The core is the hottest part of the Earth. Heat is radiated out towards the surface (crust), with heat energy spreading through the mantle, where it creates molten magma. The hot magma moved around in the mantle due to a process called convection. Heated magma rises towards the crust where it begins to cool, becomes more dense and sinks again. Once it reaches the core, it is reheated and the process continues. These convection currents are responsible for forcing the floating tectonic plates to move.