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A giant impact crater beneath the Wilkes Land ice sheet was first proposed by Richard A. Schmidt in 1962 on the basis of the seismic and gravity discovery of the feature made by the U.S. Victoria Land Traverse in 1959–60 (VLT), and the data provided to Schmidt by John G. Weihaupt, geophysicist of the VLT (Geophysical Studies in Victoria Land, Antarctica, Report No. 1, Geophysical and Polar ...
The magnetic anomalies Bangui and Jackpine Creek, [145] the gravity anomalies Wilkes Land crater and Falkland Islands, [350] and others have been considered as being of impact origin. Bangui apparently has been discredited, [ 25 ] [ 351 ] but appears again in a 2014 table of unconfirmed structures in Africa by Reimold and Koeberl.
Laramie Potts is an American [citation needed] scientist who identified the Wilkes Land mass concentration in Antarctica in collaboration with Ralph von Frese. He is from South Africa. [ citation needed ] He is an associate professor in the School of Applied Engineering and Technology and teaches geomatics ( surveying ) at the New Jersey ...
Ralph R. B. von Frese is an American geophysicist at the Ohio State University who identified the Wilkes Land mass concentration in Antarctica in collaboration with Laramie Potts. In 1969, Frese graduated B.A. cum laude from Park College in physics , mathematics , and German .
The Gravity Recovery and Climate Experiment (GRACE) was a joint mission of NASA and the German Aerospace Center (DLR). Twin satellites took detailed measurements of Earth's gravity field anomalies from its launch in March 2002 to the end of its science mission in October 2017.
The gravity anomaly is the difference between the measured gravity and the normal gravity. ... Wilkes Land crater; Global file usage. The following other wikis use ...
“No Other Land,” a documentary about the resistance of Palestinian activists against forced displacement and settler expansion in the West Bank community of Masafer Yatta, won the Millennium ...
The gravity anomaly at a location on the Earth's surface is the difference between the observed value of gravity and the value predicted by a theoretical model. If the Earth were an ideal oblate spheroid of uniform density, then the gravity measured at every point on its surface would be given precisely by a simple algebraic expression.