A mountain
When two plates made of continental lithosphere collide, they can form mountain ranges due to the intense compressional forces generated at the collision boundary. The uplift and folding of rocks during the collision can give rise to large mountain systems like the Himalayas formed from the collision of the Indian Plate with the Eurasian Plate.
When continental plates collide they form high mountains.
Fault ... ;)
Earthquakes!
When two continental plates collide they form mountains .
When two Continental plates collide, both plates lift upward and it can form mountains or mountain chains.
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
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.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
Yes, folded mountains form at convergent boundaries where two plates collide. The immense pressure from the collision pushes the edges of the plates upward, creating long, folded mountain ranges. Examples include the Himalayas and the Andes.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.