The himalayas young fold mountains
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 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. 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 called mound fold mountains because they represent topography with high peaks deep valley and fast flowing rivers the himalayan mountains began forming in the late cretaceous-tertiary period (70my) and continue to increase in elevation even today.
The major difference between young and old mountains is the level of erosion within an entire mountain range for example, the rocky mountains and himalayan mountains are young because they are still rugged, with very few signs of erosion. 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. Anyone who has travelled extensively through these young fold mountains has been entertained by many interesting tales and brought many back with them this fuse of fact and fiction leaves the curious traveler wondering and adds to the charm and mystery of the himalayas. What divides many of the fold mountain ranges is their age, some are ‘young (still growing) fold mountains’ and fold mountains over 200 million years old are ‘old fold mountains’ the ural mountains are over 250 million years old, making them an ‘old’ fold mountain.
The himalayas, which stretch some 2,900 kilometres between india, pakistan, china, and nepal, is the world’s tallest mountain range in addition to mount everest, the world’s tallest mountain by peak elevation standing at 8,848 meters tall, the range also features several other mountain peaks over 8,000 meters. The himalayan mountain range and tibetan plateau have formed as a result of the collision between the indian plate and eurasian plate which began 50 million years ago and continues today. Physical features: the himalayas are young fold mountains physiographically the mountains of the north may be divided into four parts, namely, (i) the siwalik mountains, (ii) the middle himalaya or the himachal, (iii) the great himalaya or the himadri, (iv) the trans-hima1aya. Old fold mountains of india young growing sivalik hills the sivalik hills are the southernmost and geologically youngest mountain range of the outer himalayas the tectonically active zone of the himalaya are the oldest fold mountains in india.
The great himalayas are also known as the young fold mountains the himalayas run along the northern border of india the himalayas form an arc which is about 2,400 km long the width varies from 400 km in kashmir to 150 km in arunachal pradesh. The himalayas are young fold mountains the range was formed when the indio-australian tectonic plane collided with the euro-asian tectonic plane the where we find the himala yas today was previously filled with sediments, which was carried by the rivers of the euro-asian plane. The himalayas are called young fold mountains (b) the alpine-himalayan system and circum parific mountain belt are the ‘old fold mountains’ which existed as geosynclines 50-60 million years ago question 5.
The young folded mountains of the alpine system circle the pacific, and cross eurasia from the mediterranean to the pacific, including such high ranges as the andes, sierra nevada of california, the cascades, the canadian rockies, the alaska range, the alps, the karakorum ranges, and the himalaya. The himalayas, geologically young and structurally fold mountains stretch over the northern borders of india these mountain ranges run in a west-east direction from the indus to the brahmaputra the himalayas are loftiest and one of the most rugged mountain barriers of the world. 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 types of mountains generally, mountains are split into: fold mountains, block mountains, dome mountains, and volcanic mountains plateau mountains, uplifted passive margins, and hotspot. Mountain age young mountains have steep slopes and high, pointed peaks old mountains have been eroded and are lower and more rounded or himalayan-, type mountain belts fold and thrust belts can also be associated with active continental margins or andean-type margins, where oceanic lithosphere is subducted into the asthenosphere but.
The himalayas young fold mountains
The himalayas, alps, andes and appalachian mountains are examples of fold mountains the jura mountains in switzerland and france and the zagros mountains in iran and iraq are also fold mountains. The himalayas are geographically known as young fold mountains covering the northern border of india the himalayan range is the most noteworthy and the toughest mountain range on the world. 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 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 rugged, soaring heights of the himalayas, andes, and alps are all active fold mountains the himalayas stretch through the border s of china, bhutan, nepal, india, and pakistan the crust beneath the himalaya, the most towering mountain range on earth, is still the process of being compressed.
- Building the himalayas presenter(s) students from the earth & planetary science department at uc berkeley grade level 6th grade standards connection(s) plate there is a direct bridging link with fold mountains, although the concept may be difficult for younger pupils to grasp pupils face a challenge (cognitive conflict) when they.
- The himalayas, andes, rockies hope i helped i was doing my revision on fold mountains and trying to find websites with maps that show fold mountain belts, major rivers and cities and i.
Best answer: the himalayan mountains began forming in the late cretaceous-tertiary period (70my) and continue to increase in elevation even today that makes them among the youngest of mountain chains on the earth they are fold mountains because of the compressive forces involved in the collision of the. Fold mountains young fold mountains form in many parts of the world and they form along the plate margins where great earth movements have taken placeg the himalayas in asia were formed this way they are found where a continental and oceanic plate collide (eg. Fold mountains are mountains formed mainly by the effects of folding on layers in the upper part of the earth's crust the term is rather out of date, though still fairly common in physical geography literature in the time before plate tectonics became well understood, the term was used for mountain belts, such as the himalayas.