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The temperature rises gradually toward the interior of the Earth primarily due to the decay of radioactive isotopes and the residual heat from the planet's formation. As you move deeper into the Earth, the intense pressure and the heat generated from these processes contribute to the geothermal gradient, which averages about 25-30 degrees Celsius per kilometer of depth in the crust. Additionally, the heat is conducted through the Earth's materials, leading to higher temperatures in the mantle and core. This gradual increase is essential for understanding geological processes and the behavior of materials under extreme conditions.

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1mo ago

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