The dominant type of stress associated with folded mountains is compressional stress caused by tectonic plate collision. As plates converge, the rocks are squeezed and folded, leading to the formation of folded mountain ranges such as the Himalayas and the Appalachians.
Folded mountains are formed when rock layers are bend under stress.
Folded mountains are formed when rock layers are bend under stress.
Compressional stress is the major factor that forms folded mountain ranges, such as the Himalayas. It occurs when tectonic plates collide, leading to the crust being pushed together and uplifted. Over time, this results in the crust being folded and deformed into mountain structures.
The force that forms folded mountains is called compressional force. This force occurs when tectonic plates collide, causing the Earth's crust to be pushed together and folded, leading to the formation of mountains.
Compressional Stress
Compressional tectonic stress causes folded mountains. This stress occurs when tectonic plates collide, leading to the deformation and folding of the Earth's crust. Over time, the accumulated pressure and movement result in the creation of folded mountain ranges.
conpression
Folded mountains are the result of compression stress in the earth's crust. This is a movement of plates that presses together or squeezes Earth's crust and is also known as convergent boundary.
The type of tectonic stress that forms fault-block mountains is known as extensional stress. This stress occurs when the Earth's lithosphere is being pulled apart, causing blocks of crust to move vertically. As the blocks are uplifted and tilted along fault lines, fault-block mountains are created.
FOLDED MOUNTAINS are located in the himilayas
It forms folded mountains