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The process that powers plate tectonics primarily takes place in the Earth's mantle, specifically in the asthenosphere, which is a semi-fluid layer beneath the rigid lithosphere. Convection currents in the mantle drive the movement of tectonic plates as heat from the Earth's core causes the material to rise, cool, and then sink. This continuous cycle of movement leads to the shifting of the plates on the Earth's surface. Additionally, processes at mid-ocean ridges and subduction zones contribute to the dynamics of plate tectonics.

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1mo ago

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