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The mantle is a layer of the Earth's interior that lies between the crust and the outer core. It is primarily composed of silicate rocks rich in magnesium and iron. The mantle has a thickness of approximately 2,900 kilometers and makes up about 84% of the Earth's volume.The mantle is divided into two main regions: the upper mantle and the lower mantle. The upper mantle is relatively solid but can flow slowly over long periods of time, a property known as plasticity. This movement of the upper mantle is responsible for tectonic plate motion.The lower mantle, on the other hand, is under high pressure and temperatures which cause it to behave more like a solid. It is believed to be in a semi-solid state due to the presence of partially molten rock called magma.Overall, the mantle plays a crucial role in Earth's dynamics, including plate tectonics, volcanic activity, and heat transfer from within the planet.

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