Retrogressive Thaw Slumps: Indicators of Holocene Climate Changes in the Richardson Mountains-Peel Plateau, Northwestern Canada

The ongoing climate warming is expected to increase thermokarst activity and their impacts by inducing permafrost degradation and active layer deepening. A retrogressive thaw slump, which represents the most dynamic thermokarst landform, was investigated in the Richardson Mountains-Peel Plateau regi...

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Bibliographic Details
Main Author: Frappier, Roxanne
Other Authors: Viau, André Ernest J.
Format: Thesis
Language:English
Published: Université d'Ottawa / University of Ottawa 2017
Subjects:
Ice
Online Access:http://hdl.handle.net/10393/36613
https://doi.org/10.20381/ruor-20893