A Mountain belt.
continental crust
A mid-ocean ridge forms as crust drops along a divergent boundary across a continental plate. This process occurs when two tectonic plates move away from each other, allowing magma to rise up and solidify, creating new oceanic crust.
They are two different types of crust. Continental crust is heavier than Oceanic crust, so when the two collide, the Continental crust 'subducts' under the Oceanic Crust. 'Crust' referring to the tectonic plates, the surface of the Earth we stand on.
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
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.
a valley or a canyon
a rift hope i helped
continental crust
A mid-ocean ridge forms as crust drops along a divergent boundary across a continental plate. This process occurs when two tectonic plates move away from each other, allowing magma to rise up and solidify, creating new oceanic crust.
A mountain gets made
A rift forms.
They are two different types of crust. Continental crust is heavier than Oceanic crust, so when the two collide, the Continental crust 'subducts' under the Oceanic Crust. 'Crust' referring to the tectonic plates, the surface of the Earth we stand on.
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 continental crust is the basis of the continents. It is the layer of rock, which is mostly granitic, that forms the continents and continental shelves.
The crust that forms the continents is called continental crust. It is thicker and less dense than oceanic crust, composed mainly of granite rock. Continental crust is what makes up the landmasses on Earth's surface.
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.
At some convergent boundaries, an oceanic plate collides with acontinental plate. Oceanic crust tends to be denser and thinner thancontinentalcrust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental crust. This forms what is called a subduction zone.