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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.
At a continental-continental convergence, two tectonic plates carrying continental crust collide, leading to the uplift of land and the formation of mountain ranges. This process can result in intense seismic activity and the creation of complex geological structures. Unlike oceanic-continental convergence, there is no subduction, as both plates are buoyant, leading to a compressional environment. Notable examples include the Himalayas, formed by the collision of the Indian and Eurasian plates.
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.
When tectonic plates collide, they can form various geological features depending on the nature of the collision. If two continental plates converge, they can create mountain ranges, such as the Himalayas. When an oceanic plate collides with a continental plate, it can lead to subduction, forming deep ocean trenches and volcanic arcs. Additionally, the collision of two oceanic plates can result in island arcs.
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.
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.
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.
At a continental-continental convergence, two tectonic plates carrying continental crust collide, leading to the uplift of land and the formation of mountain ranges. This process can result in intense seismic activity and the creation of complex geological structures. Unlike oceanic-continental convergence, there is no subduction, as both plates are buoyant, leading to a compressional environment. Notable examples include the Himalayas, formed by the collision of the Indian and Eurasian plates.
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.
If two continental plates collide, they will likely result in the formation of a mountain range due to the immense pressure and force generated during the collision. The leading edge of each plate is forced upwards, creating fold mountains with complex geological structures.
When tectonic plates collide, they can form various geological features depending on the nature of the collision. If two continental plates converge, they can create mountain ranges, such as the Himalayas. When an oceanic plate collides with a continental plate, it can lead to subduction, forming deep ocean trenches and volcanic arcs. Additionally, the collision of two oceanic plates can result in island arcs.
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.
Trolled
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
Yes, when two continental plates collide, they can form mountain ranges. This occurs because both plates are buoyant and resist subduction, leading to the upward folding and crumpling of the Earth's crust. The intense pressure and geological forces involved in this process result in the creation of significant mountain ranges, such as the Himalayas, which were formed by the collision of the Indian and Eurasian plates.