Plate Tectonics: Continental Drift, Plate Boundaries and Mountain Formation
1: Plate tectonics explains the movement of the continents and the formation of seas, mountain ranges, islands, volcanoes, earthquakes, and the formation of the oceanic crust and the rock cycle.
It affirms that the lithosphere is not a continuous rock mass but is divided into large blocks called plates. The plates move and displace the continents. At their borders, plates interact by separating, colliding, or rubbing against each other, and this is what causes tectonic activity.
At divergent boundaries, the lithosphere is created as magma rises and solidifies at the center of the spreading ridge. To compensate, an equal amount of oceanic lithosphere is destroyed in subduction zones, so the surface of the Earth remains constant.