The Pleistocene Glacial History of the Lake Wellman Area, Darwin Mountains, Antarctica.
The Darwin and Hatherton Glaciers form a major system that drains a significant portion of the East Antarctic Ice Sheet (EAIS) through the Transantarctic Mountains (TAM) into the Ross Sea. Flow lines along their length demonstrate that they connect back to Dome Cirque on the Polar Plateau. Very litt...
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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University of Canterbury. Geological Sciences
2009
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Online Access: | https://dx.doi.org/10.26021/7447 https://ir.canterbury.ac.nz/handle/10092/3939 |