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...
Main Authors: | , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/34648/ https://hdl.handle.net/10013/epic.42836 |