Fold mountain
The major types of mountains are fold mountains, fault-block mountains, and volcanic mountains. Fold mountains form from the folding of rocks due to tectonic forces, while fault-block mountains are created by the movement of large blocks of the Earth's crust along faults. Volcanic mountains are formed from the accumulation of volcanic materials such as lava, ash, and debris.
The appalachain mountains are fold mountains
Mt. Kenya is the highest mountain in Kenya and the second highest moutain in Africa.
Fold mountains typically form at convergent plate boundaries, where tectonic forces cause the Earth's crust to fold and uplift. Examples of fold mountain ranges include the Himalayas, Andes, Alps, and Rockies.
young fold mountains are like Himalayas, the Alps and man other.
fold mountains form
Mountains are categorized based on their elevation and prominence. The categories include major mountain ranges, individual peaks, volcanic mountains, and subranges based on geographical location. Mountains can also be classified by geological features such as fold mountains, block mountains, dome mountains, and volcanic mountains.
Yes, underwater fold mountains can form through tectonic processes where tectonic plates collide, causing rocks to fold and create underwater mountain ranges. An example of underwater fold mountains is the Mid-Atlantic Ridge.
The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.
The major types of mountains are volcanic mountains, fold mountains, block mountains, and dome mountains. Volcanic mountains are formed from volcanic activity, while fold mountains are created by the folding of rock layers. Block mountains result from the uplifting or faulting of large blocks of the Earth's crust, and dome mountains are formed by the uplift of a circular-shaped area of rock.
Yes, the mountains in northern Ethiopia are part of the Ethiopian Highlands, which are considered to be fold mountains. These mountains were formed by the movement of tectonic plates, resulting in the folding and uplifting of the Earth's crust.