Solution:Plate tectonic is a scientific theory describing the large scale motion of seven large plates and the movements of a large number of smaller plates of the Earth’s lithosphere.
The lithosphere is the rigid outermost shell of a planet (the crust and upper mantle), is broken into tectonic plates. Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere each topped by its own kind of crust.
Tectonic plates are able to move because the Earth’s lithosphere has greater mechanical strength than the underlying asthenosphere (viscous, weak, ductile region of upper mantle of the Earth). Plato boundaries are the edges where two plates meet.
Most geologic activities, including volcanoes, earthquakes and mountain building occurs at plate boundaries. Divergent plate boundaries are area where plate move away from each other forming either mid-oceanic ridges or rift valley. Earthquakes are common at mid-ocean ridges.
A convergent plate boundary is an area where two or more lithosphere collide. When oceanic crust converges with continental crust, the denser oceanic plate plunges beneath the continental plate.
This process called subduction, occurs at the oceanic trenches. The entire region is called subduction zone. This zone has a lot of intense earthquakes and volcanic eruptions. The subducting plates cause melting in the mantle.