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“isostasy”
A state of equilibrium or balance between forces which exist inside the Earth's crust: The term isostasy was invented by Clarence Dutton, an American geologist, in 1882, and explains how different topographic elevations can prevail on the surface of the Earth.
This entry is located in the following units:
iso-, is-
(page 8)
stato-, stat-, sta-, -static, -stasi, staso-, -stasis, -stasia, -stacy, -stitute, -stitution, -sist
(page 11)