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Monitoring isostatic rebound in Antarctica with the use of continuous remote GPS observations GPS Solutions, 1999 (Ref: 8408)
Category 1: Peer-reviewed literature

A solar-powered GPS receiver has been installed near Beaver Lake, Antarctica, to monitor postglacial isostatic rebound that may be occurring as a result of ice thinning near the Lambert glacier since the last glacial maximum.

Holocene sea-level change and ice-sheet history in the Vestfold Hills, East Antarctica. Earth and Planetary Science Letters, 1998 (Ref: 8457)
Category 1: Peer-reviewed literature

A new Holocene sea-level record from the Vestfold Hills, Antarctica, has been obtained by dating the lacustrine-marine and marine-lacustrine transitions that occur in sediment cores from lakes which were formerly connected to the sea. From an elevation of similar to 7.5 m 8000 years ago…

Estimates of present-day glacial rebound in the Lambert Glacier region, Antarctica Geophysical Research Letters, 1999 (Ref: 8746)
Category 1: Peer-reviewed literature

Changes in the ice load since the time of the Last Glacial Maximum (LGM) contribute to the present-day vertical motion of the Antarctic continent. The observation of these motions will reveal information on the ice load history.

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