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As one descends into the Earth's interior, both temperature and pressure increase significantly. The temperature rises at an average rate of about 25 to 30 degrees Celsius per kilometer of depth in the crust, while pressure increases due to the weight of the overlying rock. This combination affects the physical and chemical properties of rocks, leading to changes in their behavior, such as increased ductility and the potential for melting at greater depths. These conditions play a crucial role in geological processes, including plate tectonics and magma formation.

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2w ago

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