A2-1 Earth’s Layered Structure

The solid surface of the Earth that we all stand on is only one of the layers of the Earth. Studies of earthquakes and how they transmit their energy (see Unit E – Earthquakes for further details) have revealed that the Earth is composed of three different layers, each with distinct differences in chemical composition. These three layers are the crust, the mantle, and the core.

The mantle can be further subdivided into the upper mantle and the lower mantle due to the change in temperature, pressure and plasticity the further you move down to the core.

The structure of the Earth’s interior is often compared to a hard-boiled egg.