because the tectonic plate that their on are folding on top of each other.
Folded mountains. These mountains are formed when tectonic plates collide and the layers of rock are pushed together, creating folds and wrinkles in the Earth's crust. Examples include the Himalayas and the Alps.
Folded mountains are large mountain ranges that form through the folding of rock layers due to tectonic plate movements. These mountains typically have long ridges and valleys, with the rock layers appearing bent and folded. Examples include the Himalayas and the Appalachians.
Mountains produced at continent-continent convergence are called fold mountains. These mountains are formed when two continental plates collide and the rocks are compressed, folded, and uplifted to form large mountain ranges, such as the Himalayas.
yes along with the andes, rockies and himalayas.
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.
The Himalayas
Folded mountain ranges form when tectonic plates collide and the intense pressure causes the earth's crust to buckle and fold. This process is called orogeny, and the folded layers of rock are uplifted to create mountain ranges like the Alps or the Himalayas. Over time, erosion shapes and exposes these folded layers, creating the distinctive peaks and valleys of folded mountains.
The Himalayas
Mount Everest is in a group on mountains called the Himalayas.
Folded mountains are found all over the world, with major examples including the Rockies in North America, the Alps in Europe, and the Himalayas in Asia. These mountains form as a result of tectonic plate movement, where layers of rock are uplifted and folded due to compression forces.
Fold mountains form through the process of compression. This occurs when tectonic plates collide, causing rock layers to be pushed together and folded upward, forming large mountain ranges. Examples include the Himalayas and the Alps.
Fold mountains, such as the Himalayas or the Appalachians, are formed when tectonic plates collide, causing rock layers to be folded and uplifted. This sideways pressure creates large mountain ranges with distinctive folded patterns in the rocks.