Want this question answered?
The Puyehue Volcano is on the South America Plate near the Convergent boundary between the South America and Nazca Plates
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.
Galeras Volcano is on the Nazca and the South American plates. It is a convergent boundary and a strato volcano.
glucise
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
Salar de Uyuni was formed from uplift and evaporation of a giant prehistoric lake, caused by the collision of the Nazca and South American Plates.
The Andes Mountains were formed through subduction of the oceanic plate underneath the South American plate.
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.
The Andes were a result of the collision of the Nazca Plate & the South American Plate.