Question

find out about origin of himalayas . write it in story form

Answer 1

Answer:

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. 225 million years ago (Ma) India was a large island situated off the Australian coast and separated from Asia by the Tethys Ocean.

Answer 2

Explanation:

Himalayas from the International Space Station, looking south from over the Tibetan Plateau. The summits are Makalu [left (8,462 metres; 27,765 feet)], Everest [middle (8,848 metres; 29,035 feet)], Lhotse [middle (8,516 metres; 27,939 feet)] and Cho Oyu [right (8,201 metres; 26,906 feet)

The west end is in Pakistan. They run through Jammu and Kashmir, Himachal Pradesh,Uttaranchal, Sikkim and Arunachal Pradesh states in India, Nepal, and Bhutan. The east end is in the south of Tibet. They are divided into 3 parts Himadri, Himachal and Shiwaliks.

The 15 highest mountains in the world are in the Himalayas. The main ones are Mount Everest, K2, Annapurna, and Nanga Parbat. Mount Everest is the highest mountain on Earth, at 8,849 meters. Of the fifteen highest mountain peaks in the World, nine are in the Nepali Himalayas.The word "Himalaya" means House of Snow in Sanskrit, an old Indian language. The Himalayas are so high that they kept the Indian and Chinese people separate from each other most of the time. India is a peninsula that is cut off from the rest of Asia by the mountains. It is often called the Indian subcontinent because it is larger and more isolated than other peninsulas.

North of the Himalayas is the Tibetan Plateau. It is called “the roof of the world”. However, the Tibetan Plateau is very dry because the plateau and the mountains act as a gigantic rain shadow. The rain falls instead on the south side of the mountains. This has greatly influenced the climate of the Indian subcontinent. Not only does it block the extremely cold winter winds blowing from Central Asia from entering Subcontinent, it also forces the Bay of Bengal Monsoon branch to shed its moisture along NE and Northern Indian States, Bhutan, Nepal and Bangladesh.

Geologically, the origin of the Himalayas is the impact of the Indian tectonic plate. 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 the seabeds of that time being lifted up into mountains. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone.[1][2]

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. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also leads to earthquakes from time to time.