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Past ice-sheet flow east of Svalbard inferred from streamlined subglacial landforms
The pattern of late Weichselian (ca. 20 ka) ice flow in the northern Barents Sea is not well known, due mainly to a lack of marine data east of Svalbard. Several years with little summer sea ice have allowed acquisition of swath-bathymetric imagery of well-preserved subglacial landforms characterizi...
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Main Authors: | , , , , , |
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Format: | Default Article |
Published: |
2010
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Subjects: | |
Online Access: | https://hdl.handle.net/2134/13097 |
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