The type of mountain that is formed by colliding continents is the upward mountain.
Fold mountains are usually formed when two tectonic plates carrying continents collide, causing the crust to buckle and fold, resulting in the formation of mountain ranges. The collision forces the rocks to be pushed upwards, forming large mountain belts with distinct fold patterns. Examples of fold mountains include the Himalayas and the Alps.
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.
Pine Mountain was formed by the tectonic forces associated with the collision of the African and North American plates. The intense compression caused by these forces resulted in the uplifting and folding of the rock layers that make up Pine Mountain.
It depends on the type of plates coming together but two continental plates will form a mountain chain. An example would be the Indian sub-continent colliding with Asia to form the Himalayas.
Island arc mountains are formed when one oceanic plate is subducted beneath another oceanic plate, creating a volcanic island arc.
Andean
Fold mountains.
A tectonic boundary, such as a mountain range or a deep ocean trench, can divide continents. These boundaries are formed by the movement of tectonic plates and can create physical barriers between landmasses.
Folded mountains. These are formed when tectonic plates clashed together and formed in and up.
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A volcanic mountain.