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Tectonic plate motion is primarily driven by the heat from the Earth's interior, which creates convection currents in the mantle. These currents cause the semi-fluid asthenosphere beneath the rigid lithosphere to flow, pushing and pulling the tectonic plates above. Additionally, processes like slab pull, where denser oceanic plates sink into the mantle at subduction zones, and ridge push, where plates are pushed apart at mid-ocean ridges, also contribute to their movement. Together, these forces facilitate the dynamic movement of the Earth's tectonic plates.

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