collision of two contential plates
The Himalayas mountains are about 70 million years old, when the Indo-Australian Plate collided with the Eurasian Plate, forming the fold mountain during the Upper Cretaceous Period around 70 million years ago.
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.
The Himalayas are a young, fold mountain range located in northern India and Nepal, while the Peninsular Plateau is an older, stable landmass in central and southern India. The Himalayas are characterized by high peaks, deep valleys, and snow-capped mountains, while the Peninsular Plateau is a flat-topped region with extensive basaltic lava flows and plateaus. Additionally, the Himalayas have a more active geology with ongoing tectonic activities, while the Peninsular Plateau is relatively stable.
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 Himalayas today was previously filled with sediments, which was carried by the rivers of the Euro-asian plane. When the two previously mentioned plane collided this sediment folded to form the Himalayan range.
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 currently the tallest mountain range, but they're also extremely young, and have not existed for most of the history of the Earth.I don't definitively know what the tallest mountain range ever on Earth would be, but I do know that the Appalachian range has been consistently above water for about 400 million years (very few places on Earth can make this claim), and was taller than the Himalayas at its peak height.A professional geologist interested in orogenies would definitely know this, as well as anyone can.
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.
It is widely believed that the disaster that occurred during the formation of the Himalayas was the Continental Drift. The Himalayas are considered to be young mountains compared to other mountain ranges on the Earth.
Tall, rocky, jagged peaks are young: Himalayas Low, tree covered, rounded, hill-like features are old: Appalachians
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
Old mountains are usually eroded down to their roots (e.g. the Scottish Highlands) while young mountains are usually high a pointy (e.g. the Himalayas). mountains that are jagged at the top are new mountains that are more rounded are old
The Himalayas, The Alps, The Andes, the Appalachian Mountains, Aravali Range, Ural Mountains.
a young mountain range along a continental coast.