Continental crust.
Continental crust.
At the boundary where the South American Plate meets the Nazca Plate, you can find subduction zones. The oceanic Nazca Plate is being forced beneath the continental South American Plate, forming a destructive plate boundary. This collision results in the formation of deep ocean trenches and the Andes mountain range due to the intense tectonic forces at work.
The crustal plate found between the Nazca Plate and the South American Plate is the Antarctic Plate.
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 Andes Mountain Range is a result of the Nazca Plate subducting under the South American Plate.
The Nazca Plate is more dense than the South American Plate. This density difference is one of the reasons why the Nazca Plate is subducting beneath the South American Plate along the Peru-Chile Trench.
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.
Ecuador is located at the boundary of the South American Plate and the Nazca Plate. The subduction of the Nazca Plate beneath the South American Plate causes frequent earthquakes and volcanic activity in Ecuador.
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.
The Andes were a result of the collision of the Nazca Plate & the South American Plate.
The South American Plate.
Nazca