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There are three types of convergent boundaries: oceanic-oceanic, oceanic-continental, and continental-continental.

An example of continental-continental is the San Andreas Fault in California.

An example of oceanic-continental is the Peru-Chile Trench.

An example of oceanic-oceanic is almost anywhere in the ocean. Because the tectonic plates are continuously moving, although they may be moving slowly, new boundaries are formed often. Thus, oceanic-oceanic boundaries are constantly forming. A specific example would be in the western Pacific Ocean. There is a tangle of arcs in the Indian ocean; there's also the Caribbean and South Sandwich Island arcs.

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