Diamond Hill, Darwin Glacier. A proxy for the West Antarctic ice sheet?
In the Ross Sea embayment during the Last Glacial Maximum (LGM, 18-22ka), the grounding line of the West Antarctic Ice Sheet (WAIS) advanced northwards into the Ross Ice Shelf (RIS). This effectively dammed the drainage of the Transantarctic Mountain outlet glaciers and caused significant downstream...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
2010
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Subjects: | |
Online Access: | http://apo.ansto.gov.au/dspace/handle/10238/2339 |