Answer:
The convergent plate boundary is when two plates move towards each other. In this case it has three possibilities:
An oceanic-continental convergent: In this case the the oceanic plate goes beneath the continental in a subduction zone. And due to this process, the continental crust crumples and forms mountains.
An oceanic-oceanic convergent: Here the denser plate goes beneath the other in a subduction zone.
A continental-continental convergent: And in this case the thickness of the crust doubles as the convergent makes mountains.
The divergent plate boundary is when two plates move away from each other. This type of plate boundaries happens between the same plate type, this way it has two possibilities:
An oceanic-oceanic divergent: In this case when two plates goes apart, the magma from the mantle goes up to fill the gap that the separation made.
A continental-continental divergent: And here it’s characterized by rift valleys.
The third and last type is the transform plate boundary. And this one happens when two plates slide along each other horizontally.
Explanation:
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