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The shifting of the Earth's crust occurs due to the movement of tectonic plates, which float on the semi-fluid asthenosphere beneath them. These plates can interact at their boundaries in several ways: they may collide (convergent boundaries), pull apart (divergent boundaries), or slide past each other (transform boundaries). This movement is driven by forces such as mantle convection, slab pull, and ridge push, leading to geological phenomena like earthquakes, volcanic activity, and the formation of mountains. Over time, these shifts significantly reshape the Earth's surface.

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1mo ago

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