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Subglacial conditions at a sticky spot along Kamb Ice Stream, West Antarctica

Open-File Report 2007-1047-SRP-097
By:  and 
https://doi.org/10.3133/ofr20071047SRP097

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Abstract

We present the results of a seismic reflection experiment performed transverse to flow a few tens of kilometers above the main trunk of Kamb Ice Stream, West Antarctica, where we image a basal high surrounded by variable subglacial conditions. This high rises as much as 200 m above the surrounding bed, acting as a major sticking point that resists fast flow. Application of the amplitude variation with offset (AVO) seismic technique has highlighted regions of frozen sediments along our profile, suggesting that the ice stream is experiencing basal freeze-on in the region. The bedrock high appears to be at least partially draped in sediment cover, with a concentrated area of weak, dilatant till flanking one edge. This dilatant till is further dispersed along our profile, though it does not possess enough continuity to maintain streaming ice conditions. These results support the hypothesis that the ongoing shutdown of Kamb Ice Stream is due to a loss in continuous basal lubrication.

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Publication type Report
Publication Subtype USGS Numbered Series
Title Subglacial conditions at a sticky spot along Kamb Ice Stream, West Antarctica
Series title Open-File Report
Series number 2007-1047-SRP-097
DOI 10.3133/ofr20071047SRP097
Year Published 2007
Language English
Publisher U.S. Geological Survey
Publisher location Reston, VA
Description 5 p.
Larger Work Type Report
Larger Work Subtype USGS Numbered Series
Larger Work Title Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007
Other Geospatial Antarctica
Additional Online Files (Y/N) N
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