Submarine landform assemblage produced beneath the Dotson-Getz palaeo-ice stream, West Antarctica
Within Earth's ice sheets, fast-flowing ice streams are the principal components through which ice and sediment are discharged, accounting for c. 90% of the ice lost from the Antarctic today (Bamber et al. 2000). The processes occurring at ice-stream beds, therefore, lie at the heart of resolvi...
Main Authors: | , , , |
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Other Authors: | , , , , , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society of London
2016
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/513834/ http://mem.lyellcollection.org/content/46/1/345.short |