The mantle is a layer of the Earth between the outer core and the Earth's crust. It is a thick layer of solid and semi-solid rock that makes up the majority of the Earth's volume. The mantle is made up of silicate rocks rich in iron and magnesium, and it is divided into the upper mantle and the lower mantle.
The mantle is composed mainly of silicate minerals, such as olivine, pyroxene, and garnet. These minerals are rich in iron and magnesium, giving the mantle its characteristic density and composition. The upper mantle contains more olivine, while the lower mantle is dominated by high-pressure forms of olivine and other minerals.
The mantle is in a solid state, but it can deform and flow over long periods of time, a process known as mantle convection. This convection is driven by heat from the Earth's core, causing the mantle to circulate and move the tectonic plates on the Earth's surface.
The movement of the mantle is a key factor in the theory of plate tectonics. As the mantle convection causes the tectonic plates to move, it leads to the formation of mountain ranges, earthquakes, and volcanic activity. The heat and pressure from the mantle can also cause the melting of rocks, leading to the formation of magma and the eruption of volcanoes.