Glacial geomorphology of the central sector of the Cordilleran Ice Sheet, Northern British Columbia, Canada

• Main Authors: Dulfer, Helen E., Margold, Martin
• Format: Dataset
• Language: unknown
• Published: Taylor & Francis 2021
• Subjects: Medicine; 59999 Environmental Sciences not elsewhere classified; FOS Earth and related environmental sciences; Ecology; FOS Biological sciences; 20199 Astronomical and Space Sciences not elsewhere classified; FOS Physical sciences; Sociology; FOS Sociology; 69999 Biological Sciences not elsewhere classified; Plant Biology; British Columbia; Canada; Ice Sheet
• Online Access: https://dx.doi.org/10.6084/m9.figshare.14779745.v2; https://tandf.figshare.com/articles/dataset/Glacial_geomorphology_of_the_central_sector_of_the_Cordilleran_Ice_Sheet_Northern_British_Columbia_Canada/14779745/2

Northern British Columbia was repeatedly covered by the Cordilleran Ice Sheet (CIS) during the glacial periods. However, its mountainous terrain and remote location have thus far impeded our understanding of the central sector of the ice sheet. The improved resolution of remotely sensed data provides new opportunities to unravel the glacial history of this inaccessible location. Here, we present a comprehensive map of glacial landforms for the central sector of the CIS (55° to 60° N). Seven landform categories were mapped: ice flow parallel lineations, moraines (CIS outlet glacier moraines, Late Glacial moraines and moraines of unknown origin), meltwater channels (lateral and submarginal, subglacial, proglacial, and meltwater channels of unknown origin), kame terraces, eskers (single ridges and esker complexes), perched deltas and subglacial ribs. Collectively, these landforms provide a record of the extent, thickness and behaviour of the CIS, the direction of its movement and pattern of ice retreat.