Most geologists believe that the movement of Earth's tectonic plates is primarily driven by convection currents in the mantle. As hot magma rises toward the surface, it cools and sinks back down, creating a cyclical motion that helps to push and pull the plates above. Additionally, the process of slab pull, where dense oceanic plates sink into the mantle at subduction zones, and ridge push, where new material is added at mid-ocean ridges, also contribute to plate movement. These mechanisms work together to shape the dynamic nature of Earth's surface.
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