Flow and Retreat of the Late Quaternary Pine Island-Thwaites Palaeo-ice Stream, West Antarctica
[1] Multibeam swath bathymetry and sub-bottom profiler data are used to establish constraints on the flow and retreat history of a major palaeo-ice stream that carried the combined discharge from the parts of the West Antarctic Ice Sheet now occupied by the Pine Island and Thwaites glacier basins. S...
Published in: | Journal of Geophysical Research |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Digital Commons @ University of South Florida
2010
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Subjects: | |
Online Access: | https://digitalcommons.usf.edu/msc_facpub/1522 https://doi.org/10.1029/2009JF001482 https://digitalcommons.usf.edu/context/msc_facpub/article/2572/viewcontent/2009JF001482.pdf |