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...
| Main Author: | |
|---|---|
| Other Authors: | |
| Language: | en |
| Published: |
Université d'Ottawa / University of Ottawa
2017
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10393/36613 http://dx.doi.org/10.20381/ruor-20893 |