The Trench and Andes are on the boundaries of the Nazca and South American Plates. Both of those landforms are the result of a subducting Nazca Plate.
The Trench and Andes are on the boundaries of the Nazca and South American Plates. Both of those landforms are the result of a subducting Nazca Plate.
convergent boundary.
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 San Andreas Fault is part of a transform plate boundary.
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 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 Andes Mountians.
andes mo
A constructive plate boundary, as it pushes land upwards (which formed the mountains)
oceanic-continental convergence
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).
A convergent boundary between an oceanic plate and a continental plate.