the plates will push each other up and form a mountain range.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
The collision between two continental plates would most likely result in the formation of the most extensive mountain range. When two continental plates collide, neither is subducted due to their low density, leading to the crust crumpling and uplifting to form large mountain ranges like the Himalayas.
When two plates carrying continental crust collide, both plates crumple and fold due to the immense pressure. This can lead to the formation of mountain ranges and earthquakes along the convergent boundary. The collision can also result in the subduction of one continental plate beneath the other, ultimately leading to the formation of a mountain belt.
When a oceanic plate collides with a continental plate, the denser oceanic plate is usually subducted beneath the lighter continental plate. This can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches. The collision can also lead to earthquakes and the release of magma.
When two tectonic plates collide, compressional stress occurs. This stress causes the rocks to fold and deform, leading to the formation of mountain ranges, such as the Himalayas. The intense pressure and friction between the plates can also result in earthquakes and volcanic activity.
Mountain buildup.
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.
When two plates carrying continental crust collide, they can form mountain ranges through a process called continental collision. The intense pressure and heat generated during the collision can result in the uplift and folding of the crust, leading to the formation of large mountain belts such as the Himalayas.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
When plates collide, they can either crumple and fold, creating mountain ranges, or one plate can slide beneath the other, forming trenches and volcanic arcs. The type of collision depends on the type of plates involved - oceanic, continental, or a combination.
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The collision between two continental plates would most likely result in the formation of the most extensive mountain range. When two continental plates collide, neither is subducted due to their low density, leading to the crust crumpling and uplifting to form large mountain ranges like the Himalayas.
When oceanic plates collide and slide under continental plates, they can form volcanic mountain ranges called continental volcanic arcs. These arcs result from the melting of the descending oceanic plate, which then feeds magma to the Earth's surface. Examples include the Andes in South America and the Cascades in North America.
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
When two plates carrying continental crust collide, both plates crumple and fold due to the immense pressure. This can lead to the formation of mountain ranges and earthquakes along the convergent boundary. The collision can also result in the subduction of one continental plate beneath the other, ultimately leading to the formation of a mountain belt.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
When pieces of continental crust collide at a convergent boundary, it is called continental collision. This collision can result in the formation of mountain ranges, such as the Himalayas from the collision of the Indian Plate with the Eurasian Plate.