Ground ice, organic carbon and soluble cations in tundra permafrost soils and sediments near a Laurentide ice divide in the Slave Geological Province, Northwest Territories, Canada

The central Slave Geological Province is situated 450–650 km from the presumed spreading centre of the Keewatin Dome of the Laurentide Ice Sheet, and it differs from the western Canadian Arctic, where recent thaw-induced landscape changes in Laurentide ice-marginal environments are already abundant....

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Bibliographic Details
Published in:The Cryosphere
Main Authors: R. Subedi, S. V. Kokelj, S. Gruber
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Ice
Online Access:https://doi.org/10.5194/tc-14-4341-2020
https://doaj.org/article/54284ec982b94fee8d1ee4c4145b7933