Late Pleistocene Interactions of East and West Antarctic Ice-Flow Regimes: Evidence from the McMurdo Ice Shelf
We present new interpretations of deglaciation in McMurdo Sound and the western Ross Sea, with observationally based reconstructions of interactions between East and West Antarctic ice at the last glacial maximum (LGM), 16 000, 12 000, 8000 and 4000 sp. At the LGM? East Antarctic ice from Mulock Gla...
| Main Authors: | , , |
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| Format: | Text |
| Language: | unknown |
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DigitalCommons@UMaine
1996
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| Subjects: | |
| Online Access: | https://digitalcommons.library.umaine.edu/ers_facpub/56 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1055/viewcontent/hughes_42.142.486.pdf |