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Pattern and chronology of glacial Lake Peace shorelines and implications for isostacy and ice‐sheet configuration in northeastern British Columbia, Canada

Hickin, Adrian S., Lian, Olav B., Levson, Victor M., Cui, Yao·2015·Boreas
DOI 10.1111/bor.12110
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Abstract

Recognition of positions of glacial lakes along the margin of continental ice sheets is critical in reconstructing ice configuration during deglaciation. Advances in remote sensing technology (e.g. LiDAR ) have enabled the generation of accurate digital‐elevation models ( DEMs ) that reveal unprecedented geomorphic detail. Combined with geographical information systems, these tools have considerably advanced the mapping and correlation of geomorphic features such as relict shorelines. Shorelines of glacial L ake P eace ( GLP ) developed between the L aurentide and C ordilleran ice sheets in northeastern B ritish C olumbia and northwestern A lberta. Shoreline mapping from high resolution DEMs produced more than 55 500 elevation data points from 3231 shorelines, enabling the identification of four major phases of GLP : Phase I (altitude 960–990 m a.s.l.); Phase II (890–915 m a.s.l.); Phase III (810–865 m a.s.l.); and Phase IV (724–733 m a.s.l.). The timing of Phase II of GLP is estimated by two optical ages of <16.0±2.5 and 14.2±0.5 ka BP . Extensive mapping of the shorelines allows for measuring of glacial isostatic adjustment as ice retreated. Shorelines currently dip to the northeast at around 0.4–0.5 m km −1 . This slope reflects the asynchronous retreat of the C ordilleran ( CIS ) and L aurentide ( LIS ) ice sheets. The relative uplift in the southwest of the study area within the R ocky M ountains and foothills suggests that the Late Wisconsinan ( MIS 2) CIS persisted in the foothill after the LIS lost mass and retreated, or that the Late Wisconsinan CIS was very thick and caused deep crustal loading, which resulted in more uplift in the southwest before reaching equilibrium during, or shortly after deglaciation.

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  • The chronology and viability of the interior corridor remain contentious, but it likely became ice-free between 15.0 and 13.0 ka, and viable sometime thereafter.

    “The chronology and viability of this interior corridor remain contentious, but it likely became ice-free between 15.0 and 13.0 ka, and viable sometime thereafter (Heintzman et al., 2016;Hickin et al., 2015;Jackson et al., 1999;Munyikwa et al., 2017;Pedersen et al., 2016;B. A. Potter et al., 2017).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Hickin et al., 2015

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Metadata

Authors
Hickin, A. S., Lian, O. B., Levson, V. M., & Cui, Y.
Affiliations
  • British Columbia Geological Survey PO Box 9333 Stn Prov Govt Victoria BC Canada V8W 9N3
  • Department of Geography and the Environment University of the Fraser Valley 33844 King Road Abbotsford BC Canada V2S 7M8
  • Department of Earth and Ocean Sciences University of Victoria 3800 Finnerty Road Victoria BC Canada V8P 5C2
Venue
Boreas
Publisher
Wiley
Published
2015-01-30
Volume
44
Issue
2
Pages
288-304
ISSN
  • 0300-9483
  • 1502-3885
DOI
10.1111/bor.12110
Cited by
29
References
0
Language
en
Licence
onlinelibrary.wiley.com/termsAndConditions#vor (vor)
Funders
BC Ministry of Energy and Mines

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