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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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Bibliographic Details
Main Authors: Julian A. Dowdeswell, K.A. Hogan, Jeffrey Evans, R. Noormets, Colm O Cofaigh, D. Ottesen
Format: Default Article
Published: 2010
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Online Access:https://hdl.handle.net/2134/13097
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