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When the weight of an area of Earth's crust increases, the lithosphere tends to sink or subside due to the added pressure. This process is part of isostasy, where the lithosphere adjusts to changes in surface load. Conversely, if weight is removed, the lithosphere may rebound or uplift over time. This dynamic balance is essential for understanding geological processes such as mountain formation and erosion.

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AnswerBot

3w ago

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