It is a convergent/destructive plate boundary.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
The crustal plate found between the Nazca Plate and the South American Plate is the Antarctic Plate.
The plate boundary between the Nazca Plate and the South American Plate does produce volcanoes, earthquakes, and tsunamis. Hurricanes have nothing to do with plate boundaries.
It forms a convergent boundary with the South American Plate, divergent.
The South American Plate and the Nazca Plate are separated by a convergent boundary, specifically a subduction zone. This is where the Nazca Plate is forced under the South American Plate, creating the Andes mountain range and causing volcanic activity.
When the Nazca Plate pushes into the South American Plate, it creates a convergent boundary. This leads to subduction, where the denser Nazca Plate is forced beneath the South American Plate. This process can result in the formation of volcanic arcs and earthquakes along the boundary.
It forms a convergent boundary with the South American Plate, divergent.
The Andes are a result of the convergent boundary between the Nazca and South American Plate.
Chaiten is located on the South American Plate. The town of Chaiten in Chile is situated near the boundary between the South American Plate and the Nazca Plate.
The boundary between the Nazca Plate and the South American Plate is a convergent boundary, where the Nazca Plate is subducting beneath the South American Plate. This interaction results in significant geological activity, including the formation of the Andes mountain range and frequent earthquakes. The subduction process also leads to volcanic activity along the western edge of South America.
Answer this question… Subduction of oceanic crust beneath continental crust
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.