Scientific American article on the same topic:
http://www.scientificamerican.com/ar...B7809EC588F2D7
There are three main sources of heat in the deep earth: (1) heat from when the planet formed and accreted, which has not yet been lost; (2) frictional heating, caused by denser core material sinking to the center of the planet; and (3) heat from the decay of radioactive elements. ....