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...

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Bibliographic Details
Main Authors: Joy, K, Storey, B, Fink, D, Shulmeister, J
Format: Other/Unknown Material
Language:English
Published: 2010
Subjects:
Ice
Online Access:http://apo.ansto.gov.au/dspace/handle/10238/2339