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.
Trench
The contiental cdrust is forced under the continental crust in a process called subduction.
When a plate carrying oceanic crust collides with a plate carrying continental crust, the denser oceanic plate is usually subducted beneath the continental plate due to the difference in density. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity at the subduction zone.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
The contiental cdrust is forced under the continental crust in a process called subduction.
When oceanic crust collides with continental crust, the denser oceanic crust is forced beneath the continental crust in a process called subduction. This happens because oceanic crust is heavier, colder, and more dense than continental crust, making it susceptible to being subducted under the lighter continental crust. This collision can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches.
it forms a trench
subduction
The contiental cdrust is forced under the continental crust in a process called subduction.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.