continental crust
In some cases, the folded crust can be pushed up high enough to form mountains.
Folded mountains are formed when rock layers are bend under stress.
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.
Folded mountains form
Folded mountains form when two plates move towards each other by compressional forces. The movement results in sedimentary rocks moving upwards to form a series of folds.
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.
Fold mountains are formed from the collision of continental tectonic plates. Since neither plate subducts under the other, the colliding plates wrinkle and fold like a rug being pushed into a wall.
Folded mountains form when tectonic plates push against each other, causing the Earth's crust to buckle and fold. Fault block mountains, on the other hand, result from the displacement of large blocks of crust along fault lines. Fault block mountains tend to have steep cliffs on one side and a more gently sloping side known as a "fault scarp."
Folded mountains are created when plates are bent, squeezed and stretched.
Folded Mountain
is a mountain that has been form wHen two tictonic plates hit each other then fold to crate a mountain that is why is folded mountain folded mountains are formed when land is squeezed/compressed. The land buckles and folds, which can be seen in folded layers of rock. The Appellations mountains are very old folded mountains that have been worn down by weathering and erosion.
In some cases, the folded crust can be pushed up high enough to form mountains.