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...

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Bibliographic Details
Main Authors: Angelopoulos, Michael, Pollard, Wayne, Krautblatter, Michael, Lantuit, Hugues
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/41118/
https://hdl.handle.net/10013/epic.48704