Older fold mountains have undergone millions of years of erosion processes like weathering and sedimentation, which have worn down their peaks and reduced their height. In contrast, younger fold mountains are still being uplifted by tectonic forces, so they have not experienced as much erosion and retain their height.
The presence of sharp, rugged peaks and deep, narrow valleys indicates a young fold mountain, formed relatively recently. In contrast, smooth, rounded peaks and wider valleys suggest an older fold mountain that has been eroded over time. Additionally, studying the surrounding geological features and sedimentary layers can help determine the age of a fold mountain.
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.
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.
The Rocky mountains are, I believe, consisted of the Transform Fault movement.
The features of a young fold mountain are: Distinctive layers of rock that lie slightly slanted; High, then low points of the mountain range; They run along a plate boundary
There are no young fold mountains in Africa because the continent lacks active tectonic plate boundaries that would create the necessary conditions for mountain-building processes. Most of Africa's mountains formed millions of years ago and have since eroded down, leaving behind older mountain ranges like the Atlas Mountains and the Drakensberg Mountains.
The Formation of the HimalayasThe Himalayas are known to be youngfold mountains. Young, because these have been formed relatively recently in the earth's history, compared to older mountain ranges like the Aravallis in India, and the Appalachian in the USA. They are known as fold mountains because the mountains extend for 2500 km in length in a series of parallel ridges or folds.
The Himalayas are known to be youngfold mountains. Young, because these have been formed relatively recently in the earth's history, compared to older mountain ranges like the Aravallis in India, and the Appalachian in the USA. They are known as fold mountains because the mountains extend for 2500 km in length in a series of parallel ridges or folds.
young fold mountains are like Himalayas, the Alps and man other.
A fold mountain is where two pieces of land crash and make fold mountains.
The Himalayas are Fold Mountains
Fold mountains are formed when two plates under the ground move together which forces sedimentary rock upwards in to a series of folds. ' Hence fold mountains ' There are two types of fold mountain: young fold mountains ( 10-25 millions years of age e.g Rockies and Himalayas ) Old fold mountains (over 200 million years of age, e.g. Urals and Appalachians of the USA). Hope its useful :)
The Himalayas are Fold Mountains
The Urals are fold mountains.
The fold mountains that formed less than about 25 million years back are considered young . These regions may be prone to Earthquakes and volcanic eruptions because the crust of the Earth is unstable
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they are fold mountains