when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
The oceanic plate suducts or sinks below the continental plate because it is colder and more dense
an oceanic trench, earthquakes volcanos
it subducts underneath the crustal plate
oceanic as it is colder; therefore denser
Depends on the type of tectonic plate. If it is two continental plates, usually a mountain range will be formed and the plates will 'lock' together due to their thickness. The Indian sub-continent colliding with the eurasian plate is one example. If an oceanic plate is subducting under a continental plate an island arc can be formed or mountain range such as Japan and the Andies mountains respectively. This type is also where volcanoes will be commonly found unlike the collision of two continental plates, due to the magma formed from the subduction of the oceanic plate. If two oceanic plates collide, usually form an oceanic mountain range and lock together similar to the continental plates.
An earthquake is made. Shock waves move in all directions from that place ( which is called the focus) and then it reaches the ground. This point is called the epicenter. The earth then starts violently shaking.
This process is known as subduction and occurs at convergent plate boundaries because oceanic crust is denser than continental crust.
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.
The contiental cdrust is forced under the continental crust in a process called subduction.
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.
it forms a trench
subduction
It subducts under the continental plate because the oceanic plate is denser.
terranes are attached to the edge of a continent
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.
The contiental cdrust is forced under the continental crust in a process called subduction.
When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
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.