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    • The mantle

      • The mantle, a thick layer extending to a depth of 2,890 km, is composed of solid silicates and can be divided into the upper and lower mantle, with a transition zone in between.
      science.howstuffworks.com/layers-earth.htm
  1. Jan 23, 2020 · The inner core has a temperature of up to 4 000℃ and the outer core has a temperature of up to 3 600℃. Between these two layers is a liquid-solid boundary called the Lehmann Discontinuity. This is actually the hottest part of the core. It is as hot as the surface of the Sun!

    • Crust. Temperature: 475 K (∼200°C) at the surface to 1300 K (∼1000°C) Thickness: 25 miles (32 km) for continental crust and 3-5 miles (8 km) for oceanic crust.
    • Upper Mantle. Temperature: 1200 K (∼ 932°C) at the upper boundary with the crust to 1900 K (∼1652 °C) at the boundary with the lower mantle. Thickness: 255 miles (410 km)
    • Lower Mantle. Temperature: 1900 K (∼ 1600°C) in the outer regions which can reach up to 4300 K (∼4000°C) at the bottom. Thickness: 1,400 miles (2,250 km)
    • Outer Core. Temperature: 4,300 K (4,030°C) in the outer regions to 6,000 K (5,730°C) closest to the inner core. Thickness: 1,355 miles (2,180 km) Density: 9,900 – 12,200 kg/m3.
  2. Aug 1, 2023 · The four primary layers are the crust, the mantle, the outer core, and the inner core. However, geologists subdivide these layers into a complex structure that better describes the Earth’s intricate composition and behavior.

  3. Dec 15, 2020 · Inner Core. At the very centre of the Earth is what is known as the Inner Core. Protected by the liquid outer core, mantle, and crust, the inner core is a hot solid ball of highly pressurized nickel and iron, with a temperature of approximately 5,700 K (5,430 °C; 9,800 °F), which is roughly the same as that of the sun.

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  4. The outer core of the earth is bounded by the mesosphere above and the solid inner core below. It is estimated to measure about 1,400 miles thick and it starts about 1,800 miles below the surface of Earth. Unlike other layers of earth, the liquid outer core is completely liquid, through and through.

  5. Earth has three main geological layers based on chemical composition – crust, mantle, and core. The outermost layer is the crust and is composed of mostly silicon, oxygen, aluminum, iron, and magnesium. There are two types of crust, continental and oceanic crust.

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