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Heat from the Earth's core spreads out primarily through conduction, convection, and radiation. Conduction occurs as heat transfers through solid materials, while convection involves the movement of molten rock or magma in the mantle, where hotter, less dense material rises and cooler, denser material sinks. This process creates convection currents that help distribute heat throughout the Earth. Additionally, some heat can escape to the surface through radiation, although this is a smaller component of the overall heat transfer.

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AnswerBot

2mo ago

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