Activation of high-elevation alluvial fans in the Transantarctic Mountains - a proxy for Plio-Pleistocene warmth along East Antarctic ice margins
Abstract: The PIs propose to address the question of whether ice surface melting zones developed at high elevations during warm climatic phases in the Transantarctic Mountains. Evidence from sediment cores drilled by the ANDRILL program indicates that open water in the Ross Sea could have been a sou...
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Format: | Dataset |
Language: | unknown |
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IEDA: US Antarctic Program Data Center
2016
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Online Access: | http://get.iedadata.org/metadata/iso/600379 |