(Table 4) Erosion since slump initiation of retrogressive thaw slumps on Herschel Island and King Point

Estimated based on the slope angle of stabilised slump floors and the estimated position of the bottom of the massive ice layer.

Bibliographic Details
Main Authors: Lantuit, Hugues, Pollard, Wayne H, Couture, Nicole, Fritz, Michael, Schirrmeister, Lutz, Meyer, Hanno, Hubberten, Hans-Wolfgang
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2012
Subjects:
Event label
Latitude of event
Longitude of event
Description
Surface elevation
Distance
Age model
Age, standard deviation
Multiple investigations
CA-Land_2006_YukonCoast
AWI Arctic Land Expedition
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
Arctic
Herschel Island
King Point
Ice
permafrost
Online Access:https://dx.doi.org/10.1594/pangaea.810042
https://doi.pangaea.de/10.1594/PANGAEA.810042
Description
Summary:Estimated based on the slope angle of stabilised slump floors and the estimated position of the bottom of the massive ice layer.

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