young fold mountains are like Himalayas, the Alps and man other.
in Asia by the river
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.
Andes are called young fold mountains because they are young
Some examples of young fold mountains include the Himalayas in Asia, the Andes in South America, and the Rockies in North America. These mountain ranges are still actively being uplifted through tectonic processes, resulting in their rugged, steep topography.
Fold mountains are commonly found at convergent plate boundaries, where tectonic plates collide and push against each other, causing the Earth's crust to fold and create mountain ranges. Examples of fold mountains include the Himalayas, the Andes, and the Alps.
Fold and thrust mountain ranges can be found at convergent plate boundaries, where two tectonic plates collide. Examples of fold and thrust mountain ranges include the Himalayas in Asia and the Rocky Mountains in North America.
In the upper crust of the Earth
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.
Fold mountains are found in long linear patterns across continents. They form when tectonic plates collide, leading to intense compression and folding of the Earth's crust. Examples include the Rocky Mountains in North America and the Himalayas in Asia. Fold mountains are typically located near plate boundaries, such as convergent boundaries, where tectonic forces are the strongest.
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.
Old fold mountains are the mountains which were formed 50-60 million years ago. Young fold mountains are the ones formed comparatively new (30-40 million years ago). - answer by Subhrajyoti Sen