Age and extent of the Yermak Slide north of Spitsbergen, Arctic Ocean

The extent of the Yermak Slide has been revised on the basis of new acoustic and detailed bathymetric data. The true geometry, with an affected area of at least 10,000 km2 and more than 2400 km3 of involved sedimentary material, puts the Yermak Slide among the largest exposed submarine slides worldw...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Winkelmann, Daniel, Jokat, W., Niessen, F., Stein, R., Winkler, A.
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2006
Subjects:
Arctic
Arctic Ocean
Barents Sea
Kapp Ekholm
Norway
Storegga
Svalbard
Ice Sheet
Sea ice
Svalbard-Barents Sea Ice sheet
Spitsbergen
Online Access:https://oceanrep.geomar.de/id/eprint/11013/
https://oceanrep.geomar.de/id/eprint/11013/1/2005GC001130.pdf
https://doi.org/10.1029/2005GC001130
Description
Summary:The extent of the Yermak Slide has been revised on the basis of new acoustic and detailed bathymetric data. The true geometry, with an affected area of at least 10,000 km2 and more than 2400 km3 of involved sedimentary material, puts the Yermak Slide among the largest exposed submarine slides worldwide, comparable to the Storegga Slide off central Norway. Details from the side's internal structure give evidence for one main slide event during MIS 3 followed by repeated minor events. The timing coincides with the transition of the Kapp Ekholm Interstadial into Glaciation G of Svalbard (Mangerud et al., 1998) and the buildup phase of the Svalbard-Barents Sea Ice Sheet. Thus the slide occurred during a period of falling sea level, increasing ice volume, and, presumably, increasing glaciotectonic activity. The side's geometry and internal physical appearance point to a tectonically induced partial shelf collapse.

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