The processes associated with the formation of mountains and basins that may accompany oceanic-continental convergence are endogenous forces resulting from plate movement.
Convergent movement is the movement of tectonic plates that are moving towards each other. Plates that continue to approach, will then meet and give rise to plants. Convergent motion can make oceanic plates and continental plates collide. Continental plates have a higher density or rock density as well as an older age. Meanwhile, the oceanic plate has a lower density and a younger age.
The plate collision causes the edges of the oceanic plates to bend downwards and is forced down into the mantle where it melts. Meanwhile, the continental plates are much harder to bend up and create mountains. The collision produces volcanoes and is known as a subduction zone.
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