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  • Crust and Lithosphere
  • The Crust and Lithosphere are 100km layers thick. The temperature fluctuates. Their density is about 2.7 to 3.3 g/cm³. They are composed out of rocks. This layer feels Solid and hard when you go through it. Heat flows through this layer by, Convection.
  • Crust
  • Lithosphere
  • The Upper Mantle is 35-670km layers thick, and the Asthenosphere is 800-200 km layers thick. The temperature fluctuates around 450-900°C. Their density is about 3.2 to 5.7 g/cm³. They are composed of rocks. This layer feels solid and hard when you go through it. Heat flows through this layer by ,Convection. It affect the layer above it because of the hot fluid mantle.
  • Upper Mantle (Asthenosphere)
  • Upper Mantle
  • The Outer Core is 2,400 layers thick. The temperature is 5500°C. The density is about 9.9 to 12.2 g/cm³. It is composed out of iron and nickel. This layer feels like liquid when you go through it. Heat flows through this layer by ,Conduction. It affect the layer above it because of its electrical Conduction.
  • Outer Core
  • Outer Core
  • With all the information we have gathered about the layers, we can explore inside earth and have fun!
  • Inside Earth!
  • The Inner Core is 5,150km layers thick. The temperature is 5500°C. The density is 12.9 g/cm³. It is composed out of iron and nickel. This layer feels like solid metal when you go through it. Heat flows through this layer by, Conduction.
  • Inner Core
  • Inner Core
  • The Lower Mantle is, 670-2900km layers thick. The temperature fluctuates. The density is 5.0 g/cm³. It is composed out of solid rocks. This layer feels solid and soft when you go through it. Heat flows through this layer by, Convection.
  • Lower Mantle
  • Lower Mantle
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