Controversy over the exact nature of mantle convection makes the linked evolution of Earth 's heat budget and the dynamics and structure of the mantle difficult to unravel. There is evidence that the processes of plate tectonics were not active in the Earth before 3.2 billion years ago, and that early Earth 's internal heat loss could have been dominated by advection via heat - pipe volcanism. Terrestrial bodies with lower heat flows, such as the Moon and Mars, conduct their internal heat through a single lithospheric plate, and higher heat flows, such as on Jupiter 's moon Io, result in advective heat transport via enhanced volcanism, while the active plate tectonics of Earth occur with an intermediate heat flow and a convecting mantle.
how does heat inside earth cause plate tectonics
with an intermediate heat flow and a convecting mantle