Himalayas

Mountain range in Asia

This article is about a mountain range. For other uses, see Himalaya (disambiguation).

Himalaya

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The arc of the Himalayas (also Hindu Kush and Karakorams) showing the eight-thousanders (in red); Indo-Gangetic Plain; Tibetan plateau; rivers Indus, Ganges, and Yarlung Tsangpo-Brahmaputra; and the two anchors of the range (in yellow)

Highest point
Peak| Script error: No such module "WikidataIB"., Script error: No such module "WikidataIB".
Elevation| 8,848.86 m (29,031.7 ft)
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Coordinates| 27°59′N 86°55′E﻿ / ﻿27.983°N 86.917°E﻿ / 27.983; 86.917Coordinates: 27°59′N 86°55′E﻿ / ﻿27.983°N 86.917°E﻿ / 27.983; 86.917
Dimensions
Length| 2,400 km (1,500 mi)
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Naming
Native name| Himālaya (Sanskrit)
Geography

File:Himalaya annotated.jpg

Mount Everest and surrounding peaks as seen from the north-northwest over the Tibetan Plateau. Four eight-thousanders can be seen, Makalu (8,462 m), Everest (8,848 m), Kanchenjunga (8,586 m), and Lhotse (8,516 m).

Countries| Bhutan, China, India, Nepal and Pakistan. Sovereignty in the Kashmir region is disputed by China, India, and Pakistan.
Continent| Asia
Geology
Orogeny| Alpine orogeny
Age of rock| Cretaceous-to-Cenozoic
Type of rock| Metamorphic, sedimentary

Template:Wikidata image

The Himalayas, or Himalaya (/ˌhɪməˈleɪ.ə, hɪˈmɑːləjə/; Sanskrit: [ɦɪmaːlɐjɐ]; from Sanskrit himá 'snow, frost', and ā-laya 'dwelling, abode'),[1] is a mountain range in Asia, separating the plains of the Indian subcontinent from the Tibetan Plateau. The range has some of the planet's highest peaks, including the very highest, Mount Everest. Over 100 peaks exceeding 7,200 m (23,600 ft) in elevation lie in the Himalayas. By contrast, the highest peak outside Asia (Aconcagua, in the Andes) is 6,961 m (22,838 ft) tall.[2]

The Himalayas abut or cross five countries: Bhutan, India, Nepal, China, and Pakistan. The sovereignty of the range in the Kashmir region is disputed among India, Pakistan, and China.[3] The Himalayan range is bordered on the northwest by the Karakoram and Hindu Kush ranges, on the north by the Tibetan Plateau, and on the south by the Indo-Gangetic Plain. Some of the world's major rivers, the Indus, the Ganges, and the Tsangpo–Brahmaputra, rise in the vicinity of the Himalayas, and their combined drainage basin is home to some 600 million people; 53 million people live in the Himalayas.[4] The Himalayas have profoundly shaped the cultures of South Asia and Tibet. Many Himalayan peaks are sacred in Hinduism and Buddhism; the summits of several—Kangchenjunga (from the Indian side), Gangkhar Puensum, Machapuchare, Nanda Devi and Kailas in the Tibetan Transhimalaya—are off-limits to climbers.

Lifted by the subduction of the Indian tectonic plate under the Eurasian Plate, the Himalayan mountain range runs west-northwest to east-southeast in an arc 2,400 km (1,500 mi) long.[5] Its western anchor, Nanga Parbat, lies just south of the northernmost bend of the Indus river. Its eastern anchor, Namcha Barwa, lies immediately west of the great bend of the Yarlung Tsangpo River. The range varies in width from 350 km (220 mi) in the west to 150 km (93 mi) in the east.[6]

## Contents

* 1 Name
* 2 Geography and key features
* 3 Geology
* 4 Hydrology
* 4.1 Glaciers
* 4.2 Lakes
* 5 Climate
* 5.1 Temperature
* 5.2 Precipitation
* 5.3 Winds
* 5.4 Climate change
* 6 Ecology
* 7 Religions
* 8 Resources
* 9 Future Development and climate change adaptation
* 10 See also
* 11 References
* 12 Sources
* 12.1 General
* 12.2 Geology
* 12.3 Climate
* 12.4 Pilgrimage and Tourism
* 13 Further reading
* 14 External links

## Name[edit | edit source]

The name of the range hails from the Sanskrit Himālaya (हिमालय 'abode of the snow'[7]), from himá (हिम 'snow'[8]) and ā-laya (आलय 'home, dwelling'[9]).[10][11] They are now known as "the Himalaya Mountains", usually shortened to "the Himalayas".

The mountains are known as the Himālaya in Nepali and Hindi (both written हिमालय), Himāl (हिमाल) in Kumaoni, the Himalaya (ཧི་མ་ལ་ཡ་) or 'The Land of Snow' (གངས་ཅན་ལྗོངས་) in Tibetan, also known as Himālaya in Sinhala written as හිමාලය, the Himāliya Mountain Range (سلسلہ کوہ ہمالیہ) in Urdu, the Himaloy Parvatmala (হিমালয় পর্বতমালা) in Bengali and the Ximalaya Mountain Range (simplified Chinese: 喜马拉雅山脉; traditional Chinese: 喜馬拉雅山脉; pinyin: Xǐmǎlāyǎ Shānmài) in Chinese.

The name of the range is sometimes also given as Himavan in older writings, including the Sanskrit epic Mahabharata.[12] Himavat (Sanskrit: हिमवत्) or Himavan Himavān (Sanskrit: हिमवान्) is a Hindu deity who is the personification of the Himalayan Mountain Range. Other epithets include Himaraja (Sanskrit: हिमराज, lit. king of snow) or Parvateshwara (Sanskrit: पर्वतेश्वर, lit. lord of mountains).

In western literature, some writers refer to it as the Himalaya. This was also previously transcribed as Himmaleh, as in Emily Dickinson's poetry[13] and Henry David Thoreau's essays.[14]

## Geography and key features[edit | edit source]

See also: List of Himalayan peaks and passes

File:Himalayas Map.png

Map of the Himalayas (including the Hindu Kush)

The Himalayas consist of parallel mountain ranges: the Sivalik Hills on the south; the Lower Himalayan Range; the Great Himalayas, which is the highest and central range; and the Tibetan Himalayas on the north.[15] The Karakoram are generally considered separate from the Himalayas.

In the middle of the great curve of the Himalayan mountains lie the 8,000 m (26,000 ft) peaks of Dhaulagiri and Annapurna in Nepal, separated by the Kali Gandaki Gorge. The gorge splits the Himalayas into Western and Eastern sections both ecologically and orographically – the pass at the head of the Kali Gandaki the Kora La is the lowest point on the ridgeline between Everest and K2 (the highest peak of the Karakoram range). To the east of Annapurna are the 8,000 m (5.0 mi) peaks of Manaslu and across the border in Tibet, Shishapangma. To the south of these lies Kathmandu, the capital of Nepal and the largest city in the Himalayas. East of the Kathmandu Valley lies the valley of the Bhote/Sun Kosi river which rises in Tibet and provides the main overland route between Nepal and China – the Araniko Highway/China National Highway 318. Further east is the Mahalangur Himal with four of the world's six highest mountains, including the highest: Cho Oyu, Everest, Lhotse and Makalu. The Khumbu region, popular for trekking, is found here on the south-western approaches to Everest. The Arun river drains the northern slopes of these mountains, before turning south and flowing to the range to the east of Makalu.

In the far east of Nepal, the Himalayas rise to the Kangchenjunga massif on the border with India, the third highest mountain in the world, the most easterly 8,000 m (26,000 ft) summit and the highest point of India. The eastern side of Kangchenjunga is in the Indian state of Sikkim. Formerly an independent Kingdom, it lies on the main route from India to Lhasa, Tibet, which passes over the Nathu La pass into Tibet. East of Sikkim lies the ancient Buddhist Kingdom of Bhutan. The highest mountain in Bhutan is Gangkhar Puensum, which is also a strong candidate for the highest unclimbed mountain in the world. The Himalayas here are becoming increasingly rugged with heavily forested steep valleys. The Himalayas continue, turning slightly northeast, through the Indian State of Arunachal Pradesh as well as Tibet, before reaching their easterly conclusion in the peak of Namche Barwa, situated in Tibet inside the great bend of the Yarlang Tsangpo river. On the other side of the Tsangpo, to the east, are the Kangri Garpo mountains. The high mountains to the north of the Tsangpo including Gyala Peri, however, are also sometimes included in the Himalayas.

Going west from Dhaulagiri, Western Nepal is somewhat remote and lacks major high mountains, but is home to Rara Lake, the largest lake in Nepal. The Karnali River rises in Tibet but cuts through the centre of the region. Further west, the border with India follows the Sarda River and provides a trade route into China, where on the Tibetan plateau lies the high peak of Gurla Mandhata. Just across Lake Manasarovar from this lies the sacred Mount Kailash in the Kailash Ranges, which stands close to the source of the four main rivers of Himalayas and is revered in Hinduism, Buddhism, Sufism, Jainism, and Bonpo. In Uttarakhand, the Himalayas rise again as the Kumaon and Garhwal Himalayas[16] with the high peaks of Nanda Devi and Kamet. The state is also home to the important pilgrimage destinations of Chaar Dhaam, with Gangotri, the source of the holy river Ganges, Yamunotri, the source of the river Yamuna, and the temples at Badrinath and Kedarnath. Uttarakhand Himalayas are regionally divided into two, namely, Kumaon hills in Kumaon division and Garhwal hills in Garhwal division.[17]

The next Himalayan Indian state, Himachal Pradesh, is noted for its hill stations, particularly Shimla, the summer capital of the British Raj, and Dharamsala, the centre of the Tibetan community and government in exile in India. This area marks the start of the Punjab Himalaya and the Sutlej river, the most easterly of the five tributaries of the Indus, cuts through the range here. Further west, the Himalayas form much of the disputed Indian-administered union territory of Jammu and Kashmir where lies the renowned Kashmir Valley and the town and lakes of Srinagar. The Himalayas form most of the south-west portion of the disputed Indian-administered union territory of Ladakh. The twin peaks of Nun Kun are the only mountains over 7,000 m (4.3 mi) in this part of the Himalayas. Finally, the Himalayas reach their western end in the dramatic 8000 m peak of Nanga Parbat, which rises over 8,000 m (26,000 ft) above the Indus valley and is the most westerly of the 8000 m summits. The western end terminates at a magnificent point near Nanga Parbat where the Himalayas intersect with the Karakoram and Hindu Kush ranges, in the disputed Pakistani-administered territory of Gilgit-Baltistan. Some portion of the Himalayas, such as the Kaghan Valley, Margalla Hills and Galyat tract, extend into the Pakistani provinces of Khyber Pakhtunkhwa and Punjab.

## Geology[edit | edit source]

Main article: Geology of the Himalaya

File:Himalaya-formation.gif

The 6,000-kilometre-plus (3,700 mi) journey of the India landmass (Indian Plate) before its collision with Asia (Eurasian Plate) about 40 to 50 million years ago[18]

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary (Main Himalayan Thrust) between the Indo-Australian Plate and the Eurasian Plate. 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.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian Plate (which has subsequently broken into the Indian Plate and the Australian Plate[19]) was moving at about 15 cm (5.9 in) per year. 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 both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench.[18] An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.[20]

Today, the Indian plate continues to be driven horizontally at the Tibetan Plateau, which forces the plateau to continue to move upwards.[21] The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km (930 mi) 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.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west.[22][23] In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, they joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 m (3,300–6,600 ft).[22][24] While the current valley glaciers of the Himalaya reach at most 20 to 32 km (12 to 20 mi) in length, several of the main valley glaciers were 60 to 112 km (37 to 70 mi) long during the ice age.[22] The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 m (4,590–5,450 ft) lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C (12.6 to 14.9 °F) colder than it is today.[25]

## Hydrology[edit | edit source]

File:Confluence of Indus and Zanskar rivers.jpg

Confluence of the Indus River and Zanskar River in the Himalayas

File:Yumthang valley, Lachung Sikkim India 2012.jpg

Yumthang river valley in Sikkim, India

Despite their scale, the Himalayas do not form a major watershed, and a number of rivers cut through the range, particularly in the eastern part of the range. As a result, the main ridge of the Himalayas is not clearly defined, and mountain passes are not as significant for traversing the range as with other mountain ranges. The rivers of the Himalayas drain into two large river systems:

* The western rivers combine into the Indus Basin. The Indus itself forms the northern and western boundaries of the Himalayas. It begins in Tibet at the confluence of Sengge and Gar rivers and flows north-west through India into Pakistan before turning south-west to the Arabian Sea. It is fed by several major tributaries draining the southern slopes of the Himalayas, including the Jhelum, Chenab, Ravi, Beas and Sutlej rivers, the five rivers of the Punjab.
* The other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.[26]

The northern slopes of Gyala Peri and the peaks beyond the Tsangpo, sometimes included in the Himalayas, drain into the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea. The Salween, Mekong, Yangtze and 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.[27]

### Glaciers[edit | edit source]

The great ranges of central Asia, including the Himalayas, contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic.[28] The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 (2,900 cu mi) of fresh water.[29] Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

File:KhumbuIcefall.jpg

Icefall on Khumbu Glacier

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 m (18,000 ft).[30] In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 m (2,950 ft) lower.[31] The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers.

In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of climate change.[32][33] For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. 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 during the dry seasons.[34][35][36] The global climate change will affect the water resources and livelihoods of the Greater Himalayan region.

### Lakes[edit | edit source]

See also: List of Alpine lakes in India

File:Gurudongmar lake North Sikkim.jpg

Gurudongmar Lake in Sikkim

The Himalayan region is dotted with hundreds of lakes.[37] Pangong Tso, which is spread across the border between India and China, at far western end of Tibet, is among the largest with surface areas of 700 km2 (270 sq mi).

South of the main range, the lakes are smaller. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Other notable lakes include Rara Lake in western Nepal, She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.[37]

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 m (15,030 ft) has grown considerably over the last 50 years due to glacial melting.[38][39] 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 m (18,000 ft).[40]

Temperate Himalayan wetlands provide important habitat and layover sites for migratory birds. Many mid and low altitude lakes remain poorly studied in terms of their hydrology and biodiversity, like Khecheopalri in the Sikkim Eastern Himalayas.[41]

## Climate[edit | edit source]

### Temperature[edit | edit source]

The physical factors determining the climate in any location in the Himalayas include latitude, altitude, and the relative motion of the Southwest monsoon.[42] From south to north, the mountains cover more than eight degrees of latitude, spanning temperate to subtropical zones.[42] The colder air of Central Asia is prevented from blowing down into South Asia by the physical configuration of the Himalayas.[42] This causes the tropical zone to extend farther north in South Asia than anywhere else in the world.[42] The evidence is unmistakable in the Brahmaputra valley as the warm air from the Bay of Bengal bottlenecks and rushes up past Namcha Barwa, the eastern anchor of the Himalayas, and into southeastern Tibet.[42] Temperatures in the Himalayas cool by 2.0 degrees C (3.6 degrees F) for every 300 metres (980 ft) increase of altitude.[42]

As the physical features of mountains are irregular, with broken jagged contours, there can be wide variations in temperature over short distances.[43] Temperature at a location on a mountain depends on the season of the year, the bearing of the sun with respect to the face on which the location lies, and the mass of the mountain, i.e. the amount of matter in the mountain.[43] As the temperature is directly proportional to received radiation from the sun, the faces that receive more direct sunlight also have a greater heat buildup.[43] In narrow valleys—lying between steep mountain faces—there can be dramatically different weather along their two margins.[43] The side to the north with a mountain above facing south can have an extra month of the growing season.[43] The mass of the mountain also influences the temperature, as it acts as a heat island, in which more heat is absorbed and retained than the surroundings, and therefore influences the heat budget or the amount of heat needed to raise the temperature from the winter minimum winter to the summer maximum.[43] The immense scale of the Himalayas means that many summits can create their own weather, the temperature fluctuating from one summit to another, from one face to another, and all may be quite different from the weather in nearby plateaus or valleys.[43]

### Precipitation[edit | edit source]

A critical influence on the Himalayan climate is the Southwest Monsoon. This is not so much the rain of the summer months as the wind that carries the rain.[43] Different rates of heating and cooling between the Central Asian continent and the South Asian ocean create large differences in the atmospheric pressure prevailing above each.[43] In the winter, a high-pressure system forms and remains suspended above Central Asia, forcing air to flow in the southerly direction over the Himalayas.[43] But in Central Asia as there is no substantial source for water to be diffused as vapour, the winter winds blowing across South Asia are dry.[43] In the summer months the Central Asian plateau heats up more than the ocean waters to its south. As a result, the air above it rises higher and higher, creating a zone of low pressure.[43] Off-shore high-pressure systems in the Indian Ocean push the moist summer air inland toward the low-pressure system. When the moist air meets mountains, it rises and upon subsequent cooling, its moisture condenses and is released as rain, typically heavy rain.[43] The wet summer monsoon winds cause precipitation in India and all along the layered southern slopes of the Himalayas. This forced lifting of air is called the orographic effect.[43]

### Winds[edit | edit source]

The vast size, huge altitude range, and complex topography of the Himalayas mean they experience a wide range of climates, from humid subtropical in the foothills to cold and dry desert conditions on the Tibetan side of the range. For much of the Himalayas—in the areas to the south of the high mountains, the monsoon is the most characteristic feature of the climate and causes most of the precipitation, while the western disturbance brings winter precipitation, especially in the west. Heavy rain arrives on the southwest monsoon in June and persists until September. The monsoon can seriously impact transport and cause major landslides. It restricts tourism – the trekking and mountaineering season is limited to either before the monsoon in April/May or after the monsoon in October/November (autumn). In Nepal and Sikkim, there are often considered to be five seasons: summer, monsoon, autumn, (or post-monsoon), winter, and spring.

Using the Köppen climate classification, the lower elevations of the Himalayas, reaching in mid-elevations in central Nepal (including the Kathmandu valley), are classified as Cwa, Humid subtropical climate with dry winters. Higher up, most of the Himalayas have a subtropical highland climate (Cwb).

The intensity of the southwest monsoon diminishes as it moves westward along the range, with as much as 2,030 mm (80 in) of rainfall in the monsoon season in Darjeeling in the east, compared to only 975 mm (38.4 in) during the same period in Shimla in the west.[44][45]

The northern side of the Himalayas, also known as the Tibetan Himalaya, is dry, cold and, generally, windswept particularly in the west where it has a cold desert climate. The vegetation is sparse and stunted and the winters are severely cold. Most of the precipitation in the region is in the form of snow during the late winter and spring months.

File:View on Gyakar (edited).jpg

The cold desert region of Upper Mustang; the region lies to the north of the Annapurna massif (visible in the background)

File:BhurjungKhola-AK1981.jpg

A village in the Pokhara Valley during the monsoon season; the valley lies to the south of the Annapurna massif

Local impacts on climate are significant throughout the Himalayas. Temperatures fall by 0.2 to 1.2 °C for every 100 m (330 ft) rise in altitude.[46] This gives rise to a variety of climates from a nearly tropical climate in the foothills, to tundra and permanent snow and ice at higher elevations. Local climate is also affected by the topography: The leeward side of the mountains receive less rain while the well exposed slopes get heavy rainfall and the rain shadow of large mountains can be significant, for example leading to near desert conditions in the Upper Mustang which is sheltered from the monsoon rains by the Annapurna and Dhaulagiri massifs and has annual precipitation of around 300 mm (12 in), while Pokhara on the southern side of the massifs has substantial rainfall (3,900 mm or 150 in a year). Thus although annual precipitation is generally higher in east than the west, local variations are often more important.

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from 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.[47]

### Climate change[edit | edit source]

This section is an excerpt from Hindu Kush § Climate change.[edit]

File:HKH-Glacier-Mass-Change.png

Observed glacier mass loss in the HKH since the 20th century.

The 2019 Hindu Kush Himalaya Assessment[48] concluded that between 1901 to 2014, the Hindu Kush Himalaya (or HKH) region had already experienced warming of 0.1 °C per decade, with the warming rate accelerating to 0.2 °C per decade over the past 50 years.Over the past 50 years, the frequency of warm days and nights had also increased by 1.2 days and 1.7 nights per decade, while the frequency of extreme warm days and nights had increased by 1.26 days and 2.54 nights per decade. There was also a corresponding decline of 0.5 cold days, 0.85 extreme cold days, 1 cold night, and 2.4 extreme cold nights per decade. The length of the growing season has increased by 4.25 days per decade. There is less conclusive evidence of light precipitation becoming less frequent while heavy precipitation became both more frequent and more intense. Finally, since 1970s glaciers have retreated everywhere in the region beside Karakoram, eastern Pamir, and western Kunlun, where there has been an unexpected increase in snowfall. Glacier retreat had been followed by an increase in the number of glacial lakes, some of which may be prone to dangerous floods.[49]

In the future, if the Paris Agreement goal of 1.5 °C of global warming is not exceeded, warming in the HKH will be at least 0.3 °C higher, and at least 0.7 °C higher in the hotspots of northwest Himalaya and Karakoram. If the Paris Agreement goals are broken, then the region is expected to warm by 1.7–2.4 °C in the near future (2036–2065) and by 2.2–3.3 °C (2066–2095) near the end of the century under the "intermediate" Representative Concentration Pathway 4.5 (RCP4.5). Under the high-warming RCP8.5 scenario where the annual emissions continue to increase for the rest of the century, the expected regional warming is 2.3–3.2 °C and 4.2–6.5 °C, respectively. Under all scenarios, winters will warm more than the summers, and the Tibetan Plateau, the central Himalayan Range, and the Karakoram will continue to warm more than the rest of the region. Climate change will also lead to the degradation of up to 81% of the region's permafrost by the end of the century.[49]

Future precipitation is projected to increase as well, but CMIP5 models struggle to make specific projections due to the region's topography: the most certain finding is that the monsoon precipitation in the region will increase by 4–12% in the near future and by 4–25% in the long term.[49] There has also been modelling of the changes in snow cover, but it is limited to the end of century under the RCP 8.5 scenario: it projects declines of 30–50% in the Indus Basin, 50–60% in the Ganges basin, and 50–70% in the Brahmaputra Basin, as the snowline elevation in these regions will rise by between 4.4 and 10.0 m/yr. There has been more extensive modelling of glacier trends: it is projected that one third of all glaciers in the extended HKH region will be lost by 2100 even if the warming is limited to 1.5 °C (with over half of that loss in the Eastern Himalaya region), while RCP 4.5 and RCP 8.5 are likely to lead to the losses of 50% and >67% of the region's glaciers over the same timeframe. Glacier melt is projected to accelerate regional river flows until the amount of meltwater peaks around 2060, going into an irreversible decline afterwards. Since precipitation will continue to increase even as the glacier meltwater contribution declines, annual river flows are only expected to diminish in the western basins where contribution from the monsoon is low: however, irrigation and hydropower generation would still have to adjust to greater interannual variability and lower pre-monsoon flows in all of the region's rivers.[50][51][52]

## Ecology[edit | edit source]

Main article: Ecology of the Himalayas

File:Hemitragus jemlahicus Jharal.jpg

Male Himalayan tahr

File:RedPandaFullBody.JPG

Red panda

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 southern front of the range. This diversity of altitude, rainfall, and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities.[37] The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.[53][41]

At high altitudes, the elusive and previously endangered snow leopard is the main predator. Its prey includes members of the goat family grazing on the alpine pastures and living on the rocky terrain, notably the endemic bharal or Himalayan blue sheep. The Himalayan musk deer is also found at high altitudes. Hunted for its musk, it is now rare and endangered. Other endemic or near-endemic herbivores include the Himalayan tahr, the takin, the Himalayan serow, and the Himalayan goral. The critically endangered Himalayan subspecies of the brown bear is found sporadically across the range as is the Asian black bear. In the mountainous mixed deciduous and conifer forests of the eastern Himalayas, Red panda feed in the dense understories of bamboo. Lower down the forests of the foothills are inhabited by several different primates, including the endangered Gee's golden langur and the Kashmir gray langur, with highly restricted ranges in the east and west of the Himalayas respectively.[41]

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. Hydrangea hirta is an example of floral species that can be found in this area. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 m (16,080 ft) in Southeastern Tibet.[54]

This section is an excerpt from Hindu Kush § Flora and fauna.[edit]

The mountainous areas of Hindu Kush range are mostly barren or at the most sparsely sprinkled with trees and stunted bushes. From about 1,300 to 2,300 m (4,300 to 7,500 ft), states Yarshater, "sclerophyllous forests are predominant with Quercus and Olea (wild olive); above that, up to a height of about 3,300 m (10,800 ft) one finds coniferous forests with Cedrus, Picea, Abies, Pinus, and junipers". The inner valleys of the Hindu Kush see little rain and have desert vegetation.[55] On the other hand, Eastern Himalaya is home to multiple biodiversity hotspots, and 353 new species (242 plants, 16 amphibians, 16 reptiles, 14 fish, two birds, two mammals and 61+ invertebrates) have been discovered there in between 1998 and 2008, with an average of 35 new species finds every year. With Eastern Himalaya included, the entire Hindu Kush Himalaya region is home to an estimated 35,000+ species of plants and 200+ species of animals.[48]

## Religions[edit | edit source]

File:Taktshang.jpg

The Taktsang Monastery, Bhutan, also known as the "Tiger's Nest"

File:Harmukh Mountain.jpg

Harmukh is a sacred mountain for Hindus located in the Himalayas north of Kashmir Valley.

There are many cultural and mythological aspects associated with the Himalayas. In Jainism, Mount Ashtapad of the Himalayan mountain range, is a sacred place where the first Jain Tirthankara, Rishabhdeva attained moksha. It is believed that after Rishabhdeva attained nirvana, his son, Emperor Bharata Chakravartin, had constructed three stupas and twenty four shrines of the 24 Tirthankaras with their idols studded with precious stones over there and named it Sinhnishdha.[56][57][58] For the Hindus, the Himalayas are personified as Himavat, king of all mountains and the father of the goddess Parvati.[59] The Himalayas are also considered to be the father of Ganga (the personification of river Ganges).[60] Two of the most sacred places of pilgrimage for the Hindus are the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams.[61]

The Buddhists also lay a great deal of importance on the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan.[62] The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa.[63] The Himalayan people's diversity shows in many different ways. It shows through their architecture, their languages, and dialects, their beliefs and rituals, as well as their clothing.[63] The shapes and materials of the people's homes reflect their practical needs and beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display colors and patterns unique to their ethnic backgrounds. Finally, some people place great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry.[63] Several places in the Himalayas are of religious significance in Hinduism, Buddhism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan.[64]

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama.[65] Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries.

## Resources[edit | edit source]

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites.[61] Different parts of the plants – root, flower, stem, leaves, and bark – are used as remedies for different ailments. For example, a bark extract from an Abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an Andrachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a Callicarpa arborea is used for skin ailments.[61] Nearly a fifth of the gymnosperms, angiosperms and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.[61]

Most of the population in some Asian and African countries depends on medicinal plants rather than prescriptions and such.[59] Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region.[59] The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally.[66]

## Future Development and climate change adaptation[edit | edit source]

This section is an excerpt from Hindu Kush § Future development and adaptation.[edit]

A range of adaptation efforts are already undertaken across the HKH region: however, they suffer from underinvestment and insufficient coordination between the various state, institutional and other non-state efforts, and need to be "urgently" strengthened in order to be commensurate with the challenges ahead.[67]

The 2019 Hindu Kush Himalaya Assessment outlined three main "storylines" for the region between now and 2080: "business-as-usual" (or "muddling through"), with no significant change from the current trends and development/adaptation initiatives proceeding as they do now; "downhill", where the intensity of global climate change is high, local initiatives fail and regional cooperation breaks down; and "prosperous", where extensive cooperation allows region's communities to weather "moderate" climate change and increase their living standards while also preserving the region's biodiversity. In addition, it described two alternate pathways through which the "prosperous" future can be achieved: the first focuses on top-down, large-scale development and the latter describes a bottom-up, decentralized alternative.[68]

Pathway 1 [68] Actions  | Benefits  | Need  | Risk

|
|
|

Economic  | Social  | Environmental/climate  | Cross sectoral  | Finance and human resources  | Governance  | Source
Large hydro power generating capacity | Leapfrog in economic prosperity for the region as a whole, high potential for power trade | New skill development, diversified livelihood options | Air pollution reduction, both adaptation and mitigation | Large water storage to manage seasonal variability and strategic cross-sector allocation | Large corporate, global finance, sustained climate finance | HKH institution, regional tariff, cross-border policy coordination | Lack of transboundary sustainable political cooperation; lack of cross-sector water sharing formal arrangements; lack of ecosystem-based design of reservoirs/power plants; public acceptance, silt accumulation
HKH and non-HKH electric grid | Very high economic prosperity for the region and beyond | New skill, non-farm diversified livelihood options | Unplanned local resource extraction will decrease | Reliable power supply for all sectors | Large corporate, global finance, climate finance | HKH electric distribution corporation | Transboundary sustainable political cooperation;lack of ecosystem-based design
HKH ICT (information and communications technology) network | Boost to regional and local economic growth | New skill, non-farm diversified livelihood options | Connectivity across mountainous terrain without ecological impact | Extent of market cutting across sectors and regions | Large corporations, global finance, climate finance | HKH communications corporation | Transboundary sustainable political cooperation; lack of biodiversity-sensitive design
Cross-border trade corridors e.g., silk route re-development | Income, consumption, production leapfrogs as per comparative advantage, benefit to large-scale tourism industry | Food security, energy security, health service, social interdependence, non-farm livelihood generation | Comparative advantage will lead to biodiversity conservation, enhance payment for ecosystem service | Multiple opportunities across sectors emerge | Regional, global | HKH trade authority | Transboundary sustainable political cooperation; lack of biodiversity-sensitive design in transport corridor development
Large water storage and supply | Income, consumption, production leapfrog | Food security, energy security, non-farm water sector livelihood generation | Less GLOF, less flash floods, pump storage facility | Multiple opportunities across sectors emerge | Regional, global | HKH water council | Transboundary sustainable political cooperation; lack of ecosystem-sensitive development
Large water treatment facilities | Leapfrog in water resource management | Water security, non-farm water sector livelihood generation | Reduction in waste disposal | Multiple opportunities across sectors emerge | Regional, global | HKH water council | Transboundary sustainable political cooperation; lack of ecosystem sensitive development
Large-scale urbanization | Leapfrog in economic growth centers | Non-farm water sector livelihood generation | Reserve nature for biodiversity conservation | Multiple opportunities across sectors emerge | Local, national, regional, and global | National urban development authorities | Lack of ecosystem-sensitive development
Large contract farming | Leapfrog in farm-level activity and income | Income, livelihood security | Investment in environmental management | Farming based industrial/trade growth | Local, national, regional, and global | National farming development authorities | Lack of ecosystem-sensitive development; lack of public acceptance, possibility of food crop reduction, crop monoculture
Pathway 2 [68] Actions  | Benefits  | Need  | Risk

|
|
|

Economic  | Social  | Environmental/climate  | Cross sectoral  | Finance and human resources  | Governance  | Source
Distributed small hydro power generating capacity | Incremental national, local economic prosperity through self-sufficiency | Traditional skill utilization | Air pollution reduction, both adaptation and mitigation | Water flow uninterrupted | Small to medium national scale finance, programmatic finance by bundling, climate finance | Community level, local, national, multilevel coordination for tariff, etc. to ensure equity | Lack of local capacity for multi-level governance; lack of upstream- downstream water sharing arrangements; lack of ecosystem-based design
Micro grids | Local economic prosperity | Lack of ecosystem-sensitive development | Small infrastructure with less environmental impact | Reliable power supply for target group | Specialized medium-scale global finance, climate finance | Private, local electric distribution companies | Without multilevel governance, inequality may arise across social groups; not a tried and tested technology; maintenance will need local skill building
National ICT (information and communications technology) network | Incremental national growth | Lack of ecosystem-sensitive development | National connectivity in mountainous terrain improves without ecological impact | Extent of market cutting across sectors | National/global investment negotiated competitively | National institutions | Lack of local/national skill, national negotiation capacity
National culture based products, tourism | Incremental progress | Traditional skill, non-farm livelihood | Environmental conservation | Tourism related infrastructure expansion | Local, national | Local and national institutions | Lack of capacity to integrate with the rest of the world
Decentralized water storage and supply | Incremental progress | Traditional systems to be revived | Environmental conservation | Local infrastructure expansion | Local, national | Local, national | New modern technology to be developed; lack of local/national skill
Decentralized water treatment | Incremental Progress | Traditional systems to be revived | Environmental conservation | Local infrastructure expansion | Local, national | Local, national | New modern technology to be developed; lack of local/national skill
Small settlement planning | Less displacement cost | Less displacement and migration | No change in large-scale land use pattern | Local infrastructure expansion | Local, national | Local, national regulations | Localized environmental impact might go unregulated
Small farming practices | Incremental progress | Continuation of traditional practices | No change in large-scale land use pattern | Local infrastructure expansion | Local, national | Local, national regulations | Localized environmental impact might go unregulated

## See also[edit | edit source]

* Eastern and Western Himalaya
* Indian Himalayan Region
* List of Himalayan peaks and passes
* List of Himalayan topics
* List of mountains in India, Pakistan, Bhutan, Nepal and China
* List of Ultras of the Himalayas
* Trekking peak

## References[edit | edit source]

1. ^ "Himalayan". Oxford English Dictionary (Online ed.). Oxford University Press. Retrieved 2021-08-05. "Etymology: < Himālaya (Sanskrit < hima snow + ālaya dwelling, abode) + -an suffix)" (Subscription or participating institution membership required.)
2. ^ Yang, Qinye; Zheng, Du (2004). Himalayan Mountain System. ISBN 978-7-5085-0665-4. Retrieved 30 July 2016.
3. ^ Bishop, Barry. "Himalayas (mountains, Asia)". Encyclopaedia Britannica. Retrieved 30 July 2016.
4. ^ A.P. Dimri; B. Bookhagen; M. Stoffel; T. Yasunari (8 November 2019). Himalayan Weather and Climate and their Impact on the Environment. Springer Nature. p. 380\. ISBN 978-3-030-29684-1.
5. ^ Wadia, D. N. (1931). "The syntaxis of the northwest Himalaya: its rocks, tectonics and orogeny". Record Geol. Survey of India. 65 (2): 189–220.
6. ^ Apollo, M. (2017). "Chapter 9: The population of Himalayan regions – by the numbers: Past, present and future". In Efe, R.; Öztürk, M. (eds.). Contemporary Studies in Environment and Tourism. Cambridge Scholars Publishing. pp. 143–159.
7. ^ "MW Cologne Scan". www.sanskrit-lexicon.uni-koeln.de. Retrieved 2022-03-27.
8. ^ "MW Cologne Scan". www.sanskrit-lexicon.uni-koeln.de. Retrieved 2022-03-27.
9. ^ "WIL Cologne Scan". www.sanskrit-lexicon.uni-koeln.de. Retrieved 2022-03-27.
10. ^ "BEN Cologne Scan". www.sanskrit-lexicon.uni-koeln.de. Retrieved 2022-03-27.
11. ^ "WIL Cologne Scan". www.sanskrit-lexicon.uni-koeln.de. Retrieved 2022-03-27.
12. ^ Roshen Dalal (2014). Hinduism: An Alphabetical Guide. Penguin Books. ISBN 9788184752779. Entry: "Himavan"
13. ^ Dickinson, Emily, The Himmaleh was known to stoop.
14. ^ Thoreau, Henry David (1849), A Week on the Concord and Merrimack Rivers.
15. ^ Bishop, Barry C.; Chatterjee, Shiba P. Himalayas. Encyclopedia Britannica.
16. ^ Pletcher, Kenneth (March 13, 2009). "Kumaun Himalayas". Encyclopedia Britannica.
17. ^ "Division of the Himalayas: Regional Division of the Himalayas on the Basis of River Valleys". 21 November 2013.
18. ^ a b "The Himalayas: Two continents collide". USGS. 5 May 1999. Retrieved 3 January 2015.
19. ^ "Geologists Find: An Earth Plate Is Breaking in Two". Columbia University. 7 July 1995.
20. ^ Mount Everest – Overview and Information by Matt Rosenberg. ThoughtCo Updated 17 March 2017
21. ^ "Plate Tectonics -The Himalayas". The Geological Society. Retrieved 13 September 2016.
22. ^ a b c Kuhle, M. (2011). "The High Glacial (Last Ice Age and Last Glacial Maximum) Ice Cover of High and Central Asia, with a Critical Review of Some Recent OSL and TCN Dates". In Ehlers, J.; Gibbard, P.L.; Hughes, P.D. (eds.). Quaternary Glaciation – Extent and Chronology, A Closer Look. Amsterdam: Elsevier BV. pp. 943–965.
23. ^ glacier maps downloadable
24. ^ Kuhle, M. (1987). "Subtropical mountain- and highland-glaciation as ice age triggers and the waning of the glacial periods in the Pleistocene". GeoJournal. 14 (4): 393–421. doi:10.1007/BF02602717. S2CID 129366521.
25. ^ Kuhle, M. (2005). "The maximum Ice Age (Würmian, Last Ice Age, LGM) glaciation of the Himalaya – a glaciogeomorphological investigation of glacier trim-lines, ice thicknesses and lowest former ice margin positions in the Mt. Everest-Makalu-Cho Oyu massifs (Khumbu- and Khumbakarna Himal) including information on late-glacial-, neoglacial-, and historical glacier stages, their snow-line depressions and ages". GeoJournal. 62 (3–4): 193–650. doi:10.1007/s10708-005-2338-6.
26. ^ "Sunderbans the world's largest delta". gits4u.com. Archived from the original on 3 January 2015. Retrieved 3 January 2015.
27. ^ Gaillardet, J.; Métivier, F.; Lemarchand, D.; Dupré, B.; Allègre, C.J.; Li, W.; Zhao, J. (2003). "Geochemistry of the Suspended Sediments of Circum-Himalayan Rivers and Weathering Budgets over the Last 50 Myrs" (PDF). Geophysical Research Abstracts. 5: 13,617. Bibcode:2003EAEJA....13617G. Abstract 13617. Archived (PDF) from the original on 2022-10-09. Retrieved 4 November 2006.
28. ^ "The Himalayas – Himalayas Facts". Nature on PBS. 11 February 2011. Retrieved 21 January 2014.
29. ^ "the Himalayan Glaciers". Fourth assessment report on climate change. IPPC. 2007. Retrieved 22 January 2014.
30. ^ Shi, Yafeng; Xie, Zizhu; Zheng, Benxing; Li, Qichun (1978). "Distribution, Feature and Variations of Glaciers in China" (PDF). World Glacier Inventory. Archived from the original (PDF) on 24 April 2013.
31. ^ Henderson-Sellers, Ann; McGuffie, Kendal (2012). The Future of the World's Climate: A Modelling Perspective. pp. 199–201. ISBN 978-0-12-386917-3.
32. ^ Lee, Ethan; Carrivick, Jonathan L.; Quincey, Duncan J.; Cook, Simon J.; James, William H. M.; Brown, Lee E. (2021-12-20). "Accelerated mass loss of Himalayan glaciers since the Little Ice Age". Scientific Reports. 11 (1): 24284. Bibcode:2021NatSR..1124284L. doi:10.1038/s41598-021-03805-8. ISSN 2045-2322. PMC 8688493. PMID 34931039.
33. ^ "Vanishing Himalayan Glaciers Threaten a Billion". Reuters. 4 June 2007. Retrieved 13 March 2018.
34. ^ Kaushik, Saurabh; Rafiq, Mohammd; Joshi, P.K.; Singh, Tejpal (April 2020). "Examining the glacial lake dynamics in a warming climate and GLOF modelling in parts of Chandra basin, Himachal Pradesh, India". Science of the Total Environment. 714: 136455. Bibcode:2020ScTEn.714m6455K. doi:10.1016/j.scitotenv.2019.136455. PMID 31986382. S2CID 210933887.
35. ^ Rafiq, Mohammd; Romshoo, Shakil Ahmad; Mishra, Anoop Kumar; Jalal, Faizan (January 2019). "Modelling Chorabari Lake outburst flood, Kedarnath, India". Journal of Mountain Science. 16 (1): 64–76. doi:10.1007/s11629-018-4972-8. ISSN 1672-6316. S2CID 134015944.
36. ^ "Glaciers melting at alarming speed". People's Daily Online. 24 July 2007. Retrieved 17 April 2009.
37. ^ a b c O'Neill, A. R. (2019). "Evaluating high-altitude Ramsar wetlands in the Sikkim Eastern Himalayas". Global Ecology and Conservation. 20 (e00715): 19. doi:10.1016/j.gecco.2019.e00715.
38. ^ "Photograph of Tsho Rolpa".
39. ^ Tsho Rolpa
40. ^ Drews, Carl. "Highest Lake in the World". Retrieved 14 November 2010.
41. ^ a b c O'Neill, Alexander; et al. (25 February 2020). "Establishing Ecological Baselines Around a Temperate Himalayan Peatland". Wetlands Ecology & Management. 28 (2): 375–388. doi:10.1007/s11273-020-09710-7. S2CID 211081106.
42. ^ a b c d e f Zurick & Pacheco 2006, p. 50.
43. ^ a b c d e f g h i j k l m n Zurick & Pacheco 2006, pp. 50–51.
44. ^ "Climate of the Himalayas". Encyclopedia Britannica. Retrieved 18 May 2022.
45. ^ Zurick, David; Pocheco, Julsun (2006), Illustrated Atlas of the Himalaya, University Press of Kentucky, p. 52, ISBN 9780813173849
46. ^ Romshoo, Shakil Ahmad; Rafiq, Mohammd; Rashid, Irfan (March 2018). "Spatio-temporal variation of land surface temperature and temperature lapse rate over mountainous Kashmir Himalaya". Journal of Mountain Science. 15 (3): 563–576. doi:10.1007/s11629-017-4566-x. ISSN 1672-6316. S2CID 134568990.
47. ^ Devitt, Terry (3 May 2001). "Climate shift linked to rise of Himalayas, Tibetan Plateau". University of Wisconsin–Madison News. Retrieved 1 November 2011.
48. ^ a b Wester, Philippus; Mishra, Arabinda; Mukherji, Aditi; Shrestha, Arun Bhakta (2019). The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. doi:10.1007/978-3-319-92288-1. ISBN 978-3-319-92288-1. }}
49. ^ a b c Krishnan, Raghavan; Shrestha, Arun Bhakta; Ren, Guoyu; Rajbhandari, Rupak; Saeed, Sajjad; Sanjay, Jayanarayanan; Syed, Md. Abu.; Vellore, Ramesh; Xu, Ying; You, Qinglong; Ren, Yuyu (5 January 2019). "Unravelling Climate Change in the Hindu Kush Himalaya: Rapid Warming in the Mountains and Increasing Extremes". The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. pp. 57–97. doi:10.1007/978-3-319-92288-1_3.
50. ^ Damian Carrington (4 February 2019). "A third of Himalayan ice cap doomed, finds report". Retrieved 20 October 2022.
51. ^ Bolch, Tobias; Shea, Joseph M.; Liu, Shiyin; Azam, Farooq M.; Gao, Yang; Gruber, Stephan; Immerzeel, Walter W.; Kulkarni, Anil; Li, Huilin; Tahir, Adnan A.; Zhang, Guoqing; Zhang, Yinsheng (5 January 2019). "Status and Change of the Cryosphere in the Extended Hindu Kush Himalaya Region". The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. pp. 209–255. doi:10.1007/978-3-319-92288-1_7.
52. ^ Scott, Christopher A.; Zhang, Fan; Mukherji, Aditi; Immerzeel, Walter; Mustafa, Daanish; Bharati, Luna (5 January 2019). "Water in the Hindu Kush Himalaya". The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. pp. 257–299. doi:10.1007/978-3-319-92288-1_8.
53. ^ Hogan, C. Michael (2010). Monosson, E. (ed.). "Extremophile". Encyclopedia of Earth. Washington, DC: National Council for Science and the Environment.
54. ^ Miehe, Georg; Miehe, Sabine; Vogel, Jonas; Co, Sonam; Duo, La (May 2007). "Highest Treeline in the Northern Hemisphere Found in Southern Tibet" (PDF). Mountain Research and Development. 27 (2): 169–173. doi:10.1659/mrd.0792. hdl:1956/2482. S2CID 6061587. Archived from the original (PDF) on 6 June 2013.
55. ^ Ehsan Yarshater (2003). Encyclopædia Iranica. The Encyclopaedia Iranica Foundation. p. 312\. ISBN 978-0-933273-76-4.
56. ^ Jain, Arun Kumar (2009). Faith & Philosophy of Jainism. ISBN 978-81-7835-723-2.
57. ^ "To heaven and back". The Times of India. 11 January 2012. Archived from the original on 7 July 2012. Retrieved 2 March 2012.
58. ^ Jain, Arun Kumar (2009). Faith & Philosophy of Jainism. ISBN 978-81-7835-723-2.
59. ^ a b c Gupta, Pankaj; Sharma, Vijay Kumar (2014). Healing Traditions of the Northwestern Himalayas. Springer Briefs in Environmental Science. ISBN 978-81-322-1925-5.
60. ^ Dallapiccola, Anna (2002). Dictionary of Hindu Lore and Legend. ISBN 978-0-500-51088-9.
61. ^ a b c d Jahangeer A. Bhat; Munesh Kumar; Rainer W. Bussmann (2 January 2013). "Ecological status and traditional knowledge of medicinal plants in Kedarnath Wildlife Sanctuary of Garhwal Himalaya, India". Journal of Ethnobiology and Ethnomedicine. 9: 1. doi:10.1186/1746-4269-9-1. PMC 3560114. PMID 23281594.
62. ^ Cantor, Kimberly (14 July 2016). "Paro, Bhutan: The Tiger's Nest". Huffington Post. Retrieved 9 June 2018.
63. ^ a b c Zurick, David; Julsun, Pacheco; Basanta, Raj Shrestha; Birendra, Bajracharya (2006). Illustrated Atlas of the Himalaya. Lexington: U of Kentucky.
64. ^ Pommaret, Francoise (2006). Bhutan Himalayan Mountains Kingdom (5th ed.). Odyssey Books and Guides. pp. 136–137. ISBN 978-962-217-810-6.
65. ^ "Tibetan monks: A controlled life". BBC News. 20 March 2008.
66. ^ "Himalayan Forests Disappearing". Earth Island Journal. 21 (4): 7–8. 2006.
67. ^ Mishra, Arabinda; Appadurai, Arivudai Nambi; Choudhury, Dhrupad; Regmi, Bimal Raj; Kelkar, Ulka; Alam, Mozaharul; Chaudhary, Pashupati; Mu, Seinn Seinn; Ahmed, Ahsan Uddin; Lotia, Hina; Fu, Chao; Namgyel, Thinley; Sharma, Upasna (5 January 2019). "Adaptation to Climate Change in the Hindu Kush Himalaya: Stronger Action Urgently Needed". The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. pp. 457–490. doi:10.1007/978-3-319-92288-1_13.
68. ^ a b c Roy, Joyashree; Moors, Eddy; Murthy, M. S. R.; Prabhakar, V. R. K.; Khattak, Bahadar Nawab; Shi, Peili; Huggel, Christian; Chitale, Vishwas (5 January 2019). "Exploring Futures of the Hindu Kush Himalaya: Scenarios and Pathways". The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People. pp. 99–125. doi:10.1007/978-3-319-92288-1_4.

## Sources[edit | edit source]

### General[edit | edit source]

* Wester, Philippus; Mishra, Arabinda; Mukherji, Aditi; Shrestha, Arun Bhakta, eds. (2019), The Hindu Kush Himalya Assessment: Mountains, Climate Change, Sustainability and People, Springer Open, ICIMOD, HIMAP, ISBN 978-3-319-92287-4, LCCN 2018954855
* Zurick, David; Pacheco, Julsun (2006), Illustrated Atlas of the Himalayas, with Basanta Shrestha and Birendra Bajracharya, Lexington: University Press of Kentucky, ISBN 9780813123882, OCLC 1102237054

### Geology[edit | edit source]

* Chakrabarti, B. K. (2016). Geology of the Himalayan Belt: Deformation, Metamorphism, Stratigraphy. Amsterdam and Boston: Elsevier. ISBN 978-0-12-802021-0.
* Davies, Geoffrey F. (2022). Stories from the Deep Earth: How Scientists Figured Out What Drives Tectonic Plates and Mountain Building. Cham, Switzerland: Springer Nature. doi:10.1007/978-3-030-91359-5. ISBN 978-3-030-91358-8.
* Frisch, Wolfgang; Meschede, Martin; Blakey, Ronald (2011). Plate Tectonics: Continental Drift and Mountain Building. Heidelberg: Springer. doi:10.1007/978-3-540-76504-2. ISBN 978-3-540-76503-5.

### Climate[edit | edit source]

* Clift, Peter D.; Plumb, R. Alan (2008), The Asian Monsoon: Causes, History and Effects, Cambridge and New York: Cambridge University Press, ISBN 978-0-521-84799-5
* Barry, Roger E (2008), Mountain Weather and Climate (3rd ed.), Cambridge and New York: Cambridge University Press, ISBN 978-0-521-86295-0

### Pilgrimage and Tourism[edit | edit source]

* Bleie, Tone (2003), "Pilgrim Tourism in the Central Himalayas: The Case of Manakamana Temple in Gorkha, Nepal", Mountain Research and Development, International Mountain Society, 23 (2): 177–184, doi:10.1659/0276-4741(2003)023[0177:PTITCH]2.0.CO;2, S2CID 56120507
* Howard, Christopher A (2016), Mobile Lifeworlds: An Ethnography of Tourism and Pilgrimage in the Himalayas, New York: Routledge, doi:10.4324/9781315622026, ISBN 9780367877989
* Humbert-Droz, Blaise (2017), "Impacts of Tourism and Military Presence on Wetlands and Their Avifauna in the Himalayas", in Prins, Herbert H. T.; Namgail, Tsewang (eds.), Bird Migration across the Himalayas Wetland Functioning amidst Mountains and Glaciers, Foreword by H.H. The Dali Lama, Cambridge, UK: Cambridge University Press, pp. 343–358, ISBN 978-1-107-11471-5
* Lim, Francis Khek Ghee (2007), "Hotels as sites of power: tourism, status, and politics in Nepal Himalaya", Journal of the Royal Anthropological Institute, New Series, Royal Anthropological Institute, 13 (3): 721–738, doi:10.1111/j.1467-9655.2007.00452.x
* Nyaupane, Gyan P.; Chhetri, Netra (2009), "Vulnerability to Climate Change of Nature-Based Tourism in the Nepalese Himalayas", Tourism Geographies, 11 (1): 95–119, doi:10.1080/14616680802643359, S2CID 55042146
* Nyaupane, Gyan P.; Timothy, Dallen J., eds. (2022), Tourism and Development in the Himalya: Social, Environmental, and Economic Forces, Routledge Cultural Heritage and Tourism Series, London and New York: Routledge, ISBN 9780367466275
* Pati, Vishwambhar Prasad (2020), Sustainable Tourism Development in the Himalya: Constraints and Prospects, Environmental Science and Engineering, Cham, Switzerland: Springer Nature, doi:10.1007/978-3-030-58854-0, ISBN 978-3-030-58853-3, S2CID 229256111
* Serenari, Christopher; Leung, Yu-Fai; Attarian, Aram; Franck, Chris (2012), "Understanding environmentally significant behavior among whitewater rafting and trekking guides in the Garhwal Himalaya, India", Journal of Sustainable Tourism, 20 (5): 757–772, doi:10.1080/09669582.2011.638383, S2CID 153859477

## Further reading[edit | edit source]

* 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.
* Edmundson, Henry, Tales from the Himalaya, Vajra Books, Kathmandu, 2019. ISBN 978-9937-9330-3-2
* 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.
* Swami Sundaranand, Himalaya: Through the Lens of a Sadhu. Published by Tapovan Kuti Prakashan (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.
* Turner, Bethan, et al. Seismicity of the Earth 1900–2010: Himalaya and Vicinity. Denver, United States Geological Survey, 2013.

## External links[edit | edit source]

* The Digital Himalaya research project at Cambridge and Yale (archived)
* Geology of the Himalayan mountains
* Birth of the Himalaya
* South Asia's Troubled Waters Journalistic project at the Pulitzer Centre for Crisis Reporting (archived)
* Biological diversity in the Himalayas Encyclopedia of Earth

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Geography of South Asia

Mountains|

* Himalayas
* Mount Everest
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Plateaus|

* Deccan Plateau
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Deserts|

* Thar Desert

Lowlands|

* Indo-Gangetic plain
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Islands|

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By country|

* India
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Himalayan earthquakes

Notable Himalayan quakes|

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Plate tectonics|

* Geology of the Himalayas
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Physical geography

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File:Land ocean ice cloud hires.jpg

* Category
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Nepal articles

History|

| Ancient|

* Bhadrabahu

| Shakya Republic|

* Gautama Buddha
* Maya (mother of Buddha)

|

Kirata Kingdom|

* Yalamber

Lichchhavi rule|

* Manadeva
* Amshuverma
* Bhrikuti
* Araniko

Medieval
and
modern|

* Arimalla
* Khasa kingdom
* Baise Rajya
* Chaubisi Rajya
* Newa kingdoms

| Early Shah rule|

* Gorkha Kingdom
* Prithvi Narayan Shah
* Unification
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* Sino-Nepal War
* Bhimsen Thapa
* Anglo-Nepal War
* Balbhadra Kunwar
* Treaty of Sugauli

|

Rana rule|

* Kot massacre
* Jung Bahadur Rana
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* Britain Treaty (1923)
* Congress

Post-democracy|

* Democracy movements
* Jana Andolan I
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* Ganesh Man Singh
* B. P. Koirala
* Birendra
* Royal massacre
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* 2015 Earthquake

File:Emblem of Nepal (2020).svg

Geography|

| Mountains|

* Himalayas
* Mount Everest
* Kanchenjunga
* Makalu
* Dhaulagiri
* Manaslu
* Annapurna

|

Areas|

* Borders
* Kathmandu Valley
* Terai
* Inner Terai Valleys of Nepal
* Tibetan Plateau
* Siliguri Corridor (Chicken's Neck)

Rivers|

* Arun
* Karnali (Ghaghara)
* Koshi (Kosi)
* Narayani (Gandaki)
* West Rapti

Environment|

* Climate change
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* Wildlife

Politics|

* Constitution
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| Divisions|

* Districts
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|

Cities|

* Bharatpur
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* Lalitpur
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* Pokhara

Economy|

* Agriculture
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Culture|

* Cuisine
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| Festivals|

* Dashain
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| Celebrations|

* Nwaran
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|

Issues|

* Witch-hunts
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* Outline
* Index
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* Category

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Kosi basin

Rivers|

* Arun/Bum-chu
* Barun
* Bhotekoshi
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* Hongu
* Imja Khola
* Indravati
* Kosi
* Sabha
* Sangkhuwa
* Siswa
* Sunkoshi or Matsang Tsangpo
* Tamur

Dams, barrages, bridges|

* Koshi Barrage
* Kosi embankment
* Sino-Nepal Friendship Bridge

Geographical features|

* Tibetan Plateau
* Himalayas
* Mahabharat Range (Lower Himalayan Range)
* Sivalik Hills
* Chatra Gorge

Important localities|

* Nyalam/ Tsongdu
* Kodari
* Dolalghat
* Bahrabise
* Namche Bazaar
* Lukla
* Bhimnagar
* Supaul
* Khagaria

Floods|

* Floods in Bihar
* 2008 Bihar flood

Riparian districts/ areas|

| Tibet Autonomous Region of China|

* Nyalam County
* Tingri County

|

Nepal|

* Kosi Zone
* Sagarmatha Zone

Bihar, India|

* Darbhanga division
* Kosi division
* Purnia division
* Munger division

Languages/ people|

* Standard Tibetan
* Nepali
* Nepal Bhasa/Newari
* Limbu
* Maithili
* Bajjika

Transport|

* Friendship Highway
* Araniko Highway
* Mahendra Highway
* NH 27
* NH 106
* NH 107

Other basins|

* Damodar
* Godavari
* Mahanadi–Brahmani–Baitarani
* Narmada
* Son

* v
* t
* e

Mountain ranges of China

Geography of China

Northwest China|

* Altai Mountains
* Dzungarian Alatau
* Tian Shan
* Borohoro Mountains
* Tarbagatai Mountains
* Kunlun Mountains
* Altyn-Tagh
* Qilian Mountains
* Helan Mountains
* Liupan Mountains

Qinghai-Tibet
and Southwest China|

* Himalayas
* Transhimalaya
* Pamir Mountains
* Karakoram
* Argu Tagh
* Yengisogat
* Kunlun Mountains
* Hoh Xil
* Bayan Har Mountains
* Amne Machin
* Tanggula Mountains
* Nyenchen Tanglha Mountains
* Hengduan Mountains
* Gaoligong Mountains
* Yunling Mountains
* Ailao Mountains
* Qionglai Mountains
* Daxue Mountains
* Min Mountains

Northeast China|

* Greater Khingan
* Lesser Khingan
* Changbai Mountains
* Wanda Mountains
* Qian Mountains

North and East China|

* Yin Mountains
* Lang Mountains
* Lüliang Mountains
* Taihang Mountains
* Zhongtiao Mountains
* Mount Tai
* Tianmu Mountain

* Yandang Mountains
* Wuyi Mountains

Central China|

* Qinling
* Daba Mountains
* Dabie Mountains
* Wudang Mountains
* Jingshan Mountains
* Luoxiao Mountains
* Jiuling Mountains
* Mufu Mountains
* Wugong Mountains
* Huangshan
* Wuling Mountains
* Xuefeng Mountains

South China|

* Cang Mountain
* Daliang Mountains
* Dalou Mountains
* Nanling Mountains
* Jiuyi Mountains
* Yuecheng Mountains
* Longmen Mountains
* Western Mountains

Landforms of China

* v
* t
* e

Earth's primary regions and subregions

* v
* t
* e

Regions of Africa

Central|

* Guinea region
* Gulf of Guinea
* Cape Lopez
* Mayombe
* Igboland
* Mbaise
* Pool Malebo
* Congo Basin
* Chad Basin
* Cameroonian Highlands forests
* East Sudanian savanna
* Congolian rainforests
* Ouaddaï highlands
* Ennedi Plateau

East|

* African Great Lakes
* Albertine Rift
* East African Rift
* Great Rift Valley
* Gregory Rift
* Rift Valley lakes
* Virunga Mountains
* Kavirondo
* Zanj
* East African montane forests
* Eastern Arc Mountains
* Serengeti
* Horn of Africa
* Afar Triangle
* Al-Habash
* Barbaria
* Danakil Alps
* Danakil Desert
* Ethiopian Highlands
* Dahlak Archipelago
* Hanish Islands
* Gulf of Aden
* Gulf of Tadjoura
* Red Sea
* Indian Ocean islands
* Comoro Islands
* Lamu Archipelago
* Madagascar
* Central Highlands (Madagascar)
* Northern Highlands
* Zanzibar Archipelago
* Swahili coast

North|

* Eastern Desert
* Maghreb
* Ancient Libya
* Atlas Mountains
* Barbary Coast
* Gibraltar Arc
* Ifriqiya
* Nile Valley
* Nile Delta
* Bashmur
* Cataracts of the Nile
* Darfur
* Lower Egypt
* Lower Nubia
* Middle Egypt
* Nile Delta
* Nuba Mountains
* Nubia
* The Sudans
* Upper Egypt
* Tibesti Mountains
* Western Sahara

South|

* Rhodesia
* North
* South
* Thembuland
* Succulent Karoo
* Nama Karoo
* Bushveld
* Maputaland
* Highveld
* Fynbos
* Indian Ocean coastal belt
* Albany thickets
* Cape Floristic Region
* Skeleton Coast
* Kalahari Desert
* Okavango Delta
* Cape Peninsula
* False Bay

West|

* Pepper Coast
* Gold Coast
* Slave Coast
* Ivory Coast
* Cape Palmas
* Cape Mesurado
* Guinea region
* Guinean Forests of West Africa
* Upper Guinean forests
* Lower Guinean forests
* Guinean forest-savanna mosaic
* Guinea Highlands
* Gulf of Guinea
* Dahomey Gap
* Niger Basin
* Niger Delta
* Inner Niger Delta
* West Sudanian savanna
* Yorubaland

Macro-regions|

* Aethiopia
* Afromontane
* Arab world
* Commonwealth realm
* Equatorial Africa
* Françafrique
* Greater Middle East
* Guineo-Congolian region
* Islands of Africa
* List of countries where Arabic is an official language
* Mediterranean Basin
* MENA
* MENASA
* Middle East
* Miombo woodlands
* Mittelafrika
* Negroland
* Northeast Africa
* Portuguese-speaking African countries
* Sahara
* Sahel
* Southeast Africa
* Sub-Saharan Africa
* Sudan (region)
* Sudanian savanna
* Tropical Africa
* Zambezian region

* v
* t
* e

Regions of Asia

Central
(The 'stans)|

* Roof of the World
* Greater Middle East
* Aral Sea
* Aralkum Desert
* Caspian Sea
* Dead Sea
* Sea of Galilee
* Tartary
* Transoxiana
* Turan
* Greater Khorasan
* Ariana
* Arachosia
* Khwarazm
* Sistan
* Kazakhstania
* Kazakh Steppe
* Betpak-Dala
* Eurasian Steppe
* Kazakh Steppe
* Mongolian–Manchurian grassland
* Iranian Plateau
* Altai Mountains
* Pamir Mountains
* Tian Shan
* Badakhshan
* Wakhan Corridor
* Wakhjir Pass
* Mount Imeon
* Mongolian Plateau
* Western Regions
* Taklamakan Desert
* Karakoram
* Trans-Karakoram Tract
* Siachen Glacier
* Tibetan Plateau

East
(Northeast)|

* Orient
* Japanese Archipelago
* Northeastern Japan Arc
* Sakhalin Island Arc
* Korea
* Gobi Desert
* Taklamakan Desert
* Greater Khingan
* Mongolian Plateau
* Inner Asia
* Inner Mongolia
* Outer Mongolia
* China proper
* Manchuria
* Outer Manchuria
* Inner Manchuria
* Northeast China Plain
* Mongolian–Manchurian grassland
* North China Plain
* Yan Mountains
* Liaodong Peninsula
* High-mountain Asia
* Himalayas
* Tibetan Plateau
* Karakoram
* Kunlun Mountains
* Qilian Mountains
* Hengduan Mountains
* Tarim Basin
* Qinling Mountains
* Sichuan Basin
* Northern Silk Road
* Hexi Corridor
* Yunnan–Guizhou Plateau
* Lingnan
* Liangguang
* Jiangnan
* Jianghuai
* Guanzhong
* Huizhou
* Wu
* Jiaozhou
* Zhongyuan
* Shaannan
* Ordos Loop
* Loess Plateau
* Shaanbei
* Hamgyong Mountains
* Central Mountain Range
* Japanese Alps
* Suzuka Mountains
* Leizhou Peninsula
* Gulf of Tonkin
* Yangtze
* Yangtze Delta
* Yellow River
* Pearl River Delta
* Yenisey Basin
* Altai Mountains
* Wakhan Corridor
* Wakhjir Pass
* Far East
* Ring of Fire
* Asia-Pacific
* Tropical Asia

North
(Siberia)|

* Arctic
* Arctic Circle
* Inner Asia
* Northeast
* Ural
* Ural Mountains
* Far East
* Russian Far East
* Okhotsk–Manchurian taiga
* Beringia
* Chukchi Peninsula
* Kamchatka Peninsula
* Extreme North
* Tartary
* Siberia
* Baikalia (Lake Baikal)
* Baraba steppe
* Khatanga Gulf
* Transbaikal
* West
* Amur Basin
* Yenisey Gulf
* Yenisey Basin
* Sikhote-Alin
* Kolyma
* Bering Strait
* Ring of Fire
* Outer Manchuria
* Asia-Pacific

Southeast
(East Indies)|

* Orient
* Sundaland
* Mainland/Indochina
* Northern Triangle temperate forests
* Maritime/Malay Archipelago
* Peninsular Malaysia
* Sunda Islands
* Greater Sunda Islands
* Lesser Sunda Islands
* Indonesian Archipelago/Nusantara
* Wallacea
* Timor
* Philippine Archipelago
* Luzon
* Mindanao
* Visayas
* Leyte Gulf
* Gulf of Thailand
* East Indies
* Nanyang
* Alpide belt
* Far East
* Ring of Fire
* Asia-Pacific
* Tropical Asia

South
(Indian
Subcontinent)|

* Orient
* Greater India
* Indian subcontinent
* Himalayas
* Kangchenjunga
* Nanda Devi
* Hindu Kush
* Bactria
* Carnatic region
* Tamilakam
* Western Ghats
* Eastern Ghats
* Ganges Basin
* Ganges Delta
* Guzgan
* Pashtunistan
* Punjab
* Balochistan
* Gedrosia
* Makran
* Marathwada
* Kashmir
* Kashmir Valley
* Pir Panjal Range
* Thar Desert
* Indus Valley
* Indus River Delta
* Indus Valley Desert
* Indo-Gangetic Plain
* Eastern Coastal Plains
* Kalinga
* Western Coastal Plains
* Meghalaya subtropical forests
* Lower Gangetic Plains moist deciduous forests
* Northwestern Himalayan alpine shrub and meadows
* Doab
* Bagar tract
* Great Rann of Kutch
* Little Rann of Kutch
* Deccan Plateau
* Coromandel Coast
* Konkan
* False Divi Point
* Hindi Belt
* Ladakh
* Aksai Chin
* Gilgit-Baltistan
* Baltistan
* Shigar Valley
* High-mountain Asia
* Karakoram
* Saltoro Mountains
* Siachen Glacier
* Bengal
* Bay of Bengal
* Gulf of Khambhat
* Gulf of Kutch
* Halar
* Gulf of Mannar
* Palk Strait
* Trans-Karakoram Tract
* Wakhan Corridor
* Wakhjir Pass
* Lakshadweep
* Laccadive Islands
* Aminidivi
* Paropamisadae
* Andaman and Nicobar Islands
* Andaman Islands
* Nicobar Islands
* Maldives
* Alpide belt
* Asia-Pacific
* Tropical Asia
* Tibetan Plateau

West
(Middle East)|

* Greater Middle East
* MENA
* Middle East
* Red Sea
* Hanish Islands
* Caspian Sea
* Mediterranean Sea
* Zagros Mountains
* Elam
* Persian Gulf
* Pirate Coast
* Strait of Hormuz
* Greater and Lesser Tunbs
* Al-Faw Peninsula
* Gulf of Oman
* Gulf of Aqaba
* Gulf of Aden
* Balochistan
* Arabian Peninsula
* Najd
* Al-Yamama
* Hejaz
* Tihamah
* Eastern Arabia
* South Arabia
* Hadhramaut
* Arabian Peninsula coastal fog desert
* Al-Sharat
* Tigris–Euphrates
* Mesopotamia
* Upper Mesopotamia
* Lower Mesopotamia
* Sawad
* Nineveh Plains
* Akkad (region)
* Babylonia
* Suhum
* Eastern Mediterranean
* Mashriq
* Eber-Nari
* Kurdistan
* Levant (Syria region)
* Palestine region
* Transjordan
* Jordan Rift Valley
* Philistia
* Golan Heights
* Hula Valley
* Galilee
* Canaan
* Gilead
* Syrian Desert
* Judea
* Samaria
* Arabah
* Aram
* Aram-Naharaim
* Negev
* Phoenicia
* Retjenu
* Anti-Lebanon Mountains
* Bekaa valley
* Levantine Sea
* Sinai Peninsula
* Arabian Desert
* Fertile Crescent
* Azerbaijan
* Hauran
* Iranian Plateau
* Dasht-e Kavir
* Armenian Highlands
* Caucasus
* Caucasus Mountains
* Greater Caucasus
* Lesser Caucasus
* North Caucasus
* South Caucasus
* Shirvan
* Kur-Araz Lowland
* Lankaran Lowland
* Alborz
* Absheron Peninsula
* Kartli
* Anatolia
* Taurus Mountains
* Aeolis
* Paphlagonia
* Phasiane
* Isauria
* Ionia
* Bithynia
* Cilicia
* Cappadocia
* Caria
* Corduene
* Chaldia
* Doris
* Lycaonia
* Lycia
* Lydia
* Galatia
* Pisidia
* Pontus
* Mysia
* Arzawa
* Speri
* Sophene
* Biga Peninsula
* Troad
* Tuwana
* Alpide belt

* v
* t
* e

Regions of Europe

North|

* Arctic
* Arctic Circle
* Nordic
* Northwestern
* Scandinavia
* Scandinavian Peninsula
* Fennoscandia
* Baltoscandia
* Jutland
* Gotland
* Sápmi
* Ingria
* West Nordic
* Baltic
* Baltic Sea
* Gulf of Bothnia
* Gulf of Finland
* Iceland
* Faroe Islands
* British Isles
* English Channel
* Channel Islands
* Livonia
* Curonian Spit
* Nemunas Delta
* Cap of the North

East|

* Danubian countries
* Prussia
* Galicia
* Volhynia
* Wallachia
* Transylvania
* Moldavia
* Bukovina
* Bessarabia
* Livonia
* Ruthenia
* Carpathian Ruthenia
* Donbas
* Sloboda Ukraine
* Sambia Peninsula
* Amber Coast
* Curonian Spit
* Izyum Trail
* Lithuania Minor
* Nemunas Delta
* Baltic
* Baltic Sea
* Vyborg Bay
* Karelia
* East Karelia
* Karelian Isthmus
* Lokhaniemi
* Southeastern
* Balkans
* Crimea
* North Caucasus
* Greater Caucasus
* Kabardia
* European Russia
* Arctic
* Arctic Circle
* Taman Peninsula
* Southern Russia
* Kola Peninsula
* East European Plain
* Ryn Desert
* Cap of the North

Central|

* North European Plain
* Baltic
* Baltic Sea
* Alpine states
* Alpide belt
* Rhineland
* Eastphalia
* Westphalia
* Prussia
* Lusatia
* Bohemia
* Moravia
* Silesia
* Czech Silesia
* Pomerania
* Pomerelia
* Kashubia
* Bukovina
* Istria
* Transdanubia
* Polesia
* Germania
* Germania Slavica

West|

* Benelux
* Low Countries
* Northwest
* British Isles
* English Channel
* Channel Islands
* Cotentin Peninsula
* Doggerland
* Upper Rhine Plain
* Upper Rhine
* Gaul
* Gascony
* Normandy
* Brittany
* Septimania
* Batavia
* Gulf of Lion
* Iberia
* Al-Andalus
* Baetic System
* Meseta Central
* Pyrenees
* Alpide belt

South|

* Italy
* Po Valley (Padania)
* Italian Peninsula
* Tuscan Archipelago
* Insular Italy
* Aegadian Islands
* Occitania
* Iberia
* Al-Andalus
* Baetic System
* Meseta Central
* Gibraltar Arc
* Southeastern
* Epirus
* Rumelia
* Balkans
* Aegean Sea
* Aegean Islands
* Attica
* Boeotia
* Opuntian Locris
* Phocis
* Megaris
* Peloponnese
* Chalkidiki
* Aetolia
* Gulf of Chania
* Istria
* Mediterranean
* Alpide belt

* Germanic
* Romance
* Celtic
* Slavic countries
* European Plain
* Eurasian Steppe
* Pontic–Caspian steppe
* Wild Fields
* Pannonian Basin
* Great Hungarian Plain
* Little Hungarian Plain
* Eastern Slovak Lowland

* v
* t
* e

Regions of North America

Upper Northern
(i.e. Canada and Alaska (US))|

| Eastern|

* Atlantic Canada
* The Maritimes
* Central Canada
* Great Lakes

|

Northern (Canada and Alaska)|

* North American Arctic
* Arctic Circle
* Canadian Arctic Archipelago
* Alaska
* Aleutian Arc
* Aleutian Islands
* Aleutian Range
* Alaska Peninsula
* Bering Strait
* Gulf of Alaska
* Greenland

Western|

* Pacific Northwest
* Cascadia
* Prairie Pothole Region

* Acadia
* Acadian Peninsula
* Avalon Peninsula
* Bay de Verde Peninsula
* Banks Peninsula (Nunavut)
* Brodeur Peninsula
* Bruce Peninsula
* Canadian Prairies
* Canadian Shield
* Cook Peninsula
* Cypress Hills
* English Canada
* French Canada
* Gaspé Peninsula
* Georgian Bay
* Gulf Islands
* Gulf of Boothia
* Hudson Bay
* Interior Alaska–Yukon lowland taiga
* James Bay
* Kodiak Island
* Labrador Peninsula
* Melville Peninsula
* Newfoundland Island
* Palliser's Triangle
* Peace River Country
* Quebec City–Windsor Corridor
* Strait of Georgia
* The Maritimes
* Vancouver Island

Lower Northern
(i.e. United States)|

| Central|

* Midwest
* Upper Midwest
* Old Southwest
* Tallgrass prairie

|

Eastern|

* Appalachia
* East Coast
* Northeast
* Atlantic Northeast
* Mid-Atlantic
* New England
* Southeast
* Thirteen Colonies

Northern|

* East North Central states
* Great Lakes

Southern|

* Deep South
* Old South
* South Central
* Gulf Coast
* Upland South

Southwestern|

* Four Corners
* Great Basin
* Llano Estacado
* West Texas
* Santa Fe de Nuevo México
* Southern Rocky Mountains

Western|

* Basin and Range Province
* Northwest
* Cascadia
* Inland Northwest
* Pacific Northwest
* West Coast

* Pacific Coast Ranges
* Oregon Trail
* Mormon corridor
* Calumet Region
* Llano Estacado
* Third Coast
* Backcountry
* Trans-Mississippi
* Great North Woods
* Great Plains
* Interior Plains
* Great Basin
* Great Basin Desert
* Acadia
* Ozarks
* Ark-La-Tex
* Waxhaws
* Siouxland
* Twin Tiers
* Driftless Area
* Palouse
* Piedmont
* Atlantic coastal plain
* Outer Lands
* Black Dirt Region
* Blackstone Valley
* Piney Woods
* Rocky Mountains
* Mountain states
* Intermountain West
* Mojave Desert
* The Dakotas
* Carolinas
* Shawnee Hills
* San Fernando Valley
* Tornado Alley
* North Coast
* Lost Coast
* Emerald Triangle
* San Francisco Bay Area
* San Francisco Bay
* North Bay
* East Bay
* Silicon Valley
* Interior Alaska–Yukon lowland taiga
* Gulf of Mexico
* Lower Colorado River Valley
* Sacramento–San Joaquin River Delta
* Yukon–Kuskokwim Delta
* Colville Delta
* Arkansas Delta
* Mobile–Tensaw River Delta
* Mississippi Delta
* Mississippi River Delta
* Columbia River Estuary
* High Desert
* Monterey Peninsula
* Upper Peninsula of Michigan
* Lower Peninsula of Michigan
* Virginia Peninsula
* Keweenaw Peninsula
* Middle Peninsula
* Delmarva Peninsula
* Alaska Peninsula
* Kenai Peninsula
* Niagara Peninsula
* "Belt" regions
* Bible Belt
* Corn Belt
* Cotton Belt
* Rice Belt
* Rust Belt
* Sun Belt
* Snow Belt

Mexico|

| Central|

* Bajío
* Huasteca
* Islas Marías
* La Mixteca
* Mezquital Valley
* Revillagigedo Islands
* Sierra Gorda
* Tierra Caliente
* Trans-Mexican Volcanic Belt
* Trans-Mexican Volcanic Belt pine–oak forests
* Valley of Mexico

|

Northern|

* Baja California peninsula
* Basin and Range Province
* Comarca Lagunera
* Gulf of California
* Colorado River Delta
* Isla Llave
* Lerdo Landing
* Pimería Alta
* Salton Trough
* Sierra de San Francisco

Southern|

* Chiapas Highlands
* Isthmus of Tehuantepec
* Ku-Maloob-Zaap
* Petén Basin
* Puuc
* Sierra Madre de Chiapas
* Sierra Madre de Oaxaca
* Sierra Madre del Sur
* Soconusco
* Triangle of the Sun
* Yucatán Peninsula

* Gulf of Mexico
* Sierra Madre Occidental
* Sierra Madre Oriental

Central|

* Darién Gap
* Isthmus of Panama
* Lake Nicaragua
* Panama Canal
* Western Caribbean zone

West Indies|

* Caribbean
* Antilles
* Greater Antilles
* Hispaniola
* Lesser Antilles
* Leeward Islands
* Saint Martin Island
* Virgin Islands
* Southern Caribbean
* Leeward Antilles
* ABC islands
* Windward Islands
* Bajo Nuevo Bank
* San Andrés and Providencia
* Serranilla Bank
* Lucayan Archipelago

* American Cordillera
* Anglo
* Aridoamerica
* Latin America
* French
* Hispanic
* Latin America and the Caribbean
* Mesoamerica
* Middle America
* Oasisamerica
* Ring of Fire

* v
* t
* e

Regions of Oceania

* Australia-New Guinea
* Near Oceania
* Pacific Islands
* Pacific Plate
* Remote Oceania
* Zealandia

Australasia|

| Australia|

| Australian Capital Territory|

* Canberra

|

Jervis Bay Territory|

* Jervis Bay Village
* Wreck Bay Village

New South Wales|

* Central Coast
* Central Tablelands
* Central West
* Far West
* Greater Blue Mountains Area
* Hunter
* Illawarra
* Mid North Coast
* Monaro
* New England
* North West Slopes
* Northern Rivers
* Northern Tablelands
* Orana
* Riverina
* South Coast
* South West Slopes
* Southern Highlands
* Southern Tablelands

Northern Territory|

* Arnhem Land
* Barkly Tableland
* Central Australia
* Darwin
* Katherine
* Top End

Queensland|

* Central West
* Central
* Darling Downs
* Far North
* Gulf Country
* North
* South East
* South West
* Wide Bay–Burnett

South Australia|

* Adelaide Hills
* Barossa Light and Lower North
* Eastern Adelaide
* Eyre Western
* Far North
* Fleurieu and Kangaroo Island
* Limestone Coast
* Murray and Mallee
* Northern Adelaide
* Southern Adelaide
* Western Adelaide
* Yorke and Mid North

Tasmania|

* Central Highlands
* East Coast
* Midlands
* North East
* North West
* Northern
* South West
* Southern
* West Coast

Victoria|

* Barwon South West
* Gippsland
* Grampians
* Greater Melbourne
* Hume
* Loddon Mallee

Western Australia|

* Gascoyne
* Goldfields–Esperance
* Great Southern
* Greater Perth
* Perth Metropolitan Area
* Kimberley
* Mid West
* Peel
* Pilbara
* South West
* Wheatbelt

Australian External Territories|

* Ashmore and Cartier Islands
* Coral Sea Islands
* Norfolk Island

| Australian Indian Ocean Territories|

* Christmas Island
* Cocos (Keeling) Islands

|

New Zealand|

| North Island|

* Northland
* Auckland
* Waikato
* Bay of Plenty
* Gisborne
* Hawke's Bay
* Taranaki
* Manawatū-Whanganui
* Wellington

|

South Island|

* Tasman
* Nelson
* Marlborough
* West Coast
* Canterbury
* Otago
* Southland
* Stewart Island

NZ Outlying Islands|

* Chatham Islands
* Kermadec Islands
* Solander Islands
* Three Kings Islands

| NZ Subantarctic Islands|

* Antipodes Islands
* Auckland Islands
* Bounty Islands
* Campbell Islands
* Snares Islands

|

Melanesia|

| Island Melanesia|

* Fiji
* New Caledonia

| East Melanesian Islands|

* Bismarck Archipelago
* Gazelle Peninsula
* Santa Cruz Islands
* Vanuatu

| Solomon Islands Archipelago|

* Bougainville
* Bonis Peninsula
* Solomon Islands

|

New Guinea|

* Aru Islands

| Papua New Guinea|

* Highlands Region
* Momase Region
* Huon Gulf
* Huon Peninsula
* Southern Region

|

Western New Guinea|

* Papua
* West Papua
* Bird's Head Peninsula

Micronesia|

* Caroline Islands
* Federated States of Micronesia
* Palau
* Kiribati
* Banaba
* Gilbert Islands
* Mariana Islands
* Guam
* Northern Mariana Islands
* Marshall Islands
* Nauru
* Wake Island

Polynesia|

| Polynesian Triangle|

* Easter Island
* Salas and Gómez Island
* Cook Islands
* French Polynesia
* Austral Islands
* Gambier Islands
* Mangareva Islands
* Marquesas Islands
* Society Islands
* Tuamotu Islands
* Johnston Atoll
* Line Islands
* Jarvis Island
* Kingman Reef
* Kiritimati
* Palmyra Atoll
* Tabuaeran
* Teraina
* Niue
* Pitcairn Islands
* Pitcairn Island
* Henderson Island
* Ducie Island
* Oeno Island
* Samoan Islands
* American Samoa
* Independent State of Samoa
* Southeastern Hawaiian Islands
* Tokelau Islands
* Atafu
* Fakaofo
* Nukunonu
* Swains Island
* Tonga
* Tuvalu
* Wallis and Futuna
* Hoorn Islands
* Wallis Islands

| Phoenix Islands|

* Canton Island
* Howland and Baker Islands
* Baker Island
* Howland Island

|

Polynesian Outliers|

* Clipperton Island
* Desventuradas Islands
* Galápagos Islands
* Juan Fernández Islands
* Northwestern Hawaiian Islands
* Midway Atoll

* Asia-Pacific
* Indo-Australian Plate
* Indo-Pacific
* Islands Region
* Papuan Peninsula
* Ring of Fire

* v
* t
* e

Regions of South America

East|

* Amazon basin
* Atlantic Forest
* Caatinga
* Cerrado

North|

* Caribbean South America
* West Indies
* Llanos
* The Guianas
* Amazon basin
* Amazon rainforest
* Gulf of Paria
* Paria Peninsula
* Paraguaná Peninsula
* Orinoco Delta

South|

* Tierra del Fuego
* Patagonia
* Pampas
* Pantanal
* Gran Chaco
* Chiquitano dry forests
* Valdes Peninsula
* Triple Frontier
* Río de la Plata
* Río de la Plata Basin

West|

* Andes
* Tropical Andes
* Wet Andes
* Dry Andes
* Pariacaca mountain range
* Altiplano
* Atacama Desert

* Middle
* Latin
* Hispanic
* Bolivarian
* American Cordillera
* Ring of Fire
* LAC

* v
* t
* e

Earth's polar regions

Antarctic|

* Antarctic Peninsula
* East Antarctica
* West Antarctica
* Eklund Islands
* Ecozone
* Extreme points
* Islands

Arctic|

* Arctic Alaska
* British Arctic Territories
* Canadian Arctic Archipelago
* Finnmark
* Greenland
* Northern Canada
* Northwest Territories
* Nunavik
* Nunavut
* Russian Arctic
* Sakha
* Sápmi
* Yukon
* North American Arctic

* v
* t
* e

Earth's oceans and seas

Arctic Ocean|

* Amundsen Gulf
* Barents Sea
* Beaufort Sea
* Chukchi Sea
* East Siberian Sea
* Greenland Sea
* Gulf of Boothia
* Kara Sea
* Laptev Sea
* Lincoln Sea
* Prince Gustaf Adolf Sea
* Pechora Sea
* Queen Victoria Sea
* Wandel Sea
* White Sea

Atlantic Ocean|

* Adriatic Sea
* Aegean Sea
* Alboran Sea
* Archipelago Sea
* Argentine Sea
* Baffin Bay
* Balearic Sea
* Baltic Sea
* Bay of Biscay
* Bay of Bothnia
* Bay of Campeche
* Bay of Fundy
* Black Sea
* Bothnian Sea
* Caribbean Sea
* Celtic Sea
* English Channel
* Foxe Basin
* Greenland Sea
* Gulf of Bothnia
* Gulf of Finland
* Gulf of Lion
* Gulf of Guinea
* Gulf of Maine
* Gulf of Mexico
* Gulf of Saint Lawrence
* Gulf of Sidra
* Gulf of Venezuela
* Hudson Bay
* Ionian Sea
* Irish Sea
* Irminger Sea
* James Bay
* Labrador Sea
* Levantine Sea
* Libyan Sea
* Ligurian Sea
* Marmara Sea
* Mediterranean Sea
* Myrtoan Sea
* North Sea
* Norwegian Sea
* Sargasso Sea
* Sea of Åland
* Sea of Azov
* Sea of Crete
* Sea of the Hebrides
* Thracian Sea
* Tyrrhenian Sea
* Wadden Sea

Indian Ocean|

* Andaman Sea
* Arabian Sea
* Bay of Bengal
* Flores Sea
* Great Australian Bight
* Gulf of Aden
* Gulf of Aqaba
* Gulf of Khambhat
* Gulf of Kutch
* Gulf of Oman
* Gulf of Suez
* Laccadive Sea
* Mozambique Channel
* Persian Gulf
* Red Sea
* Timor Sea

Pacific Ocean|

* Arafura Sea
* Bali Sea
* Banda Sea
* Bering Sea
* Bismarck Sea
* Bohai Sea
* Bohol Sea
* Camotes Sea
* Celebes Sea
* Chilean Sea
* Coral Sea
* East China Sea
* Gulf of Alaska
* Gulf of Anadyr
* Gulf of California
* Gulf of Carpentaria
* Gulf of Fonseca
* Gulf of Panama
* Gulf of Thailand
* Gulf of Tonkin
* Halmahera Sea
* Java Sea
* Koro Sea
* Mar de Grau
* Molucca Sea
* Moro Gulf
* Philippine Sea
* Salish Sea
* Savu Sea
* Sea of Japan
* Sea of Okhotsk
* Seram Sea
* Seto Inland Sea
* Shantar Sea
* Sibuyan Sea
* Solomon Sea
* South China Sea
* Sulu Sea
* Tasman Sea
* Visayan Sea
* Yellow Sea

Southern Ocean|

* Amundsen Sea
* Bellingshausen Sea
* Cooperation Sea
* Cosmonauts Sea
* Davis Sea
* D'Urville Sea
* King Haakon VII Sea
* Lazarev Sea
* Mawson Sea
* Riiser-Larsen Sea
* Ross Sea
* Scotia Sea
* Somov Sea
* Weddell Sea

Endorheic basins|

* Aral Sea
* Caspian Sea
* Dead Sea
* Salton Sea

Others|

* Ocean
* Sea
* Superocean

* '
* Category

* v
* t
* e

Hemispheres of Earth

* Northern
* Southern
* Eastern
* Western
* Land
* Water

* Portal:Geography
* Commons page Commons:Maps of Earth's hemispheres

* v
* t
* e

State of Uttarakhand

State Capitals: (Legislative: Dehradun (Winter); Bhararisain (Summer); Judicial: Nainital)

Government|

| Executive|

* Governor
* Chief Minister
* Council of Ministers

|

Legislature|

* Legislative Assembly
* Speaker
* Leader of the Opposition

Judiciary|

* High Court
* Chief Justice
* Judges
* Lok Adalat
* Lokayukta

Departments
and
agencies|

* Symbols
* Emblem
* Song
* Motto
* Foundation day
* Departments
* Environment and Forests
* Police
* Agencies
* Bar Council
* Consumer Disputes Redressal Commission
* Election Commission
* Human Rights Commission
* Information Commission
* Public Service Commission
* Women's Commission
* Industrial Development Corporation
* Urban Development Directorate
* Waqf Board

History|

| Ancient
Kingdoms|

* Uttarakuru Kingdom
* Paurava Kingdom
* Khasa Janapada Kingdom
* Himalaya Kingdom
* Parvata Kingdom
* Kirata Kingdom
* Nanda Empire
* Maurya Empire
* Kushan Empire
* Kuninda Kingdom
* Gupta Empire

|

Medieval
Kingdoms|

* Garhwal Kingdom
* Panwar dynasty
* Kumaon Kingdom
* Katyuri dynasty
* Chand dynasty
* Khasa Kingdom
* Raika Kingdom
* Gorkha Kingdom
* Shah dynasty
* Anglo-Nepalese War
* Treaty of Sugauli

Colonial
Uttarakhand|

| Company
rule|

* Ceded and Conquered Provinces
* North-Western Provinces
* Agra Presidency

|

Crown
rule|

* United Provinces of Agra and Oudh
* United Provinces of British India
* United Provinces

Contemporary
Uttarakhand|

* Rampur Tiraha firing
* Bifurcation of Uttar Pradesh

Geography
and
Ecology|

| Geological
features|

| Mountains|

* Great Himalayas
* Garhwal Himalayas
* Sivalik Hills
* Mountain peaks
* Bugyals
* Lakes

|

Plains|

* Bhabar
* Terai
* Doab
* Ganges Basin

Ecoregions|

| Highlands|

* Western Himalayan alpine shrub and meadows
* Western Himalayan subalpine conifer forests
* Himalayan subtropical pine forests

|

Lowlands|

* Western Himalayan broadleaf forests
* Himalayan subtropical broadleaf forests
* Terai–Duar savanna and grasslands
* Upper Gangetic Plains moist deciduous forests

Demographics|

| Ethnic
groups|

| Indo-Aryans|

* Garhwalis
* Kumaonis
* Jaunsaris
* Buksas
* Tharus

|

Tibeto-Burmans|

* Bhotiyas
* Rajis
* Jads
* Banrawats

Languages|

| Official|

* Hindi
* Sanskrit

|

Spoken|

| Indo-Aryan|

* Garhwali
* Kumaoni
* Jaunsari
* Tharu

|

Tibeto-Burman|

* Rongpo
* Byangsi
* Chaudangsi
* Darmiya
* Raji
* Rawat
* Jad

Administrative
divisions|

| Urban|

* Districts
* Tehsils
* Urban Local Bodies
* Municipal Corporations

|

Rural|

* Parganas
* Community Development Blocks

Politics|

* Coolie-Begar movement
* Statehood movement
* Chipko movement
* Elections
* Local elections
* Assembly constituencies
* Former constituencies
* Parliamentary constituencies

Tourism|

| Monuments|

* World Heritage Site
* Nanda Devi and Valley of Flowers National Parks
* Ramsar Wetland
* Asan Barrage
* Monuments of National Importance
* State Protected Monuments

|

Chardham
Circuit|

* Gangotri
* Yamunotri
* Yamunotri Temple
* Badrinath
* Badrinath Temple
* Kedarnath
* Kedarnath Temple
* Sapta Badri
* Panch Kedar
* Panch Prayag
* Gomukh

National
Parks|

* Gangotri
* Govind Pashu Vihar
* Jim Corbett
* Nanda Devi
* Rajaji
* Valley of Flowers

Sports|

* Cricket
* Men's cricket team
* Women's cricket team
* Association football
* Men's football team
* Cricket Stadium
* Olympic Stadium
* Sports College

Other
topics|

* Transport
* Char Dham Highway
* Char Dham Railway
* Dehradun–Haridwar–Rishikesh Metro
* Music
* Cuisine
* Kumaoni cuisine
* Economy
* Education
* School education
* Higher education
* Awards and decorations
* Uttarakhand Ratna
* Uttarakhand Gaurav Samman

Districts|

| Kumaon|

* Almora
* Bageshwar
* Champawat
* Nainital
* Pithoragarh
* Udham Singh Nagar

|

Garhwal|

* Chamoli
* Dehradun
* Haridwar
* Pauri Garhwal
* Rudraprayag
* Tehri Garhwal
* Uttarkashi

Proposed
districts|

* Didihat
* Kotdwar
* Ranikhet
* Yamunotri
* Thalisain

Major
cities|

* Dehradun
* Haridwar
* Haldwani
* Roorkee
* Kashipur
* Rudrapur
* Kotdwar
* Rishikesh
* Ramnagar
* Pithoragarh
* Srinagar
* New Tehri
* Nainital
* Mussoorie
* Almora
* Pauri

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