Properties : geologically young structurally fold mountains stretched over north indian borders these mountains run in west to east direction from indus to brahmaputra. They are young because they are being formed from the collision between india and asia, a collision which began only about 30 million years ago and is still going on they are folded mountains because they are formed by folding of the rocks along the edges of both continents from the force, pressure, and heat of the collision. The himalayan rivers are perennial in nature where water flows throughout the year received from both snow melt and monsoon rain 4 these rivers flow across the young fold mountain and are still in youthful stage.
Himalayas are young because they are being formed from the collision between india and asia, a collision which began only about 30 million years ago and is still going on they are folded mountains because they are formed by folding of the rocks along the edges of both continents from the force, pressure, and heat of the collision. The himalayas are known to be young fold mountains young, because these have been formed relatively recently in the earth's history, compared to older. Examples of young fold mountains are the himalayas, the rockies, the andes and the alps they are mainly found in two linear belts: one down the west coast of america and the other from the mediterranean through south asia, to indonesia.
Fold mountains are mountains that form mainly by the effects of folding on layers within the upper part of the earth's crustbefore either plate tectonic theory developed, or the internal architecture of thrust belts became well understood, the term was used for most mountain belts, such as the himalayas. What kind of mountains are the himalayas volcanic mountains block mountains displaced matawarak young fold mountains submit skip. Himalayas are geologically young fold mountains formed by the collision of india and eurasia starting compressional mountain belt such as the himalayas, the rocks. The himalayas are known as the young fold mountains because they have been formed only few million years agothey were formed because of the folding of the earth's crust due to tectonic activity.
Everything you need to known about the northern mountains of india the young fold mountainous chain himalayas rise to over 8,000 meters from the sea level they run in an east-west direction along the entire northern boundary of india for 2400 kms. The himalayan mountains • it is geologically young and structurally fold mountains stretch over the northern borders of india • these himalayan mountain ranges run in a west-east direction. The himalayas, the highest mountain range on a mountain range or hill range is a series of most geologically young mountain ranges on the earth's land. Young folded mountains: the highest mountain systems of the present day are: the himalayas of india, the andes of south america, and the alps of southern europe these mountains generally exceed heights of 3000 meters above sea level and the highest peaks rise above 8000 meters (mt everest.
Mountain age young mountains have steep slopes and high, pointed peaks old mountains have been eroded and are lower and more rounded the himalayas have been. The himalayas are young fold mountains of tertiary period which were folded over tethys sea due to intercontinental collision these himalayas extend about 2500 km between indus and brahmaputra gorges from west to east in an arc shaped manner. The himalayas are known to be young fold 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.
The andes are an example of fold mountains formed at a destructive plate margin when two continental plates move towards each other, both plates are forced upwards in a series of folds this caused big problems for early geologists who struggled to explain why they were finding fossils of sea creatures high up in mountains such as the himalayas. Major physical divisions of india the himalayas (young fold mountains), indo-gangetic plain (monotonous topography - featureless topography), the peninsular plateau (one of the most stable landmasses one of the oldest plateaus of the world). The aravalli range is a range of mountains running approximately 692 km where as the himalayas being young fold mountains are still continuously rising. This feature is not available right now please try again later.
The himalayan mountain is geologically young and structurally fold mountains stretch over the northern parts of india it was uplifted from the 'tethys sea' during the tertiary period. There are two types of fold mountains: young fold mountains (10 to 25 million years of age, eg rockies and himalayas) and old fold mountains (over 200 million years of age, eg urals and appalachians of the usa. The himalayas are the highest mountains in the world and extend west-east between the indus and the brahmaputra in an arcuate form their length is about 2400 km and breadth on an average 240 km physical features: the himalayas are young fold mountains.