What are the movement of plates in various directions?

Tectonic plates can move in several directions relative to one another: they can diverge, where plates move apart, such as at mid-ocean ridges; converge, where plates collide, leading to subduction or mountain formation; and transform, where plates slide past each other horizontally, like the San Andreas Fault. These movements result from convection currents in the Earth's mantle and are responsible for geological phenomena like earthquakes, volcanic activity, and the creation of mountain ranges.