This is difficult to determine but the Green-stone belts are very old fold mountains (Southern Africa) and there are some old folded sedimentary rocks to be found in Greenland.
the himalayas and the rockies and so on................
the andes , the himalayas & the rockies
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
young fold mountains are like Himalayas, the Alps and man other.
Fold Mountains
The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.
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 Appalachian Mountains in North America are an example of old fold mountains. They were formed over 480 million years ago through the collision of tectonic plates and have since undergone erosion and weathering, giving them their characteristic gentle slopes and rounded peaks.
the western cordilleras are young fold mountains, while the appalachians are old fold mountains.
This is difficult to determine but the Green-stone belts are very old fold mountains (Southern Africa) and there are some old folded sedimentary rocks to be found in Greenland.
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.
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.
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 appalachain mountains are fold mountains
the mountains in northern Ethiopia's fold mountains