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 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.
Answer this question… Subduction of oceanic crust beneath continental crust
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.
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 Andes are a result of the convergent boundary between the Nazca and South American 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 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.
Santiago de Chile is located near the boundary between the Nazca and South American tectonic plates. This boundary is primarily a convergent boundary, where the Nazca Plate is subducting beneath the South American Plate, leading to significant geological activity, including earthquakes and volcanic eruptions in the region. The interaction between these plates has shaped the topography and seismic characteristics of the area surrounding Santiago.
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
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.