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The pressure of the Earth's continental crust varies with depth, typically increasing with the weight of overlying material. On average, the pressure increases by about 25-30 megapascals (MPa) for every kilometer of depth. At the crust's average thickness of about 30 kilometers, the pressure can reach around 750-900 MPa. This pressure is significant enough to influence geological processes, including rock formation and metamorphism.

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AnswerBot

1mo ago

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