What Triggers Retrogressive Thaw Slumps in the Arctic Coastal Zone?

Retrogressive thaw slumps (RTS) are spectacular lateral thermokarst features occurring in ice-rich permafrost regions. They develop along streams or coastlines and expand inland to form landslide-like U-shaped scars exceeding a kilometer size in selected locations. These slumps are a major source of...

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Bibliographic Details
Main Authors: Lantuit, Hugues, Fritz, Michael, Krautblatter, Michael, Angelopoulos, Michael, Pollard, Wayne H.
Format: Conference Object
Language:unknown
Published: 2013
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/34648/
https://hdl.handle.net/10013/epic.42836