A mountain range.
The density of the tectonic plates involved determines whether a subduction zone or collision zone is formed at a destructive plate margin. If one plate is denser than the other, it will subduct beneath the other plate, forming a subduction zone. If the plates have similar densities, they will collide and form a collision zone.
One example of a collision zone is the San Andreas Fault in California, where the Pacific Plate slides past the North American Plate. This interaction results in frequent earthquakes and the potential for significant seismic activity.
A subduction zone and a collision zone are the same place, a collision just happens earlier, when the crusts of the two plates are interacting. Later, when the crust of one plate is being forced under the crust of another plate into the mantle, it becomes a subduction zone.
Volcanic mountains are not formed by plate collision. These mountains are created when magma from within the Earth's mantle rises to the surface and solidifies.
They are formed by the continental contienal plates
A mountain range.
The density of the tectonic plates involved determines whether a subduction zone or collision zone is formed at a destructive plate margin. If one plate is denser than the other, it will subduct beneath the other plate, forming a subduction zone. If the plates have similar densities, they will collide and form a collision zone.
By the means of plate tectonics at a zone of collision fold mountains are formed. At a zone of collision two continental plates collide and since they are of equal densities no subduction will take place but the two will collide and crumble and fold to form fold mountains.
collision
the himalaya mountains were formed in a collision at a convergent boundary
A subductive collision.
Examples of collision mountain ranges include the Himalayas (formed by the collision of the Indian Plate with the Eurasian Plate), the Alps (formed by the collision of the African Plate with the Eurasian Plate), and the Andes (formed by the collision of the South American Plate with the Nazca Plate).
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At a collision zone, also known as a convergent boundary, one tectonic plate is forced beneath another, leading to the formation of mountain ranges, deep ocean trenches, and volcanic activity. This process can create significant landforms, such as the Himalayas, which were formed by the collision of the Indian and Eurasian plates. Additionally, subduction zones often generate volcanic arcs as magma rises to the surface.
The Himalaya mountains were formed in a collision of the Indian Plate pushing into the Eurasian Plate, in a convergent boundary known as a continental collision.
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One example of a collision zone is the San Andreas Fault in California, where the Pacific Plate slides past the North American Plate. This interaction results in frequent earthquakes and the potential for significant seismic activity.