When two continental plates collide, it is an example of convergent boundaries. Since continental crust is buoyant and brittle, it will not be easily subducted, unlike oceanic crust. Therefore, the subduction that does occur will be shallow and will not experience as many igneous intrusions. The two colliding continental plates will hit each other and will produce a buckling appearance as they both fight being subducted. These kind of collisions tend to produce immense mountains such as the Himalayas.One plate goes underneath they other and melts under the plate it went under and forms magma which causes an eruption
The contiental cdrust is forced under the continental crust in a process called subduction.
When two plates carrying continental crust collide, the continental crust is too light to subduct beneath the other plate. Instead, the plates crumple and fold, leading to the formation of mountain ranges. This process is known as continental collision.
When a plate carrying continental crust converges with a plate carrying oceanic crust, the denser oceanic plate is typically subducted beneath the less dense continental plate. This can lead to the formation of volcanic arcs and deep ocean trenches.
When two plates carrying continental crust collide, they can form mountain ranges through a process called continental collision. The intense pressure and heat generated during the collision can result in the uplift and folding of the crust, leading to the formation of large mountain belts such as the Himalayas.
Continental crust and continental crust are made of different types of rock. The rocks in the continental crust do not contain as many of the heavier elements as the ones in the oceanic crust do.
The collision of two plates carrying continental crust can cause the formation of mountain ranges due to intense compression and folding of the Earth's crust. This process can also lead to the thickening and uplift of crust, creating uplifted and deformed rock layers that make up the mountains.
When two plates carrying continental crust collide, both plates crumple and fold due to the immense pressure. This can lead to the formation of mountain ranges and earthquakes along the convergent boundary. The collision can also result in the subduction of one continental plate beneath the other, ultimately leading to the formation of a mountain belt.
The contiental cdrust is forced under the continental crust in a process called subduction.
Tectonic plates consist of both continental and oceanic crust. The Earth's lithosphere is divided into several large and small plates that constantly move and interact with each other. Some plates are predominantly made up of continental crust, while others are mostly composed of oceanic crust.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.
The contiental cdrust is forced under the continental crust in a process called subduction.
No!