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It isn't because they don't.

For any solid to regain its original form after the deforming stress has been removed, it has to be strained only within its elastic limit. That is as true of hard rock as it is of spring-steel or rubber.

Rocks have very low limits of elasticity and though they can deform under pressure, to a point, most geological processes take them far beyond their elastic limits so they can never regain their original shape.

The only significant, and it is significant, exception is that of isostatic rebound in the crust, usually after an Ice Age ice-sheet has thawed.

Scandinavia is still experiencing lingering traces of such rebound following the last glaciation of the present Ice Age. Given that the ice-sheet was up to 3km, and taking the mean density of ice as 0.9T/m3, I'll leave you to look up the area in sq km enclosed by Scandinavia and the Baltic, and thus calculate the maximum load on that area of continental crust. You'll find using index notation helps sums like that, with all those 10-powers!

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11y ago
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11y ago

elastic rebound

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8y ago

Elastic Rebound

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