Late Quaternary Ice-Surface Fluctuations of Beardmore Glacier, Transantarctic Mountains

Abstract Former longitudinal profiles of Beardmore Glacier, an outlet through the Transantarctic Mountains, constrain polar plateau elevations near the center of Antarctica and ice-shelf grouding in the southern Ross Embayment. Three gravel drift sheets of late Quaternary age occur alongside Beardmo...

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Bibliographic Details
Published in:Quaternary Research
Main Authors: Denton, George H., Bockheim, James G., Wilson, Scott C., Leide, James E., Andersen, Björn G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1989
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Online Access:http://dx.doi.org/10.1016/0033-5894(89)90005-7
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