An example of an collision zone would be types of fold mountains such as the Himalayas.
If two cont. crusts collide then you get a collision zone. If cont. crust collides with oceanic crust then you get a subduction zone.
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.
A mountain range can be formed by the collision of an oceanic plate and a continental plate. This creates a subduction zone which eventually leads to the formation of a range of mountains.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
A mountain range.
An example of an collision zone would be types of fold mountains such as the Himalayas.
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.
If two cont. crusts collide then you get a collision zone. If cont. crust collides with oceanic crust then you get a subduction zone.
collision
the himalaya mountains were formed in a collision at a convergent boundary
A subductive collision.
A mountain range can be formed by the collision of an oceanic plate and a continental plate. This creates a subduction zone which eventually leads to the formation of a range of mountains.
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.
The Dead Zone - 2002 Collision 3-3 is rated/received certificates of: USA:TV-14
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