Earth's structure consists of several layers: the crust, mantle, outer core, and inner core. The movement of tectonic plates within the Earth's lithosphere, which includes the crust and the upper mantle, leads to the formation of continents and ocean basins through processes such as continental drift and seafloor spreading. Mountain ranges arise primarily from the collision and convergence of these tectonic plates, resulting in uplift and deformation. Thus, the dynamic interactions of Earth's layers play a crucial role in shaping its surface features.
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