There are three types of plate movement. Plates can move apart (diverge), they can move alongside each other (at a transform plate boundary) and they can move towards each other (converge). At a converging boundary between two continental plates, the plates collide, creating high mountains. At a converging boundary, between an oceanic plate and a continental plate, the oceanic plate will subduct. Tectonic plates move because convection currents carry them along.