crust mantle Outer core Inner core The temperature

crust mantle Outer core Inner core

The temperature of the crust increases as you go deeper into the Earth. It starts out cool, but can get up to 400 degrees C at the boundary between the crust and the mantle

The mantle is a part of a terrestrial planet or other rocky body large enough to have differentiation by density. The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a highly viscous layer between the crust and the outer core. Earth's mantle is a rocky shell about 2, 890 km (1, 800 mi) thick[1]

The outer core is so hot that the metal is always molten, but the inner core pressures are so great that it cannot melt, even though temperatures there reach 6700ºF (3700ºC). The outer core is about 1, 370 miles (2, 200 km) thick. Because the earth rotates, the outer core spins around the inner core and that causes the earth's magnetism.

The inner part of the earth is the core. This part of the earth is about 1, 800 miles (2, 900 km) below the earth's surface. The core is a dense ball of the elements iron and nickel. It is divided into two layers, the inner core and the outer core. The inner core - the center of earth - is solid and about 780 miles (1, 250 km ) thick

Earth structure Done by: I-S-M-A-I-L W-A-Z-E-E-R A-A-D-I-L A-B-D-U-R-A-H-M-A-N Y-U-S-U-F