The Formation of the Himalayas
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.
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.
yas are called young fold mountains
young fold mountains are like Himalayas, the Alps and man other.
the andes , the himalayas & the rockies
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.
The Himalayas are Fold Mountains
andes and himalayas
The Himalayas are a young, fold mountain range formed by the collision of the Indian and Eurasian tectonic plates. They are known for their high peaks, including Mount Everest, and are home to a diverse range of ecosystems and cultures.
Andes are called young fold mountains because they are young
the himalayas and the rockies and so on................
The Himalayas are Fold Mountains
Himalayas in Asia, Alps in Europe, Andes in South America, Rockies in North America, and the Great Dividing Range in Australia are examples of young fold mountains. These mountain ranges were formed relatively recently through tectonic plate collision, resulting in the folding of rock layers and the uplift of the Earth's crust.
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 Himalayasi need a example of fault block mountains(The himalayas are NOT fault block mountains , they are fold mountains.)