
Originally Posted by
teach yourself geology by david rothery
This is still controversial, but most geologists would agree on two things, at least. The first is that, attractive as the idea might seem, plate motions are not the direct surface expressions of mantle convection... <snip>.... The plates seem to be moving around more or less independently of this deeper process...<snip>...Perhaps the most likely driving mechanism is that the old, cold edge of a subduction slab, sinking because it is negatively buoyant, drags the rest of the plate with it.