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The Andes mountains of South America and the Cascade Mountains of North America are some examples of a continental-oceanic plate boundaries.
The Andes Mountains were formed through subduction of the oceanic plate underneath the South American plate.
The mountains that are associated with convergent plate boundaries are mountain ranges or mountain belts. Examples of a mountain range is the Andes.
The Andes mountains are moving because of the plate boundaries it is placed on, and as the plates moves the mountain must move with it.
They were formed by deposition and by convergent boundaries
Stratovolcanoes are common at subduction zones, forming chains along plate tectonic boundaries where oceanic crust is drawn under continental crust. Examples are the Andes and the Aleutian Islands.
andes and himalayas
A convergent boundary between an oceanic plate and a continental plate.
Andes - continental oceanic aleutians - oceanic oceanic North American cordillera - arc continent Appalachians - continental continental
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
They were all formed at convergent boundaries
The Andes were a result of the collision of the Nazca Plate & the South American Plate.