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The four layers typically refer to the layers of the Earth: the crust, mantle, outer core, and inner core. The crust is the thin outer layer, the mantle is a thick, semi-solid layer beneath the crust, the outer core is liquid and composed mainly of iron and nickel, and the inner core is solid, also made primarily of iron and nickel. These layers vary in composition, state, and temperature, contributing to geological processes such as plate tectonics and volcanic activity.

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