A constructive plate boundary, as it pushes land upwards (which formed the mountains)
The Andes Mountains are an example of mountain building activity at a convergent plate boundary, where the South American plate is colliding with the Nazca plate. This collision has led to the uplift and formation of the Andes mountain range.
The Andes mountain range was formed at a convergent boundary where the South American Plate and the Nazca Plate are colliding. This collision has caused the crust to be uplifted and folded, creating the impressive mountain range we see today.
The Andes Mountain Chain is formed as a result of a convergent plate boundary, the collision of the South American Plate with the Nazca 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 through subduction of the oceanic plate underneath the South American 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.
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.
Yes, the Andes is a convergent boundary where the South American Plate and the Nazca Plate collide. This collision creates extensive mountain ranges along the western coast of South America.
The Andes mountain range is a result of convergent plate boundary formation, where the South American Plate is subducting beneath the Nazca Plate. This collision has led to the uplift and formation of the Andes mountains through various geological processes over millions of years.
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.
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.
No, Volcan Lanin is not located on a plate boundary. It is a stratovolcano located in the Andes mountain range in Argentina, near the border with Chile. This region is associated with subduction of the Nazca Plate under the South American Plate.