It forms a convergent boundary with the South American Plate, divergent.
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.
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 Nazca Plate is a tectonic plate beneath the Pacific Ocean and does not have people living on it. It is located off the western coast of South America and is known for its seismic activity rather than human habitation.
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.
When an oceanic plate subducts beneath a continental plate (convergent boundary) it can create enormous mountains due to the intense compression and uplift of the continental crust. An example of this is the Andes Mountains in South America, formed by the subduction of the Nazca Plate beneath the South American Plate.
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 Nazca plate shares both convergent and divergent boundaries. The Pacific plate has both a transform boundary and divergent boundary
nazca
This earthquake occurred at a convergent boundary - In this region the Nazca and South American plates are converging at a rate of approximately 80mm / year. The dense oceanic crust of the Nazca plate is being forced under or subducted beneath the less dense continental crust of the South American Plate. Please see the related question for further information.
Nazca plate
Chile is located near a special type of thrust fault known as a convergent boundary. Chile is situated on the western coast of the continent of South America, this is the boundary between two tectonic plates, the Nazca plate (which is an oceanic plate) and the South American plate (a continental crustal plate). In this region the Nazca and South American plates are converging at a rate of approximately 80mm / year. The dense oceanic crust of the Nazca plate is being forced under or subducted beneath the less dense continental crust of the South American Plate.
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 Nazca Plate is a tectonic plate beneath the Pacific Ocean and does not have people living on it. It is located off the western coast of South America and is known for its seismic activity rather than human habitation.
Pacific will definitely be involved, but it could rest on a Nazca plate.