Cynclines and anticlines are mountians "folded" or distorted into basins and ridges by powerful pressure forces within the plastic mantle of the earth. When and if they rise to the surface of the earth (either by uplifting or erosion of overlaying layers of rock) they may become mountian ranges. The basin and range region west of the Rocky mountians serve as an example of folded ranges.
Fold mountains are located in zones where tectonic plates are colliding with each other. A very good example is the Himalayas where the Indian plate is colliding with the Eurasian plate.
the Atlas Mount (north west Africa)
the Himalayas (Asia)
the Alps (Europe,Italy,France)
the Andes (south America)
the Rockies (North America)
Andes, in South America is one.
Another would be Himalayas in Asia
the alps are fold mountains as well
Fold mountains (also known as orogenic) Are distributed along plate boundaries where plates move toward eachother. They are usually along the continential coasts.
Fold mountains are found where two tectonic plates move together
Alps and Rockies
the mountains in northern Ethiopia's fold mountains
All fold mountains are found on convergent plate boundaries.
Fold mountains are mountains that are formed when the land forms a wave like shape due to the tectonic plate movements underneath so yes the Ural Mountains are fold mountains
One of the features of young fold mountains is that these are formed at destructive collision of tectonic plate boundaries. The Earth's crust are pushed to the surface therefore forming a series of fold mountains.
Fold mountains are defined as mountains created by the bending of rock layers. Volcanic mountains are mountains created by breaks in the Earth's crust. In Canada, there are many examples. For example, the Appalachian Mountains and the Rocky Mountains are fold mountains. The Canadian Shield and the coastal ranges along the North American west coast are examples of volcanic mountains.
The main fold mountains found in the Caribbean region are the Greater Antilles, which include mountains like the Sierra Maestra in Cuba, the Blue Mountains in Jamaica, and the Cordillera Central in the Dominican Republic. These mountains were formed by the tectonic activity between the North American and Caribbean plates.
Fold mountains are found along convergent plate boundaries, where tectonic plates collide and the crust is thrust upward, folded, and deformed. Some well-known examples of fold mountains include the Himalayas, the Alps, and the Andes.
In the upper crust of the Earth
In India is Himalyas..
The Himalayas are Fold Mountains
The appalachain mountains are fold mountains
the mountains in northern Ethiopia's fold mountains
All fold mountains are found on convergent plate boundaries.
The MacGillycuddy's Reeks in County Kerry are a prominent range of fold mountains in Munster. These mountains include Ireland's highest peak, Carrauntoohil. The mountains were formed by the collision of tectonic plates, leading to the folding and uplifting of rock layers.
Mountains can be found on every continent around the world. They are formed through tectonic plate movement, volcanic activity, and erosion over millions of years. Some well-known mountain ranges include the Himalayas in Asia, the Andes in South America, the Rockies in North America, and the Alps in Europe.
young fold mountains are like Himalayas, the Alps and man other.
fold mountains form