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.
The plate boundary along the coast of California is a transform boundary where the Pacific Plate and the North American Plate slide past each other horizontally, causing earthquakes. In contrast, the plate boundary along the west coast of South America is a convergent boundary where the Nazca Plate subducts beneath the South American Plate, leading to volcanic activity and mountain building.
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.
No, the two plates along the coast of South America are not a divergent boundary; they are part of a convergent boundary. The Nazca Plate is subducting beneath the South American Plate, which leads to significant geological activity, including the formation of the Andes Mountains and frequent earthquakes. Divergent boundaries, in contrast, occur where tectonic plates move apart.
The West Coast of Central America is located along a convergent plate boundary where the Cocos Plate is subducting beneath the North American Plate. This subduction zone has led to the formation of the Central American Volcanic Arc and the occurrence of frequent earthquakes in the region.
The two convergent boundaries on the largest plate, the Pacific Plate, are the boundary with the North American Plate along the west coast of North America, and the boundary with the Philippine Sea Plate in the western Pacific Ocean.
Yes, the Andes is a convergent boundary where the South American Plate and the Nazca Plate collide. This collision creates extensive mountain ranges along the western coast of South America.
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.
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.
The Nazca and Antarctic plates share a convergent tectonic boundary where the Nazca Plate is subducting beneath the Antarctic Plate. This results in volcanic activity and the formation of the Andes mountain range along the western coast of South America.
You would expect to find long mountain ranges, such as the Andes, along the west coast of South America. This is because the region is located along a convergent plate boundary where the South American Plate is colliding with the Nazca Plate, leading to intense tectonic activity and the uplift of large mountain ranges.