As an example of mountain ranges that were formed like this look to the Alps.
If the plates are moving toward each other from opposite directions, the more dense oceanic plate will subduct in a conveyor belt like operation under the less dense continental plate. Transform plate boundaries occur where plates of any combination grind alongside each other and result in faults and earthquakes.
When a continental plate collides with an oceanic plate and overtakes it, this is known as subduction.
It subducts under the continental plate because the oceanic plate is denser.
The oceanic crust will slide under the continental crust. And the reason is because the oceanic crust is much denser and the continental crust is least dense.
When an ocean plate collides with a continental plate, a subduction zone occurs and forms a deep trench. An ocean plate is more dense while a continental plate is less dense which causes the ocean plate to go under the continental plate and pull the land and water down, forming a trench.
When the Indian plate collided with the harder Asian plate, the Indian plate went underneath, eventually causing an up-thrust that raised the Himalayas.
When the oceanic plate sinks it is absorbed back into the magma.
When a continental plate collides with an oceanic plate and overtakes it, this is known as subduction.
it subducts underneath the crustal plate
The contiental cdrust is forced under the continental crust in a process called subduction.
The contiental cdrust is forced under the continental crust in a process called subduction.
It subducts under the continental plate because the oceanic plate is denser.
It will subduct under the less dense continental plate.
The contiental cdrust is forced under the continental crust in a process called subduction.
Convergent plate boundaries.
it forms a trench
subduction
terranes are attached to the edge of a continent