The largest and most complex layer of Earth is the mantle, which extends from the base of the crust to the outer core, approximately 2,900 kilometers (1,800 miles) deep. Composed mainly of silicate rocks rich in magnesium and iron, the mantle exhibits a gradual increase in temperature and pressure with depth. It is characterized by its semi-solid state, allowing for slow, convective movements that drive plate tectonics. This dynamic layer plays a crucial role in geological processes, including volcanic activity and the formation of mountain ranges.
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