Formation of himalayas pdf

This travels northward at 15 cm per year, and joined the Eurasian continent about 40-50 million years ago. The formation of the Himalayas resulted in the lighter rock of formation of himalayas pdf seabeds of that time being lifted up into mountains. The Indian plate is still moving north at 67 mm per year. Over the next 10 million years it will travel about 1,500 km into Asia.

This leads to the Himalayas rising by about 5 mm per year, making them geologically active. In the north part of the Himalayas where the temperature falls below freezing point, animals cannot survive well. The five main rivers of the Himalayas are the Jhelum, Chenab, Ravi, Beas, and Satluj. The rivers are the main source of human and animal life in those areas. The river Jhelum came from a spring called Verinag, which is 80 km south of Srinagar. It is known world wide for its nine bridges. The two rivers Chandra and Bhaga come together to form the Chenab River.

The Chenab is in the Lahaul region of Himachal Pradesh. Himalaya in the Spiti and Lahaul district. The lake of Chandra Tal also comes from these rivers. The Ravi River has come out in many love legends.

The town of Chamba is on a mountain shelf on the right bank of the river. The valley of Kullu and Kangra is formed by river Beas. The main force of this river is from the south of Larji. There it enters the Mandi district and further still into Kangra. Kailash, near the lake of Mansarovar. It cuts through the Zanskar range, and makes a deep well part at the base of the Kinner Kailash.

You can change this page. Please use the preview button before saving. The list of new changes in the wiki. This page was last changed on 13 September 2017, at 23:52. Himalaya” and “Imaus” redirect here. Mount Everest as seen from Drukair2 PLW edit. The Himalayas are distinct from the other great ranges of central Asia, although sometimes the term Himalaya is loosely used to include the Karakoram and some of the other ranges.