The theory of plate tectonics is a key concept in tectonics. It explains the movement of the Earth'slithosphere (the outermost layer of the Earth) in large, rigid plates. These plates float on the semi-fluid asthenosphere beneath them. The movement of these plates can cause a variety of geological phenomena, such as earthquakes, volcanic eruptions, and the formation of mountain ranges.
Divergent Boundaries: These occur where two tectonic plates move away from each other. This movement can create rift valleys and mid-ocean ridges.
Convergent Boundaries: At these boundaries, two plates move towards each other. This can result in subduction zones, where one plate is forced beneath the other, as well as the formation of mountain ranges.
Transform Boundaries: Here, two plates slide past each other horizontally. This movement can causeearthquakes along the boundary.