Switching of a paleo-ice stream in northwest Svalbard
Ice streams are the fast-flowing zones of ice sheets that can discharge a large flux of ice. The glaciated western Svalbard margin consists of several cross-shelf troughs which are the former ice stream drainage pathways during the Pliocene–Pleistocene glaciations. From an integrated analysis of hig...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2011
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/295589/ |