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The Himalayas are the result of a collision between the Eurasian Plate and the Indian Plate is a example of convergent boundaries.
Examples of continent-continent convergent boundaries include the collision of the India Plate with the Eurasian Plate, which resulted in the Himalaya Mountains, and the collision of the African Plate with the Eurasian Plate, which resulted in the Sahara Desert.
Divergent boundaries — where new crust is formed as the plates pull apart.
Convergent boundaries are formed when one plate dives beneath another.
Transform boundaries — where the plates slide horizontally past each other, neither producing nor destroying crust.
A convergent plate boundary is formed when two tectonic plates move toward each other and collide. Convergent plate boundaries are classified into three types: oceanic-oceanic boundaries, oceanic-continental boundaries, and continental-continental boundaries. Because of the density of the plates involved, each one is unique.
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