The document discusses convection in the mantle and how it relates to plate tectonics. It explains that convection currents, along with ridge push and slab pull, are responsible for the movement of tectonic plates. Ridge push occurs as new ocean crust is formed at mid-ocean ridges, lifting and pushing the plates apart. Slab pull results from the subduction of ocean plates at trenches, where cooling slabs pull the plates into the mantle.