Mega-Scale Glacial Lineations and Grounding-Zone Wedges in Prydz Channel, East Antarctica
The Prydz Bay continental shelf was sculpted by the Lambert Glacier–Amery Ice Shelf system, a large outlet glacier that drains 16% of the East Antarctic Ice Sheet (Allison 1979; Fig. 1a). Prydz Channel (71–73° E; Fig. 1b) is a NW-trending cross-shelf trough (500–700 m deep) in western Prydz Bay that...
Published in: | Geological Society, London, Memoirs |
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Main Authors: | , , , |
Format: | Book Part |
Language: | unknown |
Published: |
Digital Commons @ University of South Florida
2016
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Subjects: | |
Online Access: | https://digitalcommons.usf.edu/msc_facpub/594 https://doi.org/10.1144/M46.110 |