753N","2008-05-01T00:00:00",110601.712998877235805,0.110602000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230399E55753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.598971049214981,55.751912500000003]
["glac_bound",376981.000000000000000,"G223923E59903N","2008-05-01T00:00:00",973057.834170437534340,0.973058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223923E59903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.071161672706808,59.903959499999999]
["glac_bound",376984.000000000000000,"G228947E56486N","2008-05-01T00:00:00",425035.855359350214712,0.425036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228947E56486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.052830018610166,56.485422000000000]
["glac_bound",376986.000000000000000,"G228635E57185N","2008-05-01T00:00:00",496928.539836734533310,0.496929000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228635E57185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.365229907277069,57.185026499999999]
["glac_bound",376988.000000000000000,"G226908E58296N","2008-05-01T00:00:00",5109045.172559507191181,5.109050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226908E58296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.104874011618904,58.299853499999998]
["glac_bound",376991.000000000000000,"G228500E56796N","2008-05-01T00:00:00",809808.284412140725181,0.809808000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228500E56796N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.499345944280094,56.799947000000003]
["glac_bound",376992.000000000000000,"G226712E58614N","2008-05-01T00:00:00",269226.859480628627352,0.269227000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226712E58614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.290559039578909,58.617049999999999]
["glac_bound",376999.000000000000000,"G229894E56201N","2008-05-01T00:00:00",190428.083297161851078,0.190428000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229894E56201N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.105411987313687,56.201378500000004]
["glac_bound",377004.000000000000000,"G222009E59909N","2008-05-01T00:00:00",484149.399635588284582,0.484149000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222009E59909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.997839331689079,59.910178500000001]
["glac_bound",377008.000000000000000,"G228278E57229N","2008-05-01T00:00:00",531717.921913686208427,0.531718000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228278E57229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.721442660136603,57.228660000000005]
["glac_bound",377011.000000000000000,"G228747E57415N","2008-05-01T00:00:00",833692.237861246219836,0.833692000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228747E57415N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.247948792978065,57.415485500000003]
["glac_bound",377018.000000000000000,"G229228E56779N","2008-05-01T00:00:00",277649.906214888556860,0.277650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229228E56779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.772493141234804,56.781842999999995]
["glac_bound",377019.000000000000000,"G230145E56518N","2008-05-01T00:00:00",569857.476982432301156,0.569857000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230145E56518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.854263962447050,56.518606500000004]
["glac_bound",377028.000000000000000,"G226943E58282N","2008-05-01T00:00:00",159764.938597745029256,0.159765000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226943E58282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.052777786275499,58.283095500000002]
["glac_bound",377036.000000000000000,"G229177E57172N","2008-05-01T00:00:00",964833.679252649308182,0.964834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229177E57172N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.823428653605276,57.171472500000000]
["glac_bound",377037.000000000000000,"G226896E58313N","2008-05-01T00:00:00",127848.058669887046563,0.127848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226896E58313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.103703411007359,58.313065999999999]
["glac_bound",377039.000000000000000,"G222014E59912N","2008-05-01T00:00:00",97335.800851197185693,0.097336000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222014E59912N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.983447513964052,59.912602499999998]
["glac_bound",377040.000000000000000,"G225301E59883N","2008-05-01T00:00:00",142246.836637814674759,0.142247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225301E59883N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.699146255271103,59.882874000000001]
["glac_bound",377045.000000000000000,"G228114E58071N","2008-05-01T00:00:00",1326768.785535681759939,1.326770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228114E58071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.888657624390078,58.072191000000004]
["glac_bound",377047.000000000000000,"G230076E55376N","2008-05-01T00:00:00",82237.765363226179034,0.082238000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230076E55376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.922305123924275,55.378292000000002]
["glac_bound",377060.000000000000000,"G223306E59532N","2008-05-01T00:00:00",2950019.114404284395278,2.950020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223306E59532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.701426509788291,59.535929500000002]
["glac_bound",377065.000000000000000,"G229216E57175N","2008-05-01T00:00:00",467240.591935361153446,0.467241000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229216E57175N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.782933953276711,57.175086000000000]
["glac_bound",377067.000000000000000,"G230123E57187N","2008-05-01T00:00:00",140850.564772304031067,0.140851000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230123E57187N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.876749497660740,57.187302500000001]
["glac_bound",377068.000000000000000,"G229983E55691N","2008-05-01T00:00:00",280733.027373955061194,0.280733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC229983E55691N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.013453680719238,55.690695500000004]
["glac_bound",377073.000000000000000,"G227072E58517N","2008-05-01T00:00:00",221642.953762664343230,0.221643000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227072E58517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.928747467691323,58.517127500000001]
["glac_bound",377081.000000000000000,"G230477E55344N","2008-05-01T00:00:00",893678.343473676126450,0.893678000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230477E55344N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.520816775594142,55.345641999999998]
["glac_bound",377087.000000000000000,"G229252E57037N","2008-05-01T00:00:00",56633.444335778753157,0.056633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229252E57037N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.748255191847306,57.036580499999999]
["glac_bound",377089.000000000000000,"G227114E58177N","2008-05-01T00:00:00",145230.863639432907803,0.145231000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227114E58177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.887381973384038,58.176631499999999]
["glac_bound",377090.000000000000000,"G221959E59936N","2008-05-01T00:00:00",3735934.160327901132405,3.735930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221959E59936N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.055959484269749,59.947826500000005]
["glac_bound",377098.000000000000000,"G227196E58410N","2008-05-01T00:00:00",534443.118636882631108,0.534443000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227196E58410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.803203595757225,58.408749000000000]
["glac_bound",377100.000000000000000,"G222373E59713N","2008-05-01T00:00:00",520231.542899701569695,0.520232000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222373E59713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.629282882499410,59.712603000000001]
["glac_bound",377102.000000000000000,"G227620E57248N","2008-05-01T00:00:00",493458448.14619541168212,493.458000000000027,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Baird Glacier","US2N00201800","08CF227620E57248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.306352274987233,57.240605000000002]
["glac_bound",377109.000000000000000,"G225002E59255N","2008-05-01T00:00:00",44505.879280869514332,0.044506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225002E59255N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.999577669265022,59.256440999999995]
["glac_bound",377110.000000000000000,"G229249E57048N","2008-05-01T00:00:00",61788.357749129572767,0.061788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229249E57048N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.751033627150264,57.047065000000003]
["glac_bound",377115.000000000000000,"G228649E57490N","2008-05-01T00:00:00",234187.819825043377932,0.234188000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228649E57490N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.350060028398673,57.490267000000003]
["glac_bound",377117.000000000000000,"G229590E56224N","2008-05-01T00:00:00",58635.843137970128737,0.058636000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229590E56224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.413670462933766,56.224766500000001]
["glac_bound",377119.000000000000000,"G227841E57953N","2008-05-01T00:00:00",548042.270148961921223,0.548042000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227841E57953N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.160890707073747,57.952224000000001]
["glac_bound",377121.000000000000000,"G230321E54570N","2008-05-01T00:00:00",415383.389341255417094,0.415383000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230321E54570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.672877632852419,54.568900499999998]
["glac_bound",377124.000000000000000,"G225301E59530N","2008-05-01T00:00:00",65465.189164201568929,0.065465000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225301E59530N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.699146118260444,59.529836000000003]
["glac_bound",377127.000000000000000,"G228424E57461N","2008-05-01T00:00:00",266830.049350218090694,0.266830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228424E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.576070500426681,57.461804500000000]
["glac_bound",377132.000000000000000,"G229035E57000N","2008-05-01T00:00:00",762249.469117083470337,0.762249000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229035E57000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.966107017893819,56.999413000000004]
["glac_bound",377133.000000000000000,"G229090E57066N","2008-05-01T00:00:00",3886116.371710200794041,3.886120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229090E57066N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.905258790601096,57.071938500000002]
["glac_bound",377138.000000000000000,"G222413E59640N","2008-05-01T00:00:00",75042.629654582677176,0.075043000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222413E59640N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.585964958433379,59.639318500000002]
["glac_bound",377140.000000000000000,"G230449E54725N","2008-05-01T00:00:00",87503.060754357706173,0.087503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230449E54725N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.551469755167602,54.725439000000001]
["glac_bound",377141.000000000000000,"G230314E54602N","2008-05-01T00:00:00",593467.889516278868541,0.593468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230314E54602N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.688147484158605,54.601864500000005]
["glac_bound",377143.000000000000000,"G229985E57045N","2008-05-01T00:00:00",1180653.548167829634622,1.180650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229985E57045N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.013484691444603,57.044539999999998]
["glac_bound",377146.000000000000000,"G229346E57432N","2008-05-01T00:00:00",240419.919156125542941,0.240420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229346E57432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.653579219230778,57.431905499999999]
["glac_bound",377157.000000000000000,"G230138E57524N","2008-05-01T00:00:00",52977.924226202878344,0.052978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230138E57524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.859556064018534,57.524172000000000]
["glac_bound",377162.000000000000000,"G226783E58272N","2008-05-01T00:00:00",968013.754077925230376,0.968014000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226783E58272N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.226421343828804,58.275711999999999]
["glac_bound",377176.000000000000000,"G230390E55171N","2008-05-01T00:00:00",1849542.752071410184726,1.849540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230390E55171N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.605652613919688,55.171582000000001]
["glac_bound",377180.000000000000000,"G229558E57128N","2008-05-01T00:00:00",5768624.735912471078336,5.768620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229558E57128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.452501177416195,57.131241500000002]
["glac_bound",377183.000000000000000,"G224694E59892N","2008-05-01T00:00:00",305963.803431277105119,0.305964000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224694E59892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.306132746739138,59.892342499999998]
["glac_bound",377187.000000000000000,"G224250E59848N","2008-05-01T00:00:00",1811692.007016642717645,1.811690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224250E59848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.747367157272492,59.852072000000000]
["glac_bound",377190.000000000000000,"G225562E59324N","2008-05-01T00:00:00",122574.127372171366005,0.122574000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225562E59324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.436990305543105,59.323886999999999]
["glac_bound",377193.000000000000000,"G230012E56518N","2008-05-01T00:00:00",75293.318966497172369,0.075293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230012E56518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.988501819819021,56.518609499999997]
["glac_bound",377197.000000000000000,"G230626E55229N","2008-05-01T00:00:00",98078.071013077569660,0.098078000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230626E55229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.372671271308690,55.228603500000006]
["glac_bound",377202.000000000000000,"G230030E55781N","2008-05-01T00:00:00",217969.932652630726807,0.217970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230030E55781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.970826328465478,55.782986500000000]
["glac_bound",377203.000000000000000,"G228989E56554N","2008-05-01T00:00:00",1007270.597519627190195,1.007270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228989E56554N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.009207071380018,56.556360999999995]
["glac_bound",377208.000000000000000,"G228674E56557N","2008-05-01T00:00:00",1276856.718128933105618,1.276860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228674E56557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.323222276330085,56.563150000000000]
["glac_bound",377210.000000000000000,"G227370E58261N","2008-05-01T00:00:00",3000764.477505310438573,3.000760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227370E58261N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.629320087683141,58.261689000000004]
["glac_bound",377212.000000000000000,"G232876E57762N","2008-05-01T00:00:00",122261.550726411063806,0.122262000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232876E57762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.123430953126473,57.761412000000000]
["glac_bound",377215.000000000000000,"G228477E57145N","2008-05-01T00:00:00",410799.350456148502417,0.410799000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228477E57145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.523525260429210,57.144062000000005]
["glac_bound",377216.000000000000000,"G228061E57834N","2008-05-01T00:00:00",125388.857043339783559,0.125389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228061E57834N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.938686259259271,57.836697999999998]
["glac_bound",377217.000000000000000,"G225501E59546N","2008-05-01T00:00:00",285373.087604948785156,0.285373000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225501E59546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.502618017441392,59.546144499999997]
["glac_bound",377218.000000000000000,"G230166E56332N","2008-05-01T00:00:00",1320945.439226025249809,1.320950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230166E56332N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.834841389732162,56.331299500000000]
["glac_bound",377225.000000000000000,"G230647E55234N","2008-05-01T00:00:00",1725543.066056694835424,1.725540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230647E55234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.352392507097790,55.232979999999998]
["glac_bound",377226.000000000000000,"G230272E55686N","2008-05-01T00:00:00",89588.832523483913974,0.089589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230272E55686N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.727218621604408,55.686916499999995]
["glac_bound",377228.000000000000000,"G229197E56637N","2008-05-01T00:00:00",116057.217641552866553,0.116057000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229197E56637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.803080423782774,56.637745500000001]
["glac_bound",377230.000000000000000,"G229974E56980N","2008-05-01T00:00:00",69354.940812046159408,0.069355000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229974E56980N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.027559542702761,56.979850499999998]
["glac_bound",377231.000000000000000,"G224289E59992N","2008-05-01T00:00:00",447799.909970863780472,0.447800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224289E59992N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.711396535290589,59.992881999999994]
["glac_bound",377232.000000000000000,"G229470E57178N","2008-05-01T00:00:00",51159.140639760567865,0.051159000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229470E57178N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.531018876593293,57.177837499999995]
["glac_bound",377245.000000000000000,"G222619E59224N","2008-05-01T00:00:00",246156.297247284092009,0.246156000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222619E59224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.384445033581017,59.224876500000001]
["glac_bound",377248.000000000000000,"G222108E59839N","2008-05-01T00:00:00",509898.298510510474443,0.509898000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222108E59839N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.891601040572510,59.839308000000003]
["glac_bound",377249.000000000000000,"G224990E59614N","2008-05-01T00:00:00",83717.308734092715895,0.083717000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224990E59614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.010000434704580,59.613930499999995]
["glac_bound",377250.000000000000000,"G228081E57572N","2008-05-01T00:00:00",627846.669641677290201,0.627847000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228081E57572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.913281476518591,57.571816999999996]
["glac_bound",377252.000000000000000,"G230849E57290N","2008-05-01T00:00:00",150505.690976343874354,0.150506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230849E57290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.150769649845131,57.289408500000000]
["glac_bound",377253.000000000000000,"G230108E56492N","2008-05-01T00:00:00",5999276.693363183178008,5.999280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230108E56492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.910771461276852,56.496905499999997]
["glac_bound",377255.000000000000000,"G225576E59504N","2008-05-01T00:00:00",83241.190376931423089,0.083241000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225576E59504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.423482665623993,59.504077500000001]
["glac_bound",377262.000000000000000,"G227937E57356N","2008-05-01T00:00:00",1894952.889843851095065,1.894950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227937E57356N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.059310818700737,57.364432000000001]
["glac_bound",377264.000000000000000,"G228683E56581N","2008-05-01T00:00:00",55826.853763905972301,0.055827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228683E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.317183446621613,56.580674999999999]
["glac_bound",377265.000000000000000,"G223642E59568N","2008-05-01T00:00:00",377521.181482609012164,0.377521000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223642E59568N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.367246790070908,59.569927499999999]
["glac_bound",377273.000000000000000,"G228425E57423N","2008-05-01T00:00:00",3359436.789984256960452,3.359440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228425E57423N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.578477412186743,57.430903999999998]
["glac_bound",377277.000000000000000,"G229778E56596N","2008-05-01T00:00:00",2952543.594514682423323,6.991230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229778E56596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.203615513753618,56.600212999999997]
["glac_bound",377277.000000000000000,"G229778E56596N","2008-05-01T00:00:00",4038684.310141931753606,6.991230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229778E56596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.236820916008440,56.604419000000000]
["glac_bound",377279.000000000000000,"G230740E54907N","2008-05-01T00:00:00",172207.905115126777673,0.172208000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230740E54907N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.257976760364215,54.906891999999999]
["glac_bound",377280.000000000000000,"G226734E58319N","2008-05-01T00:00:00",493176.332959404098801,0.493176000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226734E58319N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.267615146889796,58.320811500000005]
["glac_bound",377284.000000000000000,"G228627E57191N","2008-05-01T00:00:00",457724.573893280816264,0.457725000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228627E57191N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.370702122461410,57.190773500000006]
["glac_bound",377291.000000000000000,"G230048E57461N","2008-05-01T00:00:00",50920.017150182211481,0.050920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230048E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.951163475128624,57.461266500000001]
["glac_bound",377296.000000000000000,"G222422E59750N","2008-05-01T00:00:00",5773738.226758553646505,5.773740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222422E59750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.576282591285661,59.743361999999998]
["glac_bound",377303.000000000000000,"G230051E57106N","2008-05-01T00:00:00",115995.085901507263770,0.115995000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230051E57106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.948814992399775,57.106294499999997]
["glac_bound",377305.000000000000000,"G231132E55222N","2008-05-01T00:00:00",93020.734603882170632,0.093021000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231132E55222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.867521639892715,55.222030000000004]
["glac_bound",377306.000000000000000,"G230517E57027N","2008-05-01T00:00:00",141432.402366828202503,0.141432000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230517E57027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.483444993260832,57.027172499999999]
["glac_bound",377309.000000000000000,"G227871E57557N","2008-05-01T00:00:00",4395653.217335617169738,4.395650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227871E57557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.123285874864592,57.570891500000002]
["glac_bound",377310.000000000000000,"G230606E56744N","2008-05-01T00:00:00",208776.997147101530572,0.208777000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230606E56744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.394416504457325,56.743960000000001]
["glac_bound",377314.000000000000000,"G229573E56177N","2008-05-01T00:00:00",476384.940780951757915,0.476385000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229573E56177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.426568919902905,56.180862500000003]
["glac_bound",377324.000000000000000,"G230713E57320N","2008-05-01T00:00:00",3764920.065952385775745,3.764920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230713E57320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.287943893282744,57.317933500000002]
["glac_bound",377326.000000000000000,"G230634E54934N","2008-05-01T00:00:00",417375.808656218403485,0.417376000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230634E54934N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.364954556362932,54.934044999999998]
["glac_bound",377327.000000000000000,"G226982E58122N","2008-05-01T00:00:00",668173.206312436843291,0.668173000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226982E58122N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.013953384896610,58.123585500000004]
["glac_bound",377333.000000000000000,"G225552E59234N","2008-05-01T00:00:00",337826.725715603155550,0.337827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225552E59234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.451118033781199,59.236599499999997]
["glac_bound",377335.000000000000000,"G229233E56818N","2008-05-01T00:00:00",1236031.430136473616585,1.236030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229233E56818N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.765413220214498,56.818567999999999]
["glac_bound",377337.000000000000000,"G223185E59703N","2008-05-01T00:00:00",4579170.089026091620326,4.579170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Samuel Glacier","None","08AC223185E59703N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.823275790976481,59.706110499999994]
["glac_bound",377340.000000000000000,"G230199E54817N","2008-05-01T00:00:00",70432.269543178641470,0.070432000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230199E54817N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.802122603896152,54.817344000000006]
["glac_bound",377342.000000000000000,"G229783E56427N","2008-05-01T00:00:00",29981863.053711958229542,29.981900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229783E56427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.282863620672998,56.448842999999997]
["glac_bound",377343.000000000000000,"G229403E56290N","2008-05-01T00:00:00",327585.777136297605466,0.327586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229403E56290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.597259036063576,56.289239999999999]
["glac_bound",377344.000000000000000,"G226291E58952N","2008-05-01T00:00:00",4135045.899179123807698,4.135050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226291E58952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.707599801919173,58.950763000000002]
["glac_bound",377358.000000000000000,"G227482E57968N","2008-05-01T00:00:00",19061723.991831108927727,19.061699999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227482E57968N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.508454764445787,57.969761500000004]
["glac_bound",377360.000000000000000,"G230172E56454N","2008-05-01T00:00:00",247569.595088345464319,0.247570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230172E56454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.827555541899443,56.454096000000000]
["glac_bound",377362.000000000000000,"G228623E57463N","2008-05-01T00:00:00",107586.668502481217729,0.107587000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228623E57463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.377455270672442,57.462719500000006]
["glac_bound",377363.000000000000000,"G224237E59997N","2008-05-01T00:00:00",126396.242378129172721,0.126396000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224237E59997N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.761566124150988,59.996695500000001]
["glac_bound",377365.000000000000000,"G225706E59321N","2008-05-01T00:00:00",274694.411570108670276,0.274694000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225706E59321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.293222442164335,59.321785500000004]
["glac_bound",377366.000000000000000,"G225655E59289N","2008-05-01T00:00:00",51275.102807098533958,0.051275000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225655E59289N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.345119995825996,59.289121999999999]
["glac_bound",377367.000000000000000,"G222674E59641N","2008-05-01T00:00:00",1737594.278328316286206,1.737590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222674E59641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.332096868268877,59.644969500000002]
["glac_bound",377369.000000000000000,"G227699E57891N","2008-05-01T00:00:00",6481025.750554895028472,6.481030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227699E57891N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.297018929258684,57.907977500000001]
["glac_bound",377370.000000000000000,"G229071E56452N","2008-05-01T00:00:00",99224.483085859304992,0.099224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229071E56452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.930435348470354,56.452854000000002]
["glac_bound",377380.000000000000000,"G227712E57933N","2008-05-01T00:00:00",662864.805047920555808,0.662865000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227712E57933N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.286457087107095,57.932893999999997]
["glac_bound",377381.000000000000000,"G228906E57678N","2008-05-01T00:00:00",502251.938604707014747,0.502252000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228906E57678N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.092972441523443,57.678292999999996]
["glac_bound",377383.000000000000000,"G222934E59357N","2008-05-01T00:00:00",89702.272907726539415,0.089702000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222934E59357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.065881998623468,59.357034999999996]
["glac_bound",377384.000000000000000,"G229576E57117N","2008-05-01T00:00:00",1409728.159455597633496,1.409730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229576E57117N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.429880708620686,57.117034500000003]
["glac_bound",377385.000000000000000,"G223105E59724N","2008-05-01T00:00:00",250578.613009360793512,0.250579000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223105E59724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.892211620443533,59.724705499999999]
["glac_bound",377387.000000000000000,"G228618E57195N","2008-05-01T00:00:00",115704.257025598504697,0.115704000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228618E57195N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.382344405122240,57.195047000000002]
["glac_bound",377388.000000000000000,"G230454E55230N","2008-05-01T00:00:00",3319187.808927160687745,3.319190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230454E55230N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.546763779605840,55.231010499999996]
["glac_bound",377389.000000000000000,"G230452E56018N","2008-05-01T00:00:00",108258.094165447793785,0.108258000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230452E56018N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.546731001892113,56.018110500000006]
["glac_bound",377390.000000000000000,"G224851E59724N","2008-05-01T00:00:00",68592.830134914867813,0.068593000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224851E59724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.149372013906856,59.723781500000001]
["glac_bound",377392.000000000000000,"G227448E58442N","2008-05-01T00:00:00",69092.145373572129756,0.069092000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227448E58442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.552594658727457,58.442444999999999]
["glac_bound",377394.000000000000000,"G228879E57395N","2008-05-01T00:00:00",156338.440417850360973,0.156338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228879E57395N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.121264396907236,57.394835999999998]
["glac_bound",377399.000000000000000,"G228036E57134N","2008-05-01T00:00:00",711636.745425654225983,0.711637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228036E57134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.963603483870969,57.134540999999999]
["glac_bound",377400.000000000000000,"G229946E57097N","2008-05-01T00:00:00",712384.722718118224293,0.712385000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229946E57097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.056039281704614,57.096608500000002]
["glac_bound",377401.000000000000000,"G228045E57225N","2008-05-01T00:00:00",1417236.416747677139938,1.417240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228045E57225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.959887898128784,57.225187000000005]
["glac_bound",377402.000000000000000,"G230788E55049N","2008-05-01T00:00:00",94794.055850575852674,0.094794000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230788E55049N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.212391141277493,55.048904499999999]
["glac_bound",377404.000000000000000,"G228607E56657N","2008-05-01T00:00:00",2180108.865098514128476,2.180110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228607E56657N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.391697631546776,56.654758500000000]
["glac_bound",377406.000000000000000,"G228699E57445N","2008-05-01T00:00:00",2618859.011161500122398,2.618860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228699E57445N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.308726336024847,57.448195499999997]
["glac_bound",377409.000000000000000,"G223144E59451N","2008-05-01T00:00:00",626443.565726238535717,0.626444000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223144E59451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.854717006532724,59.450005000000004]
["glac_bound",377417.000000000000000,"G230001E56325N","2008-05-01T00:00:00",3092110.551593984477222,3.092110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230001E56325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.005772919221272,56.324748999999997]
["glac_bound",377420.000000000000000,"G228930E57547N","2008-05-01T00:00:00",1331186.368283478775993,1.331190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228930E57547N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.069670728319466,57.546935500000004]
["glac_bound",377424.000000000000000,"G226112E58939N","2008-05-01T00:00:00",8526457.891600014641881,8.526460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226112E58939N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.876900596713625,58.943952500000002]
["glac_bound",377433.000000000000000,"G224312E59871N","2008-05-01T00:00:00",165460.709597519162344,0.165461000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224312E59871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.688184046446906,59.870805500000003]
["glac_bound",377440.000000000000000,"G230536E57075N","2008-05-01T00:00:00",55785.421570580772823,0.055785000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230536E57075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464763520359838,57.074498500000004]
["glac_bound",377446.000000000000000,"G230613E55628N","2008-05-01T00:00:00",1135307.080476009752601,1.135310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230613E55628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.383707560047128,55.628746000000007]
["glac_bound",377447.000000000000000,"G228076E57284N","2008-05-01T00:00:00",183896.982621513918275,0.183897000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228076E57284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.924815065190671,57.284102000000004]
["glac_bound",377449.000000000000000,"G226695E58308N","2008-05-01T00:00:00",577911.233952870010398,0.577911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226695E58308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.308409296935537,58.313108999999997]
["glac_bound",377450.000000000000000,"G230446E56081N","2008-05-01T00:00:00",258202.942097125633154,0.258203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230446E56081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.553366064032673,56.083462499999996]
["glac_bound",377452.000000000000000,"G228920E57357N","2008-05-01T00:00:00",725411.490823015687056,0.725411000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228920E57357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.079844805697235,57.356739000000005]
["glac_bound",377454.000000000000000,"G227964E57366N","2008-05-01T00:00:00",82572.318414004315855,0.082572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227964E57366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.036100310755160,57.366669999999999]
["glac_bound",377456.000000000000000,"G228138E57400N","2008-05-01T00:00:00",165697.885461079073139,0.165698000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228138E57400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.861081959244160,57.400483000000001]
["glac_bound",377468.000000000000000,"G228397E57436N","2008-05-01T00:00:00",58246.653866184089566,0.058247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228397E57436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.603571936950175,57.436062499999998]
["glac_bound",377470.000000000000000,"G226764E58520N","2008-05-01T00:00:00",6838777.402399979531765,6.838780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226764E58520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.240705536921269,58.533122500000005]
["glac_bound",377471.000000000000000,"G229028E57300N","2008-05-01T00:00:00",108214.316249475858058,0.108214000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229028E57300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.972243691919942,57.300548500000005]
["glac_bound",377476.000000000000000,"G230562E54713N","2008-05-01T00:00:00",718915.995847871992737,0.718916000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230562E54713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.441979564061967,54.716211000000001]
["glac_bound",377481.000000000000000,"G227727E57772N","2008-05-01T00:00:00",6886075.524154397659004,6.886080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227727E57772N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.269712931924801,57.783978500000003]
["glac_bound",377486.000000000000000,"G225863E59317N","2008-05-01T00:00:00",225433.359472804906545,0.225433000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225863E59317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.136618298598137,59.317976500000000]
["glac_bound",377487.000000000000000,"G230496E55348N","2008-05-01T00:00:00",247031.774038302508416,0.247032000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230496E55348N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.504962388739443,55.351728500000000]
["glac_bound",377490.000000000000000,"G225381E59673N","2008-05-01T00:00:00",732811.197150732856244,0.732811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225381E59673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.619496507919706,59.673648499999999]
["glac_bound",377493.000000000000000,"G222509E59868N","2008-05-01T00:00:00",812176.628834009403363,0.812177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222509E59868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.483496371176386,59.871096999999999]
["glac_bound",377497.000000000000000,"G229466E56900N","2008-05-01T00:00:00",345298.889194248185959,0.345299000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229466E56900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.535370859251969,56.899667000000001]
["glac_bound",377501.000000000000000,"G223220E59641N","2008-05-01T00:00:00",418838.585858931823168,0.418839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223220E59641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.782374022234677,59.641452000000001]
["glac_bound",377503.000000000000000,"G229373E57392N","2008-05-01T00:00:00",899135.333736086031422,0.899135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229373E57392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.629655807085555,57.392425000000003]
["glac_bound",377519.000000000000000,"G228008E57821N","2008-05-01T00:00:00",344724.350087175087538,0.344724000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228008E57821N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.990627382786897,57.823436500000000]
["glac_bound",377520.000000000000000,"G230177E55866N","2008-05-01T00:00:00",56760.502085922242259,0.056760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230177E55866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.823626739980057,55.866368500000000]
["glac_bound",377522.000000000000000,"G230405E55534N","2008-05-01T00:00:00",417899.809617704595439,0.417900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230405E55534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.594734130792233,55.534183999999996]
["glac_bound",377523.000000000000000,"G228796E56492N","2008-05-01T00:00:00",134835.289627366233617,0.134835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228796E56492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.204275000580026,56.491524499999997]
["glac_bound",377525.000000000000000,"G225443E59358N","2008-05-01T00:00:00",925994.933396159554832,0.925995000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225443E59358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.558291218899512,59.357659999999996]
["glac_bound",377526.000000000000000,"G228546E57277N","2008-05-01T00:00:00",138619.789085912663722,0.138620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228546E57277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.457895178005856,57.277669500000002]
["glac_bound",377528.000000000000000,"G229919E56788N","2008-05-01T00:00:00",802180.767216463107616,0.802181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229919E56788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.087102135912033,56.789895500000000]
["glac_bound",377529.000000000000000,"G230748E57315N","2008-05-01T00:00:00",839198.196321921539493,0.839198000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230748E57315N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.251494261033542,57.315460999999999]
["glac_bound",377530.000000000000000,"G229607E57194N","2008-05-01T00:00:00",306473.299592087103520,0.306473000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229607E57194N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.393125756822940,57.194909000000003]
["glac_bound",377531.000000000000000,"G228988E56548N","2008-05-01T00:00:00",242646.602104373014299,0.242647000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228988E56548N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.012604338243932,56.547712500000003]
["glac_bound",377535.000000000000000,"G229931E57221N","2008-05-01T00:00:00",280866.844171367934905,0.280867000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229931E57221N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.069699155954311,57.221273500000002]
["glac_bound",377536.000000000000000,"G230725E57290N","2008-05-01T00:00:00",2367351.223396509885788,2.367350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230725E57290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.278721662353348,57.296652500000000]
["glac_bound",377537.000000000000000,"G228565E56806N","2008-05-01T00:00:00",3672370.485554925631732,3.672370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228565E56806N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.435822175133751,56.808763499999998]
["glac_bound",377546.000000000000000,"G224671E59784N","2008-05-01T00:00:00",227100.523596617538715,0.227101000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224671E59784N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.329064461822668,59.783594500000000]
["glac_bound",377551.000000000000000,"G228127E57624N","2008-05-01T00:00:00",973066.963992921868339,0.973067000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228127E57624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.877817229268288,57.621192000000001]
["glac_bound",377553.000000000000000,"G230131E56249N","2008-05-01T00:00:00",58510.375234127954172,0.058510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230131E56249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.868681818435988,56.249510500000000]
["glac_bound",377555.000000000000000,"G226870E58483N","2008-05-01T00:00:00",256192.100670520972926,0.256192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226870E58483N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.130417185076340,58.483023000000003]
["glac_bound",377560.000000000000000,"G227769E57385N","2008-05-01T00:00:00",115626.730812188034179,0.115627000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227769E57385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.230616268264271,57.385034000000005]
["glac_bound",377562.000000000000000,"G224317E59830N","2008-05-01T00:00:00",661921.240350755746476,0.661921000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224317E59830N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.676941632640904,59.834609999999998]
["glac_bound",377564.000000000000000,"G226596E58768N","2008-05-01T00:00:00",89435.066937415307621,0.089435000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226596E58768N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.405040438915933,58.769236499999998]
["glac_bound",377568.000000000000000,"G222025E59942N","2008-05-01T00:00:00",369163.958327826811001,0.369164000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222025E59942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.974543570382338,59.942059999999998]
["glac_bound",377571.000000000000000,"G231099E55260N","2008-05-01T00:00:00",132373.785994455596665,0.132374000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231099E55260N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.902431705773409,55.260919000000001]
["glac_bound",377574.000000000000000,"G230306E54689N","2008-05-01T00:00:00",593573.733963487553410,0.593574000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230306E54689N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.693843043395532,54.688384499999998]
["glac_bound",377575.000000000000000,"G229492E56724N","2008-05-01T00:00:00",1460596.736644157906994,1.460600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229492E56724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.507335365505355,56.723098000000000]
["glac_bound",377581.000000000000000,"G230650E54932N","2008-05-01T00:00:00",651910.544522114912979,0.651911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230650E54932N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351324657714343,54.932642999999999]
["glac_bound",377583.000000000000000,"G222584E59600N","2008-05-01T00:00:00",851123.027682314976119,0.851123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222584E59600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.411451686894111,59.597944499999997]
["glac_bound",377588.000000000000000,"G228470E56603N","2008-05-01T00:00:00",368217.460455418098718,0.368217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228470E56603N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.529116640615655,56.607074999999995]
["glac_bound",377593.000000000000000,"G230477E56648N","2008-05-01T00:00:00",376089.499305040284526,0.376090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230477E56648N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.524311854242683,56.648399999999995]
["glac_bound",377597.000000000000000,"G227678E57854N","2008-05-01T00:00:00",50379.500164698394656,0.050380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227678E57854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.323904912813816,57.853082000000001]
["glac_bound",377598.000000000000000,"G230359E56698N","2008-05-01T00:00:00",251772.822625305940164,0.251773000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230359E56698N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.641090028615622,56.698008500000000]
["glac_bound",377603.000000000000000,"G224038E59754N","2008-05-01T00:00:00",2438992.499391816090792,2.438990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224038E59754N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.965332041514841,59.754767999999999]
["glac_bound",377610.000000000000000,"G228966E56585N","2008-05-01T00:00:00",1812631.555273617152125,1.812630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228966E56585N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.025627623577435,56.583571000000006]
["glac_bound",377611.000000000000000,"G224310E60001N","2008-05-01T00:00:00",13008.650544381293003,0.013009000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224310E60001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.689858679051667,60.000648499999997]
["glac_bound",377613.000000000000000,"G230261E54484N","2008-05-01T00:00:00",257280.679174076474737,0.257281000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230261E54484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.736069531864530,54.485355999999996]
["glac_bound",377617.000000000000000,"G228657E57456N","2008-05-01T00:00:00",3102524.868853516876698,3.102520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228657E57456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.343507168789046,57.472259500000000]
["glac_bound",377619.000000000000000,"G228115E57580N","2008-05-01T00:00:00",1852217.322853887919337,1.852220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228115E57580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.887592952972170,57.580666500000000]
["glac_bound",377625.000000000000000,"G230043E56166N","2008-05-01T00:00:00",350436.711984996974934,0.350437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230043E56166N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.955038758072533,56.166363000000004]
["glac_bound",377630.000000000000000,"G227840E57937N","2008-05-01T00:00:00",448534.547234830970410,0.448535000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227840E57937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.154717792715360,57.933993000000001]
["glac_bound",377637.000000000000000,"G225198E59314N","2008-05-01T00:00:00",96856.965539243494277,0.096857000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225198E59314N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.802884488165660,59.316017000000002]
["glac_bound",377638.000000000000000,"G228457E57148N","2008-05-01T00:00:00",154836.022436299361289,0.154836000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228457E57148N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.543531585000608,57.147778000000002]
["glac_bound",377639.000000000000000,"G225494E59565N","2008-05-01T00:00:00",448807.432316936028656,0.448807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225494E59565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.501780784017399,59.567469500000001]
["glac_bound",377641.000000000000000,"G221956E59566N","2008-05-01T00:00:00",1326314.559916918864474,1.326310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221956E59566N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.043066033058096,59.565760499999996]
["glac_bound",377647.000000000000000,"G228867E56540N","2008-05-01T00:00:00",70064.653683137643384,0.070065000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228867E56540N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.134630975661366,56.540050500000000]
["glac_bound",377657.000000000000000,"G231219E57534N","2008-05-01T00:00:00",107806.896351979317842,0.107807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231219E57534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.781186881633886,57.534081999999998]
["glac_bound",377659.000000000000000,"G228111E57461N","2008-05-01T00:00:00",97790.315641741821310,0.097790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228111E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.889720368040940,57.460903999999999]
["glac_bound",377664.000000000000000,"G226647E58539N","2008-05-01T00:00:00",1433284.828080899082124,1.433280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226647E58539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.353602764190612,58.539540500000001]
["glac_bound",377665.000000000000000,"G230195E57046N","2008-05-01T00:00:00",69995.602675507048843,0.069996000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230195E57046N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.809301119757208,57.046824000000001]
["glac_bound",377668.000000000000000,"G227612E57644N","2008-05-01T00:00:00",239979.968199889350217,0.239980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227612E57644N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.384726254672898,57.641754000000006]
["glac_bound",377669.000000000000000,"G228711E57463N","2008-05-01T00:00:00",89173.097231078805635,0.089173000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228711E57463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.288478761851138,57.463411499999999]
["glac_bound",377670.000000000000000,"G227494E58228N","2008-05-01T00:00:00",3042111.823257441632450,3.042110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227494E58228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.510812374696457,58.231489499999995]
["glac_bound",377671.000000000000000,"G228519E57577N","2008-05-01T00:00:00",133007.203465957689332,0.133007000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228519E57577N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.481563996758524,57.576941500000004]
["glac_bound",377677.000000000000000,"G230194E56252N","2008-05-01T00:00:00",1524455.296342271845788,1.524460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230194E56252N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.809848855121686,56.250719500000002]
["glac_bound",377678.000000000000000,"G228514E57177N","2008-05-01T00:00:00",184981.551954111811938,0.184982000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228514E57177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.484930303627607,57.176465999999998]
["glac_bound",377679.000000000000000,"G222506E59747N","2008-05-01T00:00:00",488334.851700452505611,0.488335000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222506E59747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.494979228395067,59.747686000000002]
["glac_bound",377681.000000000000000,"G221813E59743N","2008-05-01T00:00:00",774707.079033427522518,0.774707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221813E59743N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.186356862249852,59.742622499999996]
["glac_bound",377683.000000000000000,"G230452E56227N","2008-05-01T00:00:00",196631.589509421901312,0.196632000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230452E56227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.549036150495539,56.227520999999996]
["glac_bound",377691.000000000000000,"G228598E56599N","2008-05-01T00:00:00",251552.629570094781229,0.251553000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228598E56599N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.405250427034986,56.596896500000000]
["glac_bound",377694.000000000000000,"G230046E56096N","2008-05-01T00:00:00",456651.304794925905298,0.456651000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230046E56096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.952447026880492,56.095501999999996]
["glac_bound",377695.000000000000000,"G227087E58504N","2008-05-01T00:00:00",994719.141288659884594,0.994719000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227087E58504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.919406288671894,58.506420499999997]
["glac_bound",377696.000000000000000,"G227847E57731N","2008-05-01T00:00:00",8750820.253948373720050,8.750819999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227847E57731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.154331942873341,57.732102499999996]
["glac_bound",377698.000000000000000,"G226739E58578N","2008-05-01T00:00:00",400532.826012020290364,0.400533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226739E58578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.258727297580947,58.580050999999997]
["glac_bound",377701.000000000000000,"G226800E58306N","2008-05-01T00:00:00",396582.603660360677168,0.396583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226800E58306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.201073117788468,58.304562000000004]
["glac_bound",377709.000000000000000,"G230295E55641N","2008-05-01T00:00:00",187779.347522672760533,0.187779000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230295E55641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.703881271941867,55.641484500000004]
["glac_bound",377712.000000000000000,"G230281E55108N","2008-05-01T00:00:00",125454.761168624507263,0.125455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230281E55108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.719119216946012,55.107464499999999]
["glac_bound",377718.000000000000000,"G230292E54684N","2008-05-01T00:00:00",415307.291718049091287,0.415307000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230292E54684N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.702976620222103,54.685573500000004]
["glac_bound",377725.000000000000000,"G225699E59250N","2008-05-01T00:00:00",65559.887452608367312,0.065560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225699E59250N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.301175129568094,59.249725999999995]
["glac_bound",377729.000000000000000,"G222257E59594N","2008-05-01T00:00:00",333244.179656395222992,0.333244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222257E59594N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.742154057332925,59.593497999999997]
["glac_bound",377741.000000000000000,"G227061E58516N","2008-05-01T00:00:00",190949.832640576089034,0.190950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227061E58516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.937627706237066,58.515719500000003]
["glac_bound",377742.000000000000000,"G227721E57562N","2008-05-01T00:00:00",90458.466336247322033,0.090458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227721E57562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.278763055555572,57.561859499999997]
["glac_bound",377747.000000000000000,"G230084E56560N","2008-05-01T00:00:00",267617.420471159915905,0.267617000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230084E56560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.917233913088694,56.560599999999994]
["glac_bound",377749.000000000000000,"G230507E56787N","2008-05-01T00:00:00",238357.328334266261663,0.238357000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230507E56787N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.492716067073161,56.786441000000003]
["glac_bound",377761.000000000000000,"G230409E56081N","2008-05-01T00:00:00",509749.882075742178131,0.509750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230409E56081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.589116128424678,56.080449999999999]
["glac_bound",377762.000000000000000,"G231589E56709N","2008-05-01T00:00:00",149856.270135477185249,0.149856000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231589E56709N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.412864382935993,56.708055500000000]
["glac_bound",377765.000000000000000,"G228978E56826N","2008-05-01T00:00:00",642587.363803570624441,0.642587000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228978E56826N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.022123735275272,56.826329000000001]
["glac_bound",377769.000000000000000,"G229337E57192N","2008-05-01T00:00:00",3235006.169332721736282,3.235010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229337E57192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.660117811796681,57.193341500000002]
["glac_bound",377771.000000000000000,"G222469E59297N","2008-05-01T00:00:00",340733.029085612040944,0.340733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222469E59297N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.532477637560646,59.294993000000005]
["glac_bound",377780.000000000000000,"G227710E57559N","2008-05-01T00:00:00",3500007.800995760597289,3.500010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227710E57559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.296933680343926,57.562344500000002]
["glac_bound",377783.000000000000000,"G222815E59429N","2008-05-01T00:00:00",1513325.930589206283912,1.513330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222815E59429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.192885275487271,59.431817500000001]
["glac_bound",377784.000000000000000,"G230441E55606N","2008-05-01T00:00:00",291092.460603065148462,0.291092000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230441E55606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.561882463407301,55.603851500000005]
["glac_bound",377787.000000000000000,"G230537E54848N","2008-05-01T00:00:00",714344.176772130304016,0.714344000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230537E54848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464993079629636,54.848473499999997]
["glac_bound",377790.000000000000000,"G226468E58857N","2008-05-01T00:00:00",185344.384349013998872,0.185344000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226468E58857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.531583918001218,58.857177000000000]
["glac_bound",377792.000000000000000,"G228533E57067N","2008-05-01T00:00:00",90268.331128359539434,0.090268000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228533E57067N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.465094885231110,57.068269500000000]
["glac_bound",377796.000000000000000,"G226748E58222N","2008-05-01T00:00:00",1069253.015486608026549,1.069250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226748E58222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.250205824894692,58.222985999999999]
["glac_bound",377799.000000000000000,"G230464E57089N","2008-05-01T00:00:00",815283.724169433000498,0.815284000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230464E57089N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.535918932355969,57.088489500000001]
["glac_bound",377800.000000000000000,"G222780E59287N","2008-05-01T00:00:00",68808.865115450709709,0.068809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222780E59287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.220122305418727,59.286586999999997]
["glac_bound",377802.000000000000000,"G226427E58857N","2008-05-01T00:00:00",399543.937744015885983,0.399544000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226427E58857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.574561333902437,58.857171000000001]
["glac_bound",377804.000000000000000,"G227635E57638N","2008-05-01T00:00:00",390032.076731628272682,0.390032000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227635E57638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.366571408036918,57.639471499999999]
["glac_bound",377808.000000000000000,"G225464E59548N","2008-05-01T00:00:00",197967.753075379325310,0.197968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225464E59548N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.533869065338564,59.549234499999997]
["glac_bound",377809.000000000000000,"G224111E59815N","2008-05-01T00:00:00",234883.809528304991545,0.234884000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224111E59815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.889331748523972,59.814886000000001]
["glac_bound",377810.000000000000000,"G231255E57524N","2008-05-01T00:00:00",568601.964035627781413,0.568602000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231255E57524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.745207658430530,57.526187999999998]
["glac_bound",377811.000000000000000,"G228475E57192N","2008-05-01T00:00:00",815661.031460773432627,0.815661000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228475E57192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.518848213291335,57.195066499999996]
["glac_bound",377813.000000000000000,"G230167E57053N","2008-05-01T00:00:00",639399.354718448943458,0.639399000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230167E57053N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.836003382371189,57.053843000000001]
["glac_bound",377817.000000000000000,"G228084E56753N","2008-05-01T00:00:00",1331251.799578700913116,1.331250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228084E56753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.913546689851273,56.754598999999999]
["glac_bound",377820.000000000000000,"G225770E59204N","2008-05-01T00:00:00",101150.386124264463433,0.101150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225770E59204N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.230031491793085,59.204231000000000]
["glac_bound",377821.000000000000000,"G230242E57024N","2008-05-01T00:00:00",1890546.040472483960912,1.890550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230242E57024N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.761556516122823,57.021327499999998]
["glac_bound",377826.000000000000000,"G223516E59453N","2008-05-01T00:00:00",3043623.691312238108367,3.043620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223516E59453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.489967025052863,59.454937999999999]
["glac_bound",377827.000000000000000,"G229032E56645N","2008-05-01T00:00:00",518227.196073002007324,0.518227000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229032E56645N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.965215553005009,56.643990000000002]
["glac_bound",377829.000000000000000,"G224510E59802N","2008-05-01T00:00:00",745500.027792398119345,0.745500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224510E59802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.490682812394084,59.803347000000002]
["glac_bound",377832.000000000000000,"G231421E56058N","2008-05-01T00:00:00",277368.206096370529849,0.277368000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231421E56058N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.577676453843992,56.058758499999996]
["glac_bound",377833.000000000000000,"G228290E57241N","2008-05-01T00:00:00",1664983.034432692453265,1.664980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228290E57241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.704905174391229,57.243498500000001]
["glac_bound",377836.000000000000000,"G227144E58491N","2008-05-01T00:00:00",353720.142641659884248,0.353720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227144E58491N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.857803748134330,58.491968999999997]
["glac_bound",377842.000000000000000,"G223487E59887N","2008-05-01T00:00:00",497758.188596790016163,0.497758000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223487E59887N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.513216288297599,59.887096999999997]
["glac_bound",377844.000000000000000,"G225335E59531N","2008-05-01T00:00:00",193746.372774386371020,0.193746000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225335E59531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.665441487668318,59.531533500000002]
["glac_bound",377845.000000000000000,"G230321E57120N","2008-05-01T00:00:00",494363.524450303521007,0.494364000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08DA230321E57120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.684754917025600,57.120259000000004]
["glac_bound",377846.000000000000000,"G230313E55618N","2008-05-01T00:00:00",906564.747909283614717,0.906565000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230313E55618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.685806851725374,55.617783000000003]
["glac_bound",377858.000000000000000,"G228619E57096N","2008-05-01T00:00:00",1064366.240825499640778,1.064370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228619E57096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.383774209227397,57.093783999999999]
["glac_bound",377862.000000000000000,"G224314E59744N","2008-05-01T00:00:00",171503.269594537094235,0.171503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224314E59744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.685861069518694,59.743792999999997]
["glac_bound",377863.000000000000000,"G227877E57343N","2008-05-01T00:00:00",1154416.849616450490430,1.154420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227877E57343N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.125643030438027,57.352499999999999]
["glac_bound",377865.000000000000000,"G227199E58487N","2008-05-01T00:00:00",94586.428062597959070,0.094586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227199E58487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.802371849498400,58.485898499999998]
["glac_bound",377870.000000000000000,"G230052E55372N","2008-05-01T00:00:00",158592.721677232271759,0.158593000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230052E55372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.950351005018746,55.374108000000000]
["glac_bound",377873.000000000000000,"G230371E56966N","2008-05-01T00:00:00",78970.009143577306531,0.078970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230371E56966N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.629889498890407,56.966249000000005]
["glac_bound",377878.000000000000000,"G230917E54921N","2008-05-01T00:00:00",166672.385913951293333,0.166672000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EG230917E54921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.083038448566811,54.921424999999999]
["glac_bound",377885.000000000000000,"G228956E56805N","2008-05-01T00:00:00",15030987.736019214615226,15.031000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228956E56805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.057894890237861,56.810974999999999]
["glac_bound",377889.000000000000000,"G227082E58113N","2008-05-01T00:00:00",4078291.254006364848465,4.078290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227082E58113N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.925426774054984,58.122190000000003]
["glac_bound",377891.000000000000000,"G230526E56694N","2008-05-01T00:00:00",120817.950106463918928,0.120818000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230526E56694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.474161159382732,56.693510500000002]
["glac_bound",377899.000000000000000,"G230493E58224N","2008-05-01T00:00:00",249018.968727925297571,0.249019000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB230493E58224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.511921224016021,58.224330000000002]
["glac_bound",377900.000000000000000,"G221783E59596N","2008-05-01T00:00:00",496072.798647232237272,0.496073000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221783E59596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.211193739099684,59.597394999999999]
["glac_bound",377908.000000000000000,"G224222E59860N","2008-05-01T00:00:00",1698177.500289941206574,1.698180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224222E59860N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.781259866052068,59.862203000000001]
["glac_bound",377910.000000000000000,"G224786E59674N","2008-05-01T00:00:00",131979.265141710318858,0.131979000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224786E59674N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.217562069403982,59.672083499999999]
["glac_bound",377912.000000000000000,"G230203E56933N","2008-05-01T00:00:00",1104752.513237069360912,1.104750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230203E56933N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.805675810529181,56.933453999999998]
["glac_bound",377913.000000000000000,"G231205E57542N","2008-05-01T00:00:00",64582.486995746468892,0.064583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231205E57542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.794820628963294,57.542574999999999]
["glac_bound",377915.000000000000000,"G226220E58675N","2008-05-01T00:00:00",110782.105749720154563,0.110782000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226220E58675N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.781356562889187,58.676286000000005]
["glac_bound",377916.000000000000000,"G230137E55823N","2008-05-01T00:00:00",189215.931203970249044,0.189216000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230137E55823N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.862416995051717,55.822974500000001]
["glac_bound",377919.000000000000000,"G230290E55750N","2008-05-01T00:00:00",235741.151179222419159,0.235741000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230290E55750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.708604797196529,55.749637999999997]
["glac_bound",377922.000000000000000,"G230173E56638N","2008-05-01T00:00:00",630481.606740862713195,0.630482000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230173E56638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.829798152419926,56.641309000000000]
["glac_bound",377925.000000000000000,"G224434E59847N","2008-05-01T00:00:00",53010.830346009133791,0.053011000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224434E59847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.565192436443823,59.847178000000000]
["glac_bound",377930.000000000000000,"G230651E56773N","2008-05-01T00:00:00",190253.620412482559914,0.190254000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230651E56773N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351119476106533,56.772912500000004]
["glac_bound",377931.000000000000000,"G226953E58244N","2008-05-01T00:00:00",59474.824733632376592,0.059475000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226953E58244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.046828946861297,58.243916999999996]
["glac_bound",377935.000000000000000,"G227908E57572N","2008-05-01T00:00:00",551402.976369398995303,0.551403000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227908E57572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.098889228663779,57.572140000000005]
["glac_bound",377938.000000000000000,"G227906E57454N","2008-05-01T00:00:00",301812.950559062883258,0.301813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227906E57454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.098452311165886,57.457110499999999]
["glac_bound",377948.000000000000000,"G221781E59607N","2008-05-01T00:00:00",2331198.026270020287484,2.331200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221781E59607N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.215525871594366,59.612314499999997]
["glac_bound",377951.000000000000000,"G223405E59592N","2008-05-01T00:00:00",125135.786438576586079,0.125136000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223405E59592N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.595130994233955,59.592486500000000]
["glac_bound",377953.000000000000000,"G227286E58193N","2008-05-01T00:00:00",574061.875977291725576,0.574062000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227286E58193N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.714011818410427,58.194549499999994]
["glac_bound",377955.000000000000000,"G222508E58988N","2008-05-01T00:00:00",182856.050566455727676,0.182856000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222508E58988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.488081160714302,58.988372499999997]
["glac_bound",377959.000000000000000,"G229498E57169N","2008-05-01T00:00:00",2019561.734719284810126,2.019560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229498E57169N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.504537877969085,57.173327000000000]
["glac_bound",377961.000000000000000,"G229892E56135N","2008-05-01T00:00:00",1006803.784966512117535,1.006800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229892E56135N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.108022711495437,56.137718000000000]
["glac_bound",377962.000000000000000,"G228730E57442N","2008-05-01T00:00:00",433118.811782301228959,0.433119000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228730E57442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.271116156725782,57.441482000000001]
["glac_bound",377967.000000000000000,"G230163E55989N","2008-05-01T00:00:00",1424530.456666765036061,1.424530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230163E55989N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.842000927955411,55.990514000000005]
["glac_bound",377973.000000000000000,"G225035E59545N","2008-05-01T00:00:00",619252.554497335921042,0.619253000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225035E59545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.966553653854447,59.544729500000003]
["glac_bound",377976.000000000000000,"G230328E55121N","2008-05-01T00:00:00",259582.521962488215650,0.259583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230328E55121N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.672642758333325,55.121431500000000]
["glac_bound",377980.000000000000000,"G227247E58077N","2008-05-01T00:00:00",6333292.119207378476858,6.333290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227247E58077N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.753462935729402,58.084156999999998]
["glac_bound",377991.000000000000000,"G230279E56347N","2008-05-01T00:00:00",3306069.024905766826123,3.306070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230279E56347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.727477272495776,56.354561500000003]
["glac_bound",377995.000000000000000,"G225601E59376N","2008-05-01T00:00:00",156505.432399955985602,0.156505000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225601E59376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.399096026129570,59.375436000000001]
["glac_bound",378009.000000000000000,"G226369E58853N","2008-05-01T00:00:00",3593466.461619639769197,3.593470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226369E58853N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.632818389492769,58.854391000000007]
["glac_bound",378013.000000000000000,"G228691E57003N","2008-05-01T00:00:00",4508054.936358819715679,4.508050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228691E57003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.307572600489465,57.015085999999997]
["glac_bound",378014.000000000000000,"G228738E57086N","2008-05-01T00:00:00",9793152.107939749956131,9.793150000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228738E57086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.273340721763674,57.100114000000005]
["glac_bound",378015.000000000000000,"G225357E59432N","2008-05-01T00:00:00",312234.589696991781238,0.312235000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225357E59432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.643713133229141,59.431840500000000]
["glac_bound",378017.000000000000000,"G227427E58311N","2008-05-01T00:00:00",5306345.737413367256522,5.306350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227427E58311N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.578806876918122,58.321091499999994]
["glac_bound",378022.000000000000000,"G226673E58637N","2008-05-01T00:00:00",321643.476659846026450,0.321643000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226673E58637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.328168335294095,58.636901999999999]
["glac_bound",378026.000000000000000,"G227018E58080N","2008-05-01T00:00:00",5910265.894167451187968,5.910270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227018E58080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.959207554442344,58.079425499999999]
["glac_bound",378030.000000000000000,"G227855E57417N","2008-05-01T00:00:00",319634.496018934354652,0.319634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227855E57417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.144897048059136,57.417022000000003]
["glac_bound",378031.000000000000000,"G230508E55006N","2008-05-01T00:00:00",51276.314654116220481,0.051276000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230508E55006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.492086244376708,55.006062499999999]
["glac_bound",378039.000000000000000,"G222450E59738N","2008-05-01T00:00:00",179328.540863564732717,0.179329000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222450E59738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.549956810567011,59.737059000000002]
["glac_bound",378040.000000000000000,"G228703E57109N","2008-05-01T00:00:00",808898.920988349127583,0.808899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228703E57109N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.299339159842532,57.107411999999997]
["glac_bound",378041.000000000000000,"G230532E55893N","2008-05-01T00:00:00",604003.586563962046057,0.604004000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230532E55893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.468055391025644,55.892739500000005]
["glac_bound",378045.000000000000000,"G229428E56906N","2008-05-01T00:00:00",495263.494452389015350,0.495263000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229428E56906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.574127369773805,56.905970999999994]
["glac_bound",378053.000000000000000,"G225954E59239N","2008-05-01T00:00:00",229296.254409180313814,0.229296000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225954E59239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.048748250133031,59.237553500000004]
["glac_bound",378055.000000000000000,"G229417E56944N","2008-05-01T00:00:00",436987.527724375424441,0.436988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229417E56944N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.583842531390133,56.942906000000001]
["glac_bound",378057.000000000000000,"G230476E54655N","2008-05-01T00:00:00",421428.709351930185221,0.421429000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230476E54655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.527865358200700,54.656622999999996]
["glac_bound",378058.000000000000000,"G222534E59790N","2008-05-01T00:00:00",615688.136792994337156,0.615688000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222534E59790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.465459663950526,59.790116499999996]
["glac_bound",378061.000000000000000,"G230366E56170N","2008-05-01T00:00:00",144968.398652950883843,0.144968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230366E56170N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.633755289675406,56.169578999999999]
["glac_bound",378063.000000000000000,"G223000E59106N","2008-05-01T00:00:00",1431123.836031147278845,1.431120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223000E59106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.002463083249211,59.105111500000000]
["glac_bound",378066.000000000000000,"G229860E57097N","2008-05-01T00:00:00",136110.261961700976826,0.136110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229860E57097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.139378915029852,57.096922000000006]
["glac_bound",378067.000000000000000,"G222213E59736N","2008-05-01T00:00:00",396405.902629354561213,0.396406000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222213E59736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.784851234736209,59.735950000000003]
["glac_bound",378068.000000000000000,"G225391E59542N","2008-05-01T00:00:00",315926.672336177201942,0.315927000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225391E59542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.611025038744458,59.542563000000001]
["glac_bound",378075.000000000000000,"G222299E59664N","2008-05-01T00:00:00",346316.636460339999758,0.346317000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222299E59664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.701026830208320,59.663893000000002]
["glac_bound",378079.000000000000000,"G230264E57170N","2008-05-01T00:00:00",503791.773093260708265,0.503792000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230264E57170N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.734843779973886,57.170048000000001]
["glac_bound",378086.000000000000000,"G230847E55023N","2008-05-01T00:00:00",216155.133353097829968,0.216155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230847E55023N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.153657570789846,55.024255499999995]
["glac_bound",378088.000000000000000,"G224287E59978N","2008-05-01T00:00:00",314145.623397147923242,0.314146000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224287E59978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.712829876460603,59.978349999999999]
["glac_bound",378092.000000000000000,"G228856E56493N","2008-05-01T00:00:00",378478.594537812867202,0.378479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228856E56493N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.145496680660386,56.493161499999999]
["glac_bound",378093.000000000000000,"G230358E55622N","2008-05-01T00:00:00",826059.843006128561683,0.826060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230358E55622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.638646670270248,55.627299000000001]
["glac_bound",378095.000000000000000,"G226435E58529N","2008-05-01T00:00:00",18717.003345003056893,0.018717000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226435E58529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.565317145437575,58.528498499999998]
["glac_bound",378096.000000000000000,"G226493E59085N","2008-05-01T00:00:00",394826.782766841759440,0.394827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226493E59085N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.507218616055070,59.085050500000001]
["glac_bound",378097.000000000000000,"G228956E57230N","2008-05-01T00:00:00",516176.951875118364114,0.516177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228956E57230N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.044329141149774,57.229947499999994]
["glac_bound",378103.000000000000000,"G228014E57033N","2008-05-01T00:00:00",68500.074388239576365,0.068500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228014E57033N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.986067078495267,57.032583500000001]
["glac_bound",378105.000000000000000,"G229977E56736N","2008-05-01T00:00:00",187929.720184394012904,0.187930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229977E56736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.021515191336618,56.735208999999998]
["glac_bound",378108.000000000000000,"G228110E57128N","2008-05-01T00:00:00",1544276.612834177445620,1.544280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228110E57128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.890753166666684,57.126608500000003]
["glac_bound",378115.000000000000000,"G228817E56485N","2008-05-01T00:00:00",4055642.279170085210353,4.055640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228817E56485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.179647653956522,56.489472500000005]
["glac_bound",378117.000000000000000,"G228803E56514N","2008-05-01T00:00:00",361853.920280765392818,0.361854000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228803E56514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.195040196285959,56.513699500000001]
["glac_bound",378123.000000000000000,"G228050E57147N","2008-05-01T00:00:00",489015.051003449130803,0.489015000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228050E57147N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.947736460548896,57.147630500000005]
["glac_bound",378124.000000000000000,"G226954E58176N","2008-05-01T00:00:00",1088225.010453688446432,1.088230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226954E58176N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.045265219167760,58.177037499999997]
["glac_bound",378125.000000000000000,"G230366E54911N","2008-05-01T00:00:00",54999.103002834519430,0.054999000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230366E54911N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.632454104519240,54.911416500000001]
["glac_bound",378126.000000000000000,"G224483E59934N","2008-05-01T00:00:00",77440.474386405636324,0.077440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224483E59934N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.516627649188422,59.933464499999999]
["glac_bound",378127.000000000000000,"G230071E55632N","2008-05-01T00:00:00",335377.441019536170643,0.335377000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230071E55632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.933843606367930,55.632910500000001]
["glac_bound",378135.000000000000000,"G227179E58472N","2008-05-01T00:00:00",164705.657410215557320,0.164706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227179E58472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.822027535543299,58.472176500000003]
["glac_bound",378142.000000000000000,"G230672E55294N","2008-05-01T00:00:00",3706456.612436943221837,3.706460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230672E55294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.318951037263417,55.296332000000000]
["glac_bound",378146.000000000000000,"G229737E56785N","2008-05-01T00:00:00",497337.304244261409622,0.497337000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229737E56785N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.263744647769869,56.785290500000002]
["glac_bound",378151.000000000000000,"G229171E56501N","2008-05-01T00:00:00",625609.984420087188482,0.625610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229171E56501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.829660223920854,56.502600000000001]
["glac_bound",378152.000000000000000,"G230259E56919N","2008-05-01T00:00:00",802713.843058879254386,0.802714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230259E56919N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.738994470297484,56.919646499999999]
["glac_bound",378153.000000000000000,"G223232E59382N","2008-05-01T00:00:00",277202.071778286946937,0.277202000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223232E59382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.766324274046440,59.382501000000005]
["glac_bound",378158.000000000000000,"G228025E57478N","2008-05-01T00:00:00",161857.804550132656004,0.161858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228025E57478N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.975004991321384,57.477868000000001]
["glac_bound",378159.000000000000000,"G229475E56416N","2008-05-01T00:00:00",50546.509752040001331,0.050547000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229475E56416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.525210658716134,56.416712000000004]
["glac_bound",378162.000000000000000,"G230689E55573N","2008-05-01T00:00:00",3832590.165780549403280,3.832590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230689E55573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.300128269851086,55.581768999999994]
["glac_bound",378171.000000000000000,"G228645E56585N","2008-05-01T00:00:00",1195486.199321251362562,1.195490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228645E56585N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.351518824254526,56.584722499999998]
["glac_bound",378176.000000000000000,"G224689E59737N","2008-05-01T00:00:00",1564283.591900538187474,1.564280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224689E59737N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.318657287709385,59.737182500000003]
["glac_bound",378186.000000000000000,"G230598E56898N","2008-05-01T00:00:00",63400.182173006294761,0.063400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230598E56898N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.402143314389036,56.897929500000004]
["glac_bound",378187.000000000000000,"G228416E56635N","2008-05-01T00:00:00",215632.663941727339989,0.215633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228416E56635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584567663811470,56.634976999999999]
["glac_bound",378191.000000000000000,"G228468E57203N","2008-05-01T00:00:00",238609.957089926028857,0.238610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228468E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.536885687270228,57.204217000000000]
["glac_bound",378193.000000000000000,"G230218E57307N","2008-05-01T00:00:00",271880.024214576580562,0.271880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230218E57307N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.782214766682557,57.307139000000006]
["glac_bound",378199.000000000000000,"G228575E57499N","2008-05-01T00:00:00",450666.204186397313606,0.450666000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228575E57499N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.426589312794647,57.498374499999997]
["glac_bound",378203.000000000000000,"G228749E57203N","2008-05-01T00:00:00",209747.119054486887762,0.209747000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228749E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.251397981210914,57.204027500000002]
["glac_bound",378208.000000000000000,"G222982E59564N","2008-05-01T00:00:00",471908.930708254687488,0.471909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222982E59564N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.020253379373401,59.563862000000000]
["glac_bound",378212.000000000000000,"G230110E57562N","2008-05-01T00:00:00",264913.456784721871372,0.264913000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230110E57562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.889023304014358,57.561735999999996]
["glac_bound",378227.000000000000000,"G223397E59465N","2008-05-01T00:00:00",392138.920644967176486,0.392139000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223397E59465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.603567440302015,59.463110000000000]
["glac_bound",378229.000000000000000,"G230741E54888N","2008-05-01T00:00:00",95124.940359616681235,0.095125000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230741E54888N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.258489955269397,54.888922000000001]
["glac_bound",378230.000000000000000,"G226739E58256N","2008-05-01T00:00:00",169421.596927960723406,0.169422000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226739E58256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.260834923190544,58.256247999999999]
["glac_bound",378232.000000000000000,"G228108E58080N","2008-05-01T00:00:00",1192152.631930842762813,1.192150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228108E58080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.888312048931084,58.084189499999994]
["glac_bound",378234.000000000000000,"G223335E59905N","2008-05-01T00:00:00",70813.026273462455720,0.070813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223335E59905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.664391367509381,59.905055500000003]
["glac_bound",378240.000000000000000,"G226946E58360N","2008-05-01T00:00:00",1648478.504174234578386,1.648480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226946E58360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.061852035288268,58.361318499999996]
["glac_bound",378241.000000000000000,"G230672E55669N","2008-05-01T00:00:00",2343216.435826711356640,2.343220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230672E55669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.326848920627612,55.672041499999999]
["glac_bound",378242.000000000000000,"G228047E56949N","2008-05-01T00:00:00",16005984.744228912517428,16.006000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228047E56949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.973245948889542,56.954770499999995]
["glac_bound",378247.000000000000000,"G230107E56868N","2008-05-01T00:00:00",58023.399776690348517,0.058023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230107E56868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.892333370107565,56.868341000000001]
["glac_bound",378250.000000000000000,"G230806E57329N","2008-05-01T00:00:00",704961.507955377339385,0.704961000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230806E57329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.197703977299227,57.329180500000000]
["glac_bound",378253.000000000000000,"G228379E56671N","2008-05-01T00:00:00",77392.104781193600502,0.077392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228379E56671N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.621066113167842,56.671507500000004]
["glac_bound",378254.000000000000000,"G223436E59928N","2008-05-01T00:00:00",299191.822185321419965,0.299192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223436E59928N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.559666114515181,59.928100499999999]
["glac_bound",378256.000000000000000,"G226456E58718N","2008-05-01T00:00:00",275915.867863653344102,0.275916000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226456E58718N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.542435327327212,58.718718499999994]
["glac_bound",378258.000000000000000,"G229526E56249N","2008-05-01T00:00:00",1548435.019628306385130,1.548430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229526E56249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.477446635960149,56.249662000000001]
["glac_bound",378260.000000000000000,"G221971E59924N","2008-05-01T00:00:00",2526693.182693071663380,2.526690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221971E59924N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.032252393947601,59.925814500000001]
["glac_bound",378264.000000000000000,"G224153E59774N","2008-05-01T00:00:00",799107.853878352325410,0.799108000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224153E59774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.835906188183912,59.773823000000000]
["glac_bound",378265.000000000000000,"G229127E57085N","2008-05-01T00:00:00",3817425.974587878212333,3.817430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229127E57085N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.873266265622192,57.092772499999995]
["glac_bound",378271.000000000000000,"G225705E59148N","2008-05-01T00:00:00",153247.785142757638823,0.153248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225705E59148N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.296466563155036,59.148236499999996]
["glac_bound",378275.000000000000000,"G229025E57134N","2008-05-01T00:00:00",151384.561919503845274,0.151385000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229025E57134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.976768766062037,57.131833499999999]
["glac_bound",378277.000000000000000,"G230139E56209N","2008-05-01T00:00:00",2394286.242374412249774,2.394290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230139E56209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.860371374450551,56.211884999999995]
["glac_bound",378283.000000000000000,"G228030E58032N","2008-05-01T00:00:00",342575.006416616728529,0.342575000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228030E58032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.970243537796364,58.032834999999999]
["glac_bound",378289.000000000000000,"G228003E57636N","2008-05-01T00:00:00",718912.888271320727654,0.718913000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228003E57636N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.005950024995741,57.642568999999995]
["glac_bound",378290.000000000000000,"G228848E56486N","2008-05-01T00:00:00",1311621.517983866389841,1.311620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228848E56486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.155041665779947,56.486272499999998]
["glac_bound",378297.000000000000000,"G230552E57014N","2008-05-01T00:00:00",1891749.006626048823819,1.891750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230552E57014N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.448704438715907,57.022450499999998]
["glac_bound",378298.000000000000000,"G227591E58243N","2008-05-01T00:00:00",966202.587802787660621,0.966203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227591E58243N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.400948598772686,58.244965000000001]
["glac_bound",378302.000000000000000,"G229554E56762N","2008-05-01T00:00:00",266505.958142197749112,0.266506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229554E56762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.446420743861125,56.762041500000002]
["glac_bound",378304.000000000000000,"G228786E57348N","2008-05-01T00:00:00",1441953.657179710222408,1.441950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228786E57348N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.216274842920342,57.347921499999998]
["glac_bound",378308.000000000000000,"G226838E58302N","2008-05-01T00:00:00",166546.217390815552790,0.166546000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226838E58302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.164063369189847,58.304799000000003]
["glac_bound",378311.000000000000000,"G230047E56103N","2008-05-01T00:00:00",100102.925474436779041,0.100103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230047E56103N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.953169771322280,56.102391999999995]
["glac_bound",378315.000000000000000,"G224269E59988N","2008-05-01T00:00:00",651170.679821810219437,0.651171000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224269E59988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.731437292383305,59.991650499999999]
["glac_bound",378316.000000000000000,"G230154E57202N","2008-05-01T00:00:00",120180.819117471604841,0.120181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230154E57202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.845964500832650,57.202278000000000]
["glac_bound",378318.000000000000000,"G230034E55448N","2008-05-01T00:00:00",415755.119641533237882,0.415755000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230034E55448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.968576457881767,55.448623999999995]
["glac_bound",378321.000000000000000,"G230392E56963N","2008-05-01T00:00:00",433189.669713295705151,0.433190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230392E56963N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.607061003193564,56.963611999999998]
["glac_bound",378323.000000000000000,"G229044E56536N","2008-05-01T00:00:00",14268669.327965678647161,14.268700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229044E56536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.987719129358709,56.553887000000003]
["glac_bound",378326.000000000000000,"G225889E59305N","2008-05-01T00:00:00",674935.192551267915405,0.674935000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225889E59305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.111234694470113,59.304127999999999]
["glac_bound",378328.000000000000000,"G231710E57222N","2008-05-01T00:00:00",412840.076314343663398,0.412840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231710E57222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.291085783863082,57.222304500000000]
["glac_bound",378330.000000000000000,"G228496E57353N","2008-05-01T00:00:00",649409.858931577182375,0.649410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228496E57353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.502839871868048,57.352913500000000]
["glac_bound",378335.000000000000000,"G223136E59630N","2008-05-01T00:00:00",502960.188276943401434,0.502960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223136E59630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.869788585850159,59.630223999999998]
["glac_bound",378336.000000000000000,"G226408E58940N","2008-05-01T00:00:00",458066.027222527191043,0.458066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226408E58940N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.594479403490141,58.939960999999997]
["glac_bound",378341.000000000000000,"G230070E55663N","2008-05-01T00:00:00",1295219.440150196198374,1.295220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230070E55663N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.928740466157194,55.664788500000000]
["glac_bound",378342.000000000000000,"G229960E57045N","2008-05-01T00:00:00",368524.416156335850246,0.368524000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229960E57045N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.040623038400867,57.044862000000002]
["glac_bound",378347.000000000000000,"G229727E56729N","2008-05-01T00:00:00",2803785.222277286928147,2.803790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229727E56729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.279215766234756,56.729609499999995]
["glac_bound",378351.000000000000000,"G222067E59842N","2008-05-01T00:00:00",4338531.393590028397739,4.338530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222067E59842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.921601442900169,59.842584500000001]
["glac_bound",378353.000000000000000,"G230311E55754N","2008-05-01T00:00:00",906924.904235035530291,0.906925000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230311E55754N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.690600309826550,55.752752500000000]
["glac_bound",378357.000000000000000,"G226726E58234N","2008-05-01T00:00:00",731458.342995712184347,0.731458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226726E58234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.274213929710584,58.234279999999998]
["glac_bound",378358.000000000000000,"G227063E58426N","2008-05-01T00:00:00",542331.617634123656899,0.542332000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227063E58426N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.937941794549772,58.426569000000001]
["glac_bound",378367.000000000000000,"G225241E59462N","2008-05-01T00:00:00",90476.863500353836571,0.090477000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225241E59462N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.760298480274969,59.462253500000003]
["glac_bound",378371.000000000000000,"G228997E57249N","2008-05-01T00:00:00",430036.361286402214319,0.430036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228997E57249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.001718619815676,57.248272999999998]
["glac_bound",378376.000000000000000,"G230676E56880N","2008-05-01T00:00:00",56874.067734673204541,0.056874000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230676E56880N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.323558884008520,56.880537500000003]
["glac_bound",378377.000000000000000,"G226860E58341N","2008-05-01T00:00:00",131585.573279335076222,0.131586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226860E58341N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.139735188562099,58.340761499999999]
["glac_bound",378378.000000000000000,"G229604E57215N","2008-05-01T00:00:00",266617.006631169526372,0.266617000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229604E57215N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.394035086137023,57.214348000000001]
["glac_bound",378380.000000000000000,"G222997E59416N","2008-05-01T00:00:00",396685.519158479990438,0.396686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222997E59416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.005237016573346,59.416223500000001]
["glac_bound",378382.000000000000000,"G224648E59767N","2008-05-01T00:00:00",418848.656714367796667,0.418849000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224648E59767N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.351483321785452,59.766756000000001]
["glac_bound",378386.000000000000000,"G225620E59349N","2008-05-01T00:00:00",1079842.605217866599560,1.079840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225620E59349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.375015637758395,59.347377999999999]
["glac_bound",378388.000000000000000,"G227951E57069N","2008-05-01T00:00:00",104350820.34950499236583,104.350999999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Flood Glacier","None","08CF227951E57069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.136334966134172,57.117905000000000]
["glac_bound",378389.000000000000000,"G230701E56766N","2008-05-01T00:00:00",85944.550676008817391,0.085944000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230701E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.299162247659183,56.766007999999999]
["glac_bound",378393.000000000000000,"G226842E58545N","2008-05-01T00:00:00",102478.775344142981339,0.102479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226842E58545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.158819147236670,58.547307000000004]
["glac_bound",378400.000000000000000,"G226494E58752N","2008-05-01T00:00:00",875912.125229596742429,0.875912000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226494E58752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.505446745735753,58.754621000000000]
["glac_bound",378405.000000000000000,"G229443E56918N","2008-05-01T00:00:00",888670.473447468015365,0.888670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229443E56918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.558544590090094,56.917729999999999]
["glac_bound",378408.000000000000000,"G229815E56148N","2008-05-01T00:00:00",82501140.812523856759071,82.501099999999994,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229815E56148N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.210034989520523,56.149338999999998]
["glac_bound",378410.000000000000000,"G227605E58367N","2008-05-01T00:00:00",59161.802859982068185,0.059162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227605E58367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.392711874981359,58.365489499999995]
["glac_bound",378420.000000000000000,"G229072E56401N","2008-05-01T00:00:00",63023.262105863417673,0.063023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229072E56401N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.926350032202237,56.401418000000000]
["glac_bound",378422.000000000000000,"G221708E59638N","2008-05-01T00:00:00",4686347.261010713875294,4.686350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221708E59638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.325719345823984,59.621165500000004]
["glac_bound",378423.000000000000000,"G223610E59770N","2008-05-01T00:00:00",175178.017507496697363,0.175178000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223610E59770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.391178757352947,59.770195000000001]
["glac_bound",378426.000000000000000,"G221845E59936N","2008-05-01T00:00:00",3289085.008878871332854,3.289080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221845E59936N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.161104333435219,59.933599500000000]
["glac_bound",378428.000000000000000,"G227982E57639N","2008-05-01T00:00:00",1179122.653820267645642,1.179120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227982E57639N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.022468798848564,57.642933999999997]
["glac_bound",378433.000000000000000,"G227676E58089N","2008-05-01T00:00:00",1375922.853024205658585,1.375920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227676E58089N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.327874003916406,58.094283000000004]
["glac_bound",378436.000000000000000,"G229630E56185N","2008-05-01T00:00:00",789620.095526647404768,0.789620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229630E56185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.369688089826866,56.192878499999999]
["glac_bound",378440.000000000000000,"G223178E59714N","2008-05-01T00:00:00",1755387.843839251669124,1.755390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223178E59714N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.824689729301952,59.715856500000001]
["glac_bound",378442.000000000000000,"G225615E59450N","2008-05-01T00:00:00",169649.598345215257723,0.169650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225615E59450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.390510695143860,59.450237000000001]
["glac_bound",378443.000000000000000,"G227698E57887N","2008-05-01T00:00:00",64398.555348854140902,0.064399000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227698E57887N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.302034534375764,57.887247000000002]
["glac_bound",378444.000000000000000,"G229734E56512N","2008-05-01T00:00:00",53943.952192392192956,0.053944000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229734E56512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.265587798941738,56.512480499999995]
["glac_bound",378449.000000000000000,"G230734E55680N","2008-05-01T00:00:00",521891.233705340535380,0.521891000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230734E55680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.266285564011810,55.679881500000000]
["glac_bound",378450.000000000000000,"G222172E59713N","2008-05-01T00:00:00",4265223.226402230560780,4.265220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222172E59713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.805466160270385,59.725348499999996]
["glac_bound",378452.000000000000000,"G226730E58249N","2008-05-01T00:00:00",420980.563146868778858,0.420981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226730E58249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.268421901883244,58.249476999999999]
["glac_bound",378456.000000000000000,"G228362E57443N","2008-05-01T00:00:00",718917.429884495562874,0.718917000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228362E57443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.629970379618612,57.440718000000004]
["glac_bound",378458.000000000000000,"G227414E58408N","2008-05-01T00:00:00",579475.885297424159944,0.579476000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227414E58408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.590281672312869,58.411609499999997]
["glac_bound",378461.000000000000000,"G230468E57096N","2008-05-01T00:00:00",166322.572660712990910,0.166323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230468E57096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.531977016418864,57.095304499999997]
["glac_bound",378464.000000000000000,"G226892E58617N","2008-05-01T00:00:00",793343.347281528520398,0.793343000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226892E58617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.108354625467712,58.618398499999998]
["glac_bound",378468.000000000000000,"G223825E59756N","2008-05-01T00:00:00",271748.173310682235751,0.271748000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223825E59756N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.175795460643599,59.756178000000006]
["glac_bound",378469.000000000000000,"G223360E59544N","2008-05-01T00:00:00",1130409.078215288696811,1.130410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223360E59544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.639625549234154,59.542972500000005]
["glac_bound",378470.000000000000000,"G228528E57572N","2008-05-01T00:00:00",541938.534057586221024,0.541939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228528E57572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.477233058877118,57.573929499999998]
["glac_bound",378472.000000000000000,"G226035E59010N","2008-05-01T00:00:00",417486.228866125049535,0.417486000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226035E59010N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.969740046180704,59.010511000000001]
["glac_bound",378479.000000000000000,"G227207E58048N","2008-05-01T00:00:00",2181219.054139399435371,2.181220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227207E58048N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.792208913692150,58.056251000000003]
["glac_bound",378480.000000000000000,"G230567E54735N","2008-05-01T00:00:00",110613.918763740264694,0.110614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230567E54735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.432967251920616,54.734800499999999]
["glac_bound",378484.000000000000000,"G230045E56065N","2008-05-01T00:00:00",172401.474904286558740,0.172401000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230045E56065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.955915588631143,56.064722500000002]
["glac_bound",378486.000000000000000,"G229819E56191N","2008-05-01T00:00:00",86303.736031857843045,0.086304000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229819E56191N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.180259468548400,56.191347000000000]
["glac_bound",378490.000000000000000,"G230697E56909N","2008-05-01T00:00:00",55449.418981098941003,0.055449000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230697E56909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.305201791821560,56.910037000000003]
["glac_bound",378491.000000000000000,"G226771E58447N","2008-05-01T00:00:00",66640.247700113308383,0.066640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226771E58447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.228546118645909,58.447361999999998]
["glac_bound",378493.000000000000000,"G228507E57292N","2008-05-01T00:00:00",63251.419931197982805,0.063251000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228507E57292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.492726112986588,57.291847500000003]
["glac_bound",378499.000000000000000,"G222465E59994N","2008-05-01T00:00:00",151691.162901011673966,0.151691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222465E59994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.536287863856501,59.993550499999998]
["glac_bound",378502.000000000000000,"G226244E58746N","2008-05-01T00:00:00",205294.749862280004891,0.205295000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226244E58746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.757864372854783,58.748940500000003]
["glac_bound",378503.000000000000000,"G230455E56672N","2008-05-01T00:00:00",106806.932088573405053,0.106807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230455E56672N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.545691578239030,56.671644499999999]
["glac_bound",378507.000000000000000,"G229589E57206N","2008-05-01T00:00:00",213937.192110290576238,0.213937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229589E57206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.409697539812242,57.206341499999994]
["glac_bound",378508.000000000000000,"G232055E58382N","2008-05-01T00:00:00",190275.501068294281140,0.190276000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-15T00:00:00","okay","None","None","08CA232055E58382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.943455122346307,58.381552499999998]
["glac_bound",378511.000000000000000,"G229161E56390N","2008-05-01T00:00:00",583644.644450179883279,0.583645000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229161E56390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.835638590116275,56.388625500000003]
["glac_bound",378514.000000000000000,"G227828E58075N","2008-05-01T00:00:00",176388.141491602465976,0.176388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227828E58075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.172817624115339,58.074629000000002]
["glac_bound",378515.000000000000000,"G227607E58371N","2008-05-01T00:00:00",75401.595989851397462,0.075402000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227607E58371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.393038634706500,58.371608000000002]
["glac_bound",378518.000000000000000,"G225455E59360N","2008-05-01T00:00:00",227040.797927985258866,0.227041000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225455E59360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.544327631310466,59.358755500000001]
["glac_bound",378520.000000000000000,"G225699E59278N","2008-05-01T00:00:00",371443.452932927757502,0.371443000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225699E59278N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.299972892369027,59.277645000000000]
["glac_bound",378522.000000000000000,"G229351E57738N","2008-05-01T00:00:00",2758304.764817350078374,2.758300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229351E57738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.651947614015597,57.748815499999999]
["glac_bound",378523.000000000000000,"G227035E58002N","2008-05-01T00:00:00",1066894.028865115018561,1.066890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227035E58002N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.961051699898604,58.003743999999998]
["glac_bound",378525.000000000000000,"G227261E57969N","2008-05-01T00:00:00",13298702.795882457867265,13.298700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227261E57969N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.716034488995831,57.979063500000002]
["glac_bound",378528.000000000000000,"G231473E56082N","2008-05-01T00:00:00",343955.593981716083363,0.343956000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231473E56082N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.522892243094873,56.082812500000003]
["glac_bound",378531.000000000000000,"G227341E58089N","2008-05-01T00:00:00",1179234.186820530798286,1.179230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227341E58089N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.663360382746191,58.091574500000000]
["glac_bound",378535.000000000000000,"G225703E59273N","2008-05-01T00:00:00",305786.451705999148544,0.305786000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225703E59273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.297515046123550,59.272845000000004]
["glac_bound",378538.000000000000000,"G230392E56720N","2008-05-01T00:00:00",271647.634977780515328,0.271648000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230392E56720N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.606749464760640,56.720148500000001]
["glac_bound",378539.000000000000000,"G228573E57053N","2008-05-01T00:00:00",1376643.605555054731667,1.376640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228573E57053N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.432744045237399,57.047595000000001]
["glac_bound",378540.000000000000000,"G225510E59573N","2008-05-01T00:00:00",50423.950464732231922,0.050424000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225510E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.489035264744189,59.572761499999999]
["glac_bound",378544.000000000000000,"G230230E54527N","2008-05-01T00:00:00",741495.533666830975562,0.741496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230230E54527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.767460543411715,54.526025000000004]
["glac_bound",378545.000000000000000,"G228682E56565N","2008-05-01T00:00:00",953072.663955328054726,0.953073000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228682E56565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.315817574723098,56.570058500000002]
["glac_bound",378546.000000000000000,"G225485E59468N","2008-05-01T00:00:00",899693.295116479159333,0.899693000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225485E59468N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.511535076133953,59.468101500000003]
["glac_bound",378549.000000000000000,"G229897E56969N","2008-05-01T00:00:00",442082.544140748446807,0.442083000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229897E56969N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.103572485866096,56.969050000000003]
["glac_bound",378555.000000000000000,"G222515E59608N","2008-05-01T00:00:00",209179.403587306413101,0.209179000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222515E59608N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.485138753546096,59.608119000000002]
["glac_bound",378556.000000000000000,"G228948E57541N","2008-05-01T00:00:00",215763.501275379909202,0.215763000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228948E57541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.053128332422716,57.540703499999999]
["glac_bound",378558.000000000000000,"G230817E57280N","2008-05-01T00:00:00",2324254.630814605858177,2.324250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230817E57280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.180165933315777,57.280247000000003]
["glac_bound",378561.000000000000000,"G223258E59755N","2008-05-01T00:00:00",3189295.609984056092799,3.189300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223258E59755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.735185174324329,59.758985000000003]
["glac_bound",378568.000000000000000,"G221387E59870N","2008-05-01T00:00:00",92815.030702765303431,0.092815000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221387E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.612445208967159,59.869193999999993]
["glac_bound",378570.000000000000000,"G229531E56733N","2008-05-01T00:00:00",104839.575061629628181,0.104840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229531E56733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.471113487283958,56.732588000000000]
["glac_bound",378574.000000000000000,"G228280E57256N","2008-05-01T00:00:00",278033.783236699237023,0.278034000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228280E57256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.720582608213647,57.255497000000005]
["glac_bound",378575.000000000000000,"G228788E56614N","2008-05-01T00:00:00",88168.570897948971833,0.088169000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228788E56614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.211272794169616,56.615088999999998]
["glac_bound",378580.000000000000000,"G222102E59527N","2008-05-01T00:00:00",594438.258894077735022,0.594438000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222102E59527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.899549465177699,59.526752999999999]
["glac_bound",378581.000000000000000,"G229253E56894N","2008-05-01T00:00:00",268772.380193181976210,0.268772000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229253E56894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.749253739175941,56.895466999999996]
["glac_bound",378592.000000000000000,"G225350E59244N","2008-05-01T00:00:00",8851977.906421605497599,8.851979999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225350E59244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.675511472231335,59.241560499999999]
["glac_bound",378595.000000000000000,"G228454E57195N","2008-05-01T00:00:00",301625.067909146251623,0.301625000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228454E57195N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.545711401910523,57.199043000000003]
["glac_bound",378600.000000000000000,"G228475E57518N","2008-05-01T00:00:00",468764.060547989327461,0.468764000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228475E57518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.523461063498758,57.520611000000002]
["glac_bound",378605.000000000000000,"G230126E56883N","2008-05-01T00:00:00",276048.976949454634450,0.276049000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230126E56883N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.874250995286218,56.882933999999999]
["glac_bound",378607.000000000000000,"G224821E59688N","2008-05-01T00:00:00",701379.384808684466407,0.701379000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224821E59688N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.180302026191271,59.691332000000003]
["glac_bound",378609.000000000000000,"G221884E59541N","2008-05-01T00:00:00",1147885.469831326045096,1.147890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221884E59541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.125522817690012,59.541606500000000]
["glac_bound",378617.000000000000000,"G230009E57357N","2008-05-01T00:00:00",461320.936419037810992,0.461321000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230009E57357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.997820153406167,57.358496500000001]
["glac_bound",378619.000000000000000,"G230625E56820N","2008-05-01T00:00:00",175333.886750303063309,0.175334000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230625E56820N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.375282404833939,56.820070000000001]
["glac_bound",378620.000000000000000,"G227336E58201N","2008-05-01T00:00:00",733337.946030138526112,0.733338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227336E58201N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.663135784147272,58.201295500000001]
["glac_bound",378622.000000000000000,"G226997E58120N","2008-05-01T00:00:00",1364086.984657163964584,1.364090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226997E58120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.003515807851244,58.124578999999997]
["glac_bound",378623.000000000000000,"G229553E57150N","2008-05-01T00:00:00",391990.339665992825758,0.391990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229553E57150N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.446035478607200,57.149489500000001]
["glac_bound",378624.000000000000000,"G229502E57282N","2008-05-01T00:00:00",383964.943499100103509,0.383965000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229502E57282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.501682703411234,57.283451499999998]
["glac_bound",378631.000000000000000,"G229335E57711N","2008-05-01T00:00:00",7126325.845613494515419,7.126330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229335E57711N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.663014346473005,57.719041000000004]
["glac_bound",378632.000000000000000,"G228051E57473N","2008-05-01T00:00:00",96331.833144271775382,0.096332000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228051E57473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.949791040201660,57.472233500000002]
["glac_bound",378635.000000000000000,"G230250E57177N","2008-05-01T00:00:00",94663.615217135171406,0.094664000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230250E57177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.751102794309247,57.177195499999996]
["glac_bound",378638.000000000000000,"G230415E55632N","2008-05-01T00:00:00",1214604.700941993156448,1.214600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230415E55632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.589287401534534,55.628597499999998]
["glac_bound",378657.000000000000000,"G230840E56503N","2008-05-01T00:00:00",146759.324321413470898,0.146759000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230840E56503N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.160023810031277,56.502825999999999]
["glac_bound",378658.000000000000000,"G225744E59177N","2008-05-01T00:00:00",123382.604836069600424,0.123383000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225744E59177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.255419577076850,59.176220000000001]
["glac_bound",378660.000000000000000,"G227561E57629N","2008-05-01T00:00:00",11051258.412975180894136,11.051299999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227561E57629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.476017389698313,57.634803000000005]
["glac_bound",378666.000000000000000,"G223840E59789N","2008-05-01T00:00:00",753204.504518889705651,0.753205000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223840E59789N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.157846574665314,59.790397999999996]
["glac_bound",378667.000000000000000,"G227484E58246N","2008-05-01T00:00:00",371408.489545175747480,0.371408000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227484E58246N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.517440545142051,58.246368000000004]
["glac_bound",378668.000000000000000,"G230489E56020N","2008-05-01T00:00:00",281462.061267110519111,0.281462000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230489E56020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.510281096297888,56.021050500000001]
["glac_bound",378669.000000000000000,"G222318E59532N","2008-05-01T00:00:00",712551.443872259580530,0.712551000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222318E59532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.683635817668375,59.531185000000001]
["glac_bound",378671.000000000000000,"G221790E59736N","2008-05-01T00:00:00",1145060.067355796461925,1.145060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221790E59736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.208612931567700,59.736104499999996]
["glac_bound",378678.000000000000000,"G228589E57433N","2008-05-01T00:00:00",327580.083355048671365,0.327580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228589E57433N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.413113165713781,57.433014000000000]
["glac_bound",378680.000000000000000,"G227233E58059N","2008-05-01T00:00:00",2457843.595398624427617,2.457840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227233E58059N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.768246620995740,58.056256500000003]
["glac_bound",378683.000000000000000,"G226211E58787N","2008-05-01T00:00:00",1819067.422708553494886,1.819070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226211E58787N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.789613474627970,58.794770499999998]
["glac_bound",378697.000000000000000,"G230376E56242N","2008-05-01T00:00:00",5984356.821272668428719,5.984360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230376E56242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.631027701436778,56.250899500000003]
["glac_bound",378698.000000000000000,"G231464E56202N","2008-05-01T00:00:00",143438.173727361718193,0.143438000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231464E56202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.535038907309314,56.201995499999995]
["glac_bound",378701.000000000000000,"G230044E56158N","2008-05-01T00:00:00",115624.025145971056190,0.115624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230044E56158N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.953865131396924,56.159537499999999]
["glac_bound",378702.000000000000000,"G227292E58368N","2008-05-01T00:00:00",3152432.547761073336005,3.152430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227292E58368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.717595971691253,58.368870999999999]
["glac_bound",378706.000000000000000,"G230647E55526N","2008-05-01T00:00:00",72537.322551284771180,0.072537000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230647E55526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351476113992646,55.527479499999998]
["glac_bound",378712.000000000000000,"G221985E59916N","2008-05-01T00:00:00",83524.879769062157720,0.083525000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221985E59916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.015630424765931,59.915300500000001]
["glac_bound",378716.000000000000000,"G229384E57689N","2008-05-01T00:00:00",4423030.648569198325276,4.423030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229384E57689N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.628479599729815,57.703113999999999]
["glac_bound",378717.000000000000000,"G222231E59947N","2008-05-01T00:00:00",347222.645945278869476,0.347223000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222231E59947N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.768652461280880,59.946184000000002]
["glac_bound",378723.000000000000000,"G229978E56543N","2008-05-01T00:00:00",83659.655378682451556,0.083660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229978E56543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.020110907763751,56.543305000000004]
["glac_bound",378725.000000000000000,"G229826E56543N","2008-05-01T00:00:00",75071.700345445118728,0.075072000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229826E56543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.175477479519316,56.545286000000004]
["glac_bound",378728.000000000000000,"G230706E57255N","2008-05-01T00:00:00",349377.403490560420323,0.349377000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230706E57255N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.295069215522403,57.254815000000001]
["glac_bound",378729.000000000000000,"G230621E56639N","2008-05-01T00:00:00",111301.819774607691215,0.111302000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230621E56639N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.379414041154774,56.639443000000000]
["glac_bound",378730.000000000000000,"G226905E58137N","2008-05-01T00:00:00",374047.736535955395084,0.374048000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226905E58137N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.096774693786983,58.137858500000000]
["glac_bound",378731.000000000000000,"G230176E56067N","2008-05-01T00:00:00",779643.725893777795136,0.779644000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230176E56067N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.832629670577717,56.063333000000000]
["glac_bound",378734.000000000000000,"G223725E59982N","2008-05-01T00:00:00",141905.067839287687093,0.141905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223725E59982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.274513102437027,59.981457000000006]
["glac_bound",378736.000000000000000,"G229164E56431N","2008-05-01T00:00:00",5510015.760802160017192,5.510020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229164E56431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.853393065238720,56.439696499999997]
["glac_bound",378746.000000000000000,"G222074E59859N","2008-05-01T00:00:00",938753.062785617541522,0.938753000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222074E59859N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.937401454953601,59.862025000000003]
["glac_bound",378750.000000000000000,"G228889E57029N","2008-05-01T00:00:00",511219.630221166764386,0.511220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228889E57029N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.105240998322216,57.030916000000005]
["glac_bound",378753.000000000000000,"G227662E58016N","2008-05-01T00:00:00",10989776.843609571456909,10.989800000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227662E58016N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.352572585168446,58.030343000000002]
["glac_bound",378760.000000000000000,"G228012E57211N","2008-05-01T00:00:00",1232159.205800264142454,1.232160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228012E57211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.995151000799893,57.217113999999995]
["glac_bound",378763.000000000000000,"G224228E59910N","2008-05-01T00:00:00",79581.283493526017992,0.079581000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224228E59910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.771946666958371,59.910350500000000]
["glac_bound",378770.000000000000000,"G230412E56764N","2008-05-01T00:00:00",194290.388319556426723,0.194290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230412E56764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.587484697151410,56.763925499999999]
["glac_bound",378773.000000000000000,"G230815E56463N","2008-05-01T00:00:00",3271779.174149380996823,3.271780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230815E56463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.183806796473334,56.463565500000001]
["glac_bound",378774.000000000000000,"G230240E54525N","2008-05-01T00:00:00",911104.454095413559116,0.911104000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230240E54525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.760673570212759,54.527332000000001]
["glac_bound",378775.000000000000000,"G230592E56703N","2008-05-01T00:00:00",945046.814575612195767,0.945047000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230592E56703N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.412732052682600,56.705383499999996]
["glac_bound",378778.000000000000000,"G223964E59995N","2008-05-01T00:00:00",1503415.762423017062247,1.503420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223964E59995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.035777240291253,59.996777500000000]
["glac_bound",378779.000000000000000,"G227635E57942N","2008-05-01T00:00:00",1261343.426371267065406,1.261340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227635E57942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.367972421691093,57.940668000000002]
["glac_bound",378782.000000000000000,"G227694E57788N","2008-05-01T00:00:00",4697738.656968934461474,4.697740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227694E57788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.305045878032473,57.790831499999996]
["glac_bound",378784.000000000000000,"G229458E56401N","2008-05-01T00:00:00",746961.886712496634573,0.746962000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229458E56401N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.550362879646855,56.403698500000004]
["glac_bound",378789.000000000000000,"G228801E57445N","2008-05-01T00:00:00",100300.828757412687992,0.100301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228801E57445N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.200540774038473,57.445519000000004]
["glac_bound",378790.000000000000000,"G227484E58040N","2008-05-01T00:00:00",109710.584096446691547,0.109711000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227484E58040N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.515515675414377,58.039793000000003]
["glac_bound",378791.000000000000000,"G223270E59467N","2008-05-01T00:00:00",666497.045044115046039,0.666497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223270E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.726813729545256,59.470710999999994]
["glac_bound",378795.000000000000000,"G227488E57865N","2008-05-01T00:00:00",1399423.380702323513106,1.399420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227488E57865N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.511514306453194,57.864784000000000]
["glac_bound",378796.000000000000000,"G221727E59901N","2008-05-01T00:00:00",4099000.393686628900468,4.099000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221727E59901N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.289846051850020,59.903629000000002]
["glac_bound",378800.000000000000000,"G221916E59540N","2008-05-01T00:00:00",607256.714839772670530,0.607257000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221916E59540N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.082292813548378,59.541505000000001]
["glac_bound",378802.000000000000000,"G229273E56460N","2008-05-01T00:00:00",51496.097143057217181,0.051496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229273E56460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.724877782710280,56.459549500000001]
["glac_bound",378806.000000000000000,"G227703E57920N","2008-05-01T00:00:00",117578.281375735241454,0.117578000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227703E57920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.296348611251517,57.921638999999999]
["glac_bound",378812.000000000000000,"G227912E57453N","2008-05-01T00:00:00",245427.646014426398324,0.245428000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227912E57453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.087370960673326,57.453242500000002]
["glac_bound",378814.000000000000000,"G230218E57184N","2008-05-01T00:00:00",111500.636996793429716,0.111501000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230218E57184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.781987784217563,57.183299000000005]
["glac_bound",378821.000000000000000,"G226946E58349N","2008-05-01T00:00:00",1452027.131613048492000,1.452030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226946E58349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.055754457880511,58.349663499999998]
["glac_bound",378823.000000000000000,"G230491E56273N","2008-05-01T00:00:00",351617.837477589549962,0.351618000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230491E56273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.509265464134813,56.277144000000000]
["glac_bound",378826.000000000000000,"G230085E55705N","2008-05-01T00:00:00",102509.839146894650185,0.102510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230085E55705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.917696287038950,55.703799500000002]
["glac_bound",378827.000000000000000,"G226482E58762N","2008-05-01T00:00:00",396179.557701780169737,0.396180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226482E58762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.518799356627795,58.763883499999999]
["glac_bound",378829.000000000000000,"G230736E55657N","2008-05-01T00:00:00",114623.614708087363397,0.114624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230736E55657N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.265718103689210,55.655407499999995]
["glac_bound",378832.000000000000000,"G226511E58742N","2008-05-01T00:00:00",930117.205102392705157,0.930117000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226511E58742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.495485385029355,58.745829000000001]
["glac_bound",378834.000000000000000,"G228812E57516N","2008-05-01T00:00:00",477012.899421168898698,0.477013000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228812E57516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.187793636645125,57.515482500000005]
["glac_bound",378838.000000000000000,"G225606E59317N","2008-05-01T00:00:00",179014.936671016883338,0.179015000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225606E59317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.394415883252435,59.317024500000002]
["glac_bound",378839.000000000000000,"G225710E59354N","2008-05-01T00:00:00",345484.631993025541306,0.345485000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225710E59354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.288711507731961,59.353555999999998]
["glac_bound",378844.000000000000000,"G224839E59927N","2008-05-01T00:00:00",747245.051743276417255,0.747245000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224839E59927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.163212689814230,59.926138500000000]
["glac_bound",378845.000000000000000,"G230183E57080N","2008-05-01T00:00:00",261802.882106448843842,0.261803000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230183E57080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.816209560887501,57.080264499999998]
["glac_bound",378852.000000000000000,"G228390E56961N","2008-05-01T00:00:00",76084.068124684956274,0.076084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228390E56961N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.609386554556096,56.960487999999998]
["glac_bound",378854.000000000000000,"G227662E57590N","2008-05-01T00:00:00",1119762.455355112906545,1.119760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227662E57590N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.339721120968477,57.590970499999997]
["glac_bound",378856.000000000000000,"G225443E59343N","2008-05-01T00:00:00",388410.117278157966211,0.388410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225443E59343N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.557485718328849,59.342940999999996]
["glac_bound",378857.000000000000000,"G223034E59517N","2008-05-01T00:00:00",527956.336640943423845,0.527956000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223034E59517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.964840895027635,59.517465000000001]
["glac_bound",378870.000000000000000,"G230422E56073N","2008-05-01T00:00:00",798843.533664496848360,0.798844000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230422E56073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.575326355444417,56.079716500000004]
["glac_bound",378874.000000000000000,"G230129E56315N","2008-05-01T00:00:00",96211.227732358689536,0.096211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230129E56315N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.870989717604857,56.314583499999998]
["glac_bound",378880.000000000000000,"G227765E58033N","2008-05-01T00:00:00",1084350.913106762571260,1.084350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227765E58033N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.230848806093434,58.033689500000001]
["glac_bound",378884.000000000000000,"G230573E54858N","2008-05-01T00:00:00",295574.519375736708753,0.295575000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230573E54858N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.429430531107357,54.858979500000004]
["glac_bound",378891.000000000000000,"G224152E59959N","2008-05-01T00:00:00",663072.878344898344949,0.663073000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224152E59959N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.846198622130885,59.960881000000001]
["glac_bound",378901.000000000000000,"G225264E59467N","2008-05-01T00:00:00",56548.547138539906882,0.056549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225264E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.737166129551838,59.467600500000003]
["glac_bound",378904.000000000000000,"G230517E56368N","2008-05-01T00:00:00",155609.107321763323853,0.155609000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230517E56368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.483576772931031,56.368331499999996]
["glac_bound",378905.000000000000000,"G228616E57156N","2008-05-01T00:00:00",1031910.654661061358638,1.031910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228616E57156N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.385351629664171,57.156663500000001]
["glac_bound",378906.000000000000000,"G229729E56557N","2008-05-01T00:00:00",26346741.075323361903429,26.346699999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229729E56557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.259295867167793,56.578647500000002]
["glac_bound",378909.000000000000000,"G227302E57776N","2008-05-01T00:00:00",76603.847785142497742,0.076604000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-11T00:00:00","okay","None","None","08BC227302E57776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.697015951530631,57.776121500000002]
["glac_bound",378910.000000000000000,"G228573E57284N","2008-05-01T00:00:00",1924042.967871512053534,1.924040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228573E57284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.431639805800557,57.285086499999998]
["glac_bound",378916.000000000000000,"G228739E57146N","2008-05-01T00:00:00",108029.597440501383971,0.108030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228739E57146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.258230421925191,57.146898500000006]
["glac_bound",378917.000000000000000,"G230085E55923N","2008-05-01T00:00:00",1628919.936140551930293,1.628920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230085E55923N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.909754220159499,55.924368500000000]
["glac_bound",378928.000000000000000,"G227577E57529N","2008-05-01T00:00:00",104548.538219710157136,0.104549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BC227577E57529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.422521256491109,57.528735499999996]
["glac_bound",378929.000000000000000,"G230607E55357N","2008-05-01T00:00:00",1572830.500265011796728,1.572830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230607E55357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.392858810606185,55.356715000000001]
["glac_bound",378932.000000000000000,"G231695E56172N","2008-05-01T00:00:00",178983.288690739282174,0.178983000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231695E56172N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.303751622281538,56.171329000000000]
["glac_bound",378935.000000000000000,"G227903E57425N","2008-05-01T00:00:00",387255.837783566152211,0.387256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227903E57425N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.098505292834034,57.425915500000002]
["glac_bound",378946.000000000000000,"G229925E57003N","2008-05-01T00:00:00",169497.336650286393706,0.169497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229925E57003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.072789319233436,57.003994500000005]
["glac_bound",378955.000000000000000,"G227977E57287N","2008-05-01T00:00:00",6799403.358494789339602,6.799400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227977E57287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.997571401356197,57.293648000000005]
["glac_bound",378956.000000000000000,"G221705E59734N","2008-05-01T00:00:00",220468.778779731044779,0.220469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221705E59734N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.296134306062498,59.732332000000000]
["glac_bound",378958.000000000000000,"G226728E58225N","2008-05-01T00:00:00",67336.772243645813433,0.067337000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226728E58225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.271205161103126,58.224901500000001]
["glac_bound",378964.000000000000000,"G226791E58229N","2008-05-01T00:00:00",1714083.685638027265668,1.714080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226791E58229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.208634270726975,58.238221500000002]
["glac_bound",378966.000000000000000,"G229361E57655N","2008-05-01T00:00:00",1809568.678914995398372,1.809570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229361E57655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.638389201704541,57.654297999999997]
["glac_bound",378968.000000000000000,"G229645E56320N","2008-05-01T00:00:00",123566.507316928007640,0.123567000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229645E56320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.355143545695341,56.319748000000004]
["glac_bound",378969.000000000000000,"G229214E56877N","2008-05-01T00:00:00",2996854.948674732819200,2.996860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229214E56877N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.804615224613826,56.874223999999998]
["glac_bound",378972.000000000000000,"G227328E58299N","2008-05-01T00:00:00",771288.239496020949446,0.771288000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227328E58299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.671334766932262,58.298315500000001]
["glac_bound",378975.000000000000000,"G222568E59375N","2008-05-01T00:00:00",5849795.145317010581493,5.849800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222568E59375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.430901319374698,59.377719999999997]
["glac_bound",378982.000000000000000,"G229977E56805N","2008-05-01T00:00:00",218999.517380466277245,0.219000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229977E56805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.021579762756062,56.805333500000003]
["glac_bound",378985.000000000000000,"G222965E59306N","2008-05-01T00:00:00",63302.840230430207157,0.063303000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222965E59306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.033794464807443,59.307552000000001]
["glac_bound",378997.000000000000000,"G223059E59153N","2008-05-01T00:00:00",95523.496844896551920,0.095523000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223059E59153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.940367624942382,59.152502999999996]
["glac_bound",379006.000000000000000,"G225650E59244N","2008-05-01T00:00:00",231097.216665085696150,0.231097000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225650E59244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.349649602901195,59.244216500000000]
["glac_bound",379011.000000000000000,"G228602E56630N","2008-05-01T00:00:00",544307.750720298383385,0.544308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228602E56630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.397397853189347,56.630333499999999]
["glac_bound",379012.000000000000000,"G226055E58780N","2008-05-01T00:00:00",1779255.181867748266086,1.779260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226055E58780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.939280042192451,58.779951499999996]
["glac_bound",379015.000000000000000,"G223530E59470N","2008-05-01T00:00:00",90699.633986781831481,0.090700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223530E59470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.470950881728072,59.469780000000000]
["glac_bound",379016.000000000000000,"G224438E59795N","2008-05-01T00:00:00",13232220.490666985511780,13.232200000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224438E59795N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.590659143056428,59.792837000000006]
["glac_bound",379018.000000000000000,"G227606E58215N","2008-05-01T00:00:00",519686.128891309199389,0.519686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227606E58215N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.394297798251955,58.214880000000001]
["glac_bound",379028.000000000000000,"G227091E58467N","2008-05-01T00:00:00",840832.727529635070823,0.840833000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227091E58467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.908309851150420,58.470403500000003]
["glac_bound",379031.000000000000000,"G230134E57349N","2008-05-01T00:00:00",67139.405509793738020,0.067139000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230134E57349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.865924553003538,57.348898000000005]
["glac_bound",379036.000000000000000,"G225598E59449N","2008-05-01T00:00:00",417815.263400059717242,0.417815000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225598E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.401229968232769,59.449159999999999]
["glac_bound",379041.000000000000000,"G230039E56234N","2008-05-01T00:00:00",17327297.730726588517427,17.327300000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230039E56234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.968458266555217,56.252730499999998]
["glac_bound",379042.000000000000000,"G227949E57381N","2008-05-01T00:00:00",183647.965035089553567,0.183648000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227949E57381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.053503892005153,57.380099999999999]
["glac_bound",379043.000000000000000,"G225650E59152N","2008-05-01T00:00:00",814998.116789840860292,0.814998000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225650E59152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.347124855472430,59.149866000000003]
["glac_bound",379046.000000000000000,"G229878E56576N","2008-05-01T00:00:00",262905.863399795431178,0.262906000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229878E56576N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.121076616542041,56.575283499999998]
["glac_bound",379047.000000000000000,"G224622E59754N","2008-05-01T00:00:00",109103.013749051126069,0.109103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224622E59754N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.377233942509861,59.754376499999999]
["glac_bound",379048.000000000000000,"G222221E59577N","2008-05-01T00:00:00",603586.697838971391320,0.603587000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222221E59577N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.777607799278826,59.580658000000000]
["glac_bound",379050.000000000000000,"G229321E56581N","2008-05-01T00:00:00",1462471.504351143725216,1.462470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229321E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.685302327392890,56.579949499999998]
["glac_bound",379051.000000000000000,"G227222E58195N","2008-05-01T00:00:00",186735.929451254894957,0.186736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227222E58195N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.776431742722821,58.194239499999995]
["glac_bound",379053.000000000000000,"G228038E57486N","2008-05-01T00:00:00",110078.954833473879262,0.110079000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228038E57486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.956496328302990,57.487414999999999]
["glac_bound",379056.000000000000000,"G230304E56197N","2008-05-01T00:00:00",181612.690186067193281,0.181613000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230304E56197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.694586270905091,56.199707000000004]
["glac_bound",379057.000000000000000,"G223002E59545N","2008-05-01T00:00:00",140628.704977474873886,0.140629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223002E59545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.997294248824005,59.546124499999998]
["glac_bound",379061.000000000000000,"G222541E59610N","2008-05-01T00:00:00",570257.504494137712754,0.570257000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222541E59610N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.458957200641493,59.610708500000001]
["glac_bound",379063.000000000000000,"G230238E54425N","2008-05-01T00:00:00",431627.893004130455665,0.431628000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230238E54425N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.761810387964772,54.424502000000004]
["glac_bound",379068.000000000000000,"G228589E57042N","2008-05-01T00:00:00",202616.473220906220376,0.202616000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228589E57042N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.412184957065051,57.043396000000001]
["glac_bound",379071.000000000000000,"G225532E59277N","2008-05-01T00:00:00",1393111.702052033971995,1.393110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225532E59277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.472259209634274,59.276064500000004]
["glac_bound",379075.000000000000000,"G223236E59782N","2008-05-01T00:00:00",1340147.372192626353353,1.340150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223236E59782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.770650742870771,59.783976500000001]
["glac_bound",379076.000000000000000,"G233138E57615N","2008-05-01T00:00:00",377293.029901481990237,0.377293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233138E57615N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.860436998141267,57.613179000000002]
["glac_bound",379078.000000000000000,"G227573E57702N","2008-05-01T00:00:00",164904.229052594309906,0.164904000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227573E57702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.426633056246885,57.702104500000004]
["glac_bound",379079.000000000000000,"G225427E59336N","2008-05-01T00:00:00",177292.476149779424304,0.177292000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225427E59336N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.573507035695741,59.336389999999994]
["glac_bound",379087.000000000000000,"G224946E59379N","2008-05-01T00:00:00",1399092.735875056358054,1.399090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224946E59379N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.054383554257726,59.379625000000004]
["glac_bound",379089.000000000000000,"G230071E56439N","2008-05-01T00:00:00",737945.632520257611759,0.737946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230071E56439N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.928920364859806,56.438611500000000]
["glac_bound",379092.000000000000000,"G222500E59622N","2008-05-01T00:00:00",77105.331348125750083,0.077105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222500E59622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.499415233057846,59.621372000000001]
["glac_bound",379095.000000000000000,"G229267E56453N","2008-05-01T00:00:00",1877860.188459763536230,1.877860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229267E56453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.733881955158722,56.454549999999998]
["glac_bound",379096.000000000000000,"G224520E59840N","2008-05-01T00:00:00",496227.430325346125755,0.496227000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224520E59840N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.480912168230844,59.839770500000000]
["glac_bound",379099.000000000000000,"G229862E56990N","2008-05-01T00:00:00",1183990.541870759334415,1.183990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229862E56990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.138570582565535,56.991362500000001]
["glac_bound",379106.000000000000000,"G230137E55838N","2008-05-01T00:00:00",581950.686327623901889,0.581951000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230137E55838N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.862275690450986,55.835924500000004]
["glac_bound",379107.000000000000000,"G230672E57325N","2008-05-01T00:00:00",72028.843966479704250,0.072029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230672E57325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.328526104562798,57.325137999999995]
["glac_bound",379108.000000000000000,"G230989E56487N","2008-05-01T00:00:00",325806.095021072891541,0.325806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230989E56487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.011514880882373,56.486994500000002]
["glac_bound",379109.000000000000000,"G222798E59098N","2008-05-01T00:00:00",1066505.222239341819659,1.066510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222801E59093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.206661167086565,59.099231500000002]
["glac_bound",379110.000000000000000,"G227516E57743N","2008-05-01T00:00:00",1637899.515582146821544,1.637900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227516E57743N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.482278625234926,57.741952499999996]
["glac_bound",379116.000000000000000,"G229051E56421N","2008-05-01T00:00:00",54769.317599006317323,0.054769000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229051E56421N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.950324888049124,56.421419000000000]
["glac_bound",379117.000000000000000,"G228099E56976N","2008-05-01T00:00:00",79720.320658239972545,0.079720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228099E56976N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.901380612706362,56.974448000000002]
["glac_bound",379120.000000000000000,"G230054E56108N","2008-05-01T00:00:00",98290.035425677648163,0.098290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230054E56108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.945669085125019,56.109560000000002]
["glac_bound",379122.000000000000000,"G227079E58457N","2008-05-01T00:00:00",1340312.287799796089530,1.340310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227079E58457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.912422042326853,58.459730499999999]
["glac_bound",379123.000000000000000,"G229659E56569N","2008-05-01T00:00:00",698392.935019182623364,0.698393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229659E56569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.340842161888702,56.568341500000002]
["glac_bound",379124.000000000000000,"G228577E57071N","2008-05-01T00:00:00",12833118.225921617820859,12.833100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228577E57071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.452246003369282,57.082539999999995]
["glac_bound",379125.000000000000000,"G229102E56972N","2008-05-01T00:00:00",802269.164974865620025,0.802269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229102E56972N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.898134712766762,56.972150999999997]
["glac_bound",379127.000000000000000,"G227334E57987N","2008-05-01T00:00:00",904709.469411854399368,0.904709000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227334E57987N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.664254309777448,57.992429999999999]
["glac_bound",379131.000000000000000,"G225621E59454N","2008-05-01T00:00:00",76065.232567609389662,0.076065000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225621E59454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.380711712175639,59.455760999999995]
["glac_bound",379132.000000000000000,"G223442E59320N","2008-05-01T00:00:00",93830933.288697868585587,93.830900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Tsirku Glacier","None","08BE223442E59320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.595602225634082,59.329746999999998]
["glac_bound",379139.000000000000000,"G229855E56544N","2008-05-01T00:00:00",33446018.290932513773441,33.445999999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229855E56544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.188548811968076,56.568692999999996]
["glac_bound",379144.000000000000000,"G228764E56609N","2008-05-01T00:00:00",312420.291471653967164,0.312420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228764E56609N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.236136109226436,56.609201499999998]
["glac_bound",379150.000000000000000,"G229236E56894N","2008-05-01T00:00:00",661777.715353598003276,0.661778000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229236E56894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.763663964495805,56.894129500000005]
["glac_bound",379151.000000000000000,"G227308E58003N","2008-05-01T00:00:00",321546.917873692756984,0.321547000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227308E58003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.694896055255015,58.004445000000004]
["glac_bound",379154.000000000000000,"G223585E59660N","2008-05-01T00:00:00",87993.313922775036190,0.087993000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223585E59660N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.413518483741370,59.660345999999997]
["glac_bound",379156.000000000000000,"G226843E58371N","2008-05-01T00:00:00",56168.022107428558229,0.056168000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226843E58371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.157393391407425,58.370981000000000]
["glac_bound",379168.000000000000000,"G224214E59915N","2008-05-01T00:00:00",435596.971889608656056,0.435597000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224214E59915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.788690747690225,59.913743500000002]
["glac_bound",379172.000000000000000,"G229354E56638N","2008-05-01T00:00:00",3014925.072220503352582,3.014930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229354E56638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.642732278398512,56.642372999999999]
["glac_bound",379175.000000000000000,"G223187E59691N","2008-05-01T00:00:00",1862064.784927152795717,1.862060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223187E59691N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.820094531010568,59.689602500000007]
["glac_bound",379178.000000000000000,"G230328E55617N","2008-05-01T00:00:00",269605.674616873962805,0.269606000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230328E55617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.672183956504767,55.616280500000002]
["glac_bound",379179.000000000000000,"G231376E57347N","2008-05-01T00:00:00",123572.746059837940265,0.123573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231376E57347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.625340370846516,57.347265000000000]
["glac_bound",379180.000000000000000,"G230010E54388N","2008-05-01T00:00:00",852483.390673231915571,0.852483000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230010E54388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.988963126034946,54.389204499999998]
["glac_bound",379181.000000000000000,"G228448E57187N","2008-05-01T00:00:00",68016.359386614945834,0.068016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228448E57187N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.553297924727275,57.186822500000005]
["glac_bound",379187.000000000000000,"G230289E55110N","2008-05-01T00:00:00",370507.321200673526619,0.370507000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230289E55110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.710340826573770,55.111341499999995]
["glac_bound",379188.000000000000000,"G230418E55639N","2008-05-01T00:00:00",137094.785577587987063,0.137095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230418E55639N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.582814677453030,55.638529000000005]
["glac_bound",379189.000000000000000,"G224006E59726N","2008-05-01T00:00:00",142317.447131300927140,0.142317000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224006E59726N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.994819991698080,59.726105500000003]
["glac_bound",379190.000000000000000,"G230065E55752N","2008-05-01T00:00:00",80824.610239631438162,0.080825000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230065E55752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.934401111505707,55.752181000000000]
["glac_bound",379191.000000000000000,"G227225E58460N","2008-05-01T00:00:00",314355.596074451226741,0.314356000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227225E58460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.776571679354106,58.459908999999996]
["glac_bound",379197.000000000000000,"G222385E59994N","2008-05-01T00:00:00",321463.923471294809133,0.321464000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222385E59994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.613553986273530,59.994494500000002]
["glac_bound",379199.000000000000000,"G229601E56373N","2008-05-01T00:00:00",94832.002616688696435,0.094832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229601E56373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.396279106080669,56.374356500000005]
["glac_bound",379204.000000000000000,"G226467E58771N","2008-05-01T00:00:00",502711.451427273568697,0.502711000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226467E58771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.538342942035001,58.774720000000002]
["glac_bound",379205.000000000000000,"G224397E59865N","2008-05-01T00:00:00",1681801.558304528472945,1.681800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224397E59865N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.599462796301964,59.870291999999999]
["glac_bound",379208.000000000000000,"G231176E57504N","2008-05-01T00:00:00",534268.882355921203271,0.534269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231176E57504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.826629575311358,57.507885999999999]
["glac_bound",379210.000000000000000,"G224802E59697N","2008-05-01T00:00:00",1207117.726600355003029,1.207120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224802E59697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.196944417666316,59.697242500000002]
["glac_bound",379213.000000000000000,"G229030E57315N","2008-05-01T00:00:00",1069129.556183852721006,1.069130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229030E57315N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.971248276022322,57.321392000000003]
["glac_bound",379215.000000000000000,"G222469E59547N","2008-05-01T00:00:00",191630.047885454521747,0.191630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222469E59547N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.530053290950747,59.547469000000000]
["glac_bound",379216.000000000000000,"G228767E57431N","2008-05-01T00:00:00",248510.712253601552220,0.248511000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228767E57431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.236030900633864,57.432034999999999]
["glac_bound",379218.000000000000000,"G222620E59336N","2008-05-01T00:00:00",1706010.441283216467127,1.706010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Pentice Ice Caps","None","08AC222620E59336N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.386454768856311,59.336443000000003]
["glac_bound",379222.000000000000000,"G228811E57459N","2008-05-01T00:00:00",147936.520333434076747,0.147937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228811E57459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.189870187695931,57.457917500000001]
["glac_bound",379223.000000000000000,"G230196E57189N","2008-05-01T00:00:00",80685.303918398494716,0.080685000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230196E57189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.804517479810727,57.189020499999998]
["glac_bound",379225.000000000000000,"G229218E57049N","2008-05-01T00:00:00",204433.479777423897758,0.204433000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229218E57049N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.783154847996030,57.048850500000000]
["glac_bound",379233.000000000000000,"G224320E59873N","2008-05-01T00:00:00",590617.791363148950040,0.590618000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224320E59873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.678893706611575,59.873625000000004]
["glac_bound",379234.000000000000000,"G229856E57031N","2008-05-01T00:00:00",473438.732556771952659,0.473439000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229856E57031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.143366658543073,57.031269000000002]
["glac_bound",379235.000000000000000,"G230057E55347N","2008-05-01T00:00:00",140995.764334589737700,0.140996000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230057E55347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.944165318181831,55.347785000000002]
["glac_bound",379238.000000000000000,"G228194E57101N","2008-05-01T00:00:00",153877.982483062747633,0.153878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228194E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.805100479866553,57.102124500000002]
["glac_bound",379240.000000000000000,"G222450E59259N","2008-05-01T00:00:00",14140955.235045837238431,14.141000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222450E59259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.576393651214175,59.288351500000005]
["glac_bound",379243.000000000000000,"G222983E59302N","2008-05-01T00:00:00",25659673.138783846050501,25.659700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Peshak Glacier","None","08AC222983E59302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.040850539427510,59.334097999999997]
["glac_bound",379244.000000000000000,"G224815E59699N","2008-05-01T00:00:00",406300.067680738575291,0.406300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224815E59699N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.185774674822255,59.699877000000001]
["glac_bound",379245.000000000000000,"G229584E57414N","2008-05-01T00:00:00",93890.919837106193881,0.093891000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229584E57414N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.415080994964399,57.413840500000006]
["glac_bound",379246.000000000000000,"G228442E56810N","2008-05-01T00:00:00",1365114.485555107938126,1.365110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228442E56810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.579828390208974,56.812089499999999]
["glac_bound",379249.000000000000000,"G228678E57118N","2008-05-01T00:00:00",217200.239894318277948,0.217200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228678E57118N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.323191000000008,57.119433000000001]
["glac_bound",379253.000000000000000,"G222466E59508N","2008-05-01T00:00:00",1421533.448313411092386,1.421530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222466E59508N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.532014224545463,59.506073499999999]
["glac_bound",379257.000000000000000,"G228534E57062N","2008-05-01T00:00:00",813931.160279207513668,0.813931000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228534E57062N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.465231773069206,57.062944500000000]
["glac_bound",379258.000000000000000,"G230165E56290N","2008-05-01T00:00:00",1256206.307562721194699,1.256210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230165E56290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.825826208279466,56.290075999999999]
["glac_bound",379276.000000000000000,"G224221E59895N","2008-05-01T00:00:00",147916.244540656800382,0.147916000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224221E59895N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.779333234281467,59.895232000000000]
["glac_bound",379280.000000000000000,"G227089E58139N","2008-05-01T00:00:00",4393894.489707326516509,4.393890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227089E58139N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.879091402589040,58.144663000000001]
["glac_bound",379281.000000000000000,"G228133E57148N","2008-05-01T00:00:00",391172.156353258935269,0.391172000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228133E57148N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.868472981974207,57.145088500000000]
["glac_bound",379285.000000000000000,"G225887E59334N","2008-05-01T00:00:00",1361312.445141161326319,1.361310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225887E59334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.112160340133329,59.334143499999996]
["glac_bound",379287.000000000000000,"G225212E59276N","2008-05-01T00:00:00",1202270.882104142569005,1.202270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225212E59276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.787355589535963,59.275939999999999]
["glac_bound",379288.000000000000000,"G229422E57128N","2008-05-01T00:00:00",7439057.104577464982867,7.439060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229422E57128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.594863255637847,57.148600000000002]
["glac_bound",379291.000000000000000,"G226468E58852N","2008-05-01T00:00:00",60786.076145644670760,0.060786000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226468E58852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.533091782551082,58.852333999999999]
["glac_bound",379298.000000000000000,"G231503E56205N","2008-05-01T00:00:00",104391.542106766428333,0.104392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231503E56205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.495265877434804,56.204828500000005]
["glac_bound",379299.000000000000000,"G230735E55324N","2008-05-01T00:00:00",190629.666379873553524,0.190630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230735E55324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.264707129923920,55.323425499999999]
["glac_bound",379302.000000000000000,"G229059E56747N","2008-05-01T00:00:00",1449932.270600139629096,1.449930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229059E56747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.937035410614556,56.747110000000006]
["glac_bound",379306.000000000000000,"G230043E55208N","2008-05-01T00:00:00",100922.018109914002707,0.100922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230043E55208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.956930033954620,55.207820499999997]
["glac_bound",379311.000000000000000,"G227970E57127N","2008-05-01T00:00:00",495813.896883692184929,0.495814000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227970E57127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.025376385261211,57.127993000000004]
["glac_bound",379317.000000000000000,"G227978E57084N","2008-05-01T00:00:00",876932.608407372375950,0.876933000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227978E57084N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.019276317781618,57.089900999999998]
["glac_bound",379322.000000000000000,"G227912E57383N","2008-05-01T00:00:00",2499657.321575921494514,2.499660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227912E57383N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.091156125145631,57.392054999999999]
["glac_bound",379324.000000000000000,"G230074E55649N","2008-05-01T00:00:00",433835.369809109426569,0.433835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230074E55649N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.925665725601164,55.648380500000002]
["glac_bound",379330.000000000000000,"G225354E59864N","2008-05-01T00:00:00",182658.599372472992400,0.182659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225354E59864N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.647884251376126,59.864512500000004]
["glac_bound",379333.000000000000000,"G223292E59259N","2008-05-01T00:00:00",52339744.025372482836246,52.339700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223114E59297N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.854295452925612,59.322281500000003]
["glac_bound",379337.000000000000000,"G230220E57463N","2008-05-01T00:00:00",179893.034133742621634,0.179893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230220E57463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.779855959528703,57.462565499999997]
["glac_bound",379338.000000000000000,"G221915E59886N","2008-05-01T00:00:00",596087.166148321935907,0.596087000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221915E59886N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.078571236302480,59.884399000000002]
["glac_bound",379345.000000000000000,"G230115E56998N","2008-05-01T00:00:00",764482.426406388753094,0.764482000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230115E56998N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.886022912964307,56.998939000000000]
["glac_bound",379348.000000000000000,"G222654E58996N","2008-05-01T00:00:00",148040.226227599981939,0.148040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222654E58996N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.346311953373970,58.995826999999998]
["glac_bound",379356.000000000000000,"G226924E58255N","2008-05-01T00:00:00",96712.237852847072645,0.096712000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226924E58255N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.075487885802488,58.255823500000005]
["glac_bound",379359.000000000000000,"G224053E59725N","2008-05-01T00:00:00",6758350.522052760235965,6.758350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224053E59725N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.933654714267362,59.725615000000005]
["glac_bound",379361.000000000000000,"G225380E59487N","2008-05-01T00:00:00",640524.733586498303339,0.640525000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225380E59487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.620074557003022,59.486122500000000]
["glac_bound",379363.000000000000000,"G230113E56307N","2008-05-01T00:00:00",228515.536153002700303,0.228516000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230113E56307N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.888472645266688,56.304940999999999]
["glac_bound",379365.000000000000000,"G223770E59680N","2008-05-01T00:00:00",96829.902789321378805,0.096830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223770E59680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.229235529652328,59.680149999999998]
["glac_bound",379367.000000000000000,"G232782E57656N","2008-05-01T00:00:00",229113.361480880674208,0.229113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232782E57656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.217703597585398,57.655729500000000]
["glac_bound",379370.000000000000000,"G221784E59941N","2008-05-01T00:00:00",217161.637729315523757,0.217162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221784E59941N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.213025483392670,59.942236999999999]
["glac_bound",379372.000000000000000,"G230052E56555N","2008-05-01T00:00:00",1677610.366749644745141,1.677610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230052E56555N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.948118984569447,56.555161999999996]
["glac_bound",379375.000000000000000,"G230428E56027N","2008-05-01T00:00:00",367074.235706690000370,0.367074000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230428E56027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.574323021007444,56.028275000000001]
["glac_bound",379378.000000000000000,"G229847E56620N","2008-05-01T00:00:00",105307.266047563520260,0.105307000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229847E56620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.153458118849642,56.620518000000004]
["glac_bound",379379.000000000000000,"G229573E56287N","2008-05-01T00:00:00",50225.891017496789573,0.050226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229573E56287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.428089581537819,56.286355499999999]
["glac_bound",379384.000000000000000,"G227194E58227N","2008-05-01T00:00:00",2467513.816143997944891,2.467510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227194E58227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.804125684605197,58.230278499999997]
["glac_bound",379389.000000000000000,"G230538E55184N","2008-05-01T00:00:00",103945.715766637251363,0.103946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230538E55184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.461981127268331,55.184441500000005]
["glac_bound",379390.000000000000000,"G230008E55616N","2008-05-01T00:00:00",128241.344727283038083,0.128241000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230008E55616N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.993873911660785,55.616239999999998]
["glac_bound",379395.000000000000000,"G223144E59638N","2008-05-01T00:00:00",236533.461237622890621,0.236533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223144E59638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.854596538486305,59.641637000000003]
["glac_bound",379396.000000000000000,"G229162E57170N","2008-05-01T00:00:00",53922.300720282772090,0.053922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229162E57170N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.836512896933186,57.170995500000004]
["glac_bound",379397.000000000000000,"G225033E59501N","2008-05-01T00:00:00",903087.836563063552603,0.903088000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225033E59501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.969017881162358,59.501872500000005]
["glac_bound",379398.000000000000000,"G223425E59580N","2008-05-01T00:00:00",109690.308796866593184,0.109690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223425E59580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.574354200383596,59.579517500000001]
["glac_bound",379401.000000000000000,"G222218E59603N","2008-05-01T00:00:00",120809.456928185143624,0.120809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222218E59603N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.781898783036866,59.602423500000000]
["glac_bound",379407.000000000000000,"G230685E55597N","2008-05-01T00:00:00",52473.334302674178616,0.052473000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230685E55597N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.315610843009495,55.596593499999997]
["glac_bound",379413.000000000000000,"G224866E59823N","2008-05-01T00:00:00",149638.070074025308713,0.149638000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224866E59823N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.134579392703870,59.823840500000003]
["glac_bound",379418.000000000000000,"G230308E54867N","2008-05-01T00:00:00",119696.691071192559320,0.119697000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230308E54867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.692608794908040,54.867292499999998]
["glac_bound",379421.000000000000000,"G229418E56365N","2008-05-01T00:00:00",3857437.195622675586492,3.857440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229418E56365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.571509822923531,56.369068499999997]
["glac_bound",379424.000000000000000,"G227893E57646N","2008-05-01T00:00:00",253354.521650203940226,0.253355000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227893E57646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.105794316196778,57.645050499999996]
["glac_bound",379427.000000000000000,"G222923E59440N","2008-05-01T00:00:00",1010091.742448981385678,1.010090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222923E59440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.078805332593561,59.439967499999995]
["glac_bound",379429.000000000000000,"G225388E59432N","2008-05-01T00:00:00",3591882.349864174611866,3.591880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225388E59432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.592127986267542,59.438169000000002]
["glac_bound",379432.000000000000000,"G227191E58218N","2008-05-01T00:00:00",225540.597761830227682,0.225541000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227191E58218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.807593260389581,58.218406000000002]
["glac_bound",379433.000000000000000,"G230804E57299N","2008-05-01T00:00:00",342338.792290829296689,0.342339000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230804E57299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.202267191932947,57.296599999999998]
["glac_bound",379437.000000000000000,"G222289E59859N","2008-05-01T00:00:00",346512.490441346133593,0.346512000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222289E59859N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.709959132051210,59.859977499999999]
["glac_bound",379439.000000000000000,"G230426E55229N","2008-05-01T00:00:00",217226.300949120195583,0.217226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230426E55229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.568091004086057,55.230514999999997]
["glac_bound",379442.000000000000000,"G228613E56982N","2008-05-01T00:00:00",941902.118659046944231,0.941902000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228613E56982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.385655133864304,56.986087999999995]
["glac_bound",379443.000000000000000,"G229179E56567N","2008-05-01T00:00:00",1402779.711247262544930,1.402780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229179E56567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.817706168093224,56.573996500000000]
["glac_bound",379445.000000000000000,"G225661E59353N","2008-05-01T00:00:00",106673.612375855518621,0.106674000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225661E59353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.337788723139226,59.352045500000003]
["glac_bound",379450.000000000000000,"G225669E59259N","2008-05-01T00:00:00",521459.886688165890519,0.521460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225669E59259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.327044265748043,59.261943000000002]
["glac_bound",379452.000000000000000,"G227735E58031N","2008-05-01T00:00:00",2383079.971012803260237,2.383080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227735E58031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.266206460608799,58.032714999999996]
["glac_bound",379455.000000000000000,"G222697E58993N","2008-05-01T00:00:00",234295.948370904166950,0.234296000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222697E58993N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.309164994901835,58.993544499999999]
["glac_bound",379456.000000000000000,"G228653E57011N","2008-05-01T00:00:00",53906.022156859376992,0.053906000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228653E57011N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.346354157950060,57.011673000000002]
["glac_bound",379458.000000000000000,"G230761E55579N","2008-05-01T00:00:00",137900.583747952012345,0.137901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230761E55579N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.238948145907443,55.580228499999997]
["glac_bound",379465.000000000000000,"G227832E58013N","2008-05-01T00:00:00",10135096.126876588910818,10.135100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227832E58013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.197833128509274,58.028503999999998]
["glac_bound",379468.000000000000000,"G222764E59319N","2008-05-01T00:00:00",265570.707362155138981,0.265571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222764E59319N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.236091574666659,59.318446999999999]
["glac_bound",379470.000000000000000,"G228764E57520N","2008-05-01T00:00:00",3182501.926762105897069,3.182500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228764E57520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.234701989220213,57.521416500000001]
["glac_bound",379471.000000000000000,"G229401E56581N","2008-05-01T00:00:00",82309.515683638514020,0.082309000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229401E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.599312780345485,56.581037000000002]
["glac_bound",379475.000000000000000,"G227318E58304N","2008-05-01T00:00:00",119305.761233694996918,0.119306000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227318E58304N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.682090865406451,58.303664499999996]
["glac_bound",379482.000000000000000,"G230439E56083N","2008-05-01T00:00:00",286306.147395745501854,0.286306000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230439E56083N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.561479621078405,56.084074000000001]
["glac_bound",379488.000000000000000,"G223851E59731N","2008-05-01T00:00:00",253282.343695101939375,0.253282000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223851E59731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.147077451539872,59.731313000000000]
["glac_bound",379492.000000000000000,"G230865E56966N","2008-05-01T00:00:00",109732.099946087400895,0.109732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230865E56966N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.135479704525096,56.965541000000002]
["glac_bound",379493.000000000000000,"G223655E59579N","2008-05-01T00:00:00",680089.873684283811599,0.680090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223655E59579N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.345257048740962,59.579844499999993]
["glac_bound",379498.000000000000000,"G230063E56452N","2008-05-01T00:00:00",127344.357240762619767,0.127344000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230063E56452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.935695933874399,56.452380500000004]
["glac_bound",379506.000000000000000,"G230162E57447N","2008-05-01T00:00:00",196848.173868677811697,0.196848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230162E57447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.836572433449362,57.448994999999996]
["glac_bound",379508.000000000000000,"G229017E57266N","2008-05-01T00:00:00",309151.070237106760032,0.309151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229017E57266N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.983868822960090,57.265375499999998]
["glac_bound",379511.000000000000000,"G227260E58005N","2008-05-01T00:00:00",611287.754057007725351,0.611288000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227260E58005N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.738855685615732,58.005153000000000]
["glac_bound",379518.000000000000000,"G227953E57623N","2008-05-01T00:00:00",101729.535878304057405,0.101730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227953E57623N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.046154106909910,57.622368000000002]
["glac_bound",379519.000000000000000,"G228814E56527N","2008-05-01T00:00:00",104368.273439194599632,0.104368000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228814E56527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.186365581270024,56.526764999999997]
["glac_bound",379522.000000000000000,"G230058E56091N","2008-05-01T00:00:00",241683.328414255112875,0.241683000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230058E56091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.943736928571411,56.094285499999998]
["glac_bound",379524.000000000000000,"G227152E58404N","2008-05-01T00:00:00",7941840.498784387484193,7.941840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227152E58404N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.868422602916098,58.412742500000000]
["glac_bound",379528.000000000000000,"G230377E54866N","2008-05-01T00:00:00",105470.715951215475798,0.105471000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230377E54866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.623115486189590,54.866607000000002]
["glac_bound",379533.000000000000000,"G226598E58538N","2008-05-01T00:00:00",446490.474182872625533,0.446490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226598E58538N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.402072286048679,58.541910999999999]
["glac_bound",379545.000000000000000,"G229993E55586N","2008-05-01T00:00:00",346426.136651354841888,0.346426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC229993E55586N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.007766301587310,55.587075999999996]
["glac_bound",379548.000000000000000,"G228849E56769N","2008-05-01T00:00:00",475029.188622876361478,0.475029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228849E56769N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.145162411947524,56.770790000000005]
["glac_bound",379551.000000000000000,"G230434E54678N","2008-05-01T00:00:00",76531.572471856765333,0.076532000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230434E54678N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.565836874921899,54.678526499999997]
["glac_bound",379554.000000000000000,"G229632E56563N","2008-05-01T00:00:00",63236.766757738660090,0.063237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229632E56563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.368452086236232,56.562664499999997]
["glac_bound",379556.000000000000000,"G226514E58495N","2008-05-01T00:00:00",239445.408075708546676,0.239445000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226514E58495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.485989633005318,58.495963500000002]
["glac_bound",379558.000000000000000,"G229501E56990N","2008-05-01T00:00:00",109363.039617703543627,0.109363000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229501E56990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.499738095216912,56.989205999999996]
["glac_bound",379560.000000000000000,"G230266E54519N","2008-05-01T00:00:00",302769.787929331650957,0.302770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230266E54519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.734580394272001,54.519731000000000]
["glac_bound",379561.000000000000000,"G223844E59805N","2008-05-01T00:00:00",313030.595557593915146,0.313031000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223844E59805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.161136060003059,59.806986999999999]
["glac_bound",379562.000000000000000,"G229438E56930N","2008-05-01T00:00:00",2396602.865851582027972,2.396600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229438E56930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.566780624266869,56.929639999999999]
["glac_bound",379568.000000000000000,"G230367E55751N","2008-05-01T00:00:00",76642.803985119666322,0.076643000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230367E55751N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.632937750364079,55.751098499999998]
["glac_bound",379571.000000000000000,"G226775E58458N","2008-05-01T00:00:00",2452986.846076094545424,2.452990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226775E58458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.228819386953916,58.468057999999999]
["glac_bound",379577.000000000000000,"G227096E58094N","2008-05-01T00:00:00",88811.298666396469343,0.088811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227096E58094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.904028822928609,58.094346000000002]
["glac_bound",379580.000000000000000,"G226367E58903N","2008-05-01T00:00:00",11162371.799419075250626,11.162400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226367E58903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.644824244376281,58.898836000000003]
["glac_bound",379581.000000000000000,"G226485E59094N","2008-05-01T00:00:00",1125054.340903076343238,1.125050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226485E59094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.510416066047128,59.093297000000000]
["glac_bound",379583.000000000000000,"G228484E57369N","2008-05-01T00:00:00",13571713.580050647258759,13.571700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228484E57369N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.500438002131034,57.369994500000004]
["glac_bound",379586.000000000000000,"G228507E56766N","2008-05-01T00:00:00",657606.858621128019877,0.657607000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228507E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.491691900178864,56.764663499999997]
["glac_bound",379589.000000000000000,"G226469E58842N","2008-05-01T00:00:00",240989.775811208324740,0.240990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226469E58842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.533194055965936,58.841134999999994]
["glac_bound",379591.000000000000000,"G223554E59870N","2008-05-01T00:00:00",4272775.719656179659069,4.272780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223554E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.442918535169355,59.868385000000004]
["glac_bound",379592.000000000000000,"G224037E59706N","2008-05-01T00:00:00",171880.523408232285874,0.171881000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224037E59706N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.964798132110047,59.706662500000000]
["glac_bound",379594.000000000000000,"G231275E57544N","2008-05-01T00:00:00",50004.631414604213205,0.050005000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231275E57544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.724446972222211,57.544342999999998]
["glac_bound",379600.000000000000000,"G229988E56205N","2008-05-01T00:00:00",403075.537307126622181,0.403076000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229988E56205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.012154880384884,56.205440999999993]
["glac_bound",379604.000000000000000,"G228060E57094N","2008-05-01T00:00:00",88838.798879400244914,0.088839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228060E57094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.940079853159688,57.093451000000002]
["glac_bound",379609.000000000000000,"G230483E55341N","2008-05-01T00:00:00",299990.336507958709262,0.299990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230483E55341N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.516302161451279,55.340952999999999]
["glac_bound",379610.000000000000000,"G221750E59738N","2008-05-01T00:00:00",1139725.486407578224316,1.139730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221750E59738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.264081403562557,59.739770999999998]
["glac_bound",379611.000000000000000,"G230329E56477N","2008-05-01T00:00:00",593356.016744132153690,0.593356000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230329E56477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.671722112420696,56.476711000000002]
["glac_bound",379615.000000000000000,"G229856E56479N","2008-05-01T00:00:00",382027.926866343885195,0.382028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229856E56479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.143211072559836,56.481145499999997]
["glac_bound",379621.000000000000000,"G229512E56268N","2008-05-01T00:00:00",133414.207943715096917,0.133414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229512E56268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.488012946296294,56.268591499999999]
["glac_bound",379624.000000000000000,"G230051E55647N","2008-05-01T00:00:00",398191.293244755186606,0.398191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230051E55647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.947256232551581,55.648145999999997]
["glac_bound",379626.000000000000000,"G226302E58937N","2008-05-01T00:00:00",406239.738372678111773,0.406240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226302E58937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.695989718507320,58.936884499999998]
["glac_bound",379629.000000000000000,"G227813E57555N","2008-05-01T00:00:00",1073395.899102702969685,1.073400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227813E57555N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.188647339542797,57.555626000000004]
["glac_bound",379633.000000000000000,"G225363E59674N","2008-05-01T00:00:00",1003025.829869441688061,1.003030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225363E59674N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.639372058706044,59.680577000000000]
["glac_bound",379640.000000000000000,"G230694E55567N","2008-05-01T00:00:00",494733.179152256634552,0.494733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230694E55567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.304433333155771,55.565814500000002]
["glac_bound",379641.000000000000000,"G227764E57810N","2008-05-01T00:00:00",1644188.756857093889266,1.644190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227764E57810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.236390006585680,57.810599499999995]
["glac_bound",379644.000000000000000,"G226946E58414N","2008-05-01T00:00:00",1311806.068001741077751,1.311810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226946E58414N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.049362255861297,58.414642999999998]
["glac_bound",379645.000000000000000,"G229020E57246N","2008-05-01T00:00:00",1190122.002480861032382,1.190120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229020E57246N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.980780981291332,57.247323999999999]
["glac_bound",379648.000000000000000,"G229951E56411N","2008-05-01T00:00:00",100052.482282544428017,0.100052000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229951E56411N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.046537585427870,56.411846500000003]
["glac_bound",379651.000000000000000,"G230508E56625N","2008-05-01T00:00:00",84287.437745788745815,0.084287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230508E56625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.491682473609842,56.625364000000005]
["glac_bound",379654.000000000000000,"G224098E59909N","2008-05-01T00:00:00",1746481.572960393037647,1.746480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224098E59909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.897534487741297,59.914074999999997]
["glac_bound",379660.000000000000000,"G225216E59624N","2008-05-01T00:00:00",1073628.963677349733189,1.073630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225216E59624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.784339526893916,59.622605000000000]
["glac_bound",379661.000000000000000,"G227333E57972N","2008-05-01T00:00:00",873422.030334058101289,0.873422000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227333E57972N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.672163357113789,57.973742999999999]
["glac_bound",379668.000000000000000,"G221588E60008N","2008-05-01T00:00:00",73841273.559553489089012,73.841300000000004,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221588E60008N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.368178992894912,59.982001499999996]
["glac_bound",379671.000000000000000,"G222457E59793N","2008-05-01T00:00:00",52058222.510641768574715,52.058199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222457E59793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.513086291666667,59.756670000000000]
["glac_bound",379678.000000000000000,"G229063E56417N","2008-05-01T00:00:00",113658.885770411565318,0.113659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229063E56417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.936387004169546,56.416704500000002]
["glac_bound",379684.000000000000000,"G227963E57281N","2008-05-01T00:00:00",566266.787342162569985,0.566267000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227963E57281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.041654729421964,57.277724500000005]
["glac_bound",379690.000000000000000,"G226206E58673N","2008-05-01T00:00:00",709581.309925621724688,0.709581000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226206E58673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.792695753547434,58.677065999999996]
["glac_bound",379691.000000000000000,"G229880E56268N","2008-05-01T00:00:00",78522.614025802613469,0.078523000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229880E56268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.120260814102551,56.268256500000000]
["glac_bound",379692.000000000000000,"G227837E57905N","2008-05-01T00:00:00",1631409.676387145882472,1.631410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227837E57905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.160208336734399,57.903923500000005]
["glac_bound",379694.000000000000000,"G230572E55894N","2008-05-01T00:00:00",87645.056713865138590,0.087645000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230572E55894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.426362823757415,55.893126500000001]
["glac_bound",379699.000000000000000,"G230100E56779N","2008-05-01T00:00:00",203775.756614685727982,0.203776000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230100E56779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.900477586751833,56.778742500000000]
["glac_bound",379700.000000000000000,"G230417E56400N","2008-05-01T00:00:00",147247.529588829609565,0.147248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230417E56400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.583990997515201,56.399926499999999]
["glac_bound",379702.000000000000000,"G229591E56553N","2008-05-01T00:00:00",62537.618998795442167,0.062538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229591E56553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.408661979497538,56.554091499999998]
["glac_bound",379705.000000000000000,"G226834E58367N","2008-05-01T00:00:00",3455240.720158225391060,3.455240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226834E58367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.182156329381996,58.371505999999997]
["glac_bound",379708.000000000000000,"G230392E55545N","2008-05-01T00:00:00",2100083.545670512132347,2.100080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230392E55545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.603459193786080,55.548744999999997]
["glac_bound",379711.000000000000000,"G227113E58127N","2008-05-01T00:00:00",395028.178274428297300,0.395028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227113E58127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.887132458003123,58.127133499999999]
["glac_bound",379716.000000000000000,"G229450E57471N","2008-05-01T00:00:00",261199.930950040783500,0.261200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229450E57471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.549261903575598,57.470725000000002]
["glac_bound",379726.000000000000000,"G228691E57437N","2008-05-01T00:00:00",70210.289674931118498,0.070210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228691E57437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.309484502638725,57.438290500000001]
["glac_bound",379727.000000000000000,"G227965E57140N","2008-05-01T00:00:00",2724363.589565945789218,2.724360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227965E57140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.036125852068267,57.143012999999996]
["glac_bound",379731.000000000000000,"G225871E59324N","2008-05-01T00:00:00",70333.725987198442454,0.070334000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225871E59324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.127283801989506,59.324560500000004]
["glac_bound",379733.000000000000000,"G230686E57324N","2008-05-01T00:00:00",811817.591862312401645,0.811818000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230686E57324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.313629530534342,57.323334500000001]
["glac_bound",379735.000000000000000,"G227812E57596N","2008-05-01T00:00:00",278613.363951894745696,0.278613000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227812E57596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.189736531747684,57.598001500000002]
["glac_bound",379739.000000000000000,"G223469E59417N","2008-05-01T00:00:00",242731.484389147488400,0.242731000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223469E59417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.531216610187329,59.417096000000001]
["glac_bound",379741.000000000000000,"G223694E59895N","2008-05-01T00:00:00",1543710.331391477491707,1.543710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223694E59895N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.315595026559834,59.897836499999997]
["glac_bound",379744.000000000000000,"G227327E58234N","2008-05-01T00:00:00",1402527.690500491065904,1.402530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227327E58234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.669286725750680,58.232552499999997]
["glac_bound",379746.000000000000000,"G230286E56288N","2008-05-01T00:00:00",868403.582036867039278,0.868404000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230286E56288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.711358294389129,56.288004000000001]
["glac_bound",379749.000000000000000,"G226459E58528N","2008-05-01T00:00:00",711101.719071392901242,0.711102000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226459E58528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.539654991598240,58.528498999999996]
["glac_bound",379752.000000000000000,"G230312E55704N","2008-05-01T00:00:00",554659.554930076701567,0.554660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230312E55704N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.689820083333359,55.703146000000004]
["glac_bound",379754.000000000000000,"G229642E56563N","2008-05-01T00:00:00",112161.896770040853880,0.112162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229642E56563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.356951005328227,56.564393499999994]
["glac_bound",379757.000000000000000,"G226645E58637N","2008-05-01T00:00:00",220587.270350882434286,0.220587000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226645E58637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.354578247384836,58.638072500000000]
["glac_bound",379758.000000000000000,"G229051E56952N","2008-05-01T00:00:00",622282.583185674040578,0.622283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229051E56952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.948250218036321,56.953420000000001]
["glac_bound",379766.000000000000000,"G228577E57459N","2008-05-01T00:00:00",89303.842938327157754,0.089304000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228577E57459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.422620617927976,57.458655000000000]
["glac_bound",379768.000000000000000,"G229672E56433N","2008-05-01T00:00:00",137859.591793572733877,0.137860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229672E56433N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.329131823545765,56.433815499999994]
["glac_bound",379769.000000000000000,"G222532E59124N","2008-05-01T00:00:00",74164.780373705827515,0.074165000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222532E59124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.467373878967408,59.124779500000002]
["glac_bound",379770.000000000000000,"G225960E59206N","2008-05-01T00:00:00",215137.528089082537917,0.215138000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225960E59206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.041371833116898,59.206671999999998]
["glac_bound",379771.000000000000000,"G228351E56856N","2008-05-01T00:00:00",193576.037534555303864,0.193576000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228351E56856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.647574051149149,56.855544499999993]
["glac_bound",379775.000000000000000,"G228660E56601N","2008-05-01T00:00:00",365856.157128581893630,0.365856000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228660E56601N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.338584927421323,56.600484500000000]
["glac_bound",379776.000000000000000,"G224056E59751N","2008-05-01T00:00:00",401276.832437783014029,0.401277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224056E59751N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.944058179052632,59.751380999999995]
["glac_bound",379779.000000000000000,"G230376E55724N","2008-05-01T00:00:00",247717.621875384589657,0.247718000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230376E55724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.627227892924083,55.726137500000000]
["glac_bound",379780.000000000000000,"G227456E58210N","2008-05-01T00:00:00",4369304.010035278275609,4.369300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227456E58210N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.540035422078972,58.215030999999996]
["glac_bound",379792.000000000000000,"G228712E57436N","2008-05-01T00:00:00",119780.263608278241009,0.119780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228712E57436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.288368211042950,57.435828999999998]
["glac_bound",379793.000000000000000,"G225352E59685N","2008-05-01T00:00:00",208875.422849860013230,0.208875000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225352E59685N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.648294017234150,59.686389500000004]
["glac_bound",379794.000000000000000,"G230760E55316N","2008-05-01T00:00:00",3563074.426927874796093,3.563070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230760E55316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.233922500000006,55.316445500000000]
["glac_bound",379796.000000000000000,"G226942E58273N","2008-05-01T00:00:00",1954608.397208249196410,1.954610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226942E58273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.062289088317158,58.275458000000000]
["glac_bound",379797.000000000000000,"G228903E57291N","2008-05-01T00:00:00",7897984.892295064404607,7.897980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228903E57291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.096412841490064,57.300877999999997]
["glac_bound",379802.000000000000000,"G230403E55673N","2008-05-01T00:00:00",76230.914431849480025,0.076231000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230403E55673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.593803404853730,55.674813499999999]
["glac_bound",379813.000000000000000,"G229476E56926N","2008-05-01T00:00:00",123386.223261700462899,0.123386000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229476E56926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.522537029329612,56.926245999999999]
["glac_bound",379815.000000000000000,"G225066E59500N","2008-05-01T00:00:00",1905379.466061511076987,1.905380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225066E59500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.926883843757935,59.502000500000001]
["glac_bound",379818.000000000000000,"G228748E56618N","2008-05-01T00:00:00",2249399.030630259308964,2.249400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228748E56618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.258672286015155,56.625595000000004]
["glac_bound",379819.000000000000000,"G223237E59803N","2008-05-01T00:00:00",394678.348079055838753,0.394678000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223237E59803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.767451395678819,59.805144499999997]
["glac_bound",379823.000000000000000,"G223129E59387N","2008-05-01T00:00:00",921690.893664365052246,0.921691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223129E59387N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.873986556562272,59.387381500000004]
["glac_bound",379824.000000000000000,"G229694E56432N","2008-05-01T00:00:00",1653540.160415020305663,1.653540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229694E56432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.301943000605320,56.434255000000000]
["glac_bound",379830.000000000000000,"G229990E57117N","2008-05-01T00:00:00",59637.396702898200601,0.059637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229990E57117N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.009793555066381,57.117126999999996]
["glac_bound",379831.000000000000000,"G230078E57328N","2008-05-01T00:00:00",582669.961529848282225,0.582670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230078E57328N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.920637359731870,57.326469000000003]
["glac_bound",379834.000000000000000,"G229022E56962N","2008-05-01T00:00:00",1302237.234120300272480,1.302240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229022E56962N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.976212467938637,56.963219500000001]
["glac_bound",379847.000000000000000,"G229465E56738N","2008-05-01T00:00:00",195801.560627910890616,0.195802000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229465E56738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.535284567691548,56.737555000000000]
["glac_bound",379849.000000000000000,"G227979E56846N","2008-05-01T00:00:00",1775652.624117270810530,1.775650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227979E56846N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.025710008097576,56.841329500000001]
["glac_bound",379864.000000000000000,"G229899E56804N","2008-05-01T00:00:00",352274.187035824928898,0.352274000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229899E56804N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.101329104929562,56.805524000000005]
["glac_bound",379868.000000000000000,"G222332E59563N","2008-05-01T00:00:00",355849.918635190115310,0.355850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222332E59563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.671189274437324,59.562894999999997]
["glac_bound",379872.000000000000000,"G230429E55234N","2008-05-01T00:00:00",158733.867854746378725,0.158734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230429E55234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.569505049892598,55.235045499999998]
["glac_bound",379874.000000000000000,"G222400E59634N","2008-05-01T00:00:00",296160.689306246757042,0.296161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222400E59634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.602601887637661,59.634565499999994]
["glac_bound",379876.000000000000000,"G228159E57095N","2008-05-01T00:00:00",6112002.090760658495128,6.112000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228159E57095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.823506001042517,57.100504999999998]
["glac_bound",379879.000000000000000,"G226840E58493N","2008-05-01T00:00:00",402114.132296351133846,0.402114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226840E58493N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.161040089552216,58.493976000000004]
["glac_bound",379880.000000000000000,"G230549E57071N","2008-05-01T00:00:00",2212096.516064826399088,2.212100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230549E57071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.453213001251726,57.069483499999997]
["glac_bound",379882.000000000000000,"G227977E57196N","2008-05-01T00:00:00",811965.666645770426840,0.811966000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227977E57196N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.015800704349829,57.197731500000003]
["glac_bound",379884.000000000000000,"G227394E57803N","2008-05-01T00:00:00",636221.586368251359090,0.636222000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227394E57803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.605469477420115,57.803207499999999]
["glac_bound",379885.000000000000000,"G230070E56567N","2008-05-01T00:00:00",363210.961378637875896,0.363211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230070E56567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.929751322808954,56.568028499999997]
["glac_bound",379886.000000000000000,"G229014E57277N","2008-05-01T00:00:00",735040.363620286341757,0.735040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229014E57277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.983710371601262,57.277431000000000]
["glac_bound",379891.000000000000000,"G230298E56312N","2008-05-01T00:00:00",75726.671210929809604,0.075727000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230298E56312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.702083200073616,56.312626500000000]
["glac_bound",379894.000000000000000,"G226776E58574N","2008-05-01T00:00:00",688786.659284453140572,0.688787000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226776E58574N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.226445883764143,58.575761499999999]
["glac_bound",379897.000000000000000,"G230376E56231N","2008-05-01T00:00:00",1444080.654645499773324,1.444080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230376E56231N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.620108155405660,56.230991500000002]
["glac_bound",379913.000000000000000,"G221836E59921N","2008-05-01T00:00:00",188284.370207625383046,0.188284000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221836E59921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.163420587931057,59.919565000000006]
["glac_bound",379915.000000000000000,"G228398E56902N","2008-05-01T00:00:00",103121.498001982923597,0.103121000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228398E56902N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.601778270191176,56.901805500000002]
["glac_bound",379919.000000000000000,"G230714E55575N","2008-05-01T00:00:00",186923.381333315657685,0.186923000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230714E55575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.285246335550823,55.575676000000001]
["glac_bound",379920.000000000000000,"G229330E57383N","2008-05-01T00:00:00",675250.339115020819008,0.675250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229330E57383N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.671281636940421,57.383041500000004]
["glac_bound",379921.000000000000000,"G229035E56597N","2008-05-01T00:00:00",609534.099200546508655,0.609534000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229035E56597N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.965758121559645,56.596563000000003]
["glac_bound",379922.000000000000000,"G223738E59883N","2008-05-01T00:00:00",1089653.491354765137658,1.089650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223738E59883N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.259996368000003,59.881046499999997]
["glac_bound",379931.000000000000000,"G223116E59386N","2008-05-01T00:00:00",246751.917125953012146,0.246752000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223116E59386N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.885233428993786,59.386246999999997]
["glac_bound",379937.000000000000000,"G230796E55073N","2008-05-01T00:00:00",401240.118131983792409,0.401240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230796E55073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.201982542173539,55.072427000000005]
["glac_bound",379939.000000000000000,"G226398E58855N","2008-05-01T00:00:00",202433.194142467575148,0.202433000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226398E58855N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.603043261517570,58.855040500000001]
["glac_bound",379942.000000000000000,"G223670E59570N","2008-05-01T00:00:00",67518.111019687930821,0.067518000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223670E59570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.329779621668536,59.570063500000003]
["glac_bound",379945.000000000000000,"G224384E59890N","2008-05-01T00:00:00",56325.601446032553213,0.056326000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224384E59890N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.615597676666653,59.889640999999997]
["glac_bound",379946.000000000000000,"G230371E55728N","2008-05-01T00:00:00",163889.007143962400733,0.163889000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230371E55728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.629393027304644,55.728211999999999]
["glac_bound",379948.000000000000000,"G228439E57094N","2008-05-01T00:00:00",4458400.031950301490724,4.458400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228439E57094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.561522264384962,57.095914499999999]
["glac_bound",379951.000000000000000,"G222368E59859N","2008-05-01T00:00:00",317645.146872356766835,0.317645000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222368E59859N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.630681146341487,59.858867500000002]
["glac_bound",379957.000000000000000,"G229452E56883N","2008-05-01T00:00:00",1758600.544979092432186,1.758600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229452E56883N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.546259358008740,56.884597999999997]
["glac_bound",379958.000000000000000,"G231121E55219N","2008-05-01T00:00:00",236521.446503175946418,0.236521000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231121E55219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.878387400495569,55.219217499999999]
["glac_bound",379961.000000000000000,"G228041E57439N","2008-05-01T00:00:00",2740479.218458103481680,2.740480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228041E57439N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.948832573100901,57.438017000000002]
["glac_bound",379966.000000000000000,"G228484E57101N","2008-05-01T00:00:00",3600059.613464696332812,3.600060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228484E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.531507067093628,57.098377499999998]
["glac_bound",379967.000000000000000,"G229701E56568N","2008-05-01T00:00:00",217879.468384745123331,0.217879000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229701E56568N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.298534625716627,56.568376000000001]
["glac_bound",379971.000000000000000,"G228132E57567N","2008-05-01T00:00:00",805608.903721757116728,0.805609000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228132E57567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.868602485035410,57.567644000000001]
["glac_bound",379972.000000000000000,"G230049E56134N","2008-05-01T00:00:00",1299360.339832996949553,1.299360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230049E56134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.953709151438773,56.143032500000004]
["glac_bound",379974.000000000000000,"G231257E57546N","2008-05-01T00:00:00",497939.026319744531065,0.497939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231257E57546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.744287917103009,57.545602000000002]
["glac_bound",379975.000000000000000,"G227594E58214N","2008-05-01T00:00:00",131820.631234338099603,0.131821000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227594E58214N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.406547361695743,58.214142000000002]
["glac_bound",379976.000000000000000,"G228041E57427N","2008-05-01T00:00:00",232630.822754228109261,0.232631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228041E57427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.960387767063310,57.426762999999994]
["glac_bound",379980.000000000000000,"G228067E57789N","2008-05-01T00:00:00",469660.019242629350629,0.469660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228067E57789N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.934455097226504,57.789361000000000]
["glac_bound",379982.000000000000000,"G226811E58477N","2008-05-01T00:00:00",402110.570675058756024,0.402111000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226811E58477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.187153198545616,58.475946000000000]
["glac_bound",379987.000000000000000,"G225416E59513N","2008-05-01T00:00:00",1886128.520015883725137,1.886130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225416E59513N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.588651663690939,59.519086500000000]
["glac_bound",379988.000000000000000,"G230258E56984N","2008-05-01T00:00:00",795232.235896235797554,0.795232000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230258E56984N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.739733384554199,56.984543500000001]
["glac_bound",379996.000000000000000,"G229613E56757N","2008-05-01T00:00:00",63489.024169549047656,0.063489000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229613E56757N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.389760238878182,56.756652500000001]
["glac_bound",379998.000000000000000,"G224347E59760N","2008-05-01T00:00:00",1853822.293992382241413,1.853820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224347E59760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.651621659634401,59.756194999999998]
["glac_bound",380003.000000000000000,"G222196E59598N","2008-05-01T00:00:00",297378.267972110304981,0.297378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222196E59598N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.801296848706443,59.598661000000000]
["glac_bound",380008.000000000000000,"G229043E56450N","2008-05-01T00:00:00",5101619.055706411600113,5.101620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG229043E56450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.950598527553097,56.452246000000002]
["glac_bound",380011.000000000000000,"G228002E57115N","2008-05-01T00:00:00",3402266.956666262354702,3.402270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228002E57115N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.997778432945864,57.134849500000001]
["glac_bound",380019.000000000000000,"G230379E55157N","2008-05-01T00:00:00",221475.916193291166564,0.221476000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230379E55157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.620401582098054,55.156888500000001]
["glac_bound",380021.000000000000000,"G223021E59111N","2008-05-01T00:00:00",124394.713508643952082,0.124395000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223021E59111N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.978937549863190,59.112307500000000]
["glac_bound",380026.000000000000000,"G230754E54899N","2008-05-01T00:00:00",159100.836353904334828,0.159101000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230754E54899N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.246806824844498,54.899645500000005]
["glac_bound",380034.000000000000000,"G230151E56146N","2008-05-01T00:00:00",3090530.596037856303155,3.090530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230151E56146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.844808320309284,56.162508500000001]
["glac_bound",380039.000000000000000,"G229441E57541N","2008-05-01T00:00:00",203119.938940995227313,0.203120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229441E57541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.558796348703737,57.541925500000005]
["glac_bound",380042.000000000000000,"G229190E57095N","2008-05-01T00:00:00",495120.319734908756800,0.495120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229190E57095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.810255114845006,57.095542999999999]
["glac_bound",380043.000000000000000,"G230075E55794N","2008-05-01T00:00:00",139317.716715587914223,0.139318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230075E55794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.924816402139527,55.794283500000006]
["glac_bound",380046.000000000000000,"G228138E56921N","2008-05-01T00:00:00",539015.655384366284125,0.539016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228138E56921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.864209406057114,56.922826999999998]
["glac_bound",380049.000000000000000,"G230414E56070N","2008-05-01T00:00:00",185583.063004871655721,0.185583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230414E56070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.585030652417231,56.070209500000004]
["glac_bound",380051.000000000000000,"G224023E59934N","2008-05-01T00:00:00",659276.909616564284079,0.659277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224023E59934N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.976225827422951,59.934734000000006]
["glac_bound",380057.000000000000000,"G230556E54979N","2008-05-01T00:00:00",70981.188253969085054,0.070981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230556E54979N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.443830544634125,54.979517000000001]
["glac_bound",380069.000000000000000,"G226865E58349N","2008-05-01T00:00:00",180527.189163467701292,0.180527000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226865E58349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.135356624452015,58.348734000000000]
["glac_bound",380071.000000000000000,"G226195E58889N","2008-05-01T00:00:00",2446614.513393228873610,2.446610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226195E58889N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.809254316482509,58.891465500000002]
["glac_bound",380072.000000000000000,"G227781E57819N","2008-05-01T00:00:00",51980.870162512001116,0.051981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227781E57819N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.219160779371180,57.818839999999994]
["glac_bound",380076.000000000000000,"G224120E59920N","2008-05-01T00:00:00",131763.129479544673814,0.131763000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224120E59920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.880731215544415,59.920433000000003]
["glac_bound",380077.000000000000000,"G229319E56294N","2008-05-01T00:00:00",23322.869929700391367,0.023323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229319E56294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.681436997252746,56.293658000000001]
["glac_bound",380078.000000000000000,"G222533E59189N","2008-05-01T00:00:00",261269.356920711550629,0.261269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222533E59189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.466433979623730,59.188136999999998]
["glac_bound",380081.000000000000000,"G226766E58481N","2008-05-01T00:00:00",3362174.897486876230687,3.362170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226766E58481N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.225241187787191,58.489191000000005]
["glac_bound",380084.000000000000000,"G228827E57312N","2008-05-01T00:00:00",2233018.505493978504092,2.233020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228827E57312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.171767721276126,57.317986000000005]
["glac_bound",380099.000000000000000,"G225908E59300N","2008-05-01T00:00:00",224896.274186343420297,0.224896000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225908E59300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.092097735165652,59.300230499999998]
["glac_bound",380103.000000000000000,"G225246E59469N","2008-05-01T00:00:00",211204.651422787021147,0.211205000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225246E59469N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.757903341336089,59.468154499999997]
["glac_bound",380105.000000000000000,"G229332E56619N","2008-05-01T00:00:00",1499785.360541123896837,1.499790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229332E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.671668365686173,56.626834000000002]
["glac_bound",380114.000000000000000,"G228773E57543N","2008-05-01T00:00:00",401156.233318484271877,0.401156000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228773E57543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.222742832110953,57.543857500000001]
["glac_bound",380116.000000000000000,"G221819E59732N","2008-05-01T00:00:00",1035993.465162307722494,1.035990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221819E59732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.186015883793686,59.731385000000003]
["glac_bound",380127.000000000000000,"G227139E58444N","2008-05-01T00:00:00",74323.430150876374682,0.074323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227139E58444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.859217363568973,58.444338000000002]
["glac_bound",380128.000000000000000,"G228550E57039N","2008-05-01T00:00:00",169211.036962685815524,0.169211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228550E57039N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.449020731548615,57.039343000000002]
["glac_bound",380130.000000000000000,"G230043E56880N","2008-05-01T00:00:00",70173.121296907746000,0.070173000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230043E56880N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.957659911607067,56.880395500000006]
["glac_bound",380137.000000000000000,"G226859E58437N","2008-05-01T00:00:00",1753851.424198836786672,1.753850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226859E58437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.148821144681904,58.438879499999999]
["glac_bound",380142.000000000000000,"G221972E59953N","2008-05-01T00:00:00",2038193.392982404679060,2.038190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221972E59953N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.027359824772191,59.952376999999998]
["glac_bound",380147.000000000000000,"G222328E59657N","2008-05-01T00:00:00",346994.780670205538627,0.346995000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222328E59657N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.674255452139732,59.654960000000003]
["glac_bound",380159.000000000000000,"G230623E56828N","2008-05-01T00:00:00",352378.898982336861081,0.352379000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230623E56828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.376374151116920,56.827510000000004]
["glac_bound",380162.000000000000000,"G230168E56139N","2008-05-01T00:00:00",1320031.755850169574842,1.320030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230168E56139N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.826436904692343,56.140290000000000]
["glac_bound",380163.000000000000000,"G229238E56495N","2008-05-01T00:00:00",788937.128251945250668,0.788937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229238E56495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.764177938805346,56.495305999999999]
["glac_bound",380164.000000000000000,"G226799E58571N","2008-05-01T00:00:00",925866.983385553699918,0.925867000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226799E58571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.202991626630336,58.573041000000003]
["glac_bound",380167.000000000000000,"G229398E57207N","2008-05-01T00:00:00",127786.187799292587442,0.127786000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229398E57207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.602333088445789,57.207109000000003]
["glac_bound",380176.000000000000000,"G230364E56709N","2008-05-01T00:00:00",104000.461870505925617,0.104000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230364E56709N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.635043737373735,56.708663000000001]
["glac_bound",380178.000000000000000,"G225314E59222N","2008-05-01T00:00:00",381661.340811963018496,0.381661000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225314E59222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.690116309945495,59.222181500000005]
["glac_bound",380179.000000000000000,"G230218E55950N","2008-05-01T00:00:00",1806886.219587088795379,1.806890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230218E55950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.781338950329939,55.960036500000001]
["glac_bound",380181.000000000000000,"G225264E59793N","2008-05-01T00:00:00",168557.249357624008553,0.168557000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225264E59793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.739613512289509,59.795556500000004]
["glac_bound",380182.000000000000000,"G228044E57788N","2008-05-01T00:00:00",1810978.292158893309534,1.810980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228044E57788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.958237030402245,57.794756499999998]
["glac_bound",380184.000000000000000,"G230549E55324N","2008-05-01T00:00:00",108285.758485011960147,0.108286000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230549E55324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.449338558923387,55.322975999999997]
["glac_bound",380190.000000000000000,"G222263E59726N","2008-05-01T00:00:00",70161.432728611252969,0.070161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222263E59726N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.735933825783974,59.724786500000000]
["glac_bound",380191.000000000000000,"G230543E56736N","2008-05-01T00:00:00",198399.241398496524198,0.198399000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230543E56736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.457135438524574,56.735945500000000]
["glac_bound",380195.000000000000000,"G224290E59975N","2008-05-01T00:00:00",66060.580978179132217,0.066061000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224290E59975N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.714440130810118,59.975651499999998]
["glac_bound",380196.000000000000000,"G226331E58731N","2008-05-01T00:00:00",238369.524217014346505,0.238370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226331E58731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.669392544392508,58.730771000000004]
["glac_bound",380204.000000000000000,"G227274E58276N","2008-05-01T00:00:00",595643.847101884079166,0.595644000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227274E58276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.724707717864533,58.274297000000004]
["glac_bound",380206.000000000000000,"G230681E56792N","2008-05-01T00:00:00",420055.524978487868793,0.420056000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230681E56792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.316827155427688,56.793520000000001]
["glac_bound",380207.000000000000000,"G224884E59810N","2008-05-01T00:00:00",112889.320728439823142,0.112889000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224884E59810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.115258336293948,59.810572999999998]
["glac_bound",380208.000000000000000,"G222186E59390N","2008-05-01T00:00:00",655901.406476194737479,0.655901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222186E59390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.814078315162902,59.387606000000005]
["glac_bound",380213.000000000000000,"G223175E59355N","2008-05-01T00:00:00",3130261.878206931520253,3.130260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223175E59355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.839351435349954,59.358547999999999]
["glac_bound",380215.000000000000000,"G228745E57199N","2008-05-01T00:00:00",68282.828169974571210,0.068283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228745E57199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.254436594110587,57.198972499999996]
["glac_bound",380231.000000000000000,"G233139E57621N","2008-05-01T00:00:00",173177.037413626065245,0.173177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233139E57621N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.861743175730624,57.621077499999998]
["glac_bound",380239.000000000000000,"G227454E57825N","2008-05-01T00:00:00",837023.930491035571322,0.837024000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227454E57825N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.546506530811712,57.825101000000004]
["glac_bound",380242.000000000000000,"G226994E57994N","2008-05-01T00:00:00",58170.558573279500706,0.058171000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226994E57994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.005545843122093,57.995147500000002]
["glac_bound",380244.000000000000000,"G229264E57092N","2008-05-01T00:00:00",202462.396126625302713,0.202462000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229264E57092N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.734251030386531,57.092109499999999]
["glac_bound",380247.000000000000000,"G229980E56740N","2008-05-01T00:00:00",80069.137237212315085,0.080069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229980E56740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.020782602273471,56.739784499999999]
["glac_bound",380249.000000000000000,"G223581E59875N","2008-05-01T00:00:00",228139.340009126957739,0.228139000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223581E59875N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.423088662512214,59.876503499999998]
["glac_bound",380250.000000000000000,"G228856E57449N","2008-05-01T00:00:00",74361.054228651482845,0.074361000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228856E57449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.143188633643632,57.449361999999994]
["glac_bound",380251.000000000000000,"G227679E57332N","2008-05-01T00:00:00",26018.601576528213627,0.026019000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227679E57332N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.320511416644734,57.331459500000001]
["glac_bound",380256.000000000000000,"G230069E57453N","2008-05-01T00:00:00",68639.183276008872781,0.068639000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230069E57453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.931309542327256,57.452211500000004]
["glac_bound",380271.000000000000000,"G230918E57412N","2008-05-01T00:00:00",203593.694265927450033,0.203594000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230918E57412N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.083151863475109,57.412880999999999]
["glac_bound",380272.000000000000000,"G223486E59461N","2008-05-01T00:00:00",635776.746320263133384,0.635777000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223486E59461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.512458308206476,59.460976000000002]
["glac_bound",380273.000000000000000,"G230059E55794N","2008-05-01T00:00:00",1270248.294208975508809,1.270250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230059E55794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.939859997150734,55.794232000000001]
["glac_bound",380274.000000000000000,"G225217E59442N","2008-05-01T00:00:00",1783665.832172363763675,1.783670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225217E59442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.768270424078025,59.440027499999999]
["glac_bound",380275.000000000000000,"G230156E56637N","2008-05-01T00:00:00",1542014.783901781775057,1.542010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230156E56637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.840536791502018,56.637163500000000]
["glac_bound",380277.000000000000000,"G230860E55030N","2008-05-01T00:00:00",1203175.083646781276911,1.203180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230860E55030N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.140345633321829,55.031984999999999]
["glac_bound",380283.000000000000000,"G228529E56769N","2008-05-01T00:00:00",713300.359723406028934,0.713300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228529E56769N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.470854413872843,56.766892499999997]
["glac_bound",380291.000000000000000,"G226353E58840N","2008-05-01T00:00:00",151143.860393980692606,0.151144000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226353E58840N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.646778627789530,58.839727999999994]
["glac_bound",380301.000000000000000,"G226674E58645N","2008-05-01T00:00:00",2131530.344642134848982,2.131530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226674E58645N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.330681002018309,58.653690499999996]
["glac_bound",380302.000000000000000,"G222710E59380N","2008-05-01T00:00:00",2458582.998321983031929,2.458580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222710E59380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.295431540257425,59.391643500000001]
["glac_bound",380305.000000000000000,"G229384E57275N","2008-05-01T00:00:00",179181.423603825707687,0.179181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229384E57275N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.615661072810326,57.274874500000003]
["glac_bound",380309.000000000000000,"G227870E57366N","2008-05-01T00:00:00",1632521.190225634491071,1.632520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227870E57366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.128701456993042,57.371268999999998]
["glac_bound",380310.000000000000000,"G227519E58185N","2008-05-01T00:00:00",787078.256665150751360,0.787078000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227519E58185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.480080977452928,58.184088000000003]
["glac_bound",380312.000000000000000,"G226603E58630N","2008-05-01T00:00:00",105923.437067727150861,0.105923000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226603E58630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.397275327405850,58.630903000000004]
["glac_bound",380322.000000000000000,"G228821E57364N","2008-05-01T00:00:00",2414494.935971841681749,2.414490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228821E57364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.187781995513262,57.361519500000000]
["glac_bound",380323.000000000000000,"G226850E58544N","2008-05-01T00:00:00",205619.830171642155619,0.205620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226850E58544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.152264744151125,58.543864499999998]
["glac_bound",380326.000000000000000,"G224066E59868N","2008-05-01T00:00:00",690861.029176466632634,0.690861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224066E59868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.934149773670640,59.867983500000001]
["glac_bound",380327.000000000000000,"G225547E59486N","2008-05-01T00:00:00",268794.365856092772447,0.268794000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225547E59486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.452463108132065,59.486011000000005]
["glac_bound",380330.000000000000000,"G229212E57220N","2008-05-01T00:00:00",850508.668152557220310,0.850509000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229212E57220N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.792300923233370,57.220251000000005]
["glac_bound",380339.000000000000000,"G223736E59871N","2008-05-01T00:00:00",1354881.952513812109828,1.354880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223736E59871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.269032422796016,59.868937000000003]
["glac_bound",380344.000000000000000,"G229167E57179N","2008-05-01T00:00:00",1066143.901169159216806,1.066140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229167E57179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.832539600050552,57.178466499999999]
["glac_bound",380345.000000000000000,"G230662E54920N","2008-05-01T00:00:00",95504.688895261249854,0.095505000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230662E54920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.338714033826989,54.920182499999996]
["glac_bound",380346.000000000000000,"G230287E56266N","2008-05-01T00:00:00",386943.930423658341169,0.386944000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230287E56266N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.710898438826291,56.267161500000000]
["glac_bound",380349.000000000000000,"G224481E59885N","2008-05-01T00:00:00",150801.234514346666401,0.150801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224481E59885N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.520358986840449,59.885175000000004]
["glac_bound",380351.000000000000000,"G224091E59682N","2008-05-01T00:00:00",281959.874238204502035,0.281960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224091E59682N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.907499629885763,59.682343500000002]
["glac_bound",380353.000000000000000,"G227844E57472N","2008-05-01T00:00:00",2552718.161998014897108,2.552720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227844E57472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.158287841971571,57.474497499999998]
["glac_bound",380355.000000000000000,"G231531E57266N","2008-05-01T00:00:00",199298.425958704203367,0.199298000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231531E57266N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.469411583740055,57.266243000000003]
["glac_bound",380363.000000000000000,"G224215E59870N","2008-05-01T00:00:00",50892.652360338353901,0.050893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224215E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.784831841290952,59.871352000000002]
["glac_bound",380367.000000000000000,"G226996E57990N","2008-05-01T00:00:00",2595073.609862440731376,2.595070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226996E57990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.017352929283902,57.990201499999998]
["glac_bound",380370.000000000000000,"G231429E56061N","2008-05-01T00:00:00",288105.445732871186920,0.288105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231429E56061N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.569230922279814,56.060371500000002]
["glac_bound",380372.000000000000000,"G227725E58039N","2008-05-01T00:00:00",479841.522579663374927,0.479842000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227725E58039N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.277721452614060,58.038306500000004]
["glac_bound",380374.000000000000000,"G226255E59006N","2008-05-01T00:00:00",2896249.355526259168983,2.896250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226255E59006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.748549469376542,59.007757999999995]
["glac_bound",380382.000000000000000,"G228492E57148N","2008-05-01T00:00:00",490112.673535324167460,0.490113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228492E57148N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.509247398004220,57.147854500000001]
["glac_bound",380390.000000000000000,"G228090E57582N","2008-05-01T00:00:00",358765.874597644258756,0.358766000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228090E57582N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.906655580341692,57.583695500000005]
["glac_bound",380394.000000000000000,"G222468E59251N","2008-05-01T00:00:00",126354.429217090641032,0.126354000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222468E59251N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.531419074645328,59.252112499999996]
["glac_bound",380402.000000000000000,"G227282E58354N","2008-05-01T00:00:00",83378.532842347063706,0.083378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227282E58354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.717757530591996,58.353649000000004]
["glac_bound",380404.000000000000000,"G222583E59239N","2008-05-01T00:00:00",367139.514868524682242,180.536000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Melbern Glacier","None","08AB222583E59239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.414904333857493,59.239848500000001]
["glac_bound",380404.000000000000000,"G222583E59239N","2008-05-01T00:00:00",180169110.48197552561759,180.536000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Melbern Glacier","None","08AB222583E59239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.676311215702867,59.228444499999995]
["glac_bound",380405.000000000000000,"G227589E57558N","2008-05-01T00:00:00",1437331.481705683516338,1.437330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227589E57558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.415898524825366,57.562600500000002]
["glac_bound",380406.000000000000000,"G224941E59433N","2008-05-01T00:00:00",5339336.859920633956790,5.339340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224941E59433N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.111166472232128,59.439863500000001]
["glac_bound",380407.000000000000000,"G229410E56857N","2008-05-01T00:00:00",187590.202356358873658,0.187590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229410E56857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.587990678770069,56.857827999999998]
["glac_bound",380410.000000000000000,"G230110E56779N","2008-05-01T00:00:00",569124.573848332860507,0.569125000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230110E56779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.888733357786577,56.778894999999999]
["glac_bound",380417.000000000000000,"G230331E56238N","2008-05-01T00:00:00",4789585.061316227540374,4.789590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230331E56238N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.683257804545462,56.251719000000001]
["glac_bound",380418.000000000000000,"G225473E59480N","2008-05-01T00:00:00",238915.532648404419888,0.238916000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225473E59480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.527833311489474,59.480843000000000]
["glac_bound",380419.000000000000000,"G230297E55803N","2008-05-01T00:00:00",25137179.483673159033060,25.137200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230297E55803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.726019056464679,55.785050499999997]
["glac_bound",380422.000000000000000,"G225407E59424N","2008-05-01T00:00:00",747330.271816101158038,0.747330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225407E59424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.593702028744133,59.424374000000000]
["glac_bound",380423.000000000000000,"G226448E58760N","2008-05-01T00:00:00",3427905.051252219825983,3.427910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226448E58760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.553269750206312,58.759816999999998]
["glac_bound",380432.000000000000000,"G230288E57269N","2008-05-01T00:00:00",107465.955737578420667,0.107466000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230288E57269N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.711657181297710,57.268912000000000]
["glac_bound",380436.000000000000000,"G228830E57510N","2008-05-01T00:00:00",314469.294473147194367,0.314469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228830E57510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.170343249917494,57.510238000000001]
["glac_bound",380439.000000000000000,"G228895E57698N","2008-05-01T00:00:00",322949.853427868161816,0.322950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228895E57698N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.106221179274996,57.697452499999997]
["glac_bound",380440.000000000000000,"G222461E59641N","2008-05-01T00:00:00",3900442.129491818137467,3.900440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222461E59641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.548652966653208,59.644677999999999]
["glac_bound",380441.000000000000000,"G229682E56430N","2008-05-01T00:00:00",394808.603692880482413,0.394809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229682E56430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.318150435572988,56.431227499999999]
["glac_bound",380443.000000000000000,"G226737E58243N","2008-05-01T00:00:00",351732.778391308034770,0.351733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226737E58243N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.264168439633494,58.243499000000000]
["glac_bound",380446.000000000000000,"G222373E59512N","2008-05-01T00:00:00",2754846.795992070343345,2.754850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222373E59512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.625952194571170,59.511223999999999]
["glac_bound",380452.000000000000000,"G229786E56804N","2008-05-01T00:00:00",1328712.867342899786308,1.328710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229786E56804N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.212163107142828,56.806099000000003]
["glac_bound",380458.000000000000000,"G229316E57404N","2008-05-01T00:00:00",275935.115282862738241,0.275935000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229316E57404N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.685537681390173,57.406376000000002]
["glac_bound",380459.000000000000000,"G230472E57062N","2008-05-01T00:00:00",205458.781663438479882,0.205459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230472E57062N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.530084334351017,57.061993000000001]
["glac_bound",380461.000000000000000,"G230474E56625N","2008-05-01T00:00:00",2855496.918724131304771,2.855500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230474E56625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522884908580181,56.635227999999998]
["glac_bound",380462.000000000000000,"G228442E57203N","2008-05-01T00:00:00",335762.387550364073832,0.335762000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228442E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.557812512679845,57.203186000000002]
["glac_bound",380463.000000000000000,"G224075E59713N","2008-05-01T00:00:00",74244.321544028876815,0.074244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224075E59713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.924652082740465,59.713070999999999]
["glac_bound",380466.000000000000000,"G222293E59374N","2008-05-01T00:00:00",277436.519401048019063,0.277437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222293E59374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.706892141050560,59.374369000000002]
["glac_bound",380468.000000000000000,"G230403E55820N","2008-05-01T00:00:00",5420809.163637325167656,149.882000000000005,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230403E55820N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.469808422263100,55.847721000000000]
["glac_bound",380468.000000000000000,"G230403E55820N","2008-05-01T00:00:00",144461347.05184328556060,149.882000000000005,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230403E55820N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.659436928268235,55.840438000000006]
["glac_bound",380469.000000000000000,"G229035E57200N","2008-05-01T00:00:00",603755.652925260248594,0.603756000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229035E57200N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.963683792834900,57.199252000000001]
["glac_bound",380475.000000000000000,"G229336E56299N","2008-05-01T00:00:00",1002767.952277309144847,1.002770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229336E56299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.663259012883088,56.302127499999997]
["glac_bound",380477.000000000000000,"G229811E56819N","2008-05-01T00:00:00",949985.492189925280400,0.949986000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229811E56819N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.188492712623031,56.817157500000000]
["glac_bound",380478.000000000000000,"G229151E56390N","2008-05-01T00:00:00",212887.666461592656560,0.212888000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229151E56390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.849237394652050,56.390079499999999]
["glac_bound",380485.000000000000000,"G223086E59544N","2008-05-01T00:00:00",1853091.574131987523288,1.853090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223086E59544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.914016555554696,59.542272999999994]
["glac_bound",380486.000000000000000,"G230531E57137N","2008-05-01T00:00:00",369589.942381743632723,0.369590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230531E57137N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.469583109983716,57.138865000000003]
["glac_bound",380493.000000000000000,"G230673E56881N","2008-05-01T00:00:00",105901.733374553397880,0.105902000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230673E56881N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.324136922657004,56.882628499999996]
["glac_bound",380494.000000000000000,"G227691E57501N","2008-05-01T00:00:00",3941040.107426226604730,18.791300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227691E57501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.342147545168785,57.485636499999998]
["glac_bound",380494.000000000000000,"G227691E57501N","2008-05-01T00:00:00",4962985.769120112992823,18.791300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227691E57501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.297325486875792,57.504579500000006]
["glac_bound",380494.000000000000000,"G227691E57501N","2008-05-01T00:00:00",9887277.088528757914901,18.791300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227691E57501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.309877191107660,57.524526999999999]
["glac_bound",380496.000000000000000,"G228611E56531N","2008-05-01T00:00:00",144862.201106593973236,0.144862000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228611E56531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.389617458625992,56.531340000000000]
["glac_bound",380497.000000000000000,"G224400E59841N","2008-05-01T00:00:00",1210242.291805393062532,1.210240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224400E59841N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.600674318303277,59.841642499999999]
["glac_bound",380498.000000000000000,"G222709E59371N","2008-05-01T00:00:00",1615355.571182923857123,1.615360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222709E59371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.292665194170411,59.370109499999998]
["glac_bound",380500.000000000000000,"G228019E57965N","2008-05-01T00:00:00",938268.836150006158277,0.938269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228019E57965N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.979913648463054,57.970061999999999]
["glac_bound",380508.000000000000000,"G227036E58475N","2008-05-01T00:00:00",792146.438377934973687,0.792146000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227036E58475N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.963908539758734,58.474885999999998]
["glac_bound",380517.000000000000000,"G229949E56520N","2008-05-01T00:00:00",100648.896786530327518,0.100649000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229949E56520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.051309790773644,56.521888000000004]
["glac_bound",380518.000000000000000,"G222561E59360N","2008-05-01T00:00:00",650181.983217586064711,0.650182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222561E59360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.439953907750635,59.362667500000001]
["glac_bound",380521.000000000000000,"G227870E57490N","2008-05-01T00:00:00",2636760.453301731962711,2.636760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227870E57490N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.122377110802034,57.492372000000003]
["glac_bound",380524.000000000000000,"G229762E56313N","2008-05-01T00:00:00",156190041.66834524273872,156.189999999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DA229762E56313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.254483367191767,56.297454500000001]
["glac_bound",380529.000000000000000,"G222966E59392N","2008-05-01T00:00:00",3055875.670096427667886,3.055880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222966E59392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.032502263787649,59.397198000000003]
["glac_bound",380530.000000000000000,"G227977E57785N","2008-05-01T00:00:00",1228319.260617325082421,1.228320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227977E57785N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.017039928414874,57.783073000000002]
["glac_bound",380531.000000000000000,"G230307E55113N","2008-05-01T00:00:00",171989.788754166365834,0.171990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230307E55113N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.689430429112292,55.112679499999999]
["glac_bound",380532.000000000000000,"G222604E58936N","2008-05-01T00:00:00",29007.220208569226088,0.029007000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222604E58936N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.396851959802234,58.935683499999996]
["glac_bound",380533.000000000000000,"G229367E57753N","2008-05-01T00:00:00",2490540.255028075538576,2.490540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229367E57753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.633452747873775,57.755007500000005]
["glac_bound",380538.000000000000000,"G228798E56977N","2008-05-01T00:00:00",36361292.170857712626457,36.361300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228798E56977N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.155440934397774,57.001918000000003]
["glac_bound",380539.000000000000000,"G223015E59546N","2008-05-01T00:00:00",1318986.769570076139644,1.318990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223015E59546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.985966182365189,59.554557000000003]
["glac_bound",380544.000000000000000,"G221868E59528N","2008-05-01T00:00:00",43498187.240699775516987,43.498199999999997,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221868E59528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.203572540065210,59.546409499999996]
["glac_bound",380546.000000000000000,"G227894E57466N","2008-05-01T00:00:00",97904.687292935210280,0.097905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227894E57466N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.107971592862839,57.465794000000002]
["glac_bound",380550.000000000000000,"G227371E58087N","2008-05-01T00:00:00",19281281.829181455075741,19.281300000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Cheja West Glacier","None","08BC227371E58087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.596992758347255,58.087348500000004]
["glac_bound",380557.000000000000000,"G221675E59987N","2008-05-01T00:00:00",162766.480248085979838,0.162766000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221675E59987N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.326520042471373,59.987506499999995]
["glac_bound",380559.000000000000000,"G230287E55595N","2008-05-01T00:00:00",96786.337709465675289,0.096786000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230287E55595N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.711061664137901,55.596060999999999]
["glac_bound",380567.000000000000000,"G222728E59091N","2008-05-01T00:00:00",127916.290818092311383,0.127916000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222728E59091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.273906378553647,59.089587500000000]
["glac_bound",380568.000000000000000,"G230932E57410N","2008-05-01T00:00:00",184738.145597732043825,0.184738000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230932E57410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.066801938428625,57.409848499999995]
["glac_bound",380569.000000000000000,"G222563E59190N","2008-05-01T00:00:00",104210.482388247692143,0.104210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222563E59190N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.437403504691332,59.190208999999996]
["glac_bound",380578.000000000000000,"G230563E55299N","2008-05-01T00:00:00",37046966.689409337937832,37.046999999999997,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230563E55299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.429843189455482,55.294200000000004]
["glac_bound",380582.000000000000000,"G228659E56589N","2008-05-01T00:00:00",433130.679070011654403,0.433131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228659E56589N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.344872470341897,56.586084000000000]
["glac_bound",380585.000000000000000,"G230293E55893N","2008-05-01T00:00:00",113076756.06703509390354,113.076999999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230293E55893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.672802539842564,55.924749500000004]
["glac_bound",380597.000000000000000,"G224966E59452N","2008-05-01T00:00:00",10284698.220015246421099,10.284700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","South Glacier","None","08BE224966E59452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.036640339282314,59.447203000000002]
["glac_bound",380599.000000000000000,"G228991E56611N","2008-05-01T00:00:00",855129.110338113387115,0.855129000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228991E56611N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.016815185699642,56.609636999999999]
["glac_bound",380603.000000000000000,"G227834E57565N","2008-05-01T00:00:00",3546420.194194146897644,3.546420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227834E57565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.161073443758085,57.569530000000000]
["glac_bound",380608.000000000000000,"G229450E56368N","2008-05-01T00:00:00",1743464.335761409020051,1.743460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229450E56368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.550785507288367,56.368722500000004]
["glac_bound",380609.000000000000000,"G229299E56457N","2008-05-01T00:00:00",52480.990790447751351,0.052481000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229299E56457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.698841122395834,56.456157000000005]
["glac_bound",380614.000000000000000,"G229590E56382N","2008-05-01T00:00:00",476942.038182024087291,0.476942000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229590E56382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.409858380090498,56.381290500000006]
["glac_bound",380618.000000000000000,"G227745E57181N","2008-05-01T00:00:00",17056.483892173182539,0.017056000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227745E57181N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.254966056892783,57.180636000000000]
["glac_bound",380622.000000000000000,"G230176E57000N","2008-05-01T00:00:00",88711.223352079832694,0.088711000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230176E57000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.823095435993139,56.999775499999998]
["glac_bound",380630.000000000000000,"G229752E56545N","2008-05-01T00:00:00",122302.048312488739612,0.122302000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229752E56545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.245082195041903,56.545858500000001]
["glac_bound",380634.000000000000000,"G225514E59256N","2008-05-01T00:00:00",568113.601486993604340,0.568114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225514E59256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.484053618017128,59.256201000000004]
["glac_bound",380635.000000000000000,"G232886E57761N","2008-05-01T00:00:00",239604.509774725069292,0.239605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232886E57761N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.114103161442188,57.761633500000002]
["glac_bound",380643.000000000000000,"G227811E58061N","2008-05-01T00:00:00",1063157.043132080463693,1.063160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227811E58061N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.187331850193971,58.067807500000001]
["glac_bound",380644.000000000000000,"G229635E56575N","2008-05-01T00:00:00",8976515.379729032516479,8.976520000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229635E56575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.367968787638972,56.584035000000000]
["glac_bound",380646.000000000000000,"G222112E59522N","2008-05-01T00:00:00",51312.633900297601940,0.051313000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222112E59522N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.889258647310726,59.522007000000002]
["glac_bound",380649.000000000000000,"G221806E59965N","2008-05-01T00:00:00",237242.521146197454073,0.237243000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221806E59965N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.194468838551700,59.963934999999999]
["glac_bound",380651.000000000000000,"G227110E58294N","2008-05-01T00:00:00",352231.398972855531611,0.352231000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227110E58294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.895933524765553,58.299615500000002]
["glac_bound",380652.000000000000000,"G230564E57031N","2008-05-01T00:00:00",984621.027631360688247,0.984621000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230564E57031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.432942407832570,57.029418000000000]
["glac_bound",380653.000000000000000,"G228891E57043N","2008-05-01T00:00:00",2993402.041817217599601,2.993400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228891E57043N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.109769540643413,57.044620000000002]
["glac_bound",380654.000000000000000,"G231143E57353N","2008-05-01T00:00:00",127911.075613837005221,0.127911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231143E57353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.857336379049627,57.353013000000004]
["glac_bound",380660.000000000000000,"G221656E59657N","2008-05-01T00:00:00",345243283.45494711399078,345.242999999999995,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","Vern Ritchie Glacier","None","08AB221656E59657N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.435527809304915,59.730640000000001]
["glac_bound",380661.000000000000000,"G228272E57228N","2008-05-01T00:00:00",50181.294672070704110,0.050181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228272E57228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.728386276274023,57.228411500000000]
["glac_bound",380666.000000000000000,"G223593E59835N","2008-05-01T00:00:00",2030335.842431392986327,2.030340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223593E59835N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.405933170112064,59.834429499999999]
["glac_bound",380669.000000000000000,"G225731E59318N","2008-05-01T00:00:00",394577.119600637292024,0.394577000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225731E59318N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.268265476562476,59.317318499999999]
["glac_bound",380670.000000000000000,"G230618E56699N","2008-05-01T00:00:00",621493.198064963216893,0.621493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230618E56699N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.380679391782337,56.700208500000002]
["glac_bound",380671.000000000000000,"G227256E58270N","2008-05-01T00:00:00",261283.388298318022862,0.261283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227256E58270N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.743405345730707,58.269851500000001]
["glac_bound",380679.000000000000000,"G230040E56055N","2008-05-01T00:00:00",153016.069376575702336,0.153016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230040E56055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.960867242728170,56.055228499999998]
["glac_bound",380682.000000000000000,"G230032E57044N","2008-05-01T00:00:00",2199389.090944766066968,2.199390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230032E57044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.973345129409239,57.052037999999996]
["glac_bound",380693.000000000000000,"G229972E57047N","2008-05-01T00:00:00",84441.529560375085566,0.084442000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229972E57047N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.028083152889565,57.046643500000002]
["glac_bound",380697.000000000000000,"G223146E59487N","2008-05-01T00:00:00",464436.813420680351555,0.464437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223146E59487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.852578356325495,59.487471999999997]
["glac_bound",380700.000000000000000,"G227175E58454N","2008-05-01T00:00:00",193736.139615752472309,0.193736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227175E58454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.825191360541908,58.454082999999997]
["glac_bound",380704.000000000000000,"G228516E57084N","2008-05-01T00:00:00",1437418.613990860059857,1.437420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228516E57084N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.474036769132084,57.083774500000004]
["glac_bound",380706.000000000000000,"G230575E54693N","2008-05-01T00:00:00",734141.938215117203072,0.734142000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230575E54693N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.429676433637326,54.691738000000001]
["glac_bound",380709.000000000000000,"G226221E58683N","2008-05-01T00:00:00",244160.238028537452919,0.244160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226221E58683N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.779684730026531,58.683412000000004]
["glac_bound",380713.000000000000000,"G230106E56559N","2008-05-01T00:00:00",131984.581944309145911,0.131985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230106E56559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.893274439633785,56.559266500000000]
["glac_bound",380719.000000000000000,"G227311E58434N","2008-05-01T00:00:00",217312.192242329125293,0.217312000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227311E58434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.686517369930527,58.435775000000000]
["glac_bound",380726.000000000000000,"G229844E57791N","2008-05-01T00:00:00",92632.446984801179497,0.092633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229844E57791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.156261343971607,57.790931000000000]
["glac_bound",380727.000000000000000,"G223291E59762N","2008-05-01T00:00:00",827248.172691087238491,0.827248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223291E59762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.709218041210192,59.762981500000002]
["glac_bound",380733.000000000000000,"G227886E58070N","2008-05-01T00:00:00",312250.167576117382850,0.312250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227886E58070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.120122350155384,58.067814999999996]
["glac_bound",380736.000000000000000,"G230211E56256N","2008-05-01T00:00:00",445712.160324285447132,0.445712000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230211E56256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.786530699137813,56.257908999999998]
["glac_bound",380738.000000000000000,"G227159E58373N","2008-05-01T00:00:00",2905035.964926511980593,2.905040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227159E58373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.832190363963775,58.380939999999995]
["glac_bound",380739.000000000000000,"G226187E58786N","2008-05-01T00:00:00",453534.741956843121443,0.453535000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226187E58786N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.813815061174694,58.786312499999994]
["glac_bound",380742.000000000000000,"G228124E57632N","2008-05-01T00:00:00",266110.405340136610903,0.266110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228124E57632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.875259350967326,57.633223000000001]
["glac_bound",380743.000000000000000,"G230569E55897N","2008-05-01T00:00:00",209968.885547989571933,0.209969000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230569E55897N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.427302431581325,55.899112500000001]
["glac_bound",380744.000000000000000,"G231126E57116N","2008-05-01T00:00:00",112416.501484130902099,0.112416000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231126E57116N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.873058764349082,57.115664500000001]
["glac_bound",380746.000000000000000,"G228724E57481N","2008-05-01T00:00:00",123232.203705925217946,0.123232000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228724E57481N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.274120406269304,57.480530000000002]
["glac_bound",380748.000000000000000,"G227643E58284N","2008-05-01T00:00:00",427380.877916362951510,0.427381000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227643E58284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.350217106909440,58.285702999999998]
["glac_bound",380749.000000000000000,"G230423E56252N","2008-05-01T00:00:00",2328567.020064383745193,2.328570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230423E56252N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.586239265018833,56.255069499999998]
["glac_bound",380751.000000000000000,"G230629E57156N","2008-05-01T00:00:00",121766.978508971471456,0.121767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230629E57156N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.370868468948828,57.155688499999997]
["glac_bound",380756.000000000000000,"G229519E57173N","2008-05-01T00:00:00",1163384.216538914246485,1.163380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229519E57173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.475441660170361,57.171646499999994]
["glac_bound",380762.000000000000000,"G230399E56181N","2008-05-01T00:00:00",139877.783752849209122,0.139878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230399E56181N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.600270987593035,56.180894500000001]
["glac_bound",380767.000000000000000,"G230457E56276N","2008-05-01T00:00:00",91577.239898130617803,0.091577000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230457E56276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.543013953228126,56.275658500000006]
["glac_bound",380769.000000000000000,"G227194E58327N","2008-05-01T00:00:00",291849.662071557890158,0.291850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227194E58327N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.800312791643790,58.325843500000005]
["glac_bound",380771.000000000000000,"G228402E56927N","2008-05-01T00:00:00",592628.181602855445817,0.592628000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228402E56927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.603402756549315,56.930421500000001]
["glac_bound",380775.000000000000000,"G229008E56494N","2008-05-01T00:00:00",305959.652252547966782,0.305960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229008E56494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.992921230194725,56.494275500000001]
["glac_bound",380776.000000000000000,"G230146E55741N","2008-05-01T00:00:00",367923.751846285886131,0.367924000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230146E55741N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.853239797856361,55.741331500000001]
["glac_bound",380777.000000000000000,"G230545E56728N","2008-05-01T00:00:00",167983.711900430847891,0.167984000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230545E56728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.456630516878590,56.728336499999997]
["glac_bound",380778.000000000000000,"G227163E58316N","2008-05-01T00:00:00",304850.224612968799192,0.304850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227163E58316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.836718068027210,58.317533499999996]
["glac_bound",380780.000000000000000,"G229069E56403N","2008-05-01T00:00:00",77413.762467445223592,0.077414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229069E56403N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.930940368055559,56.402715499999999]
["glac_bound",380786.000000000000000,"G224004E59770N","2008-05-01T00:00:00",395901.012515905837063,0.395901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224004E59770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.994170936048704,59.770837499999999]
["glac_bound",380795.000000000000000,"G229029E56576N","2008-05-01T00:00:00",1568292.945976624032483,1.568290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229029E56576N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.986175347552489,56.576183499999999]
["glac_bound",380797.000000000000000,"G228867E57533N","2008-05-01T00:00:00",1511594.859712328063324,1.511590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228867E57533N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.129724895398795,57.533963499999999]
["glac_bound",380800.000000000000000,"G227031E58419N","2008-05-01T00:00:00",8438458.943238059058785,8.438459999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227031E58419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.967305970294262,58.418954499999998]
["glac_bound",380804.000000000000000,"G228542E57044N","2008-05-01T00:00:00",4204129.572716856375337,4.204130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228542E57044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.456865492596819,57.049417000000005]
["glac_bound",380807.000000000000000,"G230928E54929N","2008-05-01T00:00:00",715860.546481204801239,0.715861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230928E54929N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.075320576806234,54.930457500000003]
["glac_bound",380811.000000000000000,"G229331E56969N","2008-05-01T00:00:00",709831.836289977072738,0.709832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229331E56969N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.667432536034653,56.971773499999998]
["glac_bound",380821.000000000000000,"G229723E56799N","2008-05-01T00:00:00",1723900.227292446186766,1.723900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229723E56799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.272960800215230,56.799435000000003]
["glac_bound",380826.000000000000000,"G225852E59056N","2008-05-01T00:00:00",1500683.136120952665806,1.500680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225852E59056N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.147529771428566,59.062714999999997]
["glac_bound",380828.000000000000000,"G228606E57049N","2008-05-01T00:00:00",198975.942134710028768,0.198976000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228606E57049N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.391468554136509,57.047688999999998]
["glac_bound",380831.000000000000000,"G229004E56583N","2008-05-01T00:00:00",6070109.804301304742694,6.070110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229004E56583N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.986244919452076,56.599446000000000]
["glac_bound",380833.000000000000000,"G222455E59630N","2008-05-01T00:00:00",673487.298569347942248,0.673487000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222455E59630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.546717325347970,59.630228000000002]
["glac_bound",380835.000000000000000,"G223216E59780N","2008-05-01T00:00:00",1000301.168116112006828,1.000300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223216E59780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.782616123993478,59.780007499999996]
["glac_bound",380839.000000000000000,"G231712E56234N","2008-05-01T00:00:00",72991.080899149630568,0.072991000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EB231712E56234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.289103089010268,56.234205500000002]
["glac_bound",380842.000000000000000,"G230820E55105N","2008-05-01T00:00:00",867644.133392915595323,0.867644000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230820E55105N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.178723539159137,55.104252500000001]
["glac_bound",380848.000000000000000,"G227868E57510N","2008-05-01T00:00:00",87442.766321751638316,0.087443000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227868E57510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.132424062901180,57.510283000000001]
["glac_bound",380849.000000000000000,"G230285E55634N","2008-05-01T00:00:00",1405008.610540539491922,1.405010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230285E55634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.721417482758625,55.637609999999995]
["glac_bound",380852.000000000000000,"G229021E57024N","2008-05-01T00:00:00",1712237.099048731848598,1.712240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229021E57024N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.976088545405872,57.029829500000005]
["glac_bound",380855.000000000000000,"G227646E57855N","2008-05-01T00:00:00",160267.868416364712175,0.160268000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227646E57855N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.354579805867274,57.855062500000003]
["glac_bound",380860.000000000000000,"G222419E59673N","2008-05-01T00:00:00",465307.701017408107873,0.465308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222419E59673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.581414393122827,59.674651999999995]
["glac_bound",380865.000000000000000,"G222651E59008N","2008-05-01T00:00:00",1118536.984284024452791,1.118540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222651E59008N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.347348170009155,59.011893999999998]
["glac_bound",380868.000000000000000,"G223710E59713N","2008-05-01T00:00:00",146562.135023961163824,0.146562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223710E59713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.291176222334627,59.713409999999996]
["glac_bound",380873.000000000000000,"G228345E57427N","2008-05-01T00:00:00",1263276.220002037473023,1.263280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228345E57427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.652732370764028,57.429257500000006]
["glac_bound",380880.000000000000000,"G225678E59283N","2008-05-01T00:00:00",820838.542064359411597,0.820839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225678E59283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.322109873246745,59.281767000000002]
["glac_bound",380881.000000000000000,"G224435E59851N","2008-05-01T00:00:00",75052.184507727593882,0.075052000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224435E59851N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.562964457702719,59.851427500000000]
["glac_bound",380882.000000000000000,"G228537E56554N","2008-05-01T00:00:00",356941.506118540070020,0.356941000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228537E56554N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.464031136846074,56.554755999999998]
["glac_bound",380884.000000000000000,"G231126E55240N","2008-05-01T00:00:00",3002646.351878033019602,3.002650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231126E55240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.873206642160369,55.240978999999996]
["glac_bound",380888.000000000000000,"G225100E59357N","2008-05-01T00:00:00",115394.214904820240918,0.115394000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225100E59357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.900374576530623,59.357416999999998]
["glac_bound",380889.000000000000000,"G230569E55893N","2008-05-01T00:00:00",123237.330598931279383,0.123237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230569E55893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.430582730268668,55.891697000000001]
["glac_bound",380893.000000000000000,"G226660E58671N","2008-05-01T00:00:00",131439.165834160783561,0.131439000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226660E58671N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.340638293064359,58.671112500000000]
["glac_bound",380897.000000000000000,"G223861E59801N","2008-05-01T00:00:00",704286.340522208833136,0.704286000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223861E59801N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.139095052501460,59.801404500000004]
["glac_bound",380900.000000000000000,"G230483E56271N","2008-05-01T00:00:00",313771.280842960579321,0.313771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230483E56271N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.519274162075249,56.271585500000000]
["glac_bound",380901.000000000000000,"G227938E57926N","2008-05-01T00:00:00",2213444.036965564824641,2.213440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227938E57926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.043913123704044,57.931607499999998]
["glac_bound",380902.000000000000000,"G222856E59227N","2008-05-01T00:00:00",1685439.107217392418534,1.685440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222856E59227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.141009133573903,59.226590999999999]
["glac_bound",380904.000000000000000,"G225360E59523N","2008-05-01T00:00:00",237101.745543564233230,0.237102000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225360E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.638252648505613,59.522534499999999]
["glac_bound",380919.000000000000000,"G223255E59384N","2008-05-01T00:00:00",1264436.033953387755901,1.264440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223255E59384N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.748303041440948,59.383663499999997]
["glac_bound",380921.000000000000000,"G228043E57381N","2008-05-01T00:00:00",226559.409614984615473,0.226559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228043E57381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.959754994708533,57.380270499999995]
["glac_bound",380924.000000000000000,"G228093E58061N","2008-05-01T00:00:00",1772231.616296968422830,1.772230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228093E58061N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.903627304494933,58.060625000000002]
["glac_bound",380925.000000000000000,"G230557E57142N","2008-05-01T00:00:00",224198.423640729743056,0.224198000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230557E57142N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.442634080993344,57.141716500000001]
["glac_bound",380928.000000000000000,"G229332E57752N","2008-05-01T00:00:00",99471.292821702867514,0.099471000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229332E57752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.668559675061942,57.752096500000000]
["glac_bound",380929.000000000000000,"G230369E55543N","2008-05-01T00:00:00",737568.539279601653107,0.737569000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230369E55543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.630772876980416,55.543638000000001]
["glac_bound",380931.000000000000000,"G230354E54776N","2008-05-01T00:00:00",97380.948805685286061,0.097381000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230354E54776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.645972501543213,54.776442000000003]
["glac_bound",380932.000000000000000,"G222725E59364N","2008-05-01T00:00:00",1841101.959915110375732,1.841100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222725E59364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.280763021183077,59.362094999999997]
["glac_bound",380933.000000000000000,"G223862E59743N","2008-05-01T00:00:00",2172316.375911151990294,2.172320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223862E59743N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.142557827053849,59.743095500000003]
["glac_bound",380939.000000000000000,"G224279E59766N","2008-05-01T00:00:00",515199.840827176987659,0.515200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224279E59766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.715519299384084,59.766627000000000]
["glac_bound",380943.000000000000000,"G230636E55363N","2008-05-01T00:00:00",116458.419517097034259,0.116458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230636E55363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.363365197865704,55.362971500000000]
["glac_bound",380947.000000000000000,"G228565E57562N","2008-05-01T00:00:00",422509.727356451447122,0.422510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228565E57562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.429742664746328,57.564549999999997]
["glac_bound",380951.000000000000000,"G229487E56280N","2008-05-01T00:00:00",2820649.049605625681579,2.820650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229487E56280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.510444280141826,56.283324000000000]
["glac_bound",380952.000000000000000,"G227240E58352N","2008-05-01T00:00:00",1941299.121489123208448,1.941300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227240E58352N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.760857811452752,58.352817500000000]
["glac_bound",380954.000000000000000,"G230662E57291N","2008-05-01T00:00:00",993968.183249376947060,0.993968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230662E57291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.332387506276035,57.293592500000003]
["glac_bound",380959.000000000000000,"G222590E59747N","2008-05-01T00:00:00",605609.719002160825767,0.605610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222590E59747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.406502957194789,59.747951999999998]
["glac_bound",380961.000000000000000,"G230837E54902N","2008-05-01T00:00:00",124864.128205824279576,0.124864000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230837E54902N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.162541562499996,54.901330000000002]
["glac_bound",380962.000000000000000,"G227882E57764N","2008-05-01T00:00:00",181688.657770685182186,0.181689000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227882E57764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.118509817802817,57.763763499999996]
["glac_bound",380963.000000000000000,"G227342E58244N","2008-05-01T00:00:00",3628174.210493264719844,3.628170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227342E58244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.651255275767454,58.252190999999996]
["glac_bound",380966.000000000000000,"G226250E58773N","2008-05-01T00:00:00",155620.600285067950608,0.155621000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226250E58773N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.750308216413032,58.773143500000003]
["glac_bound",380977.000000000000000,"G227892E57483N","2008-05-01T00:00:00",1588905.387552744010463,1.588910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227892E57483N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.106219934037597,57.486170500000000]
["glac_bound",380980.000000000000000,"G230226E56096N","2008-05-01T00:00:00",349251.941249458643142,0.349252000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230226E56096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.775514925546446,56.097516999999996]
["glac_bound",380982.000000000000000,"G227110E58523N","2008-05-01T00:00:00",385102.962238562642597,0.385103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227110E58523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.887875063432830,58.523414000000002]
["glac_bound",380986.000000000000000,"G230632E55279N","2008-05-01T00:00:00",3270646.478213180322200,3.270650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230632E55279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.373936219280097,55.278585000000000]
["glac_bound",380988.000000000000000,"G223024E59532N","2008-05-01T00:00:00",507360.375964414619375,0.507360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223024E59532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.968989924300104,59.533996500000001]
["glac_bound",380989.000000000000000,"G230372E54894N","2008-05-01T00:00:00",1177910.772818484343588,1.177910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230372E54894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.627978623330364,54.893509500000000]
["glac_bound",380994.000000000000000,"G228465E56625N","2008-05-01T00:00:00",159456.987747398088686,0.159457000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228465E56625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.534905817831429,56.624368500000003]
["glac_bound",380995.000000000000000,"G227936E57952N","2008-05-01T00:00:00",1646698.445426122052595,1.646700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227936E57952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.056027982835360,57.955135499999997]
["glac_bound",380996.000000000000000,"G227241E58316N","2008-05-01T00:00:00",218955.913466540689114,0.218956000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227241E58316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.759225655704029,58.318359999999998]
["glac_bound",380997.000000000000000,"G228147E57408N","2008-05-01T00:00:00",91774.599116048309952,0.091775000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228147E57408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.852544794774673,57.408274000000006]
["glac_bound",380999.000000000000000,"G222774E59109N","2008-05-01T00:00:00",247475.405240654537920,0.247475000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222775E59110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.226445710841404,59.109473999999999]
["glac_bound",381002.000000000000000,"G229769E56741N","2008-05-01T00:00:00",436964.927584328106605,0.436965000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229769E56741N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.230430789262812,56.741288999999995]
["glac_bound",381003.000000000000000,"G225825E59126N","2008-05-01T00:00:00",129017.892007544171065,0.129018000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225825E59126N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.175865220461105,59.126288000000002]
["glac_bound",381006.000000000000000,"G227373E58129N","2008-05-01T00:00:00",402654.259445798990782,0.402654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227373E58129N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.627504717710366,58.129293500000003]
["glac_bound",381014.000000000000000,"G231153E57338N","2008-05-01T00:00:00",209821.697527378157247,0.209822000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231153E57338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.847092441215125,57.338027499999995]
["glac_bound",381015.000000000000000,"G231103E57367N","2008-05-01T00:00:00",932110.915355545352213,0.932111000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231103E57367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.897249152329721,57.367284999999995]
["glac_bound",381020.000000000000000,"G222753E59123N","2008-05-01T00:00:00",1054929.761610864428803,1.054930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222758E59119N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.246202374704325,59.122704499999998]
["glac_bound",381023.000000000000000,"G227076E58080N","2008-05-01T00:00:00",2269870.140292281284928,2.269870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227076E58080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.910379945557423,58.073735999999997]
["glac_bound",381030.000000000000000,"G224590E59994N","2008-05-01T00:00:00",538736.379938514553942,0.538736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224590E59994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.408702583675563,59.992058000000000]
["glac_bound",381041.000000000000000,"G230657E55529N","2008-05-01T00:00:00",1215469.316181987989694,1.215470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230657E55529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.345054608386931,55.529260000000001]
["glac_bound",381043.000000000000000,"G226518E58491N","2008-05-01T00:00:00",59644.849549466947792,0.059645000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226518E58491N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.482983547549395,58.490855999999994]
["glac_bound",381048.000000000000000,"G227104E58098N","2008-05-01T00:00:00",1206787.682853361824527,1.206790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227104E58098N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.897009155666240,58.097864000000001]
["glac_bound",381049.000000000000000,"G230019E55755N","2008-05-01T00:00:00",73614.790697683361941,0.073615000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230019E55755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.983247735391842,55.755142499999998]
["glac_bound",381052.000000000000000,"G229239E56837N","2008-05-01T00:00:00",2110986.679395089857280,2.110990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229239E56837N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.761320286232376,56.837623499999999]
["glac_bound",381057.000000000000000,"G230186E57056N","2008-05-01T00:00:00",1144270.772554746363312,1.144270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230186E57056N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.813901068999144,57.055717500000000]
["glac_bound",381058.000000000000000,"G229580E56558N","2008-05-01T00:00:00",55076.907231945828244,0.055077000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229580E56558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.420380702083321,56.557688499999998]
["glac_bound",381060.000000000000000,"G226848E58484N","2008-05-01T00:00:00",1261087.860700688092038,1.261090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226848E58484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.152389727152467,58.483426500000000]
["glac_bound",381062.000000000000000,"G229221E56788N","2008-05-01T00:00:00",534890.282036264776252,0.534890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229221E56788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.777183831539730,56.793493499999997]
["glac_bound",381067.000000000000000,"G225268E59556N","2008-05-01T00:00:00",130845.672587373628630,0.130846000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225268E59556N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.733101480201498,59.556361499999994]
["glac_bound",381068.000000000000000,"G227634E57454N","2008-05-01T00:00:00",376221.937553666299209,0.376222000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227634E57454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.368870204718519,57.457946499999998]
["glac_bound",381071.000000000000000,"G227052E58011N","2008-05-01T00:00:00",228390.846392507781275,0.228391000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227052E58011N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.949329692868048,58.011377999999993]
["glac_bound",381077.000000000000000,"G229610E56443N","2008-05-01T00:00:00",779572.308651722618379,0.779572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229610E56443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.390156059316382,56.442916499999995]
["glac_bound",381080.000000000000000,"G231409E56209N","2008-05-01T00:00:00",105922.331342565797968,0.105922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231409E56209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.590343342991900,56.209497999999996]
["glac_bound",381082.000000000000000,"G228783E57267N","2008-05-01T00:00:00",63633.433928198828653,0.063633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228783E57267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.216548876343325,57.267056499999995]
["glac_bound",381083.000000000000000,"G227144E58228N","2008-05-01T00:00:00",132436.086351581208874,0.132436000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227144E58228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.855273695649913,58.228659499999999]
["glac_bound",381084.000000000000000,"G230572E55266N","2008-05-01T00:00:00",17423644.355905264616013,17.423600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230572E55266N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.421596668270809,55.257934000000006]
["glac_bound",381085.000000000000000,"G224360E59774N","2008-05-01T00:00:00",37213770.646365180611610,37.213799999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224360E59774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.708812337597578,59.795681500000001]
["glac_bound",381089.000000000000000,"G224680E59790N","2008-05-01T00:00:00",229645.860704285383690,0.229646000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224680E59790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.319643316235130,59.788888000000000]
["glac_bound",381090.000000000000000,"G222144E59817N","2008-05-01T00:00:00",2327563.455072003416717,2.327560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222144E59817N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.839628301611384,59.811340000000001]
["glac_bound",381091.000000000000000,"G227264E58072N","2008-05-01T00:00:00",1652460.889356031082571,1.652460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227264E58072N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.738598168886227,58.069834499999999]
["glac_bound",381092.000000000000000,"G230583E54735N","2008-05-01T00:00:00",311526.887367177987471,0.311527000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230583E54735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.416110310914547,54.736510500000001]
["glac_bound",381107.000000000000000,"G230082E55788N","2008-05-01T00:00:00",205431.888415259221802,0.205432000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230082E55788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.918119676407372,55.787544999999994]
["glac_bound",381113.000000000000000,"G229086E56758N","2008-05-01T00:00:00",724337.873408888583072,0.724338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229086E56758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.912886167135269,56.758452500000004]
["glac_bound",381116.000000000000000,"G224004E59714N","2008-05-01T00:00:00",4567140.638452114537358,4.567140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224004E59714N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.987276741089545,59.710495000000002]
["glac_bound",381117.000000000000000,"G228861E57363N","2008-05-01T00:00:00",7709771.210444859229028,7.709770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228861E57363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.142615295008738,57.360418500000002]
["glac_bound",381118.000000000000000,"G230678E57073N","2008-05-01T00:00:00",2526185.048982239328325,2.526190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230678E57073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.320572701494200,57.073731499999994]
["glac_bound",381121.000000000000000,"G230280E56916N","2008-05-01T00:00:00",723192.811757910065353,0.723193000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230280E56916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.721074186539909,56.915779000000001]
["glac_bound",381123.000000000000000,"G229859E56208N","2008-05-01T00:00:00",33647872.016604386270046,33.647900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229859E56208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.178784698449590,56.234440500000005]
["glac_bound",381127.000000000000000,"G227887E56867N","2008-05-01T00:00:00",836855.419525500619784,0.836855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227887E56867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.111603582815178,56.866759500000001]
["glac_bound",381132.000000000000000,"G226669E58532N","2008-05-01T00:00:00",387920.334498689218890,0.387920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226669E58532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.328104377207069,58.535246500000000]
["glac_bound",381136.000000000000000,"G228490E57198N","2008-05-01T00:00:00",267630.697281306143850,0.267631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228490E57198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.510285842108487,57.197791000000002]
["glac_bound",381143.000000000000000,"G230399E55179N","2008-05-01T00:00:00",243352.582114858378191,0.243353000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230399E55179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.600743960826946,55.178983000000002]
["glac_bound",381146.000000000000000,"G228401E56619N","2008-05-01T00:00:00",169689.705350191885373,0.169690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228401E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.598522203509503,56.619883999999999]
["glac_bound",381157.000000000000000,"G226197E58957N","2008-05-01T00:00:00",924690.245590073755011,0.924690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226197E58957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.795892170385855,58.964027999999999]
["glac_bound",381159.000000000000000,"G223704E59575N","2008-05-01T00:00:00",864760.872410783078521,0.864761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223704E59575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.295601812374684,59.573355000000006]
["glac_bound",381161.000000000000000,"G227666E57598N","2008-05-01T00:00:00",87752.940081698063295,0.087753000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227666E57598N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.333963658934294,57.598555000000005]
["glac_bound",381167.000000000000000,"G230239E55750N","2008-05-01T00:00:00",942204.367797701735981,0.942204000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230239E55750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.762285917075900,55.751025499999997]
["glac_bound",381170.000000000000000,"G227224E58339N","2008-05-01T00:00:00",2178057.933221324346960,2.178060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227224E58339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.776052906858695,58.339619499999998]
["glac_bound",381177.000000000000000,"G228005E57421N","2008-05-01T00:00:00",1253840.358368349261582,1.253840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228005E57421N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.998117270162084,57.430175000000006]
["glac_bound",381179.000000000000000,"G228022E57354N","2008-05-01T00:00:00",104178.693907189634047,0.104179000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228022E57354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.978300843434340,57.354438999999999]
["glac_bound",381180.000000000000000,"G228828E57381N","2008-05-01T00:00:00",7208562.308804947882891,7.208560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228828E57381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.176458640765077,57.385615999999999]
["glac_bound",381185.000000000000000,"G230322E56329N","2008-05-01T00:00:00",226812.911798427987378,0.226813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230322E56329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.678156749270499,56.328937499999995]
["glac_bound",381188.000000000000000,"G229649E56596N","2008-05-01T00:00:00",193009.628419371700147,0.193010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229649E56596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.352408430557603,56.595511999999999]
["glac_bound",381189.000000000000000,"G223474E59420N","2008-05-01T00:00:00",56248.992705300712259,0.056249000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223474E59420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.526082178595772,59.420332500000001]
["glac_bound",381190.000000000000000,"G227824E57500N","2008-05-01T00:00:00",7170105.779381817206740,7.170110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227824E57500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.168697183627671,57.500647999999998]
["glac_bound",381193.000000000000000,"G228442E56766N","2008-05-01T00:00:00",1158265.196633298881352,1.158270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228442E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.556264300734767,56.765236500000000]
["glac_bound",381195.000000000000000,"G227954E56838N","2008-05-01T00:00:00",37908.764715250443260,0.037909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227954E56838N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.045290027629392,56.837922499999998]
["glac_bound",381198.000000000000000,"G222383E59296N","2008-05-01T00:00:00",1068678.223982039839029,1.068680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222383E59296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.616852975595805,59.295615499999997]
["glac_bound",381204.000000000000000,"G227582E58210N","2008-05-01T00:00:00",372264.072870525647886,0.372264000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227582E58210N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.416785650332372,58.209962500000003]
["glac_bound",381207.000000000000000,"G229142E56408N","2008-05-01T00:00:00",206925.974730878544506,0.206926000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229142E56408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.857516632278475,56.410915500000002]
["glac_bound",381208.000000000000000,"G222655E59673N","2008-05-01T00:00:00",246279.395544143830193,0.246279000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222655E59673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.341249250662401,59.674793000000001]
["glac_bound",381213.000000000000000,"G228137E57155N","2008-05-01T00:00:00",387212.851253702305257,0.387213000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228137E57155N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.861816018552872,57.155949000000000]
["glac_bound",381215.000000000000000,"G222150E59694N","2008-05-01T00:00:00",535055.731388414744288,0.535056000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222150E59694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.849174539990486,59.693959999999997]
["glac_bound",381221.000000000000000,"G231145E56280N","2008-05-01T00:00:00",111827.357180082763080,0.111827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA231145E56280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.855861204015810,56.279892500000003]
["glac_bound",381229.000000000000000,"G222864E59328N","2008-05-01T00:00:00",2014321.197006579721346,2.014320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222864E59328N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.144594821323352,59.325789999999998]
["glac_bound",381231.000000000000000,"G223872E59647N","2008-05-01T00:00:00",75853.884424785501324,0.075854000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223872E59647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.126291544366211,59.647034500000004]
["glac_bound",381232.000000000000000,"G228255E57264N","2008-05-01T00:00:00",191979.187131724698702,0.191979000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228255E57264N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.744732967164168,57.264159499999998]
["glac_bound",381233.000000000000000,"G229986E56731N","2008-05-01T00:00:00",692553.820610036375001,0.692554000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229986E56731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.013630573071396,56.732563999999996]
["glac_bound",381235.000000000000000,"G230183E56076N","2008-05-01T00:00:00",229686.814367947983555,0.229687000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230183E56076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.818453221910090,56.077738999999994]
["glac_bound",381238.000000000000000,"G224303E59999N","2008-05-01T00:00:00",133633.739366101770429,0.133634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224303E59999N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.695373338983046,59.998997500000002]
["glac_bound",381239.000000000000000,"G226980E58134N","2008-05-01T00:00:00",193761.517392971116351,0.193762000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226980E58134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.019345375074693,58.133361999999998]
["glac_bound",381240.000000000000000,"G230418E56378N","2008-05-01T00:00:00",353136.339546196744777,0.353136000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230418E56378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.579833996924719,56.377070500000002]
["glac_bound",381242.000000000000000,"G225480E59566N","2008-05-01T00:00:00",147861.033298446564004,0.147861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225480E59566N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.519438112206842,59.566226000000000]
["glac_bound",381243.000000000000000,"G229304E56468N","2008-05-01T00:00:00",114169.669533553053043,0.114170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229304E56468N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.697672342136002,56.469640499999997]
["glac_bound",381248.000000000000000,"G226241E58668N","2008-05-01T00:00:00",51722.962698087925673,0.051723000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226241E58668N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.758451203931202,58.667870499999999]
["glac_bound",381249.000000000000000,"G226986E58391N","2008-05-01T00:00:00",1796554.739494610810652,1.796550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226986E58391N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.011997628199140,58.390933500000003]
["glac_bound",381251.000000000000000,"G230443E57108N","2008-05-01T00:00:00",52079.566994887041801,0.052080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230443E57108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.555367482718594,57.108794000000003]
["glac_bound",381253.000000000000000,"G226904E58107N","2008-05-01T00:00:00",179492.837609791022260,0.179493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226904E58107N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.095600676173007,58.106304000000002]
["glac_bound",381258.000000000000000,"G229723E57741N","2008-05-01T00:00:00",119961.906702880907687,0.119962000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229723E57741N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.277089529717614,57.741093500000005]
["glac_bound",381264.000000000000000,"G222353E59569N","2008-05-01T00:00:00",667642.365252152783796,0.667642000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222353E59569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.645776720810716,59.569031499999994]
["glac_bound",381276.000000000000000,"G225821E59192N","2008-05-01T00:00:00",1010258.936346929054707,1.010260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225821E59192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.178450748048419,59.191565499999996]
["glac_bound",381279.000000000000000,"G227216E58222N","2008-05-01T00:00:00",2122028.234983854461461,2.122030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227216E58222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.781394859179414,58.225080500000004]
["glac_bound",381282.000000000000000,"G230103E57436N","2008-05-01T00:00:00",62789.903637347975746,0.062790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230103E57436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.897065710848096,57.435885499999998]
["glac_bound",381284.000000000000000,"G228473E57589N","2008-05-01T00:00:00",156454.979683646204649,0.156455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228473E57589N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.526331331558822,57.589184500000002]
["glac_bound",381285.000000000000000,"G225060E59844N","2008-05-01T00:00:00",221683.088446830573957,0.221683000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225060E59844N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.940677851063811,59.844655000000003]
["glac_bound",381287.000000000000000,"G224049E59679N","2008-05-01T00:00:00",52887.222368627015385,0.052887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224049E59679N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.950813980169983,59.678891000000000]
["glac_bound",381288.000000000000000,"G227404E58095N","2008-05-01T00:00:00",131679.867095328401774,0.131680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227404E58095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.595300171755753,58.095115000000000]
["glac_bound",381299.000000000000000,"G230165E57443N","2008-05-01T00:00:00",179642.467609687475488,0.179642000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230165E57443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.836030408698178,57.442708499999995]
["glac_bound",381300.000000000000000,"G227981E57277N","2008-05-01T00:00:00",140292.564099520444870,0.140293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227981E57277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.019188569568712,57.279746000000003]
["glac_bound",381301.000000000000000,"G230698E56828N","2008-05-01T00:00:00",1619786.157212456455454,1.619790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230698E56828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.301728231798904,56.828657499999998]
["glac_bound",381302.000000000000000,"G222303E59934N","2008-05-01T00:00:00",154872.852260670129908,0.154873000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222303E59934N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.695356365394559,59.934499500000001]
["glac_bound",381309.000000000000000,"G224858E59816N","2008-05-01T00:00:00",413093.085999735922087,0.413093000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224858E59816N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.141508889152988,59.815476500000003]
["glac_bound",381312.000000000000000,"G230666E54927N","2008-05-01T00:00:00",1368278.400510677136481,1.368280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230666E54927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.328335129227867,54.931218000000001]
["glac_bound",381313.000000000000000,"G229509E57013N","2008-05-01T00:00:00",1207110.894899877021089,1.207110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229509E57013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.494343163388464,57.012918499999998]
["glac_bound",381314.000000000000000,"G230536E56793N","2008-05-01T00:00:00",101390.207073897428927,0.101390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230536E56793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464581303856562,56.792835500000002]
["glac_bound",381319.000000000000000,"G222898E59217N","2008-05-01T00:00:00",3446007.658150983043015,3.446010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222898E59217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.105709480691530,59.223732499999997]
["glac_bound",381324.000000000000000,"G229451E56350N","2008-05-01T00:00:00",245071.007401383481920,0.245071000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229451E56350N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.546648718749992,56.350129500000001]
["glac_bound",381330.000000000000000,"G230023E55781N","2008-05-01T00:00:00",78508.812910720458603,0.078509000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230023E55781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.977253418526800,55.780453500000000]
["glac_bound",381331.000000000000000,"G228029E57287N","2008-05-01T00:00:00",626190.403232139069587,0.626190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228029E57287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.976816850771087,57.287942500000000]
["glac_bound",381333.000000000000000,"G230144E57349N","2008-05-01T00:00:00",111894.507921179043478,0.111895000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230144E57349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.857431605108019,57.349509999999995]
["glac_bound",381334.000000000000000,"G222048E59540N","2008-05-01T00:00:00",76487.238163143294514,0.076487000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222048E59540N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.952012392543111,59.539795499999997]
["glac_bound",381336.000000000000000,"G229554E56736N","2008-05-01T00:00:00",57904.354970118147321,0.057904000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229554E56736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.445846177950472,56.736245499999995]
["glac_bound",381341.000000000000000,"G230234E57305N","2008-05-01T00:00:00",80204.670598445038195,0.080205000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230234E57305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.766293668024446,57.305058000000002]
["glac_bound",381342.000000000000000,"G229493E57023N","2008-05-01T00:00:00",175668.352912012866000,0.175668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229493E57023N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.507248769476320,57.022657500000001]
["glac_bound",381346.000000000000000,"G229871E56302N","2008-05-01T00:00:00",711585.954457968589850,0.711586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229871E56302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.125204696459491,56.304002999999994]
["glac_bound",381358.000000000000000,"G229034E57316N","2008-05-01T00:00:00",116693.734702092115185,0.116694000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229034E57316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.966703913330605,57.316866500000003]
["glac_bound",381364.000000000000000,"G227120E58486N","2008-05-01T00:00:00",3453749.925042410381138,3.453750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227120E58486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.889588114145653,58.493080000000006]
["glac_bound",381365.000000000000000,"G225242E59366N","2008-05-01T00:00:00",24655592.703807353973389,24.655600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225242E59366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.737110125981189,59.372357500000000]
["glac_bound",381369.000000000000000,"G223678E59572N","2008-05-01T00:00:00",935728.971864841179922,0.935729000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223678E59572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.317677218632952,59.576655500000001]
["glac_bound",381373.000000000000000,"G225951E59189N","2008-05-01T00:00:00",201120.237537802982843,0.201120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225951E59189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.049053425268113,59.189224500000002]
["glac_bound",381375.000000000000000,"G223248E59558N","2008-05-01T00:00:00",294630.673867121688090,0.294631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223248E59558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.752057311184217,59.558045500000006]
["glac_bound",381379.000000000000000,"G229081E56463N","2008-05-01T00:00:00",7049571.353762202896178,7.049570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229081E56463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.932162908478176,56.474283499999999]
["glac_bound",381380.000000000000000,"G224741E59817N","2008-05-01T00:00:00",265403.620500162942335,0.265404000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224741E59817N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.258243533485825,59.817720500000000]
["glac_bound",381382.000000000000000,"G230033E56558N","2008-05-01T00:00:00",105790.695783597606351,0.105791000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230033E56558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.966686164266946,56.557803000000000]
["glac_bound",381384.000000000000000,"G227348E58155N","2008-05-01T00:00:00",213780.788858191081090,0.213781000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227348E58155N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.650955799504970,58.155493000000000]
["glac_bound",381385.000000000000000,"G228091E58037N","2008-05-01T00:00:00",401104.392493817606010,0.401104000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228091E58037N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.910815226040370,58.038247499999997]
["glac_bound",381390.000000000000000,"G229852E57789N","2008-05-01T00:00:00",96008.327048837163602,0.096008000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229852E57789N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.149070064978332,57.789025499999994]
["glac_bound",381391.000000000000000,"G222103E59519N","2008-05-01T00:00:00",104243.227029950416181,0.104243000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222103E59519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.895768309433947,59.520969500000000]
["glac_bound",381392.000000000000000,"G229499E57019N","2008-05-01T00:00:00",55644.609624019889452,0.055645000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229499E57019N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.502772136842964,57.018723999999999]
["glac_bound",381396.000000000000000,"G228003E56839N","2008-05-01T00:00:00",180488.158436532190535,0.180488000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228003E56839N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.996632574363900,56.838879499999997]
["glac_bound",381399.000000000000000,"G228810E56520N","2008-05-01T00:00:00",72821.442845543933799,0.072821000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228810E56520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.191328857052156,56.519339500000001]
["glac_bound",381403.000000000000000,"G230449E55238N","2008-05-01T00:00:00",78031.005064165117801,0.078031000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230449E55238N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.551884343137260,55.238459500000005]
["glac_bound",381404.000000000000000,"G230306E56317N","2008-05-01T00:00:00",1699613.921408455120400,1.699610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230306E56317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.698528184357542,56.324742000000001]
["glac_bound",381407.000000000000000,"G229371E56947N","2008-05-01T00:00:00",374823.439133229025174,0.374823000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229371E56947N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.628227495882868,56.947081999999995]
["glac_bound",381409.000000000000000,"G229383E57379N","2008-05-01T00:00:00",202011.969126510957722,0.202012000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229383E57379N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.616805741814460,57.379330500000002]
["glac_bound",381411.000000000000000,"G227004E58380N","2008-05-01T00:00:00",827454.489145661005750,0.827455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227004E58380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.994611321500685,58.379087499999997]
["glac_bound",381421.000000000000000,"G226084E58793N","2008-05-01T00:00:00",3478780.378463732544333,3.478780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226084E58793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.920601899246236,58.789283499999996]
["glac_bound",381426.000000000000000,"G229213E57231N","2008-05-01T00:00:00",187912.213478286954341,0.187912000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229213E57231N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.787123814514388,57.230497499999998]
["glac_bound",381427.000000000000000,"G229250E56520N","2008-05-01T00:00:00",186826.094193238473963,0.186826000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229250E56520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.750194251059440,56.520171500000004]
["glac_bound",381434.000000000000000,"G229210E56448N","2008-05-01T00:00:00",8016330.441098221577704,8.016330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229210E56448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.816595569047621,56.454797999999997]
["glac_bound",381439.000000000000000,"G225457E59074N","2008-05-01T00:00:00",65675.655455726679065,0.065676000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Field Glacier","None","08BD225416E59115N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.584325063820216,59.114353500000000]
["glac_bound",381441.000000000000000,"G230654E55218N","2008-05-01T00:00:00",1550602.643710188800469,1.550600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230654E55218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.331699342500542,55.225004499999997]
["glac_bound",381442.000000000000000,"G230521E54836N","2008-05-01T00:00:00",270416.103337504551746,0.270416000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230521E54836N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.477486114653004,54.840041999999997]
["glac_bound",381453.000000000000000,"G227131E58445N","2008-05-01T00:00:00",1271989.152385915629566,1.271990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227131E58445N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.871590370607549,58.447063999999997]
["glac_bound",381460.000000000000000,"G225507E59345N","2008-05-01T00:00:00",1884910.626885754987597,1.884910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225507E59345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.495925995865207,59.341934000000002]
["glac_bound",381462.000000000000000,"G224694E59794N","2008-05-01T00:00:00",185495.497340410365723,0.185495000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224694E59794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.305751823014532,59.794077999999999]
["glac_bound",381465.000000000000000,"G224278E59829N","2008-05-01T00:00:00",2989486.916265315841883,2.989490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224278E59829N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.728760776225045,59.834711999999996]
["glac_bound",381468.000000000000000,"G226896E58227N","2008-05-01T00:00:00",149337.093644345062785,0.149337000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226896E58227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.104461060986637,58.226338999999996]
["glac_bound",381476.000000000000000,"G225562E59231N","2008-05-01T00:00:00",87909.139662379951915,0.087909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225562E59231N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.437998016372347,59.231061499999996]
["glac_bound",381478.000000000000000,"G224697E59777N","2008-05-01T00:00:00",2200310.078882975969464,2.200310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224697E59777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.305892705685608,59.777179000000004]
["glac_bound",381481.000000000000000,"G230467E56026N","2008-05-01T00:00:00",1763309.547811044612899,1.763310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230467E56026N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.538766709190185,56.027071000000007]
["glac_bound",381483.000000000000000,"G230066E55756N","2008-05-01T00:00:00",931899.115773307974450,0.931899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230066E55756N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.929332240510462,55.758562999999995]
["glac_bound",381484.000000000000000,"G229228E56507N","2008-05-01T00:00:00",516562.939749208919238,0.516563000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229228E56507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.770804919747690,56.507673499999996]
["glac_bound",381491.000000000000000,"G224997E59329N","2008-05-01T00:00:00",231325.970741227210965,0.231326000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224997E59329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.006006145922129,59.329180000000001]
["glac_bound",381492.000000000000000,"G224038E59692N","2008-05-01T00:00:00",973769.080617720610462,0.973769000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224038E59692N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.961197438973898,59.690933500000000]
["glac_bound",381497.000000000000000,"G223150E59553N","2008-05-01T00:00:00",706297.966586529393680,0.706298000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223150E59553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.853273837672987,59.557523000000003]
["glac_bound",381510.000000000000000,"G229534E56324N","2008-05-01T00:00:00",1364394.913226657081395,1.364390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229534E56324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.463074593821403,56.322789000000000]
["glac_bound",381512.000000000000000,"G230116E55648N","2008-05-01T00:00:00",381407.431795931945089,0.381407000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230116E55648N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.884635597872546,55.650714499999999]
["glac_bound",381520.000000000000000,"G225264E59473N","2008-05-01T00:00:00",72258.570294558056048,0.072259000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225264E59473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.736172843533353,59.474574500000003]
["glac_bound",381521.000000000000000,"G229247E56508N","2008-05-01T00:00:00",987619.539573723799549,0.987620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229247E56508N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.754168771241837,56.507024000000001]
["glac_bound",381522.000000000000000,"G229215E57157N","2008-05-01T00:00:00",76304.208871192793595,0.076304000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229215E57157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.782913726757897,57.155977000000000]
["glac_bound",381523.000000000000000,"G228803E57093N","2008-05-01T00:00:00",12875711.903176873922348,12.875700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228803E57093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.207224543059510,57.087832500000005]
["glac_bound",381531.000000000000000,"G228025E57464N","2008-05-01T00:00:00",2289844.329694460611790,2.289840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228025E57464N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.972577253643976,57.461731000000000]
["glac_bound",381532.000000000000000,"G223993E59786N","2008-05-01T00:00:00",57439.487926760542905,0.057439000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223993E59786N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.007542094243831,59.786451499999998]
["glac_bound",381533.000000000000000,"G225990E58840N","2008-05-01T00:00:00",246375.721322295779828,0.246376000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB225990E58840N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.011936912507991,58.840767000000000]
["glac_bound",381543.000000000000000,"G229259E57041N","2008-05-01T00:00:00",585993.780076541355811,0.585994000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229259E57041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.735598003227977,57.046155999999996]
["glac_bound",381549.000000000000000,"G228894E57535N","2008-05-01T00:00:00",1327553.731774045852944,1.327550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228894E57535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.102955330241741,57.535135999999994]
["glac_bound",381551.000000000000000,"G228973E57055N","2008-05-01T00:00:00",505662.741339419502765,0.505663000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228973E57055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.024645704772468,57.054399000000004]
["glac_bound",381556.000000000000000,"G229369E57268N","2008-05-01T00:00:00",718278.742355373571627,0.718279000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229369E57268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.631437624009948,57.269831999999994]
["glac_bound",381558.000000000000000,"G227425E58400N","2008-05-01T00:00:00",85186.694391890894622,0.085187000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227425E58400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.574702077338145,58.399745000000003]
["glac_bound",381566.000000000000000,"G222030E59534N","2008-05-01T00:00:00",2262545.102018677629530,2.262550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222030E59534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.967113797290551,59.541721500000001]
["glac_bound",381569.000000000000000,"G231565E57268N","2008-05-01T00:00:00",123630.829913190784282,0.123631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231565E57268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.434033109638563,57.269925000000001]
["glac_bound",381570.000000000000000,"G227477E58241N","2008-05-01T00:00:00",117948.410419363732217,0.117948000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227477E58241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.521411559362548,58.240923500000001]
["glac_bound",381571.000000000000000,"G223222E59316N","2008-05-01T00:00:00",2257189.659832566976547,2.257190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223222E59316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.772208631842716,59.329605000000001]
["glac_bound",381572.000000000000000,"G229455E56253N","2008-05-01T00:00:00",728702.189177630585618,0.728702000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229455E56253N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.547264192930754,56.254857999999999]
["glac_bound",381576.000000000000000,"G229953E57340N","2008-05-01T00:00:00",422811.089702674420550,0.422811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229953E57340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.045996613727084,57.338801000000004]
["glac_bound",381581.000000000000000,"G230089E55704N","2008-05-01T00:00:00",108821.981684907266754,0.108822000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230089E55704N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.912043783030470,55.703575499999999]
["glac_bound",381582.000000000000000,"G229993E57116N","2008-05-01T00:00:00",50697.298754790564999,0.050697000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229993E57116N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.006810677082115,57.116349999999997]
["glac_bound",381584.000000000000000,"G222162E59681N","2008-05-01T00:00:00",121427.906490513982135,0.121428000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222162E59681N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.839456133137020,59.680127999999996]
["glac_bound",381585.000000000000000,"G228879E56538N","2008-05-01T00:00:00",835745.547668801387772,0.835746000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228879E56538N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.122353415057916,56.538729000000004]
["glac_bound",381586.000000000000000,"G230555E55189N","2008-05-01T00:00:00",1307283.040844917763025,1.307280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230555E55189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.443783414819308,55.193578500000001]
["glac_bound",381589.000000000000000,"G225710E59383N","2008-05-01T00:00:00",946710.260723285027780,0.946710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225710E59383N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.287462419090900,59.383061999999995]
["glac_bound",381592.000000000000000,"G228006E58017N","2008-05-01T00:00:00",359602.892883761436678,0.359603000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228006E58017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.991732904584609,58.016568499999998]
["glac_bound",381599.000000000000000,"G230360E56086N","2008-05-01T00:00:00",622098.792916541686282,0.622099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230360E56086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.636047350246770,56.087620000000001]
["glac_bound",381600.000000000000000,"G230612E56879N","2008-05-01T00:00:00",145771.100785403046757,0.145771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230612E56879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.387350003287736,56.878942500000001]
["glac_bound",381602.000000000000000,"G227883E57943N","2008-05-01T00:00:00",1110384.749045376898721,1.110380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227883E57943N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.117168399596778,57.945517500000001]
["glac_bound",381603.000000000000000,"G231289E57523N","2008-05-01T00:00:00",283382.172250050352886,0.283382000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231289E57523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.712269535476707,57.522867000000005]
["glac_bound",381606.000000000000000,"G226421E58947N","2008-05-01T00:00:00",198662.413644359272439,0.198662000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226421E58947N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.580415861198844,58.946719500000000]
["glac_bound",381608.000000000000000,"G222900E59452N","2008-05-01T00:00:00",218275.437668942613527,0.218275000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222900E59452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.101580771966525,59.453431999999999]
["glac_bound",381614.000000000000000,"G229679E56225N","2008-05-01T00:00:00",22148178.687670245766640,22.148199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229679E56225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.277695660434404,56.231072499999996]
["glac_bound",381625.000000000000000,"G229283E56467N","2008-05-01T00:00:00",767390.293124132556841,0.767390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229283E56467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.715492423431130,56.466555499999998]
["glac_bound",381627.000000000000000,"G229368E57196N","2008-05-01T00:00:00",3194523.789287351071835,3.194520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229368E57196N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.620705330060787,57.203186000000002]
["glac_bound",381629.000000000000000,"G228056E57218N","2008-05-01T00:00:00",906098.949822731781751,0.906099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228056E57218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.947980922509032,57.216507000000000]
["glac_bound",381635.000000000000000,"G225749E59098N","2008-05-01T00:00:00",160218.564864010579186,0.160219000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225749E59098N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.251247009201592,59.097867000000001]
["glac_bound",381641.000000000000000,"G226864E58538N","2008-05-01T00:00:00",908388.287404533242807,0.908388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226864E58538N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.140516822625699,58.537315000000000]
["glac_bound",381644.000000000000000,"G222390E59286N","2008-05-01T00:00:00",888426.400917412946001,0.888426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222390E59286N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.606101318233868,59.287956500000000]
["glac_bound",381646.000000000000000,"G227604E57553N","2008-05-01T00:00:00",1231188.918484288500622,1.231190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227604E57553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.396441901143447,57.557178000000000]
["glac_bound",381655.000000000000000,"G228476E57304N","2008-05-01T00:00:00",1022259.143585137324408,1.022260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228476E57304N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.516133566946678,57.305697500000001]
["glac_bound",381657.000000000000000,"G226831E58535N","2008-05-01T00:00:00",1314694.757523498032242,1.314690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226831E58535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.170200618668133,58.541281499999997]
["glac_bound",381666.000000000000000,"G230501E56016N","2008-05-01T00:00:00",788206.051447302917950,0.788206000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230501E56016N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.498899121416997,56.016981500000000]
["glac_bound",381672.000000000000000,"G229049E56587N","2008-05-01T00:00:00",1049489.760470593115315,1.049490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229049E56587N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.955561473903174,56.585110000000000]
["glac_bound",381674.000000000000000,"G230692E57083N","2008-05-01T00:00:00",184074.753142834670143,0.184075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230692E57083N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.303968649315493,57.084307000000003]
["glac_bound",381676.000000000000000,"G230227E56941N","2008-05-01T00:00:00",171921.240161630470539,0.171921000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230227E56941N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.773188334005908,56.939814499999997]
["glac_bound",381678.000000000000000,"G224388E59866N","2008-05-01T00:00:00",86482.641897226494621,0.086483000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224388E59866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.612316209969777,59.865289500000003]
["glac_bound",381682.000000000000000,"G227929E57628N","2008-05-01T00:00:00",358854.491288186341990,0.358855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227929E57628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.068893580444183,57.629283500000000]
["glac_bound",381685.000000000000000,"G227103E58150N","2008-05-01T00:00:00",323480.426840898988303,0.323480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227103E58150N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.890097853025907,58.153688000000002]
["glac_bound",381689.000000000000000,"G227514E57804N","2008-05-01T00:00:00",224236.168573376635322,0.224236000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227514E57804N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.487016626576207,57.801247000000004]
["glac_bound",381690.000000000000000,"G222628E59211N","2008-05-01T00:00:00",1354169.335322814993560,1.354170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222628E59211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.382430508526625,59.215840499999999]
["glac_bound",381699.000000000000000,"G229380E56959N","2008-05-01T00:00:00",383389.126771157549229,0.383389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229380E56959N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.618194651849308,56.959166499999995]
["glac_bound",381702.000000000000000,"G226479E58943N","2008-05-01T00:00:00",212339.686369577480946,0.212340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226479E58943N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.521055598623661,58.942798500000002]
["glac_bound",381706.000000000000000,"G230076E56560N","2008-05-01T00:00:00",131466.367141381255351,0.131466000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230076E56560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.923779940565339,56.559759000000000]
["glac_bound",381709.000000000000000,"G228082E57416N","2008-05-01T00:00:00",107503.211795373543282,0.107503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228082E57416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.916968744402993,57.415734000000000]
["glac_bound",381710.000000000000000,"G225059E59384N","2008-05-01T00:00:00",288805.768523222242948,0.288806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225059E59384N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.941793587500001,59.384135999999998]
["glac_bound",381713.000000000000000,"G227388E58012N","2008-05-01T00:00:00",441283.423456170596182,0.441283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227388E58012N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.613517607856465,58.014448999999999]
["glac_bound",381714.000000000000000,"G230315E57425N","2008-05-01T00:00:00",434602.094963438692503,0.434602000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230315E57425N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.685409955966747,57.423466000000005]
["glac_bound",381715.000000000000000,"G225429E59442N","2008-05-01T00:00:00",494126.818217306514271,0.494127000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225429E59442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.570589326426898,59.441842000000001]
["glac_bound",381719.000000000000000,"G229404E56630N","2008-05-01T00:00:00",5711893.295758360065520,5.711890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229404E56630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.601612618465424,56.630155999999999]
["glac_bound",381727.000000000000000,"G227806E57567N","2008-05-01T00:00:00",791468.934254969703034,0.791469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227806E57567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.193027189651218,57.568928999999997]
["glac_bound",381734.000000000000000,"G230106E56903N","2008-05-01T00:00:00",226286.782989555766108,0.226287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230106E56903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.898725508526809,56.903164500000003]
["glac_bound",381739.000000000000000,"G222108E59828N","2008-05-01T00:00:00",990177.725892906892113,0.990178000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222108E59828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.898201935793679,59.829973499999994]
["glac_bound",381743.000000000000000,"G229912E57235N","2008-05-01T00:00:00",155882.262913633312564,0.155882000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229912E57235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.087350000000015,57.234633500000001]
["glac_bound",381747.000000000000000,"G229387E57477N","2008-05-01T00:00:00",148572.385320248140488,0.148572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229387E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.612623475190503,57.476774500000005]
["glac_bound",381750.000000000000000,"G223244E59745N","2008-05-01T00:00:00",707083.635993653326295,0.707084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223244E59745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.753303686232158,59.744132000000000]
["glac_bound",381757.000000000000000,"G228975E57101N","2008-05-01T00:00:00",62338.076328011738951,0.062338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228975E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.024899224487001,57.100270500000001]
["glac_bound",381759.000000000000000,"G230834E55104N","2008-05-01T00:00:00",345911.165477628179360,0.345911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230834E55104N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.165885933333328,55.103579499999995]
["glac_bound",381764.000000000000000,"G227744E57735N","2008-05-01T00:00:00",140724.209097144514089,0.140724000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227744E57735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.256103089643716,57.734892000000002]
["glac_bound",381766.000000000000000,"G228730E57273N","2008-05-01T00:00:00",167545.297717530746013,0.167545000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228730E57273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.269155524367903,57.273052999999997]
["glac_bound",381775.000000000000000,"G222070E59528N","2008-05-01T00:00:00",161534.654455407697242,0.161535000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222070E59528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.928274042364762,59.527900000000002]
["glac_bound",381778.000000000000000,"G222542E59803N","2008-05-01T00:00:00",755057.543956030393019,0.755058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222542E59803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.454256420883070,59.803637500000001]
["glac_bound",381783.000000000000000,"G227143E57995N","2008-05-01T00:00:00",492360.459847301710397,0.492360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227143E57995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.858395201781661,57.994630000000001]
["glac_bound",381785.000000000000000,"G228862E56503N","2008-05-01T00:00:00",1269553.862627641297877,1.269550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228862E56503N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.139362164804595,56.503120500000001]
["glac_bound",381786.000000000000000,"G227546E58149N","2008-05-01T00:00:00",2103968.225242713000625,2.103970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227546E58149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.451859789882462,58.148554000000004]
["glac_bound",381787.000000000000000,"G230212E56287N","2008-05-01T00:00:00",516412.304718574450817,0.516412000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230212E56287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.792133895953782,56.290316500000003]
["glac_bound",381789.000000000000000,"G226927E58614N","2008-05-01T00:00:00",2446740.363296558614820,2.446740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226927E58614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.075486926282053,58.615335999999999]
["glac_bound",381791.000000000000000,"G226586E58544N","2008-05-01T00:00:00",1337603.711136173922569,1.337600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226586E58544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.415808770341982,58.554099500000000]
["glac_bound",381795.000000000000000,"G227531E57812N","2008-05-01T00:00:00",2220895.043669472448528,2.145890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227531E57812N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.467977004101272,57.813449500000004]
["glac_bound",381798.000000000000000,"G226189E58874N","2008-05-01T00:00:00",1003513.086840575560927,1.003510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226189E58874N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.808952110968562,58.875472000000002]
["glac_bound",381802.000000000000000,"G227790E57810N","2008-05-01T00:00:00",3915380.847385579254478,3.915380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227790E57810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.214676291584169,57.806604000000000]
["glac_bound",381804.000000000000000,"G221777E59733N","2008-05-01T00:00:00",1020808.772717367392033,1.020810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221777E59733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.209428858782474,59.728988999999999]
["glac_bound",381805.000000000000000,"G230531E55897N","2008-05-01T00:00:00",3164455.929952716920525,3.164460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230531E55897N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.453243569479127,55.904307000000003]
["glac_bound",381809.000000000000000,"G227919E57230N","2008-05-01T00:00:00",53259.543228668837401,0.053260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227919E57230N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.078764373150108,57.231372000000000]
["glac_bound",381814.000000000000000,"G224553E59867N","2008-05-01T00:00:00",53611.099665920526604,0.053611000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224553E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.446906892857157,59.866947499999995]
["glac_bound",381816.000000000000000,"G228591E56566N","2008-05-01T00:00:00",207685.364611816446995,0.207685000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228591E56566N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.406665994006403,56.565463000000001]
["glac_bound",381820.000000000000000,"G222466E59847N","2008-05-01T00:00:00",9144355.550127614289522,9.144360000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222466E59847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.524977501983528,59.860846500000001]
["glac_bound",381834.000000000000000,"G227202E58036N","2008-05-01T00:00:00",291136.468056512356270,0.291136000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227202E58036N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.798106908310331,58.035853000000003]
["glac_bound",381839.000000000000000,"G226792E58448N","2008-05-01T00:00:00",26168239.390635572373867,26.168199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226792E58448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.281015555339593,58.429986499999998]
["glac_bound",381840.000000000000000,"G228719E57497N","2008-05-01T00:00:00",267532.469624117715284,0.267532000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228719E57497N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.281883804818989,57.497359000000003]
["glac_bound",381853.000000000000000,"G230581E55203N","2008-05-01T00:00:00",682704.902160302386619,0.682705000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230581E55203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.412311514748922,55.201519500000003]
["glac_bound",381854.000000000000000,"G230455E54702N","2008-05-01T00:00:00",830640.229280289146118,0.830640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230455E54702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.548150994811635,54.702680500000000]
["glac_bound",381862.000000000000000,"G229246E56619N","2008-05-01T00:00:00",643330.706655405694619,0.643331000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229246E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.758768652592607,56.618375000000000]
["glac_bound",381870.000000000000000,"G228836E57296N","2008-05-01T00:00:00",420689.911867689166684,0.420690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228836E57296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.166476828438732,57.295422500000001]
["glac_bound",381871.000000000000000,"G228980E56559N","2008-05-01T00:00:00",326660.766650445235427,0.326661000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228980E56559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.021605697270445,56.558948999999998]
["glac_bound",381882.000000000000000,"G229636E56181N","2008-05-01T00:00:00",2041273.028014150913805,2.041270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229636E56181N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.357148127941173,56.189588499999999]
["glac_bound",381891.000000000000000,"G229647E56165N","2008-05-01T00:00:00",1006266.288390533532947,1.006270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229647E56165N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.353527598130825,56.170023000000000]
["glac_bound",381892.000000000000000,"G227795E57398N","2008-05-01T00:00:00",118264.339399544536718,0.118264000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227795E57398N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.204653918860231,57.398233500000003]
["glac_bound",381893.000000000000000,"G230431E55988N","2008-05-01T00:00:00",605380.724171578069218,0.605381000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230431E55988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.568514093575402,55.986958999999999]
["glac_bound",381895.000000000000000,"G229982E56149N","2008-05-01T00:00:00",308862.593259708955884,0.308863000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229982E56149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.018872937887124,56.148414000000002]
["glac_bound",381900.000000000000000,"G229729E56546N","2008-05-01T00:00:00",362156.379766997997649,0.362156000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229729E56546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.273557098975033,56.548414999999999]
["glac_bound",381903.000000000000000,"G228296E57234N","2008-05-01T00:00:00",372902.690959045896307,0.372903000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228296E57234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.704048130469630,57.232940499999998]
["glac_bound",381904.000000000000000,"G223345E59903N","2008-05-01T00:00:00",125211.812027888125158,0.125212000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223345E59903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.652395467230548,59.904608000000003]
["glac_bound",381905.000000000000000,"G230675E55570N","2008-05-01T00:00:00",693308.468087460962124,0.693308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230675E55570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.326947330143582,55.568860000000001]
["glac_bound",381906.000000000000000,"G230639E56778N","2008-05-01T00:00:00",232739.357392047677422,0.232739000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230639E56778N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.360010964199063,56.777466500000003]
["glac_bound",381907.000000000000000,"G229461E56400N","2008-05-01T00:00:00",391069.322807246644516,0.391069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229461E56400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.536792347980025,56.401488999999998]
["glac_bound",381911.000000000000000,"G230517E56017N","2008-05-01T00:00:00",212770.651178742991760,0.212771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230517E56017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.486640875676585,56.017550499999999]
["glac_bound",381915.000000000000000,"G229392E57197N","2008-05-01T00:00:00",160102.851225190795958,0.160103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229392E57197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.608496945843086,57.197088000000001]
["glac_bound",381920.000000000000000,"G226843E58395N","2008-05-01T00:00:00",4057756.011764923110604,4.057760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226843E58395N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.157212919130018,58.393817499999997]
["glac_bound",381921.000000000000000,"G230528E54620N","2008-05-01T00:00:00",1443693.996569366427138,1.443690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230528E54620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.466153694369524,54.625357500000007]
["glac_bound",381925.000000000000000,"G227886E57907N","2008-05-01T00:00:00",3852131.598146726842970,3.852130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227886E57907N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.114450727262664,57.905647000000002]
["glac_bound",381927.000000000000000,"G228024E57484N","2008-05-01T00:00:00",527052.621082071214914,0.527053000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228024E57484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.975812265692412,57.484644500000002]
["glac_bound",381929.000000000000000,"G224963E59345N","2008-05-01T00:00:00",849716.194562202435918,0.849716000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224963E59345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.031490846529380,59.349823499999999]
["glac_bound",381931.000000000000000,"G225570E59131N","2008-05-01T00:00:00",80865202.521047383546829,80.865200000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Willison Glacier","None","09AA225570E59131N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.406053588985486,59.146660999999995]
["glac_bound",381936.000000000000000,"G229251E57160N","2008-05-01T00:00:00",1197640.848786097019911,1.197640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229251E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.752356891927491,57.160575500000000]
["glac_bound",381937.000000000000000,"G231057E56281N","2008-05-01T00:00:00",307105.687523909262381,0.307106000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA231057E56281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.941617061784143,56.280258000000003]
["glac_bound",381941.000000000000000,"G226885E58070N","2008-05-01T00:00:00",2976112.456078291404992,2.976110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226885E58070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.119625138607745,58.075190999999997]
["glac_bound",381944.000000000000000,"G228036E57071N","2008-05-01T00:00:00",1576949.725188131676987,1.576950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228036E57071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.970947425987902,57.080931500000005]
["glac_bound",381945.000000000000000,"G230450E56662N","2008-05-01T00:00:00",78087.130621861200780,0.078087000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230450E56662N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.550125212747218,56.661591000000001]
["glac_bound",381946.000000000000000,"G227668E57896N","2008-05-01T00:00:00",170272.290407552878605,0.170272000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227668E57896N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.331526562282363,57.895679000000001]
["glac_bound",381947.000000000000000,"G222654E59662N","2008-05-01T00:00:00",66067.640130420797504,0.066068000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222654E59662N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.346112643684876,59.662166499999998]
["glac_bound",381949.000000000000000,"G225997E58976N","2008-05-01T00:00:00",421029.197710433392785,0.421029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB225997E58976N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.004444966613676,58.975044999999994]
["glac_bound",381950.000000000000000,"G230686E55679N","2008-05-01T00:00:00",141223.934094972239109,0.141224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230686E55679N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.313969229584927,55.678862500000001]
["glac_bound",381958.000000000000000,"G230040E55802N","2008-05-01T00:00:00",195810.997069824981736,0.195811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230040E55802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.959407718530031,55.802119000000005]
["glac_bound",381962.000000000000000,"G222444E59010N","2008-05-01T00:00:00",167659.639040321024368,0.167660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222444E59010N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.557998295737860,59.010751999999997]
["glac_bound",381970.000000000000000,"G229995E55584N","2008-05-01T00:00:00",73134.610365535147139,0.073135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC229995E55584N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.004040161373155,55.584434999999999]
["glac_bound",381973.000000000000000,"G228874E57490N","2008-05-01T00:00:00",146408.266897621360840,0.146408000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228874E57490N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.124796308122200,57.490486000000004]
["glac_bound",381978.000000000000000,"G226639E58658N","2008-05-01T00:00:00",1998038.973791853059083,1.998040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226639E58658N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.360114484295821,58.662030999999999]
["glac_bound",381979.000000000000000,"G230413E56720N","2008-05-01T00:00:00",166816.222836221597390,0.166816000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230413E56720N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.585093925598528,56.720469999999999]
["glac_bound",381988.000000000000000,"G224664E59779N","2008-05-01T00:00:00",159877.998250673874281,0.159878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224664E59779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.336153251431028,59.779160500000003]
["glac_bound",381989.000000000000000,"G230538E56769N","2008-05-01T00:00:00",595946.055543190450408,0.595946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230538E56769N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.461541226290535,56.767487000000003]
["glac_bound",381995.000000000000000,"G224467E59782N","2008-05-01T00:00:00",4009116.577949385158718,4.009120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224467E59782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.530041471130573,59.783049500000004]
["glac_bound",382000.000000000000000,"G225484E59477N","2008-05-01T00:00:00",206220.725133764906786,0.206221000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225484E59477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.518571866259435,59.478760999999999]
["glac_bound",382004.000000000000000,"G229018E57192N","2008-05-01T00:00:00",197490.215507662971504,0.197490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229018E57192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.981396185769654,57.191642000000002]
["glac_bound",382006.000000000000000,"G224793E59687N","2008-05-01T00:00:00",652840.968449139734730,0.652841000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224793E59687N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.205875315273033,59.685628999999999]
["glac_bound",382009.000000000000000,"G228812E56547N","2008-05-01T00:00:00",80297.182986463361885,0.080297000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228812E56547N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.189063048089082,56.546245999999996]
["glac_bound",382010.000000000000000,"G230497E55958N","2008-05-01T00:00:00",88112.123787318996619,0.088112000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230497E55958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.502488828163791,55.958700000000000]
["glac_bound",382015.000000000000000,"G223878E59910N","2008-05-01T00:00:00",759645.623197388136759,0.759646000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223878E59910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.118655483377665,59.909702500000002]
["glac_bound",382019.000000000000000,"G229716E56716N","2008-05-01T00:00:00",61404.276571209935355,0.061404000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229716E56716N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.284460374514993,56.715738999999999]
["glac_bound",382035.000000000000000,"G230006E56339N","2008-05-01T00:00:00",3370268.815437209326774,3.370270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230006E56339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.003845118731959,56.352923000000004]
["glac_bound",382041.000000000000000,"G227666E57873N","2008-05-01T00:00:00",2105078.833552276715636,2.105080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227666E57873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.335002500648216,57.876766500000002]
["glac_bound",382042.000000000000000,"G222819E59385N","2008-05-01T00:00:00",25483520.951655767858028,25.483499999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222819E59385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.192923160227622,59.387854000000004]
["glac_bound",382048.000000000000000,"G228944E57299N","2008-05-01T00:00:00",1404584.792298411251977,1.404580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228944E57299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.062420032725754,57.298206999999998]
["glac_bound",382053.000000000000000,"G230244E57110N","2008-05-01T00:00:00",482372.303723892080598,0.482372000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230244E57110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.755394521758575,57.110343000000000]
["glac_bound",382055.000000000000000,"G222340E59280N","2008-05-01T00:00:00",433190.869961835094728,0.433191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222340E59280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.661239098712457,59.279414500000001]
["glac_bound",382061.000000000000000,"G228896E57225N","2008-05-01T00:00:00",474416.532948098087218,0.474417000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228896E57225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.103796357836217,57.224820000000001]
["glac_bound",382062.000000000000000,"G223166E59528N","2008-05-01T00:00:00",754258.513831992982887,0.754259000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223166E59528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.831656254838720,59.526348999999996]
["glac_bound",382063.000000000000000,"G230519E55189N","2008-05-01T00:00:00",514502.169989717425779,0.514502000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230519E55189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.480681623698842,55.189113500000005]
["glac_bound",382065.000000000000000,"G227004E58304N","2008-05-01T00:00:00",709087.978442446794361,0.709088000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227004E58304N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.996108580845771,58.305641999999999]
["glac_bound",382069.000000000000000,"G231138E57357N","2008-05-01T00:00:00",259508.082022528367816,0.259508000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231138E57357N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.863652880013831,57.357752500000004]
["glac_bound",382071.000000000000000,"G222173E59779N","2008-05-01T00:00:00",348207.939847483939957,0.348208000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222173E59779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.826823449879242,59.779840000000000]
["glac_bound",382076.000000000000000,"G222876E59476N","2008-05-01T00:00:00",312372.306657481996808,0.312372000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222876E59476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.130523227177548,59.477427499999997]
["glac_bound",382085.000000000000000,"G230516E55254N","2008-05-01T00:00:00",351922.095284774957690,0.351922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230516E55254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.485155465945951,55.254174500000005]
["glac_bound",382092.000000000000000,"G230159E56426N","2008-05-01T00:00:00",118151.537697879466577,0.118152000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230159E56426N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.842389719920419,56.426163500000001]
["glac_bound",382094.000000000000000,"G228542E56668N","2008-05-01T00:00:00",1128054.607797180069610,1.128050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228542E56668N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.457501721755250,56.667521499999999]
["glac_bound",382098.000000000000000,"G229081E56766N","2008-05-01T00:00:00",488126.904768908920232,0.488127000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229081E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.918413649131537,56.768394499999999]
["glac_bound",382101.000000000000000,"G228631E57154N","2008-05-01T00:00:00",534602.653000514488667,0.534603000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228631E57154N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.368445985982873,57.155501500000000]
["glac_bound",382102.000000000000000,"G222470E59651N","2008-05-01T00:00:00",465627.401075460249558,0.465627000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222470E59651N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.538016643192009,59.651650500000002]
["glac_bound",382103.000000000000000,"G230597E56746N","2008-05-01T00:00:00",175899.468615348188905,0.175899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230597E56746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.401860061299971,56.745786500000001]
["glac_bound",382104.000000000000000,"G231704E56242N","2008-05-01T00:00:00",122058.985270713586942,0.122059000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231704E56242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.297347455470344,56.242139000000002]
["glac_bound",382112.000000000000000,"G230233E54724N","2008-05-01T00:00:00",821013.382210383191705,0.821013000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230233E54724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.766643458207852,54.726031000000006]
["glac_bound",382116.000000000000000,"G228648E56845N","2008-05-01T00:00:00",604857.177432268857956,0.604857000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228648E56845N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.350297246926800,56.842592999999994]
["glac_bound",382120.000000000000000,"G229434E56942N","2008-05-01T00:00:00",829940.647472062613815,0.829941000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229434E56942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.565396101889291,56.942315500000007]
["glac_bound",382121.000000000000000,"G230546E56794N","2008-05-01T00:00:00",193887.358872636395972,0.193887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230546E56794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.453765868830459,56.794788499999996]
["glac_bound",382124.000000000000000,"G228079E57109N","2008-05-01T00:00:00",632029.563090814161114,0.632030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228079E57109N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.920632909777908,57.109830500000001]
["glac_bound",382131.000000000000000,"G229055E56852N","2008-05-01T00:00:00",567085.348849858040921,0.567085000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229055E56852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.949132644905404,56.849453499999996]
["glac_bound",382132.000000000000000,"G230323E54685N","2008-05-01T00:00:00",613366.806550614652224,0.613367000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230323E54685N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.676516611779419,54.685979500000002]
["glac_bound",382137.000000000000000,"G227868E57790N","2008-05-01T00:00:00",981798.938506780425087,0.981799000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227868E57790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.139750728289727,57.791959000000006]
["glac_bound",382139.000000000000000,"G225125E59549N","2008-05-01T00:00:00",288884.149645078810863,0.288884000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225125E59549N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.876018979320975,59.549146000000000]
["glac_bound",382143.000000000000000,"G225614E59446N","2008-05-01T00:00:00",80304.817035090993159,0.080305000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225614E59446N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.384794933740977,59.445871499999996]
["glac_bound",382144.000000000000000,"G228104E56748N","2008-05-01T00:00:00",288948.961417682294268,0.288949000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228104E56748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.896285859689556,56.747545500000001]
["glac_bound",382146.000000000000000,"G225807E59179N","2008-05-01T00:00:00",500336.284941213554703,0.500336000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225807E59179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.195656983401335,59.179094500000005]
["glac_bound",382153.000000000000000,"G225048E59542N","2008-05-01T00:00:00",194858.428096872899914,0.194858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225048E59542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.952123521770943,59.544487000000004]
["glac_bound",382156.000000000000000,"G230322E55129N","2008-05-01T00:00:00",129452.355974693680764,0.129452000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230322E55129N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.678225997706420,55.128847999999998]
["glac_bound",382160.000000000000000,"G223558E59848N","2008-05-01T00:00:00",632169.727391267195344,0.632170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223558E59848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.434190028678813,59.843826500000006]
["glac_bound",382162.000000000000000,"G222817E59495N","2008-05-01T00:00:00",1252573.799133911728859,1.252570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222817E59495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.189868784480836,59.497143999999999]
["glac_bound",382166.000000000000000,"G230583E55646N","2008-05-01T00:00:00",1469651.567617216845974,1.469650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230583E55646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.426849810428052,55.637354999999999]
["glac_bound",382169.000000000000000,"G228439E56849N","2008-05-01T00:00:00",17760716.127918455749750,17.760700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228439E56849N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.561947408177161,56.848908500000000]
["glac_bound",382172.000000000000000,"G222226E59728N","2008-05-01T00:00:00",846304.509227291564457,0.846305000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222226E59728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.771546964258107,59.729002500000000]
["glac_bound",382173.000000000000000,"G229178E56866N","2008-05-01T00:00:00",995987.647322798497044,0.995988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229178E56866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.815847726611310,56.868899999999996]
["glac_bound",382183.000000000000000,"G228779E56619N","2008-05-01T00:00:00",3354856.025583862792701,3.354860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228779E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.216732014873514,56.619822499999998]
["glac_bound",382186.000000000000000,"G223950E59999N","2008-05-01T00:00:00",132951.602211660851026,0.132952000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223950E59999N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.049532346905551,59.998683499999999]
["glac_bound",382193.000000000000000,"G227657E58153N","2008-05-01T00:00:00",125389.924665632410324,0.125390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227657E58153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.343439974832222,58.152962500000001]
["glac_bound",382195.000000000000000,"G228768E57552N","2008-05-01T00:00:00",59404.119400187948486,0.059404000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228768E57552N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.231217116092296,57.553420000000003]
["glac_bound",382200.000000000000000,"G226503E58732N","2008-05-01T00:00:00",510094.671384074434172,0.510095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226503E58732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.497602961089257,58.732072500000001]
["glac_bound",382202.000000000000000,"G226664E58273N","2008-05-01T00:00:00",433547.688403120555449,0.433548000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226664E58273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.334792466769471,58.272500500000000]
["glac_bound",382204.000000000000000,"G230013E55592N","2008-05-01T00:00:00",239815.003910767642083,0.239815000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230013E55592N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.984557508686947,55.592565499999999]
["glac_bound",382207.000000000000000,"G228077E58066N","2008-05-01T00:00:00",1057593.373918431811035,1.057590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228077E58066N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.923152926607656,58.068748999999997]
["glac_bound",382208.000000000000000,"G225747E59274N","2008-05-01T00:00:00",250318.857967242773157,0.250319000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225747E59274N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.253264406689993,59.273646499999998]
["glac_bound",382209.000000000000000,"G227565E57981N","2008-05-01T00:00:00",12663586.413680160418153,12.663600000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227565E57981N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.433804507401305,57.997363499999999]
["glac_bound",382212.000000000000000,"G229074E56757N","2008-05-01T00:00:00",357106.856960195058491,0.357107000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229074E56757N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.925433636824948,56.758392999999998]
["glac_bound",382214.000000000000000,"G228057E57285N","2008-05-01T00:00:00",93446.611261504687718,0.093447000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228057E57285N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.940908734773814,57.284673499999997]
["glac_bound",382217.000000000000000,"G229329E56983N","2008-05-01T00:00:00",716957.981337270466611,0.716958000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229329E56983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.673778970375793,56.983636500000003]
["glac_bound",382221.000000000000000,"G224364E59854N","2008-05-01T00:00:00",435617.799776479310822,0.435618000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224364E59854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.636108311843373,59.855059999999995]
["glac_bound",382222.000000000000000,"G229965E57337N","2008-05-01T00:00:00",198614.472232628759230,0.198614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229965E57337N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.034949805423309,57.336923499999997]
["glac_bound",382224.000000000000000,"G230274E56328N","2008-05-01T00:00:00",54486.423352826051996,0.054486000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230274E56328N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.726092406756777,56.328394000000003]
["glac_bound",382226.000000000000000,"G223730E59573N","2008-05-01T00:00:00",946555.499813301023096,0.946555000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223730E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.273325221535572,59.572664000000003]
["glac_bound",382227.000000000000000,"G225000E59632N","2008-05-01T00:00:00",114139.535667351927259,0.114140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225000E59632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.000743634196397,59.632246500000001]
["glac_bound",382229.000000000000000,"G226461E58942N","2008-05-01T00:00:00",536873.877756466623396,0.536874000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226461E58942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.536027403979233,58.944389500000000]
["glac_bound",382232.000000000000000,"G226942E58247N","2008-05-01T00:00:00",845014.168382076546550,0.845014000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226942E58247N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.061367946542134,58.248835499999998]
["glac_bound",382234.000000000000000,"G229686E56385N","2008-05-01T00:00:00",19457414.243106789886951,19.457400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229686E56385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.327151542576928,56.414365000000004]
["glac_bound",382240.000000000000000,"G230505E55192N","2008-05-01T00:00:00",123096.398424656392308,0.123096000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230505E55192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.495123456878787,55.192171000000002]
["glac_bound",382245.000000000000000,"G222496E59268N","2008-05-01T00:00:00",8898721.945441601797938,8.898720000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222496E59268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.514539241490695,59.271101999999999]
["glac_bound",382251.000000000000000,"G222469E59543N","2008-05-01T00:00:00",427258.815400411665905,0.427259000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222469E59543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.535484646884640,59.542823999999996]
["glac_bound",382253.000000000000000,"G228732E57494N","2008-05-01T00:00:00",803211.436675461474806,0.803211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228732E57494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.267598782047060,57.494824999999999]
["glac_bound",382259.000000000000000,"G222965E59569N","2008-05-01T00:00:00",750969.139736251556315,0.750969000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222965E59569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.034140022076826,59.569691500000005]
["glac_bound",382261.000000000000000,"G223495E59470N","2008-05-01T00:00:00",4642538.107533760368824,4.642540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223495E59470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.502856149598102,59.473767500000001]
["glac_bound",382264.000000000000000,"G228883E56805N","2008-05-01T00:00:00",8341178.434502440504730,8.341180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228883E56805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.109726406752429,56.816527499999999]
["glac_bound",382267.000000000000000,"G224490E59879N","2008-05-01T00:00:00",459387.605982416134793,0.459388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224490E59879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.511106228162646,59.877852500000003]
["glac_bound",382282.000000000000000,"G228995E57259N","2008-05-01T00:00:00",476208.211399408406578,0.476208000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228995E57259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.004562684222947,57.258415999999997]
["glac_bound",382285.000000000000000,"G222544E59600N","2008-05-01T00:00:00",164382.117902628146112,0.164382000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222544E59600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.456226460154255,59.600216500000002]
["glac_bound",382286.000000000000000,"G228747E57277N","2008-05-01T00:00:00",7744042.094183675944805,7.744040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228747E57277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.247241260294118,57.277045000000001]
["glac_bound",382295.000000000000000,"G229566E56519N","2008-05-01T00:00:00",87295.943388703773962,0.087296000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229566E56519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.434300803526213,56.520867500000001]
["glac_bound",382301.000000000000000,"G230380E55166N","2008-05-01T00:00:00",1654024.410475333221257,1.654020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230380E55166N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.623217733650648,55.163758500000000]
["glac_bound",382302.000000000000000,"G227686E57558N","2008-05-01T00:00:00",62851.959408835566137,0.062852000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227686E57558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.315714733086963,57.558639499999998]
["glac_bound",382304.000000000000000,"G222264E59575N","2008-05-01T00:00:00",2028557.392855929676443,2.028560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222264E59575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.737210514423055,59.578651000000001]
["glac_bound",382306.000000000000000,"G229772E56076N","2008-05-01T00:00:00",1040892.318913382012397,1.040890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229772E56076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.226101091172211,56.076582500000001]
["glac_bound",382308.000000000000000,"G229859E56267N","2008-05-01T00:00:00",444052.387453529052436,0.444052000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229859E56267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.137253384076416,56.268988499999999]
["glac_bound",382309.000000000000000,"G230280E57191N","2008-05-01T00:00:00",189316.992413082305575,0.189317000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230280E57191N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.719968913601662,57.191006500000000]
["glac_bound",382314.000000000000000,"G223470E59921N","2008-05-01T00:00:00",149868.880879828502657,0.149869000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223470E59921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.528909276020784,59.921861499999999]
["glac_bound",382324.000000000000000,"G231059E57487N","2008-05-01T00:00:00",128596.859516612661537,0.128597000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231059E57487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.940903296740998,57.487603500000006]
["glac_bound",382327.000000000000000,"G228157E57074N","2008-05-01T00:00:00",64414.654185397259425,0.064415000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228157E57074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.843799104098991,57.074263000000002]
["glac_bound",382330.000000000000000,"G229615E56424N","2008-05-01T00:00:00",1546566.402019741479307,1.546570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229615E56424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.392163151785724,56.429917500000002]
["glac_bound",382331.000000000000000,"G223234E59568N","2008-05-01T00:00:00",111734.148802667317796,0.111734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223234E59568N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.766459898170126,59.567300500000002]
["glac_bound",382335.000000000000000,"G224525E59854N","2008-05-01T00:00:00",1640090.444790381472558,1.640090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224525E59854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.477849673912658,59.852569000000003]
["glac_bound",382336.000000000000000,"G228744E57252N","2008-05-01T00:00:00",606391.307596217840910,0.606391000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228744E57252N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.258529779883389,57.253916000000004]
["glac_bound",382338.000000000000000,"G226911E58345N","2008-05-01T00:00:00",451215.032498748274520,0.451215000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226911E58345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.088464868305067,58.343997000000002]
["glac_bound",382344.000000000000000,"G222944E59437N","2008-05-01T00:00:00",3887286.808804699219763,3.887290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222944E59437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.052349337494547,59.435200500000001]
["glac_bound",382347.000000000000000,"G230425E55983N","2008-05-01T00:00:00",52961.642182168528961,0.052962000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230425E55983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.574390668885201,55.982927500000002]
["glac_bound",382350.000000000000000,"G227218E58461N","2008-05-01T00:00:00",59423.220741421486309,0.059423000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227218E58461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.782022424882541,58.461492500000006]
["glac_bound",382354.000000000000000,"G228416E57447N","2008-05-01T00:00:00",141992.965304214274511,0.141993000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228416E57447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584902480164658,57.446296000000004]
["glac_bound",382357.000000000000000,"G230755E55305N","2008-05-01T00:00:00",160165.105239986616652,0.160165000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230755E55305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.246263514242258,55.304797499999999]
["glac_bound",382359.000000000000000,"G231430E56127N","2008-05-01T00:00:00",621610.668152151163667,0.621611000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231430E56127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.570347236711712,56.127830000000003]
["glac_bound",382361.000000000000000,"G230268E56994N","2008-05-01T00:00:00",1453114.655474658124149,1.453110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230268E56994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.735725491044121,56.996148000000005]
["glac_bound",382365.000000000000000,"G223756E59958N","2008-05-01T00:00:00",72664.406851050734986,0.072664000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223756E59958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.243913002390741,59.957853999999998]
["glac_bound",382366.000000000000000,"G227557E58108N","2008-05-01T00:00:00",280104.185027526458725,0.280104000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227557E58108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.443446930830930,58.107684500000005]
["glac_bound",382369.000000000000000,"G227285E58491N","2008-05-01T00:00:00",300425.774349552753847,0.300426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227285E58491N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.716708590011791,58.490222000000003]
["glac_bound",382371.000000000000000,"G226986E58027N","2008-05-01T00:00:00",796928.416402479750104,0.796928000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226986E58027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.016790602144113,58.027292000000003]
["glac_bound",382376.000000000000000,"G230491E56374N","2008-05-01T00:00:00",193968.099339038337348,0.193968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230491E56374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.507146702041354,56.374111499999998]
["glac_bound",382378.000000000000000,"G222259E59355N","2008-05-01T00:00:00",5672694.250434339046478,5.672690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222259E59355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.739565286654113,59.368980499999999]
["glac_bound",382393.000000000000000,"G231272E57518N","2008-05-01T00:00:00",2085914.007718779379502,2.085910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231272E57518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.729862998092585,57.521448500000005]
["glac_bound",382394.000000000000000,"G227432E58439N","2008-05-01T00:00:00",1085486.926575992256403,1.085490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227432E58439N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.567640100754318,58.440481000000005]
["glac_bound",382396.000000000000000,"G225415E59431N","2008-05-01T00:00:00",67474.333335663788603,0.067474000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225415E59431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.583711576543806,59.431153500000001]
["glac_bound",382398.000000000000000,"G231226E57070N","2008-05-01T00:00:00",514634.310708907898515,0.514634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231226E57070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.772677931204498,57.071339500000001]
["glac_bound",382399.000000000000000,"G230001E56277N","2008-05-01T00:00:00",3257502.462544037494808,3.257500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230001E56277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.993710078212303,56.277010500000003]
["glac_bound",382401.000000000000000,"G223775E59946N","2008-05-01T00:00:00",2790478.789970202371478,2.790480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223775E59946N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.220041262122038,59.947745499999996]
["glac_bound",382404.000000000000000,"G230208E57461N","2008-05-01T00:00:00",274421.038867277908139,0.274421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230208E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.791940323061937,57.460790000000003]
["glac_bound",382405.000000000000000,"G221470E59734N","2008-05-01T00:00:00",929256.230916073196568,0.929256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221470E59734N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.530236947956553,59.731673000000001]
["glac_bound",382406.000000000000000,"G227265E58352N","2008-05-01T00:00:00",1276920.162201788509265,1.276920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227265E58352N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.737771954136832,58.357095999999999]
["glac_bound",382407.000000000000000,"G230962E57413N","2008-05-01T00:00:00",242632.814247936476022,0.242633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230962E57413N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.038023695063089,57.412999499999998]
["glac_bound",382411.000000000000000,"G230459E56666N","2008-05-01T00:00:00",502647.633461985213216,0.502648000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230459E56666N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.542946501001325,56.665829500000001]
["glac_bound",382412.000000000000000,"G226725E58227N","2008-05-01T00:00:00",73011.658209718953003,0.073012000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226725E58227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.272500885034447,58.227086000000000]
["glac_bound",382414.000000000000000,"G227050E58151N","2008-05-01T00:00:00",4134628.468025268055499,4.134630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227050E58151N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.949157605152294,58.153581500000001]
["glac_bound",382416.000000000000000,"G228383E57079N","2008-05-01T00:00:00",423681.007002691621892,0.423681000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228383E57079N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.617897633982096,57.077829500000000]
["glac_bound",382417.000000000000000,"G224996E59638N","2008-05-01T00:00:00",434405.084864179953001,0.434405000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224996E59638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.003532151377215,59.638705999999999]
["glac_bound",382418.000000000000000,"G227750E57735N","2008-05-01T00:00:00",176613.853909075201955,0.176614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227750E57735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.249366531042142,57.735298000000000]
["glac_bound",382426.000000000000000,"G228632E56597N","2008-05-01T00:00:00",606369.168987377313897,0.606369000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228632E56597N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.368080029968667,56.597078500000002]
["glac_bound",382429.000000000000000,"G229057E56493N","2008-05-01T00:00:00",10707387.129161229357123,10.707400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229057E56493N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.938584061955481,56.501886499999998]
["glac_bound",382435.000000000000000,"G230093E55866N","2008-05-01T00:00:00",470755.455630886252038,0.470755000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230093E55866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.902991736521415,55.868086500000004]
["glac_bound",382436.000000000000000,"G228788E56633N","2008-05-01T00:00:00",1217651.478952892357484,1.217650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228788E56633N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.206347318071096,56.633203500000000]
["glac_bound",382440.000000000000000,"G230445E55301N","2008-05-01T00:00:00",143574.657381234719651,0.143575000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230445E55301N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.554595444406573,55.301046499999998]
["glac_bound",382448.000000000000000,"G227893E57235N","2008-05-01T00:00:00",14855453.486501587554812,14.855499999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227893E57235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.128078242711354,57.255479999999999]
["glac_bound",382451.000000000000000,"G229873E57098N","2008-05-01T00:00:00",137621.593571968405740,0.137622000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229873E57098N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.127487203836154,57.098439499999998]
["glac_bound",382452.000000000000000,"G227786E57823N","2008-05-01T00:00:00",307197.511260699771810,0.307198000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227786E57823N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.215235558358614,57.823364499999997]
["glac_bound",382453.000000000000000,"G229663E56328N","2008-05-01T00:00:00",5089034.142858661711216,5.089030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229663E56328N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.333344693855054,56.331854499999999]
["glac_bound",382455.000000000000000,"G228925E56766N","2008-05-01T00:00:00",5576521.421090176329017,5.576520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228925E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.086523185499459,56.780104500000000]
["glac_bound",382456.000000000000000,"G230440E56027N","2008-05-01T00:00:00",1155779.958873290801421,1.155780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230440E56027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.558453125771734,56.029964000000000]
["glac_bound",382457.000000000000000,"G229167E56373N","2008-05-01T00:00:00",2711091.180593188386410,2.711090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229167E56373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.826225834799999,56.375720999999999]
["glac_bound",382459.000000000000000,"G223312E59593N","2008-05-01T00:00:00",1609362.872269606683403,1.609360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223312E59593N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.691353386960600,59.593912000000003]
["glac_bound",382461.000000000000000,"G229713E57738N","2008-05-01T00:00:00",455117.341682911675889,0.455117000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229713E57738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.287490813413768,57.737900999999994]
["glac_bound",382467.000000000000000,"G227113E58415N","2008-05-01T00:00:00",434887.043775952246506,0.434887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227113E58415N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.887148527800491,58.414764499999997]
["glac_bound",382468.000000000000000,"G223329E59705N","2008-05-01T00:00:00",725028.758225918165408,0.725029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223329E59705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.669430508172354,59.704391999999999]
["glac_bound",382469.000000000000000,"G228973E56560N","2008-05-01T00:00:00",715393.077024589991197,0.715393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228973E56560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.030141586753757,56.562397500000003]
["glac_bound",382474.000000000000000,"G228285E57214N","2008-05-01T00:00:00",115607.714558648265665,0.115608000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228285E57214N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.717351581239541,57.215817999999999]
["glac_bound",382476.000000000000000,"G225835E59364N","2008-05-01T00:00:00",266806.151634945417754,0.266806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225835E59364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.168345758403348,59.365472999999994]
["glac_bound",382478.000000000000000,"G229530E56740N","2008-05-01T00:00:00",752151.235365254571661,0.752151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229530E56740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.471025858946064,56.739274999999999]
["glac_bound",382479.000000000000000,"G227228E58204N","2008-05-01T00:00:00",226063.692974964214955,0.226064000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227228E58204N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.771471411972385,58.206851999999998]
["glac_bound",382480.000000000000000,"G230447E56039N","2008-05-01T00:00:00",381586.002772148407530,0.381586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230447E56039N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.552380272233393,56.039502999999996]
["glac_bound",382484.000000000000000,"G230428E56655N","2008-05-01T00:00:00",167396.596891610010061,0.167397000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230428E56655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.570242983825608,56.655590500000002]
["glac_bound",382487.000000000000000,"G222497E59616N","2008-05-01T00:00:00",739333.239306267350912,0.739333000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222497E59616N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.504099245523378,59.615652999999995]
["glac_bound",382490.000000000000000,"G226687E58559N","2008-05-01T00:00:00",123989.191007398199872,0.123989000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226687E58559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.313000742484974,58.558076499999999]
["glac_bound",382493.000000000000000,"G230336E54757N","2008-05-01T00:00:00",62542.293539084326767,0.062542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230336E54757N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.663698106375364,54.757441999999998]
["glac_bound",382495.000000000000000,"G227704E57930N","2008-05-01T00:00:00",197845.449589850031771,0.197845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227704E57930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.295417793112165,57.930655500000000]
["glac_bound",382498.000000000000000,"G230476E57099N","2008-05-01T00:00:00",1612952.539587062783539,1.612950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230476E57099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522149880315794,57.100365499999995]
["glac_bound",382499.000000000000000,"G230242E56373N","2008-05-01T00:00:00",169849.509788751427550,0.169850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230242E56373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.758038095564075,56.372284000000001]
["glac_bound",382503.000000000000000,"G223061E59559N","2008-05-01T00:00:00",3006481.349968959577382,3.006480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223061E59559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.933485988826817,59.562374500000004]
["glac_bound",382512.000000000000000,"G226027E59018N","2008-05-01T00:00:00",896344.454197516199201,0.896344000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226027E59018N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.978394854969565,59.016999999999996]
["glac_bound",382516.000000000000000,"G227760E57795N","2008-05-01T00:00:00",728570.046903242124245,0.728570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227760E57795N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.235995231602374,57.792327000000000]
["glac_bound",382518.000000000000000,"G230079E55712N","2008-05-01T00:00:00",199447.191496001702035,0.199447000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230079E55712N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.920624598283268,55.713179499999995]
["glac_bound",382523.000000000000000,"G223524E59721N","2008-05-01T00:00:00",55033.065490934219270,0.055033000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223524E59721N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.475830498329856,59.721128000000000]
["glac_bound",382525.000000000000000,"G229255E57097N","2008-05-01T00:00:00",162929.926094224851113,0.162930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229255E57097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.745285647774665,57.097171500000002]
["glac_bound",382528.000000000000000,"G230639E54905N","2008-05-01T00:00:00",766572.856860696920194,0.766573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230639E54905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.356771224537113,54.905494500000003]
["glac_bound",382529.000000000000000,"G227569E58207N","2008-05-01T00:00:00",1082482.821245203958824,1.082480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227569E58207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.427662349309571,58.205129499999998]
["glac_bound",382530.000000000000000,"G229124E57075N","2008-05-01T00:00:00",1033003.190711280680262,1.033000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229124E57075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.877560369530727,57.076463500000003]
["glac_bound",382532.000000000000000,"G228602E57045N","2008-05-01T00:00:00",53808.651467933792446,0.053809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228602E57045N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.398774365595614,57.044227500000005]
["glac_bound",382533.000000000000000,"G231813E57158N","2008-05-01T00:00:00",218225.524570602137828,0.218226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EA231813E57158N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.184490506450345,57.159197500000005]
["glac_bound",382534.000000000000000,"G229140E56420N","2008-05-01T00:00:00",71771.139274654051405,0.071771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229140E56420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.859885361773479,56.420260999999996]
["glac_bound",382539.000000000000000,"G227888E57777N","2008-05-01T00:00:00",1846303.162454965757206,1.846300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227888E57777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.118658547656594,57.774240500000005]
["glac_bound",382540.000000000000000,"G228831E57539N","2008-05-01T00:00:00",560236.589112386107445,0.560237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228831E57539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.169653026952574,57.538913999999998]
["glac_bound",382544.000000000000000,"G229927E57126N","2008-05-01T00:00:00",52615.363615071873937,0.052615000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229927E57126N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.072640541888688,57.126849000000000]
["glac_bound",382548.000000000000000,"G230054E56152N","2008-05-01T00:00:00",581756.781710635870695,0.581757000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230054E56152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.941983734743928,56.153447000000000]
["glac_bound",382551.000000000000000,"G222876E59454N","2008-05-01T00:00:00",770424.456654886249453,0.770424000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222876E59454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.121122158991568,59.456506000000005]
["glac_bound",382552.000000000000000,"G226710E58319N","2008-05-01T00:00:00",417153.306520127633121,0.417153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226710E58319N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.294413962168335,58.317382500000001]
["glac_bound",382560.000000000000000,"G223430E59443N","2008-05-01T00:00:00",1204572.627064031083137,1.204570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223430E59443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.572091798428062,59.442264999999999]
["glac_bound",382562.000000000000000,"G223458E59484N","2008-05-01T00:00:00",1661896.807676700875163,1.661900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223458E59484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.540446593809833,59.490757500000001]
["glac_bound",382565.000000000000000,"G226071E58729N","2008-05-01T00:00:00",3934047.787697016727179,3.934050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226071E58729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.932494728891669,58.737588000000002]
["glac_bound",382567.000000000000000,"G222189E59395N","2008-05-01T00:00:00",66839.851734904033947,0.066840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222189E59395N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.810211944855979,59.395239000000004]
["glac_bound",382577.000000000000000,"G230444E57057N","2008-05-01T00:00:00",364543.738188230257947,0.364544000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230444E57057N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.556712477989493,57.058621000000002]
["glac_bound",382580.000000000000000,"G221986E59545N","2008-05-01T00:00:00",4269349.006190237589180,4.269350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221986E59545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.998770086178070,59.550091000000002]
["glac_bound",382581.000000000000000,"G230225E54525N","2008-05-01T00:00:00",444127.612523982243147,0.444128000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230225E54525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.770764222573831,54.524319499999997]
["glac_bound",382591.000000000000000,"G227825E57922N","2008-05-01T00:00:00",2859629.530999693088233,2.859630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227825E57922N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.174302745514183,57.921948499999999]
["glac_bound",382592.000000000000000,"G226235E58711N","2008-05-01T00:00:00",3213225.746532612480223,3.213230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226235E58711N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.763527584888038,58.710709999999999]
["glac_bound",382593.000000000000000,"G222340E59351N","2008-05-01T00:00:00",1041481.138956416049041,1.041480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222340E59351N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.661937263444770,59.352255999999997]
["glac_bound",382594.000000000000000,"G222100E59861N","2008-05-01T00:00:00",1153364.075920974137262,1.153360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222100E59861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.899525320397061,59.862882999999997]
["glac_bound",382598.000000000000000,"G230236E56987N","2008-05-01T00:00:00",201462.637719177000690,0.201463000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230236E56987N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.763587869480205,56.987697499999996]
["glac_bound",382599.000000000000000,"G228695E57242N","2008-05-01T00:00:00",104414.670612592090038,0.104415000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228695E57242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.304697626693155,57.245462500000002]
["glac_bound",382603.000000000000000,"G226861E58288N","2008-05-01T00:00:00",84732.163964680454228,0.084732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226861E58288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.139187055094595,58.287755000000004]
["glac_bound",382605.000000000000000,"G225667E59155N","2008-05-01T00:00:00",731870.732118721352890,0.731871000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225667E59155N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.333855850715139,59.155264500000001]
["glac_bound",382610.000000000000000,"G230425E56722N","2008-05-01T00:00:00",151299.897767069633119,0.151300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230425E56722N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.576320253825941,56.722405500000001]
["glac_bound",382611.000000000000000,"G230276E54824N","2008-05-01T00:00:00",793373.656348527176306,0.793374000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230276E54824N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.724547430430874,54.823822499999999]
["glac_bound",382612.000000000000000,"G230113E56312N","2008-05-01T00:00:00",158113.795252456940943,0.158114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230113E56312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.886804927845162,56.312298999999996]
["glac_bound",382613.000000000000000,"G229569E56280N","2008-05-01T00:00:00",69187.955045852620970,0.069188000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229569E56280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.430056894859831,56.280242500000000]
["glac_bound",382615.000000000000000,"G229618E56159N","2008-05-01T00:00:00",473695.860305096139200,0.473696000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229618E56159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.381454490740737,56.159248500000004]
["glac_bound",382628.000000000000000,"G225736E59390N","2008-05-01T00:00:00",256216.949190235696733,0.256217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225736E59390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.264987543853294,59.388897499999999]
["glac_bound",382634.000000000000000,"G224294E59982N","2008-05-01T00:00:00",339330.385968624847010,0.339330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224294E59982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.703054111043571,59.980682500000000]
["glac_bound",382635.000000000000000,"G222435E59632N","2008-05-01T00:00:00",385080.270655310072470,0.385080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222435E59632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.565588169934074,59.631929000000000]
["glac_bound",382636.000000000000000,"G227614E57948N","2008-05-01T00:00:00",5923170.185410805046558,5.923170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227614E57948N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.389515978101429,57.951519000000005]
["glac_bound",382639.000000000000000,"G223118E59691N","2008-05-01T00:00:00",566357.006842400995083,0.566357000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223118E59691N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.886772099999973,59.693048000000005]
["glac_bound",382642.000000000000000,"G227630E58064N","2008-05-01T00:00:00",4409680.786288957111537,4.409680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227630E58064N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.372147373550376,58.068219999999997]
["glac_bound",382644.000000000000000,"G227253E58006N","2008-05-01T00:00:00",173269.174065931350924,0.173269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227253E58006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.747068057578758,58.005116999999998]
["glac_bound",382646.000000000000000,"G224537E59802N","2008-05-01T00:00:00",4411141.413942972198129,4.411140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224537E59802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.451450383741985,59.806959000000006]
["glac_bound",382650.000000000000000,"G230051E57075N","2008-05-01T00:00:00",543558.729038597433828,0.543559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230051E57075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.945884964230743,57.075809499999998]
["glac_bound",382655.000000000000000,"G230446E56247N","2008-05-01T00:00:00",420700.101864399213810,0.420700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230446E56247N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.555338931227880,56.246425000000002]
["glac_bound",382657.000000000000000,"G229752E56078N","2008-05-01T00:00:00",4125862.264044980518520,4.125860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229752E56078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.238025920742501,56.085307499999999]
["glac_bound",382658.000000000000000,"G222521E59851N","2008-05-01T00:00:00",320781.652364310808480,0.320782000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222521E59851N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.480399340492738,59.850346500000001]
["glac_bound",382664.000000000000000,"G230353E56695N","2008-05-01T00:00:00",84773.291810827679001,0.084773000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230353E56695N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.645560192064011,56.695863000000003]
["glac_bound",382665.000000000000000,"G228407E57346N","2008-05-01T00:00:00",880357.942330702557229,0.880358000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228407E57346N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.590930987739938,57.346573500000005]
["glac_bound",382672.000000000000000,"G228041E57832N","2008-05-01T00:00:00",473848.455549008736853,0.473848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228041E57832N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.958647836442964,57.831289499999997]
["glac_bound",382682.000000000000000,"G223399E59949N","2008-05-01T00:00:00",87469.231845490561682,0.087469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223399E59949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.600950717176829,59.949123499999999]
["glac_bound",382691.000000000000000,"G222229E59373N","2008-05-01T00:00:00",248578.387362550565740,0.248578000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222229E59373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.769271116534895,59.372732499999998]
["glac_bound",382696.000000000000000,"G224586E59914N","2008-05-01T00:00:00",495150.468634294811636,0.495150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224586E59914N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.414216632243665,59.913421499999998]
["glac_bound",382697.000000000000000,"G224073E59879N","2008-05-01T00:00:00",127805.158037962799426,0.127805000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224073E59879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.927262669502625,59.878571500000000]
["glac_bound",382698.000000000000000,"G229277E56834N","2008-05-01T00:00:00",4924345.174758905544877,4.924350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229277E56834N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.723366590300458,56.836207000000002]
["glac_bound",382703.000000000000000,"G226665E58550N","2008-05-01T00:00:00",2482071.872548008337617,2.482070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226665E58550N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.337689604882485,58.552263999999994]
["glac_bound",382707.000000000000000,"G230655E55618N","2008-05-01T00:00:00",252225.922245382331312,0.252226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230655E55618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.344531172240124,55.617813999999996]
["glac_bound",382709.000000000000000,"G226773E58291N","2008-05-01T00:00:00",237263.407936047209660,0.237263000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226773E58291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.227758963179213,58.291111000000001]
["glac_bound",382720.000000000000000,"G230133E56472N","2008-05-01T00:00:00",1023473.608418804244138,1.023470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230133E56472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.861870812279562,56.473829500000001]
["glac_bound",382721.000000000000000,"G226618E58635N","2008-05-01T00:00:00",376152.868100093037356,0.376153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226618E58635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.381402889121773,58.633691999999996]
["glac_bound",382723.000000000000000,"G229009E56822N","2008-05-01T00:00:00",10571083.344615828245878,10.571099999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229009E56822N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.019001188818550,56.838419000000002]
["glac_bound",382724.000000000000000,"G224982E59639N","2008-05-01T00:00:00",154078.414606961392565,0.154078000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224982E59639N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.018635375305905,59.639110500000001]
["glac_bound",382729.000000000000000,"G231197E55222N","2008-05-01T00:00:00",92570.579242208856158,0.092571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231197E55222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.802026088714570,55.222105499999998]
["glac_bound",382735.000000000000000,"G227298E58194N","2008-05-01T00:00:00",431168.701111220172606,0.431169000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227298E58194N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.702734604184229,58.194494499999998]
["glac_bound",382737.000000000000000,"G227292E58423N","2008-05-01T00:00:00",522585.571985393355135,0.522586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227292E58423N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.706606503746769,58.422552000000003]
["glac_bound",382741.000000000000000,"G227509E57728N","2008-05-01T00:00:00",285716.952365512028337,0.285717000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227509E57728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.490891166748042,57.727283499999999]
["glac_bound",382742.000000000000000,"G225753E59146N","2008-05-01T00:00:00",295706.958574289979879,0.295707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225753E59146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.246762312944497,59.145908500000004]
["glac_bound",382744.000000000000000,"G228423E57386N","2008-05-01T00:00:00",2543732.290767341852188,2.543730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228423E57386N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584907698885388,57.385098999999997]
["glac_bound",382752.000000000000000,"G229405E56588N","2008-05-01T00:00:00",61663.076493870968989,0.061663000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229405E56588N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.596209691466868,56.587766000000002]
["glac_bound",382756.000000000000000,"G228684E57434N","2008-05-01T00:00:00",231827.253879959404003,0.231827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228684E57434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.315347386769815,57.434052500000000]
["glac_bound",382759.000000000000000,"G227172E58218N","2008-05-01T00:00:00",249332.263815345795592,0.249332000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227172E58218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.826847586527407,58.218532499999995]
["glac_bound",382761.000000000000000,"G223631E59735N","2008-05-01T00:00:00",181258.407793998048874,0.181258000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223631E59735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.369352869723230,59.735449000000003]
["glac_bound",382763.000000000000000,"G223326E59752N","2008-05-01T00:00:00",353317.899767548544332,0.353318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223326E59752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.677589126528687,59.752991999999999]
["glac_bound",382767.000000000000000,"G226468E58529N","2008-05-01T00:00:00",78685.884139749672613,0.078686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226468E58529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.531347532806819,58.528981999999999]
["glac_bound",382768.000000000000000,"G221925E59554N","2008-05-01T00:00:00",4845021.624336307868361,4.845020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221925E59554N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.076764741268136,59.559979999999996]
["glac_bound",382770.000000000000000,"G229697E56450N","2008-05-01T00:00:00",72480.428759714399348,0.072480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229697E56450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.302390875728918,56.450458999999995]
["glac_bound",382772.000000000000000,"G228502E57516N","2008-05-01T00:00:00",1179351.948890071129426,1.179350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228502E57516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.498053405081919,57.516756000000001]
["glac_bound",382779.000000000000000,"G227788E58033N","2008-05-01T00:00:00",1557147.214225256117061,1.557150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227788E58033N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.210733482931289,58.039453500000000]
["glac_bound",382784.000000000000000,"G230518E56668N","2008-05-01T00:00:00",230234.743167727312539,0.230235000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230518E56668N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.481594201462769,56.668908500000001]
["glac_bound",382785.000000000000000,"G223727E59794N","2008-05-01T00:00:00",682388.797668384155259,0.682389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223727E59794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.268401108958926,59.792867999999999]
["glac_bound",382788.000000000000000,"G222450E59502N","2008-05-01T00:00:00",826247.860205899341963,0.826248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222450E59502N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.551301273214278,59.502965000000003]
["glac_bound",382790.000000000000000,"G223622E59750N","2008-05-01T00:00:00",358689.751043259340804,0.358690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223622E59750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.379149061999783,59.750475500000000]
["glac_bound",382792.000000000000000,"G227314E58216N","2008-05-01T00:00:00",3182983.042346949223429,3.182980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227314E58216N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.668546888455523,58.214510000000004]
["glac_bound",382795.000000000000000,"G227088E57958N","2008-05-01T00:00:00",1329108.687267833855003,1.329110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227088E57958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.916042563971615,57.961895999999996]
["glac_bound",382802.000000000000000,"G221690E59986N","2008-05-01T00:00:00",1226189.093237627530470,1.226190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221690E59986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.312066732673259,59.992743000000004]
["glac_bound",382804.000000000000000,"G230169E57364N","2008-05-01T00:00:00",143234.651185955968685,0.143235000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230169E57364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.832122774643977,57.367243000000002]
["glac_bound",382818.000000000000000,"G221788E59958N","2008-05-01T00:00:00",325851.788716213195585,0.325852000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221788E59958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.208246261348449,59.959290500000002]
["glac_bound",382819.000000000000000,"G225053E59613N","2008-05-01T00:00:00",243897.946098693937529,0.243898000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225053E59613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.947011467209819,59.616510500000004]
["glac_bound",382820.000000000000000,"G230237E56937N","2008-05-01T00:00:00",160696.175773729279172,0.160696000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230237E56937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.762929128703888,56.936999000000000]
["glac_bound",382824.000000000000000,"G229581E56514N","2008-05-01T00:00:00",940517.153728404431604,2.019470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229581E56514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.417599053654925,56.526038499999999]
["glac_bound",382824.000000000000000,"G229581E56514N","2008-05-01T00:00:00",1078956.746384813683107,2.019470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229581E56514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.419535121151341,56.513592500000001]
["glac_bound",382827.000000000000000,"G228801E57503N","2008-05-01T00:00:00",1062903.203934097196907,1.062900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228801E57503N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.196438888118848,57.505102000000001]
["glac_bound",382828.000000000000000,"G230512E57210N","2008-05-01T00:00:00",968483.756204038043506,0.968484000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230512E57210N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.488962943917244,57.211086000000002]
["glac_bound",382833.000000000000000,"G225008E59629N","2008-05-01T00:00:00",78074.687717137887375,0.078075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225008E59629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.993567685077608,59.629926499999996]
["glac_bound",382845.000000000000000,"G222121E59708N","2008-05-01T00:00:00",106392.822217739914777,0.106393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222121E59708N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.879734476389331,59.708727499999995]
["glac_bound",382849.000000000000000,"G228685E57127N","2008-05-01T00:00:00",3881697.760066112969071,3.881700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228685E57127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.313520425400156,57.133358500000000]
["glac_bound",382850.000000000000000,"G227117E58358N","2008-05-01T00:00:00",265831.674620136036538,0.265832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227117E58358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.884558949501610,58.357624999999999]
["glac_bound",382851.000000000000000,"G224784E59696N","2008-05-01T00:00:00",503442.046052543679252,0.503442000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224784E59696N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.218326112978161,59.696002500000006]
["glac_bound",382859.000000000000000,"G231817E57163N","2008-05-01T00:00:00",58583.750492048144224,0.058584000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EA231817E57163N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.183794351261554,57.163909000000004]
["glac_bound",382866.000000000000000,"G223226E59388N","2008-05-01T00:00:00",4119122.950787032488734,4.119120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223226E59388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.758761647161577,59.399397999999998]
["glac_bound",382868.000000000000000,"G224167E59956N","2008-05-01T00:00:00",1035419.264805008890107,1.035420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224167E59956N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.832782826923079,59.955055000000002]
["glac_bound",382879.000000000000000,"G224802E59963N","2008-05-01T00:00:00",134759.983726885431679,0.134760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224802E59963N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.197349637772732,59.965189000000002]
["glac_bound",382880.000000000000000,"G223901E59734N","2008-05-01T00:00:00",675621.348419799818657,0.675621000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223901E59734N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.103262556539562,59.734137500000003]
["glac_bound",382886.000000000000000,"G225480E59550N","2008-05-01T00:00:00",441095.041199545201380,0.441095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225480E59550N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.519863679096716,59.550514499999998]
["glac_bound",382899.000000000000000,"G224001E59983N","2008-05-01T00:00:00",492083.957490051281638,0.492084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224001E59983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.002151144019194,59.983936000000000]
["glac_bound",382901.000000000000000,"G229259E56774N","2008-05-01T00:00:00",2208142.133415605872869,2.208140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229259E56774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.737221444278930,56.778759500000000]
["glac_bound",382903.000000000000000,"G223437E59417N","2008-05-01T00:00:00",52871365.995675504207611,52.871400000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Jarvis Glacier","None","08BE223437E59417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.607384957500017,59.443475499999998]
["glac_bound",382906.000000000000000,"G224528E59795N","2008-05-01T00:00:00",79509.576432999994722,0.079510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224528E59795N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.471140176702619,59.795419499999994]
["glac_bound",382907.000000000000000,"G222202E59796N","2008-05-01T00:00:00",2533396.282451950944960,2.533400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222202E59796N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.805858006866515,59.788092500000005]
["glac_bound",382914.000000000000000,"G222574E59797N","2008-05-01T00:00:00",962816.943233257858083,0.962817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222574E59797N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.436401338367261,59.798676000000000]
["glac_bound",382919.000000000000000,"G230244E56165N","2008-05-01T00:00:00",29096736.673596892505884,29.096699999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230244E56165N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.785108000049377,56.174524000000005]
["glac_bound",382921.000000000000000,"G225644E59388N","2008-05-01T00:00:00",257243.777709856862202,0.257244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225644E59388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.355319305043452,59.387962999999999]
["glac_bound",382924.000000000000000,"G227254E58149N","2008-05-01T00:00:00",751769.415631345123984,0.751769000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227254E58149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.744699282768863,58.148589500000000]
["glac_bound",382925.000000000000000,"G228407E57083N","2008-05-01T00:00:00",2570112.201486228033900,2.570110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228407E57083N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.594347836092425,57.088791999999998]
["glac_bound",382928.000000000000000,"G230046E55901N","2008-05-01T00:00:00",117025.999565941150649,0.117026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230046E55901N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.954851408210601,55.900656999999995]
["glac_bound",382930.000000000000000,"G230326E55128N","2008-05-01T00:00:00",206792.779573211766547,0.206793000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230326E55128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.674215607911322,55.127608500000001]
["glac_bound",382933.000000000000000,"G230613E54979N","2008-05-01T00:00:00",162392.051934478018666,0.162392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230613E54979N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.389049390748653,54.980198500000000]
["glac_bound",382934.000000000000000,"G224027E59733N","2008-05-01T00:00:00",82269.674248104740400,0.082270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224027E59733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.972967708938398,59.732338999999996]
["glac_bound",382941.000000000000000,"G228404E56623N","2008-05-01T00:00:00",100616.722960334358504,0.100617000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228404E56623N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.596708187718377,56.625055000000003]
["glac_bound",382946.000000000000000,"G230557E56228N","2008-05-01T00:00:00",280320.600443673960399,0.280321000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230557E56228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.442804499999994,56.227964499999999]
["glac_bound",382947.000000000000000,"G230044E56173N","2008-05-01T00:00:00",228723.409445885423338,0.228723000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230044E56173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.955296095801657,56.173718500000007]
["glac_bound",382949.000000000000000,"G230442E55167N","2008-05-01T00:00:00",54456.623512860642222,0.054457000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230442E55167N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.557873730975700,55.167384499999997]
["glac_bound",382957.000000000000000,"G228967E56398N","2008-05-01T00:00:00",1223763.956951463827863,1.223760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD228967E56398N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.020545102871239,56.399481500000000]
["glac_bound",382960.000000000000000,"G228706E57237N","2008-05-01T00:00:00",249908.850818304461427,0.249909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228706E57237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.294470221073766,57.236900500000004]
["glac_bound",382969.000000000000000,"G222441E59179N","2008-05-01T00:00:00",210216.682072463765508,0.210217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222442E59180N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.558789921457901,59.180069000000003]
["glac_bound",382970.000000000000000,"G230020E56041N","2008-05-01T00:00:00",134274.969340056268265,0.134275000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230020E56041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.979720184729047,56.040838000000001]
["glac_bound",382974.000000000000000,"G229086E57083N","2008-05-01T00:00:00",235670.111021366639761,0.235670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229086E57083N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.913058352264386,57.083308000000002]
["glac_bound",382977.000000000000000,"G221670E59733N","2008-05-01T00:00:00",3042449.658461938146502,3.042450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221670E59733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.310279640615732,59.732828999999995]
["glac_bound",382981.000000000000000,"G229571E56441N","2008-05-01T00:00:00",146985.852706692938227,0.146986000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229571E56441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.429197913016594,56.441418499999997]
["glac_bound",382984.000000000000000,"G230077E55697N","2008-05-01T00:00:00",724676.227287653950043,0.724676000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230077E55697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.919055416848437,55.699205499999998]
["glac_bound",382985.000000000000000,"G224003E59948N","2008-05-01T00:00:00",942874.960003313142806,0.942875000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224003E59948N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.000120786315165,59.948487499999999]
["glac_bound",382989.000000000000000,"G230266E57012N","2008-05-01T00:00:00",1346133.986311165383086,1.346130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230266E57012N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.737280270655845,57.014175500000000]
["glac_bound",382990.000000000000000,"G226763E58515N","2008-05-01T00:00:00",88302.697012966702459,0.088303000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226763E58515N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.236466153544995,58.517100999999997]
["glac_bound",382993.000000000000000,"G229065E56768N","2008-05-01T00:00:00",162017.141277024638839,0.162017000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229065E56768N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.935410313348058,56.768866500000001]
["glac_bound",382996.000000000000000,"G228741E57435N","2008-05-01T00:00:00",2811270.671530670486391,2.811270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228741E57435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.257616109561752,57.441168000000005]
["glac_bound",382997.000000000000000,"G228805E57449N","2008-05-01T00:00:00",145950.847700837301090,0.145951000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228805E57449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.195842306699035,57.449133000000003]
["glac_bound",382999.000000000000000,"G229892E57016N","2008-05-01T00:00:00",11827349.076887518167496,11.827299999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229892E57016N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.098656691860469,57.015195000000006]
["glac_bound",383006.000000000000000,"G222904E59363N","2008-05-01T00:00:00",32597042.291015338152647,32.597000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222904E59363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.064297012034388,59.380790500000003]
["glac_bound",383007.000000000000000,"G229616E56151N","2008-05-01T00:00:00",8139513.764515560120344,8.139510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229616E56151N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.374943548260092,56.167314500000003]
["glac_bound",383008.000000000000000,"G222206E59604N","2008-05-01T00:00:00",2228712.855256351176649,2.228710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222206E59604N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.793122959197774,59.606904499999999]
["glac_bound",383016.000000000000000,"G230188E57009N","2008-05-01T00:00:00",59391.568772782855376,0.059392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230188E57009N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.814335383869434,57.008420000000001]
["glac_bound",383023.000000000000000,"G223895E59917N","2008-05-01T00:00:00",2703869.387180367950350,2.703870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223895E59917N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.108691842940857,59.917646000000005]
["glac_bound",383024.000000000000000,"G224315E59842N","2008-05-01T00:00:00",142057.065673752455041,0.142057000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224315E59842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.684961613157895,59.842877000000001]
["glac_bound",383026.000000000000000,"G222401E59538N","2008-05-01T00:00:00",980391.314466429757886,0.980391000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222401E59538N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.599887728013925,59.539091499999998]
["glac_bound",383027.000000000000000,"G225577E59300N","2008-05-01T00:00:00",5144656.667307859286666,5.144660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225577E59300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.412298733167802,59.306277999999999]
["glac_bound",383028.000000000000000,"G229282E56780N","2008-05-01T00:00:00",733212.788799728034064,0.733213000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229282E56780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.713834600808184,56.783962000000002]
["glac_bound",383031.000000000000000,"G228270E57244N","2008-05-01T00:00:00",753362.766429111012258,0.753363000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228270E57244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.725658708892837,57.249157499999995]
["glac_bound",383033.000000000000000,"G225064E59583N","2008-05-01T00:00:00",287905.172811408934649,0.287905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225064E59583N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.935160836035266,59.583465000000004]
["glac_bound",383038.000000000000000,"G230068E55827N","2008-05-01T00:00:00",149618.236144681868609,0.149618000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230068E55827N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.930763545837806,55.825487500000001]
["glac_bound",383042.000000000000000,"G230083E55794N","2008-05-01T00:00:00",1551329.267425834899768,1.551330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230083E55794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.914587079642558,55.795926999999999]
["glac_bound",383044.000000000000000,"G229300E57432N","2008-05-01T00:00:00",575939.222799326293170,0.575939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229300E57432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.697191203796365,57.430532999999997]
["glac_bound",383047.000000000000000,"G228707E57076N","2008-05-01T00:00:00",87271.000643701147055,0.087271000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228707E57076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.292169751896836,57.074573999999998]
["glac_bound",383049.000000000000000,"G230057E56134N","2008-05-01T00:00:00",470256.693909690424334,0.470257000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230057E56134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.944259157239060,56.137368500000001]
["glac_bound",383050.000000000000000,"G222426E59638N","2008-05-01T00:00:00",898248.835381800541654,0.898249000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222426E59638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.572916317378485,59.637997999999996]
["glac_bound",383054.000000000000000,"G225869E59335N","2008-05-01T00:00:00",577795.316116329166107,0.577795000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225869E59335N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.135122504672893,59.335199000000003]
["glac_bound",383055.000000000000000,"G226569E58770N","2008-05-01T00:00:00",519026.056576678587589,0.519026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226569E58770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.431036511299226,58.769874999999999]
["glac_bound",383057.000000000000000,"G223207E59634N","2008-05-01T00:00:00",194587.877559065556852,0.194588000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223207E59634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.792761740449890,59.634186999999997]
["glac_bound",383060.000000000000000,"G225763E59192N","2008-05-01T00:00:00",536553.585679598036222,0.536554000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225763E59192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.237081529523266,59.191127999999999]
["glac_bound",383063.000000000000000,"G227534E58204N","2008-05-01T00:00:00",573286.941672222106718,0.573287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227534E58204N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.466500297970470,58.205164499999995]
["glac_bound",383065.000000000000000,"G226956E58422N","2008-05-01T00:00:00",253631.378480108076474,0.253631000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226956E58422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.044518292452835,58.421233500000000]
["glac_bound",383066.000000000000000,"G225738E59019N","2008-05-01T00:00:00",114098.817848607985070,0.114099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225738E59019N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.263632777950306,59.018886000000002]
["glac_bound",383068.000000000000000,"G224540E59829N","2008-05-01T00:00:00",134549.149841883685440,0.134549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224540E59829N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.460129597356570,59.828673999999999]
["glac_bound",383070.000000000000000,"G227236E57663N","2008-05-01T00:00:00",528806191.68311315774917,528.806000000000040,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-11T00:00:00","okay","South Sawyer Glacier","None","08BC227236E57663N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.842263861542392,57.734069499999997]
["glac_bound",383084.000000000000000,"G228089E57591N","2008-05-01T00:00:00",338404.047200632921886,0.338404000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228089E57591N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.910443057259272,57.591250500000001]
["glac_bound",383085.000000000000000,"G222950E59203N","2008-05-01T00:00:00",1238420.789643004536629,1.238420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222950E59203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.044561404152489,59.200842000000002]
["glac_bound",383087.000000000000000,"G230534E57080N","2008-05-01T00:00:00",185043.248765886237379,0.185043000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230534E57080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463074012910567,57.080870500000003]
["glac_bound",383088.000000000000000,"G224539E59845N","2008-05-01T00:00:00",88583.327247424065717,0.088583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224539E59845N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.460274911694853,59.845264000000000]
["glac_bound",383092.000000000000000,"G230282E56371N","2008-05-01T00:00:00",52994.604117546638008,0.052995000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230282E56371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.717944033526010,56.370840500000000]
["glac_bound",383094.000000000000000,"G225089E59372N","2008-05-01T00:00:00",275566.411113865557127,0.275566000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225089E59372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.911469638888889,59.371972000000000]
["glac_bound",383095.000000000000000,"G227018E58096N","2008-05-01T00:00:00",687358.574364346102811,0.687359000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227018E58096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.979357438449483,58.100076999999999]
["glac_bound",383097.000000000000000,"G228021E58021N","2008-05-01T00:00:00",175353.721374459244544,0.175354000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228021E58021N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.975248879868502,58.020975500000006]
["glac_bound",383098.000000000000000,"G230288E56373N","2008-05-01T00:00:00",245762.396953356917948,0.245762000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230288E56373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.713150280687273,56.372869000000001]
["glac_bound",383099.000000000000000,"G221881E59906N","2008-05-01T00:00:00",1186264.922002010513097,1.186260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221881E59906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.118601863821368,59.906756500000000]
["glac_bound",383100.000000000000000,"G226389E58942N","2008-05-01T00:00:00",1650221.209036585642025,1.650220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226389E58942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.609206533515334,58.944775500000006]
["glac_bound",383101.000000000000000,"G230719E55295N","2008-05-01T00:00:00",2458662.510909745469689,2.458660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230719E55295N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.279645510370500,55.296093499999998]
["glac_bound",383102.000000000000000,"G230702E55389N","2008-05-01T00:00:00",132706.532924735802226,0.132707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230702E55389N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.297125007944175,55.389820499999999]
["glac_bound",383106.000000000000000,"G221738E59789N","2008-05-01T00:00:00",6834008.626509949564934,6.834010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221738E59789N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.238584348165489,59.784037499999997]
["glac_bound",383108.000000000000000,"G228469E57388N","2008-05-01T00:00:00",179308.144697398762219,0.179308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228469E57388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.530735817826127,57.387408499999999]
["glac_bound",383109.000000000000000,"G230397E57422N","2008-05-01T00:00:00",453858.817921202105936,0.453859000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230397E57422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.601787746257685,57.422134499999999]
["glac_bound",383112.000000000000000,"G230804E56471N","2008-05-01T00:00:00",738390.973001812817529,0.738391000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230804E56471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.194286731981975,56.475364499999998]
["glac_bound",383114.000000000000000,"G222209E59363N","2008-05-01T00:00:00",7469471.235036478377879,7.469470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222209E59363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.788468660373695,59.380317499999997]
["glac_bound",383121.000000000000000,"G224140E59969N","2008-05-01T00:00:00",88015.465956668485887,0.088015000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224140E59969N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.858929057976127,59.969775999999996]
["glac_bound",383122.000000000000000,"G223985E59760N","2008-05-01T00:00:00",228804.357674862927524,0.228804000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223985E59760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.016903854435839,59.760862500000002]
["glac_bound",383125.000000000000000,"G229488E57290N","2008-05-01T00:00:00",465982.214797208784148,0.465982000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229488E57290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.511366549797572,57.290698000000006]
["glac_bound",383137.000000000000000,"G229594E56228N","2008-05-01T00:00:00",1090599.400222149910405,1.090600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229594E56228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.406014278468263,56.229864499999998]
["glac_bound",383139.000000000000000,"G229224E56809N","2008-05-01T00:00:00",461455.363922131131403,0.461455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229224E56809N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.775480888714725,56.809486000000000]
["glac_bound",383140.000000000000000,"G224426E59852N","2008-05-01T00:00:00",593636.073242347920313,0.593636000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224426E59852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.574114495273989,59.851373500000001]
["glac_bound",383146.000000000000000,"G228104E58093N","2008-05-01T00:00:00",418042.788045956927817,0.418043000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228104E58093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.892137366147324,58.095153999999994]
["glac_bound",383148.000000000000000,"G229247E57149N","2008-05-01T00:00:00",1090334.053650908172131,1.090330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229247E57149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.755995113887309,57.149957999999998]
["glac_bound",383149.000000000000000,"G227438E58350N","2008-05-01T00:00:00",332428.299701563781127,0.332428000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227438E58350N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.563630405625418,58.353170499999997]
["glac_bound",383152.000000000000000,"G229062E56419N","2008-05-01T00:00:00",3836555.290415590163320,3.836560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229062E56419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.935782178209479,56.434141500000003]
["glac_bound",383153.000000000000000,"G223922E59769N","2008-05-01T00:00:00",119389.640282214197214,0.119390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223922E59769N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.079144767140974,59.767693999999999]
["glac_bound",383154.000000000000000,"G227526E57562N","2008-05-01T00:00:00",17226589.960418678820133,17.226600000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227526E57562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.474337307328398,57.559890499999995]
["glac_bound",383156.000000000000000,"G229363E57140N","2008-05-01T00:00:00",267336.402987483481411,0.267336000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229363E57140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.636409687779434,57.140802000000001]
["glac_bound",383160.000000000000000,"G229333E56938N","2008-05-01T00:00:00",635890.498563547269441,0.635890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229333E56938N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.667312458383606,56.938310500000000]
["glac_bound",383171.000000000000000,"G228011E57460N","2008-05-01T00:00:00",152320.582904359092936,0.152321000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228011E57460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.989968193847801,57.458967000000001]
["glac_bound",383173.000000000000000,"G227293E58271N","2008-05-01T00:00:00",360885.705066468683071,0.360886000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227293E58271N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.707558894475937,58.269444499999999]
["glac_bound",383178.000000000000000,"G227994E57621N","2008-05-01T00:00:00",544014.629224966047332,0.544015000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227994E57621N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.001608951692560,57.622857500000002]
["glac_bound",383181.000000000000000,"G231525E56100N","2008-05-01T00:00:00",74992.868762873084052,0.074993000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231525E56100N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.475536712569692,56.099809500000006]
["glac_bound",383182.000000000000000,"G226263E58624N","2008-05-01T00:00:00",312611.694782434380613,0.312612000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226263E58624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.737999303293464,58.623657999999999]
["glac_bound",383183.000000000000000,"G226469E58522N","2008-05-01T00:00:00",720318.223649605410174,0.720318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226469E58522N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.529207091233616,58.521450999999999]
["glac_bound",383190.000000000000000,"G228334E56788N","2008-05-01T00:00:00",2292508.502493080683053,2.292510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228334E56788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.660044546094014,56.786445499999999]
["glac_bound",383192.000000000000000,"G227229E58113N","2008-05-01T00:00:00",121104.773723203674308,0.121105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227229E58113N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.771307209785419,58.114599499999997]
["glac_bound",383193.000000000000000,"G230069E56106N","2008-05-01T00:00:00",311548.561702752311248,0.311549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230069E56106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.934599670814123,56.103805000000001]
["glac_bound",383195.000000000000000,"G228704E57399N","2008-05-01T00:00:00",93310.227669580592192,0.093310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228704E57399N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.295362715719079,57.398821999999996]
["glac_bound",383196.000000000000000,"G226964E58177N","2008-05-01T00:00:00",57951.933972932216420,0.057952000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226964E58177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.037206187851609,58.176346500000001]
["glac_bound",383200.000000000000000,"G230678E55656N","2008-05-01T00:00:00",237447.527990521106403,0.237448000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230678E55656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.325459039535247,55.655662000000000]
["glac_bound",383203.000000000000000,"G225639E59255N","2008-05-01T00:00:00",4303985.264639327302575,4.303990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225639E59255N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.350049975336503,59.260503499999999]
["glac_bound",383207.000000000000000,"G226570E58545N","2008-05-01T00:00:00",1629164.617390983039513,1.629160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226570E58545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.425429222773005,58.545811499999999]
["glac_bound",383209.000000000000000,"G225036E59494N","2008-05-01T00:00:00",87173.605929963407107,0.087174000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225036E59494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.965297058596690,59.493684000000002]
["glac_bound",383217.000000000000000,"G225430E59342N","2008-05-01T00:00:00",136209.176763622701401,0.136209000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225430E59342N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.568652035328114,59.343011500000003]
["glac_bound",383222.000000000000000,"G225249E59476N","2008-05-01T00:00:00",256758.203463600133546,0.256758000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225249E59476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.752359047567097,59.475489500000002]
["glac_bound",383229.000000000000000,"G226435E58906N","2008-05-01T00:00:00",53069.182221877883421,0.053069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226435E58906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.565307845238124,58.906402000000000]
["glac_bound",383230.000000000000000,"G230121E56327N","2008-05-01T00:00:00",174702.182261501933681,0.174702000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230121E56327N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.878495339386404,56.326430000000002]
["glac_bound",383235.000000000000000,"G223863E59728N","2008-05-01T00:00:00",111111.015243788730004,0.111111000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223863E59728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.141040639608775,59.729094000000003]
["glac_bound",383237.000000000000000,"G229505E56299N","2008-05-01T00:00:00",2319026.891523879021406,2.319030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229505E56299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.493138820283576,56.300245000000004]
["glac_bound",383239.000000000000000,"G221794E59945N","2008-05-01T00:00:00",84720.879834302439122,0.084721000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221794E59945N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.206240761081546,59.944694499999997]
["glac_bound",383241.000000000000000,"G227862E57476N","2008-05-01T00:00:00",65558.187193441961426,0.065558000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227862E57476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.140540997613357,57.476932500000004]
["glac_bound",383242.000000000000000,"G227662E57905N","2008-05-01T00:00:00",150116.233339321799576,0.150116000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227662E57905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.335759667974031,57.903357999999997]
["glac_bound",383255.000000000000000,"G225344E59431N","2008-05-01T00:00:00",62512.831920405034907,0.062513000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225344E59431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.656356657845578,59.431448500000002]
["glac_bound",383256.000000000000000,"G228693E56569N","2008-05-01T00:00:00",96636.821914902931894,0.096637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228693E56569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.307642082928169,56.569319999999998]
["glac_bound",383257.000000000000000,"G230458E56083N","2008-05-01T00:00:00",270433.360576499311719,0.270433000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230458E56083N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.538553734245966,56.081528499999997]
["glac_bound",383259.000000000000000,"G223217E59479N","2008-05-01T00:00:00",22510735.517017155885696,22.510700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223217E59479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.766553032037677,59.473967999999999]
["glac_bound",383260.000000000000000,"G230828E56526N","2008-05-01T00:00:00",240247.551907795335865,0.240248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230828E56526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.176435892923678,56.528091000000003]
["glac_bound",383267.000000000000000,"G226303E58613N","2008-05-01T00:00:00",478011.523710286535788,0.478012000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226303E58613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.697427171662156,58.616470499999998]
["glac_bound",383268.000000000000000,"G222678E59026N","2008-05-01T00:00:00",245195.121619513782207,0.245195000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222679E59027N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.320264917931127,59.026680999999996]
["glac_bound",383272.000000000000000,"G229288E56591N","2008-05-01T00:00:00",599200.652962885214947,0.599201000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229288E56591N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.702640537545449,56.588544999999996]
["glac_bound",383274.000000000000000,"G225902E59340N","2008-05-01T00:00:00",99293.035633730149129,0.099293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225902E59340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.098263978582622,59.339667000000006]
["glac_bound",383277.000000000000000,"G228662E57078N","2008-05-01T00:00:00",55292.431358531997830,0.055292000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228662E57078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.338847880927460,57.079161499999998]
["glac_bound",383278.000000000000000,"G228027E56833N","2008-05-01T00:00:00",339265.450809562869836,0.339265000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228027E56833N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.968246402536749,56.835027499999995]
["glac_bound",383282.000000000000000,"G230041E56069N","2008-05-01T00:00:00",2156178.216708829160780,2.156180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230041E56069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.960621795750853,56.078772999999998]
["glac_bound",383283.000000000000000,"G229464E56925N","2008-05-01T00:00:00",626851.524532860843465,0.626851000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229464E56925N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.536907546396321,56.926355999999998]
["glac_bound",383284.000000000000000,"G222061E59976N","2008-05-01T00:00:00",1157479.390476138330996,1.157480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222061E59976N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.944547185586998,59.976052000000003]
["glac_bound",383285.000000000000000,"G228348E56781N","2008-05-01T00:00:00",123306.859960284316912,0.123307000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228348E56781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.649499184451372,56.781936500000000]
["glac_bound",383291.000000000000000,"G230561E55323N","2008-05-01T00:00:00",195992.522816294920631,0.195993000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230561E55323N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.441830709075901,55.322867000000002]
["glac_bound",383296.000000000000000,"G227719E57946N","2008-05-01T00:00:00",214834.544908131501870,0.214835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227719E57946N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.280479578226391,57.945971499999999]
["glac_bound",383305.000000000000000,"G227883E57790N","2008-05-01T00:00:00",743734.204664059448987,0.743734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227883E57790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.122591339584062,57.791396499999998]
["glac_bound",383309.000000000000000,"G228116E56927N","2008-05-01T00:00:00",1005282.492974792490713,1.005280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228116E56927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.891484620149242,56.932199999999995]
["glac_bound",383312.000000000000000,"G223661E59573N","2008-05-01T00:00:00",148028.976040037581697,0.148029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223661E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.335538131896783,59.570712499999999]
["glac_bound",383320.000000000000000,"G222390E59304N","2008-05-01T00:00:00",1206971.637329643359408,1.206970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222390E59304N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.619702731178904,59.308277000000004]
["glac_bound",383321.000000000000000,"G222432E59858N","2008-05-01T00:00:00",78538.866741769845248,0.078539000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222432E59858N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.568412953331233,59.858716500000000]
["glac_bound",383322.000000000000000,"G228370E57433N","2008-05-01T00:00:00",259160.226720213977387,0.259160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228370E57433N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.634578342554761,57.430558500000004]
["glac_bound",383324.000000000000000,"G225536E59448N","2008-05-01T00:00:00",383028.658261617296375,0.383029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225536E59448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.463176234967790,59.447570499999998]
["glac_bound",383329.000000000000000,"G223426E59503N","2008-05-01T00:00:00",3531078.484208198729903,3.531080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223426E59503N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.562058512332726,59.507768499999997]
["glac_bound",383336.000000000000000,"G222049E59527N","2008-05-01T00:00:00",177154.709259512863355,0.177155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222049E59527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.950654931597740,59.526488000000001]
["glac_bound",383337.000000000000000,"G222149E59705N","2008-05-01T00:00:00",845021.088340996881016,0.845021000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222149E59705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.849886541394369,59.705105000000003]
["glac_bound",383339.000000000000000,"G226599E58364N","2008-05-01T00:00:00",732195.628170785028487,0.732196000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226599E58364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.396981297909690,58.362236500000002]
["glac_bound",383343.000000000000000,"G222282E59558N","2008-05-01T00:00:00",587407.250348097761162,0.587407000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222282E59558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.705827919203728,59.553695000000005]
["glac_bound",383350.000000000000000,"G230826E57322N","2008-05-01T00:00:00",523636.873599557904527,0.523637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230826E57322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.178101692501002,57.322773999999995]
["glac_bound",383353.000000000000000,"G224156E59780N","2008-05-01T00:00:00",215730.331899023352889,0.215730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224156E59780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.847192243589745,59.779054500000001]
["glac_bound",383357.000000000000000,"G227226E58300N","2008-05-01T00:00:00",594468.796677184291184,0.594469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227226E58300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.773652283004566,58.299641000000001]
["glac_bound",383359.000000000000000,"G224193E59796N","2008-05-01T00:00:00",27026778.281399603933096,27.026800000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224193E59796N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.822941608380745,59.817006499999998]
["glac_bound",383360.000000000000000,"G230119E56308N","2008-05-01T00:00:00",58779.730130733907572,0.058780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230119E56308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.881482372542564,56.308652500000001]
["glac_bound",383365.000000000000000,"G229603E56457N","2008-05-01T00:00:00",72340.092537109376281,0.072340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229603E56457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.395527393228008,56.458746500000004]
["glac_bound",383367.000000000000000,"G226457E58708N","2008-05-01T00:00:00",62578.346069539940800,0.062578000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226457E58708N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.544231289303866,58.708388999999997]
["glac_bound",383370.000000000000000,"G226302E58723N","2008-05-01T00:00:00",1161362.877738688141108,1.161360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226302E58723N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.690116920031755,58.722937999999999]
["glac_bound",383374.000000000000000,"G230740E55669N","2008-05-01T00:00:00",195486.161172789550619,0.195486000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230740E55669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.262212977895047,55.669923999999995]
["glac_bound",383378.000000000000000,"G230887E56946N","2008-05-01T00:00:00",501549.927207582048140,0.501550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230887E56946N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.113539384483317,56.947182999999995]
["glac_bound",383379.000000000000000,"G223239E59565N","2008-05-01T00:00:00",92800.927817703282926,0.092801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223239E59565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.761987420693288,59.564159500000002]
["glac_bound",383385.000000000000000,"G230047E55771N","2008-05-01T00:00:00",864188.685682471957989,0.864189000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230047E55771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.960882595308078,55.772030000000001]
["glac_bound",383386.000000000000000,"G229501E56707N","2008-05-01T00:00:00",474094.027429711597506,0.474094000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229501E56707N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.498106329320024,56.706795000000000]
["glac_bound",383387.000000000000000,"G229506E57123N","2008-05-01T00:00:00",6038258.374972678720951,6.038260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229506E57123N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.487649731518957,57.133810499999996]
["glac_bound",383396.000000000000000,"G222606E59070N","2008-05-01T00:00:00",847521.574983291095123,0.847522000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222606E59070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.392627960167715,59.070710000000005]
["glac_bound",383399.000000000000000,"G230479E56619N","2008-05-01T00:00:00",376817.190905736817513,0.376817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230479E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.523055351174293,56.619784999999993]
["glac_bound",383404.000000000000000,"G230295E54856N","2008-05-01T00:00:00",212765.279058483749395,0.212765000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230295E54856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.704874246214956,54.856762000000003]
["glac_bound",383409.000000000000000,"G222365E59815N","2008-05-01T00:00:00",17734477.959443148225546,17.734500000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222365E59815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.638547026595717,59.842033999999998]
["glac_bound",383410.000000000000000,"G226381E58828N","2008-05-01T00:00:00",1089535.598769315285608,1.089540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226381E58828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.617595327875250,58.828689499999996]
["glac_bound",383417.000000000000000,"G227224E58078N","2008-05-01T00:00:00",786891.289599955547601,0.786891000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227224E58078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.777583514478920,58.080389499999995]
["glac_bound",383424.000000000000000,"G228054E57308N","2008-05-01T00:00:00",385707.939861171471421,0.385708000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228054E57308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.942840685503143,57.307842500000000]
["glac_bound",383426.000000000000000,"G230535E57064N","2008-05-01T00:00:00",431467.006369222537614,0.431467000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230535E57064N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463944772646812,57.065482500000002]
["glac_bound",383434.000000000000000,"G226890E58234N","2008-05-01T00:00:00",366427.346610538312234,0.366427000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226890E58234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.112921082825011,58.231940000000002]
["glac_bound",383436.000000000000000,"G224141E59865N","2008-05-01T00:00:00",1087927.546988059300929,1.087930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224141E59865N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.862362470192295,59.870159000000001]
["glac_bound",383443.000000000000000,"G225447E59541N","2008-05-01T00:00:00",251934.933643816504627,0.251935000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225447E59541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.554002469753357,59.541303999999997]
["glac_bound",383450.000000000000000,"G230471E55990N","2008-05-01T00:00:00",66086.799122819502372,0.066087000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230471E55990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.528499278808994,55.990891500000004]
["glac_bound",383452.000000000000000,"G227698E57579N","2008-05-01T00:00:00",149450.686853366409196,0.149451000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227698E57579N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.298664648492888,57.578876500000000]
["glac_bound",383453.000000000000000,"G221829E59782N","2008-05-01T00:00:00",196863.740493800811237,0.196864000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221829E59782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.172758240489372,59.782372000000002]
["glac_bound",383457.000000000000000,"G221805E59608N","2008-05-01T00:00:00",504800.208203053800389,0.504800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221805E59608N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.193930475979244,59.611560500000003]
["glac_bound",383459.000000000000000,"G230302E57514N","2008-05-01T00:00:00",74456.277061514469096,0.074456000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230302E57514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.698388254129100,57.513869999999997]
["glac_bound",383462.000000000000000,"G225683E59249N","2008-05-01T00:00:00",952010.471618899144232,0.952010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225683E59249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.319871911389100,59.251571499999997]
["glac_bound",383463.000000000000000,"G229322E56508N","2008-05-01T00:00:00",1373093.735375988529995,1.373090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229322E56508N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.682408557137876,56.515478999999999]
["glac_bound",383465.000000000000000,"G226755E58451N","2008-05-01T00:00:00",710731.933612417313270,0.710732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226755E58451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.246374691583270,58.451117500000002]
["glac_bound",383466.000000000000000,"G227232E58326N","2008-05-01T00:00:00",371326.699965166859329,0.371327000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227232E58326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.765611448233869,58.328018999999998]
["glac_bound",383469.000000000000000,"G230594E55203N","2008-05-01T00:00:00",419975.280574899748899,0.419975000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230594E55203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.403580988526301,55.202050499999999]
["glac_bound",383472.000000000000000,"G228671E56581N","2008-05-01T00:00:00",924857.450523957028054,0.924857000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228671E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.333458687302027,56.582389499999998]
["glac_bound",383473.000000000000000,"G228761E57293N","2008-05-01T00:00:00",1083939.188992810435593,1.083940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228761E57293N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.238280920269574,57.294724000000002]
["glac_bound",383474.000000000000000,"G228891E57306N","2008-05-01T00:00:00",279147.174090909189545,0.279147000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228891E57306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.109678346793714,57.305650499999999]
["glac_bound",383478.000000000000000,"G230392E55625N","2008-05-01T00:00:00",235088.652016074542189,0.235089000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230392E55625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.612732673819295,55.625534999999999]
["glac_bound",383481.000000000000000,"G231080E57441N","2008-05-01T00:00:00",129404.760554272565059,0.129405000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231080E57441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.919325082801464,57.442084500000000]
["glac_bound",383485.000000000000000,"G224191E59782N","2008-05-01T00:00:00",722777.512487171799876,0.722777000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224191E59782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.812270097413773,59.781711999999999]
["glac_bound",383486.000000000000000,"G228136E56884N","2008-05-01T00:00:00",2471209.363225606270134,2.471210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228136E56884N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.865371527266007,56.883189000000002]
["glac_bound",383487.000000000000000,"G230291E54485N","2008-05-01T00:00:00",402984.670926625374705,0.402985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230291E54485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.715144235952380,54.486905499999999]
["glac_bound",383489.000000000000000,"G230021E56508N","2008-05-01T00:00:00",499626.755323699850123,0.499627000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230021E56508N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.980153042094855,56.507508000000001]
["glac_bound",383494.000000000000000,"G230553E57004N","2008-05-01T00:00:00",703155.084100991836749,0.703155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230553E57004N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.446876788461537,57.006791000000000]
["glac_bound",383496.000000000000000,"G227197E58400N","2008-05-01T00:00:00",220081.768327041500015,0.220082000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227197E58400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.802152853038848,58.400051000000005]
["glac_bound",383500.000000000000000,"G230086E55387N","2008-05-01T00:00:00",381136.816645736165810,0.381137000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230086E55387N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.914625872153579,55.387568999999999]
["glac_bound",383502.000000000000000,"G222767E59342N","2008-05-01T00:00:00",7788113.643625858239830,7.788110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222767E59342N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.229514546057771,59.342713000000003]
["glac_bound",383503.000000000000000,"G225730E59271N","2008-05-01T00:00:00",210135.495393375051208,0.210135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225730E59271N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.268746995481393,59.272519000000003]
["glac_bound",383504.000000000000000,"G227875E57468N","2008-05-01T00:00:00",1425146.231271799653769,1.425150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227875E57468N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.125630698641771,57.472827000000002]
["glac_bound",383510.000000000000000,"G230448E56622N","2008-05-01T00:00:00",116503.079378536422155,0.116503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230448E56622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.552149585820985,56.621190499999997]
["glac_bound",383515.000000000000000,"G223192E59534N","2008-05-01T00:00:00",300282.600472715508658,0.300283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223192E59534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.808412614452550,59.535235000000000]
["glac_bound",383518.000000000000000,"G221941E59548N","2008-05-01T00:00:00",1200130.808889508480206,1.200130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221941E59548N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.062278449814158,59.542507999999998]
["glac_bound",383521.000000000000000,"G230457E54717N","2008-05-01T00:00:00",527444.886105506331660,0.527445000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230457E54717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.546327791632820,54.716464500000001]
["glac_bound",383522.000000000000000,"G222450E59552N","2008-05-01T00:00:00",725356.188009759294800,0.725356000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222450E59552N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.546354885464041,59.551465499999999]
["glac_bound",383527.000000000000000,"G229690E56262N","2008-05-01T00:00:00",310601.381259935558774,0.310601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229690E56262N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.308248992039012,56.261646499999998]
["glac_bound",383532.000000000000000,"G230267E56333N","2008-05-01T00:00:00",369628.607910573191475,0.369629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230267E56333N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.731241336485681,56.331711999999996]
["glac_bound",383537.000000000000000,"G230144E56187N","2008-05-01T00:00:00",3164265.210034635383636,3.164270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230144E56187N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.851804360076244,56.185243999999997]
["glac_bound",383542.000000000000000,"G225792E59120N","2008-05-01T00:00:00",417059.747773165523540,0.417060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225792E59120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.209572589523106,59.121962999999994]
["glac_bound",383544.000000000000000,"G230130E55621N","2008-05-01T00:00:00",149507.254591583885485,0.149507000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230130E55621N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.872027725223461,55.621682499999999]
["glac_bound",383547.000000000000000,"G228588E57561N","2008-05-01T00:00:00",1925432.390811966033652,1.925430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228588E57561N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.415048808236577,57.562661000000006]
["glac_bound",383553.000000000000000,"G227512E58368N","2008-05-01T00:00:00",804130.926004217937589,0.804131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227512E58368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.484341541210142,58.370755500000001]
["glac_bound",383557.000000000000000,"G228523E57091N","2008-05-01T00:00:00",154147.522584036167245,0.154148000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228523E57091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.477600181551566,57.090959999999995]
["glac_bound",383562.000000000000000,"G229046E56656N","2008-05-01T00:00:00",268777.631392763694748,0.268778000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229046E56656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.952642015530216,56.656610499999999]
["glac_bound",383564.000000000000000,"G229171E56521N","2008-05-01T00:00:00",947379.556757599231787,0.947380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229171E56521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.833278256126448,56.521947500000003]
["glac_bound",383566.000000000000000,"G229083E56749N","2008-05-01T00:00:00",353290.565374141442589,0.353291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229083E56749N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.920314701605548,56.749871499999998]
["glac_bound",383567.000000000000000,"G226854E58287N","2008-05-01T00:00:00",713924.317745374282822,0.713924000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226854E58287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.145290760205796,58.288220500000001]
["glac_bound",383570.000000000000000,"G230837E57296N","2008-05-01T00:00:00",4906498.597298816777766,4.906500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230837E57296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.167203552793154,57.301108499999998]
["glac_bound",383571.000000000000000,"G228660E56576N","2008-05-01T00:00:00",114850.773511648920248,0.114851000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228660E56576N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.342086038834964,56.574847000000005]
["glac_bound",383574.000000000000000,"G230284E57443N","2008-05-01T00:00:00",329452.504859419947024,0.329453000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230284E57443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.713215952423468,57.445107500000006]
["glac_bound",383587.000000000000000,"G228118E56745N","2008-05-01T00:00:00",200539.400106826244155,0.200539000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228118E56745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.882830305926547,56.747940000000000]
["glac_bound",383592.000000000000000,"G225274E59394N","2008-05-01T00:00:00",924391.629138382617384,0.924392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225274E59394N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.729700824585620,59.394272500000000]
["glac_bound",383594.000000000000000,"G223150E59675N","2008-05-01T00:00:00",1362805.215208225883543,1.362810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223150E59675N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.857237759912977,59.670479999999998]
["glac_bound",383599.000000000000000,"G230180E55990N","2008-05-01T00:00:00",1502522.941857298603281,1.502520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230180E55990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.818315298848120,55.990565500000002]
["glac_bound",383600.000000000000000,"G225741E59153N","2008-05-01T00:00:00",1680139.298804488498718,1.680140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225741E59153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.261592269253043,59.153480000000002]
["glac_bound",383602.000000000000000,"G222097E59071N","2008-05-01T00:00:00",342591.133092279371340,0.342591000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Grand Plateau Glacier","None","08BF222428E59003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.572169275340912,59.002483499999997]
["glac_bound",383603.000000000000000,"G223007E59114N","2008-05-01T00:00:00",493059.800703808548860,0.493060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223007E59114N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.994053802416431,59.113789499999996]
["glac_bound",383608.000000000000000,"G228037E57824N","2008-05-01T00:00:00",192805.391375749342842,0.192805000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228037E57824N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.965343765556042,57.825032500000006]
["glac_bound",383613.000000000000000,"G223143E59545N","2008-05-01T00:00:00",320922.876198515587021,0.320923000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223143E59545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.858065024265443,59.545029999999997]
["glac_bound",383616.000000000000000,"G221751E59998N","2008-05-01T00:00:00",1430163.117247764021158,1.430160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221751E59998N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.248459189427308,59.998326500000005]
["glac_bound",383618.000000000000000,"G223554E59988N","2008-05-01T00:00:00",102165.697550986267743,0.102166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223554E59988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.445828721204180,59.987634999999997]
["glac_bound",383619.000000000000000,"G229003E56455N","2008-05-01T00:00:00",354032.186189620464575,0.354032000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG229003E56455N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.997942195892222,56.454970500000002]
["glac_bound",383620.000000000000000,"G224770E59787N","2008-05-01T00:00:00",421563.451810399652459,0.421563000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224770E59787N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.230115962137575,59.786884000000001]
["glac_bound",383623.000000000000000,"G228571E57294N","2008-05-01T00:00:00",371123.039611317508388,0.371123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228571E57294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.431333299039665,57.297328500000006]
["glac_bound",383624.000000000000000,"G224528E59871N","2008-05-01T00:00:00",503605.379011582874227,0.503605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224528E59871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.472347024833113,59.871628000000001]
["glac_bound",383629.000000000000000,"G222503E59635N","2008-05-01T00:00:00",287667.671791685977951,0.287668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222503E59635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.497234730352773,59.634996000000001]
["glac_bound",383630.000000000000000,"G226922E58043N","2008-05-01T00:00:00",32646751.780275989323854,32.646799999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226922E58043N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.093321954945282,58.033193999999995]
["glac_bound",383631.000000000000000,"G228429E57440N","2008-05-01T00:00:00",139391.668066523241578,0.139392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228429E57440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.569737722543664,57.439960999999997]
["glac_bound",383635.000000000000000,"G229828E56620N","2008-05-01T00:00:00",1648202.813490271102637,1.648200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229828E56620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.175419538848587,56.615975000000006]
["glac_bound",383636.000000000000000,"G222979E59358N","2008-05-01T00:00:00",790363.227688060724176,0.790363000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222979E59358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.017166370327601,59.358137499999998]
["glac_bound",383645.000000000000000,"G228598E56602N","2008-05-01T00:00:00",2609344.313866736367345,2.609340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228598E56602N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.412990098098021,56.611421000000000]
["glac_bound",383648.000000000000000,"G230611E56894N","2008-05-01T00:00:00",99972.042390145405079,0.099972000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230611E56894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.388278053179050,56.894053999999997]
["glac_bound",383652.000000000000000,"G228996E57416N","2008-05-01T00:00:00",156733.468500139191747,0.156733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228996E57416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.003411538971818,57.415041500000001]
["glac_bound",383657.000000000000000,"G229319E57422N","2008-05-01T00:00:00",312696.240490414260421,0.312696000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229319E57422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.679754405365259,57.422168499999998]
["glac_bound",383665.000000000000000,"G228613E57465N","2008-05-01T00:00:00",6438483.973617642186582,6.438480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228613E57465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.383435896471241,57.471158500000001]
["glac_bound",383671.000000000000000,"G230568E54979N","2008-05-01T00:00:00",106507.974552325264085,0.106508000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230568E54979N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.430164199441805,54.978866500000002]
["glac_bound",383677.000000000000000,"G229886E56185N","2008-05-01T00:00:00",6277127.544134734198451,6.277130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229886E56185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.113978213364959,56.205577000000005]
["glac_bound",383682.000000000000000,"G230273E56367N","2008-05-01T00:00:00",152493.253661150811240,0.152493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230273E56367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.726670828016438,56.368294500000005]
["glac_bound",383689.000000000000000,"G228084E58047N","2008-05-01T00:00:00",351434.612595429993235,0.351435000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228084E58047N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.917886641733617,58.048058500000003]
["glac_bound",383691.000000000000000,"G228860E57280N","2008-05-01T00:00:00",15463267.662696605548263,15.463300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228860E57280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.148295829825997,57.292240000000000]
["glac_bound",383693.000000000000000,"G230418E55175N","2008-05-01T00:00:00",762939.241508372826502,0.762939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230418E55175N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.582685640879816,55.174828500000004]
["glac_bound",383696.000000000000000,"G230492E56215N","2008-05-01T00:00:00",225244.845773874345468,0.225245000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230492E56215N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.507173703506993,56.215032500000000]
["glac_bound",383698.000000000000000,"G227277E58217N","2008-05-01T00:00:00",208853.500261563633103,0.208853000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227277E58217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.723084040404046,58.216782000000002]
["glac_bound",383699.000000000000000,"G225189E59281N","2008-05-01T00:00:00",1332890.105689464369789,1.332890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225189E59281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.810962300759655,59.281115499999999]
["glac_bound",383701.000000000000000,"G223580E59865N","2008-05-01T00:00:00",1865815.091192328371108,1.865820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223580E59865N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.417329627645501,59.864255000000000]
["glac_bound",383702.000000000000000,"G229995E57099N","2008-05-01T00:00:00",3052637.792875576298684,3.052640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229995E57099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.004955160915415,57.098278499999999]
["glac_bound",383703.000000000000000,"G228961E56454N","2008-05-01T00:00:00",730181.359891426516697,0.730181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228961E56454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.041007675467625,56.456924999999998]
["glac_bound",383704.000000000000000,"G229653E56260N","2008-05-01T00:00:00",3598932.649128178600222,3.598930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229653E56260N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.349065595614888,56.272797499999996]
["glac_bound",383706.000000000000000,"G227967E57610N","2008-05-01T00:00:00",585602.006082836654969,0.585602000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227967E57610N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.032715917274061,57.614136500000001]
["glac_bound",383716.000000000000000,"G224717E59737N","2008-05-01T00:00:00",290610.070277848804835,0.290610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224717E59737N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.281784056627316,59.737658499999995]
["glac_bound",383717.000000000000000,"G228012E57230N","2008-05-01T00:00:00",1873042.935547687113285,1.873040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228012E57230N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.986788325289695,57.227519000000001]
["glac_bound",383718.000000000000000,"G223860E59932N","2008-05-01T00:00:00",1960649.613576127449051,1.960650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223860E59932N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.137847781967480,59.932246000000006]
["glac_bound",383719.000000000000000,"G230464E56620N","2008-05-01T00:00:00",1284147.340152307646349,1.284150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230464E56620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.534198326777243,56.618449999999996]
["glac_bound",383732.000000000000000,"G229389E56273N","2008-05-01T00:00:00",565045.113046399550512,0.565045000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229389E56273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.611149531039132,56.273457999999998]
["glac_bound",383734.000000000000000,"G229878E56584N","2008-05-01T00:00:00",839532.799525459646247,0.839533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229878E56584N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.124917852525641,56.583450499999998]
["glac_bound",383736.000000000000000,"G225811E59476N","2008-05-01T00:00:00",76559.924237889950746,0.076560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225811E59476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.189696790747689,59.475937500000001]
["glac_bound",383739.000000000000000,"G230125E55605N","2008-05-01T00:00:00",287927.533472092531156,0.287928000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230125E55605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.874693027898672,55.604956000000001]
["glac_bound",383741.000000000000000,"G230431E55227N","2008-05-01T00:00:00",199115.572655728989048,0.199116000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230431E55227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.569510235313913,55.227154499999997]
["glac_bound",383746.000000000000000,"G229216E57236N","2008-05-01T00:00:00",183909.229088640131522,0.183909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229216E57236N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.790190073922133,57.237480000000005]
["glac_bound",383748.000000000000000,"G226834E58385N","2008-05-01T00:00:00",65325.494469256620505,0.065325000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226834E58385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.165188553431392,58.384716999999995]
["glac_bound",383751.000000000000000,"G227862E57395N","2008-05-01T00:00:00",28268681.160251583904028,28.268699999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Pendant Glacier","None","08CE227862E57395N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.145152118313803,57.392866499999997]
["glac_bound",383756.000000000000000,"G229364E56570N","2008-05-01T00:00:00",70658.510260068083880,0.070658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229364E56570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.633782573623137,56.569336000000000]
["glac_bound",383757.000000000000000,"G224973E59352N","2008-05-01T00:00:00",10700.191138555710495,0.010700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224973E59352N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.026960689443911,59.352261499999997]
["glac_bound",383763.000000000000000,"G229980E56573N","2008-05-01T00:00:00",82680.428382278449135,0.082680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229980E56573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.019374714000008,56.572595500000006]
["glac_bound",383769.000000000000000,"G230031E57360N","2008-05-01T00:00:00",112048.777981212013401,0.112049000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230031E57360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.969097771428579,57.359741000000000]
["glac_bound",383777.000000000000000,"G228464E57144N","2008-05-01T00:00:00",203549.972705914318794,0.203550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228464E57144N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.536212177332743,57.144658000000000]
["glac_bound",383780.000000000000000,"G230621E55219N","2008-05-01T00:00:00",511308.462753452011384,0.511308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230621E55219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.376579802471838,55.218501000000003]
["glac_bound",383781.000000000000000,"G222246E59739N","2008-05-01T00:00:00",436184.098139452922624,0.436184000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222246E59739N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.755925070289265,59.739134499999999]
["glac_bound",383785.000000000000000,"G228078E57559N","2008-05-01T00:00:00",710449.338614032720216,0.710449000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228078E57559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.918652351758794,57.560870500000000]
["glac_bound",383797.000000000000000,"G230500E55181N","2008-05-01T00:00:00",234825.788618419377599,0.234826000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230500E55181N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.499431383968556,55.180910500000003]
["glac_bound",383799.000000000000000,"G227288E58277N","2008-05-01T00:00:00",883187.682761062635109,0.883188000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227288E58277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.707683401202644,58.279727500000000]
["glac_bound",383804.000000000000000,"G225014E59492N","2008-05-01T00:00:00",2114462.130284415557981,2.114460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225014E59492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.989597272894230,59.494725000000003]
["glac_bound",383805.000000000000000,"G230397E56022N","2008-05-01T00:00:00",18911970.427824024111032,18.911999999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230397E56022N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.658659436190078,56.026302500000000]
["glac_bound",383809.000000000000000,"G224014E59758N","2008-05-01T00:00:00",84289.723434363724664,0.084290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224014E59758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.987620720988218,59.758458000000005]
["glac_bound",383818.000000000000000,"G225821E59173N","2008-05-01T00:00:00",140755.334396691381698,0.140755000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225821E59173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.179548768077609,59.172382999999996]
["glac_bound",383819.000000000000000,"G233032E57747N","2008-05-01T00:00:00",158646.808722631307319,0.158647000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233032E57747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.968937665366155,57.747387500000002]
["glac_bound",383821.000000000000000,"G230094E56875N","2008-05-01T00:00:00",60601.784270366988494,0.060602000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230094E56875N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.905218951883000,56.875241000000003]
["glac_bound",383822.000000000000000,"G230805E55341N","2008-05-01T00:00:00",2169938.643191184848547,2.169940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230805E55341N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.197416061978515,55.342343000000000]
["glac_bound",383828.000000000000000,"G230003E56504N","2008-05-01T00:00:00",165461.558488923416007,0.165462000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230003E56504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.994495838973876,56.503522000000004]
["glac_bound",383831.000000000000000,"G224021E59733N","2008-05-01T00:00:00",59783.772005120772519,0.059784000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224021E59733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.978752646103658,59.732740000000000]
["glac_bound",383834.000000000000000,"G227118E58459N","2008-05-01T00:00:00",3316531.421542336698622,3.316530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227118E58459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.896026805442204,58.463769999999997]
["glac_bound",383844.000000000000000,"G229391E56618N","2008-05-01T00:00:00",424317.947818045737222,0.424318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229391E56618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.606643253147013,56.617337500000005]
["glac_bound",383846.000000000000000,"G229129E56551N","2008-05-01T00:00:00",1313488.230801267782226,1.313490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229129E56551N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.878594220351005,56.556017500000003]
["glac_bound",383853.000000000000000,"G230561E54730N","2008-05-01T00:00:00",2590109.578089068643749,2.590110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230561E54730N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.436028551851848,54.731043000000000]
["glac_bound",383855.000000000000000,"G230662E55646N","2008-05-01T00:00:00",1515587.343864539405331,1.515590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230662E55646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.338187119622376,55.646360999999999]
["glac_bound",383856.000000000000000,"G224216E59906N","2008-05-01T00:00:00",421439.043499637919012,0.421439000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224216E59906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.783584887124732,59.905929999999998]
["glac_bound",383860.000000000000000,"G222291E59561N","2008-05-01T00:00:00",3608660.558126981835812,3.608660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222291E59561N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.720180765915501,59.568576499999999]
["glac_bound",383866.000000000000000,"G224049E59741N","2008-05-01T00:00:00",548675.139710206654854,0.548675000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224049E59741N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.953983541730622,59.742161499999995]
["glac_bound",383868.000000000000000,"G230232E57444N","2008-05-01T00:00:00",1160824.580491875996813,1.160820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230232E57444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.771086624538498,57.444268000000001]
["glac_bound",383873.000000000000000,"G230540E56262N","2008-05-01T00:00:00",168888.747001435549464,0.168889000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230540E56262N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.459050089341872,56.262459500000006]
["glac_bound",383874.000000000000000,"G226083E58745N","2008-05-01T00:00:00",223842.019175087101758,0.223842000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226083E58745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.917680307548778,58.746240499999999]
["glac_bound",383884.000000000000000,"G227122E58236N","2008-05-01T00:00:00",153783.530315241834614,0.153784000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227122E58236N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.875846490582660,58.235924999999995]
["glac_bound",383886.000000000000000,"G228007E56838N","2008-05-01T00:00:00",37648.894269213225925,0.037649000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228007E56838N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.994022696916204,56.837119999999999]
["glac_bound",383889.000000000000000,"G229388E57610N","2008-05-01T00:00:00",345985.227542239474133,0.345985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229388E57610N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.612288734068613,57.609741499999998]
["glac_bound",383890.000000000000000,"G230106E55930N","2008-05-01T00:00:00",73090.371407188809826,0.073090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230106E55930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.893096180798551,55.929939500000003]
["glac_bound",383891.000000000000000,"G227461E58090N","2008-05-01T00:00:00",69798.347165940504055,0.069798000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227461E58090N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.539643245575235,58.089457499999995]
["glac_bound",383892.000000000000000,"G229083E56962N","2008-05-01T00:00:00",3428743.429596360307187,3.428740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229083E56962N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.914302098717940,56.962772999999999]
["glac_bound",383893.000000000000000,"G225615E59370N","2008-05-01T00:00:00",109387.688786784943659,0.109388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225615E59370N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.384339026118056,59.370134000000000]
["glac_bound",383895.000000000000000,"G221852E59543N","2008-05-01T00:00:00",264898.238143299473450,0.264898000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221852E59543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.147533040705440,59.543341499999997]
["glac_bound",383896.000000000000000,"G229511E56729N","2008-05-01T00:00:00",1609192.233059971826151,1.609190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229511E56729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.490050962260455,56.726723500000006]
["glac_bound",383898.000000000000000,"G227675E57860N","2008-05-01T00:00:00",2617598.598116465378553,2.617600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227675E57860N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.317239028908574,57.861824499999997]
["glac_bound",383901.000000000000000,"G229577E56299N","2008-05-01T00:00:00",474040.605871531879529,0.474041000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229577E56299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.424243947665673,56.300097000000001]
["glac_bound",383905.000000000000000,"G223873E59972N","2008-05-01T00:00:00",163329.263653443427756,0.163329000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223873E59972N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.126202313292197,59.971761999999998]
["glac_bound",383909.000000000000000,"G224971E59506N","2008-05-01T00:00:00",1594070.427415961399674,1.594070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224971E59506N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.039292095481642,59.509563000000000]
["glac_bound",383910.000000000000000,"G225503E59318N","2008-05-01T00:00:00",2499796.452979555819184,2.499800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225503E59318N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.500112337303875,59.320090000000000]
["glac_bound",383911.000000000000000,"G230673E55576N","2008-05-01T00:00:00",875149.112283078604378,0.875149000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230673E55576N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.326655532875293,55.575371000000004]
["glac_bound",383917.000000000000000,"G223040E59540N","2008-05-01T00:00:00",3096855.178195541724563,3.096860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223040E59540N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.961109524400911,59.540813000000000]
["glac_bound",383921.000000000000000,"G226196E58947N","2008-05-01T00:00:00",3466579.181953274644911,3.466580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226196E58947N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.797031866599923,58.942617999999996]
["glac_bound",383924.000000000000000,"G222254E59702N","2008-05-01T00:00:00",1779536.888864942826331,1.779540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222254E59702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.738998660754362,59.700944000000000]
["glac_bound",383934.000000000000000,"G229157E57179N","2008-05-01T00:00:00",59938.508873231396137,0.059938000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229157E57179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.843473988350411,57.178556999999998]
["glac_bound",383937.000000000000000,"G222623E59193N","2008-05-01T00:00:00",549705.587207652628422,0.549706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222623E59193N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.375191357132934,59.198293499999998]
["glac_bound",383938.000000000000000,"G227454E58004N","2008-05-01T00:00:00",33052677.408007111400366,33.052700000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Cheja South Glacier","None","08BC227454E58004N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.577507485331864,58.038180499999996]
["glac_bound",383940.000000000000000,"G229405E57220N","2008-05-01T00:00:00",203567.510001682676375,0.203568000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229405E57220N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.592636055351647,57.221548499999997]
["glac_bound",383942.000000000000000,"G230503E56372N","2008-05-01T00:00:00",89702.606158912647516,0.089703000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230503E56372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.497001733959735,56.371895000000002]
["glac_bound",383945.000000000000000,"G227284E58500N","2008-05-01T00:00:00",415817.092689097393304,0.415817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227284E58500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.715664395190629,58.500800499999997]
["glac_bound",383946.000000000000000,"G226594E58629N","2008-05-01T00:00:00",244986.393343162286328,0.244986000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226594E58629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.407999559657213,58.629512000000005]
["glac_bound",383951.000000000000000,"G222246E59567N","2008-05-01T00:00:00",1205031.223277847282588,1.205030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222246E59567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.758889192442950,59.566862000000000]
["glac_bound",383953.000000000000000,"G231476E56089N","2008-05-01T00:00:00",327212.052919498295523,0.327212000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231476E56089N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.524229603543091,56.088941500000004]
["glac_bound",383956.000000000000000,"G228439E56839N","2008-05-01T00:00:00",66580.739675780379912,0.066581000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228439E56839N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.560421119216414,56.839238999999999]
["glac_bound",383957.000000000000000,"G230135E56524N","2008-05-01T00:00:00",82650.832392962562153,0.082651000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230135E56524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.865058617638567,56.523392999999999]
["glac_bound",383959.000000000000000,"G228436E57442N","2008-05-01T00:00:00",2807783.927597403526306,2.807780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228436E57442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.558774183941807,57.447013999999996]
["glac_bound",383967.000000000000000,"G229126E56596N","2008-05-01T00:00:00",54887.231064182633418,0.054887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229126E56596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.873418106956734,56.596021499999999]
["glac_bound",383970.000000000000000,"G230308E56291N","2008-05-01T00:00:00",1384058.959018543129787,1.384060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230308E56291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.692193210181671,56.290510499999996]
["glac_bound",383976.000000000000000,"G222987E59127N","2008-05-01T00:00:00",308508.229441339557525,0.308508000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222987E59127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.013079120014879,59.126680000000000]
["glac_bound",383978.000000000000000,"G226559E58788N","2008-05-01T00:00:00",171657.390052692848258,0.171657000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226559E58788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.442690929025730,58.788489499999997]
["glac_bound",383981.000000000000000,"G228743E56598N","2008-05-01T00:00:00",1802176.045359790790826,1.802180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228743E56598N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.258445065901810,56.603922999999995]
["glac_bound",383983.000000000000000,"G222526E59805N","2008-05-01T00:00:00",53659.082641433953540,0.053659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222526E59805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.473615196916199,59.806536999999999]
["glac_bound",383984.000000000000000,"G228876E57015N","2008-05-01T00:00:00",3467606.057571130339056,3.467610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228876E57015N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.119904411282477,57.019019999999998]
["glac_bound",383990.000000000000000,"G229230E56617N","2008-05-01T00:00:00",60113.858672458765795,0.060114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229230E56617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.769248857976521,56.617635000000000]
["glac_bound",383993.000000000000000,"G229409E56618N","2008-05-01T00:00:00",623988.434276579180732,0.623988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229409E56618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.593183125465544,56.617763499999995]
["glac_bound",383994.000000000000000,"G227581E57989N","2008-05-01T00:00:00",80582.606643860592158,0.080583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227581E57989N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.419645333793369,57.987738000000000]
["glac_bound",383999.000000000000000,"G228355E56793N","2008-05-01T00:00:00",277388.454640102456324,0.277388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228355E56793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.644761516657496,56.792179500000003]
["glac_bound",384002.000000000000000,"G229482E57160N","2008-05-01T00:00:00",439067.329757241648622,0.439067000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229482E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.520373455763348,57.159552500000004]
["glac_bound",384003.000000000000000,"G222412E59927N","2008-05-01T00:00:00",331323.728393176803365,0.331324000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222412E59927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.588771424074025,59.926537500000002]
["glac_bound",384004.000000000000000,"G229159E56365N","2008-05-01T00:00:00",42894.180455089895986,0.042894000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229159E56365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.842398553127509,56.364531499999998]
["glac_bound",384011.000000000000000,"G229994E56733N","2008-05-01T00:00:00",92959.109108710195869,0.092959000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229994E56733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.006676523927865,56.732556500000001]
["glac_bound",384013.000000000000000,"G230266E56221N","2008-05-01T00:00:00",205544.448411883320659,0.205544000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230266E56221N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.731957611161420,56.224237500000001]
["glac_bound",384015.000000000000000,"G230018E55758N","2008-05-01T00:00:00",4315130.283592883497477,4.315130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230018E55758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.971004734986934,55.766280999999999]
["glac_bound",384016.000000000000000,"G227204E58205N","2008-05-01T00:00:00",1708088.337935381801799,1.708090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227204E58205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.788539354624277,58.202897999999998]
["glac_bound",384018.000000000000000,"G225567E59373N","2008-05-01T00:00:00",667338.383186402032152,0.667338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225567E59373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.436316363059944,59.373437500000001]
["glac_bound",384021.000000000000000,"G227573E57707N","2008-05-01T00:00:00",190419.497627766337246,0.190419000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227573E57707N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.428747952260721,57.705519500000001]
["glac_bound",384026.000000000000000,"G227998E57363N","2008-05-01T00:00:00",1098466.253635834436864,1.098470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227998E57363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.005956412777550,57.365784500000004]
["glac_bound",384028.000000000000000,"G228718E57464N","2008-05-01T00:00:00",116225.518574561880087,0.116226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228718E57464N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.281859975341121,57.463848999999996]
["glac_bound",384031.000000000000000,"G230610E56727N","2008-05-01T00:00:00",557791.503283261437900,0.557792000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230610E56727N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.392108980272951,56.728029999999997]
["glac_bound",384034.000000000000000,"G231675E56268N","2008-05-01T00:00:00",481071.633369733695872,0.481072000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231675E56268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.325346678382402,56.268888000000004]
["glac_bound",384036.000000000000000,"G228031E57368N","2008-05-01T00:00:00",248165.746733331558062,0.248166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228031E57368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.969514098157902,57.367737499999997]
["glac_bound",384040.000000000000000,"G228540E56904N","2008-05-01T00:00:00",53912.860358560348686,0.053913000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228540E56904N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.460672135361449,56.903823000000003]
["glac_bound",384042.000000000000000,"G222794E59423N","2008-05-01T00:00:00",235648.570292927150149,0.235649000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222794E59423N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.206788943436663,59.422439999999995]
["glac_bound",384045.000000000000000,"G224016E59693N","2008-05-01T00:00:00",204736.271849903743714,0.204736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224016E59693N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.984568692031530,59.693789500000001]
["glac_bound",384046.000000000000000,"G229538E56272N","2008-05-01T00:00:00",260241.707498045783723,0.260242000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229538E56272N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.458549675729273,56.273528999999996]
["glac_bound",384048.000000000000000,"G222203E59719N","2008-05-01T00:00:00",543538.436684122425504,0.543538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222203E59719N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.793903296513577,59.722178000000000]
["glac_bound",384050.000000000000000,"G229022E57292N","2008-05-01T00:00:00",377318.887094288191292,0.377319000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229022E57292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.976988532793513,57.292259500000000]
["glac_bound",384052.000000000000000,"G223698E59781N","2008-05-01T00:00:00",354264.940175006864592,0.354265000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223698E59781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.300562714526109,59.781755500000003]
["glac_bound",384054.000000000000000,"G224805E59822N","2008-05-01T00:00:00",217677.420605996769154,0.217677000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224805E59822N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.194749106226936,59.821563999999995]
["glac_bound",384055.000000000000000,"G227245E58420N","2008-05-01T00:00:00",98983.057237190354499,0.098983000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227245E58420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.754484144262278,58.419822500000002]
["glac_bound",384056.000000000000000,"G225394E59532N","2008-05-01T00:00:00",79421.497451299583190,0.079422000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225394E59532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.605468011480184,59.532617500000001]
["glac_bound",384057.000000000000000,"G230472E56041N","2008-05-01T00:00:00",79570.510794564586831,0.079571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230472E56041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.529303031665052,56.041100999999998]
["glac_bound",384059.000000000000000,"G228055E57467N","2008-05-01T00:00:00",573216.176067055086605,0.573216000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228055E57467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.945924482663315,57.467026000000004]
["glac_bound",384060.000000000000000,"G226361E58942N","2008-05-01T00:00:00",2197620.365402600262314,2.197620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226361E58942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.637656957127234,58.941322000000000]
["glac_bound",384063.000000000000000,"G223635E59755N","2008-05-01T00:00:00",877987.843864558264613,0.877988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223635E59755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.362379641323713,59.755886000000004]
["glac_bound",384066.000000000000000,"G223408E59523N","2008-05-01T00:00:00",501913.639704705448821,0.501914000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223408E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.591585602767850,59.524191500000001]
["glac_bound",384074.000000000000000,"G221637E59750N","2008-05-01T00:00:00",75990.021312520300853,0.075990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221637E59750N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.362274849245495,59.749424000000005]
["glac_bound",384082.000000000000000,"G231108E55253N","2008-05-01T00:00:00",515218.454442752525210,0.515218000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231108E55253N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.893813445310883,55.251306000000000]
["glac_bound",384088.000000000000000,"G230255E57308N","2008-05-01T00:00:00",493177.429659120156430,0.493177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230255E57308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.746293996153838,57.307679000000000]
["glac_bound",384092.000000000000000,"G223691E59781N","2008-05-01T00:00:00",124654.626241563586518,0.124655000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223691E59781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.310785712534084,59.780874499999996]
["glac_bound",384093.000000000000000,"G230269E55110N","2008-05-01T00:00:00",178605.360453412606148,0.178605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230269E55110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.731054001564075,55.109722000000005]
["glac_bound",384099.000000000000000,"G226946E58065N","2008-05-01T00:00:00",69376.964540528031648,0.069377000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226946E58065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.053798978204526,58.065835000000000]
["glac_bound",384103.000000000000000,"G227654E57585N","2008-05-01T00:00:00",94594.136853965625050,0.094594000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227654E57585N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.345396863860856,57.585042000000001]
["glac_bound",384105.000000000000000,"G225599E59351N","2008-05-01T00:00:00",112817.190567933823331,0.112817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225599E59351N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.400419595586044,59.351939500000000]
["glac_bound",384106.000000000000000,"G225786E59194N","2008-05-01T00:00:00",1265763.650483566801995,1.265760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225786E59194N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.215851266806709,59.193609500000001]
["glac_bound",384108.000000000000000,"G227956E57371N","2008-05-01T00:00:00",546734.150540577829815,0.546734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227956E57371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.040689572836811,57.372745500000001]
["glac_bound",384109.000000000000000,"G227665E57791N","2008-05-01T00:00:00",2699072.232669101096690,2.699070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227665E57791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.334551972458883,57.791305999999999]
["glac_bound",384113.000000000000000,"G228709E57224N","2008-05-01T00:00:00",611641.413792102597654,0.611641000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228709E57224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.293512139338759,57.226427500000000]
["glac_bound",384114.000000000000000,"G223925E59776N","2008-05-01T00:00:00",164479.416305150283733,0.164479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223925E59776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.075849475788345,59.775863999999999]
["glac_bound",384115.000000000000000,"G230609E55218N","2008-05-01T00:00:00",113122.875114464986837,0.113123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230609E55218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.390477962751731,55.219050499999994]
["glac_bound",384119.000000000000000,"G227874E57382N","2008-05-01T00:00:00",561194.261572339688428,0.561194000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227874E57382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.126629192247776,57.381885499999996]
["glac_bound",384122.000000000000000,"G229078E56746N","2008-05-01T00:00:00",169420.535444766166620,0.169421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229078E56746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.921991155434796,56.746510999999998]
["glac_bound",384123.000000000000000,"G227813E57543N","2008-05-01T00:00:00",1925352.361583233345300,1.925350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227813E57543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.187306693288861,57.545784999999995]
["glac_bound",384125.000000000000000,"G228085E58086N","2008-05-01T00:00:00",603217.121392154600471,0.603217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228085E58086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.912199469906824,58.086532500000004]
["glac_bound",384128.000000000000000,"G225607E59270N","2008-05-01T00:00:00",197857.672766103351023,0.197858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225607E59270N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.393308447492359,59.270989999999998]
["glac_bound",384131.000000000000000,"G229235E56872N","2008-05-01T00:00:00",262008.782925286242971,0.262009000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229235E56872N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.762178095186329,56.869972500000003]
["glac_bound",384132.000000000000000,"G227198E58460N","2008-05-01T00:00:00",3852541.935087344609201,3.852540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227198E58460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.792647580013750,58.466036000000003]
["glac_bound",384134.000000000000000,"G230018E56356N","2008-05-01T00:00:00",799048.347979069571011,0.799048000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230018E56356N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.987718063215937,56.358520999999996]
["glac_bound",384135.000000000000000,"G230314E56312N","2008-05-01T00:00:00",790167.256903367349878,0.790167000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230314E56312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.685304941406258,56.311301499999999]
["glac_bound",384139.000000000000000,"G223673E59727N","2008-05-01T00:00:00",107172.505078879345092,0.107173000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223673E59727N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.327566622151522,59.727128499999999]
["glac_bound",384157.000000000000000,"G226384E58822N","2008-05-01T00:00:00",1239914.706174199935049,1.239910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226384E58822N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.612071479160420,58.819012000000001]
["glac_bound",384159.000000000000000,"G225995E58986N","2008-05-01T00:00:00",3813982.210010301787406,3.813980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB225995E58986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.004847919718316,58.988287999999997]
["glac_bound",384163.000000000000000,"G228660E57441N","2008-05-01T00:00:00",3686558.534382599405944,3.686560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228660E57441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.335114904119450,57.447221499999998]
["glac_bound",384164.000000000000000,"G223410E59470N","2008-05-01T00:00:00",366742.680630749789998,0.366743000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223410E59470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.592038157870718,59.470473499999997]
["glac_bound",384167.000000000000000,"G223153E59724N","2008-05-01T00:00:00",3556783.155392460525036,3.556780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223153E59724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.863476860945070,59.722163999999999]
["glac_bound",384168.000000000000000,"G224963E59312N","2008-05-01T00:00:00",688075.040293168509379,0.688075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224963E59312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.036699019474668,59.311408999999998]
["glac_bound",384174.000000000000000,"G227933E57977N","2008-05-01T00:00:00",189835.455571976519423,0.189835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227933E57977N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.066618380353816,57.977187999999998]
["glac_bound",384175.000000000000000,"G227020E58380N","2008-05-01T00:00:00",170306.521362579340348,0.170307000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227020E58380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.980509827595540,58.380370499999998]
["glac_bound",384176.000000000000000,"G229963E56799N","2008-05-01T00:00:00",235086.933565675659338,0.235087000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229963E56799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.037974041063421,56.798204999999996]
["glac_bound",384185.000000000000000,"G228730E57411N","2008-05-01T00:00:00",226892.090664084622404,0.226892000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228730E57411N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.270237072067516,57.411203000000000]
["glac_bound",384188.000000000000000,"G226895E58363N","2008-05-01T00:00:00",343895.335398031747900,0.343895000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226895E58363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.105247027655821,58.363117000000003]
["glac_bound",384191.000000000000000,"G230107E55667N","2008-05-01T00:00:00",590032.785691124037839,0.590033000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230107E55667N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.893281232831072,55.666240999999999]
["glac_bound",384193.000000000000000,"G229375E56563N","2008-05-01T00:00:00",157128.564049050357426,0.157129000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229375E56563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.624382399580611,56.563065500000000]
["glac_bound",384198.000000000000000,"G228507E57157N","2008-05-01T00:00:00",407192.736969109508209,0.407193000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228507E57157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.492687119325183,57.157662500000001]
["glac_bound",384200.000000000000000,"G222791E59510N","2008-05-01T00:00:00",125595.760329441385693,0.125596000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222791E59510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.207243742661433,59.511161999999999]
["glac_bound",384201.000000000000000,"G227324E58249N","2008-05-01T00:00:00",119146.521218418318313,0.119147000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227324E58249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.673908566118627,58.248530500000001]
["glac_bound",384203.000000000000000,"G230390E55158N","2008-05-01T00:00:00",103218.216929301503114,0.103218000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230390E55158N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.611776896409168,55.157238000000000]
["glac_bound",384206.000000000000000,"G225259E59467N","2008-05-01T00:00:00",58073.557490245570079,0.058074000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225259E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.741866923819742,59.467023499999996]
["glac_bound",384207.000000000000000,"G223879E59940N","2008-05-01T00:00:00",106852.711166843277169,0.106853000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223879E59940N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.120911729635878,59.939085500000004]
["glac_bound",384211.000000000000000,"G225284E59347N","2008-05-01T00:00:00",83246.723280197678832,0.083247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225284E59347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.716566621988363,59.345564500000002]
["glac_bound",384217.000000000000000,"G223282E59430N","2008-05-01T00:00:00",103459.158180521568283,0.103459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223282E59430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.718119205882374,59.429657500000005]
["glac_bound",384221.000000000000000,"G230614E55348N","2008-05-01T00:00:00",61787.266945562012552,0.061787000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230614E55348N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.386147694550004,55.347831999999997]
["glac_bound",384223.000000000000000,"G229602E56449N","2008-05-01T00:00:00",823264.857129458570853,0.823265000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229602E56449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.399732902243613,56.448481500000000]
["glac_bound",384224.000000000000000,"G229321E57430N","2008-05-01T00:00:00",644855.362410486326553,0.644855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229321E57430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.680391635411411,57.429138999999999]
["glac_bound",384228.000000000000000,"G228135E57129N","2008-05-01T00:00:00",449141.922745283285622,0.449142000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228135E57129N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.869064693965527,57.130821499999996]
["glac_bound",384233.000000000000000,"G228880E57360N","2008-05-01T00:00:00",88693.148993893031729,0.088693000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228880E57360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.119175406424773,57.360123999999999]
["glac_bound",384236.000000000000000,"G230268E56974N","2008-05-01T00:00:00",591000.101333016180433,0.591000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230268E56974N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.728586362678016,56.972803499999998]
["glac_bound",384239.000000000000000,"G227921E57587N","2008-05-01T00:00:00",10926212.245146609842777,10.926200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227921E57587N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.064288211388600,57.602766000000003]
["glac_bound",384243.000000000000000,"G229978E56520N","2008-05-01T00:00:00",12918057.906681500375271,12.918100000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229978E56520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.041997739361705,56.532801000000006]
["glac_bound",384249.000000000000000,"G227701E58093N","2008-05-01T00:00:00",1671511.383473461493850,1.671510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227701E58093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.290815454291049,58.097539499999996]
["glac_bound",384252.000000000000000,"G221831E59943N","2008-05-01T00:00:00",1062874.101699651684612,1.062870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221831E59943N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.163402716353858,59.945281999999999]
["glac_bound",384256.000000000000000,"G229807E56500N","2008-05-01T00:00:00",4391908.440895518288016,4.391910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229807E56500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.172271808333335,56.493195999999998]
["glac_bound",384260.000000000000000,"G229586E56439N","2008-05-01T00:00:00",2502484.356769139878452,2.502480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229586E56439N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.413383206046262,56.439948000000001]
["glac_bound",384261.000000000000000,"G230115E56324N","2008-05-01T00:00:00",249893.337101529759821,0.249893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230115E56324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.884502629657220,56.324148500000007]
["glac_bound",384262.000000000000000,"G223882E59930N","2008-05-01T00:00:00",1626769.988583953585476,1.626770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223882E59930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.116208294293813,59.930163499999999]
["glac_bound",384264.000000000000000,"G228815E57412N","2008-05-01T00:00:00",60560.853096261475002,0.060561000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228815E57412N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.184759008106482,57.411361499999998]
["glac_bound",384265.000000000000000,"G225860E59349N","2008-05-01T00:00:00",134025.811499713367084,0.134026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225860E59349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.140017802277839,59.348686000000001]
["glac_bound",384269.000000000000000,"G221749E59731N","2008-05-01T00:00:00",1029993.174196328502148,1.029990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221749E59731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.252606579457648,59.730849499999998]
["glac_bound",384281.000000000000000,"G222467E59681N","2008-05-01T00:00:00",509111.268098608066794,0.509111000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222467E59681N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.532268033427187,59.682188499999995]
["glac_bound",384282.000000000000000,"G227318E58367N","2008-05-01T00:00:00",592777.972233672277071,0.592778000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227318E58367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.682349800428767,58.367876500000001]
["glac_bound",384285.000000000000000,"G229969E56568N","2008-05-01T00:00:00",386613.202183785440866,0.386613000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229969E56568N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.025475492486976,56.569623499999999]
["glac_bound",384286.000000000000000,"G226725E58642N","2008-05-01T00:00:00",1222281.048427298665047,1.222280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226725E58642N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.273101468763173,58.643059500000000]
["glac_bound",384296.000000000000000,"G226523E58800N","2008-05-01T00:00:00",1028668.166141461348161,1.028670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226523E58800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.478959456093492,58.804989000000006]
["glac_bound",384300.000000000000000,"G227063E58465N","2008-05-01T00:00:00",160124.153834007098339,0.160124000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227063E58465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.936546642710425,58.466948500000001]
["glac_bound",384302.000000000000000,"G227102E58305N","2008-05-01T00:00:00",1490252.181323350174353,1.490250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227102E58305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.898527428037823,58.308244500000001]
["glac_bound",384303.000000000000000,"G226714E58643N","2008-05-01T00:00:00",57270.308106950040383,0.057270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226714E58643N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.285402115605109,58.642666499999997]
["glac_bound",384305.000000000000000,"G230340E54891N","2008-05-01T00:00:00",575540.116593737853691,0.575540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230340E54891N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.658447213723946,54.890163500000000]
["glac_bound",384306.000000000000000,"G228543E56784N","2008-05-01T00:00:00",219224.054298906150507,0.219224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228543E56784N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.458786273058138,56.783502499999997]
["glac_bound",384308.000000000000000,"G228480E57316N","2008-05-01T00:00:00",1139892.088178040925413,1.139890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228480E57316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.518025830827270,57.314393999999993]
["glac_bound",384313.000000000000000,"G229556E57001N","2008-05-01T00:00:00",114021.849939163454110,0.114022000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229556E57001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.445599873434475,57.001224000000001]
["glac_bound",384315.000000000000000,"G231658E56736N","2008-05-01T00:00:00",139874.380257187178358,0.139874000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231658E56736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.341977257699455,56.735884999999996]
["glac_bound",384316.000000000000000,"G230474E55310N","2008-05-01T00:00:00",3780830.861601537093520,3.780830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230474E55310N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522265615522770,55.309693500000002]
["glac_bound",384318.000000000000000,"G230402E56649N","2008-05-01T00:00:00",332075.953019232663792,0.332076000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230402E56649N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.595125887744388,56.647548000000000]
["glac_bound",384323.000000000000000,"G229304E57219N","2008-05-01T00:00:00",1126432.223438519285992,1.126430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229304E57219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.689861806654449,57.217174999999997]
["glac_bound",384326.000000000000000,"G230566E54856N","2008-05-01T00:00:00",69866.356035929566133,0.069866000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230566E54856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.434583928340089,54.856550999999996]
["glac_bound",384329.000000000000000,"G228842E56499N","2008-05-01T00:00:00",7723868.158856053836644,7.723870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228842E56499N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.175857981999997,56.516046000000003]
["glac_bound",384330.000000000000000,"G222281E59380N","2008-05-01T00:00:00",312791.573120207351167,0.312792000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222281E59380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.717978483209492,59.379981500000000]
["glac_bound",384333.000000000000000,"G229436E57713N","2008-05-01T00:00:00",848334.841015011887066,0.848335000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229436E57713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.565038914482926,57.717003500000004]
["glac_bound",384337.000000000000000,"G227199E57962N","2008-05-01T00:00:00",76283.823399293891271,0.076284000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227199E57962N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.804890672631302,57.963517500000002]
["glac_bound",384338.000000000000000,"G229560E56136N","2008-05-01T00:00:00",11356.615860843325208,0.011357000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229560E56136N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.440412440132434,56.135949499999995]
["glac_bound",384339.000000000000000,"G230539E56758N","2008-05-01T00:00:00",157912.447327026980929,0.157912000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230539E56758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.460275050047244,56.757573500000007]
["glac_bound",384350.000000000000000,"G221867E59594N","2008-05-01T00:00:00",1090591.206273571122438,1.090590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221867E59594N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.136518832907086,59.597597000000000]
["glac_bound",384354.000000000000000,"G226733E58234N","2008-05-01T00:00:00",369201.103678741259500,0.369201000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226733E58234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.267213985528656,58.231385500000002]
["glac_bound",384359.000000000000000,"G229239E56848N","2008-05-01T00:00:00",1707551.909960150020197,1.707550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229239E56848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.762473840118645,56.850014000000002]
["glac_bound",384361.000000000000000,"G226702E58462N","2008-05-01T00:00:00",15618154.147700324654579,15.618200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226702E58462N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.306581121438228,58.477899999999998]
["glac_bound",384368.000000000000000,"G223531E59848N","2008-05-01T00:00:00",258806.138635410083225,0.258806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223531E59848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.468212222327395,59.848628500000004]
["glac_bound",384369.000000000000000,"G222710E59461N","2008-05-01T00:00:00",52291.548238982279145,0.052291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222710E59461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.291751381597066,59.462154999999996]
["glac_bound",384372.000000000000000,"G229392E56550N","2008-05-01T00:00:00",275946.802239311393350,0.275947000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229392E56550N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.606941247370571,56.549993000000001]
["glac_bound",384376.000000000000000,"G227683E58233N","2008-05-01T00:00:00",83820.282355912524508,0.083820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227683E58233N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.319663793269228,58.233783000000003]
["glac_bound",384383.000000000000000,"G230504E56740N","2008-05-01T00:00:00",237659.220929771690862,0.237659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230504E56740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.495952102494584,56.739970000000000]
["glac_bound",384384.000000000000000,"G228942E56489N","2008-05-01T00:00:00",390388.754057581245434,0.390389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228942E56489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.057592647783963,56.487017999999999]
["glac_bound",384386.000000000000000,"G222456E59994N","2008-05-01T00:00:00",300846.136412721127272,0.300846000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222456E59994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.544304118612217,59.995730999999999]
["glac_bound",384388.000000000000000,"G228624E57196N","2008-05-01T00:00:00",50605.675377753679641,0.050606000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228624E57196N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.376243574495959,57.196507499999996]
["glac_bound",384393.000000000000000,"G227116E58480N","2008-05-01T00:00:00",183349.812089486746117,0.183350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227116E58480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.884169169431260,58.479646000000002]
["glac_bound",384394.000000000000000,"G230325E57160N","2008-05-01T00:00:00",96655.437259884492960,0.096655000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230325E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.674625498602040,57.160037000000003]
["glac_bound",384404.000000000000000,"G228846E57347N","2008-05-01T00:00:00",176541.528590770642040,0.176542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228846E57347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.152573784086485,57.347290000000001]
["glac_bound",384406.000000000000000,"G231206E57371N","2008-05-01T00:00:00",258538.658196001226315,0.258539000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231206E57371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.794781731620162,57.371693500000006]
["glac_bound",384407.000000000000000,"G227617E58141N","2008-05-01T00:00:00",309353.127105180232320,0.309353000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227617E58141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.384632020175616,58.140624000000003]
["glac_bound",384414.000000000000000,"G227292E58543N","2008-05-01T00:00:00",627084.083212941652164,0.627084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227292E58543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.713377864563938,58.546982999999997]
["glac_bound",384420.000000000000000,"G230038E56207N","2008-05-01T00:00:00",1467548.671492483466864,1.467550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230038E56207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.961007630958818,56.209014500000002]
["glac_bound",384424.000000000000000,"G230047E56339N","2008-05-01T00:00:00",6628425.759884979575872,6.628430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230047E56339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.948488057657187,56.351771999999997]
["glac_bound",384427.000000000000000,"G230494E56740N","2008-05-01T00:00:00",130248.096806215966353,0.130248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230494E56740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.505488089210814,56.739356000000001]
["glac_bound",384428.000000000000000,"G229536E57147N","2008-05-01T00:00:00",2170560.874857732094824,2.170560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229536E57147N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.464711762940851,57.147742000000001]
["glac_bound",384442.000000000000000,"G222769E59321N","2008-05-01T00:00:00",1678346.668197316816077,1.678350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222769E59321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.230449291833793,59.325625500000001]
["glac_bound",384448.000000000000000,"G227133E58235N","2008-05-01T00:00:00",101225.155553625096218,0.101225000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227133E58235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.866659010261174,58.234115000000003]
["glac_bound",384449.000000000000000,"G228709E57431N","2008-05-01T00:00:00",808334.686413208139129,0.808335000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228709E57431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.285682051503159,57.428933000000001]
["glac_bound",384455.000000000000000,"G227735E57866N","2008-05-01T00:00:00",56714.404490346918465,0.056714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227735E57866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.265719382745772,57.866121000000000]
["glac_bound",384458.000000000000000,"G230045E56105N","2008-05-01T00:00:00",1276191.130594058195129,1.276190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230045E56105N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.953042796671298,56.111776500000005]
["glac_bound",384465.000000000000000,"G228032E57234N","2008-05-01T00:00:00",1073573.015131118940189,1.073570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228032E57234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.973406693158438,57.229073000000000]
["glac_bound",384466.000000000000000,"G229631E56526N","2008-05-01T00:00:00",191216.367592912050895,0.191216000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229631E56526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.369692794704747,56.525936999999999]
["glac_bound",384469.000000000000000,"G231963E57188N","2008-05-01T00:00:00",107956.512742119652103,0.107957000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA231963E57188N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.036842647912863,57.188340499999995]
["glac_bound",384471.000000000000000,"G229446E56899N","2008-05-01T00:00:00",2304439.164185385219753,2.304440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229446E56899N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.555293460140263,56.899755499999998]
["glac_bound",384472.000000000000000,"G230837E57013N","2008-05-01T00:00:00",1214533.967427044641227,1.214530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230837E57013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.163471607495751,57.010104999999996]
["glac_bound",384474.000000000000000,"G221813E60006N","2008-05-01T00:00:00",2513780.639482059516013,2.513780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221813E60006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.205644991047478,60.000935499999997]
["glac_bound",384482.000000000000000,"G230843E56468N","2008-05-01T00:00:00",761299.792701114783995,0.761300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230843E56468N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.152819808949630,56.469600499999999]
["glac_bound",384486.000000000000000,"G227870E57418N","2008-05-01T00:00:00",411022.633672284486238,0.411023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227870E57418N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.128924733108107,57.417625000000001]
["glac_bound",384487.000000000000000,"G225087E59378N","2008-05-01T00:00:00",63120.324137060648354,0.063120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225087E59378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.912558251329813,59.378017499999999]
["glac_bound",384488.000000000000000,"G226979E58413N","2008-05-01T00:00:00",3308240.472868377808481,3.308240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226979E58413N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.025229070666342,58.416128999999998]
["glac_bound",384495.000000000000000,"G228999E57224N","2008-05-01T00:00:00",1003450.443906833417714,1.003450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228999E57224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.001851189155957,57.224699999999999]
["glac_bound",384509.000000000000000,"G227447E58427N","2008-05-01T00:00:00",2303000.076669817324728,2.303000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227447E58427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.547556223755237,58.430239499999999]
["glac_bound",384510.000000000000000,"G222962E59213N","2008-05-01T00:00:00",682806.658408694900572,0.682807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222962E59213N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.036472287307674,59.212657000000000]
["glac_bound",384513.000000000000000,"G227963E57646N","2008-05-01T00:00:00",153455.579023740370758,0.153456000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227963E57646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.037799172682895,57.646142499999996]
["glac_bound",384515.000000000000000,"G226887E58495N","2008-05-01T00:00:00",374409.775594436272513,0.374410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226887E58495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.115048868897020,58.495042499999997]
["glac_bound",384516.000000000000000,"G227982E57946N","2008-05-01T00:00:00",1632238.386477900901809,1.632240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227982E57946N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.018373525188878,57.945067499999993]
["glac_bound",384519.000000000000000,"G226887E58481N","2008-05-01T00:00:00",571712.241462503094226,0.571712000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226887E58481N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.112567292740835,58.483802999999995]
["glac_bound",384524.000000000000000,"G230745E55654N","2008-05-01T00:00:00",463884.206746422860306,0.463884000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230745E55654N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.255979639152088,55.652217499999999]
["glac_bound",384526.000000000000000,"G229060E56656N","2008-05-01T00:00:00",458716.513825609174091,0.458717000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229060E56656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.941263137219721,56.655905500000003]
["glac_bound",384531.000000000000000,"G230182E55800N","2008-05-01T00:00:00",47298414.542940765619278,47.298400000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230182E55800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.791657615863130,55.821415000000002]
["glac_bound",384534.000000000000000,"G222799E59443N","2008-05-01T00:00:00",115658.460478398279520,0.115658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222799E59443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.201298516587713,59.443549000000004]
["glac_bound",384540.000000000000000,"G226290E59004N","2008-05-01T00:00:00",5708497.884509442374110,5.708500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226294E59001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.705113035147519,59.001104999999995]
["glac_bound",384541.000000000000000,"G230535E57031N","2008-05-01T00:00:00",737608.049958589952439,0.737608000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230535E57031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.462785140732763,57.031303999999999]
["glac_bound",384544.000000000000000,"G229378E57142N","2008-05-01T00:00:00",55564.395342677700683,0.055564000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229378E57142N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.624218710549030,57.141902500000000]
["glac_bound",384546.000000000000000,"G229329E56948N","2008-05-01T00:00:00",2458893.547042272053659,2.458890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229329E56948N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.670687705831710,56.955340500000005]
["glac_bound",384547.000000000000000,"G229026E57278N","2008-05-01T00:00:00",61921.996012825838989,0.061922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229026E57278N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.974415947899104,57.277905500000003]
["glac_bound",384555.000000000000000,"G228567E57264N","2008-05-01T00:00:00",186334.479791642283089,0.186334000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228567E57264N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.433202619435519,57.263919500000000]
["glac_bound",384557.000000000000000,"G227603E58276N","2008-05-01T00:00:00",396869.033803385857027,0.396869000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227603E58276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.395759391576917,58.277714500000002]
["glac_bound",384564.000000000000000,"G221677E60000N","2008-05-01T00:00:00",773907.079158156877384,0.773907000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221677E60000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.323654915108477,59.998559999999998]
["glac_bound",384570.000000000000000,"G226584E58537N","2008-05-01T00:00:00",215417.520025767647894,0.215418000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226584E58537N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.414159131482393,58.537063000000003]
["glac_bound",384571.000000000000000,"G226830E58434N","2008-05-01T00:00:00",632561.305996120907366,0.632561000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226830E58434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.169078442352941,58.432638499999996]
["glac_bound",384572.000000000000000,"G222406E59518N","2008-05-01T00:00:00",7198230.659591186791658,7.198230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222406E59518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.602131595016829,59.524096000000000]
["glac_bound",384574.000000000000000,"G230126E56329N","2008-05-01T00:00:00",267493.635895761020947,0.267494000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230126E56329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.872817427174112,56.329098000000002]
["glac_bound",384580.000000000000000,"G230405E54635N","2008-05-01T00:00:00",775788.247703090775758,0.775788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230405E54635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.592966501500143,54.634756500000002]
["glac_bound",384583.000000000000000,"G226914E58133N","2008-05-01T00:00:00",586798.833746102405712,0.586799000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226914E58133N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.089391071171519,58.135418999999999]
["glac_bound",384587.000000000000000,"G223273E59737N","2008-05-01T00:00:00",1855938.928762577939779,1.855940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223273E59737N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.728556448232382,59.736863000000000]
["glac_bound",384589.000000000000000,"G230284E56299N","2008-05-01T00:00:00",284704.640385166683700,0.284705000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230284E56299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.716326051296562,56.298628500000000]
["glac_bound",384591.000000000000000,"G223728E59696N","2008-05-01T00:00:00",487689.957661572261713,0.487690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223728E59696N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.272577748717964,59.696605000000005]
["glac_bound",384597.000000000000000,"G222908E59449N","2008-05-01T00:00:00",169200.734431743301684,0.169201000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222908E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.093075868315509,59.449373000000001]
["glac_bound",384598.000000000000000,"G223268E59719N","2008-05-01T00:00:00",2051544.958412290550768,2.051540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223268E59719N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.728721860837823,59.721024000000000]
["glac_bound",384601.000000000000000,"G221881E59591N","2008-05-01T00:00:00",223909.548241347976727,0.223910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221881E59591N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.121383937113592,59.593023000000002]
["glac_bound",384603.000000000000000,"G230354E55156N","2008-05-01T00:00:00",144959.807513857056620,0.144960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230354E55156N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.647641218154661,55.156074500000003]
["glac_bound",384608.000000000000000,"G230316E56992N","2008-05-01T00:00:00",698492.668387715704739,0.698493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230316E56992N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.687564664670276,56.992983499999994]
["glac_bound",384611.000000000000000,"G226924E58287N","2008-05-01T00:00:00",282021.346937272406649,0.282021000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226924E58287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.076299463310590,58.286144999999998]
["glac_bound",384616.000000000000000,"G229075E56406N","2008-05-01T00:00:00",122663.154247793048853,0.122663000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229075E56406N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.924871627226480,56.405488500000004]
["glac_bound",384619.000000000000000,"G222397E59851N","2008-05-01T00:00:00",4670377.923786643892527,4.670380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222397E59851N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.610362046285474,59.868905999999996]
["glac_bound",384621.000000000000000,"G228430E56926N","2008-05-01T00:00:00",3187054.529346377123147,3.187050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228430E56926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.566941080016875,56.929017000000002]
["glac_bound",384627.000000000000000,"G231532E56131N","2008-05-01T00:00:00",965735.545811948948540,0.965736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231532E56131N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.469618963602954,56.131188500000000]
["glac_bound",384632.000000000000000,"G230137E56314N","2008-05-01T00:00:00",106634.138033940907917,0.106634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230137E56314N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.863195582991750,56.312947999999999]
["glac_bound",384633.000000000000000,"G229243E57093N","2008-05-01T00:00:00",1035940.925408402807079,1.035940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229243E57093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.760263365288125,57.094943999999998]
["glac_bound",384637.000000000000000,"G228759E57438N","2008-05-01T00:00:00",328834.625250450044405,0.328835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228759E57438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.240630359567888,57.437238000000001]
["glac_bound",384638.000000000000000,"G230693E55647N","2008-05-01T00:00:00",876505.633394404896535,0.876506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230693E55647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.313457176856616,55.650634499999995]
["glac_bound",384639.000000000000000,"G229774E56509N","2008-05-01T00:00:00",1401161.182476714951918,1.401160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229774E56509N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.231444473845102,56.511043000000001]
["glac_bound",384640.000000000000000,"G229181E56877N","2008-05-01T00:00:00",75274.694172548712231,0.075275000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229181E56877N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.817952291038523,56.877521500000000]
["glac_bound",384642.000000000000000,"G228439E56635N","2008-05-01T00:00:00",1566288.021327966125682,1.566290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228439E56635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.568186526111788,56.637884999999997]
["glac_bound",384643.000000000000000,"G229663E57742N","2008-05-01T00:00:00",100549.213597723006387,0.100549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229663E57742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.336855873421939,57.742351999999997]
["glac_bound",384646.000000000000000,"G227653E57522N","2008-05-01T00:00:00",185298.747908325312892,0.185299000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227653E57522N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.346328761163733,57.521687499999999]
["glac_bound",384647.000000000000000,"G231176E57093N","2008-05-01T00:00:00",907528.802978421328589,0.907529000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231176E57093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.827636242911183,57.097291499999997]
["glac_bound",384648.000000000000000,"G230474E55282N","2008-05-01T00:00:00",7601552.574274329468608,7.601550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230474E55282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.525750999264176,55.284402999999998]
["glac_bound",384651.000000000000000,"G227101E58383N","2008-05-01T00:00:00",53607.294195462636708,0.053607000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227101E58383N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.896646906813430,58.381585500000000]
["glac_bound",384652.000000000000000,"G225732E59145N","2008-05-01T00:00:00",267479.483418678108137,0.267479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225732E59145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.268382396711644,59.145368000000005]
["glac_bound",384653.000000000000000,"G229566E56301N","2008-05-01T00:00:00",150255.969884166872362,0.150256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229566E56301N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.434052377434682,56.300610499999998]
["glac_bound",384655.000000000000000,"G228809E57317N","2008-05-01T00:00:00",425787.392170927720144,0.425787000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228809E57317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.189468672195346,57.316113999999999]
["glac_bound",384656.000000000000000,"G228953E57099N","2008-05-01T00:00:00",144678.891328495636117,0.144679000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228953E57099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.046578948478896,57.098811499999996]
["glac_bound",384660.000000000000000,"G227051E58469N","2008-05-01T00:00:00",320662.915387827961240,0.320663000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227051E58469N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.951420489734119,58.469076000000001]
["glac_bound",384662.000000000000000,"G230862E56474N","2008-05-01T00:00:00",422495.741772858833428,0.422496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230862E56474N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.138589096895714,56.473770999999999]
["glac_bound",384665.000000000000000,"G227270E58351N","2008-05-01T00:00:00",215929.185953814710956,0.215929000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227270E58351N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.731162018428677,58.351275999999999]
["glac_bound",384666.000000000000000,"G228338E57220N","2008-05-01T00:00:00",1300723.340147219831124,1.300720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228338E57220N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.661480590669015,57.219674999999995]
["glac_bound",384670.000000000000000,"G230662E54902N","2008-05-01T00:00:00",3367537.130976818967611,3.367540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230662E54902N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.335528115026875,54.902946999999998]
["glac_bound",384675.000000000000000,"G230288E56002N","2008-05-01T00:00:00",510046.848632356908638,0.510047000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230288E56002N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.707604520369927,56.002536000000006]
["glac_bound",384677.000000000000000,"G226892E58245N","2008-05-01T00:00:00",282433.158294481225312,0.282433000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226892E58245N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.110645622958600,58.244025000000001]
["glac_bound",384680.000000000000000,"G230528E57158N","2008-05-01T00:00:00",137016.439632519031875,0.137016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230528E57158N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.470936899379922,57.157977000000002]
["glac_bound",384682.000000000000000,"G229696E56717N","2008-05-01T00:00:00",1838330.173686658265069,1.838330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229696E56717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.295073918963567,56.719276000000001]
["glac_bound",384684.000000000000000,"G228489E57203N","2008-05-01T00:00:00",1804065.726168896537274,1.804070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228489E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.512578076169859,57.210419999999999]
["glac_bound",384686.000000000000000,"G228535E57179N","2008-05-01T00:00:00",72333.386648691870505,0.072333000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228535E57179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.465667831947485,57.178480000000000]
["glac_bound",384688.000000000000000,"G228015E57235N","2008-05-01T00:00:00",143233.110178869334050,0.143233000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228015E57235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.983584117091766,57.235079999999996]
["glac_bound",384689.000000000000000,"G230119E55610N","2008-05-01T00:00:00",67431.305448898492614,0.067431000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230119E55610N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.882581875260485,55.610878999999997]
["glac_bound",384694.000000000000000,"G225089E59349N","2008-05-01T00:00:00",164595.550215582159581,0.164596000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225089E59349N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.910254958764455,59.349096500000002]
["glac_bound",384695.000000000000000,"G228414E57074N","2008-05-01T00:00:00",520237.002812610822730,0.520237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228414E57074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.584920278161349,57.074335500000004]
["glac_bound",384698.000000000000000,"G228950E57043N","2008-05-01T00:00:00",113969.735994585207663,0.113970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228950E57043N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.048931319672135,57.043336499999995]
["glac_bound",384700.000000000000000,"G227198E58045N","2008-05-01T00:00:00",1718156.821582702221349,1.718160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227198E58045N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.798832926357818,58.044959000000006]
["glac_bound",384701.000000000000000,"G229404E57135N","2008-05-01T00:00:00",1933362.538014977006242,1.933360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229404E57135N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.595000256306548,57.133664499999995]
["glac_bound",384705.000000000000000,"G225599E59268N","2008-05-01T00:00:00",401630.254489585873671,0.401630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225599E59268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.402733424544124,59.267846499999997]
["glac_bound",384708.000000000000000,"G229690E56162N","2008-05-01T00:00:00",13575793.705159166827798,13.575799999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229690E56162N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.286959685185195,56.184581999999999]
["glac_bound",384712.000000000000000,"G229618E56391N","2008-05-01T00:00:00",7157407.873776156455278,7.157410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229618E56391N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.377643986681448,56.391042999999996]
["glac_bound",384714.000000000000000,"G222297E59694N","2008-05-01T00:00:00",1052488.804538753116503,1.052490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222297E59694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.700425429863401,59.693968499999997]
["glac_bound",384716.000000000000000,"G230157E54808N","2008-05-01T00:00:00",327487.743458410201129,0.327488000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230157E54808N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.842464844625908,54.807649499999997]
["glac_bound",384719.000000000000000,"G229408E56862N","2008-05-01T00:00:00",143549.774000924982829,0.143550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229408E56862N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.592710210659618,56.862681000000002]
["glac_bound",384720.000000000000000,"G225913E59312N","2008-05-01T00:00:00",302923.672569029615261,0.302924000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225913E59312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.086419039337613,59.312674999999999]
["glac_bound",384725.000000000000000,"G229764E56802N","2008-05-01T00:00:00",585542.941378469928168,0.585543000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229764E56802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.233503424273351,56.802481499999999]
["glac_bound",384730.000000000000000,"G225383E59684N","2008-05-01T00:00:00",835547.568925392581150,0.835548000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225383E59684N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.615142333800748,59.683253000000001]
["glac_bound",384731.000000000000000,"G228943E56448N","2008-05-01T00:00:00",2202624.341454418376088,2.202620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228943E56448N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.052900336192039,56.450097000000000]
["glac_bound",384748.000000000000000,"G225274E59471N","2008-05-01T00:00:00",58313.319303521915572,0.058313000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225274E59471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.723892213862257,59.470199999999998]
["glac_bound",384749.000000000000000,"G224046E59693N","2008-05-01T00:00:00",58800.628788829169935,0.058801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224046E59693N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.956313710271246,59.693613999999997]
["glac_bound",384754.000000000000000,"G230132E55658N","2008-05-01T00:00:00",412392.981988952611573,0.412393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230132E55658N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.870529948435319,55.657964000000000]
["glac_bound",384756.000000000000000,"G230564E54805N","2008-05-01T00:00:00",961651.355558255687356,0.961651000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230564E54805N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.434365799783905,54.804103999999995]
["glac_bound",384763.000000000000000,"G229323E56937N","2008-05-01T00:00:00",208909.729018044861732,0.208910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229323E56937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.676760318360948,56.939701999999997]
["glac_bound",384764.000000000000000,"G229316E56975N","2008-05-01T00:00:00",1617578.019791733240709,1.617580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Yuri Glacier","None","08CG229316E56975N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.684348096774215,56.975811000000000]
["glac_bound",384769.000000000000000,"G230296E56319N","2008-05-01T00:00:00",56121.057290367069072,0.056121000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230296E56319N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.703914942610936,56.318904000000003]
["glac_bound",384770.000000000000000,"G230684E55230N","2008-05-01T00:00:00",535592.805091179208830,0.535593000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230684E55230N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.320121630487819,55.227720500000004]
["glac_bound",384774.000000000000000,"G221716E59618N","2008-05-01T00:00:00",2554246.185847011860460,2.554250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221716E59618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.276706257366783,59.621678000000003]
["glac_bound",384783.000000000000000,"G229048E56467N","2008-05-01T00:00:00",1410973.866660954663530,1.410970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG229048E56467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.954831883720914,56.472421999999995]
["glac_bound",384786.000000000000000,"G230056E54394N","2008-05-01T00:00:00",1223077.239788619801402,1.223080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230056E54394N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.946413127712162,54.394369999999995]
["glac_bound",384789.000000000000000,"G224676E59723N","2008-05-01T00:00:00",6225945.125140218064189,6.225940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224676E59723N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.323840876969314,59.723879499999995]
["glac_bound",384790.000000000000000,"G223358E59906N","2008-05-01T00:00:00",195600.800508936808910,0.195601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223358E59906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.640560507597286,59.906002999999998]
["glac_bound",384792.000000000000000,"G229930E56981N","2008-05-01T00:00:00",14062306.747616019099951,14.062300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229930E56981N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.054235751858755,56.995625500000003]
["glac_bound",384794.000000000000000,"G228410E56896N","2008-05-01T00:00:00",727949.591369888279587,0.727950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228410E56896N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.588634470705529,56.894323499999999]
["glac_bound",384798.000000000000000,"G227398E58283N","2008-05-01T00:00:00",4256345.268764348700643,4.256350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227398E58283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.606423878108529,58.286273500000000]
["glac_bound",384804.000000000000000,"G223903E59961N","2008-05-01T00:00:00",1033967.044562992174178,1.033970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223903E59961N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.097623888587975,59.961850499999997]
["glac_bound",384810.000000000000000,"G230354E56706N","2008-05-01T00:00:00",259750.789495682576671,0.259751000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230354E56706N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.646161232115332,56.705676499999996]
["glac_bound",384811.000000000000000,"G231150E55183N","2008-05-01T00:00:00",1365583.340841517085209,1.365580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231150E55183N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.853734559334100,55.186119000000005]
["glac_bound",384813.000000000000000,"G223738E59785N","2008-05-01T00:00:00",879154.670367464073934,0.879155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223738E59785N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.264360679311807,59.784987500000000]
["glac_bound",384814.000000000000000,"G230504E56685N","2008-05-01T00:00:00",292248.262187953863759,0.292248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230504E56685N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.496416578486020,56.685763500000000]
["glac_bound",384817.000000000000000,"G228482E57393N","2008-05-01T00:00:00",4010022.170122179668397,4.010020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228482E57393N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.510178337723005,57.397035500000001]
["glac_bound",384821.000000000000000,"G222367E59681N","2008-05-01T00:00:00",9236427.051207801327109,9.236430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222367E59681N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.631738758699953,59.673012000000000]
["glac_bound",384823.000000000000000,"G228072E57413N","2008-05-01T00:00:00",300062.522083233809099,0.300063000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228072E57413N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.925697087220158,57.413707500000001]
["glac_bound",384824.000000000000000,"G230539E54803N","2008-05-01T00:00:00",1373060.337840772001073,1.373060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230539E54803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.464691530816992,54.805276999999997]
["glac_bound",384832.000000000000000,"G230594E54749N","2008-05-01T00:00:00",52920.190130479946674,0.052920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230594E54749N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.405806316916568,54.748726500000004]
["glac_bound",384833.000000000000000,"G230812E56543N","2008-05-01T00:00:00",125097.460667056089733,0.125097000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230812E56543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.186294261961280,56.543013999999999]
["glac_bound",384835.000000000000000,"G228577E56546N","2008-05-01T00:00:00",4407404.886897754855454,4.407400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228577E56546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.414682398582045,56.551458499999995]
["glac_bound",384836.000000000000000,"G228494E56827N","2008-05-01T00:00:00",405549.718485853227321,0.405550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228494E56827N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.506973236295039,56.827355999999995]
["glac_bound",384838.000000000000000,"G228978E57228N","2008-05-01T00:00:00",1101603.358657474629581,1.101600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228978E57228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.025569645276050,57.230159000000000]
["glac_bound",384839.000000000000000,"G228860E57492N","2008-05-01T00:00:00",412089.887475954834372,0.412090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228860E57492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.144020137407210,57.493506500000002]
["glac_bound",384844.000000000000000,"G227769E57950N","2008-05-01T00:00:00",797579.556423855246976,0.797580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227769E57950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.226505916294826,57.950992499999998]
["glac_bound",384847.000000000000000,"G230449E55779N","2008-05-01T00:00:00",138154.617100828269031,0.138155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230449E55779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.554603338900392,55.779780500000001]
["glac_bound",384849.000000000000000,"G230527E54847N","2008-05-01T00:00:00",264353.625176112574991,0.264354000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230527E54847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.473743652224840,54.846823000000001]
["glac_bound",384850.000000000000000,"G229294E57454N","2008-05-01T00:00:00",65977.733630022994475,0.065978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229294E57454N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.704846818557940,57.455185499999999]
["glac_bound",384861.000000000000000,"G227815E57456N","2008-05-01T00:00:00",1582671.433845398481935,1.582670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227815E57456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.185976670978789,57.465623500000000]
["glac_bound",384862.000000000000000,"G224032E59995N","2008-05-01T00:00:00",362588.786732171487529,0.362589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224032E59995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.965818841976812,59.994442500000005]
["glac_bound",384863.000000000000000,"G225667E59173N","2008-05-01T00:00:00",201057.997137436439516,0.201058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225667E59173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.332157890035120,59.172697499999998]
["glac_bound",384869.000000000000000,"G229430E57542N","2008-05-01T00:00:00",299016.103405068570282,0.299016000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229430E57542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.570125462700162,57.545736500000004]
["glac_bound",384870.000000000000000,"G227869E57923N","2008-05-01T00:00:00",5049840.549702611751854,5.049840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227869E57923N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.130292482595848,57.927906000000000]
["glac_bound",384876.000000000000000,"G228395E56812N","2008-05-01T00:00:00",2436691.106963496655226,2.436690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228395E56812N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.605484007062898,56.813174500000002]
["glac_bound",384880.000000000000000,"G230466E56014N","2008-05-01T00:00:00",135621.145107171119889,0.135621000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230466E56014N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.535761848474436,56.016080500000001]
["glac_bound",384882.000000000000000,"G229297E56827N","2008-05-01T00:00:00",51840.248790518504393,0.051840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229297E56827N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.702611502272759,56.827797500000003]
["glac_bound",384884.000000000000000,"G224909E59732N","2008-05-01T00:00:00",100698.445098367112223,0.100698000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224909E59732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.092309730100737,59.731588500000001]
["glac_bound",384887.000000000000000,"G229458E56658N","2008-05-01T00:00:00",774425.332369591109455,0.774425000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229458E56658N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.550248238335683,56.661680000000004]
["glac_bound",384888.000000000000000,"G228487E57421N","2008-05-01T00:00:00",232292.727402206830448,0.232293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228487E57421N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.508286319369603,57.419079999999994]
["glac_bound",384901.000000000000000,"G227976E57986N","2008-05-01T00:00:00",327540.382143267488573,0.327540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227976E57986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.020045850692128,57.988430500000000]
["glac_bound",384902.000000000000000,"G228549E56613N","2008-05-01T00:00:00",749030.884487796225585,0.749031000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228549E56613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.449116103554957,56.612843999999996]
["glac_bound",384906.000000000000000,"G227446E58420N","2008-05-01T00:00:00",108547.999628834280884,0.108548000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227446E58420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.554409877706689,58.419924500000000]
["glac_bound",384910.000000000000000,"G229481E57001N","2008-05-01T00:00:00",1782002.432744130492210,1.782000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229481E57001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.521204879802667,57.001555999999994]
["glac_bound",384911.000000000000000,"G227390E57963N","2008-05-01T00:00:00",29020124.109014444053173,29.020099999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227390E57963N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.581972439009633,57.976461499999999]
["glac_bound",384912.000000000000000,"G226801E58517N","2008-05-01T00:00:00",667892.554481817292981,0.667893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226801E58517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.198381536043144,58.516418000000002]
["glac_bound",384918.000000000000000,"G230411E55227N","2008-05-01T00:00:00",157242.004902326036245,0.157242000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230411E55227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.589263454627456,55.227853499999995]
["glac_bound",384921.000000000000000,"G229930E57096N","2008-05-01T00:00:00",496375.996568147442304,0.496376000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229930E57096N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.069107666201120,57.096022000000005]
["glac_bound",384922.000000000000000,"G223303E59577N","2008-05-01T00:00:00",184520.980990967364050,0.184521000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223303E59577N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.697257869527959,59.577308500000001]
["glac_bound",384924.000000000000000,"G226223E59009N","2008-05-01T00:00:00",245071.062462014844641,0.245071000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226223E59009N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.773376334620991,59.008501500000001]
["glac_bound",384925.000000000000000,"G229572E56108N","2008-05-01T00:00:00",9838492.344626791775227,9.838490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229572E56108N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.442664224524663,56.116625499999998]
["glac_bound",384930.000000000000000,"G225455E59254N","2008-05-01T00:00:00",198674.205900647444651,0.198674000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225455E59254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.544332579626428,59.255500499999997]
["glac_bound",384935.000000000000000,"G226223E58664N","2008-05-01T00:00:00",1339314.425514942966402,1.339310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226223E58664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.777774505384002,58.665376500000001]
["glac_bound",384936.000000000000000,"G227539E57990N","2008-05-01T00:00:00",76055.284799223867594,0.076055000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227539E57990N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.461260553075476,57.990754500000001]
["glac_bound",384941.000000000000000,"G233129E57606N","2008-05-01T00:00:00",74372.627409810622339,0.074373000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233129E57606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.870720613579991,57.605308500000000]
["glac_bound",384942.000000000000000,"G230143E56441N","2008-05-01T00:00:00",7681289.916341655887663,7.681290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230143E56441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.866044657379291,56.453372999999999]
["glac_bound",384943.000000000000000,"G227432E58287N","2008-05-01T00:00:00",2597245.473057446070015,2.597250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227432E58287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.562970605592795,58.290589499999996]
["glac_bound",384945.000000000000000,"G227212E58326N","2008-05-01T00:00:00",576436.476711492519826,0.576436000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227212E58326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.785291039485941,58.326864499999999]
["glac_bound",384949.000000000000000,"G224685E59883N","2008-05-01T00:00:00",190494.495175314747030,0.190494000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224685E59883N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.317187408766671,59.883720499999995]
["glac_bound",384953.000000000000000,"G223123E59452N","2008-05-01T00:00:00",617366.058723528287373,0.617366000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223123E59452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.878474252808985,59.455900000000000]
["glac_bound",384954.000000000000000,"G225350E59360N","2008-05-01T00:00:00",158783.140159703034442,0.158783000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225350E59360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.650449136398777,59.360035499999995]
["glac_bound",384960.000000000000000,"G227657E57839N","2008-05-01T00:00:00",1816756.067523405654356,1.816760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227657E57839N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.337987254210304,57.843071000000002]
["glac_bound",384963.000000000000000,"G227300E58434N","2008-05-01T00:00:00",56061.922504116126220,0.056062000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227300E58434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.700406786482461,58.434449999999998]
["glac_bound",384965.000000000000000,"G221791E59954N","2008-05-01T00:00:00",117570.363782538493979,0.117570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221791E59954N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.209544802522743,59.953511500000005]
["glac_bound",384967.000000000000000,"G223131E59374N","2008-05-01T00:00:00",367610.125287033792119,0.367610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223131E59374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.867473882951657,59.374044999999995]
["glac_bound",384968.000000000000000,"G229907E57099N","2008-05-01T00:00:00",83465.649846277985489,0.083466000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229907E57099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.092501102401741,57.098794499999997]
["glac_bound",384969.000000000000000,"G229400E56931N","2008-05-01T00:00:00",1866808.319945685565472,1.866810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229400E56931N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.590673036324517,56.933582000000001]
["glac_bound",384971.000000000000000,"G223459E59480N","2008-05-01T00:00:00",81453.653504893023637,0.081454000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223459E59480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.540541162151669,59.479781000000003]
["glac_bound",384979.000000000000000,"G229337E57215N","2008-05-01T00:00:00",3064520.168373778928071,3.064520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229337E57215N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.663570973060331,57.217324500000004]
["glac_bound",384993.000000000000000,"G222980E59134N","2008-05-01T00:00:00",488975.104562953056302,0.488975000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222980E59134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.019058921485083,59.133528499999997]
["glac_bound",384994.000000000000000,"G228075E56927N","2008-05-01T00:00:00",65700.147052496715332,0.065700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228075E56927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.926963100133406,56.927061500000001]
["glac_bound",384996.000000000000000,"G228499E57440N","2008-05-01T00:00:00",372724.379948570975102,0.372724000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228499E57440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.500042768068283,57.439887999999996]
["glac_bound",384999.000000000000000,"G222398E59909N","2008-05-01T00:00:00",738139.307752063497901,0.738139000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222398E59909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.593905824176460,59.907065500000002]
["glac_bound",385001.000000000000000,"G225072E59546N","2008-05-01T00:00:00",1512302.379648476606235,1.512300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225072E59546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.935351036516920,59.545479999999998]
["glac_bound",385005.000000000000000,"G222406E59641N","2008-05-01T00:00:00",67778.853573609478190,0.067779000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222406E59641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.593101152871384,59.641053499999998]
["glac_bound",385014.000000000000000,"G228891E57524N","2008-05-01T00:00:00",652093.696973645710386,0.652094000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228891E57524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.106943969331326,57.523313500000000]
["glac_bound",385021.000000000000000,"G224379E59845N","2008-05-01T00:00:00",1562067.856887552887201,1.562070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224379E59845N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.625832166451005,59.842594500000004]
["glac_bound",385026.000000000000000,"G229202E56632N","2008-05-01T00:00:00",75679.758218262228183,0.075680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229202E56632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.798150506153092,56.631713500000004]
["glac_bound",385027.000000000000000,"G223019E59160N","2008-05-01T00:00:00",39660393.455281697213650,39.660400000000003,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223019E59160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.958863903383758,59.170536499999997]
["glac_bound",385030.000000000000000,"G228052E57352N","2008-05-01T00:00:00",105225.836226400555461,0.105226000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228052E57352N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.949367021359933,57.351647999999997]
["glac_bound",385031.000000000000000,"G227279E57856N","2008-05-01T00:00:00",1545697.115326392930001,1.545700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227279E57856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.725066857388327,57.856301000000002]
["glac_bound",385039.000000000000000,"G223136E59535N","2008-05-01T00:00:00",939747.528478826628998,0.939748000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223136E59535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.865451225689412,59.535148000000000]
["glac_bound",385040.000000000000000,"G229067E56861N","2008-05-01T00:00:00",2125063.915305281057954,2.125060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229067E56861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.945100271944455,56.866027000000003]
["glac_bound",385041.000000000000000,"G222412E59648N","2008-05-01T00:00:00",2485632.026264279149473,2.485630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222412E59648N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.581574832746469,59.651210000000006]
["glac_bound",385042.000000000000000,"G227926E57798N","2008-05-01T00:00:00",3287992.404012241400778,3.287990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227926E57798N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.065587483171242,57.799450000000000]
["glac_bound",385048.000000000000000,"G229547E56232N","2008-05-01T00:00:00",1108708.118932331679389,1.108710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229547E56232N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.448986035249305,56.232410999999999]
["glac_bound",385051.000000000000000,"G230170E56206N","2008-05-01T00:00:00",3564394.910493159200996,3.564390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230170E56206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.825398044896872,56.211502499999995]
["glac_bound",385052.000000000000000,"G228570E57274N","2008-05-01T00:00:00",313719.010496465372853,0.313719000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228570E57274N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.428478705941444,57.274203499999999]
["glac_bound",385059.000000000000000,"G222690E58997N","2008-05-01T00:00:00",160913.792073939868715,0.160914000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222690E58997N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.309146310989490,58.997522500000002]
["glac_bound",385067.000000000000000,"G230032E56051N","2008-05-01T00:00:00",899218.876775408280082,0.899219000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230032E56051N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.967220468009032,56.054553499999997]
["glac_bound",385068.000000000000000,"G225659E59247N","2008-05-01T00:00:00",307614.086246908584144,0.307614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225659E59247N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.341927178325761,59.248008499999997]
["glac_bound",385069.000000000000000,"G228445E56920N","2008-05-01T00:00:00",462013.115026315732393,0.462013000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228445E56920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.553663074121516,56.920220499999999]
["glac_bound",385071.000000000000000,"G229394E56571N","2008-05-01T00:00:00",226247.135489189182408,0.226247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229394E56571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.606342835695614,56.570810999999999]
["glac_bound",385079.000000000000000,"G230258E56363N","2008-05-01T00:00:00",1551874.290279075736180,1.551870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230258E56363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.747584333660512,56.364176999999998]
["glac_bound",385083.000000000000000,"G230404E56719N","2008-05-01T00:00:00",114404.798787927225931,0.114405000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230404E56719N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.595905666295891,56.719612499999997]
["glac_bound",385084.000000000000000,"G229026E56483N","2008-05-01T00:00:00",296106.134096689580474,0.296106000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG229026E56483N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.972698908175857,56.482810499999999]
["glac_bound",385085.000000000000000,"G229369E57182N","2008-05-01T00:00:00",569221.903758576721884,0.569222000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229369E57182N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.631854890072191,57.181561000000002]
["glac_bound",385087.000000000000000,"G230113E55781N","2008-05-01T00:00:00",197622.531028047407744,0.197623000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230113E55781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.883326456893400,55.780110000000001]
["glac_bound",385089.000000000000000,"G228943E56469N","2008-05-01T00:00:00",147867.884591153851943,0.147868000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228943E56469N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.056068181297576,56.468597500000001]
["glac_bound",385093.000000000000000,"G228493E57578N","2008-05-01T00:00:00",677744.180491241742857,0.677744000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228493E57578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.505298906211635,57.579499999999996]
["glac_bound",385096.000000000000000,"G228384E56957N","2008-05-01T00:00:00",997237.589605647837743,0.997238000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228384E56957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.604698846391898,56.953022000000004]
["glac_bound",385099.000000000000000,"G224051E59704N","2008-05-01T00:00:00",2914643.445475531276315,2.914640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224051E59704N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.949585257022250,59.703641500000003]
["glac_bound",385102.000000000000000,"G229297E56962N","2008-05-01T00:00:00",2908591.107170159462839,2.908590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229297E56962N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.696162324938399,56.960842000000000]
["glac_bound",385106.000000000000000,"G227247E58457N","2008-05-01T00:00:00",133438.428568867006106,0.133438000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227247E58457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.753116951614970,58.457261500000001]
["glac_bound",385107.000000000000000,"G222990E59172N","2008-05-01T00:00:00",98965.127653874413227,0.098965000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222990E59172N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.010148175950206,59.171892000000000]
["glac_bound",385115.000000000000000,"G228474E56606N","2008-05-01T00:00:00",197883.275122583116172,0.197883000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228474E56606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.527087785794549,56.609274999999997]
["glac_bound",385118.000000000000000,"G225527E59572N","2008-05-01T00:00:00",544388.274834382697009,0.544388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225527E59572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.484138944353532,59.570729999999998]
["glac_bound",385119.000000000000000,"G222329E59541N","2008-05-01T00:00:00",5820408.588198804296553,5.820410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222329E59541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.669435898930828,59.547347500000001]
["glac_bound",385123.000000000000000,"G230107E56434N","2008-05-01T00:00:00",142426.179389700351749,0.142426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230107E56434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.893495642324694,56.433881499999998]
["glac_bound",385126.000000000000000,"G230794E57544N","2008-05-01T00:00:00",109366.621752109902445,0.109367000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230794E57544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.205953860921511,57.544046000000002]
["glac_bound",385131.000000000000000,"G227153E58317N","2008-05-01T00:00:00",779083.262540684780106,0.779083000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227153E58317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.843430361618346,58.319250999999994]
["glac_bound",385132.000000000000000,"G229219E57169N","2008-05-01T00:00:00",171930.669632802077103,0.171931000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229219E57169N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.782177708766056,57.167977499999999]
["glac_bound",385139.000000000000000,"G229838E56101N","2008-05-01T00:00:00",27140.449462675594987,0.027140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229838E56101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.162295129419874,56.101270000000000]
["glac_bound",385140.000000000000000,"G230519E54664N","2008-05-01T00:00:00",723253.482104729278944,0.723253000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230519E54664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.484486885940385,54.665261999999998]
["glac_bound",385143.000000000000000,"G230391E55771N","2008-05-01T00:00:00",295721.293537082092371,0.295721000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230391E55771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.610697908472019,55.770968500000002]
["glac_bound",385162.000000000000000,"G227914E57488N","2008-05-01T00:00:00",56036.847130613648915,0.056037000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227914E57488N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.085088014450122,57.487054499999999]
["glac_bound",385167.000000000000000,"G227434E58394N","2008-05-01T00:00:00",2170471.217498038895428,2.170470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227434E58394N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.573272867411220,58.401860999999997]
["glac_bound",385168.000000000000000,"G230626E56815N","2008-05-01T00:00:00",312048.538121837074868,0.312049000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230626E56815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.374950065751648,56.814569500000005]
["glac_bound",385169.000000000000000,"G228022E57492N","2008-05-01T00:00:00",595199.617001758655533,0.595200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228022E57492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.977869273499437,57.492325999999998]
["glac_bound",385172.000000000000000,"G229814E56621N","2008-05-01T00:00:00",578659.243128570145927,0.578659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229814E56621N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.184162635223572,56.621278500000003]
["glac_bound",385173.000000000000000,"G230673E56770N","2008-05-01T00:00:00",1100932.624515271978453,1.100930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230673E56770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.328461949457221,56.769943999999995]
["glac_bound",385174.000000000000000,"G228692E56562N","2008-05-01T00:00:00",329639.732905567565467,0.329640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228692E56562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.309365130548628,56.562067499999998]
["glac_bound",385181.000000000000000,"G228636E57168N","2008-05-01T00:00:00",609881.411926828906871,0.609881000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228636E57168N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.364857338001030,57.168252499999994]
["glac_bound",385187.000000000000000,"G229278E56292N","2008-05-01T00:00:00",12960.830896407967884,0.012961000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229278E56292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.721815981060615,56.291832499999998]
["glac_bound",385191.000000000000000,"G229053E57074N","2008-05-01T00:00:00",136694.509547337045660,0.136695000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229053E57074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.948734020238106,57.073688000000004]
["glac_bound",385192.000000000000000,"G228709E57451N","2008-05-01T00:00:00",577815.240960871451534,0.577815000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228709E57451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.291614577822543,57.450866000000005]
["glac_bound",385194.000000000000000,"G230095E55475N","2008-05-01T00:00:00",193781.878619416325819,0.193782000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230095E55475N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.905534780575948,55.476768000000000]
["glac_bound",385196.000000000000000,"G227673E57601N","2008-05-01T00:00:00",103263.955865713680396,0.103264000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227673E57601N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.328173615653100,57.601292999999998]
["glac_bound",385201.000000000000000,"G227548E58135N","2008-05-01T00:00:00",904189.378688334720209,0.904189000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227548E58135N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.450881222440927,58.134463499999995]
["glac_bound",385203.000000000000000,"G227422E57832N","2008-05-01T00:00:00",270210.729754261323251,0.270211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227422E57832N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.577954250593223,57.832450500000000]
["glac_bound",385204.000000000000000,"G230057E55656N","2008-05-01T00:00:00",333918.637528389866930,0.333919000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230057E55656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.944118272203696,55.655872000000002]
["glac_bound",385209.000000000000000,"G230082E55706N","2008-05-01T00:00:00",206059.392854134377558,0.206059000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230082E55706N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.922199111079465,55.706925499999997]
["glac_bound",385210.000000000000000,"G228948E56736N","2008-05-01T00:00:00",1231911.195226515876129,1.231910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228948E56736N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.051846864493569,56.738236000000001]
["glac_bound",385212.000000000000000,"G230698E56724N","2008-05-01T00:00:00",404848.709681837353855,0.404849000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230698E56724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.300889550072242,56.724164500000001]
["glac_bound",385213.000000000000000,"G230956E57491N","2008-05-01T00:00:00",70605.116803847544361,0.070605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230956E57491N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.044252891447343,57.490927999999997]
["glac_bound",385215.000000000000000,"G227540E57745N","2008-05-01T00:00:00",1127352.280765611212701,1.127350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227540E57745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.461102114769744,57.745871999999999]
["glac_bound",385218.000000000000000,"G230758E56697N","2008-05-01T00:00:00",104315.156107515169424,0.104315000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230758E56697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.242265524318753,56.697588000000003]
["glac_bound",385219.000000000000000,"G229357E56673N","2008-05-01T00:00:00",259104.408668294287054,0.259104000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229357E56673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.643545766511266,56.672550999999999]
["glac_bound",385222.000000000000000,"G224977E59330N","2008-05-01T00:00:00",3396575.640844319947064,3.396580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224977E59330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.029293780189448,59.333805999999996]
["glac_bound",385227.000000000000000,"G227840E58069N","2008-05-01T00:00:00",5672145.816092160530388,5.672150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227840E58069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.154011779730240,58.071444499999998]
["glac_bound",385228.000000000000000,"G229260E56442N","2008-05-01T00:00:00",2993761.775462131015956,2.993760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229260E56442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.755048156553414,56.446622500000004]
["glac_bound",385232.000000000000000,"G229138E56438N","2008-05-01T00:00:00",319205.943985915160738,0.319206000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229138E56438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.862603886363644,56.439627500000000]
["glac_bound",385238.000000000000000,"G229419E56877N","2008-05-01T00:00:00",1500129.921886882046238,1.500130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229419E56877N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.578147595577150,56.876897000000000]
["glac_bound",385243.000000000000000,"G230094E56560N","2008-05-01T00:00:00",246306.389602128794650,0.246306000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230094E56560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.905838952519389,56.560530999999997]
["glac_bound",385244.000000000000000,"G229004E57268N","2008-05-01T00:00:00",405194.403767176787369,0.405194000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229004E57268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.992295636553024,57.270190499999998]
["glac_bound",385247.000000000000000,"G225113E59409N","2008-05-01T00:00:00",45427275.180407434701920,45.427300000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Warm Creek Glacier","None","09AA225113E59409N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.899800326030856,59.428281499999997]
["glac_bound",385248.000000000000000,"G225472E59471N","2008-05-01T00:00:00",179199.335440413589822,0.179199000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225472E59471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.530369923583521,59.473269500000001]
["glac_bound",385254.000000000000000,"G225951E59206N","2008-05-01T00:00:00",120320.951041165637434,0.120321000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225951E59206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.048562179570894,59.204785500000000]
["glac_bound",385255.000000000000000,"G223894E59976N","2008-05-01T00:00:00",116606.704124841737212,0.116607000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223894E59976N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.106322827114440,59.975497500000003]
["glac_bound",385259.000000000000000,"G230040E54384N","2008-05-01T00:00:00",590788.458111349260435,0.590788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230040E54384N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.957594399126947,54.382758499999994]
["glac_bound",385260.000000000000000,"G225875E59302N","2008-05-01T00:00:00",468909.332988226320595,0.468909000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225875E59302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.128009297423432,59.303678500000004]
["glac_bound",385261.000000000000000,"G229404E57227N","2008-05-01T00:00:00",131331.005463863984914,0.131331000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229404E57227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.596743373203537,57.227841999999995]
["glac_bound",385265.000000000000000,"G226912E58354N","2008-05-01T00:00:00",2682696.302522486541420,2.682700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226912E58354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.088627259043506,58.358590999999997]
["glac_bound",385266.000000000000000,"G228364E57461N","2008-05-01T00:00:00",684290.766145714209415,0.684291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228364E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.640038081497607,57.464161000000004]
["glac_bound",385276.000000000000000,"G225722E59330N","2008-05-01T00:00:00",2754062.700376539491117,2.754060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225722E59330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.279325742420042,59.334726500000002]
["glac_bound",385283.000000000000000,"G224619E59861N","2008-05-01T00:00:00",132023.177188445377396,0.132023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224619E59861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.380778233301555,59.861282000000003]
["glac_bound",385288.000000000000000,"G227361E58202N","2008-05-01T00:00:00",1493355.528269519796595,1.493360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227361E58202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.640074443459412,58.203291000000000]
["glac_bound",385291.000000000000000,"G230841E56717N","2008-05-01T00:00:00",505692.107956907886546,0.505692000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230841E56717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.162857380321867,56.717579499999999]
["glac_bound",385295.000000000000000,"G229014E56486N","2008-05-01T00:00:00",569125.024819172569551,0.569125000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG229014E56486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.985761882113820,56.486232999999999]
["glac_bound",385299.000000000000000,"G228445E56777N","2008-05-01T00:00:00",1136314.853815461741760,1.136310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228445E56777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.557139031728752,56.777504999999998]
["glac_bound",385303.000000000000000,"G230302E55696N","2008-05-01T00:00:00",701491.950440815067850,0.701492000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230302E55696N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.702977515624980,55.695709500000007]
["glac_bound",385304.000000000000000,"G227890E57802N","2008-05-01T00:00:00",1405266.632964661344886,1.405270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227890E57802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.113728101008149,57.804770000000005]
["glac_bound",385309.000000000000000,"G230874E54918N","2008-05-01T00:00:00",192329.184619643958285,0.192329000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230874E54918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.125024376241726,54.917715999999999]
["glac_bound",385310.000000000000000,"G229412E56868N","2008-05-01T00:00:00",324628.547889843001030,0.324629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229412E56868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.587010571320064,56.868076500000001]
["glac_bound",385315.000000000000000,"G231030E57140N","2008-05-01T00:00:00",106450.891774174422608,0.106451000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231030E57140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.970891712552515,57.139515000000003]
["glac_bound",385317.000000000000000,"G227882E58075N","2008-05-01T00:00:00",246510.883105762040941,0.246511000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227882E58075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.121159380791255,58.074769000000003]
["glac_bound",385319.000000000000000,"G229294E57269N","2008-05-01T00:00:00",325598.125908514251933,0.325598000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229294E57269N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.706803231047900,57.269128499999994]
["glac_bound",385322.000000000000000,"G230402E57430N","2008-05-01T00:00:00",322955.219672925421037,0.322955000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230402E57430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.597815681855167,57.430650999999997]
["glac_bound",385323.000000000000000,"G228516E56857N","2008-05-01T00:00:00",47935473.959833458065987,47.935499999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228516E56857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.435711378867609,56.909435000000002]
["glac_bound",385325.000000000000000,"G230163E56625N","2008-05-01T00:00:00",186685.800353747617919,0.186686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230163E56625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.835949531582202,56.625314500000002]
["glac_bound",385332.000000000000000,"G225796E59104N","2008-05-01T00:00:00",1205311.594326874939725,1.205310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225796E59104N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.205364061739687,59.104225999999997]
["glac_bound",385336.000000000000000,"G223277E59298N","2008-05-01T00:00:00",114086861.84850864112377,114.087000000000003,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223277E59298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.661981503899398,59.333439999999996]
["glac_bound",385341.000000000000000,"G229735E56608N","2008-05-01T00:00:00",2210856.553634507581592,2.210860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229735E56608N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.264488047519649,56.611204000000001]
["glac_bound",385347.000000000000000,"G228978E56571N","2008-05-01T00:00:00",1350127.304573893779889,1.350130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228978E56571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.026201760086849,56.569833500000001]
["glac_bound",385351.000000000000000,"G226992E58032N","2008-05-01T00:00:00",182467.343645476998063,0.182467000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226992E58032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.007735945899896,58.031517500000000]
["glac_bound",385357.000000000000000,"G230526E55948N","2008-05-01T00:00:00",206725.449513301166007,0.206725000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230526E55948N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.475098638806514,55.946490499999996]
["glac_bound",385361.000000000000000,"G229326E57348N","2008-05-01T00:00:00",683290.712778831832111,0.683291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229326E57348N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.674766553909251,57.352838000000006]
["glac_bound",385362.000000000000000,"G228914E57268N","2008-05-01T00:00:00",4129945.357125884387642,4.129950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228914E57268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.074522196763127,57.271146500000000]
["glac_bound",385363.000000000000000,"G229335E56926N","2008-05-01T00:00:00",532987.935002917074598,0.532988000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229335E56926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.667737510340430,56.928629500000000]
["glac_bound",385364.000000000000000,"G228204E57122N","2008-05-01T00:00:00",107229.992819830455119,0.107230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228204E57122N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.795139780695138,57.123108000000002]
["glac_bound",385365.000000000000000,"G230157E56986N","2008-05-01T00:00:00",884570.916343454737216,0.884571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230157E56986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.847411046110096,56.990960500000000]
["glac_bound",385369.000000000000000,"G226444E58861N","2008-05-01T00:00:00",235946.980275995942065,0.235947000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226444E58861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.556828362876900,58.859076500000000]
["glac_bound",385376.000000000000000,"G228801E57461N","2008-05-01T00:00:00",132516.523435902898200,0.132517000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228801E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.198682675325131,57.460679999999996]
["glac_bound",385379.000000000000000,"G222630E59206N","2008-05-01T00:00:00",436558.775794197805226,0.436559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222630E59206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.371278281613627,59.206377000000003]
["glac_bound",385380.000000000000000,"G222415E59316N","2008-05-01T00:00:00",201262.512542311014840,0.201263000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222415E59316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.585964600686907,59.316108000000000]
["glac_bound",385382.000000000000000,"G229076E56402N","2008-05-01T00:00:00",499467.979169316997286,0.499468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229076E56402N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.923757327040846,56.399970499999995]
["glac_bound",385389.000000000000000,"G225714E59143N","2008-05-01T00:00:00",883773.839739665854722,0.883774000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225714E59143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.286045828037373,59.144244999999998]
["glac_bound",385390.000000000000000,"G229163E56509N","2008-05-01T00:00:00",245354.060166837851284,0.245354000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229163E56509N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.837333556733824,56.508340500000003]
["glac_bound",385392.000000000000000,"G230255E54824N","2008-05-01T00:00:00",613848.206534575205296,0.613848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230255E54824N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.747306270222452,54.824466000000001]
["glac_bound",385396.000000000000000,"G225999E59006N","2008-05-01T00:00:00",3054259.263177037704736,3.054260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB225999E59006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.998727398646054,59.005251000000001]
["glac_bound",385399.000000000000000,"G229459E57015N","2008-05-01T00:00:00",392981.269620129489340,0.392981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229459E57015N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.540996705982138,57.015489500000001]
["glac_bound",385405.000000000000000,"G225828E59225N","2008-05-01T00:00:00",207062.165605463320389,0.207062000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225828E59225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.169889636723013,59.226260999999994]
["glac_bound",385406.000000000000000,"G230551E55331N","2008-05-01T00:00:00",1473046.559671219205484,1.473050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230551E55331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.449269062673466,55.330882000000003]
["glac_bound",385416.000000000000000,"G225534E59288N","2008-05-01T00:00:00",2553595.141739876475185,2.553600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225534E59288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.452537182944297,59.290261000000001]
["glac_bound",385417.000000000000000,"G228949E56792N","2008-05-01T00:00:00",607283.270272899884731,0.607283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228949E56792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.055442510961086,56.792757000000002]
["glac_bound",385418.000000000000000,"G229034E57341N","2008-05-01T00:00:00",864738.025972854113206,0.864738000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229034E57341N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.965615109218447,57.342556500000001]
["glac_bound",385425.000000000000000,"G222083E59534N","2008-05-01T00:00:00",329027.567233634297736,0.329028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222083E59534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.919457069474674,59.533513999999997]
["glac_bound",385433.000000000000000,"G226910E58125N","2008-05-01T00:00:00",496819.950458323641215,0.496820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226910E58125N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.090493324302372,58.125017000000000]
["glac_bound",385434.000000000000000,"G225867E59310N","2008-05-01T00:00:00",178081.305118989548646,0.178081000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225867E59310N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.132846042182280,59.309801499999999]
["glac_bound",385437.000000000000000,"G228814E57291N","2008-05-01T00:00:00",1014480.078324954840355,1.014480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228814E57291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.185641542567055,57.291601499999999]
["glac_bound",385440.000000000000000,"G227476E58028N","2008-05-01T00:00:00",2526625.043433050625026,2.526630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227476E58028N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.535605165432116,58.033549999999998]
["glac_bound",385441.000000000000000,"G225096E59512N","2008-05-01T00:00:00",258878.058614220237359,0.258878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225096E59512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.908444734590091,59.512244499999994]
["glac_bound",385443.000000000000000,"G227032E58385N","2008-05-01T00:00:00",683520.715996367507614,0.683521000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227032E58385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.966052529494732,58.382406500000002]
["glac_bound",385451.000000000000000,"G227600E58231N","2008-05-01T00:00:00",2354308.772412610240281,2.354310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227600E58231N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.401214436062844,58.230893000000002]
["glac_bound",385452.000000000000000,"G229703E56199N","2008-05-01T00:00:00",1705465.102549544768408,1.705470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229703E56199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.291778000740749,56.202265499999996]
["glac_bound",385455.000000000000000,"G224650E59745N","2008-05-01T00:00:00",4868962.847371740266681,4.868960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224650E59745N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.354026406074752,59.747195000000005]
["glac_bound",385456.000000000000000,"G221853E59913N","2008-05-01T00:00:00",954459.003503023413941,0.954459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221853E59913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.150217327381426,59.915446000000003]
["glac_bound",385457.000000000000000,"G230367E56157N","2008-05-01T00:00:00",56223.521374273761467,0.056224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230367E56157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.633112837124031,56.157166500000002]
["glac_bound",385461.000000000000000,"G227663E58091N","2008-05-01T00:00:00",3368797.248196178581566,3.368800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227663E58091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.337827360449069,58.091266500000003]
["glac_bound",385462.000000000000000,"G223591E59852N","2008-05-01T00:00:00",6755585.768156842328608,6.755590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223591E59852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.409698945243775,59.852279500000002]
["glac_bound",385471.000000000000000,"G226693E58618N","2008-05-01T00:00:00",327180.434996612137184,0.327180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226693E58618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.306356332625683,58.616893500000003]
["glac_bound",385472.000000000000000,"G221975E59960N","2008-05-01T00:00:00",854990.942367783049121,0.854991000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221975E59960N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.030936213311776,59.961044500000000]
["glac_bound",385476.000000000000000,"G226663E58634N","2008-05-01T00:00:00",495547.410454048833344,0.495547000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226663E58634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.337924546288008,58.637075500000002]
["glac_bound",385481.000000000000000,"G222981E59421N","2008-05-01T00:00:00",4136757.111503270920366,4.136760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222981E59421N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.022068637696407,59.423904999999998]
["glac_bound",385487.000000000000000,"G222171E59677N","2008-05-01T00:00:00",186191.487341913336422,0.186191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222171E59677N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.832410865870145,59.676230000000004]
["glac_bound",385488.000000000000000,"G227074E58191N","2008-05-01T00:00:00",1528933.272977700689808,1.528930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227074E58191N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.923822818052315,58.190534000000000]
["glac_bound",385493.000000000000000,"G228579E57434N","2008-05-01T00:00:00",136955.500160026218509,0.136955000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228579E57434N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.419604380543632,57.434531500000006]
["glac_bound",385494.000000000000000,"G227476E58404N","2008-05-01T00:00:00",193941.951051519368775,0.193942000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227476E58404N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.525175121294865,58.404834000000001]
["glac_bound",385496.000000000000000,"G230287E56310N","2008-05-01T00:00:00",522685.605712839635089,0.522686000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230287E56310N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.707394941296286,56.312464499999997]
["glac_bound",385500.000000000000000,"G230602E54753N","2008-05-01T00:00:00",364268.372325678647030,0.364268000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230602E54753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.396599639637827,54.753118499999999]
["glac_bound",385505.000000000000000,"G223150E59371N","2008-05-01T00:00:00",781000.326786868623458,0.781000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223150E59371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.847989625694879,59.369762000000001]
["glac_bound",385508.000000000000000,"G228876E57127N","2008-05-01T00:00:00",19794377.621817409992218,19.794400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228876E57127N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.147689873024149,57.118199500000003]
["glac_bound",385512.000000000000000,"G225132E59472N","2008-05-01T00:00:00",106413.595208718092181,0.106414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225132E59472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.868493602532681,59.471808499999995]
["glac_bound",385515.000000000000000,"G222129E59712N","2008-05-01T00:00:00",477766.747932090831455,0.477767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222129E59712N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.874073413614894,59.712451000000001]
["glac_bound",385521.000000000000000,"G225388E59558N","2008-05-01T00:00:00",2074741.609985931077972,2.074740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225388E59558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.615395239065606,59.559463000000001]
["glac_bound",385524.000000000000000,"G228057E57067N","2008-05-01T00:00:00",253601.013324818952242,0.253601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228057E57067N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.941834058701687,57.068503500000006]
["glac_bound",385526.000000000000000,"G228031E57428N","2008-05-01T00:00:00",116581.722151146037504,0.116582000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228031E57428N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.968565911584960,57.427777000000006]
["glac_bound",385529.000000000000000,"G228626E57165N","2008-05-01T00:00:00",1095618.354150612140074,1.095620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228626E57165N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.379406881670263,57.170386499999999]
["glac_bound",385534.000000000000000,"G230092E56519N","2008-05-01T00:00:00",3301977.889211730565876,3.301980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230092E56519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.911145556438328,56.520701000000003]
["glac_bound",385540.000000000000000,"G229416E56309N","2008-05-01T00:00:00",164635.373856267920928,0.164635000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229416E56309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.584514354890047,56.309004500000000]
["glac_bound",385541.000000000000000,"G226487E58743N","2008-05-01T00:00:00",4069350.330673116259277,4.069350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226487E58743N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.507738636587533,58.738871000000003]
["glac_bound",385542.000000000000000,"G222287E59666N","2008-05-01T00:00:00",247502.106477728229947,0.247502000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222287E59666N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.713179581138661,59.665722500000001]
["glac_bound",385555.000000000000000,"G230408E56047N","2008-05-01T00:00:00",59362.997905056159652,0.059363000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230408E56047N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.591369794058636,56.046935000000005]
["glac_bound",385565.000000000000000,"G230143E56495N","2008-05-01T00:00:00",96579.953397401041002,0.096580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230143E56495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.855622694867861,56.494305999999995]
["glac_bound",385567.000000000000000,"G228887E57389N","2008-05-01T00:00:00",1300129.607542901532724,1.300130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228887E57389N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.111186493478783,57.389992500000005]
["glac_bound",385569.000000000000000,"G228310E57202N","2008-05-01T00:00:00",482229.364297895284835,0.482229000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228310E57202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.690629137269752,57.204245499999999]
["glac_bound",385574.000000000000000,"G228506E57205N","2008-05-01T00:00:00",71969.469988117096364,0.071970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228506E57205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.492839234564599,57.206059500000002]
["glac_bound",385586.000000000000000,"G229422E57702N","2008-05-01T00:00:00",80544.909770131504047,0.080545000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229422E57702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.578531751332150,57.701777000000000]
["glac_bound",385587.000000000000000,"G227920E57975N","2008-05-01T00:00:00",115033.367696196539328,0.115033000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227920E57975N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.082245072596152,57.975706500000001]
["glac_bound",385588.000000000000000,"G230088E55378N","2008-05-01T00:00:00",834953.182413838338107,0.834953000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230088E55378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.915952608803082,55.377456500000001]
["glac_bound",385590.000000000000000,"G228678E56865N","2008-05-01T00:00:00",23139534.738466445356607,23.139500000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228678E56865N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.319079137754500,56.847187000000005]
["glac_bound",385597.000000000000000,"G227540E57601N","2008-05-01T00:00:00",4531959.495618944987655,4.531960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227540E57601N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.469573670503223,57.608514499999998]
["glac_bound",385606.000000000000000,"G230485E57073N","2008-05-01T00:00:00",349434.268037447065581,0.349434000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230485E57073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.517275628992934,57.075208000000003]
["glac_bound",385607.000000000000000,"G227825E57459N","2008-05-01T00:00:00",334318.869881652761251,0.334319000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227825E57459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.174730261047443,57.458091499999995]
["glac_bound",385608.000000000000000,"G227060E58087N","2008-05-01T00:00:00",7911480.748994697816670,7.911480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227060E58087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.949486076496441,58.107784500000001]
["glac_bound",385611.000000000000000,"G230094E57329N","2008-05-01T00:00:00",118247.934149371460080,0.118248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230094E57329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.906563568929698,57.329346999999999]
["glac_bound",385613.000000000000000,"G228055E57366N","2008-05-01T00:00:00",2627463.653934814501554,2.627460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228055E57366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.951118682827598,57.362811000000001]
["glac_bound",385623.000000000000000,"G224202E59876N","2008-05-01T00:00:00",1327082.100087504601106,1.327080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224202E59876N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.803637336695317,59.879048999999995]
["glac_bound",385629.000000000000000,"G231147E57051N","2008-05-01T00:00:00",129808.976350966375321,0.129809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA231147E57051N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.854547612804879,57.051316000000000]
["glac_bound",385631.000000000000000,"G230819E57111N","2008-05-01T00:00:00",70121.811630147727556,0.070122000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230819E57111N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.182183600108999,57.111976499999997]
["glac_bound",385632.000000000000000,"G227481E58192N","2008-05-01T00:00:00",1704362.690417584264651,1.704360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227481E58192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.521658399374303,58.190203999999994]
["glac_bound",385636.000000000000000,"G232006E58375N","2008-05-01T00:00:00",230075.885783093341161,0.230076000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-15T00:00:00","okay","None","None","08CA232006E58375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.994868493762993,58.374921999999998]
["glac_bound",385639.000000000000000,"G228784E57374N","2008-05-01T00:00:00",67337.567641007481143,0.067338000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228784E57374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.216149820389234,57.374350499999998]
["glac_bound",385641.000000000000000,"G229240E56517N","2008-05-01T00:00:00",322122.759679206996225,0.322123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229240E56517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.760807147011462,56.518946000000000]
["glac_bound",385642.000000000000000,"G230178E56055N","2008-05-01T00:00:00",343902.658802626829129,0.343903000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230178E56055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.827258550487386,56.056842500000002]
["glac_bound",385644.000000000000000,"G230280E56024N","2008-05-01T00:00:00",203049.565454195020720,0.203050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230280E56024N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.721025800546215,56.024019499999994]
["glac_bound",385647.000000000000000,"G230358E56487N","2008-05-01T00:00:00",594593.560916107613593,0.594594000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230358E56487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.642111388617707,56.487169500000000]
["glac_bound",385653.000000000000000,"G230651E54881N","2008-05-01T00:00:00",2615442.292964339256287,2.615440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230651E54881N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.340041415738625,54.880517999999995]
["glac_bound",385656.000000000000000,"G230701E57290N","2008-05-01T00:00:00",2711001.701844597235322,2.711000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230701E57290N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.300342269239081,57.288628500000002]
["glac_bound",385662.000000000000000,"G230203E57305N","2008-05-01T00:00:00",272653.879472678410821,0.272654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230203E57305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.796204387626261,57.305581000000004]
["glac_bound",385667.000000000000000,"G227269E58203N","2008-05-01T00:00:00",1632988.961378453532234,1.632990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227269E58203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.739432575346314,58.207011000000001]
["glac_bound",385669.000000000000000,"G230068E55913N","2008-05-01T00:00:00",148425.783241954573896,0.148426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230068E55913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.930799407534238,55.913511000000000]
["glac_bound",385670.000000000000000,"G224391E59884N","2008-05-01T00:00:00",547019.005792235722765,0.547019000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224391E59884N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.609965030155990,59.884112000000002]
["glac_bound",385674.000000000000000,"G223196E59451N","2008-05-01T00:00:00",1698019.131459217751399,1.698020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223196E59451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.801164502762447,59.451115000000001]
["glac_bound",385682.000000000000000,"G229648E56323N","2008-05-01T00:00:00",291740.010211149987299,0.291740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229648E56323N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.350653473684190,56.323245000000000]
["glac_bound",385693.000000000000000,"G228140E56916N","2008-05-01T00:00:00",61976.520385727591929,0.061976000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228140E56916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.862426923134308,56.913780500000001]
["glac_bound",385694.000000000000000,"G222511E59617N","2008-05-01T00:00:00",397366.527473658730742,0.397367000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222511E59617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.488400525700911,59.618009999999998]
["glac_bound",385695.000000000000000,"G224475E59931N","2008-05-01T00:00:00",334588.150141013087705,0.334588000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224475E59931N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.524809697200396,59.930948000000001]
["glac_bound",385706.000000000000000,"G230212E57298N","2008-05-01T00:00:00",70409.767820631182985,0.070410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230212E57298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.787732690441175,57.298325500000004]
["glac_bound",385709.000000000000000,"G222734E59159N","2008-05-01T00:00:00",52888.129996586736524,0.052888000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222734E59159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.264881226190482,59.158220999999998]
["glac_bound",385711.000000000000000,"G226693E58525N","2008-05-01T00:00:00",291215.768834771704860,0.291216000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226693E58525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.304524229976778,58.525451000000004]
["glac_bound",385717.000000000000000,"G230046E55788N","2008-05-01T00:00:00",138970.017612534924410,0.138970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230046E55788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.955379679960060,55.788002000000006]
["glac_bound",385721.000000000000000,"G225811E59222N","2008-05-01T00:00:00",877808.917057074606419,0.877809000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225811E59222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.187368705574329,59.222590500000003]
["glac_bound",385722.000000000000000,"G230428E56015N","2008-05-01T00:00:00",69817.294135953081422,0.069817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230428E56015N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.571737796466664,56.014578999999998]
["glac_bound",385726.000000000000000,"G225425E59455N","2008-05-01T00:00:00",55395.655715365042852,0.055396000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225425E59455N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.575273769999967,59.454764499999996]
["glac_bound",385728.000000000000000,"G230766E57364N","2008-05-01T00:00:00",164896.134788725757971,0.164896000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230766E57364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.233608960797795,57.367235000000001]
["glac_bound",385730.000000000000000,"G223282E59539N","2008-05-01T00:00:00",519357.660655454499647,0.519358000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223282E59539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.716085932013129,59.539161500000006]
["glac_bound",385733.000000000000000,"G229118E56581N","2008-05-01T00:00:00",89105.100348747015232,0.089105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229118E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.883881939799352,56.583640500000001]
["glac_bound",385735.000000000000000,"G230486E56766N","2008-05-01T00:00:00",75560.237692557158880,0.075560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230486E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.513910850770856,56.765735000000006]
["glac_bound",385736.000000000000000,"G228528E57340N","2008-05-01T00:00:00",64478.714945591811556,0.064479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228528E57340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.470178254090740,57.340488999999998]
["glac_bound",385741.000000000000000,"G221947E59569N","2008-05-01T00:00:00",117414.511763637565309,0.117415000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221947E59569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.051908391760662,59.568331000000001]
["glac_bound",385745.000000000000000,"G230430E54628N","2008-05-01T00:00:00",741889.331227938644588,0.741889000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230430E54628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.567876370702379,54.628834499999996]
["glac_bound",385756.000000000000000,"G230939E56927N","2008-05-01T00:00:00",120291.083825203575543,0.120291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230939E56927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.059575667314164,56.926688499999997]
["glac_bound",385758.000000000000000,"G227879E58081N","2008-05-01T00:00:00",70870.807386465850868,0.070871000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227879E58081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.121044047415637,58.081282500000000]
["glac_bound",385759.000000000000000,"G229976E57003N","2008-05-01T00:00:00",965278.207169060246088,0.965278000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229976E57003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.025058421304237,57.002864000000002]
["glac_bound",385761.000000000000000,"G225535E59232N","2008-05-01T00:00:00",10113778.591260997578502,10.113799999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225504E59228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.494470487570112,59.242418000000001]
["glac_bound",385763.000000000000000,"G230157E55742N","2008-05-01T00:00:00",79300.998969868960558,0.079301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230157E55742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.841664959792467,55.741878000000000]
["glac_bound",385764.000000000000000,"G230370E54903N","2008-05-01T00:00:00",90112.993370028998470,0.090113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230370E54903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.631073187037828,54.902740999999999]
["glac_bound",385766.000000000000000,"G227515E58236N","2008-05-01T00:00:00",256382.298282023228239,0.256382000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227515E58236N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.485145447078764,58.237911499999996]
["glac_bound",385767.000000000000000,"G230437E56225N","2008-05-01T00:00:00",375800.730487988796085,0.375801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230437E56225N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.563032410576113,56.224983000000002]
["glac_bound",385771.000000000000000,"G227885E57520N","2008-05-01T00:00:00",357973.622734740667511,0.357974000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227885E57520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.115755593635072,57.520459000000002]
["glac_bound",385772.000000000000000,"G229887E57124N","2008-05-01T00:00:00",68219.036173683125526,0.068219000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229887E57124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.114611821222610,57.124336999999997]
["glac_bound",385783.000000000000000,"G222992E59120N","2008-05-01T00:00:00",422550.090279009775259,0.422550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222992E59120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.006221121111139,59.119750500000002]
["glac_bound",385785.000000000000000,"G225007E59541N","2008-05-01T00:00:00",88264.735040457497234,0.088265000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225007E59541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.992791907210403,59.541385500000004]
["glac_bound",385786.000000000000000,"G225346E59527N","2008-05-01T00:00:00",103770.326723630525521,0.103770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225346E59527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.652996000000002,59.526379500000004]
["glac_bound",385798.000000000000000,"G225111E59900N","2008-05-01T00:00:00",251236.698819335055305,0.251237000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225111E59900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.889120834642711,59.900727500000002]
["glac_bound",385799.000000000000000,"G224968E59523N","2008-05-01T00:00:00",1307712.334590305574238,1.307710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224968E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.036445312260525,59.523576000000006]
["glac_bound",385802.000000000000000,"G229898E56277N","2008-05-01T00:00:00",67654.095507317586453,0.067654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229898E56277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.100889792565965,56.276308000000000]
["glac_bound",385803.000000000000000,"G224842E59814N","2008-05-01T00:00:00",986818.341230969643220,0.986818000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224842E59814N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.161642415620321,59.813687500000000]
["glac_bound",385804.000000000000000,"G230029E56553N","2008-05-01T00:00:00",313655.094570246583316,0.313655000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230029E56553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.968308668367342,56.551710000000000]
["glac_bound",385806.000000000000000,"G227776E57817N","2008-05-01T00:00:00",245377.783785671577789,0.245378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227776E57817N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.221416096214000,57.819993499999995]
["glac_bound",385813.000000000000000,"G228421E57376N","2008-05-01T00:00:00",114400.139041887799976,0.114400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228421E57376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.578569221296789,57.376777500000003]
["glac_bound",385814.000000000000000,"G229007E57021N","2008-05-01T00:00:00",261126.882852444483433,0.261127000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229007E57021N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.993815451712464,57.021802000000001]
["glac_bound",385816.000000000000000,"G224313E59964N","2008-05-01T00:00:00",96144.418959876653389,0.096144000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224313E59964N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.686296857796293,59.964548500000006]
["glac_bound",385821.000000000000000,"G228057E57350N","2008-05-01T00:00:00",116857.851417090991163,0.116858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228057E57350N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.942974298355750,57.349934000000005]
["glac_bound",385822.000000000000000,"G230379E56164N","2008-05-01T00:00:00",4035983.145531403366476,4.035980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230379E56164N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.634135694929540,56.163850499999995]
["glac_bound",385827.000000000000000,"G230456E55776N","2008-05-01T00:00:00",70812.142551861485117,0.070812000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230456E55776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.544727300518133,55.776449000000000]
["glac_bound",385829.000000000000000,"G231110E55266N","2008-05-01T00:00:00",413191.460367287101690,0.413191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231110E55266N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.891364806582061,55.267453000000003]
["glac_bound",385831.000000000000000,"G228944E56732N","2008-05-01T00:00:00",74233.056989840610186,0.074233000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228944E56732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.059269561297128,56.731498999999999]
["glac_bound",385835.000000000000000,"G229083E57024N","2008-05-01T00:00:00",493245.602270674426109,0.493246000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229083E57024N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.919270263785336,57.024117500000003]
["glac_bound",385836.000000000000000,"G229045E56851N","2008-05-01T00:00:00",78066.838614838503418,0.078067000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229045E56851N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.953774623196466,56.851335500000005]
["glac_bound",385839.000000000000000,"G221896E59901N","2008-05-01T00:00:00",253967.699251122714486,0.253968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221896E59901N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.108122337588497,59.905334500000002]
["glac_bound",385846.000000000000000,"G230532E55168N","2008-05-01T00:00:00",213799.571605189179536,0.213800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230532E55168N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.467341064516120,55.167794000000001]
["glac_bound",385848.000000000000000,"G225939E58811N","2008-05-01T00:00:00",149850477.83394974470138,149.849999999999994,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Tulsequah Glacier","None","08BB225939E58811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.086123987122249,58.837434999999999]
["glac_bound",385849.000000000000000,"G225236E59429N","2008-05-01T00:00:00",24339936.817119993269444,24.339900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225236E59429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.739617722800290,59.430338000000006]
["glac_bound",385856.000000000000000,"G229383E57138N","2008-05-01T00:00:00",87805.746614709147252,0.087806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229383E57138N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.616661347858212,57.137821500000001]
["glac_bound",385860.000000000000000,"G227089E58157N","2008-05-01T00:00:00",3914878.873628785368055,3.914880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227089E58157N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.908282102011498,58.157606999999999]
["glac_bound",385865.000000000000000,"G223327E59485N","2008-05-01T00:00:00",2882868.946909960824996,2.882870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223327E59485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.681507669395870,59.494655500000000]
["glac_bound",385873.000000000000000,"G230422E56130N","2008-05-01T00:00:00",64104.755530373462534,0.064105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230422E56130N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.578538549939026,56.129554499999998]
["glac_bound",385874.000000000000000,"G227644E58081N","2008-05-01T00:00:00",67822.123266151320422,0.067822000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227644E58081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.356513952836679,58.081095000000005]
["glac_bound",385875.000000000000000,"G226782E58517N","2008-05-01T00:00:00",353600.761389036488254,0.353601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226782E58517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.215289305434624,58.515386500000005]
["glac_bound",385877.000000000000000,"G227849E57279N","2008-05-01T00:00:00",2947306.539009689353406,2.947310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227849E57279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.144533073603554,57.291820500000000]
["glac_bound",385885.000000000000000,"G230488E54595N","2008-05-01T00:00:00",3546974.101516350638121,3.546970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230488E54595N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.516135133724248,54.596133500000001]
["glac_bound",385886.000000000000000,"G229960E56742N","2008-05-01T00:00:00",1235412.235547042684630,1.235410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229960E56742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.037788285864423,56.743200000000002]
["glac_bound",385888.000000000000000,"G223824E59760N","2008-05-01T00:00:00",124191.706001412268961,0.124192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223824E59760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.178642987705189,59.761780999999999]
["glac_bound",385890.000000000000000,"G224303E59980N","2008-05-01T00:00:00",110486.598687629142660,0.110487000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224303E59980N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.698900098667821,59.977915499999995]
["glac_bound",385891.000000000000000,"G223792E59669N","2008-05-01T00:00:00",171819.432092287723208,0.171819000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223792E59669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.207626140608596,59.669404499999999]
["glac_bound",385892.000000000000000,"G226790E58728N","2008-05-01T00:00:00",1542347.196824324550107,1.542350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226790E58728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.202916278008303,58.729320999999999]
["glac_bound",385895.000000000000000,"G230368E56135N","2008-05-01T00:00:00",4241016.401015864685178,4.241020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230368E56135N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.647256510249349,56.141722999999999]
["glac_bound",385896.000000000000000,"G230703E56913N","2008-05-01T00:00:00",75073.290589658077806,0.075073000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230703E56913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.298606718854785,56.912026499999996]
["glac_bound",385902.000000000000000,"G230533E54618N","2008-05-01T00:00:00",163343.391950434976025,0.163343000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230533E54618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.467694385807476,54.618030500000003]
["glac_bound",385904.000000000000000,"G225544E59453N","2008-05-01T00:00:00",131365.726222604949726,0.131366000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225544E59453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.456890992227045,59.451679499999997]
["glac_bound",385905.000000000000000,"G227745E57420N","2008-05-01T00:00:00",80674.665167872473830,0.080675000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227745E57420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.255355241444875,57.419958999999999]
["glac_bound",385909.000000000000000,"G223701E59877N","2008-05-01T00:00:00",958982.023559529799968,0.958982000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223701E59877N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.302091872258188,59.877279999999999]
["glac_bound",385910.000000000000000,"G229521E57188N","2008-05-01T00:00:00",2199193.692833816166967,2.199190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229521E57188N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.465697762727700,57.183695999999998]
["glac_bound",385914.000000000000000,"G230144E56775N","2008-05-01T00:00:00",882670.369962155004032,0.882670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230144E56775N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.852300566696215,56.776991499999994]
["glac_bound",385920.000000000000000,"G229319E57439N","2008-05-01T00:00:00",1593747.098964044125751,1.593750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229319E57439N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.680524331380866,57.444879999999998]
["glac_bound",385931.000000000000000,"G230445E56019N","2008-05-01T00:00:00",124438.081188541691517,0.124438000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230445E56019N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.555203897124898,56.019044999999998]
["glac_bound",385936.000000000000000,"G230580E57028N","2008-05-01T00:00:00",91985.676983770536026,0.091986000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230580E57028N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.422510198697069,57.029481500000003]
["glac_bound",385942.000000000000000,"G229413E56318N","2008-05-01T00:00:00",470918.122868293954525,0.470918000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229413E56318N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.584580804402947,56.320032499999996]
["glac_bound",385944.000000000000000,"G223170E59644N","2008-05-01T00:00:00",17133423.609845992177725,17.133400000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223170E59644N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.840196929316051,59.657647499999996]
["glac_bound",385947.000000000000000,"G227371E58237N","2008-05-01T00:00:00",2626814.605168182402849,2.626810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227371E58237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.624604303089541,58.240373500000004]
["glac_bound",385949.000000000000000,"G223324E59575N","2008-05-01T00:00:00",2678142.416983201168478,2.678140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223324E59575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.678842943368920,59.574021000000002]
["glac_bound",385953.000000000000000,"G230380E56966N","2008-05-01T00:00:00",488740.264238793170080,0.488740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230380E56966N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.620909119007791,56.967225499999998]
["glac_bound",385955.000000000000000,"G230847E56983N","2008-05-01T00:00:00",375069.358659691060893,0.375069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230847E56983N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.154144997540783,56.982610000000001]
["glac_bound",385957.000000000000000,"G228505E56792N","2008-05-01T00:00:00",534454.309514038730413,0.534454000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228505E56792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.497435857933027,56.791367999999999]
["glac_bound",385964.000000000000000,"G225946E59211N","2008-05-01T00:00:00",317716.830889160395600,0.317717000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225946E59211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.055310298613790,59.211687499999996]
["glac_bound",385965.000000000000000,"G227826E57518N","2008-05-01T00:00:00",729513.758686246699654,0.729514000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227826E57518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.172630005004550,57.518444000000002]
["glac_bound",385968.000000000000000,"G223335E59459N","2008-05-01T00:00:00",147676.768634594016476,0.147677000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223335E59459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.665675224736617,59.460038499999996]
["glac_bound",385970.000000000000000,"G230457E56308N","2008-05-01T00:00:00",143679.615925927355420,0.143680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230457E56308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.544052113504904,56.308317000000002]
["glac_bound",385980.000000000000000,"G222158E59782N","2008-05-01T00:00:00",5152992.823807921260595,5.152990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222158E59782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.832168595705753,59.792665499999998]
["glac_bound",385981.000000000000000,"G225239E59473N","2008-05-01T00:00:00",278430.884707058372442,0.278431000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225239E59473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.760486695031119,59.472997999999997]
["glac_bound",385988.000000000000000,"G226761E58291N","2008-05-01T00:00:00",54536.503465908172075,0.054537000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226761E58291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.236928448459253,58.289225999999999]
["glac_bound",385990.000000000000000,"G225591E59381N","2008-05-01T00:00:00",52677.921033037724555,0.052678000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225591E59381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.408199461813581,59.380327000000001]
["glac_bound",385991.000000000000000,"G227190E58390N","2008-05-01T00:00:00",2110053.918777695856988,2.110050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227190E58390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.807437892209492,58.390749499999998]
["glac_bound",385993.000000000000000,"G230554E56798N","2008-05-01T00:00:00",277293.309923489287030,0.277293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230554E56798N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.445767878160382,56.798623500000005]
["glac_bound",386000.000000000000000,"G229419E56309N","2008-05-01T00:00:00",78005.404087515169522,0.078005000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229419E56309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.580455324395530,56.309602499999997]
["glac_bound",386001.000000000000000,"G229094E56557N","2008-05-01T00:00:00",147025.890565622044960,0.147026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229094E56557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.907231190852855,56.558765500000000]
["glac_bound",386011.000000000000000,"G230179E56935N","2008-05-01T00:00:00",84531.451069139569881,0.084531000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230179E56935N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.818499442849628,56.934419500000004]
["glac_bound",386013.000000000000000,"G227089E58241N","2008-05-01T00:00:00",173217.377165421086829,0.173217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227089E58241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.911722315886010,58.240448000000001]
["glac_bound",386016.000000000000000,"G228391E57346N","2008-05-01T00:00:00",625203.405496481107548,0.625203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228391E57346N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.607342831772200,57.344836500000000]
["glac_bound",386017.000000000000000,"G230398E56124N","2008-05-01T00:00:00",105568.432636526180431,0.105568000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230398E56124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.601765977367592,56.124359999999996]
["glac_bound",386019.000000000000000,"G223663E59730N","2008-05-01T00:00:00",1555072.661819475004449,1.555070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223663E59730N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.339009499961634,59.732104499999998]
["glac_bound",386022.000000000000000,"G229176E56517N","2008-05-01T00:00:00",87175.150630350763095,0.087175000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229176E56517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.822343462132920,56.517839500000001]
["glac_bound",386027.000000000000000,"G227925E57375N","2008-05-01T00:00:00",159769.731843608664349,0.159770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227925E57375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.073799515661250,57.375719000000004]
["glac_bound",386030.000000000000000,"G225169E59841N","2008-05-01T00:00:00",117771.173647314310074,0.117771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225169E59841N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.831066501215247,59.841231499999999]
["glac_bound",386037.000000000000000,"G228471E56616N","2008-05-01T00:00:00",85327.928800014255103,0.085328000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228471E56616N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.530473414522220,56.617677000000000]
["glac_bound",386053.000000000000000,"G229819E56507N","2008-05-01T00:00:00",17798998.181520041078329,17.798999999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229819E56507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.160837640524903,56.521191999999999]
["glac_bound",386060.000000000000000,"G225444E59330N","2008-05-01T00:00:00",1160839.557687289081514,1.160840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225444E59330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.555865727241780,59.330350500000002]
["glac_bound",386065.000000000000000,"G222292E59873N","2008-05-01T00:00:00",908837.346850380650721,0.908837000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222292E59873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.713612169087753,59.871199000000004]
["glac_bound",386068.000000000000000,"G230742E56524N","2008-05-01T00:00:00",125455.734692443249514,0.125456000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230742E56524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.258523109773535,56.525068000000005]
["glac_bound",386070.000000000000000,"G230057E56522N","2008-05-01T00:00:00",12762114.519590107724071,12.762100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230057E56522N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.946870030769247,56.522704000000004]
["glac_bound",386072.000000000000000,"G228846E57314N","2008-05-01T00:00:00",561461.153183900169097,0.561461000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228846E57314N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.155018260263006,57.313357500000002]
["glac_bound",386074.000000000000000,"G228584E56536N","2008-05-01T00:00:00",5938213.808435834012926,5.938210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228584E56536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.421642104612033,56.528990499999999]
["glac_bound",386080.000000000000000,"G230621E56871N","2008-05-01T00:00:00",56558.732069810597750,0.056559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230621E56871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.378518382786069,56.870947500000000]
["glac_bound",386095.000000000000000,"G230217E56606N","2008-05-01T00:00:00",600010.629107696237043,0.600011000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230217E56606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.783132342718432,56.604317999999999]
["glac_bound",386101.000000000000000,"G229612E56460N","2008-05-01T00:00:00",609399.429121211287566,0.609399000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229612E56460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.388666437682900,56.459914999999995]
["glac_bound",386104.000000000000000,"G224622E59974N","2008-05-01T00:00:00",186641.392939259676496,0.186641000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224622E59974N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.378306717148234,59.974817500000000]
["glac_bound",386105.000000000000000,"G223756E59677N","2008-05-01T00:00:00",77143.361553010254283,0.077143000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223756E59677N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.243102605294098,59.676856999999998]
["glac_bound",386106.000000000000000,"G227804E57438N","2008-05-01T00:00:00",291045.821093993727118,0.291046000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227804E57438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.195353203439311,57.438007499999998]
["glac_bound",386107.000000000000000,"G230846E56437N","2008-05-01T00:00:00",937942.800359497778118,0.937943000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230846E56437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.154541718081703,56.436754999999998]
["glac_bound",386109.000000000000000,"G223713E59565N","2008-05-01T00:00:00",121804.183666412049206,0.121804000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223713E59565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.290621101538704,59.566414999999999]
["glac_bound",386110.000000000000000,"G227644E58272N","2008-05-01T00:00:00",2499468.259863014332950,2.499470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227644E58272N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.359446480220242,58.270416500000003]
["glac_bound",386113.000000000000000,"G230731E56521N","2008-05-01T00:00:00",146776.078700700076297,0.146776000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230731E56521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.270110951944162,56.522569500000003]
["glac_bound",386114.000000000000000,"G230770E55580N","2008-05-01T00:00:00",190548.782320392521797,0.190549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230770E55580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.229571257988880,55.579676500000005]
["glac_bound",386118.000000000000000,"G227858E57952N","2008-05-01T00:00:00",1168107.919015248538926,1.168110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227858E57952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.138752918775424,57.953099999999999]
["glac_bound",386125.000000000000000,"G231378E56032N","2008-05-01T00:00:00",147619.400939523387933,0.147619000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231378E56032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.621780611383826,56.032367999999998]
["glac_bound",386127.000000000000000,"G228719E57018N","2008-05-01T00:00:00",395574.225421930430457,0.395574000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228719E57018N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.279725623385730,57.019340499999998]
["glac_bound",386133.000000000000000,"G230532E55945N","2008-05-01T00:00:00",151766.721423453214811,0.151767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230532E55945N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.468582084979602,55.945543999999998]
["glac_bound",386137.000000000000000,"G229454E56659N","2008-05-01T00:00:00",466443.880443602916785,0.466444000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229454E56659N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.549075741620129,56.651767499999998]
["glac_bound",386138.000000000000000,"G228745E57222N","2008-05-01T00:00:00",12728939.079465603455901,12.728899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228745E57222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.248614137209898,57.235676999999995]
["glac_bound",386141.000000000000000,"G223682E59722N","2008-05-01T00:00:00",809258.784581412794068,0.809259000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223682E59722N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.319011147293878,59.720742500000000]
["glac_bound",386145.000000000000000,"G225402E59482N","2008-05-01T00:00:00",67066.482391712561366,0.067067000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225402E59482N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.597618019088230,59.482278500000000]
["glac_bound",386147.000000000000000,"G230522E56790N","2008-05-01T00:00:00",539515.714748071390204,0.539516000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230522E56790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.478848330280528,56.789698000000001]
["glac_bound",386150.000000000000000,"G228734E57420N","2008-05-01T00:00:00",124919.749764587788377,0.124920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228734E57420N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.267448411132818,57.420066500000004]
["glac_bound",386153.000000000000000,"G223922E59772N","2008-05-01T00:00:00",232250.046496569848387,0.232250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223922E59772N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.077830089703099,59.771689000000002]
["glac_bound",386155.000000000000000,"G229230E57097N","2008-05-01T00:00:00",147059.904247268830659,0.147060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229230E57097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.770569810559010,57.096634000000002]
["glac_bound",386162.000000000000000,"G230149E56428N","2008-05-01T00:00:00",2952954.697106156032532,2.952950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230149E56428N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.848373497452684,56.431440500000001]
["glac_bound",386165.000000000000000,"G224155E59828N","2008-05-01T00:00:00",1200602.512497836723924,1.200600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224155E59828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.853892077433159,59.829332999999998]
["glac_bound",386169.000000000000000,"G228816E57444N","2008-05-01T00:00:00",477506.392855641897768,0.477506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228816E57444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.178384009545454,57.445263999999995]
["glac_bound",386170.000000000000000,"G227114E58112N","2008-05-01T00:00:00",120919.708066880659317,0.120920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227114E58112N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.887499007330803,58.112210000000005]
["glac_bound",386171.000000000000000,"G225545E59459N","2008-05-01T00:00:00",499080.182068967493251,0.499080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225545E59459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.455087413280467,59.459348500000004]
["glac_bound",386176.000000000000000,"G228504E57212N","2008-05-01T00:00:00",317319.056964634102769,0.317319000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228504E57212N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.494943457156239,57.212892499999995]
["glac_bound",386180.000000000000000,"G229191E56381N","2008-05-01T00:00:00",8908001.232877271249890,8.907999999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229191E56381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.820666176294026,56.391928000000000]
["glac_bound",386181.000000000000000,"G225185E59317N","2008-05-01T00:00:00",56541.979457533649111,0.056542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225185E59317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.814426701036865,59.317532499999999]
["glac_bound",386185.000000000000000,"G223133E59564N","2008-05-01T00:00:00",1052471.397123352624476,1.052470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223133E59564N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.867391054285065,59.564405000000001]
["glac_bound",386186.000000000000000,"G225679E59335N","2008-05-01T00:00:00",134984.424457146873465,0.134984000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225679E59335N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.322926523395040,59.336349499999997]
["glac_bound",386189.000000000000000,"G230567E54799N","2008-05-01T00:00:00",242093.397947795427172,0.242093000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230567E54799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.433581528320701,54.799678999999998]
["glac_bound",386192.000000000000000,"G221826E59780N","2008-05-01T00:00:00",301884.157429327082355,0.301884000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221826E59780N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.175382426883971,59.779893000000001]
["glac_bound",386193.000000000000000,"G224578E59845N","2008-05-01T00:00:00",205487.206520325533347,0.205487000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224578E59845N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.422563322036694,59.844357000000002]
["glac_bound",386196.000000000000000,"G227813E57580N","2008-05-01T00:00:00",636007.941525596193969,0.636008000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227813E57580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.186028731171547,57.580497999999999]
["glac_bound",386198.000000000000000,"G226724E58246N","2008-05-01T00:00:00",143360.487992437381763,0.143360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226724E58246N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.275126818965504,58.245998499999999]
["glac_bound",386199.000000000000000,"G230245E54725N","2008-05-01T00:00:00",267148.651718997454736,0.267149000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230245E54725N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.756384452842610,54.725191499999994]
["glac_bound",386201.000000000000000,"G230807E57128N","2008-05-01T00:00:00",110872.172634969625506,0.110872000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230807E57128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.191043115591413,57.129059499999997]
["glac_bound",386205.000000000000000,"G228015E57092N","2008-05-01T00:00:00",5102159.246088920161128,5.102160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228015E57092N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.984159801099054,57.095849500000000]
["glac_bound",386208.000000000000000,"G231446E56216N","2008-05-01T00:00:00",53158.898257384033059,0.053159000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231446E56216N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.554528101388541,56.216026999999997]
["glac_bound",386212.000000000000000,"G228626E57355N","2008-05-01T00:00:00",91276137.420146524906158,91.276100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228626E57355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.376550800641269,57.398234000000002]
["glac_bound",386213.000000000000000,"G226879E58322N","2008-05-01T00:00:00",6118942.326334822922945,6.118940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226879E58322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.131143988513713,58.311993500000000]
["glac_bound",386214.000000000000000,"G228374E57460N","2008-05-01T00:00:00",140512.679235655319644,0.140513000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228374E57460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.626025338768102,57.459564000000000]
["glac_bound",386217.000000000000000,"G227937E57199N","2008-05-01T00:00:00",4615003.779999708756804,4.615000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227937E57199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.045590096608947,57.202780000000004]
["glac_bound",386218.000000000000000,"G227654E57571N","2008-05-01T00:00:00",55561.782211089819612,0.055562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227654E57571N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.346147230809123,57.570727500000004]
["glac_bound",386221.000000000000000,"G223401E59597N","2008-05-01T00:00:00",120059.657995024012052,0.120060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223401E59597N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.599766201218301,59.596943500000002]
["glac_bound",386222.000000000000000,"G226739E58651N","2008-05-01T00:00:00",596099.360519708949141,0.596099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226739E58651N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.256673788901594,58.649288999999996]
["glac_bound",386223.000000000000000,"G227913E57640N","2008-05-01T00:00:00",130973.528987206154852,0.130974000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227913E57640N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.088034424262162,57.640348500000002]
["glac_bound",386224.000000000000000,"G230314E55134N","2008-05-01T00:00:00",203796.666568894113880,0.203797000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230314E55134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.685405033944505,55.133215500000006]
["glac_bound",386225.000000000000000,"G221797E59949N","2008-05-01T00:00:00",58113.287088345510710,0.058113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221797E59949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.206132904836664,59.949979499999998]
["glac_bound",386230.000000000000000,"G221848E59952N","2008-05-01T00:00:00",320830.634199965745211,0.320831000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221848E59952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.153627825066508,59.951557500000000]
["glac_bound",386232.000000000000000,"G229086E56392N","2008-05-01T00:00:00",209846.778915421251440,0.209847000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229086E56392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.914389172911683,56.392923499999995]
["glac_bound",386234.000000000000000,"G222733E59087N","2008-05-01T00:00:00",128351.894494956475683,0.128352000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222734E59087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.267840742258329,59.086800500000003]
["glac_bound",386235.000000000000000,"G228664E56988N","2008-05-01T00:00:00",745787.325492274947464,4.734120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228664E56988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.333472946776624,57.003008500000000]
["glac_bound",386235.000000000000000,"G228664E56988N","2008-05-01T00:00:00",3988336.568780854344368,4.734120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228664E56988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.332870142089234,56.989066500000000]
["glac_bound",386237.000000000000000,"G230051E55634N","2008-05-01T00:00:00",259135.175177261728095,0.259135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230051E55634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.947989399813935,55.633873000000001]
["glac_bound",386240.000000000000000,"G230146E57447N","2008-05-01T00:00:00",203099.575940489245113,0.203100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230146E57447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.855888319478908,57.448126500000001]
["glac_bound",386243.000000000000000,"G229445E57321N","2008-05-01T00:00:00",95133.556629832732142,0.095134000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229445E57321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.554356421324741,57.321235000000001]
["glac_bound",386247.000000000000000,"G229340E57694N","2008-05-01T00:00:00",4143233.659360301215202,4.143230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229340E57694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.655465503972209,57.697647000000003]
["glac_bound",386248.000000000000000,"G229950E57068N","2008-05-01T00:00:00",8014547.665372015908360,8.014550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229950E57068N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.047263647896045,57.067787499999994]
["glac_bound",386258.000000000000000,"G226641E58432N","2008-05-01T00:00:00",15506178.638660207390785,15.506200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226641E58432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.384308750891222,58.458370000000002]
["glac_bound",386259.000000000000000,"G226953E58613N","2008-05-01T00:00:00",103801.729237867315533,0.103802000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226953E58613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.045757076086943,58.614262999999994]
["glac_bound",386265.000000000000000,"G226363E58950N","2008-05-01T00:00:00",279554.826856219966430,0.279555000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226363E58950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.637635194962684,58.952155500000003]
["glac_bound",386268.000000000000000,"G230823E56429N","2008-05-01T00:00:00",461429.060720031789970,0.461429000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230823E56429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.175346139999988,56.429713000000000]
["glac_bound",386270.000000000000000,"G222328E59566N","2008-05-01T00:00:00",2749471.015649056062102,2.749470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222328E59566N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.673765244440290,59.571573000000001]
["glac_bound",386274.000000000000000,"G226903E58317N","2008-05-01T00:00:00",121268.662299494826584,0.121269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226903E58317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.098232831156736,58.316499500000006]
["glac_bound",386281.000000000000000,"G230701E55293N","2008-05-01T00:00:00",58121.683813493320486,0.058122000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230701E55293N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.299323665228997,55.292346500000001]
["glac_bound",386282.000000000000000,"G229313E57356N","2008-05-01T00:00:00",296885.944275968882721,0.296886000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229313E57356N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.688044884236064,57.356054499999999]
["glac_bound",386284.000000000000000,"G226873E58278N","2008-05-01T00:00:00",744019.141904057818465,0.744019000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226873E58278N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.129230107029798,58.285041999999997]
["glac_bound",386288.000000000000000,"G225017E59539N","2008-05-01T00:00:00",651854.713559898664244,0.651855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225017E59539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.979992034542306,59.541714999999996]
["glac_bound",386292.000000000000000,"G224922E59391N","2008-05-01T00:00:00",2044955.182569608790800,2.044960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224922E59391N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.080488957627125,59.388233999999997]
["glac_bound",386296.000000000000000,"G222227E59380N","2008-05-01T00:00:00",396060.314660059404559,0.396060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222227E59380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.772136338824424,59.379255999999998]
["glac_bound",386303.000000000000000,"G226548E58493N","2008-05-01T00:00:00",173684.963902269839309,0.173685000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226548E58493N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.452725537076390,58.494175999999996]
["glac_bound",386308.000000000000000,"G228145E57620N","2008-05-01T00:00:00",372825.837008247210179,0.372826000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228145E57620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.855043575762210,57.620416000000006]
["glac_bound",386313.000000000000000,"G228962E56417N","2008-05-01T00:00:00",726340.274397749104537,0.726340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228962E56417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.037718367187495,56.421772500000003]
["glac_bound",386315.000000000000000,"G230681E55603N","2008-05-01T00:00:00",5389832.619433734565973,5.389830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230681E55603N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.319361014745937,55.614448999999993]
["glac_bound",386318.000000000000000,"G222236E59803N","2008-05-01T00:00:00",28453283.236464891582727,28.453299999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222236E59803N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.760852791916165,59.840229500000000]
["glac_bound",386319.000000000000000,"G223749E59528N","2008-05-01T00:00:00",889905.299501815577969,0.889905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223749E59528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.253316339168663,59.528591499999997]
["glac_bound",386320.000000000000000,"G222945E59218N","2008-05-01T00:00:00",12153241.102595373988152,12.153200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222945E59218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.056554418128002,59.220188999999998]
["glac_bound",386325.000000000000000,"G230675E56758N","2008-05-01T00:00:00",183092.851242076925701,0.183093000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230675E56758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.326686719641089,56.758578999999997]
["glac_bound",386328.000000000000000,"G230267E54580N","2008-05-01T00:00:00",145294.101509063766571,0.145294000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230267E54580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.733575278036994,54.580040499999996]
["glac_bound",386335.000000000000000,"G228051E57095N","2008-05-01T00:00:00",1213236.372011762578040,1.213240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228051E57095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.954806733072047,57.093955500000000]
["glac_bound",386345.000000000000000,"G229229E56369N","2008-05-01T00:00:00",798601.017646743101068,0.798601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229229E56369N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.771951811332087,56.371600000000001]
["glac_bound",386346.000000000000000,"G225171E59628N","2008-05-01T00:00:00",606980.909562468877994,0.606981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225171E59628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.828461098272612,59.628818499999994]
["glac_bound",386348.000000000000000,"G228814E57302N","2008-05-01T00:00:00",492389.472687855770346,0.492389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228814E57302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.186745310023355,57.301954000000002]
["glac_bound",386350.000000000000000,"G230708E55660N","2008-05-01T00:00:00",6214331.958659533411264,6.214330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230708E55660N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.296411938494145,55.673935999999998]
["glac_bound",386353.000000000000000,"G221977E59978N","2008-05-01T00:00:00",1359412.336926493095234,1.359410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221977E59978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.019702873086260,59.977718499999995]
["glac_bound",386357.000000000000000,"G230061E56124N","2008-05-01T00:00:00",590528.380723388982005,0.590528000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230061E56124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.939967969028089,56.125119499999997]
["glac_bound",386358.000000000000000,"G229864E56308N","2008-05-01T00:00:00",1220434.512935573700815,1.220430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229864E56308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.137276903886573,56.308032499999996]
["glac_bound",386361.000000000000000,"G225493E59457N","2008-05-01T00:00:00",405567.380423399386927,0.405567000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225493E59457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.507608665787757,59.457913000000005]
["glac_bound",386363.000000000000000,"G230070E56293N","2008-05-01T00:00:00",17023733.281251668930054,17.023700000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230070E56293N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.910677565529056,56.307012000000000]
["glac_bound",386366.000000000000000,"G229302E57240N","2008-05-01T00:00:00",1338890.172026428859681,1.338890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229302E57240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.699112940337699,57.241841999999998]
["glac_bound",386367.000000000000000,"G223137E59367N","2008-05-01T00:00:00",977945.593741662916727,0.977946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223137E59367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.861906442484496,59.366612000000003]
["glac_bound",386369.000000000000000,"G226436E58905N","2008-05-01T00:00:00",52002.978322021532222,0.052003000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226436E58905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.562733310675867,58.905049500000004]
["glac_bound",386374.000000000000000,"G222967E59456N","2008-05-01T00:00:00",738798.132407555123791,0.738798000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222967E59456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.036286005016535,59.456918000000002]
["glac_bound",386375.000000000000000,"G229521E56704N","2008-05-01T00:00:00",3011135.208325838204473,3.011140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229521E56704N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.479496540167077,56.715210499999998]
["glac_bound",386376.000000000000000,"G222546E58925N","2008-05-01T00:00:00",16296422.375040808692575,16.296399999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222546E58925N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.441605801560854,58.933505499999995]
["glac_bound",386377.000000000000000,"G223766E59966N","2008-05-01T00:00:00",134663.505710990546504,0.134664000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223766E59966N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.235993056602695,59.966039500000001]
["glac_bound",386384.000000000000000,"G224508E59868N","2008-05-01T00:00:00",1245314.728923621820286,1.245310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224508E59868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.489162037063295,59.868539499999997]
["glac_bound",386386.000000000000000,"G223304E59602N","2008-05-01T00:00:00",365389.436150875699241,0.365389000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223304E59602N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.696647637227898,59.603158499999999]
["glac_bound",386389.000000000000000,"G230381E55532N","2008-05-01T00:00:00",1478407.481929392786697,1.478410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230381E55532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.613140396953838,55.530069499999996]
["glac_bound",386392.000000000000000,"G224088E59686N","2008-05-01T00:00:00",123595.326206190977246,0.123595000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224088E59686N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.911299080345088,59.686060499999996]
["glac_bound",386395.000000000000000,"G222432E59685N","2008-05-01T00:00:00",131945.233573886129307,0.131945000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222432E59685N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.567991095890420,59.684905999999998]
["glac_bound",386399.000000000000000,"G230444E55136N","2008-05-01T00:00:00",156633.139301108923974,0.156633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230444E55136N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.553298497392973,55.137417999999997]
["glac_bound",386406.000000000000000,"G230291E56890N","2008-05-01T00:00:00",431448.050303378084209,0.431448000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230291E56890N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.713555003528512,56.891842499999996]
["glac_bound",386413.000000000000000,"G227364E58155N","2008-05-01T00:00:00",761317.574452130938880,0.761318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227364E58155N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.635749995797028,58.155788000000001]
["glac_bound",386418.000000000000000,"G224818E59930N","2008-05-01T00:00:00",194689.604590352624655,0.194690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224818E59930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.182470422574056,59.930570000000003]
["glac_bound",386427.000000000000000,"G222261E59326N","2008-05-01T00:00:00",1072589.626535541843623,1.072590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222262E59328N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.740339420928649,59.327348999999998]
["glac_bound",386433.000000000000000,"G222843E59495N","2008-05-01T00:00:00",275383.958676506590564,0.275384000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222843E59495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.157181740223734,59.494636499999999]
["glac_bound",386452.000000000000000,"G230289E56303N","2008-05-01T00:00:00",316978.386132422252558,0.316978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230289E56303N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.709512874976838,56.303067999999996]
["glac_bound",386453.000000000000000,"G230454E55338N","2008-05-01T00:00:00",2365789.779027040116489,2.365790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230454E55338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.548753788209126,55.339067000000000]
["glac_bound",386458.000000000000000,"G222445E59873N","2008-05-01T00:00:00",115241.849682166692219,0.115242000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222445E59873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.557323773362953,59.873593000000000]
["glac_bound",386459.000000000000000,"G227274E58499N","2008-05-01T00:00:00",98016.710067327483557,0.098017000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227274E58499N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.725322624624283,58.498811000000003]
["glac_bound",386467.000000000000000,"G228573E56660N","2008-05-01T00:00:00",1694239.551843318622559,1.694240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228573E56660N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.435772738191304,56.664379499999995]
["glac_bound",386470.000000000000000,"G227469E57828N","2008-05-01T00:00:00",516858.387613181082997,0.516858000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227469E57828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.529982559601365,57.827700999999998]
["glac_bound",386473.000000000000000,"G230040E55757N","2008-05-01T00:00:00",1685768.693279283819720,1.685770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230040E55757N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.960495190269341,55.757714500000006]
["glac_bound",386474.000000000000000,"G229945E57126N","2008-05-01T00:00:00",253117.106166645797202,0.253117000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229945E57126N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.052840601485173,57.126509999999996]
["glac_bound",386479.000000000000000,"G230486E56870N","2008-05-01T00:00:00",100984.566920088531333,0.100985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230486E56870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.514364788764055,56.870108000000002]
["glac_bound",386481.000000000000000,"G230385E56081N","2008-05-01T00:00:00",1137445.210674170637503,1.137450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230385E56081N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.615909611590723,56.081310500000001]
["glac_bound",386482.000000000000000,"G225416E59449N","2008-05-01T00:00:00",155924.244525513902772,0.155924000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225416E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.584611545736891,59.449455499999999]
["glac_bound",386484.000000000000000,"G227965E57624N","2008-05-01T00:00:00",1122566.441876210737973,1.122570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227965E57624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.037856113888893,57.627713499999999]
["glac_bound",386487.000000000000000,"G229412E57204N","2008-05-01T00:00:00",2273912.062552566640079,2.273910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229412E57204N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.587598324882265,57.205095000000000]
["glac_bound",386494.000000000000000,"G226895E58129N","2008-05-01T00:00:00",732708.573376131593250,0.732709000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226895E58129N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.105549566282974,58.128755499999997]
["glac_bound",386501.000000000000000,"G226959E58086N","2008-05-01T00:00:00",16128496.722134148702025,16.128499999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226959E58086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.027660578140541,58.084233499999996]
["glac_bound",386503.000000000000000,"G223440E59340N","2008-05-01T00:00:00",2209753.147965751588345,2.209750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223440E59340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.563672061580860,59.342949500000003]
["glac_bound",386506.000000000000000,"G229159E57029N","2008-05-01T00:00:00",481753.566151737119071,0.481754000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229159E57029N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.841125478033405,57.028831499999995]
["glac_bound",386518.000000000000000,"G230596E55347N","2008-05-01T00:00:00",1930097.488967554876581,1.930100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230596E55347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.405146596404222,55.347363000000001]
["glac_bound",386524.000000000000000,"G229434E57228N","2008-05-01T00:00:00",232286.839958326832857,0.232287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229434E57228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.566578512507306,57.228073500000001]
["glac_bound",386527.000000000000000,"G229361E57209N","2008-05-01T00:00:00",1002607.193789419368841,1.002610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229361E57209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.641295891719096,57.213155499999999]
["glac_bound",386532.000000000000000,"G227982E57371N","2008-05-01T00:00:00",1112923.790470114909112,1.112920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227982E57371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.014326842531233,57.378648999999996]
["glac_bound",386549.000000000000000,"G231016E57400N","2008-05-01T00:00:00",339065.394783445342910,0.339065000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231016E57400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.983878688380088,57.399961500000003]
["glac_bound",386556.000000000000000,"G230681E55558N","2008-05-01T00:00:00",947181.832466143532656,0.947182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230681E55558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.322681818841204,55.560282500000000]
["glac_bound",386557.000000000000000,"G230428E56087N","2008-05-01T00:00:00",79079.254494136752328,0.079079000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230428E56087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.571553309702892,56.088988499999999]
["glac_bound",386561.000000000000000,"G222268E59920N","2008-05-01T00:00:00",624658.417086061323062,0.624658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222268E59920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.738837462116351,59.922352500000002]
["glac_bound",386570.000000000000000,"G230105E56872N","2008-05-01T00:00:00",379152.886822838219814,0.379153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230105E56872N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.890544223404220,56.873460000000001]
["glac_bound",386576.000000000000000,"G228201E57110N","2008-05-01T00:00:00",124175.339626451852382,0.124175000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228201E57110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.799546346364281,57.111537999999996]
["glac_bound",386577.000000000000000,"G227668E57850N","2008-05-01T00:00:00",95694.064060311589856,0.095694000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227668E57850N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.335573986665224,57.850793999999993]
["glac_bound",386582.000000000000000,"G225115E59465N","2008-05-01T00:00:00",467863.796963989560027,0.467864000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225115E59465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.887859655397051,59.466313999999997]
["glac_bound",386586.000000000000000,"G223464E59409N","2008-05-01T00:00:00",1469904.421775496797636,1.469900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223464E59409N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.537728318100335,59.408801999999994]
["glac_bound",386587.000000000000000,"G228384E56666N","2008-05-01T00:00:00",276973.681593378307298,0.276974000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228384E56666N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.615353653370789,56.665582999999998]
["glac_bound",386594.000000000000000,"G225190E59427N","2008-05-01T00:00:00",367515.581972243846394,0.367516000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225190E59427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.810066376718254,59.427509499999999]
["glac_bound",386596.000000000000000,"G225651E59467N","2008-05-01T00:00:00",711844.555001090164296,0.711845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225651E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.354323661711021,59.470195500000003]
["glac_bound",386599.000000000000000,"G229593E57109N","2008-05-01T00:00:00",104762.437385507219005,0.104762000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229593E57109N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.407053126726908,57.108988499999995]
["glac_bound",386600.000000000000000,"G222802E59512N","2008-05-01T00:00:00",467162.767087796295527,0.467163000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222802E59512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.197665210005198,59.512343500000000]
["glac_bound",386601.000000000000000,"G228806E56470N","2008-05-01T00:00:00",1624825.884163443231955,1.624830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228806E56470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.199783990411902,56.473106000000001]
["glac_bound",386613.000000000000000,"G228920E57366N","2008-05-01T00:00:00",1269311.393061905400828,1.269310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228920E57366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.079683336471618,57.365435500000004]
["glac_bound",386627.000000000000000,"G229382E57678N","2008-05-01T00:00:00",777630.401831700466573,0.777630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229382E57678N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.614347483455390,57.681270499999997]
["glac_bound",386636.000000000000000,"G221774E59590N","2008-05-01T00:00:00",379121.482694647740573,0.379121000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221774E59590N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.229422939152073,59.590670000000003]
["glac_bound",386639.000000000000000,"G227713E58074N","2008-05-01T00:00:00",3323805.942328749690205,3.323810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227713E58074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.291443219525945,58.083956999999998]
["glac_bound",386642.000000000000000,"G228789E56494N","2008-05-01T00:00:00",129905.205592160651577,0.129905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228789E56494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.211043762916319,56.493980000000001]
["glac_bound",386645.000000000000000,"G229120E56575N","2008-05-01T00:00:00",88487.257750324686640,0.088487000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229120E56575N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.880511431688149,56.575375999999999]
["glac_bound",386646.000000000000000,"G223203E59705N","2008-05-01T00:00:00",1609811.298106395406649,1.609810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223203E59705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.804430789973793,59.702095999999997]
["glac_bound",386647.000000000000000,"G226550E58790N","2008-05-01T00:00:00",970128.532035169424489,0.970129000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226550E58790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.454219470789212,58.795118000000002]
["glac_bound",386655.000000000000000,"G230649E55294N","2008-05-01T00:00:00",134496.968336714780889,0.134497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230649E55294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351706274771630,55.293588000000000]
["glac_bound",386658.000000000000000,"G230179E55140N","2008-05-01T00:00:00",78690.824575629754690,0.078691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230179E55140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.820583147096386,55.139790000000005]
["glac_bound",386661.000000000000000,"G229531E56239N","2008-05-01T00:00:00",267506.338144369772635,0.267506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229531E56239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.468674879089633,56.239051500000002]
["glac_bound",386663.000000000000000,"G228050E57284N","2008-05-01T00:00:00",61305.203987594999489,0.061305000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228050E57284N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.948858321480770,57.284327000000005]
["glac_bound",386666.000000000000000,"G230849E55035N","2008-05-01T00:00:00",78497.494708499027183,0.078497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230849E55035N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.151944400109869,55.035874000000000]
["glac_bound",386667.000000000000000,"G230176E57450N","2008-05-01T00:00:00",87906.221070282321307,0.087906000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230176E57450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.824253995906815,57.450293500000001]
["glac_bound",386668.000000000000000,"G230117E55656N","2008-05-01T00:00:00",150667.284785131574608,0.150667000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230117E55656N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.884942817817517,55.655664500000000]
["glac_bound",386670.000000000000000,"G228723E57161N","2008-05-01T00:00:00",240277.331176100880839,0.240277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228723E57161N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.277052862379350,57.161529500000000]
["glac_bound",386673.000000000000000,"G229219E56894N","2008-05-01T00:00:00",1788672.012461492326111,1.788670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229219E56894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.782214165976143,56.894652499999999]
["glac_bound",386688.000000000000000,"G227209E58075N","2008-05-01T00:00:00",149170.714211675629485,0.149171000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227209E58075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.790904638140006,58.075097000000000]
["glac_bound",386690.000000000000000,"G230457E57060N","2008-05-01T00:00:00",442468.798628261080012,0.442469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230457E57060N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.541929601072923,57.060581499999998]
["glac_bound",386697.000000000000000,"G225357E59279N","2008-05-01T00:00:00",41087159.354524202644825,41.087200000000003,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225357E59279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.720032238400336,59.293006500000004]
["glac_bound",386698.000000000000000,"G229516E57032N","2008-05-01T00:00:00",57211.050210265078931,0.057211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229516E57032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.483701357142877,57.032189000000002]
["glac_bound",386699.000000000000000,"G228902E57057N","2008-05-01T00:00:00",413286.812695450789761,0.413287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228902E57057N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.097305422587425,57.057372000000001]
["glac_bound",386707.000000000000000,"G225544E59380N","2008-05-01T00:00:00",100845.059696823052946,0.100845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225544E59380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.455694686217498,59.379535000000004]
["glac_bound",386708.000000000000000,"G229932E56554N","2008-05-01T00:00:00",8700616.221561869606376,8.700620000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229932E56554N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.071526934094265,56.559912499999996]
["glac_bound",386713.000000000000000,"G224570E59903N","2008-05-01T00:00:00",96203.469147696523578,0.096203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224570E59903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.426909353371570,59.903452500000000]
["glac_bound",386715.000000000000000,"G228660E57065N","2008-05-01T00:00:00",534698.820721365162171,0.534699000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228660E57065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.341831841305577,57.067806000000004]
["glac_bound",386717.000000000000000,"G230492E57209N","2008-05-01T00:00:00",521131.586456108372658,0.521132000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230492E57209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.506963394570278,57.209611499999994]
["glac_bound",386719.000000000000000,"G230350E54894N","2008-05-01T00:00:00",411843.605568498955108,0.411844000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230350E54894N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.648529023202173,54.895324000000002]
["glac_bound",386721.000000000000000,"G227378E58153N","2008-05-01T00:00:00",742636.722054233308882,0.742637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227378E58153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.622912125073356,58.153433500000006]
["glac_bound",386725.000000000000000,"G227993E57283N","2008-05-01T00:00:00",736354.866603038622998,0.736355000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227993E57283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.005989483574666,57.280937500000000]
["glac_bound",386728.000000000000000,"G222895E59482N","2008-05-01T00:00:00",289807.739703986269888,0.289808000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222895E59482N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.105056426829265,59.482230000000001]
["glac_bound",386733.000000000000000,"G228589E57472N","2008-05-01T00:00:00",64515.915652887160832,0.064516000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228589E57472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.411541194501524,57.471592999999999]
["glac_bound",386736.000000000000000,"G229595E56422N","2008-05-01T00:00:00",246005.356512122030836,0.246005000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229595E56422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.404773316908518,56.421548000000001]
["glac_bound",386739.000000000000000,"G229984E56541N","2008-05-01T00:00:00",65812.297360455209855,0.065812000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229984E56541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.016234453821028,56.540935500000003]
["glac_bound",386741.000000000000000,"G228998E57402N","2008-05-01T00:00:00",248608.900665794819361,0.248609000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228998E57402N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.000143359257152,57.403804500000000]
["glac_bound",386747.000000000000000,"G222031E59926N","2008-05-01T00:00:00",4198126.676456289365888,4.198130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222031E59926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.952393434488840,59.929785000000003]
["glac_bound",386750.000000000000000,"G230626E55365N","2008-05-01T00:00:00",1107916.443216592073441,1.107920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230626E55365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.373708425160970,55.365663499999997]
["glac_bound",386752.000000000000000,"G222903E59313N","2008-05-01T00:00:00",188141.295595511794090,0.188141000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222903E59313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.096439929878045,59.312581999999999]
["glac_bound",386754.000000000000000,"G224656E59864N","2008-05-01T00:00:00",320965.749776566284709,0.320966000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224656E59864N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.342729063166502,59.863809000000003]
["glac_bound",386760.000000000000000,"G228161E57076N","2008-05-01T00:00:00",828364.616239758441225,0.828365000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228161E57076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.841345530816994,57.082938999999996]
["glac_bound",386761.000000000000000,"G227774E57773N","2008-05-01T00:00:00",1419590.205882457550615,1.419590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227774E57773N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.228966004664983,57.775247999999998]
["glac_bound",386762.000000000000000,"G231103E55265N","2008-05-01T00:00:00",63519.349445365463907,0.063519000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231103E55265N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.896494897183231,55.264685000000000]
["glac_bound",386766.000000000000000,"G230139E56322N","2008-05-01T00:00:00",2268194.458229218143970,2.268190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230139E56322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.854546706870224,56.331688999999997]
["glac_bound",386771.000000000000000,"G228585E56650N","2008-05-01T00:00:00",178329.586823691934114,0.178330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228585E56650N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.413705457955700,56.649670499999999]
["glac_bound",386772.000000000000000,"G227290E58137N","2008-05-01T00:00:00",1811816.671679690480232,1.811820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227290E58137N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.713411120030912,58.139415499999998]
["glac_bound",386775.000000000000000,"G229595E56529N","2008-05-01T00:00:00",452166.153756505751517,0.452166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229595E56529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.406036473257586,56.528924000000004]
["glac_bound",386777.000000000000000,"G233038E57755N","2008-05-01T00:00:00",265217.598129609716125,0.265218000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","07EA233038E57755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.963750197983899,57.755124000000002]
["glac_bound",386778.000000000000000,"G227105E58123N","2008-05-01T00:00:00",580407.555522001348436,0.580408000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227105E58123N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.895798744239642,58.122957999999997]
["glac_bound",386779.000000000000000,"G228451E56643N","2008-05-01T00:00:00",75562.036101234160014,0.075562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228451E56643N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.548782323818898,56.642619500000002]
["glac_bound",386788.000000000000000,"G228475E56827N","2008-05-01T00:00:00",623235.722692801966332,0.623236000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228475E56827N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.530079924387735,56.830149000000006]
["glac_bound",386789.000000000000000,"G226386E58884N","2008-05-01T00:00:00",14933420.836602643132210,14.933400000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226442E58871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.598699995789048,58.881263500000003]
["glac_bound",386792.000000000000000,"G222485E59665N","2008-05-01T00:00:00",2586197.457099045626819,2.586200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222485E59665N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.520410255407114,59.666042500000003]
["glac_bound",386793.000000000000000,"G226750E58441N","2008-05-01T00:00:00",1169000.604595042532310,1.169000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226750E58441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.250306810220422,58.440866000000000]
["glac_bound",386795.000000000000000,"G224138E59770N","2008-05-01T00:00:00",93609.694460084938328,0.093610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224138E59770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.862816324900280,59.771055000000004]
["glac_bound",386797.000000000000000,"G223132E59713N","2008-05-01T00:00:00",203187.215013464650838,0.203187000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223132E59713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.868954699882522,59.712851000000001]
["glac_bound",386799.000000000000000,"G230242E56053N","2008-05-01T00:00:00",7817555.809688271023333,7.817560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230242E56053N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.748315105418357,56.069410500000004]
["glac_bound",386805.000000000000000,"G228693E57239N","2008-05-01T00:00:00",251056.327653605694650,0.251056000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228693E57239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.305686427351930,57.239191000000005]
["glac_bound",386806.000000000000000,"G230310E56353N","2008-05-01T00:00:00",616011.887029353412800,0.616012000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230310E56353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.689284227745958,56.352935000000002]
["glac_bound",386812.000000000000000,"G226661E58296N","2008-05-01T00:00:00",7005656.072645969688892,7.005660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226661E58296N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.336468080223881,58.305166000000000]
["glac_bound",386813.000000000000000,"G229150E57082N","2008-05-01T00:00:00",552450.261474203434773,0.552450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229150E57082N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.856289815241212,57.081247500000003]
["glac_bound",386815.000000000000000,"G223437E59450N","2008-05-01T00:00:00",150459.731326274952153,0.150460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223437E59450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.562430773809524,59.449854999999999]
["glac_bound",386816.000000000000000,"G223818E59748N","2008-05-01T00:00:00",3925200.973560153972358,3.925200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223818E59748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.169029172571697,59.748632999999998]
["glac_bound",386818.000000000000000,"G224225E59801N","2008-05-01T00:00:00",2738392.128168593160808,2.738390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224225E59801N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.767533500000013,59.804711499999996]
["glac_bound",386823.000000000000000,"G228754E56647N","2008-05-01T00:00:00",638295.396282016532496,0.638295000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228754E56647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.248056652111643,56.646947999999995]
["glac_bound",386825.000000000000000,"G226805E58562N","2008-05-01T00:00:00",454333.215142946923152,0.454333000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226805E58562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.197479714260112,58.561813999999998]
["glac_bound",386834.000000000000000,"G230387E55631N","2008-05-01T00:00:00",3798375.468183082528412,3.798380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230387E55631N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.614374101950659,55.638512500000004]
["glac_bound",386845.000000000000000,"G226711E58400N","2008-05-01T00:00:00",78002.601899862376740,0.078003000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BD226711E58400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.288985511513147,58.400362500000000]
["glac_bound",386848.000000000000000,"G230459E55782N","2008-05-01T00:00:00",330247.704986077966169,0.330248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230459E55782N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.542819237961567,55.782266499999999]
["glac_bound",386851.000000000000000,"G230409E55683N","2008-05-01T00:00:00",128794.933462103654165,0.128795000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230409E55683N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.592832748943010,55.683864499999999]
["glac_bound",386854.000000000000000,"G230083E55811N","2008-05-01T00:00:00",112476.946031907529687,0.112477000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230083E55811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.916425765899334,55.809782499999997]
["glac_bound",386855.000000000000000,"G229697E56849N","2008-05-01T00:00:00",499869.970262136484962,0.499870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229697E56849N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.304495636914282,56.849958999999998]
["glac_bound",386856.000000000000000,"G229701E56608N","2008-05-01T00:00:00",299908.177214823139366,0.299908000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229701E56608N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.297238101336802,56.607588000000000]
["glac_bound",386858.000000000000000,"G225615E59314N","2008-05-01T00:00:00",256486.366427673841827,0.256486000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225615E59314N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.382627437390710,59.314222500000000]
["glac_bound",386861.000000000000000,"G229692E56458N","2008-05-01T00:00:00",690287.751064041396603,0.690288000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229692E56458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.304193009353469,56.456691499999998]
["glac_bound",386863.000000000000000,"G221753E59893N","2008-05-01T00:00:00",1088599.035880300682038,1.088600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221753E59893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.253502429317564,59.893546999999998]
["glac_bound",386868.000000000000000,"G225431E59522N","2008-05-01T00:00:00",56026.110556945764984,0.056026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225431E59522N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.569174026119413,59.522158500000003]
["glac_bound",386869.000000000000000,"G223108E59559N","2008-05-01T00:00:00",4904117.458748264238238,4.904120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223108E59559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.888820225850736,59.557830500000001]
["glac_bound",386874.000000000000000,"G227835E57467N","2008-05-01T00:00:00",223687.657903295505093,0.223688000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227835E57467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.164412201463790,57.466775499999997]
["glac_bound",386877.000000000000000,"G222522E59184N","2008-05-01T00:00:00",315452.082871932070702,0.315452000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222522E59184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.477894656090825,59.184605500000004]
["glac_bound",386878.000000000000000,"G227577E58359N","2008-05-01T00:00:00",280860.969943979231175,0.280861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227577E58359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.425203548061376,58.360041500000001]
["glac_bound",386881.000000000000000,"G229383E56325N","2008-05-01T00:00:00",931284.683515245676972,0.931285000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229383E56325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.618727408582089,56.324459500000003]
["glac_bound",386883.000000000000000,"G229468E57300N","2008-05-01T00:00:00",233746.168884570040973,0.233746000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229468E57300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.532129219154115,57.300128500000000]
["glac_bound",386889.000000000000000,"G231824E57162N","2008-05-01T00:00:00",237013.709339976165211,0.237014000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EA231824E57162N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.176175535434709,57.162369999999996]
["glac_bound",386890.000000000000000,"G227585E57984N","2008-05-01T00:00:00",168667.739755079441238,0.168668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227585E57984N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.414231215865982,57.983181000000002]
["glac_bound",386893.000000000000000,"G230532E57155N","2008-05-01T00:00:00",55167.013496247280273,0.055167000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230532E57155N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.468150130415950,57.155227500000002]
["glac_bound",386896.000000000000000,"G230513E54680N","2008-05-01T00:00:00",366057.869518458319362,0.366058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230513E54680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.488710047050375,54.679887000000001]
["glac_bound",386899.000000000000000,"G225663E59269N","2008-05-01T00:00:00",275864.114129446446896,0.275864000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225663E59269N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.337046425063960,59.268808999999997]
["glac_bound",386900.000000000000000,"G222267E59289N","2008-05-01T00:00:00",363068.694843650446273,0.363069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222267E59289N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.732716260450161,59.288257000000002]
["glac_bound",386903.000000000000000,"G222518E59879N","2008-05-01T00:00:00",1083837.456674650078639,1.083840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222518E59879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.479917915019513,59.884085999999996]
["glac_bound",386905.000000000000000,"G230193E57453N","2008-05-01T00:00:00",334266.126111409626901,0.334266000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230193E57453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.807792321633059,57.453150500000000]
["glac_bound",386906.000000000000000,"G230389E57416N","2008-05-01T00:00:00",53235.555400456585630,0.053236000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230389E57416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.612439190397339,57.416401000000000]
["glac_bound",386907.000000000000000,"G226878E58401N","2008-05-01T00:00:00",128163.965737962949788,0.128164000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226878E58401N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.122212561111382,58.401502999999998]
["glac_bound",386911.000000000000000,"G226810E58382N","2008-05-01T00:00:00",577652.189509995630942,0.577652000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226810E58382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.190340316936386,58.380939999999995]
["glac_bound",386920.000000000000000,"G224282E59985N","2008-05-01T00:00:00",103052.114077845209977,0.103052000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224282E59985N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.718114133297149,59.986387000000001]
["glac_bound",386921.000000000000000,"G228458E56771N","2008-05-01T00:00:00",1243196.056023615412414,1.243200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228458E56771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.538621794498397,56.769744000000003]
["glac_bound",386925.000000000000000,"G229661E56364N","2008-05-01T00:00:00",9525360.576453635469079,9.525359999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229661E56364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.333872737704922,56.363636000000000]
["glac_bound",386928.000000000000000,"G227677E57424N","2008-05-01T00:00:00",130562.232329769132775,0.130562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BC227677E57424N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.322666160388991,57.423864500000001]
["glac_bound",386933.000000000000000,"G225352E59483N","2008-05-01T00:00:00",2454121.705985286738724,2.454120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225352E59483N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.653862917989443,59.491150500000003]
["glac_bound",386935.000000000000000,"G229224E57050N","2008-05-01T00:00:00",185056.814795184182003,0.185057000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229224E57050N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.775616466275437,57.052186500000005]
["glac_bound",386938.000000000000000,"G222328E59303N","2008-05-01T00:00:00",74563960.401876226067543,74.563999999999993,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Konamoxt Glacier","None","08AB222328E59303N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.704468332761536,59.307769499999999]
["glac_bound",386944.000000000000000,"G227123E58376N","2008-05-01T00:00:00",237803.267222150403541,0.237803000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227123E58376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.874427944485404,58.377881000000002]
["glac_bound",386947.000000000000000,"G230606E56635N","2008-05-01T00:00:00",178884.992688711703522,0.178885000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230606E56635N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.396402225901170,56.634403500000005]
["glac_bound",386950.000000000000000,"G228702E57071N","2008-05-01T00:00:00",263966.330588751763571,0.263966000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228702E57071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.298003230483260,57.071554500000005]
["glac_bound",386955.000000000000000,"G229077E56411N","2008-05-01T00:00:00",1179993.149298396892846,1.179990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229077E56411N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.922693685434183,56.411118999999999]
["glac_bound",386957.000000000000000,"G227497E58309N","2008-05-01T00:00:00",1878546.416317974217236,1.878550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227497E58309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.507033182331099,58.312737499999997]
["glac_bound",386959.000000000000000,"G230576E57038N","2008-05-01T00:00:00",6686846.752936300821602,6.686850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230576E57038N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.412322257094218,57.043613000000001]
["glac_bound",386960.000000000000000,"G230149E54806N","2008-05-01T00:00:00",78355.280746162214200,0.078355000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230149E54806N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.852518426949132,54.805056000000000]
["glac_bound",386967.000000000000000,"G229703E56544N","2008-05-01T00:00:00",2386812.761846359353513,2.386810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229703E56544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.287604159847263,56.551440999999997]
["glac_bound",386969.000000000000000,"G230799E55029N","2008-05-01T00:00:00",182738.883425292093307,0.182739000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230799E55029N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.200456600322724,55.028736000000002]
["glac_bound",386971.000000000000000,"G230617E56873N","2008-05-01T00:00:00",104396.428241729838192,0.104396000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230617E56873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.384421972530134,56.872875499999999]
["glac_bound",386979.000000000000000,"G221644E59740N","2008-05-01T00:00:00",784717.607110166340135,0.784718000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221644E59740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.356236624327437,59.740276000000001]
["glac_bound",386988.000000000000000,"G223507E59866N","2008-05-01T00:00:00",156022.808203034626786,0.156023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223507E59866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.492303743688637,59.866224500000001]
["glac_bound",386995.000000000000000,"G222953E59461N","2008-05-01T00:00:00",126180.790333815413760,0.126181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222953E59461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.047920005634751,59.461779499999999]
["glac_bound",386996.000000000000000,"G223161E59455N","2008-05-01T00:00:00",3288438.890521883033216,3.288440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223161E59455N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.840466102824593,59.461146499999998]
["glac_bound",387009.000000000000000,"G229200E56861N","2008-05-01T00:00:00",1282500.167149326065555,1.282500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229200E56861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.807093359228048,56.863137999999999]
["glac_bound",387011.000000000000000,"G229333E57673N","2008-05-01T00:00:00",1292964.449483531760052,1.292960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229333E57673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.658835759282852,57.679144000000001]
["glac_bound",387012.000000000000000,"G228617E57146N","2008-05-01T00:00:00",241870.852349492779467,0.241871000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228617E57146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.383934712443363,57.145621500000004]
["glac_bound",387013.000000000000000,"G229665E57303N","2008-05-01T00:00:00",208787.068228771386202,0.208787000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229665E57303N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.337694290968813,57.302808499999998]
["glac_bound",387017.000000000000000,"G227223E58453N","2008-05-01T00:00:00",203638.192289632948814,0.203638000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227223E58453N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.777417556542275,58.454186499999999]
["glac_bound",387022.000000000000000,"G226562E58776N","2008-05-01T00:00:00",956034.885005756048486,0.956035000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226562E58776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.442436640536698,58.779991000000003]
["glac_bound",387025.000000000000000,"G228810E56452N","2008-05-01T00:00:00",1323395.694858971051872,1.323400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228810E56452N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.196924975922570,56.454994499999998]
["glac_bound",387027.000000000000000,"G222647E59324N","2008-05-01T00:00:00",941320.150039247237146,0.941320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222647E59324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.356413928873224,59.322321500000001]
["glac_bound",387029.000000000000000,"G229289E56600N","2008-05-01T00:00:00",7192683.109673364087939,7.192680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229289E56600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.734174264611909,56.601461999999998]
["glac_bound",387030.000000000000000,"G231008E57393N","2008-05-01T00:00:00",110371.034066244756104,0.110371000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231008E57393N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.991646929049580,57.392613499999996]
["glac_bound",387031.000000000000000,"G224045E59664N","2008-05-01T00:00:00",579095.320167261525057,0.579095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224045E59664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.952910156206968,59.667668500000005]
["glac_bound",387037.000000000000000,"G227134E58402N","2008-05-01T00:00:00",331647.842288184503559,0.331648000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227134E58402N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.866807089748988,58.402024500000003]
["glac_bound",387038.000000000000000,"G228399E57077N","2008-05-01T00:00:00",452537.145573775982484,0.452537000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228399E57077N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.593529246588901,57.076570000000004]
["glac_bound",387041.000000000000000,"G224052E59893N","2008-05-01T00:00:00",4508536.193295994773507,4.508540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224052E59893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.955388070553852,59.890934999999999]
["glac_bound",387043.000000000000000,"G221457E59849N","2008-05-01T00:00:00",93418.539666118202149,0.093419000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221457E59849N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.545403144451967,59.849602000000004]
["glac_bound",387045.000000000000000,"G228845E57535N","2008-05-01T00:00:00",530528.302911236649379,0.530528000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228845E57535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.153007944118031,57.536697500000002]
["glac_bound",387049.000000000000000,"G225703E59391N","2008-05-01T00:00:00",54626.526101586736331,0.054627000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225703E59391N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.297820681372571,59.390884000000000]
["glac_bound",387052.000000000000000,"G223471E59842N","2008-05-01T00:00:00",499008.275953877950087,0.499008000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223471E59842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.525206799332352,59.843431500000001]
["glac_bound",387058.000000000000000,"G223039E59341N","2008-05-01T00:00:00",761740.529824037686922,0.761741000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223039E59341N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.959946935658536,59.346790999999996]
["glac_bound",387062.000000000000000,"G224976E59514N","2008-05-01T00:00:00",195034.910628168057883,0.195035000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224976E59514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.028812710317254,59.515073500000000]
["glac_bound",387064.000000000000000,"G229390E57752N","2008-05-01T00:00:00",2078693.997299218317494,2.078690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229390E57752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.616863674766108,57.755732500000001]
["glac_bound",387068.000000000000000,"G228567E56796N","2008-05-01T00:00:00",90461.270454895668081,0.090461000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228567E56796N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.433074882787139,56.796149999999997]
["glac_bound",387069.000000000000000,"G222179E59606N","2008-05-01T00:00:00",531813.063925625290722,0.531813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222179E59606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.818984263993173,59.605848500000000]
["glac_bound",387076.000000000000000,"G229952E56786N","2008-05-01T00:00:00",372278.921156491152942,0.372279000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229952E56786N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.045263315997488,56.789186999999998]
["glac_bound",387083.000000000000000,"G230543E55338N","2008-05-01T00:00:00",109781.353080957327620,0.109781000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230543E55338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.456476501509030,55.338645499999998]
["glac_bound",387084.000000000000000,"G227351E58197N","2008-05-01T00:00:00",204122.288637227262370,0.204122000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227351E58197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.647664454847245,58.196339999999999]
["glac_bound",387091.000000000000000,"G229973E56211N","2008-05-01T00:00:00",106130.092937866706052,0.106130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229973E56211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.026307201923089,56.210580499999999]
["glac_bound",387095.000000000000000,"G222463E59202N","2008-05-01T00:00:00",682573.005427412106656,0.682573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222463E59202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.537191231076406,59.207211500000000]
["glac_bound",387103.000000000000000,"G224494E59927N","2008-05-01T00:00:00",653235.123392916284502,0.653235000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224494E59927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.501846200068371,59.929687500000000]
["glac_bound",387109.000000000000000,"G223945E59776N","2008-05-01T00:00:00",74000.215933731626137,0.074000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223945E59776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.058736752882595,59.775636500000005]
["glac_bound",387111.000000000000000,"G227398E58355N","2008-05-01T00:00:00",198933.607753284042701,0.198934000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227398E58355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.603783533967373,58.356644000000003]
["glac_bound",387114.000000000000000,"G233105E57632N","2008-05-01T00:00:00",153467.488876218121732,0.153467000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233105E57632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.895788559149722,57.633032999999998]
["glac_bound",387128.000000000000000,"G228916E57132N","2008-05-01T00:00:00",62423.508289133176731,0.062423000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228916E57132N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.085558319377981,57.132007000000002]
["glac_bound",387131.000000000000000,"G221821E59924N","2008-05-01T00:00:00",126244.389301187678939,0.126244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221821E59924N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.179794095687328,59.924126000000001]
["glac_bound",387141.000000000000000,"G229868E57792N","2008-05-01T00:00:00",152067.661494428582955,0.152068000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229868E57792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.130203693630619,57.791837500000000]
["glac_bound",387142.000000000000000,"G228644E57139N","2008-05-01T00:00:00",3021561.131597462110221,3.021560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228644E57139N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.358077102928519,57.140492000000002]
["glac_bound",387149.000000000000000,"G224307E59988N","2008-05-01T00:00:00",734796.843311119708233,0.734797000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224307E59988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.688667692352880,59.989800000000002]
["glac_bound",387154.000000000000000,"G224694E59867N","2008-05-01T00:00:00",295446.243691315234173,0.295446000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224694E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.308362569095806,59.869574999999998]
["glac_bound",387160.000000000000000,"G221720E59595N","2008-05-01T00:00:00",61971.713372370257275,0.061972000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221720E59595N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.279482634351609,59.596024499999999]
["glac_bound",387161.000000000000000,"G227275E58143N","2008-05-01T00:00:00",822988.602091960259713,0.822989000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227275E58143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.724650284028769,58.146051999999997]
["glac_bound",387163.000000000000000,"G229492E56251N","2008-05-01T00:00:00",5861954.381574755534530,5.861950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","Clara Smith Glacier","None","08DD229492E56251N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.511046726526359,56.257604000000001]
["glac_bound",387176.000000000000000,"G228030E57305N","2008-05-01T00:00:00",1670750.193255213322118,1.670750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228030E57305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.968898309490669,57.304038000000006]
["glac_bound",387182.000000000000000,"G224543E59870N","2008-05-01T00:00:00",613384.848596149124205,0.613385000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224543E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.456414689897713,59.869673000000006]
["glac_bound",387184.000000000000000,"G224904E59732N","2008-05-01T00:00:00",52010.021797461718961,0.052010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224904E59732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.097001705364619,59.731800000000000]
["glac_bound",387188.000000000000000,"G227931E57423N","2008-05-01T00:00:00",186110.451355535944458,0.186110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227931E57423N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.069043787783443,57.425273500000003]
["glac_bound",387192.000000000000000,"G230718E55650N","2008-05-01T00:00:00",147734.241754894464975,0.147734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230718E55650N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.282258582723529,55.649127000000000]
["glac_bound",387194.000000000000000,"G230402E56070N","2008-05-01T00:00:00",294355.843955225311220,0.294356000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230402E56070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.597587728817501,56.069600000000001]
["glac_bound",387198.000000000000000,"G227661E58053N","2008-05-01T00:00:00",1719305.634316159412265,1.719310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227661E58053N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.341667213424785,58.053558500000001]
["glac_bound",387206.000000000000000,"G226274E58882N","2008-05-01T00:00:00",23902865.040519025176764,23.902899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226274E58882N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.730329801785700,58.875462999999996]
["glac_bound",387209.000000000000000,"G230571E57152N","2008-05-01T00:00:00",419709.369015778647736,0.419709000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230571E57152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.431836482292454,57.152443500000004]
["glac_bound",387210.000000000000000,"G228574E56614N","2008-05-01T00:00:00",2487410.162449771538377,2.487410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228574E56614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.431023687317179,56.617620000000002]
["glac_bound",387215.000000000000000,"G227781E57783N","2008-05-01T00:00:00",789833.989991636597551,0.789834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227781E57783N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.221177213779839,57.782927000000001]
["glac_bound",387217.000000000000000,"G222874E59222N","2008-05-01T00:00:00",233977.347570385347353,0.233977000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Taghum Glacier","None","08BF222874E59222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.125429194969058,59.220893500000003]
["glac_bound",387219.000000000000000,"G230832E57110N","2008-05-01T00:00:00",269106.848599283257499,0.269107000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230832E57110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.172932220274959,57.110789499999996]
["glac_bound",387221.000000000000000,"G227763E57925N","2008-05-01T00:00:00",2330587.022807049099356,2.330590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227763E57925N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.250752134703987,57.930275000000002]
["glac_bound",387226.000000000000000,"G228663E56906N","2008-05-01T00:00:00",101846433.32912530004978,101.846000000000004,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228663E56906N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.267041289735459,56.931074500000001]
["glac_bound",387232.000000000000000,"G227627E57972N","2008-05-01T00:00:00",18297816.235302336513996,18.297799999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227627E57972N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.377828138303187,57.984712000000002]
["glac_bound",387238.000000000000000,"G225139E59456N","2008-05-01T00:00:00",2211201.925066269934177,2.211200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225139E59456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.856751198162499,59.460687499999999]
["glac_bound",387239.000000000000000,"G230835E56999N","2008-05-01T00:00:00",107714.005023740479373,0.107714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230835E56999N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.164584832807265,56.999812500000004]
["glac_bound",387243.000000000000000,"G222419E59680N","2008-05-01T00:00:00",181572.279494765738491,0.181572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222419E59680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.580121750431033,59.680051500000005]
["glac_bound",387253.000000000000000,"G230479E56766N","2008-05-01T00:00:00",91392.534324769338127,0.091393000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230479E56766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.519554897143053,56.764571000000004]
["glac_bound",387264.000000000000000,"G230538E57020N","2008-05-01T00:00:00",58910.915579489133961,0.058911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230538E57020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.462622293754009,57.023198999999998]
["glac_bound",387265.000000000000000,"G229566E57002N","2008-05-01T00:00:00",266137.436471817200072,0.266137000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229566E57002N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.435217746824890,57.002358000000001]
["glac_bound",387266.000000000000000,"G226732E58242N","2008-05-01T00:00:00",50442.057422143043368,0.050442000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226732E58242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.268280839910119,58.241961000000003]
["glac_bound",387267.000000000000000,"G229545E56993N","2008-05-01T00:00:00",866767.265254518599249,0.866767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229545E56993N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.455307488605911,56.996246999999997]
["glac_bound",387274.000000000000000,"G230059E56463N","2008-05-01T00:00:00",163348.502177572023356,0.163348000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230059E56463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.941004543421684,56.463121500000000]
["glac_bound",387275.000000000000000,"G228829E57203N","2008-05-01T00:00:00",351927.879836457083002,0.351928000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228829E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.168940304054047,57.202705999999999]
["glac_bound",387278.000000000000000,"G230023E55596N","2008-05-01T00:00:00",259047.877929648471763,0.259048000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230023E55596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.977980647720955,55.595767499999994]
["glac_bound",387290.000000000000000,"G230591E56633N","2008-05-01T00:00:00",164579.235738640185446,0.164579000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230591E56633N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.409811931933973,56.633006500000000]
["glac_bound",387291.000000000000000,"G228987E57017N","2008-05-01T00:00:00",48512561.313430793583393,48.512599999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228987E57017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.059384666684139,57.026747000000000]
["glac_bound",387293.000000000000000,"G231692E56097N","2008-05-01T00:00:00",154028.711268552724505,0.154029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EB231692E56097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.309511566202900,56.097151500000002]
["glac_bound",387297.000000000000000,"G222193E59614N","2008-05-01T00:00:00",618802.543906552949920,0.618803000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222193E59614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.808294829497612,59.613406999999995]
["glac_bound",387305.000000000000000,"G230277E56273N","2008-05-01T00:00:00",234609.519693925714819,0.234610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230277E56273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.724177054046862,56.273251000000002]
["glac_bound",387309.000000000000000,"G227015E58390N","2008-05-01T00:00:00",630410.469068348291330,0.630410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227015E58390N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.986757277706431,58.389217500000001]
["glac_bound",387310.000000000000000,"G230446E56256N","2008-05-01T00:00:00",150214.704873050883180,0.150215000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230446E56256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.552740409627319,56.256658500000000]
["glac_bound",387312.000000000000000,"G230299E56218N","2008-05-01T00:00:00",13945983.223220538347960,13.946000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230299E56218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.670136949437421,56.229317500000001]
["glac_bound",387316.000000000000000,"G231528E56101N","2008-05-01T00:00:00",100564.891304974938976,0.100565000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231528E56101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.471128181408346,56.102291999999998]
["glac_bound",387318.000000000000000,"G224542E59843N","2008-05-01T00:00:00",52894.675487970525865,0.052895000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224542E59843N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.458874877099817,59.843102000000002]
["glac_bound",387323.000000000000000,"G230412E56269N","2008-05-01T00:00:00",193877.579151600977639,0.193878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230412E56269N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.586599750036441,56.267789499999999]
["glac_bound",387324.000000000000000,"G230244E54521N","2008-05-01T00:00:00",51131.043242301304417,0.051131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230244E54521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.756980371951215,54.520074000000001]
["glac_bound",387329.000000000000000,"G224075E59911N","2008-05-01T00:00:00",693937.300659561296925,0.693937000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224075E59911N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.924538345433234,59.911053000000003]
["glac_bound",387347.000000000000000,"G229224E56364N","2008-05-01T00:00:00",80999.121911744456156,0.080999000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229224E56364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.775940131992172,56.364642500000002]
["glac_bound",387348.000000000000000,"G230273E56031N","2008-05-01T00:00:00",1695770.253260928904638,1.695770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230273E56031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.726997429864241,56.035920500000003]
["glac_bound",387349.000000000000000,"G230317E55115N","2008-05-01T00:00:00",144135.127534792467486,0.144135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230317E55115N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.681691965032428,55.115282499999999]
["glac_bound",387351.000000000000000,"G230097E56510N","2008-05-01T00:00:00",103797.770457497157622,0.103798000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230097E56510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.903642400534864,56.509870500000005]
["glac_bound",387362.000000000000000,"G230537E57041N","2008-05-01T00:00:00",185123.964135579182766,0.185124000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230537E57041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.462854289252732,57.041577500000002]
["glac_bound",387366.000000000000000,"G226045E58759N","2008-05-01T00:00:00",1949135.375241977861151,1.949140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226045E58759N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.970558860299604,58.765477000000004]
["glac_bound",387369.000000000000000,"G223058E59316N","2008-05-01T00:00:00",5325530.804046756587923,5.325530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223058E59316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.932585223289607,59.325764500000005]
["glac_bound",387375.000000000000000,"G230365E56693N","2008-05-01T00:00:00",256454.809027365903603,0.256455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230365E56693N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.635015743979807,56.693027499999999]
["glac_bound",387380.000000000000000,"G222592E59354N","2008-05-01T00:00:00",2286835.891688812058419,2.286840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222592E59354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.391549484612284,59.358765000000005]
["glac_bound",387381.000000000000000,"G228939E57044N","2008-05-01T00:00:00",6853362.431577579118311,6.853360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228939E57044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.078008375570448,57.057947499999997]
["glac_bound",387384.000000000000000,"G224315E59877N","2008-05-01T00:00:00",84499.941407233680366,0.084500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224315E59877N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.686610893041234,59.877935500000007]
["glac_bound",387393.000000000000000,"G225334E59484N","2008-05-01T00:00:00",329052.601660468033515,0.329053000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225334E59484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.668004766126842,59.484820999999997]
["glac_bound",387396.000000000000000,"G229920E57055N","2008-05-01T00:00:00",2913528.843475181143731,2.913530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229920E57055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.080641185951578,57.061187500000003]
["glac_bound",387397.000000000000000,"G227087E58417N","2008-05-01T00:00:00",5754233.636435134336352,5.754230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227087E58417N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.911531224379758,58.415424000000002]
["glac_bound",387401.000000000000000,"G228321E57504N","2008-05-01T00:00:00",335495.172220529813785,0.335495000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228321E57504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.682135596871063,57.505633500000002]
["glac_bound",387403.000000000000000,"G230649E55625N","2008-05-01T00:00:00",111606.215296838243376,0.111606000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230649E55625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.351108395845699,55.625201500000003]
["glac_bound",387406.000000000000000,"G226311E58925N","2008-05-01T00:00:00",12387752.364320024847984,12.387800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226311E58925N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.707919372569648,58.932398499999998]
["glac_bound",387407.000000000000000,"G229231E57084N","2008-05-01T00:00:00",183849.310961818438955,0.183849000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229231E57084N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.768294757721833,57.086836500000004]
["glac_bound",387409.000000000000000,"G228802E57406N","2008-05-01T00:00:00",605164.031811046297662,0.605164000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228802E57406N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.197080692975078,57.403739999999999]
["glac_bound",387414.000000000000000,"G230171E55729N","2008-05-01T00:00:00",449544.179133328783792,0.449544000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230171E55729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.829882721654258,55.728596500000002]
["glac_bound",387417.000000000000000,"G228708E57457N","2008-05-01T00:00:00",110663.048686486479710,0.110663000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228708E57457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.291534357059390,57.457082000000000]
["glac_bound",387420.000000000000000,"G225658E59271N","2008-05-01T00:00:00",388943.004613902186975,0.388943000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225658E59271N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.339314827052817,59.272194999999996]
["glac_bound",387433.000000000000000,"G230259E56968N","2008-05-01T00:00:00",275420.515140489034820,0.275421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230259E56968N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.740189734372166,56.967675999999997]
["glac_bound",387436.000000000000000,"G228934E56781N","2008-05-01T00:00:00",239743.588929316640133,0.239744000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228934E56781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.065813414159663,56.780675000000002]
["glac_bound",387440.000000000000000,"G228689E57110N","2008-05-01T00:00:00",639341.467521462007426,0.639341000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228689E57110N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.310318965733103,57.110670499999998]
["glac_bound",387442.000000000000000,"G227555E58029N","2008-05-01T00:00:00",73270775.357260525226593,73.270799999999994,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227555E58029N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.503020147041241,58.073392999999996]
["glac_bound",387443.000000000000000,"G230009E57092N","2008-05-01T00:00:00",101456.053984787431546,0.101456000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230009E57092N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.991992236347755,57.090858499999996]
["glac_bound",387444.000000000000000,"G230672E55234N","2008-05-01T00:00:00",777558.344731579301879,0.777558000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230672E55234N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.331820547030247,55.239273499999996]
["glac_bound",387448.000000000000000,"G228111E57464N","2008-05-01T00:00:00",92852.948110759418341,0.092853000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228111E57464N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.890424480819945,57.464205000000000]
["glac_bound",387454.000000000000000,"G227245E58323N","2008-05-01T00:00:00",56660.156646929957788,0.056660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227245E58323N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.754885294476765,58.322810500000003]
["glac_bound",387458.000000000000000,"G228892E56767N","2008-05-01T00:00:00",7984673.476281877607107,7.984670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228892E56767N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.111243599898501,56.763838499999999]
["glac_bound",387465.000000000000000,"G222015E59553N","2008-05-01T00:00:00",92203.135523521763389,0.092203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222015E59553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.987665833722417,59.553850499999996]
["glac_bound",387467.000000000000000,"G226706E58637N","2008-05-01T00:00:00",518153.294140923244413,0.518153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226706E58637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.295041746931474,58.636289000000005]
["glac_bound",387469.000000000000000,"G229292E57410N","2008-05-01T00:00:00",3545203.638210993725806,3.545200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229292E57410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.703794736778605,57.410286999999997]
["glac_bound",387471.000000000000000,"G228950E56459N","2008-05-01T00:00:00",286598.916301448887680,0.286599000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228950E56459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.050237296325065,56.459508499999998]
["glac_bound",387476.000000000000000,"G230134E56801N","2008-05-01T00:00:00",256086.323582956974860,0.256086000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230134E56801N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.866568869733925,56.800969500000001]
["glac_bound",387478.000000000000000,"G224571E59794N","2008-05-01T00:00:00",3333469.655656021554023,3.333470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224571E59794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.424136423144034,59.796128500000002]
["glac_bound",387479.000000000000000,"G227706E57545N","2008-05-01T00:00:00",937893.841531322221272,0.937894000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227706E57545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.298368784457466,57.544257999999999]
["glac_bound",387481.000000000000000,"G229193E56527N","2008-05-01T00:00:00",52025.469680691530812,0.052026000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229193E56527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.806598506600210,56.527304999999998]
["glac_bound",387483.000000000000000,"G230067E56343N","2008-05-01T00:00:00",365738.435891750676092,0.365738000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230067E56343N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.933506178908203,56.342178000000004]
["glac_bound",387484.000000000000000,"G227760E57430N","2008-05-01T00:00:00",348269.216745544283185,0.348269000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227760E57430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.238611624853803,57.432819000000002]
["glac_bound",387486.000000000000000,"G230616E56995N","2008-05-01T00:00:00",633125.963472574250773,0.633126000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230616E56995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.387217702637599,56.994827000000001]
["glac_bound",387488.000000000000000,"G230252E54521N","2008-05-01T00:00:00",282983.415469445113558,0.282983000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230252E54521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.749122524904067,54.521725500000002]
["glac_bound",387490.000000000000000,"G230322E55746N","2008-05-01T00:00:00",3340393.752480144146830,3.340390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230322E55746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.696015250424466,55.740118500000001]
["glac_bound",387492.000000000000000,"G225721E59353N","2008-05-01T00:00:00",96063.430001980712404,0.096063000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225721E59353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.279702519968055,59.353174500000002]
["glac_bound",387493.000000000000000,"G230692E57298N","2008-05-01T00:00:00",3357810.233159041963518,3.357810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230692E57298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.306248460946506,57.300303000000000]
["glac_bound",387495.000000000000000,"G228046E57479N","2008-05-01T00:00:00",2503345.050094997044653,2.503350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228046E57479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.952609791924090,57.480847999999995]
["glac_bound",387502.000000000000000,"G226873E58334N","2008-05-01T00:00:00",50308.199691817950225,0.050308000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226873E58334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.127410952516016,58.334485999999998]
["glac_bound",387505.000000000000000,"G222692E58955N","2008-05-01T00:00:00",120425.225673261476913,0.120425000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222692E58955N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.309340817302427,58.953375500000000]
["glac_bound",387513.000000000000000,"G227358E58219N","2008-05-01T00:00:00",3914724.614068594761193,3.914720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227358E58219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.640754580597218,58.219965500000001]
["glac_bound",387514.000000000000000,"G222265E59558N","2008-05-01T00:00:00",353348.677030349208508,0.353349000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222265E59558N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.735625246900668,59.558224500000001]
["glac_bound",387517.000000000000000,"G229214E56631N","2008-05-01T00:00:00",727702.881661709980108,0.727703000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229214E56631N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.783372865729348,56.635292500000006]
["glac_bound",387520.000000000000000,"G229200E57017N","2008-05-01T00:00:00",1441044.504755286267027,1.441040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229200E57017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.801071862935714,57.022992500000001]
["glac_bound",387521.000000000000000,"G227148E57963N","2008-05-01T00:00:00",7862428.967892894521356,7.862430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227148E57963N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.886297354232255,57.959158500000001]
["glac_bound",387526.000000000000000,"G226432E58531N","2008-05-01T00:00:00",28628.614559276829823,0.028629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226432E58531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.567272508413453,58.530486000000003]
["glac_bound",387527.000000000000000,"G224630E59858N","2008-05-01T00:00:00",223161.743617249972885,0.223162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224630E59858N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.369518321728577,59.858171999999996]
["glac_bound",387528.000000000000000,"G229361E56326N","2008-05-01T00:00:00",559261.311148801702075,0.559261000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229361E56326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.636424293404446,56.326184499999997]
["glac_bound",387529.000000000000000,"G230391E55667N","2008-05-01T00:00:00",1236915.765317890793085,1.236920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230391E55667N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.610814489044429,55.666520000000006]
["glac_bound",387534.000000000000000,"G222535E59605N","2008-05-01T00:00:00",199076.386997128633084,0.199076000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222535E59605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.464936054956155,59.604851499999995]
["glac_bound",387535.000000000000000,"G226198E58781N","2008-05-01T00:00:00",321118.757160229841247,0.321119000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226198E58781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.803917620282078,58.778639999999996]
["glac_bound",387538.000000000000000,"G222844E59487N","2008-05-01T00:00:00",474892.847007096395828,0.474893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222844E59487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.157793067241698,59.486430999999996]
["glac_bound",387540.000000000000000,"G230799E57135N","2008-05-01T00:00:00",2343946.523236016277224,2.343950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230799E57135N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.201863799625471,57.133910499999999]
["glac_bound",387544.000000000000000,"G230210E56088N","2008-05-01T00:00:00",2293582.097217217087746,2.293580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230210E56088N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.793827278352182,56.087468500000000]
["glac_bound",387545.000000000000000,"G222546E59604N","2008-05-01T00:00:00",138314.617296897427877,0.138315000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222546E59604N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.455937003971769,59.603983999999997]
["glac_bound",387548.000000000000000,"G230289E54572N","2008-05-01T00:00:00",2478806.870206353254616,2.478810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230289E54572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.711678484837904,54.573824500000001]
["glac_bound",387554.000000000000000,"G226991E58399N","2008-05-01T00:00:00",226302.288744279794628,0.226302000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226991E58399N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.011765808513019,58.399789499999997]
["glac_bound",387556.000000000000000,"G229441E56350N","2008-05-01T00:00:00",1357934.833026734413579,1.357930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229441E56350N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.561641283279755,56.351084000000000]
["glac_bound",387559.000000000000000,"G229423E57227N","2008-05-01T00:00:00",841761.047026067040861,0.841761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229423E57227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.580981341838481,57.229377499999998]
["glac_bound",387560.000000000000000,"G227579E58161N","2008-05-01T00:00:00",331188.716587073053233,0.331189000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227579E58161N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.418642285123553,58.161601500000003]
["glac_bound",387561.000000000000000,"G228392E56677N","2008-05-01T00:00:00",75811.804885791672859,0.075812000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228392E56677N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.605926672904843,56.676853999999999]
["glac_bound",387564.000000000000000,"G223163E59487N","2008-05-01T00:00:00",284061.112660423328634,0.284061000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223163E59487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.837934849274916,59.489829499999999]
["glac_bound",387565.000000000000000,"G230153E56139N","2008-05-01T00:00:00",1342789.331133323488757,1.342790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230153E56139N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.843864563497817,56.141058500000000]
["glac_bound",387568.000000000000000,"G230173E56437N","2008-05-01T00:00:00",81435.084803209203528,0.081435000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230173E56437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.825521835276106,56.437311500000000]
["glac_bound",387573.000000000000000,"G230532E57022N","2008-05-01T00:00:00",136125.627124188729795,0.136126000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230532E57022N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.467353380789007,57.022937999999996]
["glac_bound",387577.000000000000000,"G229751E56735N","2008-05-01T00:00:00",1777173.171611840138212,1.777170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229751E56735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.251610617543690,56.736908499999998]
["glac_bound",387578.000000000000000,"G230135E56516N","2008-05-01T00:00:00",73925.015171462946455,0.073925000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230135E56516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.863392767344578,56.517856500000001]
["glac_bound",387582.000000000000000,"G229398E56273N","2008-05-01T00:00:00",65862.473992359242402,0.065863000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229398E56273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.602247158886371,56.272241000000001]
["glac_bound",387584.000000000000000,"G228629E56653N","2008-05-01T00:00:00",397497.777155574120115,0.397498000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228629E56653N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.370935790322591,56.653855000000000]
["glac_bound",387589.000000000000000,"G228581E57038N","2008-05-01T00:00:00",55964.555799451147323,0.055965000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228581E57038N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.417882539059690,57.038271000000002]
["glac_bound",387592.000000000000000,"G230060E56120N","2008-05-01T00:00:00",248596.936454561771825,0.248597000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230060E56120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.945505631132789,56.119050999999999]
["glac_bound",387594.000000000000000,"G230099E57445N","2008-05-01T00:00:00",247750.278361435834086,0.247750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230099E57445N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.899955970283457,57.444631999999999]
["glac_bound",387599.000000000000000,"G225326E59535N","2008-05-01T00:00:00",83320.380058366092271,0.083320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225326E59535N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.674722957773497,59.534680500000000]
["glac_bound",387600.000000000000000,"G228672E57079N","2008-05-01T00:00:00",10434352.870640566572547,10.434400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228672E57079N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.344674880080419,57.094605000000001]
["glac_bound",387601.000000000000000,"G229357E57146N","2008-05-01T00:00:00",191480.131223576812772,0.191480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229357E57146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.645052386630226,57.146136999999996]
["glac_bound",387604.000000000000000,"G230715E56759N","2008-05-01T00:00:00",88146.892913633229909,0.088147000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230715E56759N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.284007914031406,56.759591499999999]
["glac_bound",387610.000000000000000,"G224996E59480N","2008-05-01T00:00:00",3384339.396819184068590,3.384340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224996E59480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.012972989990033,59.479130499999997]
["glac_bound",387616.000000000000000,"G226460E58841N","2008-05-01T00:00:00",817478.266422615968622,0.817478000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226460E58841N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.538293049824631,58.842088000000004]
["glac_bound",387619.000000000000000,"G221631E59915N","2008-05-01T00:00:00",180134.894944416417275,0.180135000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221631E59915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.365698783014807,59.915222499999999]
["glac_bound",387621.000000000000000,"G230355E55642N","2008-05-01T00:00:00",951113.209619710687548,0.951113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230355E55642N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.647285463896139,55.651074500000000]
["glac_bound",387622.000000000000000,"G222506E59817N","2008-05-01T00:00:00",9097494.252329384908080,9.097490000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222506E59817N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.494493262044386,59.826069000000004]
["glac_bound",387625.000000000000000,"G224189E59775N","2008-05-01T00:00:00",96194.168248858826701,0.096194000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224189E59775N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.810479270322986,59.774548499999995]
["glac_bound",387630.000000000000000,"G229373E57302N","2008-05-01T00:00:00",169964.361405586765613,0.169964000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229373E57302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.627403031792340,57.302272000000002]
["glac_bound",387637.000000000000000,"G229885E56376N","2008-05-01T00:00:00",214968.759652311040554,0.214969000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229885E56376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.111948324458467,56.377117499999997]
["glac_bound",387639.000000000000000,"G230247E54429N","2008-05-01T00:00:00",325667.909952324815094,0.325668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230247E54429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.753006216214885,54.429528500000004]
["glac_bound",387641.000000000000000,"G228593E57043N","2008-05-01T00:00:00",543414.366231775842607,0.543414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228593E57043N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.408213000226993,57.046558500000003]
["glac_bound",387644.000000000000000,"G228462E56603N","2008-05-01T00:00:00",116783.702436862135073,0.116784000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228462E56603N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.537334019732839,56.602779499999997]
["glac_bound",387649.000000000000000,"G227438E57917N","2008-05-01T00:00:00",44493733.761972270905972,44.493699999999997,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227438E57917N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.578655230505774,57.921031499999998]
["glac_bound",387652.000000000000000,"G230522E56287N","2008-05-01T00:00:00",104780.133971363480669,0.104780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230522E56287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.479041579294687,56.286081499999995]
["glac_bound",387653.000000000000000,"G229868E57015N","2008-05-01T00:00:00",2620881.693129081744701,2.620880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229868E57015N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.125007064541080,57.020143500000003]
["glac_bound",387654.000000000000000,"G232679E57847N","2008-05-01T00:00:00",112324.677687858958961,0.112325000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232679E57847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.320720712898932,57.847498999999999]
["glac_bound",387657.000000000000000,"G225586E59250N","2008-05-01T00:00:00",1337375.128434250131249,1.337380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225586E59250N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.412423395749755,59.252780000000001]
["glac_bound",387658.000000000000000,"G230134E56258N","2008-05-01T00:00:00",62547.055896884339745,0.062547000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230134E56258N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.865447300461057,56.257548000000000]
["glac_bound",387662.000000000000000,"G230220E56595N","2008-05-01T00:00:00",258812.161756375106052,0.258812000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230220E56595N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.775718458634969,56.593518000000003]
["glac_bound",387665.000000000000000,"G228685E56556N","2008-05-01T00:00:00",260072.173095236852532,0.260072000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228685E56556N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.314154888454766,56.557932000000001]
["glac_bound",387668.000000000000000,"G224253E59996N","2008-05-01T00:00:00",142776.800921569461934,0.142777000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224253E59996N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.748554039517074,59.995000000000005]
["glac_bound",387669.000000000000000,"G226675E58291N","2008-05-01T00:00:00",2655525.662887000478804,2.655530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226675E58291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.333171092724683,58.289540000000002]
["glac_bound",387673.000000000000000,"G226411E58907N","2008-05-01T00:00:00",260784.901239017373882,0.260785000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226411E58907N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.589126950454897,58.907268500000001]
["glac_bound",387682.000000000000000,"G227507E58327N","2008-05-01T00:00:00",925310.380268440232612,0.925310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227507E58327N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.493776418912319,58.327095000000000]
["glac_bound",387684.000000000000000,"G224585E59843N","2008-05-01T00:00:00",87991.237379052559845,0.087991000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224585E59843N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.414843561184000,59.842787000000001]
["glac_bound",387693.000000000000000,"G226928E58241N","2008-05-01T00:00:00",1003556.992638023104519,1.003560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226928E58241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.073647556691469,58.241014000000000]
["glac_bound",387694.000000000000000,"G230127E56775N","2008-05-01T00:00:00",698901.498074364848435,0.698901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230127E56775N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.878703041593383,56.778672999999998]
["glac_bound",387697.000000000000000,"G230778E57133N","2008-05-01T00:00:00",101068.770032955595525,0.101069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230778E57133N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.221063908831923,57.132231000000004]
["glac_bound",387698.000000000000000,"G228090E57099N","2008-05-01T00:00:00",100122.454205229689251,0.100122000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228090E57099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.909865052808868,57.099239499999996]
["glac_bound",387699.000000000000000,"G230173E56279N","2008-05-01T00:00:00",2727949.437645371071994,2.727950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230173E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.831678713349532,56.277602999999999]
["glac_bound",387702.000000000000000,"G222444E59211N","2008-05-01T00:00:00",232518.510176243697060,0.232519000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222444E59211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.556562250000013,59.211609000000003]
["glac_bound",387706.000000000000000,"G230471E56070N","2008-05-01T00:00:00",586360.345496488502249,0.586360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230471E56070N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.526802995945957,56.075407999999996]
["glac_bound",387710.000000000000000,"G230525E55192N","2008-05-01T00:00:00",273549.747440068633296,0.273550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230525E55192N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.475963222155315,55.192482999999996]
["glac_bound",387716.000000000000000,"G225074E59843N","2008-05-01T00:00:00",114437.302840332660708,0.114437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225074E59843N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.924757854485904,59.844317500000002]
["glac_bound",387721.000000000000000,"G229644E56586N","2008-05-01T00:00:00",678478.213460345286876,0.678478000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229644E56586N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.364502416349808,56.591623999999996]
["glac_bound",387724.000000000000000,"G226225E58963N","2008-05-01T00:00:00",669446.751672771875747,0.669447000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226225E58963N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.773257069626169,58.967315499999998]
["glac_bound",387727.000000000000000,"G223218E59793N","2008-05-01T00:00:00",733834.845029314397834,0.733835000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223218E59793N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.783448479742930,59.795006000000001]
["glac_bound",387740.000000000000000,"G225247E59393N","2008-05-01T00:00:00",262883.258345056266990,0.262883000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225247E59393N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.753693614993210,59.393048499999999]
["glac_bound",387741.000000000000000,"G225138E59478N","2008-05-01T00:00:00",56917.063832734187599,0.056917000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225138E59478N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.860317946413687,59.479101000000000]
["glac_bound",387742.000000000000000,"G229245E56770N","2008-05-01T00:00:00",85200.977567479436402,0.085201000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229245E56770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.753862691305869,56.771201500000004]
["glac_bound",387744.000000000000000,"G222441E59658N","2008-05-01T00:00:00",4677029.285886568017304,4.677030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222441E59658N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.556627285476992,59.673536499999997]
["glac_bound",387745.000000000000000,"G229286E56288N","2008-05-01T00:00:00",12026.825619511932018,0.012027000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229286E56288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.713810693103454,56.287508500000001]
["glac_bound",387746.000000000000000,"G222602E59599N","2008-05-01T00:00:00",165441.490167688549263,0.165441000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222602E59599N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.398188834938708,59.598613000000000]
["glac_bound",387747.000000000000000,"G229590E56560N","2008-05-01T00:00:00",72314.141416563245002,0.072314000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229590E56560N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.409079383957248,56.560056500000002]
["glac_bound",387750.000000000000000,"G229475E57173N","2008-05-01T00:00:00",736760.869761532754637,0.736761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229475E57173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.528509735055707,57.172359000000000]
["glac_bound",387752.000000000000000,"G230550E55207N","2008-05-01T00:00:00",2305627.459162428975105,2.305630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230550E55207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.452528765123532,55.209319499999999]
["glac_bound",387765.000000000000000,"G226746E58250N","2008-05-01T00:00:00",120053.347382831590949,0.120053000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226746E58250N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.252299485447367,58.250281000000001]
["glac_bound",387767.000000000000000,"G221930E59892N","2008-05-01T00:00:00",800025.059271986712702,0.800025000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221930E59892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.071275449652575,59.892262500000001]
["glac_bound",387769.000000000000000,"G230730E57256N","2008-05-01T00:00:00",1322493.983815734740347,1.322490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230730E57256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.281033876967399,57.257491000000002]
["glac_bound",387772.000000000000000,"G230274E54886N","2008-05-01T00:00:00",94241.688887537558912,0.094242000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230274E54886N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.725990396855025,54.885289000000000]
["glac_bound",387773.000000000000000,"G226424E58910N","2008-05-01T00:00:00",142831.822771808278048,0.142832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226424E58910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.576090354561586,58.909607500000000]
["glac_bound",387778.000000000000000,"G229896E56265N","2008-05-01T00:00:00",192503.178657049109461,0.192503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229896E56265N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.103282700072356,56.264941000000000]
["glac_bound",387781.000000000000000,"G225821E59232N","2008-05-01T00:00:00",56732.414393896848196,0.056732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225821E59232N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.179851801215989,59.231342999999995]
["glac_bound",387783.000000000000000,"G225359E59324N","2008-05-01T00:00:00",122324.868595173946233,0.122325000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225359E59324N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.641943558010723,59.324107499999997]
["glac_bound",387787.000000000000000,"G228380E56676N","2008-05-01T00:00:00",781210.818748034187593,0.781211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228380E56676N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.618297448653834,56.676908499999996]
["glac_bound",387788.000000000000000,"G231230E57370N","2008-05-01T00:00:00",450179.257723062706646,0.450179000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231230E57370N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.768166261458077,57.370722499999999]
["glac_bound",387796.000000000000000,"G228806E57347N","2008-05-01T00:00:00",269511.417725814564619,0.269511000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228806E57347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.194911838421433,57.346146500000003]
["glac_bound",387803.000000000000000,"G226939E58604N","2008-05-01T00:00:00",546179.883176670642570,0.546180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226939E58604N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.062304838075448,58.603582500000002]
["glac_bound",387807.000000000000000,"G226901E58076N","2008-05-01T00:00:00",73675.506286877032835,0.073676000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226901E58076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.099421860366959,58.075387000000006]
["glac_bound",387808.000000000000000,"G230681E54929N","2008-05-01T00:00:00",737834.391031221952289,0.737834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230681E54929N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.318701472149087,54.930942999999999]
["glac_bound",387810.000000000000000,"G226891E58095N","2008-05-01T00:00:00",2276771.717734624166042,2.276770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226891E58095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.112532112799755,58.102142999999998]
["glac_bound",387812.000000000000000,"G228886E57353N","2008-05-01T00:00:00",77939.144904300017515,0.077939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228886E57353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.113115424528303,57.352443000000001]
["glac_bound",387814.000000000000000,"G228377E57351N","2008-05-01T00:00:00",4988051.304953474551439,4.988050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228377E57351N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.625751788862431,57.357622499999998]
["glac_bound",387815.000000000000000,"G228595E57481N","2008-05-01T00:00:00",121550.224789934291039,0.121550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228595E57481N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.404299599824583,57.481284500000001]
["glac_bound",387820.000000000000000,"G230293E56918N","2008-05-01T00:00:00",168331.139542877615895,0.168331000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230293E56918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.707348557010391,56.918472999999999]
["glac_bound",387832.000000000000000,"G222544E59717N","2008-05-01T00:00:00",159167.580864040122833,0.159168000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222544E59717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.457797407250695,59.717046500000002]
["glac_bound",387837.000000000000000,"G228750E57145N","2008-05-01T00:00:00",77653.050788874053978,0.077653000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228750E57145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.248172639857984,57.145392999999999]
["glac_bound",387840.000000000000000,"G230465E55954N","2008-05-01T00:00:00",69559.104141082993010,0.069559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230465E55954N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.537076029033756,55.954521499999998]
["glac_bound",387841.000000000000000,"G230647E55382N","2008-05-01T00:00:00",96688.912019527197117,0.096689000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230647E55382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.354031019925969,55.382232000000002]
["glac_bound",387845.000000000000000,"G227610E58067N","2008-05-01T00:00:00",295209.273629763396457,0.295209000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227610E58067N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.391795933916427,58.070053000000001]
["glac_bound",387851.000000000000000,"G230061E55916N","2008-05-01T00:00:00",793959.907072168891318,0.793960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230061E55916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.938028072231134,55.916018000000001]
["glac_bound",387852.000000000000000,"G231126E55267N","2008-05-01T00:00:00",503270.533301962015685,0.503271000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231126E55267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.871970251836615,55.268040999999997]
["glac_bound",387855.000000000000000,"G229572E56306N","2008-05-01T00:00:00",678834.496290583629161,0.678834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229572E56306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.430693467542937,56.305423500000003]
["glac_bound",387857.000000000000000,"G226309E58851N","2008-05-01T00:00:00",1210279.420451738871634,1.210280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226309E58851N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.688799760523636,58.850404499999996]
["glac_bound",387862.000000000000000,"G231738E57207N","2008-05-01T00:00:00",121227.922957856819266,0.121228000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231738E57207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.260014697513014,57.206855000000004]
["glac_bound",387878.000000000000000,"G224096E59907N","2008-05-01T00:00:00",108704.856858709099470,0.108705000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224096E59907N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.905857840146666,59.906703000000000]
["glac_bound",387880.000000000000000,"G229596E56376N","2008-05-01T00:00:00",536724.918870163499378,0.536725000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229596E56376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.404199348260477,56.375045499999999]
["glac_bound",387882.000000000000000,"G230395E56240N","2008-05-01T00:00:00",1269570.389298335416242,1.269570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230395E56240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.605878129333178,56.238882500000003]
["glac_bound",387883.000000000000000,"G230299E55638N","2008-05-01T00:00:00",90062.182576244609663,0.090062000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230299E55638N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.699717401344259,55.636972999999998]
["glac_bound",387885.000000000000000,"G228406E57427N","2008-05-01T00:00:00",159386.823824408260407,0.159387000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228406E57427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.592480768505482,57.427543499999999]
["glac_bound",387887.000000000000000,"G227868E57950N","2008-05-01T00:00:00",101215.980897467146860,0.101216000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227868E57950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.132317403100785,57.948376000000003]
["glac_bound",387889.000000000000000,"G228959E56599N","2008-05-01T00:00:00",1378736.995910994941369,1.378740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228959E56599N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.036808830888617,56.598166000000006]
["glac_bound",387890.000000000000000,"G230415E55557N","2008-05-01T00:00:00",426196.719144487695303,0.426197000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230415E55557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.582600716767104,55.558783000000005]
["glac_bound",387894.000000000000000,"G222562E59702N","2008-05-01T00:00:00",402411.464485208969563,0.402411000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222562E59702N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.438742558549762,59.701612499999996]
["glac_bound",387896.000000000000000,"G229044E56648N","2008-05-01T00:00:00",338407.631810520659201,0.338408000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229044E56648N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.956256546808106,56.648876500000000]
["glac_bound",387897.000000000000000,"G230453E54619N","2008-05-01T00:00:00",1409378.516006196849048,1.409380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230453E54619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.543519033151370,54.620732500000003]
["glac_bound",387903.000000000000000,"G229073E56742N","2008-05-01T00:00:00",553646.415371231734753,0.553646000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229073E56742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.927405617457737,56.742996500000004]
["glac_bound",387904.000000000000000,"G229025E56651N","2008-05-01T00:00:00",115362.046971993171610,0.115362000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229025E56651N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.974561266558794,56.651415000000000]
["glac_bound",387907.000000000000000,"G230707E55242N","2008-05-01T00:00:00",201715.334353516256670,0.201715000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230707E55242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.291152025523871,55.242492499999997]
["glac_bound",387909.000000000000000,"G230241E56978N","2008-05-01T00:00:00",1187035.763444121927023,1.187040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230241E56978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.759158581787915,56.979528000000002]
["glac_bound",387910.000000000000000,"G228512E57094N","2008-05-01T00:00:00",250413.608065251755761,0.250414000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228512E57094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.488350895833321,57.093563500000002]
["glac_bound",387912.000000000000000,"G230063E56565N","2008-05-01T00:00:00",213829.419241070718272,0.213829000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230063E56565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.931873797129072,56.562939000000000]
["glac_bound",387914.000000000000000,"G223118E59751N","2008-05-01T00:00:00",191598.846106708951993,0.191599000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223118E59751N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.887476082542321,59.751601000000001]
["glac_bound",387918.000000000000000,"G230401E56405N","2008-05-01T00:00:00",1433158.835162328556180,1.433160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230401E56405N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.597417039193431,56.404769500000000]
["glac_bound",387919.000000000000000,"G223237E59760N","2008-05-01T00:00:00",386266.221626971440855,0.386266000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223237E59760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.760042708731874,59.761904000000001]
["glac_bound",387923.000000000000000,"G224547E59951N","2008-05-01T00:00:00",105942.666432649828494,0.105943000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224547E59951N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.451926162002508,59.951458500000001]
["glac_bound",387925.000000000000000,"G227052E58408N","2008-05-01T00:00:00",62734.554368257275200,0.062735000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227052E58408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.948129337837855,58.408326000000002]
["glac_bound",387937.000000000000000,"G227913E57492N","2008-05-01T00:00:00",339160.186045443813782,0.339160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227913E57492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.086790128022102,57.492863499999999]
["glac_bound",387939.000000000000000,"G225214E59652N","2008-05-01T00:00:00",165406.442333496175706,0.165406000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225214E59652N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.785284585941952,59.653568500000006]
["glac_bound",387942.000000000000000,"G229562E56235N","2008-05-01T00:00:00",522714.315214726608247,0.522714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229562E56235N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.437578666905949,56.234612999999996]
["glac_bound",387943.000000000000000,"G227771E58025N","2008-05-01T00:00:00",704831.649772674893029,0.704832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227771E58025N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.230862436164500,58.025945000000000]
["glac_bound",387944.000000000000000,"G229362E56316N","2008-05-01T00:00:00",728220.806095564039424,0.728221000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229362E56316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.636680013833995,56.315249000000001]
["glac_bound",387950.000000000000000,"G225858E59017N","2008-05-01T00:00:00",171059.159939924284117,0.171059000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225858E59017N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.142285071360163,59.017108500000006]
["glac_bound",387954.000000000000000,"G227645E58261N","2008-05-01T00:00:00",1779682.744561725528911,1.779680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227645E58261N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.354836415096088,58.261006999999999]
["glac_bound",387956.000000000000000,"G227612E58368N","2008-05-01T00:00:00",101689.654523831981351,0.101690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227612E58368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.387972952779080,58.367460500000000]
["glac_bound",387962.000000000000000,"G227659E57903N","2008-05-01T00:00:00",244509.625599107705057,0.244510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227659E57903N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.339819227033331,57.902560500000000]
["glac_bound",387963.000000000000000,"G228912E57541N","2008-05-01T00:00:00",239908.237737091956660,0.239908000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228912E57541N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.089020008261315,57.542209499999998]
["glac_bound",387964.000000000000000,"G227751E57948N","2008-05-01T00:00:00",1244653.914596363436431,1.244650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227751E57948N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.248501102546015,57.947869500000003]
["glac_bound",387967.000000000000000,"G229525E57030N","2008-05-01T00:00:00",255928.361879437929019,0.255928000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229525E57030N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.474555676421403,57.030241500000002]
["glac_bound",387968.000000000000000,"G227336E58136N","2008-05-01T00:00:00",5024467.208009254187346,5.024470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227336E58136N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.663592182499542,58.137094000000005]
["glac_bound",387969.000000000000000,"G230400E55227N","2008-05-01T00:00:00",395161.753040162380785,0.395162000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230400E55227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.598886798137556,55.227766000000003]
["glac_bound",387970.000000000000000,"G230050E56075N","2008-05-01T00:00:00",932041.162263917154633,0.932041000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230050E56075N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.949198364074562,56.072994000000001]
["glac_bound",387972.000000000000000,"G223164E59523N","2008-05-01T00:00:00",280000.909612218674738,0.280001000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223164E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.835743416390500,59.521899500000004]
["glac_bound",387976.000000000000000,"G221723E59763N","2008-05-01T00:00:00",29976165.245611969381571,29.976199999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221723E59763N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.355704458186096,59.765965999999999]
["glac_bound",387977.000000000000000,"G228726E57470N","2008-05-01T00:00:00",148581.961001502990257,0.148582000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228726E57470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.273793783897190,57.469812500000003]
["glac_bound",387979.000000000000000,"G227541E57677N","2008-05-01T00:00:00",1418566.211284526158124,1.418570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227541E57677N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.451888287583358,57.680900500000000]
["glac_bound",387983.000000000000000,"G229276E56852N","2008-05-01T00:00:00",407633.440765431732871,0.407633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229276E56852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.723440900272294,56.851793999999998]
["glac_bound",387988.000000000000000,"G233099E57620N","2008-05-01T00:00:00",182861.148128462489694,0.182861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA233099E57620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-126.900536216957605,57.620272499999999]
["glac_bound",387994.000000000000000,"G226202E58991N","2008-05-01T00:00:00",70561.082977535275859,0.070561000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226202E58991N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.800644167751045,58.991523500000000]
["glac_bound",387997.000000000000000,"G222407E59531N","2008-05-01T00:00:00",290939.377663475053851,0.290939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222407E59531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.592351760185352,59.531040000000004]
["glac_bound",387998.000000000000000,"G228411E57355N","2008-05-01T00:00:00",72803.716337676654803,0.072804000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228411E57355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.589913238962083,57.355557500000003]
["glac_bound",388000.000000000000000,"G228428E57150N","2008-05-01T00:00:00",204542.154358435334871,0.204542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228428E57150N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.573264734932707,57.150850500000004]
["glac_bound",388001.000000000000000,"G229157E57102N","2008-05-01T00:00:00",899283.067221878096461,0.899283000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229157E57102N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.847270163768258,57.102962500000004]
["glac_bound",388007.000000000000000,"G224943E59747N","2008-05-01T00:00:00",152157.060967254423304,0.152157000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224943E59747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.055737322968866,59.745795500000000]
["glac_bound",388009.000000000000000,"G229244E57168N","2008-05-01T00:00:00",146361.530154278472764,0.146362000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229244E57168N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.755873776381918,57.168334999999999]
["glac_bound",388010.000000000000000,"G230400E56386N","2008-05-01T00:00:00",51552.635403695094283,0.051553000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230400E56386N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.598324874999150,56.386141500000001]
["glac_bound",388011.000000000000000,"G229318E57674N","2008-05-01T00:00:00",50768.509121083385253,0.050769000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229318E57674N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.682339941151895,57.673484999999999]
["glac_bound",388015.000000000000000,"G229366E57673N","2008-05-01T00:00:00",4023835.707889682613313,4.023840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229366E57673N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.630675097767096,57.673461500000002]
["glac_bound",388016.000000000000000,"G222311E59825N","2008-05-01T00:00:00",362322.781089206750039,0.362323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222311E59825N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.688762945872043,59.824534000000000]
["glac_bound",388018.000000000000000,"G227486E58325N","2008-05-01T00:00:00",1657455.189589781919494,1.657460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227486E58325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.522272263467528,58.328834000000001]
["glac_bound",388021.000000000000000,"G228771E57198N","2008-05-01T00:00:00",56493.605118991712516,0.056494000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228771E57198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.230544961097394,57.199270499999997]
["glac_bound",388023.000000000000000,"G230684E55686N","2008-05-01T00:00:00",235196.643787312874338,0.235197000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230684E55686N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.314801803063432,55.684680999999998]
["glac_bound",388024.000000000000000,"G230063E55654N","2008-05-01T00:00:00",498936.292568517499603,0.498936000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230063E55654N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.936281616888778,55.653477500000001]
["glac_bound",388027.000000000000000,"G228827E57410N","2008-05-01T00:00:00",508440.989272262027953,0.508441000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228827E57410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.173442464584014,57.409417500000004]
["glac_bound",388028.000000000000000,"G227350E58097N","2008-05-01T00:00:00",151767.694359244313091,0.151768000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227350E58097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.651277811516366,58.096901500000001]
["glac_bound",388030.000000000000000,"G225054E59277N","2008-05-01T00:00:00",79263.764440832135733,0.079264000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225054E59277N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.947669311357686,59.277845499999998]
["glac_bound",388036.000000000000000,"G230381E55759N","2008-05-01T00:00:00",1205848.343581885332242,1.205850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230381E55759N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.613623619024850,55.757782500000005]
["glac_bound",388038.000000000000000,"G228558E57497N","2008-05-01T00:00:00",834387.387953807367012,0.834387000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228558E57497N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.440083696745603,57.495451000000003]
["glac_bound",388040.000000000000000,"G228576E57107N","2008-05-01T00:00:00",473196.702730317425448,0.473197000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228576E57107N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.425831333429414,57.105060999999999]
["glac_bound",388041.000000000000000,"G225657E59165N","2008-05-01T00:00:00",335845.371064612525515,0.335845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225657E59165N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.350269025751857,59.170085999999998]
["glac_bound",388042.000000000000000,"G227016E58114N","2008-05-01T00:00:00",533836.697353673167527,0.533837000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227016E58114N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.984321047347180,58.113715999999997]
["glac_bound",388047.000000000000000,"G228800E57536N","2008-05-01T00:00:00",3372643.557744501624256,3.372640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228800E57536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.205802507819214,57.540590999999999]
["glac_bound",388049.000000000000000,"G229985E56346N","2008-05-01T00:00:00",625731.896967260981910,0.625732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229985E56346N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.010127084771312,56.349463000000000]
["glac_bound",388054.000000000000000,"G226570E58566N","2008-05-01T00:00:00",107427.158258796305745,0.107427000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226570E58566N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.429277702183015,58.565922999999998]
["glac_bound",388057.000000000000000,"G231177E55226N","2008-05-01T00:00:00",59596.026979453818058,0.059596000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231177E55226N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.822399438195021,55.226137999999999]
["glac_bound",388058.000000000000000,"G221814E59930N","2008-05-01T00:00:00",1326506.573846107115969,1.326510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221814E59930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.177857635908595,59.937219999999996]
["glac_bound",388059.000000000000000,"G226484E58512N","2008-05-01T00:00:00",520036.936257851601113,0.520037000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226484E58512N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.520170694875333,58.514195000000001]
["glac_bound",388069.000000000000000,"G223329E59720N","2008-05-01T00:00:00",974375.078069566283375,0.974375000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223329E59720N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.672011713235293,59.720565999999998]
["glac_bound",388070.000000000000000,"G229413E57605N","2008-05-01T00:00:00",113639.095777910581091,0.113639000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229413E57605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.586627300940961,57.605225500000003]
["glac_bound",388076.000000000000000,"G228973E57220N","2008-05-01T00:00:00",177156.816207753407070,0.177157000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228973E57220N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.027796753043560,57.219766999999997]
["glac_bound",388085.000000000000000,"G229631E56405N","2008-05-01T00:00:00",608881.962565948721021,0.608882000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229631E56405N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.369865992753631,56.405259000000001]
["glac_bound",388087.000000000000000,"G227533E57800N","2008-05-01T00:00:00",1812387.987052902579308,1.812390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227533E57800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.474603643096486,57.799040500000004]
["glac_bound",388089.000000000000000,"G229581E56539N","2008-05-01T00:00:00",1058107.354470671853051,1.058110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229581E56539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.414760849866468,56.542946000000001]
["glac_bound",388091.000000000000000,"G226512E58731N","2008-05-01T00:00:00",635832.648664415813982,0.635833000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226512E58731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.487351405649804,58.732371499999999]
["glac_bound",388095.000000000000000,"G228671E57068N","2008-05-01T00:00:00",381788.403280669765081,0.381788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228671E57068N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.328988552795010,57.066887500000000]
["glac_bound",388097.000000000000000,"G225150E59614N","2008-05-01T00:00:00",843095.295431916369125,0.843095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225150E59614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.857363577264238,59.614668500000001]
["glac_bound",388101.000000000000000,"G230148E55940N","2008-05-01T00:00:00",4320125.565908589400351,4.320130000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230148E55940N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.850986630115642,55.943430500000005]
["glac_bound",388112.000000000000000,"G224620E59748N","2008-05-01T00:00:00",81905.349761457633576,0.081905000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224620E59748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.378304193811061,59.747725000000003]
["glac_bound",388116.000000000000000,"G229220E56777N","2008-05-01T00:00:00",420874.238645831588656,0.420874000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229220E56777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.779384752958208,56.779860999999997]
["glac_bound",388118.000000000000000,"G223134E59735N","2008-05-01T00:00:00",3077338.923703493550420,3.077340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223134E59735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.874676881399040,59.733096500000002]
["glac_bound",388131.000000000000000,"G223485E59489N","2008-05-01T00:00:00",529363.782796854269691,0.529364000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223485E59489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.515307517572637,59.488848500000003]
["glac_bound",388136.000000000000000,"G227645E58283N","2008-05-01T00:00:00",52434.268816131676431,0.052434000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227645E58283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.355167176536099,58.282656500000002]
["glac_bound",388137.000000000000000,"G229399E57217N","2008-05-01T00:00:00",285999.436712216993328,0.285999000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229399E57217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.601067597796145,57.216723000000002]
["glac_bound",388143.000000000000000,"G225967E58996N","2008-05-01T00:00:00",541201.517740183509886,0.541202000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225967E58996N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.028813336254018,58.998371500000005]
["glac_bound",388144.000000000000000,"G230228E57460N","2008-05-01T00:00:00",314921.297708890400827,0.314921000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230228E57460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.769925715260541,57.460825999999997]
["glac_bound",388145.000000000000000,"G229864E56581N","2008-05-01T00:00:00",134689.903991242201300,0.134690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229864E56581N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.135261900238959,56.580921000000004]
["glac_bound",388152.000000000000000,"G229701E57738N","2008-05-01T00:00:00",84048.182992197806016,0.084048000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229701E57738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.299252242436523,57.739342999999998]
["glac_bound",388157.000000000000000,"G230610E54763N","2008-05-01T00:00:00",1159550.269865004811436,1.159550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230610E54763N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.400400165808151,54.766218500000001]
["glac_bound",388159.000000000000000,"G223256E59373N","2008-05-01T00:00:00",554474.665332765667699,0.554475000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223256E59373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.744508415068481,59.373581999999999]
["glac_bound",388164.000000000000000,"G224782E59954N","2008-05-01T00:00:00",114804.369483127418789,0.114804000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224782E59954N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.219238193367659,59.954392999999996]
["glac_bound",388169.000000000000000,"G230487E55224N","2008-05-01T00:00:00",2614414.751160527113825,2.614410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230487E55224N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.514318020719713,55.229035499999995]
["glac_bound",388173.000000000000000,"G225731E59392N","2008-05-01T00:00:00",154693.700285855244147,0.154694000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225731E59392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.268779095798834,59.391990000000000]
["glac_bound",388181.000000000000000,"G222402E59674N","2008-05-01T00:00:00",304458.756353991164360,0.304459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222402E59674N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.597525878549561,59.674242499999998]
["glac_bound",388185.000000000000000,"G227657E57891N","2008-05-01T00:00:00",1763726.364452125737444,1.763730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227657E57891N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.351844534452681,57.895063499999999]
["glac_bound",388187.000000000000000,"G230176E55961N","2008-05-01T00:00:00",12764030.138051701709628,12.763999999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230176E55961N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.817115787229824,55.964427499999999]
["glac_bound",388188.000000000000000,"G225511E59444N","2008-05-01T00:00:00",2681220.375243120826781,2.681220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225511E59444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.494697098244160,59.444299500000000]
["glac_bound",388189.000000000000000,"G228595E57477N","2008-05-01T00:00:00",243629.401643924880773,0.243629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228595E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.403536048494573,57.476169999999996]
["glac_bound",388190.000000000000000,"G229304E56294N","2008-05-01T00:00:00",2591679.956372499465942,2.591680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229304E56294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.684394238213201,56.297893500000001]
["glac_bound",388191.000000000000000,"G228290E57221N","2008-05-01T00:00:00",483095.568126436031889,0.483096000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228290E57221N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.714160655461853,57.225819000000001]
["glac_bound",388194.000000000000000,"G228794E57457N","2008-05-01T00:00:00",152095.211906606564298,0.152095000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228794E57457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.208425022941555,57.458663999999999]
["glac_bound",388202.000000000000000,"G230517E56764N","2008-05-01T00:00:00",1461659.807136355200782,1.461660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230517E56764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.477744341499942,56.762202500000001]
["glac_bound",388205.000000000000000,"G230014E57456N","2008-05-01T00:00:00",255498.780779356573476,0.255499000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230014E57456N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.986787682820392,57.455942499999999]
["glac_bound",388206.000000000000000,"G223462E59476N","2008-05-01T00:00:00",55190.526771765304147,0.055191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223462E59476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.538323685049022,59.476905500000001]
["glac_bound",388208.000000000000000,"G227422E58415N","2008-05-01T00:00:00",317509.947980471362825,0.317510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227422E58415N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.578063009928712,58.414992499999997]
["glac_bound",388209.000000000000000,"G224573E59907N","2008-05-01T00:00:00",123822.720882533976692,0.123823000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224573E59907N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.428149353564294,59.908549499999999]
["glac_bound",388211.000000000000000,"G228118E57928N","2008-05-01T00:00:00",96885.123742119467352,0.096885000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228118E57928N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.882087705284562,57.927181000000004]
["glac_bound",388219.000000000000000,"G229029E56435N","2008-05-01T00:00:00",678089.272500685998239,0.678089000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229029E56435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.971134844863741,56.439571000000001]
["glac_bound",388220.000000000000000,"G225676E59134N","2008-05-01T00:00:00",3319233.555997444316745,3.319230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225676E59134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.326764814105161,59.137214499999999]
["glac_bound",388226.000000000000000,"G230204E57294N","2008-05-01T00:00:00",485668.267448295082431,0.485668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230204E57294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.795326020586288,57.294874499999999]
["glac_bound",388241.000000000000000,"G230077E55479N","2008-05-01T00:00:00",547919.839229059638456,0.547920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230077E55479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.921560747808343,55.480750000000000]
["glac_bound",388246.000000000000000,"G225382E59293N","2008-05-01T00:00:00",186152.606330317532411,0.186153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225382E59293N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.618522525762785,59.291916999999998]
["glac_bound",388255.000000000000000,"G226622E58680N","2008-05-01T00:00:00",397696.166288043314125,0.397696000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226622E58680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.377985384195199,58.680011000000000]
["glac_bound",388260.000000000000000,"G229250E56470N","2008-05-01T00:00:00",6924428.801581037230790,6.924430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229250E56470N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.754350197323674,56.476348999999999]
["glac_bound",388262.000000000000000,"G226358E58917N","2008-05-01T00:00:00",1706678.201860390137881,1.706680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226358E58917N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.644168000000008,58.918439999999997]
["glac_bound",388268.000000000000000,"G227035E57936N","2008-05-01T00:00:00",239535709.30631133913993,239.536000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Sawyer Glacier","None","08BC227035E57936N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.771538348883666,57.907309999999995]
["glac_bound",388276.000000000000000,"G222730E59449N","2008-05-01T00:00:00",1569237.989631653530523,1.569240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222730E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.264946185123478,59.453845999999999]
["glac_bound",388284.000000000000000,"G224326E59867N","2008-05-01T00:00:00",389772.168905290192924,0.389772000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224326E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.676707732405561,59.867186500000003]
["glac_bound",388287.000000000000000,"G222433E59509N","2008-05-01T00:00:00",837811.337571304757148,0.837811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222433E59509N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.564043201499999,59.508395499999999]
["glac_bound",388288.000000000000000,"G229386E56953N","2008-05-01T00:00:00",387203.323696106090210,0.387203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229386E56953N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.615803669373008,56.952368000000000]
["glac_bound",388292.000000000000000,"G228647E56601N","2008-05-01T00:00:00",481961.364934947749134,0.481961000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228647E56601N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.352536772727262,56.600839000000001]
["glac_bound",388299.000000000000000,"G230351E55641N","2008-05-01T00:00:00",777882.202038813033141,0.777882000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230351E55641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.646673478487457,55.638821000000000]
["glac_bound",388302.000000000000000,"G229467E56254N","2008-05-01T00:00:00",1527227.701835374347866,1.527230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229467E56254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.540171419589115,56.258254000000001]
["glac_bound",388303.000000000000000,"G224021E59857N","2008-05-01T00:00:00",420345.912988173658960,0.420346000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224021E59857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.977567394099850,59.857070000000000]
["glac_bound",388320.000000000000000,"G226812E58229N","2008-05-01T00:00:00",2460642.724903732072562,2.460640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226812E58229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.188712414459246,58.229713500000003]
["glac_bound",388329.000000000000000,"G229932E56747N","2008-05-01T00:00:00",464675.907594004762359,0.464676000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229932E56747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.067711887377413,56.746017000000002]
["glac_bound",388335.000000000000000,"G229268E56870N","2008-05-01T00:00:00",941951.798915852908976,0.941952000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229268E56870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.731585910736698,56.870294999999999]
["glac_bound",388337.000000000000000,"G226964E58074N","2008-05-01T00:00:00",979085.731653336086310,0.979086000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226964E58074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.033084308685176,58.072777000000002]
["glac_bound",388342.000000000000000,"G223159E59475N","2008-05-01T00:00:00",292509.884492792072706,0.292510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223159E59475N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.841601100767321,59.474918500000001]
["glac_bound",388346.000000000000000,"G230533E56706N","2008-05-01T00:00:00",1471239.416604085592553,1.471240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230533E56706N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.469273555930727,56.707722500000003]
["glac_bound",388347.000000000000000,"G224582E59905N","2008-05-01T00:00:00",111197.006026374758221,0.111197000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224582E59905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.417579280029855,59.904966000000002]
["glac_bound",388350.000000000000000,"G230361E54910N","2008-05-01T00:00:00",73657.613454446021933,0.073658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230361E54910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.638488391677299,54.909844499999998]
["glac_bound",388351.000000000000000,"G229338E56311N","2008-05-01T00:00:00",1260182.255350676830858,1.260180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229338E56311N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.664239259397107,56.311183999999997]
["glac_bound",388352.000000000000000,"G228908E56921N","2008-05-01T00:00:00",494652.190738767851144,0.494652000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228908E56921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.085713481376018,56.922000499999996]
["glac_bound",388360.000000000000000,"G228578E56915N","2008-05-01T00:00:00",3690985.827890484593809,3.690990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228578E56915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.419173240498026,56.920358999999998]
["glac_bound",388364.000000000000000,"G229315E57177N","2008-05-01T00:00:00",397679.390625569096301,0.397679000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229315E57177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.682979370491807,57.179440999999997]
["glac_bound",388371.000000000000000,"G224553E59799N","2008-05-01T00:00:00",106222.752767891855910,0.106223000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224553E59799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.446146870651376,59.798890000000000]
["glac_bound",388374.000000000000000,"G222315E59334N","2008-05-01T00:00:00",1204690.298876587999985,1.204690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222315E59334N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.690903241173942,59.332924499999997]
["glac_bound",388379.000000000000000,"G230203E55141N","2008-05-01T00:00:00",56496.118930879310938,0.056496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230203E55141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.797709815100916,55.140974999999997]
["glac_bound",388382.000000000000000,"G227095E58446N","2008-05-01T00:00:00",2897381.783346842043102,2.897380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227095E58446N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.904881245862072,58.447900500000003]
["glac_bound",388384.000000000000000,"G230136E55891N","2008-05-01T00:00:00",19587799.449349299073219,19.587800000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230136E55891N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.854662208700233,55.909500000000001]
["glac_bound",388387.000000000000000,"G225639E58914N","2008-05-01T00:00:00",103737.482513717666734,0.103737000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Gilkey Glacier","None","08BD225690E58899N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.310572809052957,58.898970000000006]
["glac_bound",388388.000000000000000,"G230298E57528N","2008-05-01T00:00:00",116017.675604781339644,0.116018000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230298E57528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.702564135364241,57.527481000000002]
["glac_bound",388390.000000000000000,"G222422E59926N","2008-05-01T00:00:00",68345.942576106768684,0.068346000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222422E59926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.577731999999997,59.926181000000000]
["glac_bound",388393.000000000000000,"G230521E56279N","2008-05-01T00:00:00",265174.484005984617397,0.265174000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230521E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.479183100000000,56.278614500000003]
["glac_bound",388396.000000000000000,"G228416E57066N","2008-05-01T00:00:00",460565.164133079815656,0.460565000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228416E57066N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.587319017402365,57.065800500000002]
["glac_bound",388397.000000000000000,"G227127E58239N","2008-05-01T00:00:00",56467.586688249124563,0.056468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227127E58239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.874269140222964,58.241038000000003]
["glac_bound",388398.000000000000000,"G228760E57502N","2008-05-01T00:00:00",178450.517664303974016,0.178451000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228760E57502N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.239900997416783,57.502904000000001]
["glac_bound",388400.000000000000000,"G229886E56981N","2008-05-01T00:00:00",289364.476982905587647,0.289364000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229886E56981N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.117903915792596,56.982860000000002]
["glac_bound",388409.000000000000000,"G222166E59680N","2008-05-01T00:00:00",146623.140984217345249,0.146623000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222166E59680N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.830395714202552,59.680002000000002]
["glac_bound",388412.000000000000000,"G224719E59874N","2008-05-01T00:00:00",122068.441816573860706,0.122068000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224719E59874N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.281021668644655,59.874818000000005]
["glac_bound",388421.000000000000000,"G229043E57325N","2008-05-01T00:00:00",132694.553895953256870,0.132695000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229043E57325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.956474590236382,57.324882500000001]
["glac_bound",388428.000000000000000,"G229880E57791N","2008-05-01T00:00:00",210817.206287055101711,0.210817000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229880E57791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.118627265269652,57.791281999999995]
["glac_bound",388429.000000000000000,"G229391E56280N","2008-05-01T00:00:00",988100.531634641462006,0.988101000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229391E56280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.613229659087295,56.286186499999999]
["glac_bound",388435.000000000000000,"G229452E57715N","2008-05-01T00:00:00",164878.606347471446497,0.164879000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229452E57715N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.548067483562022,57.715266000000000]
["glac_bound",388440.000000000000000,"G230311E57300N","2008-05-01T00:00:00",91771.712775397405494,0.091772000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230311E57300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.688857498636139,57.299654000000004]
["glac_bound",388442.000000000000000,"G227997E57415N","2008-05-01T00:00:00",149083.692738113517407,0.149084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227997E57415N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.005356394048817,57.414067500000002]
["glac_bound",388443.000000000000000,"G230836E55029N","2008-05-01T00:00:00",1951026.328363423701376,1.951030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230836E55029N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.162301676806635,55.029102500000000]
["glac_bound",388449.000000000000000,"G228086E57548N","2008-05-01T00:00:00",1719409.818375183502212,1.719410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228086E57548N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.910285508769448,57.549384500000002]
["glac_bound",388450.000000000000000,"G228146E57487N","2008-05-01T00:00:00",160028.320166154997423,0.160028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228146E57487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.853828625440940,57.487067500000002]
["glac_bound",388452.000000000000000,"G231910E57222N","2008-05-01T00:00:00",147425.518313382635824,0.147426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA231910E57222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.090432059458124,57.222518500000000]
["glac_bound",388460.000000000000000,"G224728E59767N","2008-05-01T00:00:00",762402.497670370968990,0.762402000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224728E59767N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.278321299098252,59.769300500000000]
["glac_bound",388461.000000000000000,"G229085E56404N","2008-05-01T00:00:00",86690.301632190879900,0.086690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229085E56404N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.913081408525898,56.405650500000000]
["glac_bound",388463.000000000000000,"G228928E56746N","2008-05-01T00:00:00",418505.696509775181767,0.418506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228928E56746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.071276179164954,56.743825000000001]
["glac_bound",388468.000000000000000,"G229349E56308N","2008-05-01T00:00:00",148496.259518466860754,0.148496000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229349E56308N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.652258897214267,56.307958499999998]
["glac_bound",388469.000000000000000,"G227761E57219N","2008-05-01T00:00:00",20314.012284218217246,0.020314000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227761E57219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.237958409413352,57.220230999999998]
["glac_bound",388470.000000000000000,"G226081E58982N","2008-05-01T00:00:00",105244.703678452438908,0.105245000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226081E58982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.920890005195417,58.983084000000005]
["glac_bound",388471.000000000000000,"G231187E57505N","2008-05-01T00:00:00",52220.479892254319566,0.052221000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231187E57505N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.812207474409433,57.504664500000004]
["glac_bound",388473.000000000000000,"G230342E55623N","2008-05-01T00:00:00",432995.188873223378323,0.432995000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230342E55623N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.652670538196787,55.623408499999996]
["glac_bound",388474.000000000000000,"G229517E57282N","2008-05-01T00:00:00",93848.880384261166910,0.093849000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229517E57282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.483294566492447,57.282355000000003]
["glac_bound",388475.000000000000000,"G224009E59705N","2008-05-01T00:00:00",249419.086353918741224,0.249419000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224009E59705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.987412451139846,59.704289000000003]
["glac_bound",388476.000000000000000,"G230346E54625N","2008-05-01T00:00:00",134782.925391399039654,0.134783000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230346E54625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.652682457606659,54.624105999999998]
["glac_bound",388477.000000000000000,"G225022E59465N","2008-05-01T00:00:00",24940496.667456965893507,24.940500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225054E59449N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.989687063421542,59.459654000000000]
["glac_bound",388478.000000000000000,"G227901E57478N","2008-05-01T00:00:00",538134.017231157631613,0.538134000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227901E57478N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.099672655751078,57.477939500000005]
["glac_bound",388482.000000000000000,"G227584E58001N","2008-05-01T00:00:00",267157.412653305917047,0.267157000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227584E58001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.414268691249987,58.001360500000004]
["glac_bound",388491.000000000000000,"G227113E57825N","2008-05-01T00:00:00",2257766.506076939404011,2.257770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-11T00:00:00","okay","None","None","08BC227113E57825N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.886872198317974,57.825939499999997]
["glac_bound",388498.000000000000000,"G227037E58013N","2008-05-01T00:00:00",2026166.720330222044140,2.026170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227037E58013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.965279343830616,58.009833000000000]
["glac_bound",388499.000000000000000,"G228682E56556N","2008-05-01T00:00:00",102212.718257128362893,0.102213000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228682E56556N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.318186105091399,56.556328499999999]
["glac_bound",388511.000000000000000,"G226903E58286N","2008-05-01T00:00:00",1447203.037151612341404,1.447200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226903E58286N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.106427984120245,58.285963000000002]
["glac_bound",388513.000000000000000,"G229342E57647N","2008-05-01T00:00:00",5156002.756241831928492,5.156000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229342E57647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.660230655190134,57.662575000000004]
["glac_bound",388523.000000000000000,"G227602E58360N","2008-05-01T00:00:00",451862.035226319276262,0.451862000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227602E58360N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.405026400923475,58.361872000000005]
["glac_bound",388524.000000000000000,"G228594E56601N","2008-05-01T00:00:00",145199.130469112104038,0.145199000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228594E56601N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.406093482546538,56.600258499999995]
["glac_bound",388525.000000000000000,"G230040E55792N","2008-05-01T00:00:00",699482.555646227090620,0.699483000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230040E55792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.958024725000001,55.790819499999998]
["glac_bound",388530.000000000000000,"G230249E56613N","2008-05-01T00:00:00",211255.704725966119440,0.211256000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230249E56613N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.751336686943972,56.614665000000002]
["glac_bound",388533.000000000000000,"G229598E56239N","2008-05-01T00:00:00",239573.014164134423481,0.239573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229598E56239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.400022585051545,56.239776500000005]
["glac_bound",388534.000000000000000,"G228617E56636N","2008-05-01T00:00:00",578083.678234683466144,0.578084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228617E56636N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.383843579887440,56.635984999999998]
["glac_bound",388537.000000000000000,"G230151E56473N","2008-05-01T00:00:00",123807.424753686282202,0.123807000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230151E56473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.850564391425394,56.472576500000002]
["glac_bound",388538.000000000000000,"G222499E59189N","2008-05-01T00:00:00",1705507.648646560963243,1.705510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222499E59189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.508575809882984,59.192098000000001]
["glac_bound",388544.000000000000000,"G226440E58752N","2008-05-01T00:00:00",71633.107763447391335,0.071633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226440E58752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.560717948717979,58.751856000000004]
["glac_bound",388547.000000000000000,"G223521E59695N","2008-05-01T00:00:00",503564.360601032385603,0.503564000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223521E59695N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.478984339799922,59.695062000000000]
["glac_bound",388549.000000000000000,"G230184E57186N","2008-05-01T00:00:00",113145.755263343104161,0.113146000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230184E57186N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.818838229196217,57.187149500000004]
["glac_bound",388551.000000000000000,"G230382E54884N","2008-05-01T00:00:00",246327.451916980469832,0.246327000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230382E54884N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.618343088004110,54.883728500000004]
["glac_bound",388564.000000000000000,"G229616E56536N","2008-05-01T00:00:00",7560217.154667901806533,7.560220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229616E56536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.399564804918043,56.541215500000000]
["glac_bound",388569.000000000000000,"G228920E57117N","2008-05-01T00:00:00",435245.670535122335423,0.435246000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228920E57117N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.079265274641614,57.116850499999998]
["glac_bound",388571.000000000000000,"G229893E57095N","2008-05-01T00:00:00",508444.763139233633410,0.508445000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229893E57095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.102834933583608,57.094256999999999]
["glac_bound",388578.000000000000000,"G228216E57125N","2008-05-01T00:00:00",54606.971101979877858,0.054607000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228216E57125N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.783065053897190,57.125658000000001]
["glac_bound",388579.000000000000000,"G226991E57998N","2008-05-01T00:00:00",6886814.236827343702316,6.886810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226991E57998N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.015851185915523,58.008585999999994]
["glac_bound",388583.000000000000000,"G225556E59447N","2008-05-01T00:00:00",2119871.061888497322798,2.119870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225556E59447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.444402640025316,59.449055000000001]
["glac_bound",388589.000000000000000,"G230537E58208N","2008-05-01T00:00:00",74356.244554027696722,0.074356000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB230537E58208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463297720423412,58.208787999999998]
["glac_bound",388594.000000000000000,"G229174E56511N","2008-05-01T00:00:00",405049.353707393805962,0.405049000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229174E56511N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.826592731147542,56.511786000000001]
["glac_bound",388600.000000000000000,"G229306E57279N","2008-05-01T00:00:00",459481.436909624375403,0.459481000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229306E57279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.695691617080996,57.279744500000000]
["glac_bound",388607.000000000000000,"G230410E56014N","2008-05-01T00:00:00",469984.617078553186730,0.469985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230410E56014N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.589261754150755,56.014187499999998]
["glac_bound",388615.000000000000000,"G230338E54628N","2008-05-01T00:00:00",660786.410596357658505,0.660786000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230338E54628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.655510028244919,54.631287999999998]
["glac_bound",388622.000000000000000,"G228471E57209N","2008-05-01T00:00:00",66861.216070212190971,0.066861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228471E57209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.527787295396649,57.209568500000003]
["glac_bound",388631.000000000000000,"G227329E58061N","2008-05-01T00:00:00",950661.564953349414282,0.950662000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227329E58061N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.672001377266099,58.061372000000006]
["glac_bound",388632.000000000000000,"G231810E57171N","2008-05-01T00:00:00",232701.733108569082106,0.232702000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EA231810E57171N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.190690055980951,57.171457000000004]
["glac_bound",388634.000000000000000,"G230946E54937N","2008-05-01T00:00:00",1478629.652734018862247,1.478630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230946E54937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.054249862096157,54.936616999999998]
["glac_bound",388640.000000000000000,"G227315E58428N","2008-05-01T00:00:00",233034.157551559997955,0.233034000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227315E58428N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.682803949337767,58.429798000000005]
["glac_bound",388643.000000000000000,"G228034E58022N","2008-05-01T00:00:00",355427.740296057134401,0.355428000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228034E58022N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.965128642468869,58.021681000000001]
["glac_bound",388644.000000000000000,"G228546E56777N","2008-05-01T00:00:00",879896.620127141359262,0.879897000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228546E56777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.451520160740245,56.774113499999999]
["glac_bound",388645.000000000000000,"G227222E58476N","2008-05-01T00:00:00",115059.289703339309199,0.115059000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227222E58476N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.777720153136954,58.475801500000003]
["glac_bound",388646.000000000000000,"G222028E59957N","2008-05-01T00:00:00",9606640.560550484806299,9.606640000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222028E59957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.977354109355531,59.982309000000001]
["glac_bound",388652.000000000000000,"G225385E59419N","2008-05-01T00:00:00",808978.461434759083204,0.808978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225385E59419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.615681403685073,59.423279000000001]
["glac_bound",388653.000000000000000,"G230309E54862N","2008-05-01T00:00:00",204379.516090267105028,0.204380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230309E54862N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.691659540575927,54.862143500000002]
["glac_bound",388654.000000000000000,"G230549E54717N","2008-05-01T00:00:00",225674.223074125300627,0.225674000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230549E54717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.452060620182209,54.716404499999996]
["glac_bound",388657.000000000000000,"G230342E56292N","2008-05-01T00:00:00",287524.518529386492446,0.287525000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230342E56292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.658036141163137,56.292321000000001]
["glac_bound",388658.000000000000000,"G228735E56847N","2008-05-01T00:00:00",69973145.076411291956902,69.973100000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228735E56847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.272125189701399,56.848604999999999]
["glac_bound",388659.000000000000000,"G227061E57958N","2008-05-01T00:00:00",879975.489310911856592,0.879975000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227061E57958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.951082307818780,57.959282500000000]
["glac_bound",388666.000000000000000,"G228126E56905N","2008-05-01T00:00:00",1806816.451383533421904,1.806820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228126E56905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.874233464876028,56.902747500000004]
["glac_bound",388670.000000000000000,"G222166E59371N","2008-05-01T00:00:00",21098503.265888862311840,21.098500000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","Netland Glacier","None","08AB222166E59371N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.910197776862219,59.390347000000006]
["glac_bound",388672.000000000000000,"G230336E54683N","2008-05-01T00:00:00",152763.725109357765177,0.152764000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230336E54683N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.662296319909672,54.683790000000002]
["glac_bound",388673.000000000000000,"G227456E57816N","2008-05-01T00:00:00",623451.394608458853327,0.623451000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227456E57816N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.544368808016714,57.815215000000002]
["glac_bound",388677.000000000000000,"G227992E57630N","2008-05-01T00:00:00",530726.039406194002368,0.530726000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227992E57630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.009983698929091,57.631375499999997]
["glac_bound",388681.000000000000000,"G229515E56994N","2008-05-01T00:00:00",2221533.618654251098633,2.221530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229515E56994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.489565780184222,56.995705000000001]
["glac_bound",388684.000000000000000,"G227088E58484N","2008-05-01T00:00:00",158999.153394963534083,0.158999000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227088E58484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.912142716977058,58.484384499999997]
["glac_bound",388685.000000000000000,"G228948E57550N","2008-05-01T00:00:00",300377.675353153550532,0.300378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228948E57550N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.052378480689697,57.549589499999996]
["glac_bound",388686.000000000000000,"G224056E59744N","2008-05-01T00:00:00",534975.931557906907983,0.534976000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224056E59744N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.942365915314042,59.744672999999999]
["glac_bound",388688.000000000000000,"G230318E54822N","2008-05-01T00:00:00",178455.386861772713019,0.178455000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230318E54822N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.682357698038800,54.822727499999999]
["glac_bound",388689.000000000000000,"G227317E58073N","2008-05-01T00:00:00",5585949.723493206314743,5.585950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227317E58073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.657161709510945,58.069237999999999]
["glac_bound",388694.000000000000000,"G230282E56331N","2008-05-01T00:00:00",2320144.160062924493104,2.320140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230282E56331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.718135742532638,56.334134500000005]
["glac_bound",388699.000000000000000,"G225422E59268N","2008-05-01T00:00:00",3967932.436237299349159,3.967930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225422E59268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.574158167174915,59.272448500000003]
["glac_bound",388700.000000000000000,"G230432E56644N","2008-05-01T00:00:00",512733.229182618670166,0.512733000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230432E56644N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.570888676833079,56.645712500000002]
["glac_bound",388701.000000000000000,"G230525E55184N","2008-05-01T00:00:00",1562660.024386512115598,1.562660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230525E55184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.480650953680765,55.179467000000002]
["glac_bound",388703.000000000000000,"G230159E54913N","2008-05-01T00:00:00",111166.341684156781412,0.111166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230159E54913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.839817650408662,54.913881500000002]
["glac_bound",388705.000000000000000,"G229228E57176N","2008-05-01T00:00:00",248517.872087340889266,0.248518000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229228E57176N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.774718722222246,57.177447999999998]
["glac_bound",388708.000000000000000,"G228643E57416N","2008-05-01T00:00:00",2103688.771666666492820,2.103690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228643E57416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.350725597276465,57.420219500000002]
["glac_bound",388710.000000000000000,"G224303E59913N","2008-05-01T00:00:00",594765.215115430997685,0.594765000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224303E59913N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.698360247440519,59.912441999999999]
["glac_bound",388711.000000000000000,"G223248E59489N","2008-05-01T00:00:00",502030.831032736867201,0.502031000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223248E59489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.753774253957005,59.487534999999994]
["glac_bound",388712.000000000000000,"G228590E57487N","2008-05-01T00:00:00",2237159.428888701833785,2.237160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228590E57487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.422983197063360,57.483829000000000]
["glac_bound",388714.000000000000000,"G228994E57239N","2008-05-01T00:00:00",812913.346660125534981,0.812913000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228994E57239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.002821611460718,57.242481999999995]
["glac_bound",388715.000000000000000,"G224817E59818N","2008-05-01T00:00:00",633291.706846448709257,0.633292000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224817E59818N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.183563204325139,59.820005499999994]
["glac_bound",388717.000000000000000,"G221936E59884N","2008-05-01T00:00:00",580075.425898995716125,0.580075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221936E59884N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.064706492376303,59.884637999999995]
["glac_bound",388720.000000000000000,"G223138E59533N","2008-05-01T00:00:00",259911.216784647665918,0.259911000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223138E59533N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.861623303909994,59.532370499999999]
["glac_bound",388722.000000000000000,"G222708E59000N","2008-05-01T00:00:00",91211.958631890418474,0.091212000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222708E59000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.291689350338800,58.999781499999997]
["glac_bound",388725.000000000000000,"G228329E57203N","2008-05-01T00:00:00",1541668.617757602361962,1.541670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228329E57203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.675006544737840,57.208987499999999]
["glac_bound",388729.000000000000000,"G230499E56372N","2008-05-01T00:00:00",64518.084392086944717,0.064518000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230499E56372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.501545842250039,56.372711000000002]
["glac_bound",388736.000000000000000,"G228135E56932N","2008-05-01T00:00:00",137027.900180444150465,0.137028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228135E56932N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.864731476151860,56.931793999999996]
["glac_bound",388737.000000000000000,"G227987E57953N","2008-05-01T00:00:00",3858954.138844140805304,3.858950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227987E57953N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.007161388698819,57.959741500000000]
["glac_bound",388751.000000000000000,"G229384E56553N","2008-05-01T00:00:00",1440982.998123678611591,1.440980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229384E56553N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.625771475973551,56.554153999999997]
["glac_bound",388754.000000000000000,"G228493E57141N","2008-05-01T00:00:00",129166.114849348305142,0.129166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228493E57141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.506574328886700,57.141125000000002]
["glac_bound",388756.000000000000000,"G230527E55871N","2008-05-01T00:00:00",17329850.426666606217623,17.329899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230527E55871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.506615653779988,55.875529000000000]
["glac_bound",388764.000000000000000,"G227120E58239N","2008-05-01T00:00:00",94530.455736888005049,0.094531000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227120E58239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.879754858142746,58.238788499999998]
["glac_bound",388765.000000000000000,"G222582E59350N","2008-05-01T00:00:00",383756.594405351788737,0.383757000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222582E59350N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.417562932330782,59.349670000000003]
["glac_bound",388770.000000000000000,"G225955E59215N","2008-05-01T00:00:00",204847.793845567241078,0.204848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225955E59215N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.040252535459757,59.216372000000000]
["glac_bound",388774.000000000000000,"G226779E58405N","2008-05-01T00:00:00",1696264.693171332590282,1.696260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226779E58405N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.221240902331317,58.408014500000000]
["glac_bound",388775.000000000000000,"G231833E57160N","2008-05-01T00:00:00",140352.847791835229145,0.140353000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08EA231833E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.166756637881377,57.160528499999998]
["glac_bound",388777.000000000000000,"G230420E54685N","2008-05-01T00:00:00",883555.340569257386960,0.883555000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230420E54685N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.582592645692813,54.685702500000005]
["glac_bound",388783.000000000000000,"G227631E57665N","2008-05-01T00:00:00",231676.205153728747973,0.231676000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227631E57665N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.368717257205589,57.666134499999998]
["glac_bound",388789.000000000000000,"G229381E56270N","2008-05-01T00:00:00",260850.241977289260831,0.260850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229381E56270N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.621725838217344,56.269137499999999]
["glac_bound",388791.000000000000000,"G228417E56643N","2008-05-01T00:00:00",148783.833679100993322,0.148784000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228417E56643N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.581525306003584,56.643405000000001]
["glac_bound",388797.000000000000000,"G229913E56147N","2008-05-01T00:00:00",67467.618565254568239,0.067468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229913E56147N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.086760344201480,56.146189499999998]
["glac_bound",388798.000000000000000,"G225030E59614N","2008-05-01T00:00:00",123304.291315089358250,0.123304000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225030E59614N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.971508643028841,59.615229499999998]
["glac_bound",388799.000000000000000,"G222787E59257N","2008-05-01T00:00:00",5776998.315392266027629,5.777000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222787E59257N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.197148385188427,59.266393000000001]
["glac_bound",388806.000000000000000,"G228837E57302N","2008-05-01T00:00:00",1296033.897942979820073,1.296030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228837E57302N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.164671321485912,57.301876000000000]
["glac_bound",388808.000000000000000,"G230614E57031N","2008-05-01T00:00:00",56314.766385423063184,0.056315000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230614E57031N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.387690249652280,57.031435500000001]
["glac_bound",388811.000000000000000,"G227603E58134N","2008-05-01T00:00:00",478122.567090238560922,0.478123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227603E58134N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.397325772025397,58.133503500000003]
["glac_bound",388817.000000000000000,"G224421E59825N","2008-05-01T00:00:00",2499345.840515892487019,2.499350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224421E59825N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.592049636490231,59.827601000000001]
["glac_bound",388820.000000000000000,"G229473E56416N","2008-05-01T00:00:00",60800.517651184774877,0.060801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229473E56416N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.525782298372945,56.417442500000000]
["glac_bound",388821.000000000000000,"G227133E58362N","2008-05-01T00:00:00",665022.826149854226969,0.665023000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227133E58362N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.866708768695162,58.362501000000002]
["glac_bound",388822.000000000000000,"G229039E56435N","2008-05-01T00:00:00",646492.684037378639914,0.646493000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229039E56435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.962123190694626,56.434389499999995]
["glac_bound",388823.000000000000000,"G225066E59507N","2008-05-01T00:00:00",250431.844024512160104,0.250432000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225066E59507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.934912607944739,59.507292000000000]
["glac_bound",388832.000000000000000,"G228022E58028N","2008-05-01T00:00:00",153903.360972786351340,0.153903000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228022E58028N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.977499309151540,58.028379000000001]
["glac_bound",388836.000000000000000,"G229093E56970N","2008-05-01T00:00:00",73560.588249543114216,0.073561000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229093E56970N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.907443972911778,56.970275500000000]
["glac_bound",388837.000000000000000,"G226611E58430N","2008-05-01T00:00:00",826946.007324210833758,0.826946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BD226611E58430N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.391117368487642,58.427959500000000]
["glac_bound",388838.000000000000000,"G230486E56755N","2008-05-01T00:00:00",106633.957799658368458,0.106634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230486E56755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.513278869767760,56.756541999999996]
["glac_bound",388849.000000000000000,"G223209E59345N","2008-05-01T00:00:00",287537.707640573964454,0.287538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223209E59345N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.786436347411353,59.348549000000006]
["glac_bound",388851.000000000000000,"G230500E55186N","2008-05-01T00:00:00",161674.627684984501684,0.161675000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230500E55186N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.500586040502810,55.186298999999998]
["glac_bound",388853.000000000000000,"G225436E59249N","2008-05-01T00:00:00",1915899.471981462556869,1.915900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225436E59249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.562492641437302,59.254342999999999]
["glac_bound",388856.000000000000000,"G229880E56624N","2008-05-01T00:00:00",195574.556551210233010,0.195575000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229880E56624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.119711317906422,56.624484499999994]
["glac_bound",388859.000000000000000,"G230415E56242N","2008-05-01T00:00:00",249606.798904205177678,0.249607000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230415E56242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.584494659155268,56.243610000000004]
["glac_bound",388866.000000000000000,"G230535E56900N","2008-05-01T00:00:00",116985.640397084789583,0.116986000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230535E56900N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463863691314543,56.900434000000004]
["glac_bound",388868.000000000000000,"G222579E59758N","2008-05-01T00:00:00",722715.405840987921692,0.722715000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222579E59758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.421031625823076,59.762636999999998]
["glac_bound",388875.000000000000000,"G227882E57288N","2008-05-01T00:00:00",898983.826240823254921,0.898984000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227882E57288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.118500421889223,57.289337500000002]
["glac_bound",388876.000000000000000,"G230189E56080N","2008-05-01T00:00:00",257040.256630381685682,0.257040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230189E56080N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.809420687768437,56.079249000000004]
["glac_bound",388879.000000000000000,"G230415E56388N","2008-05-01T00:00:00",883531.225565183674917,0.883531000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230415E56388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.583184154580152,56.388255999999998]
["glac_bound",388882.000000000000000,"G229353E56592N","2008-05-01T00:00:00",7911062.191022087819874,7.911060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229353E56592N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.643299476618381,56.603757500000000]
["glac_bound",388886.000000000000000,"G230121E56681N","2008-05-01T00:00:00",291209.064469023433048,0.291209000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230121E56681N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.879653194792979,56.681060500000001]
["glac_bound",388889.000000000000000,"G228682E57069N","2008-05-01T00:00:00",552407.366235899273306,0.552407000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228682E57069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.317341094857937,57.068917499999998]
["glac_bound",388890.000000000000000,"G230513E54607N","2008-05-01T00:00:00",491977.984095420280937,0.491978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230513E54607N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.485173681375016,54.612650000000002]
["glac_bound",388892.000000000000000,"G232903E57760N","2008-05-01T00:00:00",323275.094034024223220,0.323275000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232903E57760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.096610447771923,57.760002999999998]
["glac_bound",388899.000000000000000,"G222155E59399N","2008-05-01T00:00:00",917977.475240242783912,0.917977000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222155E59399N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.841026533565213,59.400150499999995]
["glac_bound",388902.000000000000000,"G230471E55950N","2008-05-01T00:00:00",126450.460134585897322,0.126450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230471E55950N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.526799457290281,55.949036500000005]
["glac_bound",388911.000000000000000,"G225174E59385N","2008-05-01T00:00:00",52263.802893688531185,0.052264000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225174E59385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.828645735812586,59.385905500000000]
["glac_bound",388913.000000000000000,"G225756E59280N","2008-05-01T00:00:00",131155.442539454117650,0.131155000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225756E59280N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.244902900373603,59.280110499999999]
["glac_bound",388914.000000000000000,"G230803E56487N","2008-05-01T00:00:00",268052.847307013464160,0.268053000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230803E56487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.195627907563050,56.486595000000001]
["glac_bound",388919.000000000000000,"G227180E58243N","2008-05-01T00:00:00",442614.455740856472403,0.442614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227180E58243N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.819305186015299,58.242293000000004]
["glac_bound",388920.000000000000000,"G229055E56641N","2008-05-01T00:00:00",1634866.563391559291631,1.634870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229055E56641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.949799610779479,56.640172000000000]
["glac_bound",388923.000000000000000,"G230018E56539N","2008-05-01T00:00:00",1587522.738024399150163,1.587520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230018E56539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.981673674239687,56.535969999999999]
["glac_bound",388926.000000000000000,"G230561E55898N","2008-05-01T00:00:00",355558.670111675048247,0.355559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230561E55898N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.436911903138082,55.899625000000000]
["glac_bound",388927.000000000000000,"G222301E59540N","2008-05-01T00:00:00",332529.990087201993447,0.332530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222301E59540N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.698796233432063,59.538662000000002]
["glac_bound",388930.000000000000000,"G230754E55650N","2008-05-01T00:00:00",216289.529909937118646,0.216290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230754E55650N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.247772765096926,55.647893500000002]
["glac_bound",388931.000000000000000,"G227781E57790N","2008-05-01T00:00:00",173564.006752707588021,0.173564000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227781E57790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.216177575335223,57.790165999999999]
["glac_bound",388933.000000000000000,"G225915E59304N","2008-05-01T00:00:00",236886.499153766140807,0.236887000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225915E59304N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.084153208022371,59.305355499999997]
["glac_bound",388934.000000000000000,"G226397E58868N","2008-05-01T00:00:00",2095195.558961400296539,2.095200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226397E58868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.607582783018870,58.867529500000003]
["glac_bound",388939.000000000000000,"G228497E57482N","2008-05-01T00:00:00",1293679.212484819814563,1.293680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228497E57482N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.496639456689195,57.481522499999997]
["glac_bound",388940.000000000000000,"G230254E57440N","2008-05-01T00:00:00",350887.594405881420244,0.350888000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230254E57440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.748101728818909,57.442673999999997]
["glac_bound",388945.000000000000000,"G230140E56261N","2008-05-01T00:00:00",390657.775966192071792,0.390658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230140E56261N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.861829238432847,56.263987000000000]
["glac_bound",388947.000000000000000,"G230709E56777N","2008-05-01T00:00:00",77402.341353445386630,0.077402000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230709E56777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.290580581032287,56.776768500000003]
["glac_bound",388950.000000000000000,"G225112E59660N","2008-05-01T00:00:00",311375.045946600264870,0.311375000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225112E59660N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.888880090909083,59.659015999999994]
["glac_bound",388954.000000000000000,"G229991E55647N","2008-05-01T00:00:00",2046385.594313240144402,2.046390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC229991E55647N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.017856110076536,55.651429499999999]
["glac_bound",388962.000000000000000,"G222395E59668N","2008-05-01T00:00:00",1047204.625492209568620,1.047200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222395E59668N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.601759015196421,59.666636999999994]
["glac_bound",388974.000000000000000,"G230291E56205N","2008-05-01T00:00:00",181390.900790892512305,0.181391000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230291E56205N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.711381828262745,56.205207500000000]
["glac_bound",388976.000000000000000,"G230376E54909N","2008-05-01T00:00:00",130457.585744854121003,0.130458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230376E54909N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.624435757212837,54.908968000000002]
["glac_bound",388978.000000000000000,"G230319E56268N","2008-05-01T00:00:00",6478498.122158058919013,6.478500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230319E56268N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.691492361245650,56.271178000000006]
["glac_bound",388979.000000000000000,"G230368E56403N","2008-05-01T00:00:00",411140.175858734524809,0.411140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230368E56403N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.633805132706698,56.402279000000000]
["glac_bound",388981.000000000000000,"G228486E57152N","2008-05-01T00:00:00",5117991.601260016672313,5.117990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228486E57152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.529137709312579,57.161702500000004]
["glac_bound",388985.000000000000000,"G230459E55989N","2008-05-01T00:00:00",702167.245739615755156,0.702167000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230459E55989N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.541259301164587,55.990680499999996]
["glac_bound",388986.000000000000000,"G230487E55247N","2008-05-01T00:00:00",8252795.347408929839730,8.252800000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230487E55247N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.507925794653886,55.266007500000001]
["glac_bound",388988.000000000000000,"G229387E57143N","2008-05-01T00:00:00",9400112.096123090013862,9.400110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229387E57143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.630632183728096,57.166865000000001]
["glac_bound",388994.000000000000000,"G229228E56788N","2008-05-01T00:00:00",400788.343685791536700,0.400788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229228E56788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.770440803858264,56.792681999999999]
["glac_bound",389000.000000000000000,"G222895E59467N","2008-05-01T00:00:00",774502.428350400878116,0.774502000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222895E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.102547591389566,59.466370499999996]
["glac_bound",389004.000000000000000,"G225456E59557N","2008-05-01T00:00:00",57070.162620802977472,0.057070000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225456E59557N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.543531351792637,59.557242000000002]
["glac_bound",389006.000000000000000,"G223740E59968N","2008-05-01T00:00:00",896247.771606467431411,0.896248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223740E59968N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.261560297397068,59.967069499999994]
["glac_bound",389011.000000000000000,"G227817E58045N","2008-05-01T00:00:00",451453.011542667984031,0.451453000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227817E58045N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.182489241477299,58.045490000000001]
["glac_bound",389013.000000000000000,"G221346E59800N","2008-05-01T00:00:00",71096.613751055643661,0.071097000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221346E59800N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.653289437141780,59.799846000000002]
["glac_bound",389015.000000000000000,"G230474E57074N","2008-05-01T00:00:00",162838.876129458716605,0.162839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230474E57074N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.527368569420048,57.074302500000002]
["glac_bound",389022.000000000000000,"G230491E56763N","2008-05-01T00:00:00",181087.403418517147657,0.181087000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230491E56763N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.508877887667893,56.763465999999994]
["glac_bound",389023.000000000000000,"G224178E59857N","2008-05-01T00:00:00",2817820.271542558912188,2.817820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224178E59857N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.803075984983707,59.859111999999996]
["glac_bound",389027.000000000000000,"G230445E55996N","2008-05-01T00:00:00",311623.875393303809687,0.311624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230445E55996N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.552063517076590,55.998522999999999]
["glac_bound",389031.000000000000000,"G229423E56323N","2008-05-01T00:00:00",99437.097840258182259,0.099437000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229423E56323N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.577319559278351,56.323103500000002]
["glac_bound",389033.000000000000000,"G225048E59259N","2008-05-01T00:00:00",12180.422844722523223,0.012180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225048E59259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.952365149353739,59.259278500000001]
["glac_bound",389036.000000000000000,"G230531E55198N","2008-05-01T00:00:00",61589.128010614171217,0.061589000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230531E55198N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.469120953407980,55.197102000000001]
["glac_bound",389039.000000000000000,"G223879E59960N","2008-05-01T00:00:00",262525.735720890457742,0.262526000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223879E59960N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.123745473787665,59.958652499999999]
["glac_bound",389042.000000000000000,"G221699E59985N","2008-05-01T00:00:00",141288.122126443835441,0.141288000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221699E59985N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.304449363539504,59.985749999999996]
["glac_bound",389043.000000000000000,"G230497E57097N","2008-05-01T00:00:00",1129557.495584722375497,1.129560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230497E57097N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.502635325730893,57.097423499999998]
["glac_bound",389047.000000000000000,"G225436E59523N","2008-05-01T00:00:00",75509.825681740709115,0.075510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225436E59523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.564023512129950,59.523063499999999]
["glac_bound",389048.000000000000000,"G226625E58544N","2008-05-01T00:00:00",574477.050255241570994,0.574477000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226625E58544N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.374703346439162,58.543943499999997]
["glac_bound",389051.000000000000000,"G229408E57368N","2008-05-01T00:00:00",336192.597057397535536,0.336193000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229408E57368N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.592377313742560,57.368278500000002]
["glac_bound",389056.000000000000000,"G227676E57592N","2008-05-01T00:00:00",271614.998679027834442,0.271615000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227676E57592N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.327797079838547,57.593999500000002]
["glac_bound",389060.000000000000000,"G227654E57957N","2008-05-01T00:00:00",4644423.913892159238458,4.644420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227654E57957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.344009033157590,57.960421499999995]
["glac_bound",389063.000000000000000,"G229404E56294N","2008-05-01T00:00:00",176596.886639150936389,0.176597000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229404E56294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.595142996363052,56.293143000000001]
["glac_bound",389075.000000000000000,"G230371E55151N","2008-05-01T00:00:00",576180.849684813292697,0.576181000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230371E55151N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.628674814693341,55.151657499999999]
["glac_bound",389084.000000000000000,"G228758E57145N","2008-05-01T00:00:00",54839.829246975241404,0.054840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228758E57145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.241812922727263,57.145803500000000]
["glac_bound",389088.000000000000000,"G227425E57815N","2008-05-01T00:00:00",11816556.132717402651906,11.816599999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227425E57815N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.593371420989513,57.830712500000004]
["glac_bound",389089.000000000000000,"G224224E59887N","2008-05-01T00:00:00",252328.587381550896680,0.252329000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224224E59887N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.780169230697197,59.886184999999998]
["glac_bound",389090.000000000000000,"G229794E57778N","2008-05-01T00:00:00",51140.583417123118124,0.051141000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229794E57778N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.204624920934009,57.777840999999995]
["glac_bound",389092.000000000000000,"G225657E59377N","2008-05-01T00:00:00",306300.197400848614052,0.306300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225657E59377N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.343058003203737,59.377287499999994]
["glac_bound",389098.000000000000000,"G230562E55892N","2008-05-01T00:00:00",52057.653496202663518,0.052058000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230562E55892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.437535011261900,55.891495000000006]
["glac_bound",389101.000000000000000,"G228965E57046N","2008-05-01T00:00:00",293224.186577626911458,0.293224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228965E57046N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.035193652146404,57.044228000000004]
["glac_bound",389105.000000000000000,"G229348E57264N","2008-05-01T00:00:00",337326.985253680031747,0.337327000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229348E57264N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.650408749862095,57.265920000000001]
["glac_bound",389113.000000000000000,"G224727E59812N","2008-05-01T00:00:00",176024.904073355777655,0.176025000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224727E59812N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.270423442812216,59.812428499999996]
["glac_bound",389119.000000000000000,"G226810E58217N","2008-05-01T00:00:00",281850.467389325902332,0.281850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226810E58217N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.190941803857356,58.216346000000001]
["glac_bound",389120.000000000000000,"G227297E58495N","2008-05-01T00:00:00",282122.514127944712527,0.282123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227297E58495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.701391934738979,58.493932000000001]
["glac_bound",389121.000000000000000,"G222331E59664N","2008-05-01T00:00:00",556754.486065841629170,0.556754000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222331E59664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.667112385287311,59.663380000000004]
["glac_bound",389123.000000000000000,"G230440E56665N","2008-05-01T00:00:00",1533888.889830357627943,1.533890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230440E56665N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.561313735669103,56.667365500000002]
["glac_bound",389129.000000000000000,"G230083E56958N","2008-05-01T00:00:00",1172971.095337597653270,1.172970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230083E56958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.917996887362619,56.959100999999997]
["glac_bound",389137.000000000000000,"G230520E54916N","2008-05-01T00:00:00",143476.707975722587435,0.143477000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230520E54916N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.480853292565484,54.915006000000005]
["glac_bound",389140.000000000000000,"G229502E57002N","2008-05-01T00:00:00",797007.681009985739365,0.797008000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229502E57002N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.500119545057203,57.002433500000002]
["glac_bound",389142.000000000000000,"G227085E58492N","2008-05-01T00:00:00",728071.795173796941526,0.728072000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227085E58492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.906518331581594,58.493986000000000]
["glac_bound",389160.000000000000000,"G224061E59690N","2008-05-01T00:00:00",586895.705351103679277,0.586896000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224061E59690N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.938808863020142,59.692360000000001]
["glac_bound",389162.000000000000000,"G227931E57973N","2008-05-01T00:00:00",125312.151915073482087,0.125312000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227931E57973N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.069929962982570,57.972054499999999]
["glac_bound",389163.000000000000000,"G222019E59545N","2008-05-01T00:00:00",65098.895765767287230,0.065099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222019E59545N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.983418790158169,59.546522499999995]
["glac_bound",389169.000000000000000,"G226444E58946N","2008-05-01T00:00:00",1350439.574042897438630,1.350440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226444E58946N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.554269560631440,58.948338499999998]
["glac_bound",389172.000000000000000,"G227636E57652N","2008-05-01T00:00:00",4835666.819748783484101,4.835670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227636E57652N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.374177478358206,57.652732999999998]
["glac_bound",389180.000000000000000,"G228704E57248N","2008-05-01T00:00:00",543699.696921423543245,0.543700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228704E57248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.295151226844382,57.247716499999996]
["glac_bound",389182.000000000000000,"G229468E56893N","2008-05-01T00:00:00",302253.153805973706767,0.302253000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229468E56893N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.533694363278187,56.893900000000002]
["glac_bound",389184.000000000000000,"G228758E57150N","2008-05-01T00:00:00",4161234.574776123277843,4.161230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228758E57150N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.242298272445851,57.155023999999997]
["glac_bound",389190.000000000000000,"G223853E59978N","2008-05-01T00:00:00",618330.293057969189249,0.618330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223853E59978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.148081931973934,59.978289500000002]
["glac_bound",389192.000000000000000,"G228515E57356N","2008-05-01T00:00:00",475740.417229897517245,0.475740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228515E57356N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.484571680833028,57.355710000000002]
["glac_bound",389194.000000000000000,"G227267E58154N","2008-05-01T00:00:00",137649.724543855758384,0.137650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227267E58154N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.733627020716000,58.154426000000001]
["glac_bound",389197.000000000000000,"G222546E59373N","2008-05-01T00:00:00",76870.184941221974441,0.076870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222546E59373N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.452599064022138,59.372336500000003]
["glac_bound",389198.000000000000000,"G228564E56605N","2008-05-01T00:00:00",572171.631576585932635,0.572172000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228564E56605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.433730967840262,56.604253999999997]
["glac_bound",389199.000000000000000,"G227479E58145N","2008-05-01T00:00:00",3824010.188327872660011,3.824010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227479E58145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.517450158594869,58.145564499999999]
["glac_bound",389202.000000000000000,"G223532E59464N","2008-05-01T00:00:00",204731.561085439461749,0.204732000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223532E59464N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.467051384542685,59.463826999999995]
["glac_bound",389205.000000000000000,"G229709E56461N","2008-05-01T00:00:00",1084959.486825640546158,1.084960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229709E56461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.291342681459355,56.462090500000002]
["glac_bound",389209.000000000000000,"G229892E57799N","2008-05-01T00:00:00",309519.121512488287408,0.309519000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229892E57799N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.107145563252743,57.799690999999996]
["glac_bound",389210.000000000000000,"G226026E59026N","2008-05-01T00:00:00",150555.065207198553253,0.150555000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA226026E59026N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.974720612360613,59.025313499999996]
["glac_bound",389213.000000000000000,"G226507E58582N","2008-05-01T00:00:00",1315963.161380398320034,1.315960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226507E58582N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.502368217201337,58.584432499999998]
["glac_bound",389216.000000000000000,"G228017E58004N","2008-05-01T00:00:00",1132378.343759161885828,1.132380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228017E58004N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.987588135642341,58.003066000000004]
["glac_bound",389218.000000000000000,"G228760E56626N","2008-05-01T00:00:00",155530.638640512421262,0.155531000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228760E56626N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.240802595567857,56.625691000000003]
["glac_bound",389226.000000000000000,"G229914E57228N","2008-05-01T00:00:00",77762.499817701158463,0.077762000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229914E57228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.084654326785852,57.227987499999998]
["glac_bound",389227.000000000000000,"G229340E57180N","2008-05-01T00:00:00",1638477.152549299178645,1.638480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229340E57180N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.659672968283587,57.180024500000002]
["glac_bound",389231.000000000000000,"G229002E57107N","2008-05-01T00:00:00",6403075.344774220138788,6.403080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229002E57107N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.015350466509005,57.120851999999999]
["glac_bound",389236.000000000000000,"G222940E59400N","2008-05-01T00:00:00",459144.495196263596881,0.459145000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222940E59400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.061260202651511,59.398361500000000]
["glac_bound",389241.000000000000000,"G227173E57988N","2008-05-01T00:00:00",4174388.099063850473613,4.174390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227173E57988N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.840390407735555,57.992782000000005]
["glac_bound",389246.000000000000000,"G230961E57294N","2008-05-01T00:00:00",456895.984204023960046,0.456896000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230961E57294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.038313381837440,57.294542500000006]
["glac_bound",389248.000000000000000,"G229621E56563N","2008-05-01T00:00:00",107242.397057888301788,0.107242000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229621E56563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.379848416356879,56.562769000000003]
["glac_bound",389250.000000000000000,"G225243E59338N","2008-05-01T00:00:00",75835.682818999281153,0.075836000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225243E59338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.757622280701753,59.338947000000005]
["glac_bound",389254.000000000000000,"G226249E58739N","2008-05-01T00:00:00",326715.086921587120742,0.326715000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226249E58739N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.751485634764123,58.742190999999998]
["glac_bound",389258.000000000000000,"G227328E58363N","2008-05-01T00:00:00",439608.852409597137012,0.439609000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227328E58363N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.673260706453902,58.363093500000005]
["glac_bound",389259.000000000000000,"G229097E57088N","2008-05-01T00:00:00",635633.698941747541539,0.635634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229097E57088N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.903565547529354,57.087843499999998]
["glac_bound",389261.000000000000000,"G230399E56078N","2008-05-01T00:00:00",263708.385139231861103,0.263708000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230399E56078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.601013378522225,56.077680000000001]
["glac_bound",389264.000000000000000,"G228711E56636N","2008-05-01T00:00:00",3218837.217352279461920,3.218840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228711E56636N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.282655927554572,56.638553500000000]
["glac_bound",389265.000000000000000,"G230686E55291N","2008-05-01T00:00:00",92377.905389700230444,0.092378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230686E55291N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.312475149097622,55.291817500000001]
["glac_bound",389266.000000000000000,"G230423E55565N","2008-05-01T00:00:00",130470.512788664433174,0.130471000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230423E55565N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.577164325653371,55.565098000000006]
["glac_bound",389268.000000000000000,"G227954E57116N","2008-05-01T00:00:00",3964784.708401930984110,3.964780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227954E57116N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.041171122867809,57.122544500000004]
["glac_bound",389270.000000000000000,"G228401E56871N","2008-05-01T00:00:00",1681556.721623504068702,1.681560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228401E56871N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.599193944671839,56.870961500000007]
["glac_bound",389271.000000000000000,"G223087E59569N","2008-05-01T00:00:00",186783.991523468721425,0.186784000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223087E59569N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.912634030365439,59.569228499999994]
["glac_bound",389275.000000000000000,"G228784E57227N","2008-05-01T00:00:00",819621.251429882715456,41.715600000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228784E57227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.261118362107453,57.306883499999998]
["glac_bound",389275.000000000000000,"G228784E57227N","2008-05-01T00:00:00",40895995.470871277153492,41.715600000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228784E57227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.212409123300120,57.299030000000002]
["glac_bound",389282.000000000000000,"G229299E56467N","2008-05-01T00:00:00",293391.596890823449939,0.293392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229299E56467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.699749766568857,56.466546500000007]
["glac_bound",389283.000000000000000,"G227522E57866N","2008-05-01T00:00:00",4845224.879726636223495,4.845220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227522E57866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.479386092977023,57.875860500000002]
["glac_bound",389289.000000000000000,"G231065E57547N","2008-05-01T00:00:00",148229.769348753150553,0.148230000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231065E57547N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.935204387080574,57.547602499999996]
["glac_bound",389291.000000000000000,"G224117E59881N","2008-05-01T00:00:00",358780.250759393733460,0.358780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224117E59881N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.881119455152657,59.880726499999994]
["glac_bound",389292.000000000000000,"G222764E59134N","2008-05-01T00:00:00",301558.848125274584163,0.301559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222765E59133N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.239019258333315,59.133656500000001]
["glac_bound",389296.000000000000000,"G229104E56507N","2008-05-01T00:00:00",3839717.942091067321599,3.839720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229104E56507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.888313485071308,56.493136999999997]
["glac_bound",389298.000000000000000,"G222776E59354N","2008-05-01T00:00:00",1687410.336614491418004,1.687410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222776E59354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.226080666351208,59.356098000000003]
["glac_bound",389306.000000000000000,"G223980E59982N","2008-05-01T00:00:00",183678.602047252439661,0.183679000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223980E59982N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.020417399501014,59.982158999999996]
["glac_bound",389309.000000000000000,"G230767E56485N","2008-05-01T00:00:00",512474.736842272221111,0.512475000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230767E56485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.239932671568624,56.487041500000004]
["glac_bound",389312.000000000000000,"G227719E57860N","2008-05-01T00:00:00",4298235.673271162435412,4.298240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227719E57860N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.280179817589669,57.860135999999997]
["glac_bound",389315.000000000000000,"G227928E56868N","2008-05-01T00:00:00",5106952.322174233384430,5.106950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227928E56868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.049907336956608,56.853723500000001]
["glac_bound",389316.000000000000000,"G230290E56010N","2008-05-01T00:00:00",1921187.109331925399601,1.921190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230290E56010N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.714795897406475,56.013072999999999]
["glac_bound",389320.000000000000000,"G223202E59516N","2008-05-01T00:00:00",801845.041668663616292,0.801845000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223202E59516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.800398931072209,59.515170499999996]
["glac_bound",389330.000000000000000,"G227630E57675N","2008-05-01T00:00:00",567385.594422474503517,0.567386000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227630E57675N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.368748788977371,57.674684499999998]
["glac_bound",389332.000000000000000,"G229209E57033N","2008-05-01T00:00:00",381562.331132169405464,0.381562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229209E57033N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.790959279731965,57.032333999999999]
["glac_bound",389335.000000000000000,"G229312E56542N","2008-05-01T00:00:00",195062.126078427012544,0.195062000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229312E56542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.687654655698225,56.542326000000003]
["glac_bound",389340.000000000000000,"G223514E59721N","2008-05-01T00:00:00",525728.684084635577165,0.525729000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223514E59721N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.485423970739248,59.720981500000001]
["glac_bound",389343.000000000000000,"G229995E57037N","2008-05-01T00:00:00",98471.627995153088705,0.098472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229995E57037N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.005462107105132,57.037071999999995]
["glac_bound",389348.000000000000000,"G227226E58113N","2008-05-01T00:00:00",146460.615092459484003,0.146461000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227226E58113N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.774051462396017,58.114609500000000]
["glac_bound",389350.000000000000000,"G229568E56514N","2008-05-01T00:00:00",218471.775780690804822,0.218472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229568E56514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.433005417889916,56.513536500000001]
["glac_bound",389351.000000000000000,"G228801E57513N","2008-05-01T00:00:00",2685727.832420675549656,2.685730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228801E57513N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.209053837355299,57.516432000000002]
["glac_bound",389357.000000000000000,"G229014E57400N","2008-05-01T00:00:00",555360.327144454233348,0.555360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229014E57400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.990589278766379,57.401629499999999]
["glac_bound",389359.000000000000000,"G221948E59556N","2008-05-01T00:00:00",86299.819917459579301,0.086300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221948E59556N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.051737091714642,59.556325000000001]
["glac_bound",389365.000000000000000,"G228443E56866N","2008-05-01T00:00:00",709605.160676188766956,0.709605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228443E56866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.556801729004377,56.867931499999997]
["glac_bound",389369.000000000000000,"G223372E59473N","2008-05-01T00:00:00",229582.385462592093972,0.229582000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223372E59473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.629267888743470,59.471710000000002]
["glac_bound",389372.000000000000000,"G230752E56523N","2008-05-01T00:00:00",123496.974875017651357,0.123497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230752E56523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.249432173472997,56.522792499999994]
["glac_bound",389373.000000000000000,"G230458E54671N","2008-05-01T00:00:00",384505.575570113724098,0.384506000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230458E54671N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.542531696474242,54.671778500000002]
["glac_bound",389377.000000000000000,"G230467E56372N","2008-05-01T00:00:00",227378.275794152374147,0.227378000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230467E56372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.533125923879965,56.372436000000000]
["glac_bound",389380.000000000000000,"G229059E57077N","2008-05-01T00:00:00",66396.342917332702200,0.066396000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229059E57077N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.940528405681931,57.076858000000001]
["glac_bound",389389.000000000000000,"G225364E59563N","2008-05-01T00:00:00",1394448.145948689896613,1.394450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225364E59563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.636777282692321,59.563642000000002]
["glac_bound",389390.000000000000000,"G230673E54921N","2008-05-01T00:00:00",63105.237533859166433,0.063105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230673E54921N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.327336178406028,54.920973000000004]
["glac_bound",389396.000000000000000,"G229582E56231N","2008-05-01T00:00:00",330590.909304402186535,0.330591000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229582E56231N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.418576382397845,56.230569500000001]
["glac_bound",389397.000000000000000,"G226586E58771N","2008-05-01T00:00:00",444216.655825763591565,0.444217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226586E58771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.414866640656072,58.770515500000002]
["glac_bound",389398.000000000000000,"G229066E56632N","2008-05-01T00:00:00",1241690.092464060755447,1.241690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229066E56632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.940033086354248,56.630403999999999]
["glac_bound",389399.000000000000000,"G223436E59529N","2008-05-01T00:00:00",207613.925364664843073,0.207614000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223436E59529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.565661732996546,59.530937000000002]
["glac_bound",389401.000000000000000,"G226837E58438N","2008-05-01T00:00:00",101174.474635324906558,0.101174000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226837E58438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.162722114272384,58.437324500000003]
["glac_bound",389402.000000000000000,"G229718E56611N","2008-05-01T00:00:00",1139252.346916003851220,1.139250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229718E56611N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.283439699074052,56.610618000000002]
["glac_bound",389407.000000000000000,"G230182E56226N","2008-05-01T00:00:00",3756456.893018164206296,3.756460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230182E56226N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.813185589356124,56.229118499999998]
["glac_bound",389412.000000000000000,"G221603E59887N","2008-05-01T00:00:00",518963134.82237279415130,518.962999999999965,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","Tweedsmuir Glacier","None","08AB221603E59887N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.445622477396569,59.907463500000006]
["glac_bound",389413.000000000000000,"G225197E59431N","2008-05-01T00:00:00",157068.724834629683755,0.157069000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225197E59431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.802722901036816,59.431429999999999]
["glac_bound",389418.000000000000000,"G230626E56810N","2008-05-01T00:00:00",296369.816092135035433,0.296370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230626E56810N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.374417762995904,56.808727000000005]
["glac_bound",389420.000000000000000,"G228646E56632N","2008-05-01T00:00:00",741697.369986227946356,0.741697000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228646E56632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.353962265882558,56.632820499999994]
["glac_bound",389421.000000000000000,"G228541E57087N","2008-05-01T00:00:00",5286529.079853979870677,5.286530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228541E57087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.442776773384423,57.098842500000003]
["glac_bound",389423.000000000000000,"G227500E58149N","2008-05-01T00:00:00",502113.348761638859287,0.502113000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227500E58149N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.499074092418198,58.148878999999994]
["glac_bound",389429.000000000000000,"G230312E54911N","2008-05-01T00:00:00",61607.474009543628199,0.061608000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230312E54911N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.687759872040573,54.911022000000003]
["glac_bound",389433.000000000000000,"G225486E59340N","2008-05-01T00:00:00",99419.760380212377640,0.099420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225486E59340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.514638186231963,59.340269500000005]
["glac_bound",389436.000000000000000,"G228636E57068N","2008-05-01T00:00:00",4848939.043484861962497,4.848940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228636E57068N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.354924368654224,57.072113500000000]
["glac_bound",389442.000000000000000,"G230399E56767N","2008-05-01T00:00:00",267780.069684015179519,0.267780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230399E56767N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.600009125147295,56.766693500000002]
["glac_bound",389446.000000000000000,"G231440E56216N","2008-05-01T00:00:00",210331.447342999221291,0.210331000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231440E56216N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.559735748623979,56.215695499999995]
["glac_bound",389447.000000000000000,"G227659E57578N","2008-05-01T00:00:00",433413.132900046359282,0.433413000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227659E57578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.340457426262731,57.578717499999996]
["glac_bound",389449.000000000000000,"G227128E58366N","2008-05-01T00:00:00",62035.287333738931920,0.062035000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227128E58366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.872554821184366,58.366028499999999]
["glac_bound",389452.000000000000000,"G230554E56770N","2008-05-01T00:00:00",364028.039071197737940,0.364028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230554E56770N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.446020626984136,56.769230499999999]
["glac_bound",389453.000000000000000,"G230493E55330N","2008-05-01T00:00:00",2817777.014549586456269,2.817780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230493E55330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.514516052064153,55.333915500000003]
["glac_bound",389454.000000000000000,"G230000E56309N","2008-05-01T00:00:00",4361056.444227574393153,4.361060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230000E56309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.998125264659279,56.308624999999999]
["glac_bound",389459.000000000000000,"G226444E58526N","2008-05-01T00:00:00",730970.118238406837918,0.730970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226444E58526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.552314694907977,58.528380999999996]
["glac_bound",389464.000000000000000,"G228134E58065N","2008-05-01T00:00:00",165639.357364306517411,0.165639000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA228134E58065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.869680215586811,58.065571499999997]
["glac_bound",389467.000000000000000,"G226649E58649N","2008-05-01T00:00:00",1290988.909635766642168,1.290990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226649E58649N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.350368515261948,58.647765500000006]
["glac_bound",389468.000000000000000,"G227278E58267N","2008-05-01T00:00:00",1620462.163881354266778,1.620460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227278E58267N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.722832370572206,58.267371499999996]
["glac_bound",389472.000000000000000,"G227818E57400N","2008-05-01T00:00:00",282487.917751817265525,0.282488000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227818E57400N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.180792314610869,57.399643999999995]
["glac_bound",389476.000000000000000,"G228649E56627N","2008-05-01T00:00:00",507922.327378545305692,0.507922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228649E56627N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.349327363787893,56.629102500000002]
["glac_bound",389479.000000000000000,"G230349E54686N","2008-05-01T00:00:00",715136.312566992361099,0.715136000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230349E54686N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.648190053217235,54.685570999999996]
["glac_bound",389485.000000000000000,"G228620E57141N","2008-05-01T00:00:00",177133.622962137946161,0.177134000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228620E57141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.380654700211551,57.141150499999995]
["glac_bound",389487.000000000000000,"G221171E59964N","2008-05-01T00:00:00",117357.936398314093822,0.117358000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221171E59964N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.835370177042790,59.968412000000001]
["glac_bound",389494.000000000000000,"G230640E57286N","2008-05-01T00:00:00",978843.498053389135748,0.978844000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230640E57286N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.356214912037046,57.284129999999998]
["glac_bound",389505.000000000000000,"G228821E57276N","2008-05-01T00:00:00",262946.225251223600935,0.262946000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228821E57276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.179498854339954,57.276325499999999]
["glac_bound",389507.000000000000000,"G222158E59730N","2008-05-01T00:00:00",1338382.499408457428217,1.338380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222158E59730N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.843559903306613,59.736725000000000]
["glac_bound",389510.000000000000000,"G227918E57636N","2008-05-01T00:00:00",109625.984515705044032,0.109626000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227918E57636N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.081813406617215,57.636003000000002]
["glac_bound",389516.000000000000000,"G222352E59771N","2008-05-01T00:00:00",55556373.070816688239574,55.556399999999996,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222352E59771N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.658199843175851,59.744224000000003]
["glac_bound",389520.000000000000000,"G230307E54822N","2008-05-01T00:00:00",289660.057694905437529,0.289660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230307E54822N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.692797639250784,54.823456000000000]
["glac_bound",389524.000000000000000,"G227468E58306N","2008-05-01T00:00:00",1800012.712718736613169,1.800010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227468E58306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.532201125011852,58.304884999999999]
["glac_bound",389528.000000000000000,"G222287E59366N","2008-05-01T00:00:00",160413.114056058344431,0.160413000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222287E59366N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.714499765780715,59.370271000000002]
["glac_bound",389530.000000000000000,"G230286E56322N","2008-05-01T00:00:00",197421.174185373820364,0.197421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230286E56322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.715329844324742,56.322350999999998]
["glac_bound",389540.000000000000000,"G224477E59949N","2008-05-01T00:00:00",182705.711588950071018,0.182706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224477E59949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.523601195871549,59.948680499999995]
["glac_bound",389541.000000000000000,"G222781E59444N","2008-05-01T00:00:00",3336380.577590947039425,3.336380000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222781E59444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.220113382543730,59.441704000000001]
["glac_bound",389542.000000000000000,"G229601E56437N","2008-05-01T00:00:00",56332.636238832892559,0.056333000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229601E56437N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.399342967128376,56.436751999999998]
["glac_bound",389543.000000000000000,"G228285E57261N","2008-05-01T00:00:00",288485.047576008713804,0.288485000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228285E57261N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.715107804836293,57.260866000000000]
["glac_bound",389544.000000000000000,"G223151E59562N","2008-05-01T00:00:00",817508.256636959849857,0.817508000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223151E59562N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.846863420327423,59.566243499999999]
["glac_bound",389546.000000000000000,"G230156E56326N","2008-05-01T00:00:00",90383.757248951485963,0.090384000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230156E56326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.845544914324762,56.327802500000004]
["glac_bound",389549.000000000000000,"G230185E56642N","2008-05-01T00:00:00",265098.667564288014546,0.265099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230185E56642N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.816718150945491,56.644281499999998]
["glac_bound",389550.000000000000000,"G228577E57578N","2008-05-01T00:00:00",227210.664111004967708,0.227211000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228577E57578N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.423051578948275,57.577683000000000]
["glac_bound",389560.000000000000000,"G228779E57444N","2008-05-01T00:00:00",2489724.415431945584714,2.489720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228779E57444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.222284220080553,57.445973499999994]
["glac_bound",389566.000000000000000,"G230244E56353N","2008-05-01T00:00:00",744839.489683574298397,0.744839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230244E56353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.757636891555535,56.353038499999997]
["glac_bound",389574.000000000000000,"G227568E57615N","2008-05-01T00:00:00",1218748.060868903761730,1.218750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227568E57615N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.430500846902646,57.619010500000002]
["glac_bound",389578.000000000000000,"G228608E57354N","2008-05-01T00:00:00",259810.231577795348130,0.259810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228608E57354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.392393082706775,57.353695000000002]
["glac_bound",389581.000000000000000,"G230356E55159N","2008-05-01T00:00:00",54295.130069821432699,0.054295000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230356E55159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.644269450115019,55.158462499999999]
["glac_bound",389584.000000000000000,"G230862E54915N","2008-05-01T00:00:00",308347.616016365878750,0.308348000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230862E54915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.142322134924314,54.916921500000001]
["glac_bound",389587.000000000000000,"G227942E57282N","2008-05-01T00:00:00",830874.372292839223519,0.830874000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227942E57282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.059815855799371,57.279606000000001]
["glac_bound",389589.000000000000000,"G222395E59923N","2008-05-01T00:00:00",898685.443562303902581,0.898685000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222395E59923N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.607913264021363,59.924337999999999]
["glac_bound",389601.000000000000000,"G229145E56552N","2008-05-01T00:00:00",83623.676495645995601,0.083624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229145E56552N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.856024463312508,56.552285499999996]
["glac_bound",389605.000000000000000,"G223145E59379N","2008-05-01T00:00:00",617252.594357057125308,0.617253000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223145E59379N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.863826514896175,59.379234500000003]
["glac_bound",389607.000000000000000,"G228716E57460N","2008-05-01T00:00:00",71475.016641222318867,0.071475000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228716E57460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.283684442567562,57.458940499999997]
["glac_bound",389610.000000000000000,"G228766E57004N","2008-05-01T00:00:00",647530.215810374123976,0.647530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228766E57004N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.237486472305363,57.009125499999996]
["glac_bound",389613.000000000000000,"G227849E57362N","2008-05-01T00:00:00",2627680.855735388584435,2.627680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227849E57362N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.135263916584790,57.353687499999999]
["glac_bound",389617.000000000000000,"G228068E57478N","2008-05-01T00:00:00",161323.040198824455729,0.161323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228068E57478N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.932244255797684,57.477815000000000]
["glac_bound",389619.000000000000000,"G230658E55607N","2008-05-01T00:00:00",233246.770177921687718,0.233247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230658E55607N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.337001167754579,55.608958999999999]
["glac_bound",389624.000000000000000,"G225689E59340N","2008-05-01T00:00:00",2126353.265628121793270,2.126350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225689E59340N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.308436762636035,59.347075000000004]
["glac_bound",389626.000000000000000,"G223268E59542N","2008-05-01T00:00:00",551198.573753812699579,0.551199000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223268E59542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.732539360264639,59.540850500000005]
["glac_bound",389631.000000000000000,"G225586E59500N","2008-05-01T00:00:00",272772.335820456384681,0.272772000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225586E59500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.409748106793501,59.498297500000000]
["glac_bound",389638.000000000000000,"G228502E57462N","2008-05-01T00:00:00",175723.851665107125882,0.175724000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228502E57462N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.499690938149143,57.461202000000000]
["glac_bound",389639.000000000000000,"G229064E57011N","2008-05-01T00:00:00",1083581.193691439228132,1.083580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229064E57011N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.930806267245714,57.011860999999996]
["glac_bound",389640.000000000000000,"G226261E58734N","2008-05-01T00:00:00",11058787.668387955054641,11.058800000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226261E58734N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.733800522319143,58.739983500000001]
["glac_bound",389645.000000000000000,"G230701E55239N","2008-05-01T00:00:00",171661.743064133479493,0.171662000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230701E55239N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.301312086363623,55.237154500000003]
["glac_bound",389657.000000000000000,"G229272E57091N","2008-05-01T00:00:00",65948.096061849355465,0.065948000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229272E57091N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.728073997179905,57.090684499999995]
["glac_bound",389661.000000000000000,"G228038E57457N","2008-05-01T00:00:00",3259955.198077480774373,3.259960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228038E57457N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.961122644180506,57.455083000000002]
["glac_bound",389674.000000000000000,"G225084E59594N","2008-05-01T00:00:00",178770.469959477544762,0.178770000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225084E59594N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.914349492819099,59.593804500000005]
["glac_bound",389675.000000000000000,"G229825E56847N","2008-05-01T00:00:00",889713.592663084855303,0.889714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229825E56847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.173647340803115,56.851877000000002]
["glac_bound",389684.000000000000000,"G232488E57787N","2008-05-01T00:00:00",120956.148041949709295,0.120956000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232488E57787N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.512138540264715,57.787293000000005]
["glac_bound",389685.000000000000000,"G230003E56337N","2008-05-01T00:00:00",138560.748198716144543,0.138561000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230003E56337N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.994419499558887,56.336005000000000]
["glac_bound",389687.000000000000000,"G228963E57102N","2008-05-01T00:00:00",99090.820965028950013,0.099091000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228963E57102N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.036876346496854,57.102322000000001]
["glac_bound",389691.000000000000000,"G226912E58059N","2008-05-01T00:00:00",287978.313982925086748,0.287978000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226912E58059N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.087045402725948,58.059123499999998]
["glac_bound",389693.000000000000000,"G227283E58000N","2008-05-01T00:00:00",2341272.389233034104109,2.341270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227283E58000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.718103334708246,58.003054000000006]
["glac_bound",389694.000000000000000,"G230194E57307N","2008-05-01T00:00:00",107301.475560237377067,0.107301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230194E57307N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.805709159281093,57.307211500000001]
["glac_bound",389697.000000000000000,"G231460E56131N","2008-05-01T00:00:00",140224.216062422288815,0.140224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231460E56131N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.542012007943924,56.130645999999999]
["glac_bound",389698.000000000000000,"G230340E56487N","2008-05-01T00:00:00",577943.621322102611884,0.577944000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230340E56487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.660257099489797,56.488036500000000]
["glac_bound",389700.000000000000000,"G225967E59006N","2008-05-01T00:00:00",361316.434453042049427,0.361316000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225967E59006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.031315430071999,59.006084500000000]
["glac_bound",389701.000000000000000,"G222440E59162N","2008-05-01T00:00:00",419546546.47414183616638,419.547000000000025,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Melbern Glacier","CA2N002FA001","08BF222646E59030N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.556734527892559,59.073252500000002]
["glac_bound",389705.000000000000000,"G229435E56387N","2008-05-01T00:00:00",3216158.994747716002166,3.216160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229435E56387N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.565026621499811,56.389408500000002]
["glac_bound",389708.000000000000000,"G223275E59192N","2008-05-01T00:00:00",561240.530663540586829,0.561241000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223274E59189N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.722481525929538,59.191151500000004]
["glac_bound",389714.000000000000000,"G230506E55254N","2008-05-01T00:00:00",1117024.177025597309694,1.117020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230506E55254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.499481154564535,55.254547000000002]
["glac_bound",389716.000000000000000,"G228029E57824N","2008-05-01T00:00:00",242600.741436213691486,0.242601000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228029E57824N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.970733749651004,57.824511000000001]
["glac_bound",389717.000000000000000,"G226995E58422N","2008-05-01T00:00:00",259342.735444322141120,0.259343000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226995E58422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.004710884578543,58.422097999999998]
["glac_bound",389722.000000000000000,"G230484E56622N","2008-05-01T00:00:00",127767.972634946738253,0.127768000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230484E56622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.515714167608280,56.622404000000003]
["glac_bound",389723.000000000000000,"G230089E56257N","2008-05-01T00:00:00",8710490.735953727737069,8.710490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230089E56257N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.915412037133677,56.249853999999999]
["glac_bound",389725.000000000000000,"G229802E57778N","2008-05-01T00:00:00",101192.350781171553535,0.101192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229802E57778N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.195822708365142,57.778040500000003]
["glac_bound",389726.000000000000000,"G228494E57529N","2008-05-01T00:00:00",127850.423698466067435,0.127850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228494E57529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.503105207895885,57.529021000000000]
["glac_bound",389727.000000000000000,"G229571E56272N","2008-05-01T00:00:00",879725.062944913748652,0.879725000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229571E56272N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.431897338411716,56.272520999999998]
["glac_bound",389728.000000000000000,"G230589E55244N","2008-05-01T00:00:00",2436197.489866755902767,2.436200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230589E55244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.413639170375859,55.243443499999998]
["glac_bound",389729.000000000000000,"G230310E55597N","2008-05-01T00:00:00",168652.815188370092073,0.168653000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230310E55597N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.690538760169488,55.597927999999996]
["glac_bound",389731.000000000000000,"G223048E59563N","2008-05-01T00:00:00",602839.419093571137637,0.602839000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223048E59563N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.951090877833167,59.561992500000002]
["glac_bound",389744.000000000000000,"G226469E58764N","2008-05-01T00:00:00",175436.316874148382340,0.175436000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226469E58764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.529069566437499,58.764195999999998]
["glac_bound",389749.000000000000000,"G229001E56440N","2008-05-01T00:00:00",2600167.515622898470610,2.600170000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229001E56440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.995311075829392,56.443443000000002]
["glac_bound",389751.000000000000000,"G228425E56920N","2008-05-01T00:00:00",188766.946678127045743,0.188767000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228425E56920N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.576843233428605,56.921110999999996]
["glac_bound",389753.000000000000000,"G230124E56517N","2008-05-01T00:00:00",584177.514089912991039,0.584177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230124E56517N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.874891715794433,56.516969000000003]
["glac_bound",389763.000000000000000,"G223720E59973N","2008-05-01T00:00:00",156065.988142562855501,0.156066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223720E59973N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.279912184635805,59.972997499999998]
["glac_bound",389771.000000000000000,"G229424E56859N","2008-05-01T00:00:00",1052780.736364434473217,1.052780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229424E56859N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.581093630813939,56.866794999999996]
["glac_bound",389775.000000000000000,"G229731E56789N","2008-05-01T00:00:00",67224.090800563295488,0.067224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229731E56789N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.269743591488577,56.789473000000001]
["glac_bound",389776.000000000000000,"G230948E56525N","2008-05-01T00:00:00",404702.694577490270603,0.404703000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230948E56525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.052054178571439,56.524948499999994]
["glac_bound",389779.000000000000000,"G227872E57431N","2008-05-01T00:00:00",14026433.167672242969275,14.026400000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227872E57431N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.153022662653200,57.427292500000000]
["glac_bound",389780.000000000000000,"G230071E57359N","2008-05-01T00:00:00",168176.636129218037240,0.168177000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230071E57359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.928125492351569,57.359492000000003]
["glac_bound",389787.000000000000000,"G221843E59958N","2008-05-01T00:00:00",142824.475291896291310,0.142824000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221843E59958N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.157335601936211,59.956608000000003]
["glac_bound",389792.000000000000000,"G225334E59516N","2008-05-01T00:00:00",1145689.247399621177465,1.145690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225334E59516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.662306901858585,59.516103000000001]
["glac_bound",389795.000000000000000,"G222537E59380N","2008-05-01T00:00:00",976959.763062330544926,0.976960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222537E59380N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.462586059903401,59.380285499999999]
["glac_bound",389796.000000000000000,"G222274E59297N","2008-05-01T00:00:00",556545.992873314418830,0.556546000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222274E59297N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.729732050840170,59.298699499999998]
["glac_bound",389800.000000000000000,"G228558E56788N","2008-05-01T00:00:00",896039.877180589013733,0.896040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228558E56788N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.442909753570575,56.785456499999995]
["glac_bound",389805.000000000000000,"G223926E59766N","2008-05-01T00:00:00",149788.475660015596077,0.149788000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223926E59766N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.073445983392673,59.767428499999994]
["glac_bound",389808.000000000000000,"G227122E58245N","2008-05-01T00:00:00",1127183.537314953049645,1.127180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227122E58245N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.879543977671744,58.245838500000005]
["glac_bound",389813.000000000000000,"G230382E55655N","2008-05-01T00:00:00",442704.847461540193763,0.442705000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230382E55655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.617953153738256,55.654626000000000]
["glac_bound",389816.000000000000000,"G223016E59521N","2008-05-01T00:00:00",643657.488412557402626,0.643658000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223016E59521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.986323990384619,59.521023499999998]
["glac_bound",389825.000000000000000,"G225752E59184N","2008-05-01T00:00:00",938152.230341736692935,0.938152000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225752E59184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.251169596435574,59.185563999999999]
["glac_bound",389827.000000000000000,"G221760E59992N","2008-05-01T00:00:00",403888.055762116215192,0.403888000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221760E59992N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.238700295454549,59.991102999999995]
["glac_bound",389832.000000000000000,"G223757E59964N","2008-05-01T00:00:00",61199.614516193018062,0.061200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223757E59964N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.241905149202751,59.963496500000005]
["glac_bound",389833.000000000000000,"G226950E58041N","2008-05-01T00:00:00",71975.540797016801662,0.071975000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226950E58041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.048146151391052,58.041766500000001]
["glac_bound",389837.000000000000000,"G227645E57466N","2008-05-01T00:00:00",814582.982800488360226,0.814583000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227645E57466N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.358217427042348,57.466403000000000]
["glac_bound",389847.000000000000000,"G230590E56720N","2008-05-01T00:00:00",798665.167862088070251,0.798665000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230590E56720N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.412261922029927,56.723033000000001]
["glac_bound",389853.000000000000000,"G228504E57443N","2008-05-01T00:00:00",346949.089887708891183,0.346949000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228504E57443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.490699623644559,57.443919500000007]
["glac_bound",389856.000000000000000,"G224606E59986N","2008-05-01T00:00:00",948278.063016159110703,0.948278000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224606E59986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.390286669427724,59.987816499999994]
["glac_bound",389860.000000000000000,"G229855E56618N","2008-05-01T00:00:00",814538.280711367609911,0.814538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229855E56618N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.143226987899141,56.617407499999999]
["glac_bound",389862.000000000000000,"G230787E55069N","2008-05-01T00:00:00",351751.945781689137220,0.351752000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230787E55069N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.211175821775385,55.072975999999997]
["glac_bound",389867.000000000000000,"G225247E59464N","2008-05-01T00:00:00",51503.018785926331475,0.051503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225247E59464N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.752693144658508,59.463870499999999]
["glac_bound",389868.000000000000000,"G228851E56765N","2008-05-01T00:00:00",336972.272831353242509,0.336972000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228851E56765N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.144434370489677,56.762180000000001]
["glac_bound",389872.000000000000000,"G231073E57142N","2008-05-01T00:00:00",917706.552962838439271,0.917707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231073E57142N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.925347467426832,57.141794500000003]
["glac_bound",389876.000000000000000,"G229815E56605N","2008-05-01T00:00:00",547854.086420012754388,0.547854000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229815E56605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.185220445113060,56.606649000000004]
["glac_bound",389880.000000000000000,"G226089E58811N","2008-05-01T00:00:00",410048.816044257604517,0.410049000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226089E58811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.911081386746957,58.811756500000001]
["glac_bound",389882.000000000000000,"G230740E55661N","2008-05-01T00:00:00",163168.626950103003765,0.163169000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230740E55661N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.263499090972232,55.661109499999995]
["glac_bound",389886.000000000000000,"G227466E58188N","2008-05-01T00:00:00",89975.660691466895514,0.089976000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227466E58188N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.532756061841440,58.187410499999999]
["glac_bound",389889.000000000000000,"G230082E56530N","2008-05-01T00:00:00",204615.624520711920923,0.204616000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230082E56530N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.918764985130110,56.530580000000000]
["glac_bound",389897.000000000000000,"G227576E57662N","2008-05-01T00:00:00",9881534.644635612145066,9.881530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227576E57662N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.451414737339860,57.666832999999997]
["glac_bound",389906.000000000000000,"G228509E56781N","2008-05-01T00:00:00",4946681.046861628070474,4.946680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228509E56781N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.489627448759450,56.783753000000004]
["glac_bound",389907.000000000000000,"G230327E56292N","2008-05-01T00:00:00",221256.868261502328096,0.221257000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230327E56292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.670053756127601,56.292776000000003]
["glac_bound",389909.000000000000000,"G230607E55342N","2008-05-01T00:00:00",403799.154590153775644,0.403799000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230607E55342N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.393101329834820,55.342622499999997]
["glac_bound",389912.000000000000000,"G229229E57208N","2008-05-01T00:00:00",55038.460145071345323,0.055038000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229229E57208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.770432360158509,57.208410999999998]
["glac_bound",389914.000000000000000,"G224301E59742N","2008-05-01T00:00:00",255151.167103372310521,0.255151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224301E59742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.698412096915263,59.741320500000000]
["glac_bound",389915.000000000000000,"G225774E59152N","2008-05-01T00:00:00",1279278.392762648174539,1.279280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225774E59152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.229634194574089,59.156534499999999]
["glac_bound",389916.000000000000000,"G230435E55199N","2008-05-01T00:00:00",83004.701340742889442,0.083005000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230435E55199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.566338542964047,55.199072000000001]
["glac_bound",389917.000000000000000,"G227677E58229N","2008-05-01T00:00:00",51087.616448853397742,0.051088000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227677E58229N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.321969011350348,58.229911999999999]
["glac_bound",389920.000000000000000,"G229284E56861N","2008-05-01T00:00:00",1631713.395468556787819,1.631710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229284E56861N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.716701057613164,56.861874000000000]
["glac_bound",389922.000000000000000,"G230229E57036N","2008-05-01T00:00:00",126664.504808655910892,0.126665000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230229E57036N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.770476966163187,57.035964500000006]
["glac_bound",389925.000000000000000,"G230095E57000N","2008-05-01T00:00:00",66775.091023471410153,0.066775000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230095E57000N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.905143249532642,57.000272500000001]
["glac_bound",389927.000000000000000,"G225680E59169N","2008-05-01T00:00:00",467755.865768167364877,0.467756000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225680E59169N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.321307690633603,59.168876999999995]
["glac_bound",389928.000000000000000,"G226078E58902N","2008-05-01T00:00:00",11421623.718482160940766,11.421600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226078E58902N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.896692594658418,58.908603999999997]
["glac_bound",389930.000000000000000,"G230534E56724N","2008-05-01T00:00:00",247187.655495285434881,0.247188000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230534E56724N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.467275946397706,56.723735000000005]
["glac_bound",389932.000000000000000,"G226666E58487N","2008-05-01T00:00:00",367079.242591351736337,0.367079000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226666E58487N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.336210186098413,58.487268999999998]
["glac_bound",389933.000000000000000,"G229863E56375N","2008-05-01T00:00:00",260785.360741183423670,0.260785000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229863E56375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.140489323536201,56.374998500000004]
["glac_bound",389939.000000000000000,"G230094E57355N","2008-05-01T00:00:00",124342.390807169897016,0.124342000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230094E57355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.905641638507063,57.355034000000003]
["glac_bound",389940.000000000000000,"G228623E56626N","2008-05-01T00:00:00",1094502.590853680158034,1.094500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228623E56626N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.370695792603954,56.629176999999999]
["glac_bound",389941.000000000000000,"G229050E56742N","2008-05-01T00:00:00",319038.960261625179555,0.319039000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229050E56742N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.949618608814035,56.742870999999994]
["glac_bound",389943.000000000000000,"G227947E57362N","2008-05-01T00:00:00",112890.291226718545659,0.112890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227947E57362N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.052622282658376,57.362376999999995]
["glac_bound",389949.000000000000000,"G225156E59628N","2008-05-01T00:00:00",100846.707283461713814,0.100847000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225156E59628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.843929513715693,59.627476000000001]
["glac_bound",389950.000000000000000,"G223343E59516N","2008-05-01T00:00:00",13089396.299651261419058,13.089399999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223343E59516N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.671453043233100,59.522395500000002]
["glac_bound",389951.000000000000000,"G223664E59718N","2008-05-01T00:00:00",288471.246833110169973,0.288471000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223664E59718N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.335738367768670,59.718083000000000]
["glac_bound",389957.000000000000000,"G230710E55652N","2008-05-01T00:00:00",273388.082588363729883,0.273388000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230710E55652N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.292400589372363,55.652374500000001]
["glac_bound",389960.000000000000000,"G230747E56528N","2008-05-01T00:00:00",102472.105203946935944,0.102472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230747E56528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.252581906796109,56.528410999999998]
["glac_bound",389966.000000000000000,"G228297E57273N","2008-05-01T00:00:00",1043679.104215837083757,1.043680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228297E57273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.706411402616425,57.271808000000000]
["glac_bound",389969.000000000000000,"G228523E57072N","2008-05-01T00:00:00",657041.758757588686422,0.657042000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228523E57072N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.476019507219235,57.072364499999999]
["glac_bound",389972.000000000000000,"G230900E54917N","2008-05-01T00:00:00",4142288.378940634429455,4.142290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230900E54917N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.098207181446355,54.929203500000000]
["glac_bound",389973.000000000000000,"G223707E59791N","2008-05-01T00:00:00",3505892.017711755819619,3.505890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223707E59791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.295586676279783,59.792600500000006]
["glac_bound",389978.000000000000000,"G223355E59555N","2008-05-01T00:00:00",3372630.400913370307535,3.372630000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223355E59555N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.647027053054046,59.557524500000000]
["glac_bound",389983.000000000000000,"G226931E58259N","2008-05-01T00:00:00",519457.569389696698636,0.519458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226931E58259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.069801773566866,58.260429500000001]
["glac_bound",389985.000000000000000,"G229058E56624N","2008-05-01T00:00:00",234260.538456048525404,0.234261000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229058E56624N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.941949822008098,56.623849000000000]
["glac_bound",389990.000000000000000,"G222513E59627N","2008-05-01T00:00:00",296302.186317836341914,0.296302000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222513E59627N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.489454139753576,59.626421999999998]
["glac_bound",389991.000000000000000,"G230431E55615N","2008-05-01T00:00:00",1176048.837180173490196,1.176050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230431E55615N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.570135888422499,55.613924499999996]
["glac_bound",389995.000000000000000,"G230628E55355N","2008-05-01T00:00:00",431649.656696502410341,0.431650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230628E55355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.372004082179927,55.355675500000004]
["glac_bound",389997.000000000000000,"G229416E57123N","2008-05-01T00:00:00",961400.429938084445894,0.961400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229416E57123N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.583112671305855,57.122338999999997]
["glac_bound",390000.000000000000000,"G229232E56868N","2008-05-01T00:00:00",324458.226000749447849,0.324458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229232E56868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.768454196202526,56.867888500000007]
["glac_bound",390003.000000000000000,"G230153E55743N","2008-05-01T00:00:00",50503.933086476507015,0.050504000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230153E55743N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.847379200354624,55.742909999999995]
["glac_bound",390004.000000000000000,"G228854E57152N","2008-05-01T00:00:00",95908153.269682198762894,95.908100000000005,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228854E57152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.071784773806996,57.174298499999999]
["glac_bound",390010.000000000000000,"G228097E57355N","2008-05-01T00:00:00",170078.410823670506943,0.170078000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228097E57355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.903016451491595,57.355154999999996]
["glac_bound",390012.000000000000000,"G228931E56761N","2008-05-01T00:00:00",220213.460543612280162,0.220213000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228931E56761N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.068514851115424,56.760688500000001]
["glac_bound",390014.000000000000000,"G230550E54661N","2008-05-01T00:00:00",298947.661496142740361,0.298948000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230550E54661N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.449652910602623,54.661189499999999]
["glac_bound",390020.000000000000000,"G228738E56646N","2008-05-01T00:00:00",162652.924151300947415,0.162653000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228738E56646N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.262056444179734,56.646291500000004]
["glac_bound",390021.000000000000000,"G228924E57529N","2008-05-01T00:00:00",1937346.195463269716129,1.937350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228924E57529N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.080004738754752,57.528618999999999]
["glac_bound",390024.000000000000000,"G222696E59152N","2008-05-01T00:00:00",1418310.402994755655527,1.418310000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222696E59152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.316920534820497,59.155928500000002]
["glac_bound",390026.000000000000000,"G230497E56758N","2008-05-01T00:00:00",699508.539856415591203,0.699509000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230497E56758N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.503039339604697,56.759530999999996]
["glac_bound",390030.000000000000000,"G227620E58274N","2008-05-01T00:00:00",561652.965230308356695,0.561653000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227620E58274N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.380940262097113,58.275909499999997]
["glac_bound",390037.000000000000000,"G230578E56709N","2008-05-01T00:00:00",624941.623124788631685,0.624942000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230578E56709N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.421319676165808,56.713337499999994]
["glac_bound",390039.000000000000000,"G228528E57281N","2008-05-01T00:00:00",4314828.223047559149563,4.314830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228528E57281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.498063780806831,57.286740000000002]
["glac_bound",390043.000000000000000,"G228013E57372N","2008-05-01T00:00:00",5481980.982637508772314,5.481980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228013E57372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.982924342063001,57.386787499999997]
["glac_bound",390050.000000000000000,"G228895E57381N","2008-05-01T00:00:00",324450.883266692631878,0.324451000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228895E57381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.103814504269451,57.381242499999999]
["glac_bound",390053.000000000000000,"G227485E58238N","2008-05-01T00:00:00",125798.324874950543744,0.125798000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227485E58238N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.515645623977662,58.238558499999996]
["glac_bound",390056.000000000000000,"G223654E59755N","2008-05-01T00:00:00",59826.474485228238336,0.059826000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223654E59755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.347395662815870,59.754796499999998]
["glac_bound",390058.000000000000000,"G228021E57427N","2008-05-01T00:00:00",1117367.995252393186092,1.117370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228021E57427N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.982639621626163,57.425970499999998]
["glac_bound",390062.000000000000000,"G227688E57848N","2008-05-01T00:00:00",2277903.194643493276089,2.277900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227688E57848N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.312163228149075,57.847453000000002]
["glac_bound",390063.000000000000000,"G223426E59498N","2008-05-01T00:00:00",227119.191686150123132,0.227119000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223426E59498N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.573480586646042,59.497743499999999]
["glac_bound",390066.000000000000000,"G223187E59528N","2008-05-01T00:00:00",1511288.058899235678837,1.511290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223187E59528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.814778229869233,59.529830500000003]
["glac_bound",390070.000000000000000,"G225661E59240N","2008-05-01T00:00:00",136238.613492912001675,0.136239000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225661E59240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.338249346454575,59.241253999999998]
["glac_bound",390071.000000000000000,"G226867E58617N","2008-05-01T00:00:00",2096692.219202069565654,2.096690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226867E58617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.134991089093887,58.623178500000002]
["glac_bound",390077.000000000000000,"G230793E56465N","2008-05-01T00:00:00",102060.396996213195962,0.102060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230793E56465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.206255988643363,56.465126499999997]
["glac_bound",390079.000000000000000,"G223304E59444N","2008-05-01T00:00:00",27253411.424344249069691,27.253399999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223304E59444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.709795072518546,59.482598000000003]
["glac_bound",390081.000000000000000,"G230122E56184N","2008-05-01T00:00:00",585306.209841329837218,0.585306000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230122E56184N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.877078289809162,56.183576500000001]
["glac_bound",390087.000000000000000,"G229308E56507N","2008-05-01T00:00:00",119505.400333752069855,0.119505000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229308E56507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.690335785532994,56.507019499999998]
["glac_bound",390094.000000000000000,"G222057E59534N","2008-05-01T00:00:00",876270.950533406343311,0.876271000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222057E59534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.942860256812423,59.534621000000001]
["glac_bound",390104.000000000000000,"G230508E56620N","2008-05-01T00:00:00",55471.591923834326735,0.055472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230508E56620N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.492690814429380,56.620497499999999]
["glac_bound",390106.000000000000000,"G228965E56409N","2008-05-01T00:00:00",320734.423827997467015,0.320734000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD228965E56409N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.040874571766551,56.405667000000001]
["glac_bound",390117.000000000000000,"G230526E56254N","2008-05-01T00:00:00",918707.720877774176188,0.918708000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230526E56254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.472541578476864,56.253606500000004]
["glac_bound",390125.000000000000000,"G230296E55645N","2008-05-01T00:00:00",119490.611592640649178,0.119491000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230296E55645N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.703858340007571,55.644804500000006]
["glac_bound",390127.000000000000000,"G229266E56847N","2008-05-01T00:00:00",102335.266099248750834,0.102335000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229266E56847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.733528262886608,56.847198499999998]
["glac_bound",390129.000000000000000,"G230211E56300N","2008-05-01T00:00:00",701968.297951390268281,0.701968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230211E56300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.791591969555498,56.299436999999998]
["glac_bound",390135.000000000000000,"G230381E55525N","2008-05-01T00:00:00",59420.705310220233514,0.059421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230381E55525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.618091542357490,55.524614499999998]
["glac_bound",390139.000000000000000,"G229990E56580N","2008-05-01T00:00:00",494008.417609481664840,0.494008000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229990E56580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.010207303546593,56.579965500000000]
["glac_bound",390140.000000000000000,"G227688E56917N","2008-05-01T00:00:00",90471.823852437926689,0.090472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","LeConte Glacier","US2NOO2O1803","08CF227919E57041N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.082713615081786,57.041606000000002]
["glac_bound",390144.000000000000000,"G230358E56691N","2008-05-01T00:00:00",79549.410462292187731,0.079549000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230358E56691N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.640808568775384,56.690917499999998]
["glac_bound",390150.000000000000000,"G230647E57071N","2008-05-01T00:00:00",1840913.613490956369787,1.840910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230647E57071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.345393233737838,57.074026000000003]
["glac_bound",390152.000000000000000,"G230232E54432N","2008-05-01T00:00:00",259984.951960828329902,0.259985000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08EG230232E54432N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.768844109738950,54.432105500000006]
["glac_bound",390154.000000000000000,"G230709E56785N","2008-05-01T00:00:00",1362081.931903817690909,1.362080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230709E56785N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.290614460586823,56.784822000000005]
["glac_bound",390155.000000000000000,"G224482E59956N","2008-05-01T00:00:00",367497.331077936105430,0.367497000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224482E59956N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.518763160116009,59.955910500000002]
["glac_bound",390156.000000000000000,"G229825E56089N","2008-05-01T00:00:00",8791096.836940025910735,8.791100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","Texas Glacier","None","08DD229825E56089N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.194956876981564,56.091057500000005]
["glac_bound",390167.000000000000000,"G226745E58492N","2008-05-01T00:00:00",545894.430404183221981,0.545894000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226745E58492N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.262375064365671,58.494540999999998]
["glac_bound",390168.000000000000000,"G228930E57661N","2008-05-01T00:00:00",281756.963945684779901,0.281757000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228930E57661N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.069766468522744,57.660606500000000]
["glac_bound",390173.000000000000000,"G229323E57273N","2008-05-01T00:00:00",1113561.181473039556295,1.113560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229323E57273N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.674992229613395,57.271846499999995]
["glac_bound",390184.000000000000000,"G230202E57287N","2008-05-01T00:00:00",176020.487862350855721,0.176020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230202E57287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.798563960362742,57.286815500000003]
["glac_bound",390186.000000000000000,"G225742E59331N","2008-05-01T00:00:00",170698.728677123726811,0.170699000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225742E59331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.256647821504771,59.331282500000000]
["glac_bound",390188.000000000000000,"G230248E55777N","2008-05-01T00:00:00",65843.617719331232365,0.065844000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230248E55777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.753280092350735,55.776316500000000]
["glac_bound",390189.000000000000000,"G229197E57076N","2008-05-01T00:00:00",2318893.366013083606958,2.318890000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229197E57076N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.792906198774205,57.086028499999998]
["glac_bound",390193.000000000000000,"G228154E57410N","2008-05-01T00:00:00",301962.568275482219178,0.301963000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228154E57410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.845966006737058,57.411136999999997]
["glac_bound",390195.000000000000000,"G222959E59580N","2008-05-01T00:00:00",995798.037246990250424,0.995798000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222959E59580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.046386316348986,59.580941500000002]
["glac_bound",390203.000000000000000,"G227268E58339N","2008-05-01T00:00:00",2002643.645875446731225,2.002640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227268E58339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.733699933654407,58.341660500000003]
["glac_bound",390206.000000000000000,"G229499E56713N","2008-05-01T00:00:00",738969.051970783038996,0.738969000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229499E56713N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.500753764408103,56.712894500000004]
["glac_bound",390213.000000000000000,"G226067E58945N","2008-05-01T00:00:00",49894380.858024492859840,49.894399999999997,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226067E58945N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.993024453956195,58.964062499999997]
["glac_bound",390214.000000000000000,"G224529E59829N","2008-05-01T00:00:00",775467.908013476990163,0.775468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224529E59829N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.469044039789054,59.829902000000004]
["glac_bound",390217.000000000000000,"G228084E57532N","2008-05-01T00:00:00",713464.892108674626797,0.713465000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228084E57532N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.916799551199176,57.531629500000001]
["glac_bound",390219.000000000000000,"G227114E58180N","2008-05-01T00:00:00",412502.920208314899355,0.412503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227114E58180N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.884928853388061,58.183047000000002]
["glac_bound",390221.000000000000000,"G226809E58426N","2008-05-01T00:00:00",1756331.750743341632187,1.756330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226809E58426N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.186942067345967,58.430269499999994]
["glac_bound",390224.000000000000000,"G228540E56918N","2008-05-01T00:00:00",1250918.678168271901086,1.250920000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228540E56918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.460669087205133,56.925538000000003]
["glac_bound",390225.000000000000000,"G227679E57570N","2008-05-01T00:00:00",3236262.791916410438716,3.236260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227679E57570N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.322812961101761,57.572649499999997]
["glac_bound",390237.000000000000000,"G221769E59802N","2008-05-01T00:00:00",518666.851416810415685,0.518667000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221769E59802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.229181395005099,59.804184499999998]
["glac_bound",390242.000000000000000,"G230162E57028N","2008-05-01T00:00:00",3749753.037996730767190,3.749750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230162E57028N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.830215311955726,57.034888000000002]
["glac_bound",390245.000000000000000,"G224008E59728N","2008-05-01T00:00:00",629519.555077668279409,0.629520000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224008E59728N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.995624236062412,59.730585000000005]
["glac_bound",390246.000000000000000,"G223139E59705N","2008-05-01T00:00:00",1167471.212718497496098,1.167470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223139E59705N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.858549553840874,59.706496500000000]
["glac_bound",390247.000000000000000,"G227973E57606N","2008-05-01T00:00:00",235634.354603887361009,0.235634000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227973E57606N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.027220569478004,57.606436500000001]
["glac_bound",390248.000000000000000,"G230349E56314N","2008-05-01T00:00:00",143933.887046361051034,0.143934000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230349E56314N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.649898510487162,56.314781999999994]
["glac_bound",390249.000000000000000,"G228933E57309N","2008-05-01T00:00:00",1162592.360786768374965,1.162590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228933E57309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.068295923501438,57.308609500000003]
["glac_bound",390257.000000000000000,"G227978E57106N","2008-05-01T00:00:00",523087.953089752059896,0.523088000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227978E57106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.023915485374914,57.105665999999999]
["glac_bound",390259.000000000000000,"G227588E58364N","2008-05-01T00:00:00",113202.128529473935487,0.113202000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227588E58364N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.412898693063198,58.364381999999999]
["glac_bound",390262.000000000000000,"G222757E59429N","2008-05-01T00:00:00",755698.282125603873283,0.755698000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222757E59429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.238851045355062,59.431286499999999]
["glac_bound",390265.000000000000000,"G230381E55521N","2008-05-01T00:00:00",122536.240716563857859,0.122536000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230381E55521N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.619469406256599,55.520136999999998]
["glac_bound",390266.000000000000000,"G227904E57935N","2008-05-01T00:00:00",321893.053264266578481,0.321893000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227904E57935N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.094877494354421,57.935471500000006]
["glac_bound",390267.000000000000000,"G225101E59605N","2008-05-01T00:00:00",1165008.057786196703091,1.165010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225101E59605N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.898445923743736,59.604090999999997]
["glac_bound",390269.000000000000000,"G225463E59531N","2008-05-01T00:00:00",2060051.181490037590265,2.060050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225463E59531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.538169629022462,59.531935500000003]
["glac_bound",390273.000000000000000,"G222062E59965N","2008-05-01T00:00:00",1321762.175559354946017,1.321760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222062E59965N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.940170925752795,59.964730000000003]
["glac_bound",390277.000000000000000,"G230261E55694N","2008-05-01T00:00:00",1224273.393831310328096,1.224270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230261E55694N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.733124890514318,55.694292000000004]
["glac_bound",390278.000000000000000,"G230648E55637N","2008-05-01T00:00:00",3639532.000259906984866,3.639530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230648E55637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.347820949461834,55.636364000000000]
["glac_bound",390280.000000000000000,"G226750E58213N","2008-05-01T00:00:00",60294.801324181200471,0.060295000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226750E58213N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.251813225577450,58.214241999999999]
["glac_bound",390296.000000000000000,"G226947E58256N","2008-05-01T00:00:00",336104.993006551696453,0.336105000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226947E58256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.055446252121840,58.254924500000001]
["glac_bound",390298.000000000000000,"G226211E58756N","2008-05-01T00:00:00",574247.295927408384159,0.574247000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226211E58756N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.789836114279581,58.760980500000002]
["glac_bound",390299.000000000000000,"G230349E54632N","2008-05-01T00:00:00",71066.242743984170374,0.071066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230349E54632N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.652120770901632,54.633335000000002]
["glac_bound",390300.000000000000000,"G227191E58419N","2008-05-01T00:00:00",356138.163442786782980,0.356138000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227191E58419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.814099021319294,58.418631500000004]
["glac_bound",390303.000000000000000,"G230216E57458N","2008-05-01T00:00:00",73669.305059519363567,0.073669000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230216E57458N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.783957703980093,57.458681999999996]
["glac_bound",390309.000000000000000,"G225486E59329N","2008-05-01T00:00:00",675793.238371198764071,0.675793000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225486E59329N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.514228464265841,59.329102499999998]
["glac_bound",390312.000000000000000,"G222407E59310N","2008-05-01T00:00:00",407970.966324540670030,0.407971000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222407E59310N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.592162951297297,59.308731000000002]
["glac_bound",390313.000000000000000,"G228742E57409N","2008-05-01T00:00:00",167756.430586030211998,0.167756000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228742E57409N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.258795231445333,57.408767499999996]
["glac_bound",390321.000000000000000,"G230767E57305N","2008-05-01T00:00:00",1939009.733269868418574,1.939010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230767E57305N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.233172985054694,57.308168500000001]
["glac_bound",390322.000000000000000,"G229616E57374N","2008-05-01T00:00:00",219966.649866605817806,0.219967000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229616E57374N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.379646341752959,57.376051000000004]
["glac_bound",390325.000000000000000,"G227823E57298N","2008-05-01T00:00:00",2978571.229317784775048,2.978570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227823E57298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.190607037129126,57.308838000000002]
["glac_bound",390328.000000000000000,"G230427E56388N","2008-05-01T00:00:00",105653.645306897291448,0.105654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230427E56388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.572705613636373,56.388841499999998]
["glac_bound",390334.000000000000000,"G229145E56479N","2008-05-01T00:00:00",1719666.338236038107425,1.719670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229145E56479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.851978504683331,56.480489500000004]
["glac_bound",390338.000000000000000,"G224497E59873N","2008-05-01T00:00:00",143860.149572750349762,0.143860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224497E59873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.503037114963490,59.872440499999996]
["glac_bound",390341.000000000000000,"G225257E59806N","2008-05-01T00:00:00",206116.076585014612647,0.206116000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225257E59806N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.745202097651259,59.805656999999997]
["glac_bound",390344.000000000000000,"G229044E56967N","2008-05-01T00:00:00",14776475.443192889913917,14.776500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229044E56967N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.976369343750008,56.979515000000006]
["glac_bound",390345.000000000000000,"G230700E55240N","2008-05-01T00:00:00",183269.600781810469925,0.183270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230700E55240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.300659024348420,55.239260000000002]
["glac_bound",390349.000000000000000,"G224043E59873N","2008-05-01T00:00:00",3801688.409898368641734,3.801690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224043E59873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.954688407053112,59.872793500000000]
["glac_bound",390360.000000000000000,"G227308E58295N","2008-05-01T00:00:00",860840.876903112977743,0.860841000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227308E58295N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.691380442540463,58.299390500000001]
["glac_bound",390368.000000000000000,"G223291E59259N","2008-05-01T00:00:00",332130.891081974259578,0.332131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223292E59259N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.706025137237759,59.259659999999997]
["glac_bound",390369.000000000000000,"G227794E58050N","2008-05-01T00:00:00",1539758.268462202977389,1.539760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227794E58050N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.204136583815000,58.048895000000002]
["glac_bound",390370.000000000000000,"G228391E56627N","2008-05-01T00:00:00",95761.546654828038299,0.095761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228391E56627N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.608880609478575,56.626763500000003]
["glac_bound",390371.000000000000000,"G227809E57447N","2008-05-01T00:00:00",241424.508232962602051,0.241425000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227809E57447N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.190664761664266,57.446410999999998]
["glac_bound",390372.000000000000000,"G226908E58248N","2008-05-01T00:00:00",2319057.039973808452487,2.319060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226908E58248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.085866321751467,58.251080999999999]
["glac_bound",390377.000000000000000,"G229304E57436N","2008-05-01T00:00:00",772757.418656122288667,0.772757000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE229304E57436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.699245102698967,57.436577000000000]
["glac_bound",390382.000000000000000,"G230503E54655N","2008-05-01T00:00:00",1724463.653423438081518,1.724460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230503E54655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.492853360637014,54.657074000000001]
["glac_bound",390383.000000000000000,"G224966E59596N","2008-05-01T00:00:00",96322.642561922912137,0.096323000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224966E59596N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.033820461504718,59.596370000000000]
["glac_bound",390387.000000000000000,"G227861E57777N","2008-05-01T00:00:00",203113.809945612389129,0.203114000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227861E57777N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.138573512284296,57.776395999999998]
["glac_bound",390394.000000000000000,"G227014E58375N","2008-05-01T00:00:00",228441.312115856067976,0.228441000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227014E58375N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.984937000643498,58.374530000000000]
["glac_bound",390395.000000000000000,"G227784E57753N","2008-05-01T00:00:00",28794617.974521536380053,28.794599999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227784E57753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.209818949808323,57.762411999999998]
["glac_bound",390399.000000000000000,"G227642E57882N","2008-05-01T00:00:00",298612.224830827850383,0.298612000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227642E57882N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.357695852793313,57.883435500000004]
["glac_bound",390405.000000000000000,"G224123E59849N","2008-05-01T00:00:00",139043.005074376123957,0.139043000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224123E59849N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.873613769959263,59.851462499999997]
["glac_bound",390410.000000000000000,"G228272E57258N","2008-05-01T00:00:00",137927.337753347528633,0.137927000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228272E57258N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.727755363518753,57.257869999999997]
["glac_bound",390411.000000000000000,"G230497E55359N","2008-05-01T00:00:00",342831.735329705232289,0.342832000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230497E55359N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.503235387931056,55.359649500000003]
["glac_bound",390418.000000000000000,"G226184E58866N","2008-05-01T00:00:00",287653.533084454596974,0.287654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226184E58866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.819339571566047,58.867830999999995]
["glac_bound",390422.000000000000000,"G231221E57523N","2008-05-01T00:00:00",994945.354149779188447,0.994945000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231221E57523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.779116286363603,57.522457000000003]
["glac_bound",390425.000000000000000,"G227922E58087N","2008-05-01T00:00:00",349805.078847911790945,0.349805000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227922E58087N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.076860101893033,58.090045500000002]
["glac_bound",390427.000000000000000,"G228960E56737N","2008-05-01T00:00:00",75565.049304211643175,0.075565000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228960E56737N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.040590053358073,56.737272500000003]
["glac_bound",390428.000000000000000,"G223835E59986N","2008-05-01T00:00:00",504209.943112657638267,0.504210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223835E59986N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.161240757686414,59.987591500000001]
["glac_bound",390432.000000000000000,"G227282E58153N","2008-05-01T00:00:00",112130.884538045531372,0.112131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227282E58153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.717648910592061,58.153727000000003]
["glac_bound",390436.000000000000000,"G228716E57219N","2008-05-01T00:00:00",162352.716818786808290,0.162353000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228716E57219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.283691512458574,57.218418499999999]
["glac_bound",390442.000000000000000,"G222898E59317N","2008-05-01T00:00:00",501960.600892563757952,0.501961000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222898E59317N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.101389093585681,59.316391999999993]
["glac_bound",390443.000000000000000,"G230336E54884N","2008-05-01T00:00:00",349833.794291663507465,0.349834000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230336E54884N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.664019940964749,54.885712499999997]
["glac_bound",390446.000000000000000,"G226793E58723N","2008-05-01T00:00:00",1860828.888062170008197,1.860830000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226793E58723N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.217823653592546,58.720077000000003]
["glac_bound",390449.000000000000000,"G222398E59887N","2008-05-01T00:00:00",2377327.235190324485302,2.377330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222398E59887N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.619870881437578,59.898027499999998]
["glac_bound",390450.000000000000000,"G229915E57093N","2008-05-01T00:00:00",320915.263245395442937,0.320915000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229915E57093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.080876584810028,57.094636500000000]
["glac_bound",390454.000000000000000,"G225402E59283N","2008-05-01T00:00:00",1840080.741103376261890,1.840080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225402E59283N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.603032054219142,59.287436000000000]
["glac_bound",390463.000000000000000,"G230082E54459N","2008-05-01T00:00:00",1176587.713881792966276,1.176590000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230082E54459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.918046228547666,54.467966000000004]
["glac_bound",390465.000000000000000,"G230099E56954N","2008-05-01T00:00:00",1607668.734275840921327,1.607670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230099E56954N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.903146877141296,56.952809500000001]
["glac_bound",390466.000000000000000,"G225336E59679N","2008-05-01T00:00:00",93503.415850963268895,0.093503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225336E59679N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.664462537966813,59.679017999999999]
["glac_bound",390467.000000000000000,"G228888E57488N","2008-05-01T00:00:00",267271.722575204272289,0.267272000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228888E57488N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.117556327221280,57.489907000000002]
["glac_bound",390471.000000000000000,"G227136E58388N","2008-05-01T00:00:00",78249.091322178632254,0.078249000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227136E58388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.864610292248926,58.388138499999997]
["glac_bound",390472.000000000000000,"G222540E59842N","2008-05-01T00:00:00",2649618.210612277500331,2.649620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222540E59842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.457822366303333,59.841858500000001]
["glac_bound",390477.000000000000000,"G228534E56813N","2008-05-01T00:00:00",14781920.234034027904272,14.781900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228534E56813N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.467206772091345,56.812994500000002]
["glac_bound",390481.000000000000000,"G230213E56611N","2008-05-01T00:00:00",627922.182944901986048,0.627922000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230213E56611N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.781415081555906,56.613345500000001]
["glac_bound",390482.000000000000000,"G229475E56279N","2008-05-01T00:00:00",113670.158810382825322,0.113670000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229475E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.525508486211891,56.278694000000002]
["glac_bound",390488.000000000000000,"G228007E57450N","2008-05-01T00:00:00",477291.893713288358413,0.477292000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228007E57450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.991966037222426,57.449038999999999]
["glac_bound",390490.000000000000000,"G230295E56295N","2008-05-01T00:00:00",80160.939737359352876,0.080161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230295E56295N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.704173598704642,56.296035500000002]
["glac_bound",390491.000000000000000,"G230290E56025N","2008-05-01T00:00:00",83891.754502703974140,0.083892000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230290E56025N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.709676784511259,56.025097500000001]
["glac_bound",390492.000000000000000,"G228865E57040N","2008-05-01T00:00:00",173796.722052214056021,0.173797000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228865E57040N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.133261553145928,57.042338500000000]
["glac_bound",390497.000000000000000,"G230558E55228N","2008-05-01T00:00:00",214447.517803196329623,0.214448000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230558E55228N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.441324624086377,55.227380499999995]
["glac_bound",390499.000000000000000,"G227864E58013N","2008-05-01T00:00:00",563102.525849279481918,0.563103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227864E58013N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.139390486011280,58.014565500000003]
["glac_bound",390500.000000000000000,"G230483E58227N","2008-05-01T00:00:00",140704.338292560540140,0.140704000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB230483E58227N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.517383758257836,58.226843500000001]
["glac_bound",390503.000000000000000,"G226853E58548N","2008-05-01T00:00:00",303144.751481099578086,0.303145000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226853E58548N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.144256992700718,58.546453000000000]
["glac_bound",390505.000000000000000,"G222713E59455N","2008-05-01T00:00:00",91543.790885534326662,0.091544000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222713E59455N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.288966649122813,59.457391999999999]
["glac_bound",390506.000000000000000,"G230152E57003N","2008-05-01T00:00:00",5511857.236853770911694,5.511860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230152E57003N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.858445417896377,57.000626499999996]
["glac_bound",390510.000000000000000,"G229886E56279N","2008-05-01T00:00:00",2580610.581970750819892,2.580610000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229886E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.117919911458330,56.280257500000005]
["glac_bound",390511.000000000000000,"G230327E56994N","2008-05-01T00:00:00",102301.265878853111644,0.102301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230327E56994N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.672631791400818,56.993042500000001]
["glac_bound",390512.000000000000000,"G225619E59210N","2008-05-01T00:00:00",322699.821915336768143,0.322700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225619E59210N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.379793433953552,59.212829499999998]
["glac_bound",390518.000000000000000,"G230759E56704N","2008-05-01T00:00:00",291055.434200549090747,0.291055000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230759E56704N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.240612107271090,56.703096500000001]
["glac_bound",390519.000000000000000,"G228580E57044N","2008-05-01T00:00:00",127287.933880843251245,0.127288000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228580E57044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.418531985955241,57.045140000000004]
["glac_bound",390522.000000000000000,"G227427E58423N","2008-05-01T00:00:00",241488.362427877873415,0.241488000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227427E58423N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.573449999999980,58.423407999999995]
["glac_bound",390526.000000000000000,"G224070E59676N","2008-05-01T00:00:00",1919735.613767074653879,1.919740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224070E59676N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.930995836454088,59.680531000000002]
["glac_bound",390527.000000000000000,"G230979E56485N","2008-05-01T00:00:00",218914.739488148101373,0.218915000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230979E56485N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.018977305903519,56.484893999999997]
["glac_bound",390532.000000000000000,"G227272E58093N","2008-05-01T00:00:00",240288.888061338686384,0.240289000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227272E58093N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.728625496163090,58.093343000000004]
["glac_bound",390535.000000000000000,"G224452E59942N","2008-05-01T00:00:00",1069369.553503120085225,1.069370000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224452E59942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.549286737570014,59.944243499999999]
["glac_bound",390536.000000000000000,"G225967E59237N","2008-05-01T00:00:00",121085.178713017623522,0.121085000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225967E59237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.033627642225781,59.237633500000001]
["glac_bound",390537.000000000000000,"G228577E57101N","2008-05-01T00:00:00",110192.210919314195053,0.110192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228577E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.422625849760607,57.101379500000000]
["glac_bound",390539.000000000000000,"G232895E57762N","2008-05-01T00:00:00",94130.634873676433926,0.094131000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08CA232895E57762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-127.105363867903918,57.761889499999995]
["glac_bound",390550.000000000000000,"G226643E58491N","2008-05-01T00:00:00",1150504.337996287737042,1.150500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226643E58491N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.354944240322595,58.492506500000005]
["glac_bound",390551.000000000000000,"G230303E55642N","2008-05-01T00:00:00",144003.536203576280968,0.144004000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230303E55642N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.698322464023107,55.642375000000001]
["glac_bound",390552.000000000000000,"G226960E58008N","2008-05-01T00:00:00",97860.681919948678114,0.097861000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226960E58008N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.041766170113419,58.007021000000002]
["glac_bound",390553.000000000000000,"G224080E59717N","2008-05-01T00:00:00",116771.302446589368628,0.116771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224080E59717N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.919765669208289,59.717165000000001]
["glac_bound",390554.000000000000000,"G229028E56654N","2008-05-01T00:00:00",73862.704328842562973,0.073863000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229028E56654N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.971563058150991,56.653960499999997]
["glac_bound",390555.000000000000000,"G228560E57299N","2008-05-01T00:00:00",834404.977587099303491,0.834405000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228560E57299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.442961620225560,57.299351500000000]
["glac_bound",390556.000000000000000,"G227076E58394N","2008-05-01T00:00:00",9204537.709741787984967,9.204540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227076E58394N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.914650432264068,58.394041999999999]
["glac_bound",390558.000000000000000,"G229382E56573N","2008-05-01T00:00:00",1830750.307825478725135,1.830750000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229382E56573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.615809873814840,56.575136000000001]
["glac_bound",390559.000000000000000,"G225357E59306N","2008-05-01T00:00:00",303214.127160475240089,0.303214000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225357E59306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.642192536475761,59.304324500000000]
["glac_bound",390560.000000000000000,"G230451E55203N","2008-05-01T00:00:00",70150.657579917504336,0.070151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230451E55203N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.549189603571421,55.203395499999999]
["glac_bound",390563.000000000000000,"G229315E56527N","2008-05-01T00:00:00",910195.651929129729979,0.910196000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229315E56527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.684892932489902,56.527484000000001]
["glac_bound",390575.000000000000000,"G228815E57466N","2008-05-01T00:00:00",126163.100812762946589,0.126163000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228815E57466N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.185153463167268,57.466272500000002]
["glac_bound",390579.000000000000000,"G226537E58494N","2008-05-01T00:00:00",2181638.392727632075548,2.181640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226537E58494N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.465299096882632,58.494619999999998]
["glac_bound",390582.000000000000000,"G222718E59036N","2008-05-01T00:00:00",1379415.753545650979504,1.379420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222713E59035N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.286457576882981,59.035103499999998]
["glac_bound",390589.000000000000000,"G229136E56444N","2008-05-01T00:00:00",142398.700033913046354,0.142399000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229136E56444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.863287094284999,56.443571499999997]
["glac_bound",390591.000000000000000,"G223607E59679N","2008-05-01T00:00:00",154746.161276679864386,0.154746000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223607E59679N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.390467254589737,59.678057499999994]
["glac_bound",390596.000000000000000,"G222270E59866N","2008-05-01T00:00:00",479768.293082842254080,0.479768000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222270E59866N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.729189135471017,59.867379000000000]
["glac_bound",390597.000000000000000,"G230490E55945N","2008-05-01T00:00:00",1666712.003316310234368,1.666710000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230490E55945N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.502184303562956,55.948929000000007]
["glac_bound",390600.000000000000000,"G226254E58776N","2008-05-01T00:00:00",103145.181519585050410,0.103145000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226254E58776N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.746468749763807,58.774241500000002]
["glac_bound",390609.000000000000000,"G226808E58219N","2008-05-01T00:00:00",119536.155813382065389,0.119536000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226808E58219N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.189692611883146,58.220532500000004]
["glac_bound",390610.000000000000000,"G226768E58730N","2008-05-01T00:00:00",1621484.930067191598937,1.621480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226768E58730N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.233328230826658,58.729719000000003]
["glac_bound",390611.000000000000000,"G230439E54692N","2008-05-01T00:00:00",458030.095484840101562,0.458030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230439E54692N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.559676146849597,54.693439999999995]
["glac_bound",390614.000000000000000,"G230957E54936N","2008-05-01T00:00:00",97714.494978545233607,0.097714000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230957E54936N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.042748510013666,54.935535999999999]
["glac_bound",390619.000000000000000,"G228883E57241N","2008-05-01T00:00:00",6307493.895280012860894,6.307490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228883E57241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.109295397082462,57.248214000000004]
["glac_bound",390622.000000000000000,"G230698E55598N","2008-05-01T00:00:00",72299.850474837585352,0.072300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230698E55598N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.302530570110719,55.598545500000000]
["glac_bound",390624.000000000000000,"G225105E59908N","2008-05-01T00:00:00",316959.241632714518346,0.316959000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225105E59908N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.896115026386525,59.907766000000002]
["glac_bound",390625.000000000000000,"G230586E55206N","2008-05-01T00:00:00",4457000.052532560192049,4.457000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230586E55206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.417462529889747,55.214623500000002]
["glac_bound",390626.000000000000000,"G224305E59752N","2008-05-01T00:00:00",1635355.118161999154836,1.635360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224305E59752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.692276815154884,59.750852999999999]
["glac_bound",390632.000000000000000,"G223353E59480N","2008-05-01T00:00:00",312571.574023083550856,0.312572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223353E59480N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.646061240820558,59.478822000000001]
["glac_bound",390633.000000000000000,"G229937E56411N","2008-05-01T00:00:00",317805.902638530824333,0.317806000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229937E56411N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.069846996298168,56.411877000000004]
["glac_bound",390635.000000000000000,"G227522E58195N","2008-05-01T00:00:00",455480.257490389281884,0.455480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227522E58195N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.479776385420053,58.195037999999997]
["glac_bound",390637.000000000000000,"G229442E56873N","2008-05-01T00:00:00",608040.653086423058994,0.608041000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229442E56873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.558964201249978,56.873891999999998]
["glac_bound",390641.000000000000000,"G229536E56735N","2008-05-01T00:00:00",155297.083621744473930,0.155297000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229536E56735N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.463289438543512,56.737581000000006]
["glac_bound",390642.000000000000000,"G223739E59977N","2008-05-01T00:00:00",169550.661507550161332,0.169551000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223739E59977N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.260820844909745,59.976926000000006]
["glac_bound",390644.000000000000000,"G227983E56895N","2008-05-01T00:00:00",145170368.20568051934242,145.169999999999987,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Great Glacier","CA2N001FA186","08CF227983E56895N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.058002285817309,56.916981000000000]
["glac_bound",390645.000000000000000,"G221736E59802N","2008-05-01T00:00:00",1028760.002907300135121,1.028760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221736E59802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.270389864414028,59.805418500000002]
["glac_bound",390651.000000000000000,"G230353E56254N","2008-05-01T00:00:00",738952.047873325180262,0.738952000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230353E56254N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.648660503378522,56.254154499999999]
["glac_bound",390654.000000000000000,"G228024E57807N","2008-05-01T00:00:00",5118463.827511780895293,5.118460000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228024E57807N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.988408544957252,57.801381500000005]
["glac_bound",390655.000000000000000,"G225049E59275N","2008-05-01T00:00:00",10190.683921110881784,0.010191000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225049E59275N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.951175286775111,59.275655499999999]
["glac_bound",390656.000000000000000,"G230373E55622N","2008-05-01T00:00:00",272877.655490406032186,0.272878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230373E55622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.633885700810907,55.622183499999998]
["glac_bound",390658.000000000000000,"G225210E59410N","2008-05-01T00:00:00",118625.738189595882432,0.118626000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225210E59410N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.791081359485702,59.410680999999997]
["glac_bound",390659.000000000000000,"G229410E56326N","2008-05-01T00:00:00",1066683.142017709091306,1.066680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229410E56326N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.590719318941694,56.323880500000001]
["glac_bound",390661.000000000000000,"G230816E55339N","2008-05-01T00:00:00",64342.716464132361580,0.064343000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230816E55339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.184634722975829,55.338476999999997]
["glac_bound",390667.000000000000000,"G230130E56243N","2008-05-01T00:00:00",659873.267397927935235,0.659873000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230130E56243N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.862737425516286,56.241911999999999]
["glac_bound",390670.000000000000000,"G226339E58855N","2008-05-01T00:00:00",12285188.035732807591558,12.285200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226339E58855N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.663784039065007,58.848900499999999]
["glac_bound",390673.000000000000000,"G230567E54698N","2008-05-01T00:00:00",387711.302895480766892,0.387711000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230567E54698N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.432418513206784,54.697792000000000]
["glac_bound",390674.000000000000000,"G223285E59697N","2008-05-01T00:00:00",847373.903430075151846,0.847374000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223285E59697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.716864228168845,59.697423499999999]
["glac_bound",390676.000000000000000,"G227227E58473N","2008-05-01T00:00:00",201518.888509159383830,0.201519000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227227E58473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.772869298217188,58.473374500000006]
["glac_bound",390677.000000000000000,"G229397E56577N","2008-05-01T00:00:00",329224.827176735212561,0.329225000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229397E56577N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.603348521899534,56.577410000000000]
["glac_bound",390684.000000000000000,"G225191E59634N","2008-05-01T00:00:00",1483410.710682497359812,1.483410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225191E59634N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.808570475530672,59.633678500000002]
["glac_bound",390693.000000000000000,"G229310E56968N","2008-05-01T00:00:00",309214.289826074673329,0.309214000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229310E56968N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.690386196121949,56.967915500000004]
["glac_bound",390695.000000000000000,"G227106E58107N","2008-05-01T00:00:00",1917852.520842584548518,1.917850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227106E58107N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.905985384826863,58.111595500000000]
["glac_bound",390698.000000000000000,"G223562E59833N","2008-05-01T00:00:00",90507.641626274562441,0.805600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223562E59833N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.432826640961537,59.832611999999997]
["glac_bound",390698.000000000000000,"G223562E59833N","2008-05-01T00:00:00",715092.236839191522449,0.805600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223562E59833N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.439334110551670,59.837225500000002]
["glac_bound",390699.000000000000000,"G229553E56321N","2008-05-01T00:00:00",51696.947506027747295,0.051697000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229553E56321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.446743255405408,56.322060000000000]
["glac_bound",390700.000000000000000,"G223716E59775N","2008-05-01T00:00:00",776571.792935845325701,0.776572000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223716E59775N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.280134771507875,59.774857999999995]
["glac_bound",390705.000000000000000,"G230557E57145N","2008-05-01T00:00:00",86864.229614276424400,0.086864000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230557E57145N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.443539981523600,57.145038999999997]
["glac_bound",390706.000000000000000,"G227467E58183N","2008-05-01T00:00:00",562671.582343290909193,0.562672000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227467E58183N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.530878051525121,58.182550499999998]
["glac_bound",390708.000000000000000,"G231121E55269N","2008-05-01T00:00:00",89771.037333697633585,0.089771000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231121E55269N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.878321790365760,55.270249000000000]
["glac_bound",390709.000000000000000,"G229253E57048N","2008-05-01T00:00:00",270907.546735956682824,0.270908000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229253E57048N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.746211369473286,57.047547500000000]
["glac_bound",390710.000000000000000,"G228906E57388N","2008-05-01T00:00:00",193901.104626299144002,0.193901000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228906E57388N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.093272181243719,57.389113500000001]
["glac_bound",390714.000000000000000,"G227417E57765N","2008-05-01T00:00:00",52660649.534449949860573,52.660600000000002,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-11T00:00:00","okay","None","None","08CE227417E57765N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.642761018543240,57.770067999999995]
["glac_bound",390717.000000000000000,"G222572E59697N","2008-05-01T00:00:00",778979.183041477110237,0.778979000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222572E59697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.426989932851228,59.696634000000003]
["glac_bound",390721.000000000000000,"G228901E57682N","2008-05-01T00:00:00",450864.678388846630696,0.450865000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228901E57682N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.099887711959695,57.681773000000000]
["glac_bound",390729.000000000000000,"G222829E59339N","2008-05-01T00:00:00",5565109.650646775960922,5.565110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222829E59339N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.174964479754465,59.334198000000001]
["glac_bound",390733.000000000000000,"G229257E56856N","2008-05-01T00:00:00",3058551.783445253036916,3.058550000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229257E56856N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.750678228577385,56.862241500000003]
["glac_bound",390735.000000000000000,"G228820E56500N","2008-05-01T00:00:00",218878.466441506141564,0.218878000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228820E56500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.184246691220238,56.500796500000000]
["glac_bound",390736.000000000000000,"G226644E58615N","2008-05-01T00:00:00",568035.888481785426848,0.568036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226644E58615N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.357841297169784,58.620594499999996]
["glac_bound",390738.000000000000000,"G227633E58241N","2008-05-01T00:00:00",4877973.258958630263805,4.877970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227633E58241N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.382604716213251,58.241038500000002]
["glac_bound",390743.000000000000000,"G229281E56779N","2008-05-01T00:00:00",74646.450085882825078,0.074647000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229281E56779N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.719975328078078,56.778913000000003]
["glac_bound",390745.000000000000000,"G227174E58465N","2008-05-01T00:00:00",303667.861766987829469,0.303668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227174E58465N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.825043995654767,58.465951500000003]
["glac_bound",390748.000000000000000,"G229467E57461N","2008-05-01T00:00:00",70297.968573516714969,0.070298000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229467E57461N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.533314689028543,57.461477500000001]
["glac_bound",390749.000000000000000,"G224031E59978N","2008-05-01T00:00:00",146968.328701542748604,0.146968000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224031E59978N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.969253253094450,59.978312500000001]
["glac_bound",390751.000000000000000,"G230503E55006N","2008-05-01T00:00:00",69341.630455888051074,0.069342000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230503E55006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.497204753268988,55.006406999999996]
["glac_bound",390752.000000000000000,"G226634E58630N","2008-05-01T00:00:00",1196292.091696307295933,1.196290000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226634E58630N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.365799798898706,58.631410500000001]
["glac_bound",390765.000000000000000,"G225614E59459N","2008-05-01T00:00:00",50421.299908207831322,0.050421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225614E59459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.385811857750411,59.458675999999997]
["glac_bound",390768.000000000000000,"G230051E56163N","2008-05-01T00:00:00",89005.488915865789750,0.089006000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230051E56163N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.952434088353414,56.162928000000001]
["glac_bound",390769.000000000000000,"G228845E56472N","2008-05-01T00:00:00",1305206.610237195156515,1.305210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228845E56472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.160154834072756,56.473042000000000]
["glac_bound",390773.000000000000000,"G230292E56153N","2008-05-01T00:00:00",19464556.347474351525307,19.464600000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230292E56153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.702830886692425,56.153041000000002]
["glac_bound",390776.000000000000000,"G224477E59891N","2008-05-01T00:00:00",235802.240616995666642,0.235802000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224477E59891N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.528630103618752,59.891028000000006]
["glac_bound",390778.000000000000000,"G227144E58237N","2008-05-01T00:00:00",281098.650043532892596,0.281099000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227144E58237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.855951993626491,58.236373499999999]
["glac_bound",390779.000000000000000,"G225340E59132N","2008-05-01T00:00:00",434374246.23968946933746,434.374000000000024,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Meade Glacier","None","08BD225340E59132N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.793611548841739,59.266989000000002]
["glac_bound",390780.000000000000000,"G230423E55612N","2008-05-01T00:00:00",730270.395038877963088,0.730270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230423E55612N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.566272293747431,55.606437999999997]
["glac_bound",390786.000000000000000,"G226308E58942N","2008-05-01T00:00:00",268575.889041570597328,0.268576000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226308E58942N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.693729395407985,58.942172999999997]
["glac_bound",390787.000000000000000,"G229311E56519N","2008-05-01T00:00:00",716455.650025157025084,0.716456000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229311E56519N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.689768029946634,56.516500000000001]
["glac_bound",390790.000000000000000,"G229878E57092N","2008-05-01T00:00:00",547461.575014031375758,0.547462000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229878E57092N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.120307826401472,57.096452999999997]
["glac_bound",390793.000000000000000,"G227525E57688N","2008-05-01T00:00:00",1532866.694105569738895,1.532870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227525E57688N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.470640392650239,57.691418999999996]
["glac_bound",390794.000000000000000,"G226707E58715N","2008-05-01T00:00:00",247841.340207071392797,0.247841000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226707E58715N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.293965918247693,58.717235000000002]
["glac_bound",390798.000000000000000,"G230163E56244N","2008-05-01T00:00:00",5091581.702954248525202,5.091580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230163E56244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.837752371565841,56.250253499999999]
["glac_bound",390799.000000000000000,"G229392E57740N","2008-05-01T00:00:00",246471.868932653364027,0.246472000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229392E57740N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.608482245067080,57.740223499999999]
["glac_bound",390804.000000000000000,"G229885E57128N","2008-05-01T00:00:00",65795.465092283600825,0.065796000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229885E57128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.114895508972324,57.128152999999998]
["glac_bound",390805.000000000000000,"G224686E59872N","2008-05-01T00:00:00",187089.438170205015922,0.187089000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224686E59872N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.314816597086974,59.871293500000000]
["glac_bound",390809.000000000000000,"G230136E55790N","2008-05-01T00:00:00",543335.668937915004790,0.543336000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230136E55790N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.869970340018881,55.793700500000000]
["glac_bound",390810.000000000000000,"G229104E56564N","2008-05-01T00:00:00",1339539.769253146136180,1.339540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229104E56564N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.896123682874702,56.565691500000000]
["glac_bound",390812.000000000000000,"G228842E57321N","2008-05-01T00:00:00",597371.686533990083262,0.597372000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228842E57321N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.157845848461250,57.321124999999995]
["glac_bound",390814.000000000000000,"G226901E58119N","2008-05-01T00:00:00",121049.803901673425571,0.121050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226901E58119N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.099140467021272,58.119228500000006]
["glac_bound",390818.000000000000000,"G228983E56619N","2008-05-01T00:00:00",643126.118106009555049,0.643126000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228983E56619N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.020820834778419,56.622250000000001]
["glac_bound",390823.000000000000000,"G230106E55821N","2008-05-01T00:00:00",628709.333743384107947,0.628709000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230106E55821N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.889639706760335,55.819621499999997]
["glac_bound",390824.000000000000000,"G230103E56669N","2008-05-01T00:00:00",767375.635489950538613,0.767376000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230103E56669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.901759713828113,56.671531500000000]
["glac_bound",390825.000000000000000,"G227517E57995N","2008-05-01T00:00:00",754592.926267876289785,0.754593000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227517E57995N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.483315873256913,57.995478500000004]
["glac_bound",390827.000000000000000,"G230512E56738N","2008-05-01T00:00:00",272431.034466472803615,0.272431000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230512E56738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.485820288883872,56.737785000000002]
["glac_bound",390831.000000000000000,"G224562E59919N","2008-05-01T00:00:00",462261.943322517909110,0.462262000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224562E59919N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.437696196620891,59.918885000000003]
["glac_bound",390832.000000000000000,"G228900E57678N","2008-05-01T00:00:00",55736.951488950609928,0.055737000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228900E57678N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.099571686517947,57.677889999999998]
["glac_bound",390837.000000000000000,"G225456E59248N","2008-05-01T00:00:00",1010931.944784586434253,1.010930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225456E59248N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.547177631917634,59.245753499999999]
["glac_bound",390841.000000000000000,"G229904E57794N","2008-05-01T00:00:00",399707.444168383313809,0.399707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229904E57794N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.094698377309726,57.792408999999999]
["glac_bound",390842.000000000000000,"G225532E59387N","2008-05-01T00:00:00",52701.295588392851641,0.052701000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225532E59387N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.468049670793505,59.387382500000001]
["glac_bound",390845.000000000000000,"G231507E56142N","2008-05-01T00:00:00",634036.440467965439893,0.634036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231507E56142N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.492963330660018,56.141735499999996]
["glac_bound",390854.000000000000000,"G224559E59841N","2008-05-01T00:00:00",1368432.302663710201159,1.368430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224559E59841N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.439676311488654,59.841525000000004]
["glac_bound",390864.000000000000000,"G227709E57580N","2008-05-01T00:00:00",155093.623408417304745,0.155094000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227709E57580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.291234923130219,57.580309999999997]
["glac_bound",390865.000000000000000,"G227945E57312N","2008-05-01T00:00:00",522391.712425962497946,0.522392000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227945E57312N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.061050310686142,57.311368500000000]
["glac_bound",390866.000000000000000,"G230056E56099N","2008-05-01T00:00:00",305248.127825040777680,0.305248000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230056E56099N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.945839599551789,56.098740500000005]
["glac_bound",390868.000000000000000,"G228936E56749N","2008-05-01T00:00:00",690646.527670287410729,0.690647000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228936E56749N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.059448203101567,56.753210500000002]
["glac_bound",390870.000000000000000,"G225569E59185N","2008-05-01T00:00:00",221333.797395326226251,0.221334000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225569E59185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.433426963116091,59.183118000000000]
["glac_bound",390876.000000000000000,"G229408E56650N","2008-05-01T00:00:00",2118946.712493676226586,2.118950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229408E56650N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.595411893244375,56.650202000000000]
["glac_bound",390880.000000000000000,"G224999E59612N","2008-05-01T00:00:00",548187.400276147178374,0.548187000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224999E59612N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.998980079161356,59.611882500000000]
["glac_bound",390885.000000000000000,"G225393E59303N","2008-05-01T00:00:00",2124176.157712543383241,2.124180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225393E59303N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.609567708231452,59.303320999999997]
["glac_bound",390890.000000000000000,"G225133E59587N","2008-05-01T00:00:00",317323.523302201821934,0.317324000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225133E59587N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.869380781926338,59.586557499999998]
["glac_bound",390892.000000000000000,"G223522E59711N","2008-05-01T00:00:00",843970.321134714060463,0.843970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223522E59711N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.479540283762788,59.711033999999998]
["glac_bound",390896.000000000000000,"G229544E57118N","2008-05-01T00:00:00",280285.083176530897617,0.280285000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229544E57118N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.453174860528549,57.116486999999999]
["glac_bound",390897.000000000000000,"G225588E59244N","2008-05-01T00:00:00",242168.285324499011040,0.242168000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225588E59244N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.412321707117286,59.244162000000003]
["glac_bound",390898.000000000000000,"G230397E55622N","2008-05-01T00:00:00",1164964.631182312499732,1.164960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230397E55622N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.605586761310491,55.619745999999999]
["glac_bound",390899.000000000000000,"G226886E58440N","2008-05-01T00:00:00",395604.967508327914402,0.395605000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226886E58440N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.116423771739107,58.441175000000001]
["glac_bound",390905.000000000000000,"G226917E58111N","2008-05-01T00:00:00",1929855.510666100541130,1.929860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226917E58111N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.082458828728647,58.112388500000002]
["glac_bound",390908.000000000000000,"G228540E56791N","2008-05-01T00:00:00",151885.821973684651311,0.151886000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228540E56791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.459395487579144,56.794951999999995]
["glac_bound",390912.000000000000000,"G222553E59617N","2008-05-01T00:00:00",393868.189782988862135,0.393868000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222553E59617N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.445665111311399,59.617874000000000]
["glac_bound",390915.000000000000000,"G229984E57165N","2008-05-01T00:00:00",2920650.873486750293523,2.920650000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229984E57165N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.015822101675099,57.164984500000003]
["glac_bound",390916.000000000000000,"G228985E56406N","2008-05-01T00:00:00",269704.040691076079383,0.269704000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD228985E56406N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.012043362204707,56.404609000000001]
["glac_bound",390919.000000000000000,"G230584E57153N","2008-05-01T00:00:00",313699.301136449561454,0.313699000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230584E57153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.415004427966096,57.152174000000002]
["glac_bound",390920.000000000000000,"G228371E56669N","2008-05-01T00:00:00",230140.668473963043652,0.230141000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228371E56669N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.630013123860920,56.669498000000004]
["glac_bound",390922.000000000000000,"G225467E59435N","2008-05-01T00:00:00",2193363.874413604382426,2.193360000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225467E59435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.522280896640979,59.440370500000000]
["glac_bound",390924.000000000000000,"G222405E59507N","2008-05-01T00:00:00",526292.002343430416659,0.526292000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222405E59507N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.600953705819279,59.507095500000005]
["glac_bound",390929.000000000000000,"G222735E59040N","2008-05-01T00:00:00",484451.837651807873044,0.484452000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222735E59040N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.265139042135445,59.040275000000001]
["glac_bound",390930.000000000000000,"G222607E59218N","2008-05-01T00:00:00",190701.126698485022644,0.190701000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222607E59218N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.394353950980417,59.219549000000001]
["glac_bound",390933.000000000000000,"G225629E59451N","2008-05-01T00:00:00",160009.886306623462588,0.160010000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225629E59451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.367771875190897,59.450885499999998]
["glac_bound",390937.000000000000000,"G231855E58382N","2008-05-01T00:00:00",152301.405262192740338,0.152301000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-15T00:00:00","okay","None","None","08CA231855E58382N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.146493350657352,58.381806499999996]
["glac_bound",390938.000000000000000,"G230284E55969N","2008-05-01T00:00:00",90203.324614115364966,0.090203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230284E55969N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.715137251159518,55.969172999999998]
["glac_bound",390939.000000000000000,"G222288E59384N","2008-05-01T00:00:00",389735.666972142527811,0.389736000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222288E59384N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.717305885344160,59.387230000000002]
["glac_bound",390941.000000000000000,"G227709E57879N","2008-05-01T00:00:00",5707089.133661821484566,5.707090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227709E57879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.302689653397323,57.879487499999996]
["glac_bound",390950.000000000000000,"G229979E55687N","2008-05-01T00:00:00",952203.995718485442922,0.952204000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC229979E55687N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.021113798252088,55.688608000000002]
["glac_bound",390955.000000000000000,"G230592E57159N","2008-05-01T00:00:00",176202.853084669652162,0.176203000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230592E57159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.408404083023072,57.159841999999998]
["glac_bound",390957.000000000000000,"G225830E59220N","2008-05-01T00:00:00",459795.110685220861342,0.459795000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225830E59220N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.169518265581644,59.219936000000004]
["glac_bound",390959.000000000000000,"G230714E55609N","2008-05-01T00:00:00",491501.256023056281265,0.491501000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230714E55609N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.285395623598845,55.608983500000001]
["glac_bound",390963.000000000000000,"G222504E59860N","2008-05-01T00:00:00",715347.171400982188061,0.715347000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222504E59860N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.496972680590318,59.860916500000002]
["glac_bound",390965.000000000000000,"G230733E56747N","2008-05-01T00:00:00",301102.685771439515520,0.301103000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230733E56747N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.265376147022323,56.748232500000000]
["glac_bound",390969.000000000000000,"G228055E57525N","2008-05-01T00:00:00",3385270.526534656528383,3.385270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228055E57525N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.946999063386841,57.522067000000000]
["glac_bound",390973.000000000000000,"G224374E59858N","2008-05-01T00:00:00",398999.980645550356712,0.399000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224374E59858N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.627025666896316,59.857411499999998]
["glac_bound",390975.000000000000000,"G230152E57365N","2008-05-01T00:00:00",312142.717973891471047,0.312143000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230152E57365N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.853645321423812,57.365467500000001]
["glac_bound",390976.000000000000000,"G223127E59659N","2008-05-01T00:00:00",908042.380194791476242,0.908042000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223127E59659N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.875803130039770,59.662022499999999]
["glac_bound",390977.000000000000000,"G224221E59908N","2008-05-01T00:00:00",50542.125570499993046,0.050542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224221E59908N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.778834785924943,59.907668999999999]
["glac_bound",390978.000000000000000,"G223243E59125N","2008-05-01T00:00:00",81691.551178220979637,0.081692000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Carroll Glacier","None","08BF223255E59211N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.745567655172408,59.211081000000000]
["glac_bound",390983.000000000000000,"G230362E55156N","2008-05-01T00:00:00",52183.710640399214753,0.052184000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230362E55156N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.638402915399240,55.157145000000000]
["glac_bound",390992.000000000000000,"G225770E59172N","2008-05-01T00:00:00",1857262.769085987238213,1.857260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225770E59172N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.223849116076252,59.175569500000002]
["glac_bound",390995.000000000000000,"G225609E59249N","2008-05-01T00:00:00",2660141.854437496513128,2.660140000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225609E59249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.388362238990368,59.247473999999997]
["glac_bound",391002.000000000000000,"G227639E58150N","2008-05-01T00:00:00",1752509.661953231086954,1.752510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227639E58150N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.361204709520621,58.150629500000001]
["glac_bound",391005.000000000000000,"G225534E59467N","2008-05-01T00:00:00",527060.658595721586607,0.527061000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225534E59467N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.465960525320753,59.466970000000003]
["glac_bound",391007.000000000000000,"G228962E56463N","2008-05-01T00:00:00",630559.758871161844581,0.630560000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228962E56463N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.038769994626421,56.466370999999995]
["glac_bound",391009.000000000000000,"G227469E58237N","2008-05-01T00:00:00",368223.364767112187110,0.368223000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227469E58237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.529489024258908,58.238763000000006]
["glac_bound",391011.000000000000000,"G230208E57038N","2008-05-01T00:00:00",2627883.762322364840657,2.627880000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230208E57038N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.792405722414031,57.038398500000000]
["glac_bound",391013.000000000000000,"G228027E57372N","2008-05-01T00:00:00",106706.144779302470852,0.106706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228027E57372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.976732975781545,57.370159000000001]
["glac_bound",391014.000000000000000,"G231111E55209N","2008-05-01T00:00:00",259780.204742798960069,0.259780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB231111E55209N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.884820044653281,55.210013500000002]
["glac_bound",391017.000000000000000,"G225648E59358N","2008-05-01T00:00:00",572312.417262292234227,0.572312000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225648E59358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.351674236940283,59.358172499999995]
["glac_bound",391020.000000000000000,"G230182E57477N","2008-05-01T00:00:00",326182.388288628368173,0.326182000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230182E57477N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.816532054438284,57.476691000000002]
["glac_bound",391023.000000000000000,"G228313E57376N","2008-05-01T00:00:00",318234.416527575172950,0.318234000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228313E57376N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.686846117161281,57.375444000000002]
["glac_bound",391028.000000000000000,"G222480E59300N","2008-05-01T00:00:00",434317.596397705725394,0.434318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222480E59300N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.521052258581562,59.299857500000002]
["glac_bound",391029.000000000000000,"G228757E57106N","2008-05-01T00:00:00",6004903.544523665681481,6.004900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228757E57106N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.231335269682262,57.123432500000000]
["glac_bound",391032.000000000000000,"G227469E57864N","2008-05-01T00:00:00",690149.858546508126892,0.690150000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227469E57864N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.530811560650989,57.863072000000003]
["glac_bound",391033.000000000000000,"G226312E58732N","2008-05-01T00:00:00",871625.366906271432526,0.871625000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226312E58732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.688294067073173,58.730509999999995]
["glac_bound",391034.000000000000000,"G223041E59101N","2008-05-01T00:00:00",518270.147534185147379,0.518270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223041E59101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.960779867088604,59.102523500000004]
["glac_bound",391036.000000000000000,"G227732E57937N","2008-05-01T00:00:00",2217636.665589283686131,2.217640000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227732E57937N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.272128888408872,57.937704500000002]
["glac_bound",391037.000000000000000,"G229588E57111N","2008-05-01T00:00:00",162066.126504752552137,0.162066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229588E57111N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.410957084507032,57.110899000000003]
["glac_bound",391038.000000000000000,"G228547E57306N","2008-05-01T00:00:00",21001086.916375879198313,21.001100000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228547E57306N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.442181451516774,57.332199000000003]
["glac_bound",391040.000000000000000,"G225340E59441N","2008-05-01T00:00:00",705337.297247093520127,0.705337000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225340E59441N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.661685159484364,59.442399999999999]
["glac_bound",391046.000000000000000,"G221908E59897N","2008-05-01T00:00:00",1683992.569174303207546,1.683990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221908E59897N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.096459743865012,59.898299999999999]
["glac_bound",391052.000000000000000,"G221722E59729N","2008-05-01T00:00:00",893346.510489330277778,0.893346000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221722E59729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.282888955345072,59.732066000000003]
["glac_bound",391054.000000000000000,"G222830E59355N","2008-05-01T00:00:00",236846.363638954702765,0.236846000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222830E59355N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.171549782813031,59.354766999999995]
["glac_bound",391055.000000000000000,"G228001E57040N","2008-05-01T00:00:00",10173319.872569354251027,10.173299999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228001E57040N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.005682558416083,57.057271999999998]
["glac_bound",391064.000000000000000,"G229343E56664N","2008-05-01T00:00:00",211160.748766462289495,0.211161000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229343E56664N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.657092589951475,56.664128499999997]
["glac_bound",391065.000000000000000,"G224438E59961N","2008-05-01T00:00:00",76981.152042512054322,0.076981000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224438E59961N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.562440945346651,59.961846000000001]
["glac_bound",391066.000000000000000,"G223648E59604N","2008-05-01T00:00:00",157401.843275194434682,0.157402000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223648E59604N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.351855544340708,59.604469000000002]
["glac_bound",391067.000000000000000,"G230462E56044N","2008-05-01T00:00:00",141319.480073451268254,0.141319000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230462E56044N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.537208133470330,56.044402000000005]
["glac_bound",391069.000000000000000,"G227990E57999N","2008-05-01T00:00:00",855361.982328351936303,0.855362000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227990E57999N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.008074027154635,58.001640500000001]
["glac_bound",391071.000000000000000,"G227132E58240N","2008-05-01T00:00:00",500579.368522353994194,0.500579000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227132E58240N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.865785685833004,58.240019500000002]
["glac_bound",391073.000000000000000,"G230458E56653N","2008-05-01T00:00:00",2062762.686910671647638,2.062760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230458E56653N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.551656760130157,56.651119499999993]
["glac_bound",391074.000000000000000,"G229844E56100N","2008-05-01T00:00:00",63660.499981609056704,0.063660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229844E56100N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.155642829616966,56.099558000000002]
["glac_bound",391075.000000000000000,"G222202E59591N","2008-05-01T00:00:00",561651.044048077659681,0.561651000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222202E59591N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.798143985456193,59.590975999999998]
["glac_bound",391076.000000000000000,"G221754E59881N","2008-05-01T00:00:00",1939682.517744591692463,1.939680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221754E59881N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.265126565038742,59.885164500000002]
["glac_bound",391079.000000000000000,"G224777E59678N","2008-05-01T00:00:00",2412208.952786497771740,2.412210000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224777E59678N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.222474235022986,59.676992999999996]
["glac_bound",391084.000000000000000,"G228622E57055N","2008-05-01T00:00:00",889728.980766017222777,0.889729000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228622E57055N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.374875634716773,57.056298999999996]
["glac_bound",391085.000000000000000,"G227107E58294N","2008-05-01T00:00:00",55467.898808943253243,0.055468000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227107E58294N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.895279511394847,58.294814000000002]
["glac_bound",391087.000000000000000,"G229065E56518N","2008-05-01T00:00:00",317848.026174223341513,0.317848000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229065E56518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.938030139271063,56.518707500000005]
["glac_bound",391102.000000000000000,"G224331E59751N","2008-05-01T00:00:00",255629.389210371184163,0.255629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224331E59751N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.669386463009147,59.751570500000000]
["glac_bound",391109.000000000000000,"G221395E59746N","2008-05-01T00:00:00",4631060.941587422974408,4.631060000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221395E59746N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.603534649379640,59.755380000000002]
["glac_bound",391110.000000000000000,"G230046E56208N","2008-05-01T00:00:00",495895.468057314923499,0.495895000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230046E56208N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.953574449445568,56.207933499999996]
["glac_bound",391115.000000000000000,"G228374E56873N","2008-05-01T00:00:00",1607048.471944123972207,1.607050000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228374E56873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.616488844232094,56.874482499999999]
["glac_bound",391118.000000000000000,"G228431E57072N","2008-05-01T00:00:00",1448737.421768116764724,1.448740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228431E57072N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.567907685564478,57.076431999999997]
["glac_bound",391130.000000000000000,"G227810E57802N","2008-05-01T00:00:00",2443938.096363744232804,2.443940000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227810E57802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.194200625647341,57.802019999999999]
["glac_bound",391132.000000000000000,"G230685E55237N","2008-05-01T00:00:00",1299656.964611655334011,1.299660000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230685E55237N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.312481341444254,55.238499500000003]
["glac_bound",391135.000000000000000,"G227656E57101N","2008-05-01T00:00:00",14506186.357347827404737,14.506200000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227656E57101N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.347633032655409,57.105839500000002]
["glac_bound",391136.000000000000000,"G228938E56732N","2008-05-01T00:00:00",141862.049393747438444,0.141862000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228938E56732N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.061515658326812,56.732639500000005]
["glac_bound",391137.000000000000000,"G228497E57471N","2008-05-01T00:00:00",488503.596401689806953,0.488504000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228497E57471N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.504960992514043,57.471207500000006]
["glac_bound",391141.000000000000000,"G228614E56559N","2008-05-01T00:00:00",1008529.902590604731813,1.008530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228614E56559N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.380494985318876,56.562492500000005]
["glac_bound",391150.000000000000000,"G231997E58381N","2008-05-01T00:00:00",187298.438057021819986,0.187298000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-15T00:00:00","okay","None","None","08CA231997E58381N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.003447971049468,58.380396500000003]
["glac_bound",391152.000000000000000,"G230652E55611N","2008-05-01T00:00:00",196339.008109849557513,0.196339000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230652E55611N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.346311576653108,55.611903999999996]
["glac_bound",391153.000000000000000,"G226212E58697N","2008-05-01T00:00:00",1651755.177708723582327,1.651760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226212E58697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.777811863300286,58.695717500000001]
["glac_bound",391159.000000000000000,"G230257E56335N","2008-05-01T00:00:00",1084984.417585669085383,1.084980000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230257E56335N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.740661501753237,56.340104499999995]
["glac_bound",391161.000000000000000,"G230765E57082N","2008-05-01T00:00:00",523629.515813832636923,0.523629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230765E57082N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.236651723971704,57.082224499999995]
["glac_bound",391175.000000000000000,"G230531E56690N","2008-05-01T00:00:00",162029.679622575902613,0.162030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230531E56690N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.471071537673254,56.690224000000001]
["glac_bound",391177.000000000000000,"G229658E56162N","2008-05-01T00:00:00",64258.039704571761831,0.064258000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229658E56162N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.342594522171623,56.162022500000006]
["glac_bound",391179.000000000000000,"G223652E59573N","2008-05-01T00:00:00",76934.006416754607926,0.076934000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223652E59573N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.347957459446036,59.573854999999995]
["glac_bound",391181.000000000000000,"G225510E59215N","2008-05-01T00:00:00",16217619.064104096964002,16.217600000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225568E59197N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.429497907529566,59.205257500000002]
["glac_bound",391183.000000000000000,"G229193E56486N","2008-05-01T00:00:00",17691260.407591629773378,17.691299999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229193E56486N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.809422574984524,56.496246499999998]
["glac_bound",391187.000000000000000,"G231493E56202N","2008-05-01T00:00:00",199594.430850115022622,0.199594000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DA231493E56202N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.509218805095031,56.202964999999999]
["glac_bound",391188.000000000000000,"G225955E59185N","2008-05-01T00:00:00",149521.664778847742127,0.149522000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225955E59185N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.045882911801726,59.184745000000007]
["glac_bound",391189.000000000000000,"G224376E59867N","2008-05-01T00:00:00",550699.946147698559798,0.550700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224376E59867N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.622611317317023,59.867081499999998]
["glac_bound",391192.000000000000000,"G221962E59539N","2008-05-01T00:00:00",386285.622024779673666,0.386286000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221962E59539N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.037734249480337,59.539338000000001]
["glac_bound",391198.000000000000000,"G229196E56572N","2008-05-01T00:00:00",431244.919156322022900,0.431245000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229196E56572N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.804984604901676,56.573689999999999]
["glac_bound",391206.000000000000000,"G228009E58012N","2008-05-01T00:00:00",456514.892195796186570,0.456515000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228009E58012N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.994617566143347,58.010587500000000]
["glac_bound",391207.000000000000000,"G227996E57032N","2008-05-01T00:00:00",84060.705772847068147,0.084061000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227996E57032N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.004529144736864,57.032510000000002]
["glac_bound",391209.000000000000000,"G228129E57926N","2008-05-01T00:00:00",197574.183786895329831,0.197574000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228129E57926N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.871822364847247,57.926663500000004]
["glac_bound",391217.000000000000000,"G230654E55385N","2008-05-01T00:00:00",117037.420912738321931,0.117037000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230654E55385N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.345490452029537,55.385295499999998]
["glac_bound",391218.000000000000000,"G229638E56287N","2008-05-01T00:00:00",357753.605322062794585,0.357754000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229638E56287N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.356517638978914,56.282426500000000]
["glac_bound",391221.000000000000000,"G230195E57021N","2008-05-01T00:00:00",4998498.198969688266516,4.998500000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230195E57021N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.806776217367826,57.020534999999995]
["glac_bound",391223.000000000000000,"G230500E56629N","2008-05-01T00:00:00",889281.767430501524359,0.889282000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230500E56629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.497462799414961,56.629400500000003]
["glac_bound",391225.000000000000000,"G227993E57659N","2008-05-01T00:00:00",478821.707285325683188,0.478822000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227993E57659N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.007375711153855,57.660237500000001]
["glac_bound",391227.000000000000000,"G227500E57811N","2008-05-01T00:00:00",4774265.863460747525096,4.774270000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08CE227500E57811N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.518979653264921,57.819868499999998]
["glac_bound",391230.000000000000000,"G228466E57436N","2008-05-01T00:00:00",118068.418910452659475,0.118068000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228466E57436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.533693596716603,57.435882499999998]
["glac_bound",391233.000000000000000,"G225369E59309N","2008-05-01T00:00:00",1400445.015800212044269,1.400440000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225369E59309N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.632323981660250,59.308857000000003]
["glac_bound",391237.000000000000000,"G223108E59542N","2008-05-01T00:00:00",71138.840952713842853,0.071139000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223108E59542N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.891977210093046,59.542080999999996]
["glac_bound",391244.000000000000000,"G227258E58325N","2008-05-01T00:00:00",890192.325547344167717,0.890192000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227258E58325N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.742901439034711,58.324382499999999]
["glac_bound",391245.000000000000000,"G222984E59289N","2008-05-01T00:00:00",57239.400967318062612,0.057239000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222984E59289N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.014645424004613,59.288383000000003]
["glac_bound",391247.000000000000000,"G224319E59885N","2008-05-01T00:00:00",593150.799981826450676,0.593151000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224319E59885N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.680563852420335,59.886706000000004]
["glac_bound",391254.000000000000000,"G229741E56510N","2008-05-01T00:00:00",61420.506574197257578,0.061421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229741E56510N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.255585328415606,56.510571999999996]
["glac_bound",391256.000000000000000,"G229341E56991N","2008-05-01T00:00:00",434566.529953053570352,0.434567000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229341E56991N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.658419134358780,56.991491999999994]
["glac_bound",391263.000000000000000,"G222265E59737N","2008-05-01T00:00:00",18188490.906578715890646,18.188500000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222265E59737N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.690808189120901,59.757558500000002]
["glac_bound",391269.000000000000000,"G226263E58764N","2008-05-01T00:00:00",668822.612978378892876,0.668823000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226263E58764N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.734477359731784,58.767429000000000]
["glac_bound",391272.000000000000000,"G229214E56502N","2008-05-01T00:00:00",222654.819097800820600,0.222655000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229214E56502N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.787811435089964,56.503650000000000]
["glac_bound",391275.000000000000000,"G226452E58938N","2008-05-01T00:00:00",134861.780444123374764,0.134862000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226452E58938N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.546874758674107,58.937795999999999]
["glac_bound",391276.000000000000000,"G227151E57834N","2008-05-01T00:00:00",2001914.941503524314612,2.001910000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227151E57834N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.855657289291003,57.834516499999999]
["glac_bound",391277.000000000000000,"G225028E59256N","2008-05-01T00:00:00",3650860.208057243376970,3.650860000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE225028E59256N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.969446655334025,59.265507499999998]
["glac_bound",391282.000000000000000,"G223825E59641N","2008-05-01T00:00:00",429267.567581409122795,0.429268000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223825E59641N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.175167960674173,59.641410000000000]
["glac_bound",391283.000000000000000,"G230595E55336N","2008-05-01T00:00:00",72990.252435597198200,0.072990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230595E55336N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.405860001396832,55.336593000000001]
["glac_bound",391288.000000000000000,"G230047E57068N","2008-05-01T00:00:00",369243.894058690406382,0.369244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG230047E57068N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.952857980688805,57.067546000000000]
["glac_bound",391291.000000000000000,"G227863E57523N","2008-05-01T00:00:00",7461869.271508551202714,7.461870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227863E57523N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.139905561287264,57.537629499999994]
["glac_bound",391292.000000000000000,"G230539E57144N","2008-05-01T00:00:00",634828.571566707454622,0.634829000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230539E57144N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.463417581607303,57.145202999999995]
["glac_bound",391295.000000000000000,"G227896E56842N","2008-05-01T00:00:00",638852.597113081254065,0.638853000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227896E56842N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.100950100872382,56.848792000000003]
["glac_bound",391296.000000000000000,"G228762E57384N","2008-05-01T00:00:00",11478677.528176898136735,11.478700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228762E57384N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.267704665850999,57.393628999999997]
["glac_bound",391299.000000000000000,"G227872E57514N","2008-05-01T00:00:00",786031.676209111930802,0.786032000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227872E57514N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.125686338453534,57.513152500000004]
["glac_bound",391303.000000000000000,"G231202E57073N","2008-05-01T00:00:00",73420.871293797565158,0.073421000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231202E57073N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.798166752733152,57.073594999999997]
["glac_bound",391304.000000000000000,"G221552E59952N","2008-05-01T00:00:00",905899.421921991626732,0.905899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221552E59952N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.456553855136633,59.959738500000000]
["glac_bound",391307.000000000000000,"G228863E56531N","2008-05-01T00:00:00",309691.284847622562665,0.309691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228863E56531N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.138374079044638,56.531169500000004]
["glac_bound",391309.000000000000000,"G222380E59693N","2008-05-01T00:00:00",87624.537913084132015,0.087624000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222380E59693N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.618688614779018,59.692375499999997]
["glac_bound",391313.000000000000000,"G229649E57760N","2008-05-01T00:00:00",191918.094395932334010,0.191918000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CB229649E57760N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.349911001234261,57.760660000000001]
["glac_bound",391316.000000000000000,"G230709E56718N","2008-05-01T00:00:00",528986.633772398112342,0.528987000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230709E56718N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.288650772443873,56.719020000000000]
["glac_bound",391318.000000000000000,"G226682E58367N","2008-05-01T00:00:00",156383489.13472896814346,156.383000000000010,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","Wright Glacier","None","08BD226682E58367N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.543988429826243,58.411777499999999]
["glac_bound",391322.000000000000000,"G227889E58088N","2008-05-01T00:00:00",712511.640872613294050,0.712512000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227889E58088N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.116112620682884,58.086387999999999]
["glac_bound",391323.000000000000000,"G230431E57094N","2008-05-01T00:00:00",113841.952266276915907,0.113842000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230431E57094N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.568677172852375,57.093336999999998]
["glac_bound",391329.000000000000000,"G230368E55520N","2008-05-01T00:00:00",116532.913850922312122,0.116533000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230368E55520N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.630834679438124,55.519738500000003]
["glac_bound",391330.000000000000000,"G223927E59892N","2008-05-01T00:00:00",1195430.685469574993476,1.195430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223927E59892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.072298853272628,59.892780999999999]
["glac_bound",391334.000000000000000,"G229349E56322N","2008-05-01T00:00:00",1042303.187699188594706,1.042300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229349E56322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.651148865671644,56.321675999999997]
["glac_bound",391335.000000000000000,"G230191E57495N","2008-05-01T00:00:00",282564.078694506955799,0.282564000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230191E57495N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.805999611684456,57.496321500000001]
["glac_bound",391337.000000000000000,"G230065E55711N","2008-05-01T00:00:00",305801.169024114438798,0.305801000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230065E55711N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.935681919239869,55.709305000000001]
["glac_bound",391338.000000000000000,"G222525E59120N","2008-05-01T00:00:00",216029.210785061935894,0.216029000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222523E59122N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.477717813368059,59.122284499999999]
["glac_bound",391340.000000000000000,"G228510E57299N","2008-05-01T00:00:00",365198.936781761585735,0.365199000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228510E57299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.488358125115440,57.299026999999995]
["glac_bound",391341.000000000000000,"G227316E58281N","2008-05-01T00:00:00",1689848.278883526800200,1.689850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227316E58281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.693156215307681,58.284238000000002]
["glac_bound",391347.000000000000000,"G230119E57333N","2008-05-01T00:00:00",65875.522370570295607,0.065876000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230119E57333N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.878877859821415,57.333629500000001]
["glac_bound",391351.000000000000000,"G225214E59636N","2008-05-01T00:00:00",888891.688509330386296,0.888892000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225214E59636N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.785616377459064,59.635781500000000]
["glac_bound",391353.000000000000000,"G222536E59712N","2008-05-01T00:00:00",552105.987757478840649,0.552106000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222536E59712N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.460245407287857,59.710406500000005]
["glac_bound",391354.000000000000000,"G228531E56915N","2008-05-01T00:00:00",161091.774341379204998,0.161092000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228531E56915N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.469706689357281,56.915323500000000]
["glac_bound",391358.000000000000000,"G230493E55910N","2008-05-01T00:00:00",11818737.590259514749050,11.818700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230493E55910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.526791351190468,55.920777000000001]
["glac_bound",391360.000000000000000,"G230360E56175N","2008-05-01T00:00:00",7531116.155906639061868,7.531120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230360E56175N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.652797417415627,56.184484499999996]
["glac_bound",391372.000000000000000,"G229401E57715N","2008-05-01T00:00:00",8282320.704386820085347,8.282320000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229401E57715N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.600908897763560,57.725459499999999]
["glac_bound",391378.000000000000000,"G231021E57387N","2008-05-01T00:00:00",397745.960354613605887,0.397746000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231021E57387N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.979128994127507,57.388569000000004]
["glac_bound",391384.000000000000000,"G230113E55876N","2008-05-01T00:00:00",157036.577777136815712,1.002970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230113E55876N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.890300567448662,55.875114499999995]
["glac_bound",391384.000000000000000,"G230113E55876N","2008-05-01T00:00:00",845933.691512836958282,1.002970000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230113E55876N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.882371719366006,55.882271500000002]
["glac_bound",391388.000000000000000,"G229609E56372N","2008-05-01T00:00:00",369972.650390008930117,0.369973000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229609E56372N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.390666130108968,56.372411000000000]
["glac_bound",391393.000000000000000,"G228331E57504N","2008-05-01T00:00:00",107094.100512784454622,0.107094000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228331E57504N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.669389642113572,57.504126999999997]
["glac_bound",391395.000000000000000,"G227171E58526N","2008-05-01T00:00:00",645829.114986222237349,0.645829000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227171E58526N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.834050175030995,58.527531000000003]
["glac_bound",391396.000000000000000,"G229997E57065N","2008-05-01T00:00:00",12690198.930213660001755,12.690200000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229997E57065N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.999299593524626,57.069204499999998]
["glac_bound",391399.000000000000000,"G228106E57600N","2008-05-01T00:00:00",481008.888210558274295,0.481009000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228106E57600N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.890654616864111,57.599917000000005]
["glac_bound",391400.000000000000000,"G222752E59361N","2008-05-01T00:00:00",456036.307271186029539,0.456036000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222752E59361N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.247330228758130,59.360960000000006]
["glac_bound",391402.000000000000000,"G230152E55748N","2008-05-01T00:00:00",96811.122275624176837,0.096811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230152E55748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.847172429911922,55.747687999999997]
["glac_bound",391408.000000000000000,"G225579E59443N","2008-05-01T00:00:00",1576488.402197658317164,1.576490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225579E59443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.420206177124669,59.449617500000002]
["glac_bound",391416.000000000000000,"G225846E59353N","2008-05-01T00:00:00",265409.645020178519189,0.265410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225846E59353N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.154015473674917,59.351752500000003]
["glac_bound",391418.000000000000000,"G227865E57768N","2008-05-01T00:00:00",899302.946359098190442,0.899303000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227865E57768N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.134919210304474,57.768856499999998]
["glac_bound",391423.000000000000000,"G230939E56436N","2008-05-01T00:00:00",291939.487785921082832,0.291939000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230939E56436N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.063343846996247,56.436312999999998]
["glac_bound",391424.000000000000000,"G229978E56162N","2008-05-01T00:00:00",2901527.885729009285569,2.901530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD229978E56162N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.024351026315799,56.161474499999997]
["glac_bound",391426.000000000000000,"G225677E59378N","2008-05-01T00:00:00",254107.112439225282287,0.254107000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225677E59378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.323819180348494,59.378787000000003]
["glac_bound",391432.000000000000000,"G229726E56718N","2008-05-01T00:00:00",285303.741369607974775,0.285304000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229726E56718N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.273681632795729,56.718657000000000]
["glac_bound",391433.000000000000000,"G223055E59179N","2008-05-01T00:00:00",55489.817303435782378,0.055490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223055E59179N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.944611407963464,59.178713000000002]
["glac_bound",391438.000000000000000,"G224089E59892N","2008-05-01T00:00:00",176459.440235138346907,0.176459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224089E59892N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.912609319301652,59.891455000000001]
["glac_bound",391445.000000000000000,"G229902E57126N","2008-05-01T00:00:00",237413.298839965456864,0.237413000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229902E57126N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.095639335282243,57.126673499999995]
["glac_bound",391454.000000000000000,"G230533E55172N","2008-05-01T00:00:00",86401.166542309540091,0.086401000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230533E55172N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.467087599646845,55.172612500000000]
["glac_bound",391458.000000000000000,"G224911E59398N","2008-05-01T00:00:00",53666.741819570452208,0.053667000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224911E59398N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.089352910412742,59.397846500000000]
["glac_bound",391465.000000000000000,"G227918E57298N","2008-05-01T00:00:00",4993296.759268478490412,4.993300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227918E57298N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.087528356532516,57.299595500000002]
["glac_bound",391470.000000000000000,"G230859E56435N","2008-05-01T00:00:00",274827.390164385840762,0.274827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230859E56435N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.141728783170805,56.435333000000000]
["glac_bound",391473.000000000000000,"G231524E57264N","2008-05-01T00:00:00",226668.141352402220946,0.226668000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231524E57264N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.475894988879730,57.263357999999997]
["glac_bound",391474.000000000000000,"G229020E57169N","2008-05-01T00:00:00",56372.654833754088031,0.056373000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229020E57169N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.979511547082240,57.168830999999997]
["glac_bound",391477.000000000000000,"G228932E57688N","2008-05-01T00:00:00",355878.639164343767334,0.355879000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228932E57688N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.068277018526402,57.687283499999999]
["glac_bound",391480.000000000000000,"G228758E57001N","2008-05-01T00:00:00",488761.119359019503463,0.488761000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228758E57001N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.241577587249651,56.999958500000005]
["glac_bound",391481.000000000000000,"G227096E58182N","2008-05-01T00:00:00",2634483.628019514959306,2.634480000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227096E58182N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.909063121531858,58.185138499999994]
["glac_bound",391486.000000000000000,"G225667E59352N","2008-05-01T00:00:00",1736601.728979723295197,1.736600000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225667E59352N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.330653176926376,59.358823500000000]
["glac_bound",391488.000000000000000,"G227971E57806N","2008-05-01T00:00:00",2021868.086131680756807,2.021870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227971E57806N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.028976693553034,57.802164500000003]
["glac_bound",391489.000000000000000,"G230730E54888N","2008-05-01T00:00:00",1003342.326547205913812,1.003340000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230730E54888N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.273641597234985,54.891222999999997]
["glac_bound",391491.000000000000000,"G230050E56173N","2008-05-01T00:00:00",234956.431270168715855,0.234956000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230050E56173N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.951098480270588,56.175426999999999]
["glac_bound",391492.000000000000000,"G230277E56282N","2008-05-01T00:00:00",612443.469281932804734,0.612443000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230277E56282N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.719485020613604,56.280381000000006]
["glac_bound",391494.000000000000000,"G222338E59729N","2008-05-01T00:00:00",199536.954632838576799,0.199537000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222338E59729N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.661314432213203,59.728379500000003]
["glac_bound",391497.000000000000000,"G227227E58212N","2008-05-01T00:00:00",189276.532771725731436,0.189277000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227227E58212N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.774388751459554,58.211981500000000]
["glac_bound",391499.000000000000000,"G230190E56292N","2008-05-01T00:00:00",1817216.665017280727625,1.817220000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230190E56292N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.815104461761166,56.296482999999995]
["glac_bound",391510.000000000000000,"G230332E55616N","2008-05-01T00:00:00",256937.625248517171713,0.256938000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230332E55616N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.670066031058582,55.615603499999999]
["glac_bound",391517.000000000000000,"G227789E57924N","2008-05-01T00:00:00",1670454.526474812766537,1.670450000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227789E57924N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.200359898876400,57.923699999999997]
["glac_bound",391521.000000000000000,"G228099E57567N","2008-05-01T00:00:00",579066.117744274553843,0.579066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228099E57567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.905475042077910,57.565421000000001]
["glac_bound",391523.000000000000000,"G225161E59847N","2008-05-01T00:00:00",157585.567394930345472,0.157586000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225161E59847N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.839267577741481,59.845723499999998]
["glac_bound",391524.000000000000000,"G231245E57534N","2008-05-01T00:00:00",88166.105677317144000,0.088166000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231245E57534N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.755568034916223,57.534108500000002]
["glac_bound",391526.000000000000000,"G230419E55232N","2008-05-01T00:00:00",114458.611674887200934,0.114459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230419E55232N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.580185120344112,55.231835500000003]
["glac_bound",391533.000000000000000,"G223807E59642N","2008-05-01T00:00:00",413928.606363732891623,0.413929000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223807E59642N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.197568337433921,59.644703000000000]
["glac_bound",391534.000000000000000,"G227731E57419N","2008-05-01T00:00:00",54201026.288631796836853,54.201000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Triumph Glacier","None","08CE227731E57419N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.294118646747791,57.454758499999997]
["glac_bound",391535.000000000000000,"G227579E58143N","2008-05-01T00:00:00",4928264.709835174493492,4.928260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227579E58143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.427806115168551,58.147050000000000]
["glac_bound",391542.000000000000000,"G222999E59392N","2008-05-01T00:00:00",2701513.729531672317535,2.701510000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222999E59392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.010208224451446,59.398515500000002]
["glac_bound",391547.000000000000000,"G228714E56655N","2008-05-01T00:00:00",365313.291747825744096,0.365313000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228714E56655N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.288611300338914,56.656576500000000]
["glac_bound",391552.000000000000000,"G225209E59313N","2008-05-01T00:00:00",170479.202603639190784,0.170479000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BD225209E59313N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.793008548754074,59.315649000000001]
["glac_bound",391557.000000000000000,"G227911E57484N","2008-05-01T00:00:00",142987.383744949620450,0.142987000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227911E57484N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.088653238416669,57.485281499999999]
["glac_bound",391558.000000000000000,"G222728E59392N","2008-05-01T00:00:00",776562.388445679447614,0.776562000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222728E59392N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.272026134900926,59.390861500000000]
["glac_bound",391561.000000000000000,"G222974E59443N","2008-05-01T00:00:00",283184.202771981246769,0.283184000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222974E59443N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.023733749999991,59.442205000000001]
["glac_bound",391563.000000000000000,"G228581E57493N","2008-05-01T00:00:00",173223.553380456840387,0.173224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228581E57493N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.419260820701481,57.492614500000002]
["glac_bound",391564.000000000000000,"G229915E57126N","2008-05-01T00:00:00",385781.015960454533342,0.385781000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229915E57126N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.085169491387944,57.126202500000005]
["glac_bound",391567.000000000000000,"G223202E59418N","2008-05-01T00:00:00",7657847.814393133856356,7.657850000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223202E59418N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.807277338449268,59.428575000000002]
["glac_bound",391573.000000000000000,"G229557E56146N","2008-05-01T00:00:00",8390838.294469190761447,8.390840000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229557E56146N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.427891593060991,56.154059000000004]
["glac_bound",391575.000000000000000,"G229444E57177N","2008-05-01T00:00:00",7284764.673502473160625,7.284760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229444E57177N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.568464389925396,57.176666499999996]
["glac_bound",391585.000000000000000,"G228210E57120N","2008-05-01T00:00:00",225304.601753967901459,0.225305000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228210E57120N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.789235218977012,57.119623000000004]
["glac_bound",391588.000000000000000,"G222818E59479N","2008-05-01T00:00:00",2018869.048129374161363,2.018870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222818E59479N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.191177630162684,59.482945999999998]
["glac_bound",391592.000000000000000,"G223268E59236N","2008-05-01T00:00:00",379867.741572894155979,0.379868000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF223268E59236N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.729678862801052,59.237651499999998]
["glac_bound",391596.000000000000000,"G228633E56665N","2008-05-01T00:00:00",316537.760191419918556,0.316538000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228633E56665N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.365738314128777,56.665663500000001]
["glac_bound",391597.000000000000000,"G225788E59153N","2008-05-01T00:00:00",388426.338337086839601,0.388426000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225788E59153N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.214316913799877,59.152903499999994]
["glac_bound",391598.000000000000000,"G230834E56546N","2008-05-01T00:00:00",110534.624802880440257,0.110535000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230834E56546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.166566433188393,56.546343499999999]
["glac_bound",391611.000000000000000,"G229203E57160N","2008-05-01T00:00:00",1462253.623872837750241,1.462250000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229203E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.797702229477636,57.166954000000004]
["glac_bound",391613.000000000000000,"G230582E56580N","2008-05-01T00:00:00",199285.289830760419136,0.199285000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230582E56580N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.419082076012671,56.580809000000002]
["glac_bound",391614.000000000000000,"G226799E58533N","2008-05-01T00:00:00",2067159.898891825228930,2.067160000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226799E58533N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.198598017989127,58.539294499999997]
["glac_bound",391615.000000000000000,"G229399E57753N","2008-05-01T00:00:00",1460842.863135106861591,1.460840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CB229399E57753N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.598066652203954,57.754483000000000]
["glac_bound",391618.000000000000000,"G230619E55637N","2008-05-01T00:00:00",1033741.191772029036656,1.033740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230619E55637N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.380882502224836,55.637195500000004]
["glac_bound",391621.000000000000000,"G229692E56128N","2008-05-01T00:00:00",66839977.596180789172649,66.840000000000003,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","Chickamin Glacier","None","08DD229692E56128N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.299688380952375,56.101381000000003]
["glac_bound",391622.000000000000000,"G229947E56955N","2008-05-01T00:00:00",586065.548167787957937,0.586066000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229947E56955N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.050921049506002,56.955073499999997]
["glac_bound",391626.000000000000000,"G223242E59561N","2008-05-01T00:00:00",135318.031915452709654,0.135318000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223242E59561N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.759047836617697,59.561099499999997]
["glac_bound",391639.000000000000000,"G222312E59249N","2008-05-01T00:00:00",23540.644465458844934,0.023541000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222312E59249N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.687458994167969,59.248757499999996]
["glac_bound",391652.000000000000000,"G228111E56752N","2008-05-01T00:00:00",1344703.675059503410012,1.344700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228111E56752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.891919545494318,56.754636500000004]
["glac_bound",391656.000000000000000,"G225111E59662N","2008-05-01T00:00:00",60525.317100222928275,0.060525000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225111E59662N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.888257921737591,59.661907499999998]
["glac_bound",391659.000000000000000,"G228974E56444N","2008-05-01T00:00:00",2826870.453003440983593,2.826870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228974E56444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.023058995074479,56.445861499999999]
["glac_bound",391661.000000000000000,"G227986E57034N","2008-05-01T00:00:00",292924.819175119104329,0.292925000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227986E57034N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.013336455792910,57.033835500000002]
["glac_bound",391662.000000000000000,"G223298E59609N","2008-05-01T00:00:00",525618.160624017124064,0.525618000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223298E59609N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.697772115914802,59.607361499999996]
["glac_bound",391663.000000000000000,"G229183E57026N","2008-05-01T00:00:00",5421492.404849266633391,5.421490000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229183E57026N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.828522161994499,57.037683500000000]
["glac_bound",391664.000000000000000,"G222723E59079N","2008-05-01T00:00:00",1139567.573940586065874,1.139570000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BF222724E59078N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.276009676299452,59.078885499999998]
["glac_bound",391670.000000000000000,"G222440E59875N","2008-05-01T00:00:00",1688814.385691946372390,1.688810000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222440E59875N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.565124698946761,59.882211999999996]
["glac_bound",391671.000000000000000,"G230250E55801N","2008-05-01T00:00:00",15453090.806856635957956,15.453099999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230250E55801N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.745067299366212,55.807999500000001]
["glac_bound",391678.000000000000000,"G225354E59524N","2008-05-01T00:00:00",76989.292170625776635,0.076989000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225354E59524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.645756641273749,59.525448499999996]
["glac_bound",391680.000000000000000,"G229224E57086N","2008-05-01T00:00:00",499824.224567471130285,0.499824000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229224E57086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.776687588610230,57.086365999999998]
["glac_bound",391684.000000000000000,"G230110E55933N","2008-05-01T00:00:00",664948.060780264204368,0.664948000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230110E55933N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.895290712202240,55.936749500000005]
["glac_bound",391686.000000000000000,"G227909E57489N","2008-05-01T00:00:00",261620.583720240945695,0.261621000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227909E57489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.092037828614934,57.488780500000004]
["glac_bound",391688.000000000000000,"G230185E56222N","2008-05-01T00:00:00",154307.373671587498393,0.154307000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230185E56222N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.812006448617922,56.222712999999999]
["glac_bound",391690.000000000000000,"G228839E56835N","2008-05-01T00:00:00",31338900.167060740292072,31.338899999999999,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228839E56835N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.160887395292463,56.856381999999996]
["glac_bound",391691.000000000000000,"G221818E59784N","2008-05-01T00:00:00",2087044.807640812592581,2.087040000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221818E59784N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.183617439739407,59.788816999999995]
["glac_bound",391696.000000000000000,"G229254E56828N","2008-05-01T00:00:00",1219838.227420956129208,1.219840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229254E56828N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.749771643310567,56.822917000000004]
["glac_bound",391700.000000000000000,"G230789E57049N","2008-05-01T00:00:00",121018.269775257329457,0.121018000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230789E57049N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.209229840663966,57.049277500000002]
["glac_bound",391702.000000000000000,"G227832E57322N","2008-05-01T00:00:00",13015001.750635147094727,13.015000000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227832E57322N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.209075366295252,57.339765000000000]
["glac_bound",391706.000000000000000,"G226133E58757N","2008-05-01T00:00:00",1278758.918307791929692,1.278760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226133E58757N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.865820457167843,58.761378499999999]
["glac_bound",391712.000000000000000,"G226689E58536N","2008-05-01T00:00:00",3829676.795519149862230,3.829680000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226689E58536N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.312714679370288,58.541815999999997]
["glac_bound",391714.000000000000000,"G230688E56774N","2008-05-01T00:00:00",2257789.061893906444311,2.257790000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230688E56774N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.307435330188667,56.774780999999997]
["glac_bound",391717.000000000000000,"G226802E58398N","2008-05-01T00:00:00",11611652.043372925370932,11.611700000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226802E58398N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.212341940044951,58.382515999999995]
["glac_bound",391720.000000000000000,"G230284E55731N","2008-05-01T00:00:00",1231092.539908569538966,1.231090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230284E55731N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.713363506416584,55.737479999999998]
["glac_bound",391721.000000000000000,"G230234E57113N","2008-05-01T00:00:00",93238.071206454711501,0.093238000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230234E57113N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.766391146279091,57.112633500000001]
["glac_bound",391722.000000000000000,"G221875E59588N","2008-05-01T00:00:00",432912.212250979966484,0.432912000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221875E59588N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.128216372494990,59.588879000000006]
["glac_bound",391728.000000000000000,"G230198E56154N","2008-05-01T00:00:00",10309350.444322180002928,10.309400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230198E56154N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.815145390483565,56.154534999999996]
["glac_bound",391729.000000000000000,"G227326E58206N","2008-05-01T00:00:00",266897.436334296246059,0.266897000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227326E58206N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.674066385135120,58.204962500000001]
["glac_bound",391732.000000000000000,"G229004E57178N","2008-05-01T00:00:00",1062737.346786198904738,1.062740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229004E57178N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.993693234557043,57.184573000000000]
["glac_bound",391733.000000000000000,"G230605E56733N","2008-05-01T00:00:00",154598.334921483939979,0.154598000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230605E56733N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.395228747636224,56.733131000000000]
["glac_bound",391740.000000000000000,"G227889E57748N","2008-05-01T00:00:00",2018739.994417658774182,2.018740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227889E57748N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.126013235493360,57.747759500000001]
["glac_bound",391741.000000000000000,"G222230E59739N","2008-05-01T00:00:00",316056.593581202148926,0.316057000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222230E59739N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.766063722750971,59.737684000000002]
["glac_bound",391742.000000000000000,"G230866E54949N","2008-05-01T00:00:00",348030.291843327693641,0.348030000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230866E54949N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.134788860054414,54.950617500000000]
["glac_bound",391744.000000000000000,"G230541E54977N","2008-05-01T00:00:00",80457.672567977017025,0.080458000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230541E54977N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.457882266196009,54.978254500000006]
["glac_bound",391745.000000000000000,"G227706E58071N","2008-05-01T00:00:00",276658.725918331241701,0.276659000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08BA227706E58071N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.298764335499129,58.072739999999996]
["glac_bound",391757.000000000000000,"G224649E59855N","2008-05-01T00:00:00",300713.180663678911515,0.300713000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224649E59855N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.350660012483445,59.854084999999998]
["glac_bound",391758.000000000000000,"G224313E59901N","2008-05-01T00:00:00",1880409.355364032089710,1.880410000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224313E59901N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.685374077077768,59.904030500000005]
["glac_bound",391760.000000000000000,"G228976E56833N","2008-05-01T00:00:00",56291.270086753407668,0.056291000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228976E56833N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.026233796384560,56.832104000000001]
["glac_bound",391762.000000000000000,"G227724E57905N","2008-05-01T00:00:00",2441624.448831304907799,2.441620000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227724E57905N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.268738263009766,57.908557000000002]
["glac_bound",391763.000000000000000,"G229517E57112N","2008-05-01T00:00:00",1356991.420693659223616,1.356990000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229517E57112N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.490577089970600,57.114717499999998]
["glac_bound",391764.000000000000000,"G226234E58919N","2008-05-01T00:00:00",17355905.735296592116356,17.355899999999998,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226234E58919N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.737501522937293,58.910559500000005]
["glac_bound",391765.000000000000000,"G226472E58715N","2008-05-01T00:00:00",1815693.840126762399450,1.815690000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226472E58715N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.528790550005624,58.716217999999998]
["glac_bound",391768.000000000000000,"G224198E59898N","2008-05-01T00:00:00",511286.181248920911457,0.511286000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224198E59898N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.806432381712966,59.900663999999999]
["glac_bound",391772.000000000000000,"G229059E56739N","2008-05-01T00:00:00",68759.630633206965285,0.068760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229059E56739N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.941998738992993,56.738821000000002]
["glac_bound",391778.000000000000000,"G223750E59697N","2008-05-01T00:00:00",527284.390795048791915,0.527284000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223750E59697N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.254381573970022,59.699669499999999]
["glac_bound",391783.000000000000000,"G226597E58442N","2008-05-01T00:00:00",81286.660093064638204,0.081287000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BD226597E58442N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.401443473401059,58.441001499999999]
["glac_bound",391794.000000000000000,"G230142E54804N","2008-05-01T00:00:00",98183.075804876236361,0.098183000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230142E54804N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.858695534257976,54.804125999999997]
["glac_bound",391800.000000000000000,"G230585E55338N","2008-05-01T00:00:00",505169.132847898290493,0.505169000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230585E55338N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.412422450343200,55.338532499999999]
["glac_bound",391805.000000000000000,"G231266E57543N","2008-05-01T00:00:00",165563.019948278582888,0.165563000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231266E57543N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.733435884322716,57.543345000000002]
["glac_bound",391806.000000000000000,"G226753E58295N","2008-05-01T00:00:00",7545953.148888527415693,7.545950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226753E58295N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.215274360312321,58.307456999999999]
["glac_bound",391811.000000000000000,"G222161E59684N","2008-05-01T00:00:00",722775.342780161648989,0.722775000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222161E59684N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.834796427428273,59.685480499999997]
["glac_bound",391812.000000000000000,"G224207E59870N","2008-05-01T00:00:00",383502.931959824752994,0.383503000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224207E59870N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.792040629976441,59.869270999999998]
["glac_bound",391814.000000000000000,"G230501E57025N","2008-05-01T00:00:00",292653.681113302824087,0.292654000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230501E57025N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.499712207258995,57.024744499999997]
["glac_bound",391817.000000000000000,"G230406E55792N","2008-05-01T00:00:00",5643114.786554240621626,5.643110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230406E55792N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.597411716034117,55.788249499999999]
["glac_bound",391823.000000000000000,"G228879E56786N","2008-05-01T00:00:00",5464527.617184286005795,5.464530000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228879E56786N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.119196593191759,56.785451500000001]
["glac_bound",391824.000000000000000,"G229614E57379N","2008-05-01T00:00:00",279011.414354253734928,0.279011000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229614E57379N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.385727603803815,57.379275500000006]
["glac_bound",391826.000000000000000,"G230633E57276N","2008-05-01T00:00:00",120559.014832401138847,0.120559000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230633E57276N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.368284814601964,57.276461499999996]
["glac_bound",391829.000000000000000,"G225548E59299N","2008-05-01T00:00:00",975489.178267979295924,0.975489000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225548E59299N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.450995884502447,59.297967499999999]
["glac_bound",391831.000000000000000,"G221332E59802N","2008-05-01T00:00:00",2365097.267831539269537,2.365100000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","Art Lewis Glacier","None","08AB221332E59802N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.669305813778834,59.804823499999998]
["glac_bound",391834.000000000000000,"G230050E56122N","2008-05-01T00:00:00",89315.953250311518786,0.089316000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DD230050E56122N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.948497148305080,56.121343999999993]
["glac_bound",391836.000000000000000,"G230588E56714N","2008-05-01T00:00:00",114903.054965766554233,0.114903000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230588E56714N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.411731043814427,56.714003500000004]
["glac_bound",391838.000000000000000,"G229870E56288N","2008-05-01T00:00:00",1305957.521382269915193,1.305960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229870E56288N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.136055305762085,56.291771499999996]
["glac_bound",391839.000000000000000,"G228761E57501N","2008-05-01T00:00:00",153719.354630179615924,0.153719000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228761E57501N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.239217925989180,57.500624500000001]
["glac_bound",391841.000000000000000,"G228889E57665N","2008-05-01T00:00:00",776571.053404497564770,0.776571000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CE228889E57665N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.109866031645197,57.666771499999996]
["glac_bound",391844.000000000000000,"G230797E57124N","2008-05-01T00:00:00",92109.827805481399992,0.092110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230797E57124N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.204696523002440,57.123816500000004]
["glac_bound",391846.000000000000000,"G227932E57378N","2008-05-01T00:00:00",62024.959097036597086,0.062025000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227932E57378N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.068797221642399,57.378954999999998]
["glac_bound",391847.000000000000000,"G221867E59586N","2008-05-01T00:00:00",55464.426045315194642,0.055464000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221867E59586N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.134861993611452,59.586874500000000]
["glac_bound",391855.000000000000000,"G224461E59791N","2008-05-01T00:00:00",236611.448149572213879,0.236611000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224461E59791N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.541031147208628,59.790809000000003]
["glac_bound",391860.000000000000000,"G231050E57141N","2008-05-01T00:00:00",54945.171505877318850,0.054945000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC231050E57141N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.949820541681561,57.140992999999995]
["glac_bound",391870.000000000000000,"G230424E57428N","2008-05-01T00:00:00",320541.612295152910519,0.320542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CC230424E57428N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.575468835565630,57.429862000000000]
["glac_bound",391871.000000000000000,"G223905E59703N","2008-05-01T00:00:00",1631112.971783335786313,1.631110000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223905E59703N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.100166419280299,59.703297500000005]
["glac_bound",391873.000000000000000,"G230478E55957N","2008-05-01T00:00:00",123572.558560427816701,0.123573000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230478E55957N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522073188957478,55.956761999999998]
["glac_bound",391877.000000000000000,"G223652E59725N","2008-05-01T00:00:00",543954.670793789322488,0.543955000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE223652E59725N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.347480787693826,59.725333500000005]
["glac_bound",391880.000000000000000,"G222628E59316N","2008-05-01T00:00:00",2866723.877582086715847,2.866720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AB222628E59316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.364432165380663,59.319450500000002]
["glac_bound",391882.000000000000000,"G228314E57500N","2008-05-01T00:00:00",181592.516032804793213,0.181593000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228314E57500N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.685646106533625,57.500229000000004]
["glac_bound",391887.000000000000000,"G230077E56358N","2008-05-01T00:00:00",574925.799038291443139,0.574926000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230077E56358N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.922688490958791,56.357827000000000]
["glac_bound",391890.000000000000000,"G229301E56459N","2008-05-01T00:00:00",438787.119433460233267,0.438787000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229301E56459N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.697190615035595,56.462141500000001]
["glac_bound",391893.000000000000000,"G227245E58331N","2008-05-01T00:00:00",207315.067430402938044,0.207315000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227245E58331N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.755817380544215,58.330593999999998]
["glac_bound",391899.000000000000000,"G223721E59881N","2008-05-01T00:00:00",1638351.741259128553793,1.638350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223721E59881N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.271109464947642,59.885047499999999]
["glac_bound",391914.000000000000000,"G228072E57489N","2008-05-01T00:00:00",568456.993404663284309,0.568457000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228072E57489N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.927650340659341,57.488259999999997]
["glac_bound",391921.000000000000000,"G229357E56528N","2008-05-01T00:00:00",1873263.054915926419199,1.873260000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229357E56528N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.645391295195964,56.528539000000002]
["glac_bound",391926.000000000000000,"G229967E57170N","2008-05-01T00:00:00",185598.513798964180751,0.185599000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229967E57170N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.033053631733026,57.169543000000004]
["glac_bound",391935.000000000000000,"G222431E59897N","2008-05-01T00:00:00",2188184.388405065052211,2.188180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222431E59897N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.579176244146140,59.907274500000000]
["glac_bound",391938.000000000000000,"G228030E57216N","2008-05-01T00:00:00",981414.707114253658801,0.981415000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228030E57216N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.967169506294738,57.214772500000002]
["glac_bound",391939.000000000000000,"G227462E58408N","2008-05-01T00:00:00",2432243.416212669108063,2.432240000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227462E58408N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.551102964758229,58.412096000000005]
["glac_bound",391940.000000000000000,"G227857E57207N","2008-05-01T00:00:00",4736092.096162502653897,4.736090000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227857E57207N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.145536451257470,57.206721500000000]
["glac_bound",391941.000000000000000,"G222298E59938N","2008-05-01T00:00:00",239826.632632758817635,0.239827000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222298E59938N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.700017403265235,59.938523500000002]
["glac_bound",391943.000000000000000,"G228552E57270N","2008-05-01T00:00:00",2327275.863551268354058,2.327280000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228552E57270N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.446098715678829,57.269369999999995]
["glac_bound",391951.000000000000000,"G229563E56242N","2008-05-01T00:00:00",9832611.998823983594775,9.832610000000001,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229563E56242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.446709217391287,56.252492000000004]
["glac_bound",391956.000000000000000,"G228134E57086N","2008-05-01T00:00:00",190882.500595080666244,0.190883000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228134E57086N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.866057503221668,57.084238999999997]
["glac_bound",391957.000000000000000,"G230306E55762N","2008-05-01T00:00:00",2534076.431393107399344,2.534080000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230306E55762N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.699264933398865,55.763002499999999]
["glac_bound",391961.000000000000000,"G229473E57160N","2008-05-01T00:00:00",69970.849369796109386,0.069971000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229473E57160N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.528014062100709,57.160465500000001]
["glac_bound",391963.000000000000000,"G230804E55105N","2008-05-01T00:00:00",562836.582030462101102,0.562837000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-24T00:00:00","okay","None","None","08DB230804E55105N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.196611507999904,55.105461500000004]
["glac_bound",391964.000000000000000,"G227101E58242N","2008-05-01T00:00:00",830216.622240299126133,0.830217000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC227101E58242N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.899221638599329,58.242293500000002]
["glac_bound",391967.000000000000000,"G228979E56863N","2008-05-01T00:00:00",99177779.708087831735611,99.177800000000005,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG228979E56863N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.099317829384063,56.887060500000004]
["glac_bound",391972.000000000000000,"G221866E59927N","2008-05-01T00:00:00",1760775.818606012035161,1.760780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221866E59927N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.132195103794629,59.926179500000003]
["glac_bound",391978.000000000000000,"G230335E56330N","2008-05-01T00:00:00",272434.439500039385166,0.272434000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230335E56330N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.665917887310684,56.330119999999994]
["glac_bound",391979.000000000000000,"G230260E56042N","2008-05-01T00:00:00",876959.419056253507733,0.876959000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230260E56042N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.744311308253145,56.041454000000002]
["glac_bound",391983.000000000000000,"G230105E55879N","2008-05-01T00:00:00",197690.799513434525579,0.197691000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230105E55879N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.894601188005112,55.878921499999997]
["glac_bound",391986.000000000000000,"G230155E56438N","2008-05-01T00:00:00",279389.674267933063675,0.279390000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230155E56438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.844540602710595,56.437170500000001]
["glac_bound",391989.000000000000000,"G223103E59527N","2008-05-01T00:00:00",3731733.720346522051841,3.731730000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223103E59527N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.895791674649331,59.530950000000004]
["glac_bound",391991.000000000000000,"G227624E57337N","2008-05-01T00:00:00",11083.688456260269959,0.011084000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","Dawes Glacier","None","08CF227624E57337N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.377477977443618,57.336419999999997]
["glac_bound",391992.000000000000000,"G230110E56319N","2008-05-01T00:00:00",162812.614972500421572,0.162813000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230110E56319N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.889488066889157,56.318928999999997]
["glac_bound",391996.000000000000000,"G222900E59293N","2008-05-01T00:00:00",61156598.144501365721226,61.156599999999997,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","Tikke Glacier","None","08AC222900E59293N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.148621523882809,59.273402500000003]
["glac_bound",391999.000000000000000,"G228012E57816N","2008-05-01T00:00:00",198898.561935930774780,0.198899000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228012E57816N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.988055299766700,57.815772000000003]
["glac_bound",392000.000000000000000,"G225661E59337N","2008-05-01T00:00:00",1459400.381211868487298,1.459400000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225661E59337N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.328212822972745,59.340756999999996]
["glac_bound",392007.000000000000000,"G222493E59628N","2008-05-01T00:00:00",410927.444492319249548,0.410927000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222493E59628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.502131831880320,59.628421000000003]
["glac_bound",392011.000000000000000,"G222292E59546N","2008-05-01T00:00:00",212132.661909715156071,0.212133000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222292E59546N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.706026472503595,59.546407000000002]
["glac_bound",392015.000000000000000,"G226596E58552N","2008-05-01T00:00:00",52807.953572778533271,0.052808000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226596E58552N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.404305510568037,58.551721000000001]
["glac_bound",392024.000000000000000,"G230276E55686N","2008-05-01T00:00:00",447854.541756140009966,0.447855000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230276E55686N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.727039578288327,55.688698500000001]
["glac_bound",392028.000000000000000,"G224729E59783N","2008-05-01T00:00:00",105961.515149293642025,0.105962000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA224729E59783N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.269327317933516,59.783389999999997]
["glac_bound",392031.000000000000000,"G222841E59505N","2008-05-01T00:00:00",730027.342293746769428,0.730027000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC222841E59505N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.166259053254009,59.504292500000005]
["glac_bound",392040.000000000000000,"G230448E56281N","2008-05-01T00:00:00",2128781.607994945254177,2.128780000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230448E56281N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.559873836895292,56.283168500000002]
["glac_bound",392043.000000000000000,"G225556E59316N","2008-05-01T00:00:00",435311.621805801114533,0.435312000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225556E59316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.443906453445550,59.316172499999993]
["glac_bound",392048.000000000000000,"G229227E57159N","2008-05-01T00:00:00",2852818.176264041569084,2.852820000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229227E57159N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.771035445402447,57.162476499999997]
["glac_bound",392051.000000000000000,"G229175E57014N","2008-05-01T00:00:00",1284004.838098705979064,1.284000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229175E57014N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.831939468240932,57.017133999999999]
["glac_bound",392063.000000000000000,"G230208E54820N","2008-05-01T00:00:00",411629.063647030910943,0.411629000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230208E54820N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.792525851318402,54.820442499999999]
["glac_bound",392067.000000000000000,"G230707E55567N","2008-05-01T00:00:00",121694.924602904065978,0.121695000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230707E55567N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.292197614250085,55.568246500000001]
["glac_bound",392068.000000000000000,"G229230E56626N","2008-05-01T00:00:00",1563576.231212818296626,1.563580000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229230E56626N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.758851758435412,56.627458000000004]
["glac_bound",392086.000000000000000,"G230852E57278N","2008-05-01T00:00:00",2699300.816510209813714,2.699300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CC230852E57278N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.144925742783528,57.279048500000002]
["glac_bound",392087.000000000000000,"G230296E56993N","2008-05-01T00:00:00",1190469.254343094537035,1.190470000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230296E56993N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.704076706998308,56.993697999999995]
["glac_bound",392090.000000000000000,"G230776E57050N","2008-05-01T00:00:00",210811.317396158468910,0.210811000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230776E57050N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.223899936619716,57.049622999999997]
["glac_bound",392097.000000000000000,"G226300E59020N","2008-05-01T00:00:00",450759.898032916593365,0.450760000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226300E59020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.700341039783439,59.019916500000001]
["glac_bound",392099.000000000000000,"G230115E56472N","2008-05-01T00:00:00",4789702.323432444594800,4.789700000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230115E56472N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.890721545933275,56.470849000000001]
["glac_bound",392103.000000000000000,"G227997E57196N","2008-05-01T00:00:00",2219120.610246033873409,2.219120000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF227997E57196N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.002664481282437,57.205124499999997]
["glac_bound",392104.000000000000000,"G230147E56279N","2008-05-01T00:00:00",625632.518674226826988,0.625633000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230147E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.851940328386888,56.283176499999996]
["glac_bound",392112.000000000000000,"G230524E57152N","2008-05-01T00:00:00",233153.006453788344515,0.233153000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230524E57152N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.475934778968679,57.152003999999998]
["glac_bound",392114.000000000000000,"G226844E58628N","2008-05-01T00:00:00",1392946.440377673832700,1.392950000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226844E58628N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.155581022978197,58.629376999999998]
["glac_bound",392117.000000000000000,"G230220E56967N","2008-05-01T00:00:00",269867.442902254231740,0.269867000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230220E56967N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.780144517434962,56.967662500000003]
["glac_bound",392119.000000000000000,"G228705E57354N","2008-05-01T00:00:00",1836188.048391582677141,1.836190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228705E57354N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.295201601950339,57.354444999999998]
["glac_bound",392128.000000000000000,"G226722E58625N","2008-05-01T00:00:00",181180.140103833866306,0.181180000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226722E58625N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.276466206118670,58.624395000000000]
["glac_bound",392131.000000000000000,"G230559E54852N","2008-05-01T00:00:00",1316959.683023990364745,1.316960000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230559E54852N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.447005109157089,54.853386999999998]
["glac_bound",392135.000000000000000,"G230533E56271N","2008-05-01T00:00:00",141706.816998555208556,0.141707000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230533E56271N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.465274794570519,56.272406000000004]
["glac_bound",392136.000000000000000,"G228081E57422N","2008-05-01T00:00:00",317671.716419465432409,0.317672000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228081E57422N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.919145922945233,57.420479499999999]
["glac_bound",392138.000000000000000,"G231157E57509N","2008-05-01T00:00:00",323468.884242048952729,0.323469000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231157E57509N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.842060465974953,57.509231000000000]
["glac_bound",392154.000000000000000,"G230267E55722N","2008-05-01T00:00:00",102739.820942000500509,0.102740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230267E55722N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.732677550319494,55.722247000000003]
["glac_bound",392157.000000000000000,"G228764E57199N","2008-05-01T00:00:00",179011.357417461083969,0.179011000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228764E57199N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.236293118436748,57.199315499999997]
["glac_bound",392158.000000000000000,"G230630E55347N","2008-05-01T00:00:00",548772.696419276646338,0.548773000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230630E55347N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.369434315783707,55.348087499999998]
["glac_bound",392161.000000000000000,"G228824E57399N","2008-05-01T00:00:00",800966.489352151402272,0.800967000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228824E57399N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.178705691972027,57.399842000000000]
["glac_bound",392164.000000000000000,"G230435E56020N","2008-05-01T00:00:00",134027.665381787257502,0.134028000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230435E56020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.564208138256362,56.019386499999996]
["glac_bound",392168.000000000000000,"G228346E56854N","2008-05-01T00:00:00",116539.732659562650952,0.116540000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228346E56854N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.652156922017355,56.855421000000000]
["glac_bound",392171.000000000000000,"G230553E55716N","2008-05-01T00:00:00",438584.248896161268931,0.438584000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230553E55716N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.447882727310571,55.717079999999996]
["glac_bound",392172.000000000000000,"G229264E57095N","2008-05-01T00:00:00",599122.737235972774215,0.599123000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229264E57095N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.733229074833787,57.097443999999996]
["glac_bound",392174.000000000000000,"G229867E56279N","2008-05-01T00:00:00",73070.928964203922078,0.073071000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA229867E56279N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.133382860372336,56.279943500000002]
["glac_bound",392176.000000000000000,"G230189E57006N","2008-05-01T00:00:00",155849.054844454774866,0.155849000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA230189E57006N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.810974082906228,57.006136499999997]
["glac_bound",392179.000000000000000,"G230478E56020N","2008-05-01T00:00:00",667541.501154500758275,0.667542000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230478E56020N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.522963675662425,56.021287500000000]
["glac_bound",392181.000000000000000,"G229759E56444N","2008-05-01T00:00:00",837458.878366281744093,0.837459000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DD229759E56444N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.235963087772404,56.448864000000000]
["glac_bound",392184.000000000000000,"G229898E56783N","2008-05-01T00:00:00",1130721.712159683462232,1.130720000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229898E56783N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.101450835322055,56.786822000000001]
["glac_bound",392186.000000000000000,"G225803E59114N","2008-05-01T00:00:00",802844.157883826410398,0.802844000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225803E59114N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.194811466366986,59.114031999999995]
["glac_bound",392188.000000000000000,"G229091E56751N","2008-05-01T00:00:00",78706.034297259349842,0.078706000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229091E56751N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.909151605098771,56.750895999999997]
["glac_bound",392190.000000000000000,"G227517E58140N","2008-05-01T00:00:00",2907430.565577274654061,2.907430000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA227517E58140N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.483011249338603,58.142623000000000]
["glac_bound",392193.000000000000000,"G223996E59955N","2008-05-01T00:00:00",238637.095036897080718,0.238637000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223996E59955N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.003903168872455,59.954830999999999]
["glac_bound",392194.000000000000000,"G230570E55333N","2008-05-01T00:00:00",414825.490855614014436,0.414825000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230570E55333N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.429943339825400,55.333478999999997]
["glac_bound",392195.000000000000000,"G229960E57343N","2008-05-01T00:00:00",208758.163482200441649,0.208758000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229960E57343N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.039192541218625,57.344853999999998]
["glac_bound",392196.000000000000000,"G230510E55919N","2008-05-01T00:00:00",65725.774720849687583,0.065726000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230510E55919N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.490111892053960,55.919402500000004]
["glac_bound",392198.000000000000000,"G225484E59451N","2008-05-01T00:00:00",181924.508317000203533,0.181925000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225484E59451N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.514878677170884,59.451399500000001]
["glac_bound",392199.000000000000000,"G226835E58429N","2008-05-01T00:00:00",135953.949401699908776,0.135954000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BA226835E58429N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.163975396973285,58.428347500000001]
["glac_bound",392200.000000000000000,"G226259E58962N","2008-05-01T00:00:00",15366041.619437521323562,15.366000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226259E58962N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.745442253992280,58.962394500000002]
["glac_bound",392201.000000000000000,"G230384E56403N","2008-05-01T00:00:00",457423.822663158294745,0.457424000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230384E56403N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.616243653846112,56.403132999999997]
["glac_bound",392202.000000000000000,"G230731E56460N","2008-05-01T00:00:00",340478.307140818971675,0.340478000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DA230731E56460N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.268956355656769,56.462233499999996]
["glac_bound",392205.000000000000000,"G229281E56873N","2008-05-01T00:00:00",330204.996787164360285,0.330205000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229281E56873N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.723354264619388,56.874454000000000]
["glac_bound",392207.000000000000000,"G230134E56252N","2008-05-01T00:00:00",51897.403818641192629,0.051897000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DC230134E56252N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.866341791666684,56.252268500000000]
["glac_bound",392208.000000000000000,"G229098E56985N","2008-05-01T00:00:00",75075.149634353947476,0.075075000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229098E56985N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.902438525519017,56.985061000000002]
["glac_bound",392213.000000000000000,"G229969E57143N","2008-05-01T00:00:00",2543865.427527904976159,2.543870000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG229969E57143N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.026876113588685,57.141719999999999]
["glac_bound",392216.000000000000000,"G228763E57067N","2008-05-01T00:00:00",53189.527466274608742,0.053190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228763E57067N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.238686454687013,57.065805499999996]
["glac_bound",392218.000000000000000,"G229921E56752N","2008-05-01T00:00:00",391953.014390188036487,0.391953000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08DA229921E56752N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.077165062417691,56.751998499999999]
["glac_bound",392228.000000000000000,"G228853E56438N","2008-05-01T00:00:00",4454345.894795004278421,4.454350000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228853E56438N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.147515757429289,56.438813500000002]
["glac_bound",392229.000000000000000,"G224029E59844N","2008-05-01T00:00:00",132224.356920987513149,0.132224000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224029E59844N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.971200545826548,59.843028000000004]
["glac_bound",392231.000000000000000,"G225876E59320N","2008-05-01T00:00:00",119728.611657401183038,0.119729000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","09AA225876E59320N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.124541567670576,59.320440500000004]
["glac_bound",392233.000000000000000,"G229406E56316N","2008-05-01T00:00:00",128506.873282604705309,0.128507000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08DD229406E56316N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.591401788631430,56.317572499999997]
["glac_bound",392240.000000000000000,"G228058E57778N","2008-05-01T00:00:00",252026.559202766773524,0.252027000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228058E57778N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.940354124876478,57.776877499999998]
["glac_bound",392243.000000000000000,"G226738E58530N","2008-05-01T00:00:00",396664.885894417529926,0.396665000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BB226738E58530N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.258031782404004,58.526595499999999]
["glac_bound",392247.000000000000000,"G230217E57450N","2008-05-01T00:00:00",1660837.306929701240733,1.660840000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-08-10T00:00:00","okay","None","None","08CG230217E57450N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.785618022112203,57.449123000000000]
["glac_bound",392251.000000000000000,"G222317E59755N","2008-05-01T00:00:00",74300.021142979050637,0.074300000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB222317E59755N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.680899044761247,59.755306500000003]
["glac_bound",392255.000000000000000,"G223290E59594N","2008-05-01T00:00:00",169606.317100436455803,0.169606000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223290E59594N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.708232200062412,59.592642499999997]
["glac_bound",392258.000000000000000,"G224321E59830N","2008-05-01T00:00:00",1155933.430946921929717,1.155930000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC224321E59830N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.668836209715636,59.832777000000000]
["glac_bound",392262.000000000000000,"G226821E58311N","2008-05-01T00:00:00",472942.156929602206219,0.472942000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2006-07-29T00:00:00","okay","None","None","08BC226821E58311N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-133.179941730074859,58.309983000000003]
["glac_bound",392265.000000000000000,"G221610E59918N","2008-05-01T00:00:00",203244.158047796343453,0.203244000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AB221610E59918N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-138.388922732331480,59.918422500000005]
["glac_bound",392268.000000000000000,"G230321E54910N","2008-05-01T00:00:00",87498.126755768418661,0.087498000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230321E54910N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.679703610468380,54.910899000000001]
["glac_bound",392272.000000000000000,"G222234E59579N","2008-05-01T00:00:00",3740332.300929470453411,3.740330000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-09-08T00:00:00","okay","None","None","08AC222234E59579N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-137.759797498954839,59.589342000000002]
["glac_bound",392274.000000000000000,"G224017E59738N","2008-05-01T00:00:00",855773.071375566418283,0.855773000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224017E59738N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.980842134927627,59.735875499999999]
["glac_bound",392275.000000000000000,"G228866E56513N","2008-05-01T00:00:00",507292.942266541649587,0.507293000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2007-09-13T00:00:00","okay","None","None","08CG228866E56513N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.133721423857708,56.514276500000001]
["glac_bound",392282.000000000000000,"G225559E59473N","2008-05-01T00:00:00",1363423.638806370086968,1.363420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AA225559E59473N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-134.441287208915526,59.476053000000000]
["glac_bound",392283.000000000000000,"G223100E59406N","2008-05-01T00:00:00",113830.546289479811094,0.113831000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223100E59406N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.900552074749328,59.405431500000006]
["glac_bound",392286.000000000000000,"G228079E56932N","2008-05-01T00:00:00",1085192.358697162475437,1.085190000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CF228079E56932N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.921336352641902,56.933725499999994]
["glac_bound",392288.000000000000000,"G229027E57182N","2008-05-01T00:00:00",2135420.659873226191849,2.135420000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE229027E57182N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.973668691524125,57.180362500000001]
["glac_bound",392295.000000000000000,"G228747E57524N","2008-05-01T00:00:00",95739.754837127256906,0.095740000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228747E57524N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.254188731862598,57.524407499999995]
["glac_bound",392299.000000000000000,"G227742E57868N","2008-05-01T00:00:00",474935.778834071708843,0.474936000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227742E57868N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.255371951158509,57.868609999999997]
["glac_bound",392301.000000000000000,"G224978E59599N","2008-05-01T00:00:00",635234.381226032855920,0.635234000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08BE224978E59599N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-135.016822304103442,59.597902500000004]
["glac_bound",392302.000000000000000,"G229116E56518N","2008-05-01T00:00:00",361782.384683046664577,0.361782000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CG229116E56518N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-130.882705743305394,56.518888500000003]
["glac_bound",392305.000000000000000,"G223419E59930N","2008-05-01T00:00:00",143346.069136333244387,0.143346000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","08AC223419E59930N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.581881203583464,59.930593000000002]
["glac_bound",392307.000000000000000,"G223891E59886N","2008-05-01T00:00:00",4650017.659066158346832,4.650020000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-09T00:00:00","okay","None","None","09AC223891E59886N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-136.127726416009693,59.894214500000004]
["glac_bound",392316.000000000000000,"G230330E54826N","2008-05-01T00:00:00",214588.213234053924680,0.214588000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08DB230330E54826N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-129.668741910287281,54.826651499999997]
["glac_bound",392317.000000000000000,"G228899E57370N","2008-05-01T00:00:00",2985897.488869435619563,2.985900000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE228899E57370N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-131.101623048319340,57.371960000000001]
["glac_bound",392318.000000000000000,"G227980E57629N","2008-05-01T00:00:00",144263.388628204818815,0.144263000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2005-08-13T00:00:00","okay","None","None","08CE227980E57629N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-132.018450878112446,57.630273000000003]
["glac_bound",392326.000000000000000,"G231291E57513N","2008-05-01T00:00:00",51774.206414407075499,0.051774000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,0.000000000000000,"2004-07-27T00:00:00","okay","None","None","08CA231291E57513N","exists",623.000000000000000,"2009-06-27T00:10:31","; An existing ice polygon layer from a provincial mapping program based on aerial imagery from around 1985 was used as additional information.  Glacier flowsheds were automatically generated based on a 25m DEM to split larger continuous icefields into si",536.000000000000000,"Northern Cordillera","University of Northern British Columbia",0.000000000000000,15,15,50,50,"Bolch, Tobias","Bolch, Tobias",-128.709600074486303,57.514341500000000]