GSI Leveling Data
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https://cmr.earthdata.nasa.gov/search/concepts/C1214590208-SCIOPS.html
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Leveling was conducted on East Ongul Island in order to detect the uplift rate of post-glacial rebound confirmed by the crustal activity of the Antarctic area and the coastal area of Antarctica. Leveling was planned because raised water's edge was observed in the exposed rock area and it was assumed that slopes would be observed both on the west and east sides of Ongul Island due to the difference in uplift rate. All leveling was conducted in conformity with first-order leveling.
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SCIOPS
