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.
young fold mountains are like Himalayas, the Alps and man other.
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
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.
andes and himalayas
Young fold mountains are characterized by rugged and sharp peaks, steep slopes, and active tectonic activity. Old fold mountains, on the other hand, are more rounded with lower elevations due to erosion over time, and have less tectonic activity. Examples of young fold mountains include the Himalayas, while the Appalachian Mountains are an example of old fold mountains.
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
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 three tallest fold mountains in the world are Mount Everest in the Himalayas, K2 in the Karakoram Range, and Kangchenjunga, also in the Himalayas.
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 :)