Glacial isostatic motion in Antarctica from continuous global positioning system measurements: results from the northern transantarctic Mountains and Marie Byrd Land
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Engineering topics
Publications and source records attributed to Ivins, E..
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Assessment of Antarctic rebound is complicated by two issues: (1) The total ice volume at Last Glacial Maximum is contentious, with estimates ranging from just a few meters to several tens of meters equivalent eustatic sea level rise.
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An autonomous GPS array is being implemented in the Transantarctic Mountains, sponsored by NSF and NASA, for the purpose of measuring uplift resulting from post-glacial rebound (PGR).
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Ivins used three relations for estimating the effective viscosity of quartzites and crustal rocks having strong quartz affinity.
The late Holocene glacial moraine chronology in the southernmost South American Andes includes four (sup 14)C dated Neoglacial advances and retreats.
Much of the late-Quaternary ice sheet history in the northern hemisphere is now relatively well-constrained, with the total contributions to eustatic sea level change from North America and Eurasia estimated at roughly 60 (+-12) and 20 (+-7) m, respectively, and with deglaciation bracketed at 22 to 8.5 kyr BP.