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A subduction zone occurs when one tectonic plate is forced underneath another, leading to the formation of deep oceanic trenches and volcanic arcs. In contrast, a continent-continent collision zone happens when two plates carrying continental crust collide, resulting in the uplift of mountain ranges and intense seismic activity.
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A collision earthquake occurs when two tectonic plates collide, creating intense pressure and friction that results in seismic activity. These earthquakes are typically shallow and can be quite powerful due to the immense forces involved in the collision of the plates. Examples of collision earthquakes can be found in regions like the Himalayas and where the Pacific Plate collides with other plates along the Ring of Fire.
Its called the mountain time zone because its the mountain area
collision
A subductive collision.
A mountain range.
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The Himalayan Mountain Range was thrust upwards when the Indian Plate crashed into the European Plate.
The Hayward Fault Zone
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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.
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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.
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.
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