The Andes are a result of the convergent boundary between the Nazca and South American Plate.
Oceanic - oceanic divergent boundary and Continental - oceanic divergent boundary.
Divergent plate boundary: The Mid-Atlantic Ridge where the Eurasian Plate and North American Plate are moving apart. Convergent plate boundary: The Andes Mountains where the South American Plate is colliding with the Nazca Plate. Transform plate boundary: The San Andreas Fault in California where the Pacific Plate and North American Plate are sliding past each other.
convergent boundary.
The Villarrica Volcano is located on a convergent boundary where the South American tectonic plate is subducting beneath the Nazca plate. This subduction leads to the formation of the Andes mountain range and associated volcanic activity.
Divergent
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.
Peru is located along a convergent boundary where the Nazca Plate is subducting beneath the South American Plate. This tectonic interaction leads to significant geological activity, including earthquakes and volcanic eruptions in the region. The Andes mountain range, which runs along Peru's western edge, is a direct result of this convergent boundary process.
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.
No, the two plates along the coast of South America are not a divergent boundary; they are part of a convergent boundary. The Nazca Plate is subducting beneath the South American Plate, which leads to significant geological activity, including the formation of the Andes Mountains and frequent earthquakes. Divergent boundaries, in contrast, occur where tectonic plates move apart.
There are three main types of plate boundaries: divergent boundaries (plates move apart), convergent boundaries (plates move towards each other), and transform boundaries (plates slide past each other). Each boundary type can result in different geologic features and events such as earthquakes, volcanic eruptions, and mountain building.
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.