Final answer:
Tectonic plates can move in three main ways: divergent, convergent, and transform boundaries. Each type of boundary creates different geological features.
Step-by-step explanation:
Tectonic plates can move relative to each other in three main ways: divergent, convergent, and transform boundaries. In divergent boundaries, plates move away from each other, creating a gap where magma rises to form new crust. This process can lead to the formation of mid-ocean ridges and rift valleys.
In convergent boundaries, plates collide, and one plate can be forced beneath the other, creating subduction zones. This can result in the formation of mountain ranges and ocean trenches. In transform boundaries, plates slide past each other horizontally, causing earthquakes along the fault line.