The document summarizes the structure of the Earth, describing its three main layers - the core, mantle, and crust. The mantle is very hot at 1200°C, very thick at 2900km, and under great pressure. It moves due to convection currents. The crust varies in thickness between 8-75km depending on if it is oceanic or continental crust, with oceanic crust being heavier basalt and continental crust being lighter granite. The crust is broken into tectonic plates that move.