Indus River

"Indus Valley" redirects here. For the Bronze Age civilisation, see Indus Valley Civilisation.

"Indus" and "Darya-e-Sindh" redirect here. For دریا سندھ, see Sindhu.

Indus Darya-e-Sindh
Satellite image of the Indus River basin in Pakistan and Kashmir (International boundaries are superimposed)
Map of the Indus River basin excluding the tributaries draining in to Rann of Kutch
Location
Country	China, India, Pakistan
State	Jammu and Kashmir, Punjab, Khyber Pakhtunkhwa, Sindh, Gilgit-Baltistan, Tibet
Cities	Leh, Skardu, Dasu, Besham, Thakot, Swabi, Dera Ismail Khan, Sukkur, Hyderabad
Physical characteristics
Source	Sênggê Zangbo
- location	Tibetan Plateau
2nd source	Gar Tsangpo
Source confluence
- location	Shiquanhe, Ngari Prefecture, Tibet and India
- coordinates	32°29′54″N 79°41′28″E / 32.49833°N 79.69111°E / 32.49833; 79.69111
- elevation	4,255 m (13,960 ft)
Mouth	Arabian Sea (primary), Rann of Kutch (secondary)
- location	Indus River Delta (primary), Kori Creek (secondary), Pakistan, India
- coordinates	23°59′40″N 67°25′51″E / 23.99444°N 67.43083°E / 23.99444; 67.43083Coordinates: 23°59′40″N 67°25′51″E / 23.99444°N 67.43083°E / 23.99444; 67.43083
- elevation	0 m (0 ft)
Length	3,610 km (2,240 mi)
Basin size	1,165,000 km2 (450,000 sq mi)
Discharge
- location	Arabian Sea
- average	6,600 m3/s (230,000 cu ft/s)
- minimum	1,200 m3/s (42,000 cu ft/s)
- maximum	58,000 m3/s (2,000,000 cu ft/s)
Basin features
Tributaries
- left	Zanskar River, Suru River, Soan River, Jhelum River, Chenab River, Ravi River, Beas River, Sutlej River, Panjnad River, Ghaggar-Hakra River, Luni River
- right	Shyok River, Hunza River, Gilgit River, Swat River, Kunar River, Kabul River, Kurram River, Gomal River, Zhob River

Indus River in Kharmang District, Pakistan.

The Indus River (locally called Darya-e-Sindh) is one of the longest rivers in Asia. Originating in the Tibetan Plateau in the vicinity of Lake Manasarovar, the river runs a course through the Ladakh region of Kashmir, towards Gilgit-Baltistan and the Hindukush ranges, and then flows in a southerly direction along the entire length of Pakistan to merge into the Arabian Sea near the port city of Karachi in Sindh.^[1][2] It is the longest river and national river of Pakistan.^[3]

The river has a total drainage area exceeding 1,165,000 km² (450,000 sq mi). Its estimated annual flow stands at around 243 km³ (58 cu mi), twice that of the Nile River and three times that of the Tigris and Euphrates rivers combined, making it the twenty-first largest river in the world in terms of annual flow.^[4] The Zanskar is its left bank tributary in Ladakh. In the plains, its left bank tributary is the Panjnad which itself has five major tributaries, namely, the Chenab, Jhelum, the Ravi, the Beas, and the Sutlej. Its principal right bank tributaries are the Shyok, the Gilgit, the Kabul, the Gomal, and the Kurram. Beginning in a mountain spring and fed with glaciers and rivers in the Himalayas, the river supports ecosystems of temperate forests, plains and arid countryside.

The northern part of the Indus Valley, with its tributaries, forms the Punjab region, while the lower course of the Indus is known as Sindh and ends in a large delta. The river has historically been important to many cultures of the region. The 3rd millennium BC saw the rise of a major urban civilization of the Bronze Age. During the 2nd millennium BC, the Punjab region was mentioned in the hymns of the Hindu Rigveda as Sapta Sindhu and the Zoroastrian Avesta as Hapta Hindu (both terms meaning "seven rivers"). Early historical kingdoms that arose in the Indus Valley include Gandhāra, and the Ror dynasty of Sauvīra. The Indus River came into the knowledge of the West early in the Classical Period, when King Darius of Persia sent his Greek subject Scylax of Caryanda to explore the river, ca. 515 BC.

Contents

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  1 Etymology and names
  
  
  
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    1.1 Indus and the name of India
    
  
  
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    1.2 Rigveda and the Indus
    
  
  
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    1.3 Other names
    
  
  
  
  


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  2 Description
  


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  3 History
  


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  4 Geography
  
  
  
  • 
    4.1 Tributaries
    
  
  
  
  


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  5 Geology
  


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  6 Wildlife
  


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  7 Mammals
  
  
  
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    7.1 Fish
    
  
  
  
  


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  8 Economy
  


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  9 People
  


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  10 Modern issues
  
  
  
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    10.1 Indus delta
    
  
  
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    10.2 Effects of climate change on the river
    
  
  
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    10.3 Pollution
    
  
  
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    10.4 2010 floods
    
  
  
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    10.5 2011 floods
    
  
  
  
  


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  11 Barrages, bridges and dams
  
  
  
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    11.1 Gallery
    
  
  
  
  


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  12 See also
  


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  13 References
  
  
  
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    13.1 Citations
    
  
  
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    13.2 Sources
    
  
  
  
  


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  14 External links
  

Etymology and names

This river was known to the ancient Indians in Sanskrit as Sindhu and the Achaemenids as Hiduš (𐏃𐎡𐎯𐎢𐏁, H-i-du-u-š), which was regarded by both of them as "the border river".^{[5][6][7][8][9]} The variation between the two names is explained by the Old Iranian sound change *s > h, which occurred between 850–600 BCE according to Asko Parpola.^[10][11] From the Achaemenid Empire, the name passed to the Greeks as Indós (Ἰνδός).^[12] It was adopted by the Romans as Indus.

The meaning of Sindhu as a "large body of water, sea, or ocean" is a later meaning in Classical Sanskrit.^[13] A later Persian name for the river was Darya,^[14] which similarly has the connotations of large body of water and sea.^{[citation needed]}

Other variants of the name Sindhu include Assyrian Sinda (as early as the 7th century BC), Persian Ab-e-sind, Pashto Abasind, Arab Al-Sind, Chinese Sintow, and Javanese Santri.^{[citation needed]}

Indus and the name of India

India is a Greek and Latin term for "the country of the River Indus". The region through which the river drains into sea is called Sindh and owes its name to the river (Sanskrit: Sindhu).^[15]

Megasthenes' book Indica derives its name from the river's Greek name, "Indós" (Ἰνδός), and describes Nearchus's contemporaneous account of how Alexander the Great crossed the river. The ancient Greeks referred to the Indians (people of present-day northwest India and Pakistan) as "Indói" (Ἰνδοί), literally meaning "the people of the Indus".^[16]

Rigveda and the Indus

Rigveda also describes several mythical rivers, including one named "Sindhu". The Rigvedic "Sindhu" is thought to be the present-day Indus river and is attested 176 times in its text – 95 times in the plural, more often used in the generic meaning. In the Rigveda, notably in the later hymns, the meaning of the word is narrowed to refer to the Indus river in particular, as in the list of rivers mentioned in the hymn of Nadistuti sukta. The Rigvedic hymns apply a feminine gender to all the rivers mentioned therein but "Sindhu" is the only river attributed the masculine gender which means Sindhu is the warrior and greatest among all other rivers in whole world.^{[citation needed]}

Other names

In other languages of the region, the river is known as सिन्धु (Sindhu) in Hindi and Nepali, سنڌو (Sindhu) in Sindhi, سندھ‬ (Sindh) in Shahmukhi Punjabi, ਸਿੰਧ ਨਦੀ (Sindh Nadī) in Gurmukhī Punjabi, اباسين (Abāsin lit. "Father of Rivers") in Pashto, نهر السند (Nahar al-Sind) in Arabic, སེང་གེ་གཙང་པོ། (singi khamban lit. "Lion River" or Lion Spring) in Tibetan, 印度 (Yìndù) in Chinese, and Nilab in Turki.^{[citation needed]}

Description

Babur crossing the Indus River.

The Indus River provides key water resources for Pakistan's economy – especially the breadbasket of Punjab province, which accounts for most of the nation's agricultural production, and Sindh. The word Punjab means "land of five rivers" and the five rivers are Jhelum, Chenab, Ravi, Beas and Sutlej, all of which finally flow into the Indus. The Indus also supports many heavy industries and provides the main supply of potable water in Pakistan.

The ultimate source of the Indus is in Tibet; the river begins at the confluence of the Sengge Zangbo and Gar Tsangpo rivers that drain the Nganglong Kangri and Gangdise Shan (Gang Rinpoche, Mt. Kailas) mountain ranges. The Indus then flows northwest through Ladakh and Baltistan into Gilgit, just south of the Karakoram range. The Shyok, Shigar and Gilgit rivers carry glacial waters into the main river. It gradually bends to the south, coming out of the hills between Peshawar and Rawalpindi. The Indus passes gigantic gorges 4,500–5,200 metres (15,000–17,000 feet) deep near the Nanga Parbat massif. It flows swiftly across Hazara and is dammed at the Tarbela Reservoir. The Kabul River joins it near Attock. The remainder of its route to the sea is in the plains of the Punjab^[17] and Sindh, where the flow of the river becomes slow and highly braided. It is joined by the Panjnad at Mithankot. Beyond this confluence, the river, at one time, was named the Satnad River (sat = "seven", nadī = "river"), as the river now carried the waters of the Kabul River, the Indus River and the five Punjab rivers. Passing by Jamshoro, it ends in a large delta to the east of Thatta.

The Indus is one of the few rivers in the world to exhibit a tidal bore. The Indus system is largely fed by the snows and glaciers of the Himalayas, Karakoram and the Hindu Kush ranges of Tibet, the Indian states of Jammu and Kashmir and Himachal Pradesh and Gilgit-Baltistan region of Pakistan. The flow of the river is also determined by the seasons – it diminishes greatly in the winter, while flooding its banks in the monsoon months from July to September. There is also evidence of a steady shift in the course of the river since prehistoric times – it deviated westwards from flowing into the Rann of Kutch and adjoining Banni grasslands after the 1816 earthquake.^[18][19] Presently, Indus water flows in to the Rann of Kutch during its floods breaching flood banks.^[20]

The traditional source of the river is the Senge Khabab or "Lion's Mouth", a perennial spring, not far from the sacred Mount Kailash marked by a long low line of Tibetan chortens. There are several other tributaries nearby, which may possibly form a longer stream than Senge Khabab, but unlike the Senge Khabab, are all dependent on snowmelt. The Zanskar River, which flows into the Indus in Ladakh, has a greater volume of water than the Indus itself before that point.^[21]

History

Extent and major sites of the Indus Valley Civilisation 3000 BC

Main articles: Indus Valley Civilization and History of Sindh

The major cities of the Indus Valley Civilisation, such as Harappa and Mohenjo-daro, date back to around 3300 BC, and represent some of the largest human habitations of the ancient world. The Indus Valley Civilisation extended from across northeast Afghanistan to Pakistan and northwest India,^[22] with an upward reach from east of Jhelum River to Ropar on the upper Sutlej. The coastal settlements extended from Sutkagan Dor at the Pakistan, Iran border to Kutch in modern Gujarat, India. There is an Indus site on the Amu Darya at Shortughai in northern Afghanistan, and the Indus site Alamgirpur at the Hindon River is located only 28 km (17 mi) from Delhi. To date, over 1,052 cities and settlements have been found, mainly in the general region of the Ghaggar-Hakra River and its tributaries. Among the settlements were the major urban centres of Harappa and Mohenjo-daro, as well as Lothal, Dholavira, Ganeriwala, and Rakhigarhi. Only 90–96 of more than 800 known Indus Valley sites have been discovered on the Indus and its tributaries.^{[citation needed]} The Sutlej, now a tributary of the Indus, in Harappan times flowed into the Ghaggar-Hakra River, in the watershed of which were more Harappan sites than along the Indus.

Most scholars believe that settlements of Gandhara grave culture of the early Indo-Aryans flourished in Gandhara from 1700 BC to 600 BC, when Mohenjo-daro and Harappa had already been abandoned.

The word "India" is derived from the Indus River. In ancient times, "India" initially referred to those regions immediately along the east bank of the Indus, but by 300 BC, Greek writers including Herodotus and Megasthenes were applying the term to the entire subcontinent that extends much farther eastward.^[23][24]

The lower basin of the Indus forms a natural boundary between the Iranian Plateau and the Indian subcontinent; this region embraces all or parts of the Pakistani provinces Balochistan, Khyber Pakhtunkhwa, Punjab and Sindh and the countries Afghanistan and India. It was crossed by the invading armies of Alexander, but after his Macedonians conquered the west bank—joining it to the Hellenic Empire, they elected to retreat along the southern course of the river, ending Alexander's Asian campaign. The Indus plains were later dominated by the Persian empire and then the Kushan empire. Over several centuries Muslim armies of Muhammad bin Qasim, Mahmud of Ghazni, Mohammed Ghori, Tamerlane and Babur crossed the river to invade the inner regions of the Punjab and points farther south and east

Geography

The Indus River near Leh, Ladakh

Tributaries

• Beas River


• Chenab River


• Gar River


• Gilgit River


• Gomal River


• Hunza River


• Jhelum River


• Kabul River


• Kunar River


• Kurram River


• Panjnad River


• Ravi River


• Shyok River


• Soan River


• Suru River


• Satluj River


• Swat River


• Zanskar River


• Zhob River

Geology

Indus River viewed from the Karakoram Highway.

Indus River near Leh, India, 2014

Confluence of Indus and Zanskar rivers. The Indus is at the bottom of the picture, flowing left-to-right; the Zanskar, carrying more water, comes in from the middle left of the picture.

The Indus river feeds the Indus submarine fan, which is the second largest sediment body on the Earth.^[25] It consists of around 5 million cubic kilometres of material eroded from the mountains. Studies of the sediment in the modern river indicate that the Karakoram Mountains in northern Pakistan and India are the single most important source of material, with the Himalayas providing the next largest contribution, mostly via the large rivers of the Punjab (Jhelum, Ravi, Chenab, Beas and Sutlej). Analysis of sediments from the Arabian Sea has demonstrated that prior to five million years ago the Indus was not connected to these Punjab rivers which instead flowed east into the Ganga and were captured after that time.^[26] Earlier work showed that sand and silt from western Tibet was reaching the Arabian Sea by 45 million years ago, implying the existence of an ancient Indus River by that time.^[27] The delta of this proto-Indus river has subsequently been found in the Katawaz Basin, on the Afghan-Pakistan border.

In the Nanga Parbat region, the massive amounts of erosion due to the Indus river following the capture and rerouting through that area is thought to bring middle and lower crustal rocks to the surface.^[28]

In November 2011, satellite images showed that the Indus river had re-entered India, feeding Great Rann of Kutch, Little Rann of Kutch and a lake near Ahmedabad known as Nal Sarovar.^[20] Heavy rains had left the river basin along with the Lake Manchar, Lake Hemal and Kalri Lake (all in modern-day Pakistan) inundated. This happened two centuries after the Indus river shifted its course westwards following the 1819 Rann of Kutch earthquake.

The Induan Age at start of the Triassic Period of geological time is named for the Indus region.

Wildlife

Footbridge on the Indus River in Pakistan

Fishermen on the Indus River, c. 1905

Accounts of the Indus valley from the times of Alexander's campaign indicate a healthy forest cover in the region, which has now considerably receded. The Mughal Emperor Babur writes of encountering rhinoceroses along its bank in his memoirs (the Baburnama). Extensive deforestation and human interference in the ecology of the Shivalik Hills has led to a marked deterioration in vegetation and growing conditions. The Indus valley regions are arid with poor vegetation. Agriculture is sustained largely due to irrigation works.
The Indus river and its watershed has a rich biodiversity. It is home to around 25 amphibian species and 147 fish species, 22 of which are only found in the Indus.^[29]

Mammals

The Indus River Dolphin (Platanista indicus minor) is a sub-species of dolphin found only in the Indus River. It formerly also occurred in the tributaries of the Indus river. According to the World Wildlife Fund it is one of the most threatened cetaceans with only about 1,000 still existing.^[30]

Fish

Palla fish, Tenualosa ilisha, of the river is a delicacy for people living along the river. The population of fish in the river is moderately high, with Sukkur, Thatta, and Kotri being the major fishing centres – all in the lower Sindh course. As a result, damming and irrigation has made fish farming an important economic activity. Located southeast of Karachi, the large delta has been recognized by conservationists as one of the world's most important ecological regions. Here, the river turns into many marshes, streams and creeks and meets the sea at shallow levels. Here, marine fishes are found in abundance, including pomfret and prawns.

Economy

The Indus is the most important supplier of water resources to the Punjab and Sindh plains – it forms the backbone of agriculture and food production in Pakistan. The river is especially critical since rainfall is meagre in the lower Indus valley. Irrigation canals were first built by the people of the Indus Valley Civilisation, and later by the engineers of the Kushan Empire and the Mughal Empire. Modern irrigation was introduced by the British East India Company in 1850 – the construction of modern canals accompanied with the restoration of old canals. The British supervised the construction of one of the most complex irrigation networks in the world. The Guddu Barrage is 1,350 m (4,430 ft) long – irrigating Sukkur, Jacobabad, Larkana and Kalat. The Sukkur Barrage serves over 20,000 km² (7,700 sq mi).

After Pakistan came into existence, a water control treaty signed between India and Pakistan in 1960 guaranteed that Pakistan would receive water from the Indus River and its two tributaries the Jhelum River & the Chenab River independently of upstream control by India.^[31]

The Indus Basin Project consisted primarily of the construction of two main dams, the Mangla Dam built on the Jhelum River and the Tarbela Dam constructed on the Indus River, together with their subsidiary dams.^[32] The Pakistan Water and Power Development Authority undertook the construction of the Chashma-Jhelum link canal – linking the waters of the Indus and Jhelum rivers – extending water supplies to the regions of Bahawalpur and Multan. Pakistan constructed the Tarbela Dam near Rawalpindi – standing 2,743 metres (9,000 ft) long and 143 metres (470 ft) high, with an 80-kilometre (50 mi) long reservoir. It supports the Chashma Barrage near Dera Ismail Khan for irrigation use and flood control and the Taunsa Barrage near Dera Ghazi Khan which also produces 100,000 kilowatts of electricity. The Kotri Barrage near Hyderabad is 915 metres (3,000 ft) long and provides additional water supplies for Karachi. The extensive linking of tributaries with the Indus has helped spread water resources to the valley of Peshawar, in the Khyber Pakhtunkhwa. The extensive irrigation and dam projects provide the basis for Pakistan's large production of crops such as cotton, sugarcane and wheat. The dams also generate electricity for heavy industries and urban centers.

People

The Indus River near Skardu, in Gilgit–Baltistan.

The Dubair Khwarr, a tributary of the Indus, near Shaikhdara, in Khyber Pakhtunkhwa.

The inhabitants of the regions are mainly Muslim as Pakistan is an Islamic country through which the Indus river passes and forms a major natural feature and resource are diverse in ethnicity, religion, national and linguistic backgrounds. On the northern course of the river in the state of Jammu and Kashmir in India, live the Buddhist people of Ladakh, of Tibetan stock, and the Dards of Indo-Aryan or Dardic stock and practising Islam. Then it descends into Baltistan, northern Pakistan passing the main Balti city of Skardu. A river from Dubair Bala also drains into it at Dubair Bazar. People living in this area are mainly Kohistani and speak the Kohistani language. Major areas through which the Indus river passes in Kohistan are Dasu, Pattan and Dubair. As it continues through Pakistan, the Indus river forms a distinctive boundary of ethnicity and cultures – upon the western banks the population is largely Pashtun, Baloch, and of other Iranian stock. The eastern banks are largely populated by people of Indo-Aryan stock, such as the Punjabis and the Sindhis. In northern Punjab and the Khyber Pakhtunkhwa, ethnic Pashtun tribes live alongside Dardic people in the hills (Khowar, Kalash, Shina, etc.), Burushos (in Hunza), and Punjabi people.

The people living along the Indus river speak Punjabi and Sindhi on the eastern side (in Punjab and Sindh provinces respectively), Pushto plus Balochi as well as Barohi (in Khyber Pakhtoonkha and Baluchistan provinces). In the province of Sindh, the upper third of the river is inhabited by people speaking Saraiki; which is a somewhat transitional dialect of the Punjabi and Sindhi languages.

Modern issues

Satellite images of the upper Indus River valley, comparing water-levels on 1 August 2009 (top) and 31 July 2010 (bottom)

The Indus is a strategically vital resource for Pakistan's economy and society. After Pakistan and India declared Independence from the British Raj, the use of the waters of the Indus and its five eastern tributaries became a major dispute between India and Pakistan. The irrigation canals of the Sutlej valley and the Bari Doab were split – with the canals lying primarily in Pakistan and the headwork dams in India disrupting supply in some parts of Pakistan. The concern over India building large dams over various Punjab rivers that could undercut the supply flowing to Pakistan, as well as the possibility that India could divert rivers in the time of war, caused political consternation in Pakistan. Holding diplomatic talks brokered by the World Bank, India and Pakistan signed the Indus Waters Treaty in 1960. The treaty gave India control of the three easternmost rivers of the Punjab, the Sutlej, the Beas and the Ravi, while Pakistan gained control of the three western rivers, the Jhelum, the Chenab and the Indus. India retained the right to use of the western rivers for non-irrigation projects.^[33]

There are concerns that extensive deforestation, industrial pollution and global warming are affecting the vegetation and wildlife of the Indus delta, while affecting agricultural production as well. There are also concerns that the Indus River may be shifting its course westwards – although the progression spans centuries. On numerous occasions, sediment clogging owing to poor maintenance of canals has affected agricultural production and vegetation. In addition, extreme heat has caused water to evaporate, leaving salt deposits that render lands useless for cultivation.

Indus delta

Main article: Indus River Delta

Originally, the delta used to receive almost all of the water from the Indus river, which has an annual flow of approximately 180 billion cubic metres (240 billion cubic yards), and is accompanied by 400 million tonnes of silt. Since the 1940s, dams, barrages and irrigation works have been constructed on the river Indus.^[34] The Indus Basin Irrigation System is the "largest contiguous irrigation system developed over the past 140 years" anywhere in the world.^[35] This has reduced the flow of water and by 2018, the average annual flow of water below the Kotri barrage was 32×10^⁹ m³ (1.1×10^¹² cu ft), and annual amount of silt discharged was estimated to be 100 million tonnes (98 million long tons).^[36] Substantial annual chemical/dissolved load of 46 million tons in the river basin is unable to reach the sea as it is getting trapped in the irrigated areas by increasing the ground water salinity.^[37] Nearly 90% of the water from Indus River System has been harnessed already in Pakistan and India leaving rest of water to join the sea. Any further utilization of the river basin water is not economically feasible.^[38][39] The result has been catastrophic for both the environment and the local population. The reduction of freshwater due to the dams also increases salinity, making the surface and ground water available in the delta area unsuitable for the freshwater species and crops.^[40][41] As a result, the 2010 Pakistan floods were considered "good news" for the ecosystem and population of the river delta as they brought much needed fresh water.^[42][43] In case of the Indus dolphin, the damming of the river has isolated the delta dolphin population from those dolphins upstream.

Effects of climate change on the river

The Tibetan Plateau contains the world's third-largest store of ice. Qin Dahe, the former head of the China Meteorological Administration, said the recent fast pace of melting and warmer temperatures will be good for agriculture and tourism in the short term, but issued a strong warning:

"Temperatures are rising four times faster than elsewhere in China, and the Tibetan glaciers are retreating at a higher speed than in any other part of the world... In the short term, this will cause lakes to expand and bring floods and mudflows.. In the long run, the glaciers are vital lifelines of the Indus River. Once they vanish, water supplies in Pakistan will be in peril."^[44]

"There is insufficient data to say what will happen to the Indus," says David Grey, the World Bank's senior water advisor in South Asia. "But we all have very nasty fears that the flows of the Indus could be severely, severely affected by glacier melt as a consequence of climate change," and reduced by perhaps as much as 50 percent. "Now what does that mean to a population that lives in a desert [where], without the river, there would be no life? I don't know the answer to that question," he says. "But we need to be concerned about that. Deeply, deeply concerned."^[45]

U.S. diplomat Richard Holbrooke said, shortly before his death in 2010, that he believed that falling water levels in the Indus River "could very well precipitate World War III."^[46]

Pollution

Over the years factories on the banks of the Indus River have increased levels of water pollution in the river and the atmosphere around it. High levels of pollutants in the river have led to the deaths of endangered Indus River Dolphin. The Sindh Environmental Protection Agency has ordered polluting factories around the river to shut down under the Pakistan Environmental Protection Act, 1997.^[47] Death of the Indus River Dolphin has also been attributed to fishermen using poison to kill fish and scooping them up.^[48][49] As a result, the government banned fishing from Guddu Barrage to Sukkur.^[50]

Coming second after the Yangtze, and together with 9 other rivers, the Indus transports 90 % of all the plastic that reaches the oceans.^[51][52]

2010 floods

Affected areas as of 26 August 2010

Main article: 2010 Pakistan floods

Frequently, Indus river is prone to moderate to severe flooding.^[53] In July 2010, following abnormally heavy monsoon rains, the Indus River rose above its banks and started flooding. The rain continued for the next two months, devastating large areas of Pakistan. In Sindh, the Indus burst its banks near Sukkur on 8 August, submerging the village of Mor Khan Jatoi.^[54] In early August, the heaviest flooding moved southward along the Indus River from severely affected northern regions toward western Punjab, where at least 1,400,000 acres (570,000 ha) of cropland was destroyed, and the southern province of Sindh.^[55] As of September 2010^[update], over two thousand people had died and over a million homes had been destroyed since the flooding began.^[56][57]

2011 floods

Main article: 2011 Sindh floods

The 2011 Sindh floods began during the Pakistani monsoon season in mid-August 2011, resulting from heavy monsoon rains in Sindh, eastern Balochistan, and southern Punjab.^[58] The floods caused considerable damage; an estimated 434 civilians were killed, with 5.3 million people and 1,524,773 homes affected.^[59] Sindh is a fertile region and often called the "breadbasket" of the country; the damage and toll of the floods on the local agrarian economy was said to be extensive. At least 1.7 million acres (690,000 ha; 2,700 sq mi) of arable land were inundated. The flooding followed the previous year's floods, which devastated a large part of the country.^[59] Unprecedented torrential monsoon rains caused severe flooding in 16 districts of Sindh.^[60]

Barrages, bridges and dams

In Pakistan currently there are three barrages on the Indus: Guddu barrage, Sukkur Barrage, and Kotri barrage (also called Ghulam Muhammad barrage). There are some bridges on river Indus, such as, Dadu Moro Bridge, Larkana Khairpur Indus River Bridge, Thatta-Sujawal bridge, Jhirk-Mula Katiar bridge and recently planned Kandhkot-Ghotki bridge.^[61]

Kala Bagh Barrage, Chasma Barrage, and Taunsa Barrage are also built in Punjab on the Indus.

Tarbela Dam in Pakistan is constructed on the Indus River, while the controversial Kalabagh dam is also being constructed on Indus river.

Gallery

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  Video of River Indus at Kotri Barrage, Sindh, Pakistan.
  

  
  

  
  


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  Frozen Indus, Near Nyoma
  

  
  

  
  


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  Indus at Skardu
  

  
  

  
  

See also

• Chura Sharif


• Ghaggar-Hakra River


• HMS Indus


• Indus Valley Civilisation


• Rivers of Jammu and Kashmir


• Sarasvati River


• Sind Sagar Doab


• Sindhology


• Sindhu Darshan Festival


• Sindhu Pushkaram


• Rigvedic rivers

References

Citations

1. 
   ^ Swain, Ashok (2004). Managing Water Conflict: Asia, Africa and the Middle East. Routledge. p. 46. ISBN 1135768838. 1,800 miles long river after flowing out of Tibet through the Himalayas enters Kashmir and then moves into Pakistan.mw-parser-output cite.citation{font-style:inherit}.mw-parser-output q{quotes:"""""""'""'"}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-limited a,.mw-parser-output .cs1-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:#555}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}
   


2. 
   ^ The Indus Basin of Pakistan: The Impacts of Climate Risks on Water and Agriculture. World Bank publications. p. 59. ISBN 9780821398753.
   


3. 
   ^ "Geography: The rivers of Pakistan". Dawn. 26 September 2009. Retrieved 15 August 2017.
   


4. 
   ^ "Indus water flow data in to reservoirs of Pakistan". Retrieved 15 August 2017.
   


5. 
   ^ Witzel, Michael (1995), "Early Indian history: Linguistic and textual parameters", in Erdosy, George, The Indo-Aryans of Ancient South Asia: Language, Material Culture and Ethnicity, Walter de Gruyter, pp. 85–125, ISBN 978-3-11-014447-5
   


6. 
   ^ Thieme, P. (1970), "Sanskrit sindu-/Sindhu- and Old Iranian hindu-/Hindu-", in Mary Boyce; Ilya Gershevitch, W. B. Henning memorial volume, Lund Humphries, p. 450: "As the great frontier river that represents the natural dividing line between India and Iran, the Indus could most easily and fittingly be called Sindhu- 'Frontier' by the Indians and Hindu- 'Frontier' by the Iranians."
   


7. 
   ^ Osada, Toshiki (2006), Indus Civilization: Text & Context, Manohar Publishers & Distributors, p. 100, ISBN 978-81-7304-682-7: 'P. Theme (1991) understood the Indus as the "border river" dividing IA and Iran. tribes and has derived it from IE with an etymology from the root "si(n)dh" to divide."'
   


8. 
   ^ Boyce, Mary (1989), A History of Zoroastrianism: The Early Period, BRILL, pp. 136–, ISBN 90-04-08847-4: "The word hindu- (Skt. sindhu-), used thus to mean a river-frontier of the inhabited world, was also applied generally, it seems, to any big river which, like the Indus, formed a natural frontier between peoples or lands."
   


9. 
   ^ Bailey, H. W. (1975), "Indian Sindhu-, Iranian Hindu- (Notes and Communications)", Bulletin of the School of Oriental and African Studies, 38 (3): 610–611, JSTOR 613711: "The word sindhu- is used of a 'mass of water' (samudra-), not therefore primarily 'flowing' water. Hence the second derivation of 'enclosed banks' is clearly preferable."
   


10. 
    ^ Parpola 2015, Chapter 9.
    


11. 
    ^ Prasad, R.U.S. (25 May 2017), River and Goddess Worship in India: Changing Perceptions and Manifestations of Sarasvati, Taylor & Francis, pp. 23–, ISBN 978-1-351-80655-8
    


12. 
    ^ Mukherjee, Bratindra Nath (2001), Nationhood and Statehood in India: A historical survey, Regency Publications, p. 3, ISBN 978-81-87498-26-1: "Apparently the same territory was referred to as Hi(n)du(sh) in the Naqsh‐i‐Rustam inscription of Darius I as one of the countries in his empire.[10] The terms Hindu and India ('Indoi) indicate an original indigenous expression like Sindhu. The name Sindhu could have been pronounced by the Persians as Hindu (replacing s by h and dh by d) and the Greeks would have transformed the latter as Indo‐ (Indoi, Latin Indica, India) with h dropped..."
    


13. 
    ^ Mountjoy, Shane (2004), The Indus River, Infobase Publishing, pp. 8–, ISBN 978-1-4381-2003-4
    


14. 
    ^ Possehl, Gregory L. (1999), Indus age: the beginnings, University of Pennsylvania Press
    


15. 
    ^ "An A-Z of country name origins | OxfordWords blog". OxfordWords blog. 2016-05-17. Retrieved 2017-06-23.
    


16. 
    ^ Kuiper 2010, p. 86.
    


17. 
    ^  Holdich, Thomas Hungerford (1911). "Indus". In Chisholm, Hugh. Encyclopædia Britannica. 14 (11th ed.). Cambridge University Press. pp. 507–508.
    


18. 
    ^ 70% of cattle-breeders desert Banni; by Narandas Thacker, TNN, 14 February 2002; The Times of India
    


19. 
    ^ "564 Charul Bharwada & Vinay Mahajan, Lost and forgotten: grasslands and pastoralists of Gujarat".
    


20. 
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21. 
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22. 
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23. 
    ^ Henry Yule: India, Indies Archived 28 June 2012 at Archive.is. In Hobson-Jobson: A glossary of colloquial Anglo-Indian words and phrases, and of kindred terms, etymological, historical, geographical and discursive. New ed. edited by William Crooke, B.A. London: J. Murray, 1903
    


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    ^ "Was the Ramayana actually set in and around today's Afghanistan?".
    


25. 
    ^ Clift; Gaedicke; Edwards; Lee; Hildebrand; Amjad; White; and Schlüter (2002). "The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea". Marine Geophysical Researches. 23 (3): 223–245.CS1 maint: Uses authors parameter (link)
    


26. 
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27. 
    ^ Clift, Peter D.; Shimizu, N.; Layne, G.D.; Blusztajn, J.S.; Gaedicke, C.; Schlüter, H.-U.; Clark, M.K.; Amjad, S. (August 2001). "Development of the Indus Fan and its significance for the erosional history of the Western Himalaya and Karakoram". GSA Bulletin. 113 (8): 1039–1051. doi:10.1130/0016-7606(2001)113<1039:DOTIFA>2.0.CO;2.
    


28. 
    ^ Zeitler, Peter K.; Koons, Peter O.; Bishop, Michael P.; Chamberlain, C. Page; Craw, David; Edwards, Michael A.; Hamidullah, Syed; Jam, Qasim M.; Kahn, M. Asif; Khattak, M. Umar Khan; Kidd, William S. F.; Mackie, Randall L.; Meltzer, Anne S.; Park, Stephen K.; Pecher, Arnaud; Poage, Michael A.; Sarker, Golam; Schneider, David A.; Seeber, Leonardo; Shroder, John F. (October 2001). "Crustal reworking at Nanga Parbat, Pakistan: Metamorphic consequences of thermal-mechanical coupling facilitated by erosion". Tectonics. 20 (5): 712–728. doi:10.1029/2000TC001243.
    


29. 
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30. 
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31. 
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32. 
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33. 
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34. 
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35. 
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36. 
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37. 
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38. 
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39. 
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40. 
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41. 
    ^ "Irrigation water quality—salinity and soil structure stability" (PDF). Retrieved 25 June 2018.
    


42. 
    ^ Walsh, Declan (2010-10-21). "Pakistan floods: The Indus delta". The Guardian.
    


43. 
    ^ Walsh, Declan (2010-10-05). "Pakistan's floodwaters welcomed along Indus delta". The Guardian.
    


44. 
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45. 
    ^ Pulitzercenter.org^{[dead link]}
    


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    ^ Farrow, Ronan (2018). War on Peace: The End of Diplomacy and the Decline of American Influence. W. W. Norton. ISBN 978-0393652109.
    


47. 
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48. 
    ^ "Fishing poison killing Indus dolphins, PA told". Dawn. 8 Mar 2012. Retrieved 27 April 2016.
    


49. 
    ^ "'18 dolphins died from poisoning in Jan'". Dawn. 1 May 2012. Retrieved 28 June 2012.
    


50. 
    ^ "Threat to dolphin: Govt bans fishing between Guddu and Sukkur". The Express Tribune. 9 Mar 2012. Retrieved 28 June 2012.
    


51. 
    ^ "Almost all plastic in the ocean comes from just 10 rivers - 30.11.2017". DW.COM. Retrieved 2018-08-22. about 90 percent of all the plastic that reaches the world's oceans gets flushed through just 10 rivers: The Yangtze, the Indus, Yellow River, Hai River, the Nile, the Ganges, Pearl River, Amur River, the Niger, and the Mekong (in that order).
    


52. 
    ^ Schmidt, Christian; Krauth, Tobias; Wagner, Stephan (2017-10-11). "Export of Plastic Debris by Rivers into the Sea". Environmental Science & Technology. American Chemical Society (ACS). 51 (21): 12246–12253. doi:10.1021/acs.est.7b02368. ISSN 0013-936X.
    


53. 
    ^ "Indus Basin Floods" (PDF). Asian Development Bank. 2013. Retrieved 20 November 2018.
    


54. 
    ^ Bodeen, Christopher (8 August 2010). "Asia flooding plunges millions into misery". Associated Press. Retrieved 8 August 2010.
    


55. 
    ^ Guerin, Orla (7 August 2010). "Pakistan issues flooding 'red alert' for Sindh province". British Broadcasting Corporation. Retrieved 7 August 2010.
    


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    ^ Government of Pakistan Pakmet.com.pk Retrieved on 19 September 2011 Archived 24 April 2012 at the Wayback Machine.
    


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Sources

.mw-parser-output .refbegin{font-size:90%;margin-bottom:0.5em}.mw-parser-output .refbegin-hanging-indents>ul{list-style-type:none;margin-left:0}.mw-parser-output .refbegin-hanging-indents>ul>li,.mw-parser-output .refbegin-hanging-indents>dl>dd{margin-left:0;padding-left:3.2em;text-indent:-3.2em;list-style:none}.mw-parser-output .refbegin-100{font-size:100%}

• 
  G.P. Malalasekera (1 September 2003), Dictionary of Pali Proper Names, Volume 1, Asian Educational Services, ISBN 978-81-2061-823-7
  


• Albinia, Alice. (2008) Empires of the Indus: The Story of a River. First American Edition (20101) W. W. Norton & Company, New York.
  ISBN 978-0-393-33860-7.


• World Atlas, Millennium Edition, p. 265.


• Jean Fairley, "The Lion River", Karachi, 1978.

External links

Wikimedia Commons has media related to: Indus River (category)

• 
  Blankonthemap The Northern Kashmir Website


• 
  Bibliography on Water Resources and International Law Peace Palace Library


• Northern Areas Development Gateway


• The Mountain Areas Conservancy Project


• Indus River watershed map (World Resources Institute)


• Indus Treaty


• Baglihar Dam issue


• Indus


• 
  Indus Wildlife at the Wayback Machine (archived 7 October 2006)


• First raft and kayak descents of the Indus headwaters in Tibet


• Pulitzer Center on Crisis Reporting's project on water issues in South Asia

Links to related articles

v t e Hydrography of Pakistan Lakes Attabad Ansoo Baghsar Banjosa Borith Chitta Katha Dudipatsar Hadero Haleji Hanna Karambar Keenjhar Khabikki Kundol Lower Kachura Lulusar Mahodand Manchar Namal Payee Pyala Rama Rawal Rush Saiful Muluk Satpara Sheosar Shonter Siri Subri Uchhali Upper Kachura Rivers Indus Astore Bara Basol Braldu Bunhar Chenab Dasht Dori Gambila Ghaggar-Hakra Gilgit Gomal Haro Hingol Hispar Hunza Jhelum Jindi Kabul Kech Korang Kunar Mula Neelum Panjkora Panjnad Poonch Rakshan Ravi Rupal Shaksgam Shigar Shingo Shyok Soan Suru Sutlej Swan Swat Tawi Zhob Coastal Indian Ocean Arabian Sea Gulf of Oman Categories Lakes Rivers v t e Hydrography of the Indian subcontinent Inland rivers Beas Betwa Bhagirathi Brahmaputra Chambal Chenab Damodar Godavari Gandaki Ganges Ghaghara Indus Jhelum Kali Kaveri Kosi Krishna Luni Mahanadi Mahaweli Meghna Narmada Padma Ravi Sarasvati Sankosh Sharda Son Sutlej Tapti Yamuna Inland lakes, deltas, etc. Ganges Basin Ganges Delta Indus Delta Dal Lake Pookode Lake Skeleton Lake Chilika Lake Lake Powai Borith Lake Saiful Muluk Gosaikunda Nizam Sagar Red Hills Lake Malampuzha Kerala backwaters Pulicat Lake Coastal Indian Ocean Arabian Sea Bay of Bengal Gulf of Kutch Gulf of Khambhat Gulf of Mannar Laccadive Sea Palk Strait Categories Lakes of Bangladesh / India / Nepal / Pakistan Reservoirs and dams in India Rivers of Bangladesh / Bhutan / India / Nepal / Pakistan v t e Rivers of India Seven Great Rivers of India Indus . Ganges · Yamuna · Brahmaputra · Krishna · Godavari · Kaveri Indus River Basin Indus River Panjnad River (Pakistan) Sutlej River Beas River Parbati River (Himachal Pradesh) Chenab River Ravi River Jhelum River Neelum River or Kishanganga Suru River Dras River Shingo River Yapola River Zanskar River Markha River Khurna River Tsarap River Doda River Hanley River Marutsudha River Ganges River Basin Ganga River Hooghly River Damodar River Barakar River Jahanavi River Jalangi River River Churni Ichamati River Rupnarayan River Ajay River Mayurakshi River Dwarakeswar River Mundeswari River Meghna River Padma River Punarbhaba River Atrai River Mahananda River Kosi River Bagmati River Bhurhi Gandak River Phalgu Gandaki River Son River North Koel River Amanat River Rihand River Gopad River Goini River Neur River Banas River Johilla River Ghaghara River West Rapti River Rohni River Sarda River Ladhiya River Sarayu River Gori Ganga River Darma River Gomati River Sarayan River Kathna River Yamuna River Ban Ganga River Ken River Betwa River Dhasan River Halali River Kaliasote River Sindh River Kwari River Hindon River Karban River Pahuj River Chambal River Kuno River Banas River Berach River Bandi River Mashi River Morel River Kotari River Shipra River Ahar River Kali Sindh River Parbati River (Madhya Pradesh) Gambhir River Parbati River (Rajasthan) Ramganga River Khoh River Mandal River Alaknanda River Mandakini River Pindar River Nandakini River Dhauliganga River Rishiganga River Bhagirathi River Bhilangna River Jahnavi River Godavari River Basin Purna River Pranahita River Wainganga River Kanhan River Kolar River Pench River Kulbehra River Nag River Wardha River Penganga River Pedda Vagu River Indravati River Bandiya River Sabari River Pravara River Manjira River Manair River Other minor tributaries: Taliperu River Kinnerasani River Darna River Sindphana River Krishna River Basin Krishna River Koyna Venna River Varna River Panch ganga Vedganga river Tillari Bhima Agrani Yerala Varada River Tungabhadra River Tunga River Bhadra River Vedavathi River Suvarnamukhi River Veda River Avathi River Bhima River Sina River Nira River Mula-Mutha River Mula River Mutha River Chandani River Kamini River Moshi River Ambi River Bori River Man River Bhogwati River Indrayani River Kundali River Kumandala River Ghod River Bhama River Pavna River Malaprabha River Ghataprabha River Varma River Venna River Urmodi River Koyna River Pennar River Basin Pennar River Kaveri River Basin Kaveri River (Cauvery) Kollidam (distributary) Amaravati River Arkavathy River Bhavani River Sarabanga River Noyyal River Hemavati River Kabini River Lakshmana Tirtha River Tapi River Basin Tapi River Tapi River Gomai River Arunavati River Panzara River Kaan River Aner River Girna River Titur River Waghur River Purna River Nalganga River Vaan River Morna River Katepurna River Umaa River Sangiya River Mahi River Basin Mahi River Som River Gomati Riverty5h65 Sabarmati River Basin Sabarmati River 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River Shastri River Gad River Vashishti River Savitri River Kundalika River Gandhari River Patalganga River Ulhas River Thane Creek Vasai Creek Mithi River or Mahim River Oshiwara River Dahisar River Tansa River in Thane Vaitarna River Surya River Chenna River Terna river Other major rivers Ghaggar River Musi River Samir River, India/ india Luni River Bhavani River v t e Indus Valley Civilisation History and culture Indus River Periodisation Bhirrana Culture Mehrgarh Culture Kulli Culture Amri Culture Bara Culture Cemetery H Culture Architecture Harappan architecture Sanitation of the Indus Valley Civilisation Great Bath, Mohenjo-daro Inventions of the Indus Valley Civilisation Language and script Harappan language Indus script Indus Valley sites in Pakistan Harappa Mohenjo-daro Nausharo Chanhudaro Mehrgarh Lakhueen-jo-daro Larkana Pirak Kot Diji Rehman Dheri Amri Sutkagan Dor Sokhta Koh Tharro Hills Pir Shah Jurio Allahdino Balakot Ongar Ganeriwala Nindowari Judeir-jo-daro Dabarkot Indus Valley sites in India Dholavira Gola Dhoro Lothal Bhagatrav Rangpur Jognakhera Surkotada Kalibangan Manda Alamgirpur Daimabad Malwan Kunal Rakhigarhi Rupnagar Rupar Hulas Kanmer Oriyo timbo Dher Majra Lohari Ragho Dwarka Kuntasi Loteshwar Mandi Farmana Ganeshwar Sothi Siswal Sanauli Sanghol Pabumath Nagwada Babar Kot Balu Bara Bargaon Bhagwanpura Bhirrana Banawali Rojdi Kotla Nihang Khan Kerala-no-dhoro Mitathal Desalpur Indus Valley sites in Afghanistan Mundigak Shortugai Related topics Meluhha Ochre Coloured Pottery culture Northern Black Polished Ware Painted Grey Ware culture v t e Rigveda Mandalas 1 2 3 4 5 6 7 8 9 10 Deities Devas Agni Indra Soma Ushas Visvedevas Maruts Ashvins Tvastar Rbhus Pushan Rudra Asuras Mitra Varuna Aryaman Apam Napat Demons Vritra Susna Dasas Danu Danavas Rivers Sapta Sindhu Nadistuti Sarasvati Sindhu Sarayu Rasā Rishis Saptarishi Gritsamada Vishvamitra Vamadeva Atri Angiras Bharadvaja Vasishta Dirghatamas v t e Punjab geography Beas River Bari 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Hydrography of surrounding areas Himachal Pradesh Punjab, India Pakistan v t e Geography of South Asia Mountains and plateaus Himalayas Mount Everest Western Ghats Eastern Ghats Aravalli Range Nilgiris Vindhya Range Satpura Range Garo Hills Shivalik Hills Mahabharat Range Khasi Hills Anaimalai Hills Cardamom Hills Sulaiman Mountains Toba Kakar Range Karakoram Hindu Kush Chittagong Hill Tracts Deccan Plateau Thar Desert Makran Chota Nagpur Naga Hills Mysore Plateau Ladakh Plateau Gandhamardan Hills Malwa Lushai Hills Lowlands and islands Indo-Gangetic plain Doab Indus Valley Indus River Delta Ganges Basin Ganges Delta Terai Atolls of the Maldives Coromandel Coast Konkan Lakshadweep Andaman and Nicobar Islands Sundarbans Reserve Forest Greater Rann of Kutch Little Rann of Kutch Protected areas in Tamil Nadu By country India Pakistan Nepal Bhutan Sri Lanka Bangladesh Maldives Afghanistan

v t e Major rivers of China
Seven Great Rivers of Eastern China Yangtze · Yellow · Pearl · Heilongjiang · Huai · Hai · Liao
Yangtze system	Yalong Min Dadu Qingyi (Sichuan) Tuo Jialing Bailong Fu (Sichuan) Qu Wu Hanshui Muma Chi Du Bao Qing Chishui Xiang Xiao Lei Mi Zi Yuan Lishui Miluo Gan Fu (Jiangxi) Xin Qingyi (Anhui) Qinhuai Xitiao Huangpu Suzhou Creek
Yellow system	Daxia Tao Qingshui Wuding Fen Wei Jing Luo (Henan) Luo (Shaanxi) Qin Xiaoqing
Pearl system	North East Han (Guangdong) Mei Ting West Yujiang Yong Xun Qian Hongshui Nanpan Beipan Rong Li (Guangxi) Gui Liu
Heilongjiang system	Songhua 2nd Songhua Nen Mudan Ussuri Argun Kherlen Woken Huifa
Huai system	Guo Ying Shiguan Quan Hui Hong
Hai system	Chaobai Yongding Hutuo Ziya Daqing Wenyu Juma Sanggan Fuyang Wei Ju Jiyunhe
Liao system	Hun Taizi Xar Moron Xinkai Western Liao Eastern Liao
Other major rivers	Tarim Black Karatash Ili Shule Tumen Yalu Luan Red Minjiang Longjiang Lancang Beilun Nujiang Lion Spring Elephant Spring Yarlung Tsangpo Nyang Subansiri Irtysh Suifen Qiantang Puyang Jiao (Shandong) Dai Si Shu Cao'e Jiao (Zhejiang) Ou Mulan Jin (Fujian) Nandu Wanquan Taping
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