The Himalayas, Andes, and Alps are examples of mountain ranges formed by continental-continental convergent boundaries. These boundaries occur when two continental plates collide, resulting in intense folding, faulting, and uplift of the Earth's crust to create mountain ranges.
No, the Alps are not a divergent boundary. The Alps are a mountain range formed from the collision of the African and Eurasian tectonic plates, a result of convergent boundary activity.
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.
Intercontinental convergent boundary.
No, Teide is not formed on a convergent plate boundary. It is a volcano located on the island of Tenerife, which is part of the Canary Islands, formed by a hotspot beneath the Earth's crust, creating a volcanic hotspot.
The physical feature that formed the northeast boundary of Asoka's empire was the Himalayan mountain range.
Continental Collision Boundary
it is a convergent continental continental
continental continental convergent boundary
A convergent or constructive continental boundary formed the Himalayas.
convergent boundary ^.<
Continental Collision Boundary
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The Himalayas are formed at a continental-continental convergent boundary.The Andes are formed at an oceanic-continental boundary.
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
Continental Collision Boundary
The Andes Mountains were formed through subduction of the oceanic plate underneath the South American plate.
A convergent boundary with no subduction is a continental-continental boundary. Because oceanic crust is denser than continental crust, it is always the subducting plate in a oceanic-continental boundary. In an oceanic-oceanic boundary, one of the plates will subduct, depending on several factors. Continental plates are thicker and less dense than oceanic plates, and when they converge, they push up the area where the plates meet, forming mountain ranges (note that this is not the only, or even the predominant, method of mountain formation). The Himalayas are being formed as a result of a continental-continental boundary.