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 nazca plate
Transform boundary. It's transform boundary because there are mainly earthquakes in the west coast so, the transform boundary is when the plates move horizontally past each other which cause earthquakes.
The Andes were a result of the collision of the Nazca Plate & the South American Plate.
Probably Ann from Cycle 15.
What countries in South America have snakes?
Canada
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.
Convergent
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.
divergent boundary
A simple answer is: Colliding and subductive as they consume the Earth as a portion of the plate is moved beneath another plate and remelted into magma. A common example is the western side of South America where the denser oceanic Pacific Plate moves under the less dense continental South American Plate. The Pacific melts into magma and the South American rises to form the Andes Mts. with a great deal of volcanic activity.
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.
The Puyehue Volcano is on the South America Plate near the Convergent boundary between the South America and Nazca Plates
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.
El Chinchon is not a shield volcano it is a lava dome volcano. Lava dome volcanoes have a layering of lava that fans up and outward in the center.
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.
The mid-oceanic ridge in the Atlantic Ocean is one. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries. This map shows the tectonic plate boundaries. With the help of the legend, you should see where all the divergent, spreading boundaries are: http://www.globalchange.umich.edu/globalchange1/current/lectures/evolving_earth/tectonic_map.jpg Like the word "convergent" implies, convergent boundaries occur where tectonic plates converge, or come together. There are convergent boundaries on the west coast of South America, along the coast of Oregon and Washington in the Pacific Northwest of the US, along the southern edge of the Aleutian Islands of Alaska, along the eastern edge of Japan. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries.