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 oceanic crust slides down and burns in the mantle and forms a volcano
The contiental cdrust is forced under the continental crust in a process called subduction.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is 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.
The contiental cdrust is forced under the continental crust in a process called subduction.
tides will occur.
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 subducts underneath the crustal plate
The oceanic crust consists of heavier rock, mostly Basalt, so that if a oceanic plate collides with a continental plate the oceanic plate will be forced down below the continental plate, forming island arcs.continental plates are thicker than oceanic plates.
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.
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.