andes and himalayas
The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.
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.
Yes, there are fold mountains in the Caribbean. The islands in the Caribbean were formed by tectonic plate movements that led to the creation of fold mountains. The Greater Antilles, including islands like Cuba, Hispaniola, and Jamaica, have mountain ranges that are examples of fold mountains in the region.
Sure! Some examples of old fold mountains include the Appalachian Mountains in North America, the Ural Mountains in Russia, and the Caledonian Mountains in the British Isles.
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.
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.
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.
types of fold mountains are.1.symmetricla fold2.asymetrical fold3.over fold4.recumbent fold5.over thrust fold
Mountains formed by continental plates colliding are known as fold mountains. These mountains are created when the intense pressure from the converging plates causes rocks to buckle and fold, resulting in uplifted and folded mountain ranges. Examples of fold mountains include the Himalayas and the Alps.
Old fold mountains are characterized by their folded and deformed rock layers, which have been uplifted and eroded over millions of years. They often exhibit steep slopes, rugged terrain, and high elevations. Examples of old fold mountains include the Appalachian Mountains in North America and the Caledonian Mountains in Europe.
The appalachain mountains are fold mountains
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.