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Plate tectonics is the scientific theory that explains how the Earth’s outermost layer, the lithosphere, is divided into several large, rigid plates that move relative to each other. These plates move because of the convection of the Earth’s mantle, causing geological events such as earthquakes, volcanic eruptions, and mountain-building. Plate tectonics also explains the formation of oceanic and continental crust, the distribution of land masses and sea floor features, and the geological history of the Earth.
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