Convergent boundaries, additionally referred to as adverse barriers, are locations wherein two or extra plates flow toward every other. Convergent boundary motion is split into two sorts, subduction and collision, relying on the density of the concerned plates.
where tectonic plates converge, the one with skinny oceanic crust subducts below the only capped by using thick continental crust. A subduction sector includes material scraped off the sea floor near the coast (accretionary wedge) and a series of volcanoes farther inland (volcanic arc)
At convergent barriers, plates pass towards every other. they could push collectively and cause mountain ranges to shape. In different instances, one plate gets pushed down underneath the alternative plate. this may reason for volcanoes.
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