the andes , the himalayas & the rockies
because this are the young mountains that recently formed in the earth.
Caledonian and Hercynian
the himalayas and the rockies and so on................
The Jura Mountains and the Zagros Mountains are examples of the fold mountains. The fold mountain is formed as a result of the effects if the folding on layers within the upper part of the crust of the earth.
types of fold mountains are.1.symmetricla fold2.asymetrical fold3.over fold4.recumbent fold5.over thrust fold
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.
young fold mountains are like Himalayas, the Alps and man other.
Appalachian
Andes are called young fold mountains because they are young
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.
The major fold mountain range in the Caribbean is the Northern Andes, which extends from Venezuela through Colombia and Ecuador. Additionally, the Sierra Maestra range in Cuba is another smaller fold mountain range in the Caribbean region.
because this are the young mountains that recently formed in the earth.
The Rocky Mountains The Andes Mountains The Himalayas
Fold Mountains
The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.
the western cordilleras are young fold mountains, while the appalachians are old fold mountains.
Old fold mountains are mountains that were formed millions of years ago through the process of folding and faulting of the Earth's crust. These mountains have undergone significant erosion and are typically characterized by rounded peaks and deep valleys. Young fold mountains, on the other hand, are mountains that are still actively being formed through tectonic processes, such as the collision of tectonic plates. These mountains tend to have sharp, rugged peaks and steep slopes.