Geochemical and geological evidence for a palaeo-subglacial lake in Pine Island Bay, Antarctica
Subglacial meltwater facilitates rapid ice flow beneath concurrent ice sheets, and there is widespread evidence for a dynamic subglacial water system beneath the Antarctic ice sheet. It steers and affects the pattern of ice flow and is a direct result from boundary processes acting at the base of th...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
International Glaciological Society
2015
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/38968/ https://hdl.handle.net/10013/epic.46226 |