The theory that describes the depression and rebound of continental crust due to adding or removing weight is called:

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The theory that describes the depression and rebound of continental crust due to adding or removing weight is called isostasy. This theory explains how the lithosphere, which includes the crust and the uppermost part of the mantle, behaves in response to changes in the distribution of mass within or on top of it. Isostasy is also responsible for the phenomena of post-glacial rebound, where the land slowly rises after being depressed by the weight of ice sheets during the last ice age.

The Theory That Describes the Depression and Rebound of Continental