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The Earth's structure consists of four main layers: the crust, mantle, outer core, and inner core. The crust is the thinnest layer, ranging from about 5 to 70 kilometers thick, characterized by solid rock and varying compositions. The mantle, extending approximately 2,900 kilometers deep, is semi-solid and convective, driving plate tectonics. The outer core, around 2,200 kilometers thick, is liquid and composed mainly of iron and nickel, while the inner core, with a radius of about 1,220 kilometers, is solid and extremely hot, also made primarily of iron and nickel.

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