Isostasy
because the oceanic plate is more heavier than contental plate so the oceanic plate sinks under the contental.
The contiental cdrust is forced under the continental crust in a process called subduction.
A basic mountain should be formed from the collision of continental crust and oceanic crustAnswerWhen an oceanic and a continental crust collide, the heavier oceanic crust tends to subduct under the lighter continental crust. Because of the collision and corresponding compression and also because of volcanism related to dehydration and melting of the subducted plate a mountain range is formed. The Andes mountain range is a, if not the, most typical example.
Crust under the oceans is called oceanic crust.
the lithosphere is thinner under the oceanic crust
yes, The contiental goes over it.
The contiental cdrust is forced under the continental crust in a process called subduction.
Oceanic and Contintental crust are different in composition as well as size and density Continental- granitic/50-100km thick Oceanic- basaltic/ up to 10km thick Oceanic crust is more dense making it subduct under continental crust
The contiental cdrust is forced under the continental crust in a process called subduction.
because the oceanic plate is more heavier than contental plate so the oceanic plate sinks under the contental.
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.
The contiental cdrust is forced under the continental crust in a process called subduction.
A basic mountain should be formed from the collision of continental crust and oceanic crustAnswerWhen an oceanic and a continental crust collide, the heavier oceanic crust tends to subduct under the lighter continental crust. Because of the collision and corresponding compression and also because of volcanism related to dehydration and melting of the subducted plate a mountain range is formed. The Andes mountain range is a, if not the, most typical example.
Crust under the oceans is called oceanic crust.
Oceanic crust sinking under a plate with continental crust
the lithosphere is thinner under the oceanic crust