Landscape Evolution Triggered by Polycyclic Thermokarst on Herschel Island, Yukon Territory
Retrogressive thaw slumps are a common thermokarst landform in areas of ice-rich continuous permafrost characterized by large massive ground ice bodies, often several metres thick and hundreds of metres in extent. These features can retreat inland by as much as 15-20 metres annually (Figure 1) and a...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2016
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/41118/ https://hdl.handle.net/10013/epic.48704 |