Answer:
There are three types of convergent plate boundary interactions:
Oceanic-Continental Convergence: In this type of convergence, an oceanic plate subducts (dives beneath) a continental plate. The subducting oceanic plate is denser than the continental plate, so it sinks beneath it, forming a deep-sea trench at the boundary. This process causes volcanic activity and earthquake activity in the region.
Oceanic-Oceanic Convergence: In this type of convergence, two oceanic plates collide with each other, and the denser plate subducts beneath the other. This can result in the formation of island arcs, a chain of volcanic islands that forms as a result of the melting and solidification of magma.
Continental-Continental Convergence: In this type of convergence, two continental plates collide with each other. As both plates are equally dense, neither subducts beneath the other. Instead, the two plates crumple and buckle, forming mountains. This process is slow and can take millions of years to complete, resulting in the formation of the highest and longest mountain ranges on the planet.
Step-by-step explanation: