On the west coast of South America the denser ballistic ocean crust of the pacific plate is pushed under the lighter granite continental crust of South America. This causes a subduction zone.By Donovan Lopez
Convergent
It is a convergent boundary The subduction of the pacific plate underneath the west coast of South America creates the uplift and volcanoes that is still producing the Andean mountain range. A divergent boundary would create a mid-ocean ridge, or somthing akin to the great rift valley in Africa.
It is a convergent boundary The subduction of the pacific plate underneath the west coast of South America creates the uplift and volcanoes that is still producing the Andean mountain range. A divergent boundary would create a mid-ocean ridge, or somthing akin to the great rift valley in Africa.
California is a slip fault and Chile is a thrust fault.
The western coast of South America is a very good example of an oceanic to continental convergent boundary where the Nazca plate is colliding (and being subducted beneath) the South American plate.
Oceanic crust is destroyed at a convergent boundary where subduction occurs. An example includes the boundary between the Nazca and South American plate on the west coast South America.
In plate tectonics, a convergent boundary, also known as a destructive plate boundary (because of ... 1 Descriptions; 2 Convergent margins ... An example of a continental-oceanic subduction zone is the area along the western coast of South.
a tectonic plate fault-
All three! Convergent, divergent, and transform.
Where an oceanic plate dives under a continental plate (e.g. just offshore the Washington/Oregon coast, creating a line of explosive volcanos just inland).
Mount Rainier, Washington, isn't located on a divergent plate boundary but a convergent one. The Juan de Fuca Plate off the coast is pushing under the northern US and Canada, creating volcanism (such as Mt St Helens).
Located along the entire western coast of South America.