The movement of Earth's tectonic plates is primarily driven by the forces generated by mantle convection, which is the slow circulation of molten rock in the Earth's mantle. This convection is caused by the heat from the Earth's core, leading to the rising and sinking of material. Additionally, slab pull, where denser oceanic plates sink into the mantle at subduction zones, and ridge push, where new material pushes plates apart at mid-ocean ridges, also contribute to plate movement. Together, these forces create the dynamic system that reshapes the Earth's surface over geological time.
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