The nazca plate
Nazca
The South American Plate and the Nazca Plate are the two plates that converge to form the Andes mountain range. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift of the Andes through volcanic activity and compression.
The Nazca Plate and the South American Plate are colliding. Because oceanic plates like the Nazca are more dense than continental plates, they are forced below the continental plate and subduct, or flow downward into the mantle at varying degrees of descent from the area of collision!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
Convergent boundaries can be found where tectonic plates collide. This collision can result in the oceanic plate subducting beneath the continental plate or two continental plates colliding and forming mountain ranges. Examples of convergent boundaries include the west coast of South America, where the Nazca Plate is subducting beneath the South American Plate, and the Himalayas, where the Indian Plate is colliding with the Eurasian 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.
north american
north american
north american
north american
The Nazca Plate is subducting beneath the South American Plate along the western coast of South America, leading to the formation of the Andes mountain range through volcanic activity and tectonic forces.
Nazca
The South American Plate and the Nazca Plate are responsible for the creation of the Andes mountain ranges. The Nazca Plate is subducting beneath the South American Plate, causing the formation of the Andes through tectonic activity and volcanic processes.
The South American Plate and the Nazca Plate are the two plates that converge to form the Andes mountain range. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift of the Andes through volcanic activity and compression.
The Pacific Plate is subducting beneath the South American Plate to form the Andes mountain range, not the San Andreas mountain range. The San Andreas Fault is a transform boundary between the Pacific Plate and the North American Plate in California.
The Nazca Plate is an oceanic tectonic plate bordering the South American Plate. These plates are subducting along the Peru-Chile Trench and causing most of the Andean geography we see today as the Nazca Plate is being forced beneath the South American plate.
The Andes mountain range is being formed by the convergence of the Nazca and South American plates. This process involves the oceanic Nazca Plate subducting beneath the South American Plate, leading to the uplift of the Andes mountains.
The Nazca Plate and the South American Plate are colliding. Because oceanic plates like the Nazca are more dense than continental plates, they are forced below the continental plate and subduct, or flow downward into the mantle at varying degrees of descent from the area of collision!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!