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.
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.
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.
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
Convergent boundaries can be found where tectonic plates collide. This collision can result in the oceanic plate subducting beneath the continental plate or two continental plates colliding and forming mountain ranges. Examples of convergent boundaries include the west coast of South America, where the Nazca Plate is subducting beneath the South American Plate, and the Himalayas, where the Indian Plate is colliding with the Eurasian 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.
There are three main types of plate boundaries: divergent boundaries (plates move apart), convergent boundaries (plates move towards each other), and transform boundaries (plates slide past each other). Each boundary type can result in different geologic features and events such as earthquakes, volcanic eruptions, and mountain building.
Yes, the Pacific Plate is involved in multiple plate boundaries, including converging boundaries where it moves towards and collides with other plates, such as the North American Plate along the west coast of North America.
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.
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.