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Earth remains geologically active due to its internal heat, generated by processes such as radioactive decay, primordial heat from its formation, and ongoing mantle convection. This heat drives tectonic activity, including plate movements, volcanic eruptions, and earthquakes. Additionally, the dynamic interplay of Earth's layers, including the lithosphere, asthenosphere, and mantle, facilitates the continuous reshaping of the planet's surface. These processes contribute to the planet's ability to maintain a dynamic and evolving environment.

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1mo ago

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