island arcs.gif (39562 bytes) This is a convergent plate boundary, the plates move towards each other. The amount of crust on the surface of the earth remains relatively constant. Therefore, when plates diverge (separate) and form new crust in one area, the plates must converge (come together) in another area and be destroyed. An example of this is the Nazca plate being sub-ducted under the South American plate to form the Andes Mountain Chain. The North and South American plates are crashing into the thinner and denser oceanic plates of the Pacific. This drives the oceanic plates deep into the mantle destroying the oceanic plates. This boundary in which an oceanic plate is driven down and destroyed by a continental plate is called a subduction zone.
 

 Himalayas collision.gif (37280 bytes)

Continental/continental collisions is when two tectonic plates with continental crust collide, they buckle and thicken, pushing the continental crust upward. This creates some of the world's tallest mountain ranges, such as the Himalayas.

 

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