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The Himalayan mountain range and Tibetan plateau have formed as a consequence of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today.
Features ofHimalayan mountains
Himalayan Region is the shape of an arc.
Himalayan Region is composed of sedimentary rocks.
In the Himalayan Region, the average height of Mountain peaks is around 6000 metres.
It is the northernmost and continuous range.
It is covered with snow and comprise of snow glaciers.
By nature it is symmetrical and comprises of granite.
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