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The movement of Earth's tectonic plates is primarily driven by the process of mantle convection. In this process, heat from the Earth's core causes the mantle to circulate, creating convection currents that push and pull the plates above. Additionally, slab pull, where denser oceanic plates sink into the mantle at subduction zones, and ridge push, where new crust forms at mid-ocean ridges, also contribute to plate movement. Together, these mechanisms shape the dynamics of plate tectonics.

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1w ago

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