also Him+alaya (Sanskrit for “abode of snow”), mountain system in Asia, forming a broad continuous arc for nearly 2600 km (1600 mi) along the northern fringes of the Indian subcontinent, from the bend of the Indus River in the northwest to the Brahmaputra River in the east. The Himalayas range, averaging 320 to 400 km (200 to 250 mi) in width, rises sharply from the Gangetic Plain. North of this mountain belt lies the Tibetan Plateau (Qing Zang Gaoyuan). The Himalayas form the earth’s highest mountain region, containing 9 of the 10 highest peaks in the world. Among these peaks are the world’s highest mountain, Mount Everest (8848 m/29,028 ft), which is on the Nepal-Tibet border; the second highest peak, K2 or Mount Godwin Austen (8,611 m/28,251 ft), located on the border between China and Jammu and Kashmir, a territory claimed by India and Pakistan; the third highest peak, Kanchenjunga (8,598 m/28,209 ft) on the Nepal-India border; Makalu (8481 m/27,824 ft) on the Nepal-Tibet border; Dhaulagiri (8,172 m/26,811 ft) and Annapurna 1 (8,091 m/26,545 ft) in Nepal; Nanga Parbat (8,125 m/26,657 ft) in the Pakistani-controlled portion of Jammu and Kashmir; and Nanda Devi (7817 m/25,645 ft) in India.

Lesser Himalaya

Also called Mahabharat Range, the Lesser Himalayas is a prominent range 2,000 to 3,000 meters (6,600 to 9,800 ft) high formed along the Main Boundary Thrust fault zone, with a steep southern face and gentler northern slopes. They are nearly continuous except for river gorges, where rivers from to the north gather like candelabra in a handful of places to break through the range.

At these elevations and above the biogeography of the Himalayas is generally divided by the Kali Gandaki Gorge in central Nepal, one of the deepest canyons in the world.

At the middle elevations of the range, the subtropical forests yield to a belt of temperate broadleaf and mixed forests growing between 1,500 and 3,000 meters (4,900 and 9,800 ft), with the western Himalayan broadleaf forests to the west of the Gandaki River, and the eastern Himalayan broadleaf forests to the east. The western broadleaf forests stretch from the Kashmir Valley, across Himachal Pradesh and Uttarakhand, and through western Nepal. The eastern broadleaf forests stretch across eastern Nepal, through Sikkim and Bhutan, and through much of Arunachal Pradesh.


This ‘hilly’ region (Pahad), averaging about 1,000 meters (3,300 ft) immediately north of the Mahabharat Range, rises over about 100 kilometres (330,000 ft) to about 4,000 meters (13,000 ft) at the Main Central Thrust fault zone, where the Greater Himalaya begin.

Above the broadleaf forests, between 3,000 and 4,000 meters (9,800 and 13,000 ft), are temperate coniferous forests, likewise split by the Gandaki River. The western Himalayan subalpine conifer forests are found below treeline in northern Pakistan, Jammu and Kashmir, Himachal Pradesh, Uttarakhand, and western Nepal. The eastern Himalayan subalpine conifer forests are found in eastern Nepal, Sikkim, Bhutan, and Arunachal Pradesh. Along the border between Arunachal Pradesh and Tibet, the eastern subalpine conifer forests mix with the north-eastern Himalayan subalpine conifer forests. East Himalayan Fir, West Himalayan Spruce, and Himalayan Hemlock are some important trees of these forests. Rhododendrons are exceptionally diverse here, with over 60 species recorded in the north-eastern Himalayan subalpine conifer forests.

Greater Himalaya

North of the Main Central Thrust, the highest ranges rise abruptly as much as 4,000 meters (13,000 ft) into the realm of perpetual snow and ice. As the Himalayan system becomes wider from east to west, the number of parallel high ranges increases. For example, the Kagmara and Kanjiroba ranges both reach well over 6,000 meters (20,000 ft) north of the Dhaulagiri Himalaya in central Nepal.

Montane grasslands and scrublands grow above tree line. The north-western Himalayan alpine shrub and meadows are found in the high elevations of northern Pakistan, Jammu and Kashmir, and Himachal Pradesh. To the east, the western Himalayan alpine shrub and meadows cover extensive areas along the Tibetan border with Uttarakhand and western Nepal. The eastern Himalayan alpine shrub and meadows grow above the eastern and north-eastern subalpine conifer forests, along the Tibetan border with eastern Nepal, Sikkim, Bhutan, and Arunachal Pradesh. The scrublands are composed of junipers as well as a wide variety of rhododendrons. They also possess a remarkable variety of wildflowers: Valley of Flowers National Park in the western Himalayan alpine shrub and meadows contains hundreds of species. The upper limit of the grasslands increases from west to east, rising from 3,500 meters (11,500 ft) to 5,500 meters (18,000 ft). The grasslands are the summer habitat of the endangered snow leopard.


The watershed between rivers flowing south into the Ganges or Indus and rivers flowing north into the Brahmaputra or mainstem Indus that flow around the ends of the entire range often follows somewhat lower, less rugged mountains tens of kilometers north of the highest ranges. South-flowing rivers form valleys in this region, often semi-arid due to rain shadow effects. These valleys hold some of the highest permanent villages on earth.

Geologic Formation and Structure

The Himalayan mountain system developed in a series of stages 30 to 50 million years ago. The Himalayan range was created from powerful earth movements that occurred as the Indian plate pressed against the Eurasian continental plate. The earth movements raised the deposits laid down in the ancient, shallow Tethys Sea (on the present site of the mountains) to form the Himalayan ranges from Pakistan eastward across northern India, and from Nepal and Bhutan to the Myanmar (Burmese) border. Even today the mountains continue to develop and change, and earthquakes and tremors are frequent in the area


Physically, the Himalayas forms three parallel zones: the Great Himalayas, the Middle Himalayas (also known as the Inner or Lesser Himalayas), and the Sub-Himalayas, which includes the Siwalik Range and foothills and the Tarai and Duars piedmont (an area of land formed or lying at the foot of a mountain or mountain range). Each of these lateral divisions exhibits certain similar topographic features. The Great Himalayas, the highest zone, consists of a huge line of snowy peaks with an average height exceeding 6100 m (20,000 ft). The width of this zone, composed largely but not entirely of gneiss and granite, is about 24 km (about 15 mi). Spurs from the Great Himalayas project southwards into the Middle Himalayas in an irregular fashion. The Nepal and Sikkim (a state of northern India) portion of the Great Himalayas contains the greatest number of high peaks. The snow line on the southern slopes of the Great Himalayas varies from 4480 m (14,700 ft) in the eastern and central Himalayas of Nepal and Sikkim to 5180 m (17,000 ft) in the western Himalayas. To the north of the Great Himalayas are several ranges such as the Zaskar, Ladakh, and the Kailas. The Karakoram Range lies on the Tibetan side of the Great Himalayas.

The Great Himalayan region is one of the few remaining isolated and inaccessible areas in the world today. Some high valleys in the Great Himalayas are occupied by small clustered settlements. Extremely cold winters and a short growing season limit the farmers to one crop per year, most commonly potatoes or barley. The formidable mountains have limited the development of large-scale trade and commerce despite the construction of highways across the mountains linking Nepal and Pakistan to China. Older trails, which cross the mountains at high passes, also have limited trade and are open only during the summer months.

The Middle Himalayas range, which has a width of about 80 km (about 50 mi), borders the Great Himalayan range on the south. It consists principally of high ranges both within and outside of the Great Himalayan range. Some of the ranges of the Middle Himalayas are the Nag Tibba, the Dhaola Dhar, the Pir Panjal, and the Mahabharat. The Middle Himalayas possess a remarkable uniformity of height; most are between 1830 and 3050 m (between 6000 and 10,000 ft).

The Middle Himalayas region is a complex mosaic of forest-covered ranges and fertile valleys. While not as forbidding as the Great Himalayas to the north, this range has nonetheless served to isolate the valleys of the Himalayas from the plains of the Indus and Ganges rivers in Pakistan and northern India. Except for the major valley centers such as Srinagar, Kangra, and Kathmandu, and hill towns such as Simla, Mussoorie, and Darjiling (Darjeeling), the region is moderately populated. Within the Middle Himalayas the intervening mountain ranges tend to separate the densely populated valleys. The numerous gorges and rugged mountains make surface travel difficult in any direction. Few roads or transport routes exist between towns, partly because it is expensive to build them over the high, rough terrain. Only major population centers are linked by air and roads with principal cities in India and Pakistan.

The Sub-Himalayas, which is the southernmost and the lowest zone, borders the plains of North India and Pakistan. It comprises the Siwalik Range and foothills as well as the narrow piedmont plain at the base of the mountains. The width of the Sub-Himalayas gradually narrows from about 48 km (about 30 mi) in the west until it nearly disappears in Bhutan and eastern India. A characteristic feature of the Sub-Himalayas is the large number of long, flat-bottomed valleys known as duns, which are usually spindle-shaped and filled with gravelly alluvium. South of the foothills lies the Tarai and Duars plains. The southern part of the Tarai and Duars plains is heavily farmed. The northern part was forest inhabited by wild animals until about the 1950s. Most of the forests of this region have been destroyed, and much of the land has been reclaimed for agriculture.

Plant and Animal Life


The natural vegetation is influenced by climate and elevation. Tropical, moist deciduous forest at one time covered all of the Sub-Himalayan area. With few exceptions most of this forest has been cut for commercial lumber or agricultural land. In the Middle Himalayas at elevations between 1520 and 3660 m (between 5000 and 12,000 ft) natural vegetation consists of many species of pine, oak, rhododendron, poplar, walnut, and larch. Most of this area has been deforested; forest cover remains only in inaccessible areas and on steep slopes. Below the timber line the Great Himalayas contains valuable forests of spruce, fir, cypress, juniper, and birch. Alpine vegetation occupies higher parts of the Great Himalayas just below the snow line and includes shrubs, rhododendrons, mosses, lichens, and wildflowers such as blue poppies and edelweiss. These areas are used for grazing in summer by the highland people of the Great Himalayas.

Animals such as tigers, leopards, rhinoceroses, and many varieties of deer once inhabited the forested areas of the Sub-Himalayan foothills and the Tarai plain. As a result of deforestation the habitat of most of the wildlife has been destroyed. They are now restricted to special protected areas such as the Jaldapara and Kaziranga sanctuaries in India and the Chitawan preserve in Nepal. There are few animals in the Middle Himalayas because of extensive deforestation. In the Great Himalayas musk deer, wild goats, sheep, wolves, and snow leopards are found. The existence of the  Yeti has been reported by highland Sherpas in Nepal but has eluded discovery by several expeditions.

People and Economy

The population, settlement, and economic patterns within the Himalayas have been greatly influenced by the variations in topography and climate, which impose harsh living conditions and tend to restrict movement and communication. People living in remote, isolated valleys have generally preserved their cultural identities. However, improvements in transportation and communication, particularly satellite television programs from Europe and the United States, are bringing access from the outside world to remote valleys. These outside influences are affecting traditional social and cultural structure.

Nearly 40 million people inhabit the Himalayas. Generally, Hindus of Indian heritage are dominant in the Sub-Himalayas and the Middle Himalayan valleys from eastern Kashmir to Nepal. To the north Tibetan Buddhists inhabit the Great Himalayas from Ladakh to northeast India. In central Nepal, in an area between about 1830 and 2440 m (between about 6000 and 8000 ft), the Indian and Tibetan cultures have intermingled, producing a combination of Indian and Tibetan traits. The eastern Himalayas in India and nearby areas of eastern Bhutan are inhabited by animistic people whose culture is similar to those living in northern Myanmar and Yunnan province in China. People of western Kashmir are Muslims and have a culture similar to the inhabitants of Afghanistan and Iran.

The economy of the Himalayas as a whole is poor with low per capita income. Much of the Himalayas area is characterized by a very low economic growth rate combined with a high rate of population growth, which contributes to stagnation in the already low level of per capita gross national product. Most of the population is dependent on agriculture, primarily subsistence agriculture; modern industries are lacking. Mineral resources are limited. The Himalayas has major hydroelectric potential, but the development of hydroelectric resources requires outside capital investment. The skilled labor needed to organize and manage development of natural resources is also limited due to low literacy rates. Most of the Himalayan communities face malnutrition, a shortage of safe drinking water, and poor health services and education systems.

Agricultural land is concentrated in the Tarai plain and in the valleys of the Middle Himalayas. Patches of agricultural land have also been carved out in the mountainous forested areas. Rice is the principal crop in eastern Tarai and the well-watered valleys. Corn is also an important rain-fed crop on the hillsides. Other cereal crops are wheat, millet, barley, and buckwheat. Sugarcane, tea, oilseeds, and potatoes are other major crops. Food production in the Himalayas has not kept up with the population growth.

The major industries include processing food grains, making vegetable oil, refining sugar, and brewing beer. Fruit processing is also important. A wide variety of fruits are grown in each of the major zones of the Himalayas, and making fruit juices is a major industry in Nepal, Bhutan, and in the Indian Himalayas.

Since 1950 tourism has emerged as a major growth industry in the Himalayas. Nearly 1 million visitors come to the Himalayas each year for mountain trekking, wildlife viewing, and pilgrimages to major Hindu and Buddhist sacred places. The number of foreign visitors has increased in recent years, as organized treks to the icy summits of the Great Himalayas have become popular. While tourism is important to the local economy, it has had an adverse impact on regions where tourist numbers exceed the capacity of recreational areas.

Historically, all transport in the Himalayas has been by porters and pack animals. Porters and pack animals are still important, but the construction of major roads and the development of air routes have changed the traditional transportation pattern. Major urban centers such as Kathmandu, Simla, and Srinagar, as well as important tourist destinations, are served by airlines. Railways link Simla and Darjiling, but in most of the Himalayas there are no railroads. The bulk of goods from the Himalayas, as well as goods destined for places within the Himalayas, generally come to Indian railheads, located in the Tarai, by road. The pack animals and porters transport goods from road heads to the interior and back.