The major processes that heat the interiors of the terrestrial worlds are:
A) (1) Heat deposited as the planets were built from planetesimals; (2) heat of accretion; (3) heat that came from the gravitational potential energy of incoming planetesimals.
B) (1) Heat of accretion; (2) heat from convection; (3) heat from thermal radiation.
C)(1) Heat deposited as the planets were built from planetesimals; (2) heat deposited as the planets underwent differentiation; (3) heat released by radioactive decay.
D)(1) Volcanism; (2) tectonics; (3) erosion.