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Internal Structure of the Earth contains the crust, mantle and core.
The Earth's internal structure is made up of four main layers: Inner core: A solid sphere made of iron and nickel metals, about 759 miles (1,221 kilometers) in radius. Outer core: Made of nickel, iron, and molten rock, temperatures here can reach up to 50,000 C. Mantle: Mostly solid rocks and minerals, but punctuated by malleable areas of semi-solid magma. Crust: The outside layer of the Earth, made of solid rock, mostly basalt and granite.
Each layer has a unique chemical composition and physical state, and can impact life on Earth's surface. The Earth's basic structure—crust, mantle, and core—appears to be replicated on the other terrestrial planets.
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