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* ''[[Seven Years in Tibet (1997 film)]]'' is a [[1997 in film|1997]] film based on [[Seven Years in Tibet|the book of the same name]] written by [[Austria]]n [[mountaineer]] [[Heinrich Harrer]].
* ''[[Seven Years in Tibet (1997 film)]]'' is a [[1997 in film|1997]] film based on [[Seven Years in Tibet|the book of the same name]] written by [[Austria]]n [[mountaineer]] [[Heinrich Harrer]].
* [http://www.lunamdocs.com/ Journey of a Red Fridge ] (2007), directed by Lucian and Natasa Muntean ([[Lunam Docs]]), is an award-winning documentary that tells the story of child [[Porter (carrier)|porters]] working in the Himalayan mountains of [[Nepal]].
* [http://www.lunamdocs.com/ Journey of a Red Fridge ] (2007), directed by Lucian and Natasa Muntean ([[Lunam Docs]]), is an award-winning documentary that tells the story of child [[Porter (carrier)|porters]] working in the Himalayan mountains of [[Nepal]].
*"[[G.I.Joe The Movie]]" is a [[1987]] animated feature in which an ancient civilization known as [[Cobra La]] has taken refuge deep within the Himalayas after the [[Ice Age]] that nearly wiped them off the face of the Earth.
*"[[G.I.Joe: The Movie]]" is a [[1987]] [[animated]] feature in which an ancient civilization known as [[Cobra La]] has taken refuge deep within the Himalayas after the [[Ice Age]] that nearly wiped them off the face of the Earth.


==See also==
==See also==

Revision as of 20:55, 24 November 2010

"Himalaya" redirects here. For other uses, see Himalaya (disambiguation).

Template:Geobox The Himalaya Range (Sanskrit: literally, "abode of snow", Hindi/Sanskrit: हिमालय, IPA: /hɪˈmɑːləj(ə)/), the Himalayas or Himalaya for short, is a mountain range in Asia, separating the Indian subcontinent from the Tibetan Plateau. By extension, it is also the name of a massive mountain system that includes the Karakoram, the Hindu Kush, and other, lesser, ranges that extend out from the Pamir Knot.

Together, the Himalayan mountain system is the planet's highest, and home to the world's highest peaks, the Eight-thousanders, which include Mount Everest and K2. To comprehend the enormous scale of this mountain range, consider that Aconcagua, in the Andes, at 6,962 metres (22,841 ft) is the highest peak outside Asia, whereas the Himalayan system includes over 100 mountains exceeding Template:M to ft.[1]

Some of the world's major rivers, the Ganges, Indus, Brahmaputra, Yangtze, Mekong, Salween, Red River (Asia), Xunjiang, Chao Phraya, Irrawaddy River, Amu Darya, Syr Darya, Tarim River and Yellow River, rise in the Himalayas, and their combined drainage basin is home to some 3 billion people (almost half of Earth's population) in Afghanistan, Bangladesh, Bhutan, People's Republic of China, India, Nepal, Burma, Cambodia, Tajikistan, Uzbekistan, Turkmenistan, Kazakhstan, Kyrgyzstan, Thailand, Laos, Vietnam, Malaysia and Pakistan.

The Himalayas have profoundly shaped the cultures of South Asia; many Himalayan peaks are sacred in Hinduism, Buddhism and Sikhism. The main Himalaya range runs west to east, from the Indus river valley to the Brahmaputra river valley, forming an arc Template:Km to mi long, which varies in width from Template:Km to mi in the western Kashmir-Xinjiang region to Template:Km to mi in the eastern Tibet-Arunachal Pradesh region. The range consists of three coextensive sub-ranges, with the northernmost, and highest, known as the Great or Inner Himalayas.

Ecology

Everest, the highest peak of the Himalayas (left) and Lhotse (right), no. 5
K2, on the border of Pakistan and People's Republic of China
Kangchenjunga, on the border of Nepal and Sikkim, India

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the front of the range. This diversity of climate, altitude, rainfall and soil conditions generates a variety of distinct plant and animal communities.

Lowland forests

On the Indo-Gangetic plain at the base of the mountains, an alluvial plain drained by the Indus and Ganges-Brahmaputra river systems, vegetation varies from west to east with rainfall. The xeric Northwestern thorn scrub forests occupy the plains of Pakistan and the Indian Punjab. Further east lie the Upper Gangetic plains moist deciduous forests of Uttarakhand and Uttar Pradesh and Lower Gangetic plains moist deciduous forests of Bihar and West Bengal. These are monsoon forests, with drought-deciduous trees that lose their leaves during the dry season. The moister Brahmaputra Valley semi-evergreen forests occupy the plains of Assam.

The Terai belt

Above the alluvial plain lies the Terai strip, a seasonally marshy zone of sand and clay soils. The Terai has higher rainfall than the plains, and the downward-rushing rivers of the Himalaya slow down and spread out in the flatter Terai zone, depositing fertile silt during the monsoon season and receding in the dry season. The Terai has a high water table due to groundwater percolating down from the adjacent zone. The central part of the Terai belt is occupied by the Terai-Duar savanna and grasslands, a mosaic of grasslands, savannas, deciduous and evergreen forests that includes some of the world's tallest grasslands. The grasslands of the Terai belt are home to the Indian rhinoceros (Rhinoceros unicornis).

Bhabhar belt

Above the Terai belt is an upland zone known as the Bhabhar, a zone of porous and rocky soils made up of debris washed down from the higher ranges. The Bhabhar and the lower Shiwalik ranges have a subtropical climate. The Himalayan subtropical pine forests occupy the western end of the subtropical belt, with forests dominated by Chir Pine (Pinus roxburghii). The central part of the range is home to the Himalayan subtropical broadleaf forests, dominated by the sal tree (Shorea robusta). They are at the foot of the Himalayas where the Himalayan streams descend on to the plains.

Shiwalik Hills

Also called Churia or Margalla Hills, Sivalik Hills is an intermittent outermost range of foothills extending across the Himalayan region through Pakistan, India, Nepal and Bhutan. This region consists of many sub-ranges. Summits are generally 600 to 1,200 metres (2,000 to 3,900 ft). Steeper southern slopes form along a fault zone called Himalayan Frontal Thrust (HFT); northern slopes are gentler. Permeable conglomerates and other rocks allow rainwater to percolate downslope into the Bhabhar and Terai, supporting only scrubby forests upslope. The Himalayan subtropical pine and broadleaf forests continue here.

Inner Terai or Dun Valleys

The Inner Terai valleys are open valleys north of Shiwalik Hills or nestled between Shiwalik subranges. Examples include Dehra Dun in India and Chitwan in Nepal. Himalayan subtropical broadleaf forests grow here.

Lesser Himalaya

Also called Mahabharat Range, the Lesser Himalayas is a prominent range 2,000 to 3,000 metres (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 metres (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.

Midlands

This 'hilly' region (Pahad), averaging about 1,000 metres (3,300 ft) immediately north of the Mahabharat Range, rises over about 100 kilometres (330,000 ft) to about 4,000 metres (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 metres (9,800 and 13,100 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 northeastern 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 northeastern Himalayan subalpine conifer forests.

Greater Himalaya

North of the Main Central Thrust, the highest ranges rise abruptly as much as 4,000 metres (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 metres (20,000 ft) north of the Dhaulagiri Himalaya in central Nepal.

Montane grasslands and shrublands grow above treeline. The northwestern 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 northeastern subalpine conifer forests, along the Tibetan border with eastern Nepal, Sikkim, Bhutan, and Arunachal Pradesh. The shrublands 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 metres (11,500 ft) to 5,500 metres (18,000 ft). The grasslands are the summer habitat of the endangered snow leopard (Uncia uncia).

Trans-Himalaya

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 rainshadow effects. These valleys hold some of the highest permanent villages on earth.

Origins and growth

The 6,000 km plus journey of the India landmass (Indian Plate) before its collision with Asia (Eurasian Plate) about 40 to 50 million years ago
Main article: Geology of the Himalaya

The Himalayas are among the youngest mountain ranges on the planet and consist mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, their formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. This is referred to as a fold mountain.

The collision began in the Upper Cretaceous period about 70 million years ago, when the north-moving Indo-Australian Plate, moving at about 15 cm per year, collided with the Eurasian Plate. About 50 million years ago, this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since these sediments were light, they crumpled into mountain ranges rather than sinking to the floor. The Indo-Australian plate continues to be driven horizontally below the Tibetan plateau, which forces the plateau to move upwards. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

The Indo-Australian plate is still moving at 67 mm per year, and 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 makes this region seismically active, leading to earthquakes from time to time.

Glaciers and river systems

The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of freshwater. The 70 km-long Siachen Glacier at the India-Pakistan border is the second longest glacier in the world outside the polar region. Some of the other more famous glaciers include the Gangotri and Yamunotri (Uttarakhand), Nubra, Biafo and Baltoro (Karakoram region), Zemu (Sikkim) and Khumbu glaciers (Mount Everest region).

The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources for several large perennial rivers, most of which combine into two large river systems:

  • The western rivers combine into the Indus Basin, of which the Indus River is the largest. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

The eastern-most Himalayan rivers feed the Ayeyarwady River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and the Huang He (Yellow River) all originate from parts of the Tibetan plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers.[3] In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change.[4] Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers of northern India during the dry seasons.[5]

  • Glaciers near K2 in the People's Republic of China and Pakistan.
    Glaciers near K2 in the People's Republic of China and Pakistan.
  • This image shows the termini of the glaciers in the Bhutan-Himalaya. Glacial lakes have been forming rapidly on the surface of the debris-covered glaciers in this region during the last few decades.
    This image shows the termini of the glaciers in the Bhutan-Himalaya. Glacial lakes have been forming rapidly on the surface of the debris-covered glaciers in this region during the last few decades.
  • Snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in south-western China.
    Snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in south-western China.

Lakes

A high Himalayan lake at an altitude of around 5,000 metres Sikkim, India

The Himalaya region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with a surface area of (700 km²), respectively (638 km²). Other notable lakes include Gurudogmar lake in North Sikkim, Tsongmo lake, near the Indo-China border in Sikkim, and Tilicho lake in Nepal in the Annapurna massif.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.[6]

Impact on climate

Pass in Ladakh with the typical Buddhist prayer flags and chorten

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan plateau. They prevent frigid, dry Arctic winds blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

The mountain ranges also prevent western winter disturbances in Iran from traveling further, resulting in snow in Kashmir and rainfall for parts of Punjab and northern India. Despite being a barrier to the cold, northernly winter winds, the Brahmaputra valley receives part of the frigid winds, thus lowering the temperature in the North East India and Bangladesh.

The Himalayas, which are often called "The Roof of the World", contain the greatest area of glaciers and permafrost outside of the poles. Ten of Asia’s largest rivers flow from here, and more than a billion people’s livelihoods depend on them. To complicate matters, temperatures are rising more rapidly here than the global average. In Nepal, the temperature has risen 0.6 degree C over the last decade, whereas the global warming has been around 0.7 degree C over the last hundred years.[7]

Mountain passes

The Himalayan range at Yumesongdong in Sikkim, in the Yumthang River valley

The rugged terrain makes few routes through the mountains possible. Some of these routes include:

Impact on politics and culture

Mountain sheds like these are used by the rural populace as shelter for cattle in summer months as they take them for grazing in higher altitudes.

It should be noted that almost half of the humans and livestock of India live on one-third of the landscape within 500 km of the Himalayan range.[citation needed]

The Himalayas, due to their large size and expanse, have been a natural barrier to the movement of people for tens of thousands of years. In particular, this has prevented intermingling of people from the Indian subcontinent with people from China and Mongolia, causing significantly different languages and customs between these regions. The Himalayas have also hindered trade routes and prevented military expeditions across its expanse. For instance, Genghis Khan could not expand his empire south of the Himalayas into the subcontinent.

Notable peaks of the Himalayan system (includes outlying ranges)

Peak Name Other names and meaning Elevation (m) Elevation (ft) First Western ascent Notes
Everest Sagarmatha (Nepali), "Head of the World",[8]
Chomolangma (Tibetan), "Goddess mother of the snows"[9]		 8,848 29,035.44 1953 Highest mountain on Earth, on the border between Nepal and Tibet Autonomous Region, People's Republic of China.
K2 Chogo Gangri 8,611 28,251 1954 2nd highest mountain on Earth. Located on the border between the Taxkorgan Tajik Autonomous County of Xinjiang, People's Republic of China and the Northern Areas of Pakistan.
Kangchenjunga Kangchen Dzö-nga, "Five Treasures of the Great Snow" 8,586 28,169 1955 3rd highest mountain on Earth. Located on the border between Nepal and Sikkim, India.
Lhotse "South Peak" 8,516 27,940 1956 4th highest mountain on Earth. Situated between Tibet Autonomous Region, People's Republic of China, and Nepal, in the shadow of Mount Everest.
Makalu "The Great Black" 8,462 27,765 1955 5th highest mountain on Earth. Situated on the border between, Tibet Autonomous Region, People's Republic of China and Nepal.
Cho Oyu Qowowuyag, "Turquoise Goddess" 8,201 26,905 1954 6th highest mountain on Earth. Situated on the border between Tibet Autonomous Region, People's Republic of China, and Nepal
Dhaulagiri "White Mountain" 8,167 26,764 1960 7th highest mountain on Earth. Situated in Nepal.
Manaslu Kutang, "Mountain of the Spirit" 8,156 26,758 1956 8th highest mountain on Earth. Located in the Gurkha Himal, Nepal.
Nanga Parbat Diamir, "Naked Mountain" 8,126 26,660 1953 9th highest mountain on Earth. Located in the Northern Areas of Pakistan.
Annapurna "Goddess of the Harvests" 8,091 26,545 1950 10th highest mountain on Earth. Situated in Nepal.
Gasherbrum I "Beautiful Mountain" 8,080 26,509 1958 11th highest mountain on Earth. Located in the Karakoram of Pakistan
Broad Peak Faichan Kangri 8,047 26,401 1957 12th highest mountain on Earth. Located in the Karakoram of Pakistan.
Gasherbrum II - 8,035 26,362 1956 13th highest mountain on Earth. Located in the Karakoram of Pakistan.
Shishapangma Xixiabangma, "Crest Above The Grassy Plains" 8,013 26,289 1964 14th highest mountain on Earth. Located in Tibet Autonomous Region, People's Republic of China.
Gyachung Kang unknown 7,952 26,089 1964 15th highest mountain on Earth. Located on the border between Tibet Autonomous Region, People's Republic of China, and Nepal, it is the highest mountain under 8,000 meters.
Gasherbrum IV - 7,925 26,001 1958 17th highest mountain on Earth. Located in the Karakoram of Pakistan.
Masherbrum unknown 7,821 25,660 1960 22nd highest mountain on Earth. Located in the Karakoram of Pakistan.
Nanda Devi "Bliss-giving Goddess" 7,817 25,645 1936 23rd highest mountain on Earth. Located in Uttarakhand, India. It is the highest peak entirely within India.
Rakaposhi "Shining Wall" 7,788 25,551 1958 A massive peak that towers above local terrain. Located in the Pakistani Karakoram.
Gangkhar Puensum Gankar Punzum, "Three Mountain Siblings" 7,570 24,836 Unclimbed World's highest unclimbed peak remains off limits to mountaineers. Located in the Kingdom of Bhutan.
Ama Dablam "Mother And Her Necklace" 6,848 22,467 1961 Considered by some[who?] to be one of the most beautiful peaks in the Himalayas. Located in the Khumbu, Nepal.

Panorama

2004 photo mosaic the Himalayas with Makalu and Mount Everest from the International Space Station, Expedition 8.
A panorama of Garhwal Himalaya from Dhanaulti, India

Notable Himalayan mountaineers

  • George Mallory (1886–1924) Attempted first ascent of Mount Everest in 1922 and 1924; died on North Face along with Sandy Irvine.
  • Noel Odell (1890–1987) British. First ascent, in 1936, of Nanda Devi, which remained the highest summitted peak until 1950. Last person to see Mallory and Irvine high up on Everest in 1924.
  • Bill Tilman (1898–1977) British. First ascent of Nanda Devi in 1936. In 1934, first person to penetrate Nanda Devi sanctuary
  • Frank Smythe (1900–1949) British. Kamet, and early attempt on Kangchenjunga.
  • Eric Shipton (1907–1977) British. With Bill Tilman, first to penetrate Nanda Devi sanctuary. Discovered route to Everest over Khumbu Glacier.
  • John Hunt (1910–1998) British. Leader of 1953 expedition of Mount Everest.
  • Tenzing Norgay (1914–1986) Nepalese Sherpa mountaineer. First man on Everest's summit along with Edmund Hillary.
  • Maurice Herzog (b. 1919) First person to summit an Eight-thousander, Annapurna, in 1950. Lost all toes and most fingers due to frostbite. Peak not climbed again until 1970.
  • Sir Edmund Hillary (1919–2008) New Zealand mountaineer and explorer, the first man on Everest's summit along with Tenzing Norgay.
  • Tom Bourdillon (1924–1956) member of British Everest expeditions 1951, 1952, and 1953, reached 300 feet (90 m) from summit of Everest three days before Edmund Hillary and Tenzing Norgay finally conquered it.
  • Hermann Buhl (1924–1957) First ascent of Nanga Parbat in 1953 (feat accomplished solo and without oxygen). First ascent of Broad Peak. Died in fall on Chogolisa, body never found.
  • Willi Unsoeld (1926–1979) United States. First ascent of Everest from West Face and first major traverse of a Himalayan peak, with Tom Hornbein 1963. Daughter Nanda Devi Unsoeld killed during Nanda Devi expedition 1976. Died during avalanche on Mount Rainier, 1979.
  • Chris Bonington (b. 1934) First ascent of Annapurna (South Face), 4 ascents of Everest.
  • Nawang Gombu (b. 1936) Indian mountaineer. First person to climb Everest twice: 1963 and 1965.
  • Jim Whittaker (b. 1936) United States. First American to summit Everest.
  • Reinhold Messner (born 1944) Italian mountaineer. First man to climb all fourteen mountains over 8000 metres (collectively known as the eight-thousanders).
  • Jerzy Kukuczka (1948–1989) Polish mountaineer. Ascended all fourteen eight-thousanders faster than anybody else, establishing ten new routes.
  • Nazir Sabir Pakistani mountaineer. First ascent of two eight thousanders (Broad Peak & Gasherbrum II) in a single attempt.
  • Swami Sundaranand (b. 1926 India) Climbed 25 mountains with little or no equipment from 1950-1990 to experience open eyed Samādhi using the ancient techniques of the Himalayan yogis. Noted also for his extensive photography of the Indian Himalayas.[10][11][12]
  • Casey Mackins An English mountaineer who climbed Mt Everest by a new route without oxygen from Tibet in 1984 and then again from Nepal in 1990 during his famous Sea to Summit expedition where he became the first person to climb Everest starting from sea level
  • José Antonio Delgado Sucre(1965–2006) was the first Venezuelan mountaineer to reach the summit of five eight-thousanders. He was one of the most experienced climbers in Latin America.
  • Ed Viesturs (b. June 22, 1959) is the first American, and 12th person overall, to summit all fourteen eight-thousanders, and the sixth climber to do it without bottled oxygen.
  • Pemba Dorjie (born c. 1977) a Sherpa who currently holds the world record for the quickest climb to the summit of Mount Everest from camp. On May 21, 2004 Dorjie set that record, with a total time of 8 hours and 10 minutes.
  • Apa Sherpa (born c. 1960) On May 21, 2009, successfully summited Mt. Everest for the 19th time, breaking his own record for most successful ascents.
  • Krzysztof Wielicki (born 1950) Polish mountaineer, the fifth man to climb all fourteen eight-thousanders. Three of them (Mount Everest, Kangchenjunga and Lhotse) he ascended as the first man ever to do it in winter.

Religion

The Taktshang Monastery, also known as the "Tiger's Nest"
The Vaishno Devi shrine in Jammu & Kashmir, India.

Several places in the Himalaya are of religious significance in Hinduism and Buddhism. In Hinduism, the Himalaya have also been personified as the god Himavat, the father of Shiva's consort, Parvati.

Some of the important religious places in the Himalayas are:-

In addition to the above, a number of Tibetan Buddhist sites are situated in the Himalaya, including the residence of the Dalai Lama. There were over 6,000 monasteries in Tibet.[13] The Tibetan Muslims had their own mosques in Lhasa and Shigatse.[14]

The following mystic entities are associated with the Himalayas:

  • The Yeti is one of the most famous creatures in cryptozoology. It is a large primate-like creature that is supposed to live in the Himalaya. Most mainstream scientists and experts consider current evidence of the Yeti's existence unpersuasive, and the result of hoaxes, legend or misidentification of mundane creatures.
  • Shambhala is a mystical city with various legends associated with it, it is one of twenty-four Himalayan hidden realms, or beyul, in Vajrayana Buddhism.[15] While some legends consider it to be a real city where secret Buddhist doctrines are being preserved, other legends believe that the city does not physically exist, and can only be reached in the mental realm.
«Tibet. Himalayas», 1933
Nicholas Roerich

The Himalayas in art, literature, and film

See also

References

  1. ^ Yang, Qinye (2004). Himalayan Mountain System. ISBN 9787508506654. Retrieved 2007-08-07.
  2. ^ "Sunderbans the world's largest delta". gits4u.com.
  3. ^ Gaillardet, J (2003). "Geochemistry of the Suspended Sediments of Circum-Himalayan Rivers and Weathering Budgets over the Last 50 Myrs" (PDF). Geophysical Research Abstracts. 5 (13617). Retrieved 2006-11-04. {{cite journal}}: Cite has empty unknown parameters: |month= and |quotes= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  4. ^ "Vanishing Himalayan Glaciers Threaten a Billion". Planet Ark. June 5, 2007. Retrieved 2009-04-17.
  5. ^ "Glaciers melting at alarming speed". People's Daily Online. July 24, 2007. Retrieved 2009-04-17.
  6. ^ Drews, Carl. "Highest Lake in the World". Retrieved 2010-11-14. {{cite web}}: Text "The Highest Lake in the World" ignored (help)
  7. ^ Gravgaard, Anna-Katarina (2009-12-13). "Nepalis note climate change". Global Post.
  8. ^ Unsworth, Walt (2000). Everest - The Mountaineering History (3rd ed.). Bâton Wicks. p. 584. ISBN 978-1898573401. {{cite book}}: Cite has empty unknown parameter: |coauthors= (help)
  9. ^ "No Longer Everest but Mount Qomolangma". People's Daily Online. 2002-11-20. Retrieved 2005-06-09.
  10. ^ United Nations, May 2007, Our Planet magazine
  11. ^ Personal Time with Swami-ji, 157 mins Film, The Center for Healing Arts [1]
  12. ^ Himalaya: Through the Lens of a Sudu Published August 2001 ISBN 81-901326-0-1
  13. ^ Tibetan monks: A controlled life. BBC News. March 20, 2008.
  14. ^ Mosques in Lhasa, Tibet. People's Daily Online. October 27, 2005.
  15. ^ Levine, Norma (1993). Blessing Power of the Buddhas: Sacred Objects, Secret Lands. Element Books. p. 132. ISBN 1-85230-305-0.

Further reading

  • Aitken, Bill, Footloose in the Himalaya, Delhi, Permanent Black, 2003. ISBN 81-7824-052-1
  • Berreman, Gerald Duane, Hindus of the Himalayas: Ethnography and Change, 2nd rev. ed., Delhi, Oxford University Press, 1997.
  • Bisht, Ramesh Chandra, Encyclopedia of the Himalayas, New Delhi, Mittal Publications, c2008.
  • Everest, the IMAX movie (1998). ISBN 0-7888-1493-1
  • Fisher, James F., Sherpas: Reflections on Change in Himalayan Nepal, 1990. Berkeley, University of California Press, 1990. ISBN 0-520-06941-2
  • Gansser, Augusto, Gruschke, Andreas, Olschak, Blanche C., Himalayas. Growing Mountains, Living Myths, Migrating Peoples, New York, Oxford: Facts On File, 1987. ISBN 0-8160-1994-0 and New Delhi: Bookwise, 1987.
  • Gupta, Raj Kumar, Bibliography of the Himalayas, Gurgaon, Indian Documentation Service, 1981
  • Hunt, John, Ascent of Everest, London, Hodder & Stoughton, 1956. ISBN 0-89886-361-9
  • Isserman, Maurice and Weaver, Stewart, Fallen Giants: The History of Himalayan Mountaineering from the Age of Empire to the Age of Extremes. Yale University Press, 2008. ISBN 978-0-300-11501-7
  • Ives, Jack D. and Messerli, Bruno, The Himalayan Dilemma: Reconciling Development and Conservation. London / New York, Routledge, 1989. ISBN 0-415-01157-4
  • Lall, J.S. (ed.) in association with Moddie, A.D., The Himalaya, Aspects of Change. Delhi, Oxford University Press, 1981. ISBN 0-19-561254-X
  • Nandy, S.N., Dhyani, P.P. and Samal, P.K., Resource Information Database of the Indian Himalaya, Almora, GBPIHED, 2006.
  • Palin, Michael, Himalaya, London, Weidenfeld & Nicolson Illustrated, 2004. ISBN 0-297-84371-0
  • Swami Sundaranand, Himalaya: Through the Lens of a Sadhu. Published by Tapovan Kuti Prakashan (August 2001). ISBN 81-901326-0-1
  • Swami Tapovan Maharaj, Wanderings in the Himalayas, English Edition, Madras, Chinmaya Publication Trust, 1960. Translated by T.N. Kesava Pillai.
  • Tilman, H. W., Mount Everest, 1938, Cambridge University Press, 1948.
  • ‘The Mighty Himalaya: A Fragile Heritage,’ National Geographic, 174:624-631(November 1988).
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28°00′N 82°00′E / 28.000°N 82.000°E / 28.000; 82.000

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