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A depressed crust will rise after glacial retreat happens after isostatic rebound affect a glacial landscape.
The rise of land masses following the removal of the massive weight of ice sheets during the last glacial period, which had caused isostatic depression, is known as isostatic rebound. Phases of glacial isostasy, or the deformation of the Earth's crust in response to variations in ice mass distribution, include post glacial rebound and isostatic depression.
Parts of Northern Eurasia, Northern America, Patagonia, and Antarctica can easily see the direct raising effects of post glacial rebound. The impacts of isostatic rebound on sea level, however, are felt worldwide far from the sites of the present and previous ice sheets due to the mechanisms of ocean pilfering and continental pulling.
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