Title:
Late Cenozoic glacial history of the McMurdo Sound region as derived from surficial sediments, and its relation to DVDP cores (abstract).
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Glacial features in the McMurdo Sound region record two series of major events. One involves flucturations of inland ice in East Antarctica. The second series of events involves repreated northward advances of large grounded ice sheets into the McMurdo sector of the Ross Sea during the last 1.2 million years. Includes discussion of the Taylor and Garwood Valleys.
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no.4:24,
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Bibliographic Citation:
Denton, G.H.Late Cenozoic glacial history of the McMurdo Sound region as derived from surficial sediments, and its relation to DVDP cores (abstract).Dry Valleys Drilling Project Bulletinno.4:24,1974
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