Glacial geomorphology and its links to ice sheet thicknesses, Diamond Hill, Transantarctic Mountains.
An understanding of how the Antarctic continent has reacted to past climates is necessary to accurately predict the response of its ice sheets to current and future climate changes. The thickness and proximity of the peripheral ice to the continental margin are key to the discussion and relate direc...
| Main Authors: | , , , |
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| Format: | Other/Unknown Material |
| Language: | English |
| Published: |
2009
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| Subjects: | |
| Online Access: | http://apo.ansto.gov.au/dspace/handle/10238/2746 |