A range of very high mountains.
One common result of the collision of two continental plates is the formation of mountain ranges, such as the Himalayas where the Indian Plate collided with the Eurasian Plate. The intense pressure and folding of the Earth's crust during the collision lead to the uplift of the land and the creation of tall mountain peaks.
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.
When two continental plates converge, they can create large mountain ranges due to the intense pressure and folding of the Earth's crust. This process is known as continental collision and can result in the formation of features like the Himalayas where the Indian plate collided with the Eurasian plate.
The oceanic plate is forced beneath the continental plate in a process called subduction. This collision can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes due to the intense pressure and friction between the two plates.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
when two plates collide they form trenches.
One common result of the collision of two continental plates is the formation of mountain ranges, such as the Himalayas where the Indian Plate collided with the Eurasian Plate. The intense pressure and folding of the Earth's crust during the collision lead to the uplift of the land and the creation of tall mountain peaks.
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.
When two continental plates converge, they can create large mountain ranges due to the intense pressure and folding of the Earth's crust. This process is known as continental collision and can result in the formation of features like the Himalayas where the Indian plate collided with the Eurasian plate.
According to the modern theory of plate tectonics, its formation is a result of a continental collision along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.
Convergent Continental collision is where two tectonic plates move towards each other and the plate that is more dense moves underneath the less dense plate.
An example of a continental-continental plate convergence is the collision boundary between the Indian Plate and the Eurasian Plate that formed the Himalayas. The convergence between these two plates has led to the uplift of the Himalayan mountain range over millions of years due to the ongoing collision between the two continental plates.
The collision of an oceanic plate with a continental plate typically results in subduction, where the denser oceanic plate sinks beneath the continental plate, creating features like deep ocean trenches and volcanic arcs. In contrast, the collision of two continental plates leads to the formation of mountain ranges due to the compression and buckling of the crust, as neither plate is subducted easily. This process can create significant geological activity, such as earthquakes, but generally lacks the volcanic activity associated with oceanic-continental collisions.
Its when the oceanic crust and the continental crsut colide together.
mountain formation
The collision between two continental plates would result in the formation of the most extensive mountain range. When two continents collide, the continental crust buckles and folds, leading to the creation of large mountain ranges such as the Himalayas.
The oceanic plate is forced beneath the continental plate in a process called subduction. This collision can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes due to the intense pressure and friction between the two plates.