Open AccessRegional stagnation of the western Keewatin ice sheet and the significance of meltwater corridors and eskers, northern Canada
Author(s) -
D R Sharpe,
Jérôme-Etienne Lesemann,
R D Knight,
Bruce A. Kjarsgaard
Publication year - 2021
Publication title -
canadian journal of earth sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.525
H-Index - 75
eISSN - 1480-3313
pISSN - 0008-4077
DOI - 10.1139/cjes-2020-0136
Subject(s) - meltwater , geology , deglaciation , ice sheet , geomorphology , bedrock , cityscape , erosion , moraine , drumlin , glacier , ice stream , glacial period , physical geography , cryosphere , oceanography , geography , sea ice , art , visual arts
The glacial land system of western Keewatin region, northern Canada, consists of three significant events: (1) regional emplacement of subglacial sediments, mainly till; (2) landscape erosion with development of an integrated, anabranched network of meltwater drainage routes leading to meltwater corridors; and (3) deposition of an extensive array of eskers, and related landforms, within meltwater corridors. Integration of extensive field observations, mapping, and remotely sensed data allow us to link scoured bedrock and till surfaces, truncated drumlins, scour pits, glaciofluvial terraces, boulder lags, and a large-scale network of corridors, as part of regional meltwater erosion events. The network of long (∼100–200 km), relatively wide (∼1–3 km) meltwater corridors record confined subglacial erosion that scoured sediment (and bedrock) prior to glaciofluvial sedimentation (predominately eskers). Despite considerable sediment erosion along meltwater corridors, moraines and other ice-marginal deposits are rarely observed on the western Keewatin landscape. The absence of these features is inconsistent with deglacial models relying on step-wise active retreat of the ice margin. Instead, we propose that deglaciation of the western Keewatin sector of the Laurentide Ice Sheet was predominantly controlled by regional thinning and stagnation. These findings raise fundamental questions about deglacial patterns and processes and thus suggest that further evaluation and revision of existing models of deglacial chronology for this sector of the Laurentide Ice Sheet is needed.