Mountains form at convergent plate boundaries.
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.
Convergent Boundaries.
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.
Volcanic mountains form because of a divergent plate boundary, where two lithospheric plates move apart. Magma rises to the surface through the gap, creating new crust and forming volcanic mountains. An example of this is the East African Rift.
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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.
(A+LS) Convergent Boundary
The collision boundary type modeled the formation of the Himalayan mountains, where the Indian tectonic plate collided with the Eurasian plate. This collision resulted in the uplift and formation of the massive mountain range.
The Cascade Mountains are primarily located along the boundary between the Juan de Fuca Plate and the North American Plate. This boundary is a convergent plate boundary, where the Juan de Fuca Plate is subducting beneath the North American Plate, leading to the formation of the Cascade Range through volcanic activity.
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The Himalayas resulted from the collision of the Indian Plate into the European plate. The softer Indian Plate was forced underneath the harder European Plate, which caused the European Plate to rise up and form the Himalayas.
The Pacific Plate and the North American Plate form a transform plate boundary where they slide past each other horizontally. This boundary is known as the San Andreas Fault system in California.