The process of heat transfer thought to be responsible for the movement of the lithospheric plates on the surface of the Earth is mantle convection. In this process, heat from the Earth's interior causes the mantle material to circulate. Hot, less dense material rises toward the surface, while cooler, denser material sinks. This convective movement in the mantle generates the forces that drive the tectonic plates on the lithosphere.
The process of heat transfer thought to be responsible for the movement of the lithospheric plates on the surface of the earth is
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