Adventure Tour India

History of Himalayas

Forty million years ago, a collision between two plates of the earth’s crust resulted in the creation of the earth’s highest mountain Himalayas. The magnificent range of the Himalayas harbors breathtakingly beautiful scenery and dramatic environment. The high Himalayas constituting a spectacular mountain scope are being able to attract the heart of any new comer who is in search of challenge and grandeur.

The beauty, mystery and majesty of these mountains are due to the thick layers of ice and snow that perpetually cover them up. Since time immemorial, the Himalayas has captured the dream, desires and Imagination of human beings. Even the early Aryans looked upon these mountains as the abode of gods and goddess and the extra ordinary objects of beauty, scenic grandeur, peace and tranquility. These towering mountains have aptly been called the “Top of the World” and “ The Third Pole” on the basis of the fact that they constitute the latitudinal extremity.

Nepal, renowned all over the world for its scenic and panoramic peaks, is the land of supernatural virgin beauty and a real paradise for nature lovers.

In 1852 the highest mountain in the world was determined by and later named after Sir George Everest. After determination of Mt. Everest, no climber had been a scaled mountain of Nepal till 1949. But, it is fact that the history of trekking in Nepal is started after climbing and expedition of many majestic peaks.

In 1949 the Swiss who had been earlier refused permission to attempt Dhaulagiri, entered-east Nepal by way of Darjeeling. The team who led by Sutter – Lohner and they explored Ramtang Glacier, Kang Bachen peak (7902m) and the triangle of Drohmo (7008m) Jongsang peak (7473m) and Nupchu (7028) on the Nepal – Tibet – Sikkim border. They also climb Tang Kangma (6249m) on outlays of Drohmo as well as Dzange peak (6709m) before they returned to Darjeeling on the nineteenth day of their expedition.

In 1949 Nepal opened its frontiers to the outside world and within eight years ten of the fourteen 8000m peaks had been climbed, Annapurna (8091m) was the first to be climbed in 1950, this was followed in 1953 by Everest (8848m) and Nanga Parbat (8125m). From then on the number of expeditions coming from many different countries of the world multiplied and by 1964 all these Himalayan giants had been climbed, one being Shisa Pangma (8046m) scaled by the Chinese in 1964.

The highest Peak Mt. Everest of the world and other numerous peaks have been climbed many times now. Tenzing Norge Sherpa and Edmund Hillary reached at top of the world Mt. Everest in 1953. Sir. Edmond Hillary stated “Nepal is the only country in the world which is also one of the world’s great trekking paradises and one of the nicest countries in the world for trekking.”

In addition to its lofty mountains, Nepal provides beautiful displays of its resplendent flora and fauna.

Himalayas, the highest mountain range in the world, extend along the northern frontiers of Pakistan, India, Nepal, Bhutan, and Burma. They were formed geologically as a result of the collision of the Indian subcontinent with Asia. This process of plate tectonics is ongoing, and the gradual northward drift of the Indian subcontinent still causes earthquakes (see Earthquakes, this ch.). Lesser ranges jut southward from the main body of the Himalayas at both the eastern and western ends.

The Himalayan system, about 2,400 kilometers in length and varying in width from 240 to 330 kilometers, is made up of three parallel ranges--the Greater Himalayas, the Lesser Himalayas, and the Outer Himalayas--sometimes collectively called the Great Himalayan Range. The Greater Himalayas, or northern range, average approximately 6,000 meters in height and contain the three highest mountains on earth: Mount Everest (8,796 meters) on the China-Nepal border; K2 (8,611 meters, also known as Mount Godwin-Austen, and in China as Qogir Feng) in an area claimed by India, Pakistan, and China; and Kanchenjunga (8,598 meters) on the India-Nepal border.

Many major mountains are located entirely within India, such as Nanda Devi (7,817 meters) in the state of Uttar Pradesh. The snow line averages 4,500 to 6,000 meters on the southern side of the Greater Himalayas and 5,500 to 6,000 on the northern side. Because of climatic conditions, the snow line in the eastern Himalayas averages 4,300 meters, while in the western Himalayas it averages 5,800 meters.

The Lesser Himalayas, located in northwestern India in the states of Himachal Pradesh and Uttar Pradesh, in north-central India in the state of Sikkim, and in northeastern India in the state of Arunachal Pradesh, range from 1,500 to 5,000 meters in height. Located in the Lesser Himalayas are the hill stations of Shimla (Simla) and Darjiling (Darjeeling).

During the colonial period, these and other hill stations were used by the British as summer retreats to escape the intense heat of the plains. It is in this transitional vegetation zone that the contrasts between the bare southern slopes and the forested northern slopes become most noticeable.

The Outer or Southern Himalayas, averaging 900 to 1,200 meters in elevation, lie between the Lesser Himalayas and the Indo-Gangetic Plain. In Himachal Pradesh and Uttar Pradesh, this southernmost range is often referred to as the Siwalik Hills. It is possible to identify a fourth, and northernmost range, known as the Trans-Himalaya.

This range is located entirely on the Qinghai-Xizang Plateau, north of the great west-to-east trending valley of the Yarlung Zangbo River. Although the Trans-Himalaya Range is divided from the Great Himalayan Range for most of its length, it merges with the Great Himalayan Range in the western section--the Karakoram Range--where India, Pakistan, and China meet.

The southern slopes of each of the Himalayan ranges are too steep to accumulate snow or support much tree life; the northern slopes generally are forested below the snow line. Between the ranges are extensive high plateaus, deep gorges, and fertile valleys, such as the vales of Kashmir and Kulu. The Himalayas serve a very important purpose.

They provide a physical screen within which the monsoon system operates and are the source of the great river systems that water the alluvial plains below (see Climate, this ch.). As a result of erosion, the rivers coming from the mountains carry vast quantities of silt that enrich the plains.

The area of northeastern India adjacent to Burma and Bangladesh consists of numerous hill tracts, averaging between 1,000 and 2,000 meters in elevation, that are not associated with the eastern part of the Himalayas in Arunachal Pradesh. The Naga Hills, rising to heights of more than 3,000 meters, form the watershed between India and Burma.

The Mizo Hills are the southern part of the northeastern ranges in India. The Garo, Khasi, and Jaintia hills are centered in the state of Meghalaya and, isolated from the northeastern ranges, divide the Assam Valley from Bangladesh to the south and west.