New continental crust forms as a result of plate tectonics, a process ultimately driven by the continuous loss of heat from Earth's interior. Over the period of hundreds of millions of years, tectonic forces have caused areas of continental crust to group together to form supercontinents that have subsequently broken apart. At approximately , one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia at , then finally Pangaea, which also began to break apart at .