It is called a convergent 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.
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.
The crustal plate found between the Nazca Plate and the South American Plate is the Antarctic Plate.
The East Pacific Rise separates the Nazca Plate from the Pacific Plate.
The Andes mountains were formed from the interaction of the South American Plate and the Nazca Plate, which is a convergent plate boundary. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift and formation of the Andes mountains.
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.
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 is a convergent/destructive plate boundary.
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.
The East Pacific Rise separates the Nazca Plate from the Pacific Plate.
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 Andes mountains were formed from the interaction of the South American Plate and the Nazca Plate, which is a convergent plate boundary. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift and formation of the Andes mountains.
It forms a convergent boundary with the South American Plate, divergent.
It forms a convergent boundary with the South American Plate, divergent.
The Nazca plate has more than one boundary. The western and northern boundaries are divergent as the plates are moving apart from one another. However, the Nazca plate's eastern boundary is convergent as it collides with and subducts under the South American Plate.
The Nazca plate shares both convergent and divergent boundaries. The Pacific plate has both a transform boundary and divergent boundary