Tributaries of brahmaputra nadi

Continue For others, see Brahmaputra(disambiguation). Rivers of China, India, and Bangladeshi BrahmaputraDilao, LauhityaThe Brahmaputra in Guwahati, Assam, IndiaPath of the [1]Etymologyskrit; Brahmaputra for Sound (Metera) in BrahmāLocationCountriesChinaIndiaBangladeshAutonomous RegionTibetCibetCibetciesDibrughorGorhatzpurGuhatidhuburiSirganjuganjymensingphymenshingPhyphysicalSourceSourceAng Glacier, Manasarovar • whereHimalayas • coordinates30°23′ 82°0′E/30.383°N 82.000° E / 30.383; 82,000 • elevation5,210 m (17,090 ft) MouthGanges • Where Delta • coordinator 13′24N 89°41′41E/25.2233° N89.69472° E / 25.22333; 89.69472Codordinates: 25° 13′24N 89°41′41E/25.2233° N 89.69472° E / 25.22333; 89.69472 • Elevation0 m (0 ft) LengthMaped 3.969 km (2.466 mi). [1] Actual 4,696 kim (2,918 mi). Basin size712,035 km2 (274,918 sq mi)Discharge • average19,800 m3/s (700,000 cu ft/s) • maximum100,000 m3/s (3,500,000 cu ft/s) Basin featuresTributaries • leftLhasa River, Nyang River, Parlung Zangbo, Lohit River, , • rightKameng River, , Beki River, Raidak River, Jaldhaka River, Teesta River, Subansiri River The Brahmaputra (/ˌbrɑːməˈpuːtrə/), called Yarlung Tsangpo in Tibet, Siang/Dihang River ,, in and Luit, Dilao[2] in Assam, is a trans-boundary river which flows through Tibet, India and Bangladesh. [a] It is the largest river in the world by disecute, and the 15th longest. With its origin in the Lake Manasarovar region, Near the Kailash Mountain, Located on the north side of Italayas in Burang County of Tibet as the Yarlung Tsangpo river, [1] it flows to the south of Small collapsed via the Himalayas to major targets (including the Yarlung Tsangpo Grand Canyon) and the Arunachal Pradesh (India). [4] It flows westside of the Assam Value as Brahmaputra and to the south across Bangladeshi as Jamuna (not to be mistaken with Yamuna in India). In the vast Delta Ganges, he merged with the Padma, the popular name of the River Ganges of the River in Bangladeshi, and finally, after being merged with Padma, he gets Meghna and out here, it flows like the Meghna River before empty in the Bengal. [5] Approximately 4,696 kim (2,918 mi)[1] long, the Brahmaputra is an important river for irrigation and transport in the region. The average depth of the river is 140 m (450 ft) and maximum depth is 370 m (1.200 ft). The river tends to flood catastrophic in the spring when the snow melted the Himalayan snow. The average discharge of the river is about 19,800 m3/s (700,000 cu ft/s), [4] and floods reach about 100,000 m3/s (3,500,000 cut ft/s). [6] It is a classic example of a stream and is highly sensitive to channel migration and avulsion. [7] He is also one of the rivers in the world expose a tire. It is navigable for most of its length. The river crossed eastern Himalayan through the Indo-Nepal border, the south-central portion of the Tibetan plateau above bowl in Ganga, the southern part of the east of Tibet, the cholin Patkai-Bum, the northern slope of the Meghalaya mountains, the plain Assam, and the northern portion of the Banglades. The bowl, especially in southern Tibet, is characterised by high levels of rain. Kangchenjunga (8.586 m) is the only shovels above 8,000 m, hence is the highest point of the Brahmaputra belt. Brahmaputra's upper neck was long unknown, and its identity with the Tsangpo Yarlung was only established by exploration in 1884–86. This river is often called the Tsangpo-Brahmaputra river. [summons needed] Lower reach is sarcast for Hindu. While most streams on the Indian substance have female names, this river has a rare male name. Brahmaputra means Brahma's child in Sanskrit. [8] Geography Course Tibet Main Article: Yarlung Tsangpo Yarlung River Tsangpong in tibet above reaches the river brahmaputra, known as the Yarlung Tsangpo from the Tibetan language, origins on the Glascier to Angsi, near Mount Kailash, is located on the north side of the Italayas of Burang County of Tibet. The source of the River Was earlier thought to be on the Chemayung Glacier, which covers the slope of the Italayas about 97 kilometers (60 mi) of southeast Lake Manasarovar in southern Tibet. The river is 3.969 kim (2.466 mi) long, and its drainage area is 712.035 km2 (274.918 sq) according to the new results, while previous documents showed its length varies from 2,916 kim (1,812 mi) to 3,364 kim (2,090 mi)and its drainage area between 520,000 and 1.73 million km2. This finding was provided by Liu Shaochuang, a researcher with the Institute of Remote Applications under the analysis using expedition and satellite imagery from the Chinese Academy of Sciences (CAS). [1] [9] From its sources, the river runs for almost 1,100 kilometers (680 walls) in a generally conveniently direction between the main range of Healayas in the south and Range of Kailas to the north. In Tibet, the Tsangpo receives a number of tributaries. The most important kite-bank courts are the Raka Zangbo (Raka Tsangpo), which join the western river Xigazê (Shigatse), and the Lhasa (Kyi), which flows past the Tibetan capital of Lhasa and joining the Tsangpog in Qüxüxü. The Nyang River enters the Tsangpo from the north of Zela (Tsela Dg). On the right bank, a second river called Nyang Qu (Nyang Chu) meets Tsangpo's in Xigazê. After passing Pi (Pe) into Tibet, the river turns suddenly to the north and northeast and cuts a course of a succession of narrow chargeous charges between the mountainous masses of Gyala Peri and Namcha Barking in a quick and cascading range. And the river turned around and sidwestern and leaking across a deep throat (the Yarlung Tsangpo Grand Canyon) via the eastern extremists of the Italayas and canyon walls extended above to 5,000 m (16,000 ft) and more on each side. During this stretch, the river enters the northern state of Arunachal Pradesh in , where it is known as the Dihang (or Siang) River, and turns more please. Assam and premiers of Brahmaputra region bowl in India A view at sundown of the Brahmaputra from the Dibrugarh Yarlung Tsangpo to enter the state of Arunachal Pradesh in India, where it is called Siang. It makes a very quick descent from its original height in Tibet and finally appears in the plain, where it is called Dihang. It flows for about 35 kim (22 mi) south after that, it is joined by the and the Lohit River at the top of the Assam Valley. Below the Lohit, the river is called Brahmaputra and Doima (Mothers of Water) and Burlung-Buthur by native Bodo tribal, it then enters the state of Assam, and becomes wide as 20 km (12 mi) in parts of Asam. The dihang, winds from the mountains, turn towards the southeast and down to a low basin as it enters the state of Ascent northeast. Just west of the city of Sadiya, the river is again back in the southwestern and is joined by two mountain water sources, the Lohit, and the Dibang Turtles. Under this conflict, about 1,450 km (900 walls) from the Bay of Bengal, the river becomes conventionally known as the Brahmaputra (Son of Brahma). In Assam, the river is mighty, even in the dry season, and during the rains, its banks have more than 8 kim (5.0 mi) apart. As the river follows it 700 kilometers (430 mi) of the value, it receives several rapidly flowing Italayan fighting, including the Subansiri, Kameng, Bhareli, Dhansiri, Manas, Champamati, Saralbhanga, and Sankosh Rivers. The main courts from the hills and in the plateau to the south are the Burhi Dihing, the Disang, the Dikhu, and the Copying. Between Dibrugarh and Lakhimpur Districts, the river is divided into two channels—north of the channel Kherkutia and channels south of Bramamaputra. The two channels join again about 100 kim (62 mi) fishermen, forming the Islands, which is the largest river island in the world. [10] In Guwahati, near the ancient pelgrimage center of Hajo, the Brahmaputra is cut off from the rocks of the Shillong Plateau, and is at its narrow within 1 kilometer (1,100 yd) bank-to-bank. The landslide in that area made it logistically ideal for the battle of Saraighat, the military showdown between the Empir Mughal and the Kingdom of Ahom in March 1671. The first combined railroad bridge/road via the Brahmaputra was constructed in Saraighat. It opened to traffic in April 1962. The environment of the flooding Brahmaputra in Assam has been described as the Valley of Brahmaputra forest ecoregion. The Bangladeshi River Bangladeshi, including the Brahmaputra in Bangladeshi, is the Brahmaputra together by the Teesta River (or Tista), one of its largest courts. Below the Tista, split the Brahmaputra into two branch dispensers. The western branch, which has the majority of the river flow, continues due to south as the Jamuna (Jomuna) to merge with lower Ganga, called the Padma River (Pôdda). The eastern branch, the former largest, but now smaller, is called the Lower or Old Brahmaputra (Brommoputro). It curve centuries to join the river Meghna near Dhaka. Padma and Meghna converge near Chandpur and flow from the Bay of Bengal. This final part of the river is called Meghna. Brahmaputra's side enter the plains of Bangladeshi after turning southward around the Garo Mountains under the Dhuburi, India. After sink past Chilmari, Bangladeshi, it is joined on its right bank by the Tista River and then follow a 240 kilometer (150-mi) course due south as the Jamuna River. (South Gaibanda, the former Brahmaputra left the bank of the mainstream and past colors Jamalpur and Mymensingh to join the Meghna River in Bhairab Bazar.) Prior to his controversy with the Ganga, the Jamuna receives the combined waters of the Baral, Artrai, and Hurasagar River on its right bank and becomes the point of departure of the Dhaleswari River on its left bank. A tribulation of the Dhaleswari, the Buriganga (Old Ganga), flowed past Dhaka, the capital of Bangladeshi, and joining the Meghna River above Munshiganj. The Jamuna join with the Ganga north of Goalundo Ghat, below which, as the Padma, flows water to the southeast for a distance of about 120 kim (75 mi). After several smaller branch channels of Ganga-Brahmaputra delta foods in the south, the main body of Padma has reached its controversy with the Meghna River near Chandpur and then entered the Bay of Bengal in estimated Meghna and smaller channels flowed into the delta. The growth of the Ganga- Brahmaputra delta is dominated by tidal processing. The Ganga Delta, nurtured by the waters of many rivers, including Ganga and Brahmaputra, is 59.570 square kilometers (23,000 sq miq) the largest delta in the world. [11] Brahmaputra Bath River features Brahmaputra from the barrel space of the Brahmaputra river is 651 334 km2 and it is a good example of a wide river and median quite a bit and often temporary sand form. A region of important technical activities developed in the Jamuna River and is associated with himalayan edification and development of the Bengal forep. Several researchers have hypothesis that the underlying structural control on the location of the major river systems in Bangladeshi. An area of 'structural weakness' over the present course of the Ganga-Jamuna-Padma-Padma River due to either a hard subsidized or a in depth observed by Morgan and Melntire. (1959). Scijmonsbergen (1999) ringed that the breadth of changes in Jamuna's can respond to these faults and may also cause sedimentation of investments in the fault. It presented a few images arguing that a doom fault in the Bangabandhu Multipurpose Bridge has affected migration channels. Large accumulation of sediments produced in Himalayan erosion was produced due to depths of the Bengal basin, with the thickness of sediments above the Precambrian foundation of increase from a few hundred meters to the region shelves more than 18 kilometers of bengal evidence in the south. The tekonic and climatic context for the water resilient and disseminated sediments of Bangladeshi rivers were set by the ongoing subsidy of Bengal basin, combined with high rates of Himalayan education. The control of lift and subsidence is, however, clear. The courses in the Jamuna and Ganga Rivers are first order control due to the fact that they are more influenced by the rise of Plcistocnc [the necessary clarification] terrace in Barind and Madhupur tracts. [12] The Hydrology System of the Ganga-Brahmaputra has the third-oldest medium river delay in the world -- roughly 30.770 m3 (1.086.500 ft3) per second; and the Brahmaputra river alone supplies about 19,800 m3 (700,000 ft3) per second of the total discharge. The combined river stops sediments of approximately 1.87 billion tonnes (1.84 billion tonnes) per year is the highest in the world. [4][13] In the past, the lower course of the Brahmaputra was different with than in the Jamalpur and Mymensingh districts. In an earthquake of 8.8 on 2 April 1762, however, the main channel of the Brahmaputra in Point Bhahadurabad has changed south direction and opened as Jamuna due to the result of relief techniques of tracturer in Madhupur. [14] Rising climate temperature is one of the biggest causes of snow-melted in the upper delivery of Brahmaputra. [15] The dispatch of the river Brahmaputra is highly affected by snow melted in the upper part of its place. Then in river flow due to the melt of snow in the river Brahmaputra affects the dispatch down to the river. This increase in the releases due to the significant withdrawal of snow gives rise to severe catastrophic problems such as flooding and erosion. The weather is a purely cold climate and pepper buckle. The unloading of the Brahmaputra river is characterised by its significant rate of sediment sediments, concrete flow and variables, along with its rapid channel's agradation and rate and accelerated in basin demand. After a time, deepening of the basin in Bengal caused by erosion will cause the increase in hydraulic rays, with consequently allowing for the huge accumulation of food sediments in the Himalayan erosion by transport sediment effective sediments. Thickness of the accumulated sediment above The basement has increased over the years to some hundred meters more than 18 kilometers of deep-deep bengal in the south. The continuous subsidies of basin in Bengal and the high rate of Himalayan edification continue to contribute to the huge water with sand circulation sediments and belt, and 1% clay, in the Brahmaputra river. Climatic changes play a critical role in affecting the basin ideology. Throughout the year, there is a significant increase in hydrography, with a large spft between July and September. Brahmaputra's rivers experience two major winter water seasons, one of early summer caused by snow caused by snow in the mountains, and one in late summer caused by runof from monster rain. The flow of rivers strongly influenced by snow and ice flows melt in the glaciers, which make them mainly over the eastern Himalayas regions of the mainstream parts of the bowl. The snow and dissolved contribution to the annual total is about 27%, while annual rain contributes to about 1.9m and 19,830 m3/s in dispatch. The highest registered daily disposer of the Brahmaputra in Pandu was 72,726 m3/s August 1962 while the lowest was 1,757 m3/s in February 1968. The increasing rates of snow and melted glaciers are likely to increase summer drimmup in some river systems for a few decades, followed by a reduction in color as the glaciers disappear and snow decrease. This is particularly true for the dry season when water availability is critical for the irrigation systems. The evolution of the flooding course in the Brahmaputra River has changed drastically in the past two centuries and a half century, moving its river course west to a distance of approximately 80 miles (50 walls), leaving its ancient river neck, suitable called the ancient Brahmaputra river, behind. In the past, the flooding of the old river's neck had terrain that was better formed compared with class sediments along the River Jamuna river Jamuna. This change in the river neck causes modification to the tel-formed process, including asdification, the breakage of clay and the building of organic matter, with soil showing an increasing amount of biotic homogenization, motling, the layers around Peds and terrain accommodation, shapes and patterns. In the future, the consequences of local soil subsidy coupled with flood proposals, for example, the localized flood waters, which increase flood water in depth outside water breaks, can change the water levels in the floods. Throughout the years, the bars rolled, and the sand formed at the edge of the plain of flooding by storage. The height difference in the channel topography is often no more than 1m-2m. In addition, flooding on the history of the Nile River caused the formation of river levels due to deposition from flow of sybanks. The difference between the top left and plain floods is that enthusiasm is typically sets small channels with 2-3m along major channels. Crevasse spies, an sedimentary flivial deposit that forms when a current breaks natural or artificial levels and deposit sediments on a plain flood, are often formed due to a breach at the level, forming a fat mass that adgrades on the adjacent flood. At the end, basin floods are often formed between levels of adjacent rivers. The flooding village along the Brahmaputra during the monsoon season (June-October), the floods are a very common occurrence. Deforestation of the Brahmaputra water has caused increased sultation levels, flash floods, and erosion resulted in critical downstream habitats, such as the Kaziran National Park among Assam. Occasionally, massive flooding causes huge losses of crops, life, and property. Periodic flooding is a natural phenomenon that is ecologically important because it helps keep the lowland grasland and associated wildlife. Periodic flooding also deposits alloy fees, filling the fertil soil in the Brahmaputra River Valley. So flooding, agriculture, and agricultural practices are well connected. [16] [17] [18] The effects of flooding can be devastated and cause major damage to crops and houses, severe bank euros and the consequent loss of hotel houses, schools and land, and loss of numerous lives, livestock, and sins. During the 1998 flood, about 70% of the Bangladeshi area was founded, affecting 31 million people and 1 million otestead. In the 1998 floods that had a long-term duration from July to September, claimed 918 people's lives and was responsible for damage 16 00 and 6000 foam roads and embarkment respectively, and affected 6000 km2 of crop standing. The 2004 floods, about 25% of the population of Bangladeshi or 36 million people, have been affected by the floods; 800 lives have been lost; 952 000 homes were destroyed and 1.4 million were badly damaged; Four four 000 educational institutions were affected such as the destruction of 1200 primary schools, 2 million government and private tube assets being affected, over 3 million washing or washing away, this increased risk of diseases with diarrhea and cholera. Also, the 1.1M ha of the rice crop was submerged and lost before it could harvest, with 7% of the hacking per year (early season) crops of rice lost; 270 000 ha of glasses were affected, 5600 livestock had perished along with 254 000 poultry and 63 MT of lost fish production. Flood control measures are taken by the Water Resources Department and Brahmaputra's Flood Control Commission, but till now the flood problem remains idle. At least one third of Majuli land was crossed by the river. Recently, it suggests that a highway protected by concrete match on the river and the exclusion of the river bed can heal this threat. This project, named This Project The River Restoration Project is yet to be implemented by the government. The central government recently approved the construction of Brahmaputra's Old Deliberate Highway. The neck morphology channel of the Brahmaputra River has changed dramatically over the past 250 years, with evidence of large-scale avulsion, in the period 1776–1850, to 80 km from the east of the trak to the Madhupur in the west of it. Before 1843, Brahmaputra's shed in the channel has now witnessed Brahmaputra's old centuries. Banks of the nile river are mostly weak sand chorus and sixty, which are usually euros of large-scale failure, where they have already filed materials undergoing a hurricane and bank erosion during flood periods. Currently, the river erosion has decreased to 30mm per year as compared with 150m per year from 1973 to 1992. This erosion has, however, destroyed many lands that caused 0.7 million people to be homeless because of losses in the country. Several studies discussed the reasons for the avilation of the River in its present course, and suggested a number of reasons including teconic activities, switched to the upstream course of the Teesta River, the influence of increasing dissorder, catastrophic flooding and captured ancient rivers. From an analysis of the river's map between 1776 and 1843, concluded in a study that the avulsion of the river was more likely to be more likely gradual than catastrophic and sudden, and may have been produced by bank erosion, possibly around a large mid-channel bar, resulting in a diversion of the channels through the existing flood channel. The Brahmaputra channel is governed by the pak and low flow period during which her bed underwent formidable modification. Brahmaputra's bank migration is consistent with time. Beds in the Brahmaputra river have been largely great since 1916 and seems to be moving further towards the south than toward the north. Along with the contemporary migration of the nile river, the bank is left being eroded far beyond the right bank. [19] The River Engineering Brahmaputra River Experiences high levels of bank erosion (usually through slab failure) and migration channels caused by its current false, lack of vegetation of the river, and loose sand and verbose compounding its banks. It is so difficult to build permanent structures along the river, and protection structures designed to limit the effects of the erosional river often face many problems during and after construction. In fact, a 2004 [20] report by the Bangladeshi Disaster and Sub-Emergency Groups (BDER) stated that several of these protection systems had 'just failed'. However, some progress has been made in the form of construction work that stabilized sections of the river, albeit the need for heavy maintenance. The Bangabandu Bridge, the only bridge for the displaced greater distribution of the river, Jamuna, was thus opens in June Constructed in a narrow belt in the nile river, it is 4.8km long with an 18.5m wide platform, and is used to carry rail traffic as well as gas, power and telecommunications lines. Due to the variable nature of the nile river, the prediction of the River Nile is critical to planning engineers to prevent flooding on the bridge. China has built the Zangmu Dam in the upper neck of the Brahmaputra River in the Tibet region and was operationalized on 13 October 2015. The story of the Brahmaputra River is seen from a satellite place Brahmaputra and its courts in northeast India and Bangladeshi James Rennell in 1776 the map shows Brahmaputra's color before an earthquake on April 2, 1762 and the Teesta River will flow through three channels through the Ganga before a flood in 1787. Earlier accounts earlier stories gave his name as Dyardanes (ancient Greek Δυαρδάνης). [22] In the past, the course of the lower Brahmaputra was different with than in the Jamalpur and Mymensingh districts. Some water is still flowing in this course, now called the Ancient Brahmaputra, as a distribute of the main channel. One question about the river system in Bangladeshi is when and why the Brahmaputra changed its main course, at the site of the Jamuna and Old Brahmaputra to forks that can be seen by comparing modern maps of historical maps before the 1800s. [23] The Brahmaputra is likely to flow directly south along its main channel for much of time since the last maximum glacier, switching back and forth between the two strokes several times throughout the Holocene. One idea about the most recent absence is that the change in the course of the main waters of Brahmaputra's forest took place suddenly in 1787, the year of the heavy flood of the Tista River. In the mid-18th century, at least three water-sized sources flowed between the Rajshahi and Dhaka Divisions, Viz., Daokoba, a branch of the Tista, Monash or the Konayi, and Salangi's. Lahajang and the Elengjani were also important rivers. In Renault's time, The Brahmaputra as a first step towards concealing a more direct course to the sea by letting the Mahdupur Forest in the East began to send a considerable volume of water down the Jinai or Jabuna from Jamalpur to Monash and Salang. These rivers gradually calculated and kept displacement in the west until daokoba's encounter, showing an equally rapid trend of cutting in the east direction. The judgment of these rivers gave the Brahmaputra a worthy course for its immense power, and the rivers are straightforward and left untrue. In Altas Renault's are very similar to The River Jessore, drying up after Ganga's bloody mouth cut its new channel to join Meghna in the south of the Munshiganj subdisition. In 1809, Francis Buchanan- Hamilton wrote that the new channel between Bhawanipur and Dewanranj was clearly to the river, and threatens to sweep the intermediate country. By 1830, the old channel was reduced to its present insignificance. It was navigable by country boat throughout the year and not launched only during rain, but to the point as low as Jamalpur it was premidable throughout the cold temperature. The same was the position for two or three months just under Mymensingh as well. International water cooperation flows through the Brahmaputra River by China, India, and Bangladeshi. In the 1990s and 2000s, there was repeated speculation that mentioned Chinese plans to build a battle of the Great Bend, with a view of the diverse waters in the north of the country. This has been declined by the Chinese government for many years. [24] In the Kathmandu Workshop of the Foreight Strategic Group in August 2009 on water security in the Himalayan region, which led together in a rare development leading hydroologist from the basin countries, Chinese scientists have argued that it was not possible for China to undertake such a diversion. [25] However, on 22 April 2010, China confirmed that it was indeed built the Zangmu dam on the Brahmaputra in Tibet,[24] but assured India that the project would have no significant effect on the flow of fishermen in India. [26] This claim was also recovered by the Government of India, in an attempt to allocate domestic criticism of Chinese domestic construction on the river, but one remains warm to debate. [27] The last two years have seen a buildup of grassroots, especially in the state of Assam, against the Chinese registration building, as well as criticism from the Indian government for failure to perceive it for responding appropriate to Chinese hydropower plans. [28] At a meeting of scientists in Dhaka in 2010, 25 leading experts from the basin countries provided a Dhaka Statement on Water Safety [29] calling for information exchange in low-flow period, and other means of collaboration. Though the 1997 Un watercourss Convention doesn't prevent any of the bosine countries from building an investment harm, customer laws offer some relief to the lower lands. There is also potential for China, India, and Bangladeshi to cooperate on navigation of transbounde waters. Meaning gives people fishing in the River Brahmaputra lives many millions in India and Bangladeshi citizens are courageous on the river Brahmaputra. Delta it is home to 130 million people and 600 000 people live on the river islands. These people rely on the 'normal' flood to bring moisture and fresh sediments to the flooding grounds, hence providing the necessity for agricultural and marine agricultural sediments. In fact, two of the three seasonal rice varieties (aus and fine) cannot survive without the flood water. In addition, the fish keep both on the flood during the flood season from the flood medications they are the main source of protein for many rural populations. India Development Bridge Current Bridge Ranaghatt Bridge or Churni River Bridge on The Brahmaputra River near Pasighat in Arunachal Prades from the east to west until Parshuram Kund, then from the northwestern to northeast from Parshuram Kund to Patum, finally from east to southwestern from Parshuram to Kund Burhidhing: Sankosh Bridge near Gossaigaon on tributory in Brahmaputra on west Bengal-Assam border to Sankos Railway Bridge near Gossaigaon on tributory of Brahmaputra on west Bengal-Assam border Chilarai Bridge near Rupsi Airport on court of Brahmaputra Golakganj Bridge just to the southern Pont Chilarai near Rupsi Airport on tributory of Brahmaputra Old Saraighat Bridge, road and railway bridge near Guwahati in Assam New Saraighat Bridge, road bridge near Guwahati in Assam Kolia Bhomora Setu Road Bridge near Tezzpur in Assam, 3,015 Kim Naranarayan Setu , road and rail bridge near Bongaigaon in Assam, 2,284 km , road and railway bridge near Dibrugarh of Assam , 4.94 kilometers Dhola–Sadiya Bridge (Bhupen Harizaka Bridge), road and rail bridge along the Brahmaputra River of Brahmaputra near Chongkham in Assam, 9.15am long Dibang River Bridge, bridge over the river Brahmaputra to Court Aruchal Prades , 6.2km long connecting Bomjir and Malek Parshuram Kund Bridge road over the Lohmaputra River Court Arunachal Pradesh, Silluk-Dambuk Bridge, the bridge route to Arunachal Pradesh on the Tributary River Lohit Brahmaputra between the Silluk- Dambuk Ranaguhat Bridge on Brahmaputra in Pasighat of Arunachal Prades Patum Bridge on Brahmaputra Court near Aalo (ex-together) of the Arunachal Pradesh Wakro Bridge, bridges the road over the River Brahmaputra court in Arunachal Pradesh , Nao-Dihing Bridge paved on Brahmaputra courthouse of the Dihing River near Margherita, Assam and Ledo in Assam's NEEPCO Pont Bridge road on Brahmaputra's courtyard river near Jeypore Township. Assam Naharkatiya Bridge on Brahmaputra'' River tough court near Naharkatiya in Assam Burhidhing Railway Bridge on Brahmaputra court pushes river near Khowang to the Assam Bridge planned besides the Dhubri-Phulbari bridge , the five new bridges were announced in December 2017 by Indian Highway Minister Nitin Gadkari. [30] [31] From the east to the west: the Dhubri-Phulbari bridge, road and rail bridge of Assam, near tri-junction in east Meghalaya, Eastern Assam and northern Bangladeshi[30][31] Guwahati -North Guwahati [30][31] Bhomoraguri-Tezpur Bridge between Bhomoraguri-Tezzpur assembly [31] Numaligarh-Gozpur Between Gohpur-Numaligarh in Assam[30][31] Since the most vulnerable bridges to attack, on the request of the army this is being built as 4-lane 14.85km long tunnels and barriers and crash barriers , slits system, fire-fighting mechanism, footpath, a drainage system and emergency exits, and The 2020 update status by the construction government will begin in December 2020. [31] The Jorhat- Nematighat Bridge between Jojhat-Tezpur in Assam[30][31] Disangmukh-Tekeliphuta Bridge between Disangmu Tekh - Tekeliphuta near Sivasagar in Assam[30][31] Louit-Khablu Bridge (maybe it is one of the bridge with different names in the middle above?) [30] Under-river tunnels Gohpur-Numaligarh under-river tunnels[32] Bangladeshi See also: List of Bridges of Bangladeshi Shadows Bridge in Bangladeshi Bangladeshi Bridgeh (former Jamuna Bridge), road and rail bridge Padma Bridge, road and rail bridge on the Tributory River Padma of Brahmaputra Lalon Shah Bridge road on the River Court at Brahmaputra Hard Bridge, train bridge over Padma river next to Lalon Shah bridge planned at Bangladeshi Gaibandha-Bakshiganj Bridge , road and rail bridge to link existing railway and highway to Gaibandha-Bakshiganj on the other side of the Siraiganj River-Tangail Bridge, Road and rail bridge to connect existing railway with the route of Siraiganj-Tangail on the River River National Water 2 of India National Waterway 2 (NW2) is 891 kilometers long Sadiya-Dhubri stretch of the Brahmaputra river of Asam. [33] [34] See also BrahMos (missile) - A missile named partly after the Brahmaputra river Brahmaputra-class frigate Dhola-Sadiya bridge in Asian River Asia Listing of the Assam River in The Bangladeshi River List of China's River Rivers in India Reference River ^ as such, it is known by various names in the region: Assembly: লুইত Fruit [luɪt] , বৰ্পুতৰ্ ন Brohmoputro noi , বৰ্পুতৰ্ নদ (tatsama to ' ' none, masculine form of the tatsama ' ' nodi river) Brohmoputro [bɹɔɦmɔputɹɔ]; Sanskrit: , IAST: Brahmaputra; Tibetan: , Wylie: yar klung gtsang port Yarlung Tsangpo; simplified Chinese: ; traditional Chinese: ; Pinyin: Bùlāmǎpǔtelā Hé. It is also নদ নদী पु ཡར་ངས་གཙང་པོ་ 布拉⻢普特拉河 布拉⾺普特拉河 called Tsangpo-Brahmaputra and the Red River of India (when referring to the entire River including the stretch of the Autobet Autonomous Region). [3] ^ a b c d scientists pinpoint sources of four major international rivers. Xinhua News Agency. August 22, 2011. Archived from the original on 3 May 2016. Retrieved September 8, 2015. ^ Boruah, Sanjib (1999). India against itself: Assam and the Politics of Nationality. ^ Michael Buckley (30 March 2015). The price of Tibet's Damming River.The New York Times. p. A25. Archived from the original on 31 March 2015. Retrieved April 1, 2015. Two of the continent's wild rivers have the sources in Tibet: the Salween and the Brahmaputra. Though they are under threat of retired glaciers, a more immediate concern is Chinese engineering plans. A Waterfall Five the dam is planned for both the Salween, which currently flows freely, and the Brahmaputra, where one dom is already operational. ^ a b b c Brahmaputra River. Encyclopædia Britishca. Archived from the original on 30 January 2017. Retrieved 13 November 2016. ^ Brahmaputra River Flowing Down From Himalayas Bay in Bengal. Archived from the original on November 6, 2011. Retrieved 22 November 2011. ^ Water Resources in Bangladeshi. FAO. Archived from the original on 6 August 2009. Retrieved November 18, 2010. ^ Catling, David (1992). Rice in deep water. International Rice Research Institute. 177. ISBN 978-971-22-0005-2. Archived from the original on 14 May 2016. Retrieved November 15, 2015. ᘂ ᘁ Gautam Goals (help.). India through the ages. Publication Division, Ministry of Information and Broadcasting, Government of India. 80. ^ China Map Source Brahmaputra, Course. Assam Courthouse. August 24, 2011. Archived from the original on 22 July 2012. Retrieved November 9, 2011. ^ Majuli, River Island. Island's largest. Guinness World Records. Archived from the original on 3 September 2016. Retrieved September 6, 2016. ^ Singh, Vijay P.; Sharma, Nayan; C. Shekhar; P. Ojha (2004). Brahmaputra Basin Water Resources. Spring. 113. ISBN 978-1-4020-1737- 7. Retrieved November 15, 2015. ^ Gupta, Avijit (2008). Big Rivers: Geomorphology and Management. John Wiley & Son. 5–. Isbn 978-0-470-72371-5. Archived from the original on 6 August 2018. Retrieved 13 November 2016. Geography of India: Sacred and Historical Locations. Britannica Education Publishing. 2010.pp. 85–. ISBN 978-1-61530-202-4. Archived from the original on 6 August 2018. Retrieved 13 November 2016. ᘂ Suess, Eduard (1904). Earth's surface: (Das antlitz der erde). Clarendon press. pp. 50–. Retrieved November 15, 2015. ^ Barman, Swapnali; Bhattacharjya, R. K. (2015). Switch to snow cover area in Brahmaputra river bowl and its sensitivity to temperatures. Search System Settings. 4. Doi:10.1186/s40068-015-0043-0. 2000. Landuse Agriculture and Productivity Patterns in Lower Brahmaputra values (1970–71 and 1994–95). PhD Tez, Department of Geography, North East Hill University, Shillong. ^ Mipun, B.S. 1989. The impact of Migrants and Agricultural Changes in Lower Brahmaputra Valley: A case study in Darrang District. Unpublished PhD Tez, Department of Geography, North Hill University, Shillong. ^ Shrivastava, R.J.; Heinen, J.T. (2005). Migration and Home Field to the Brahmaputra Value, Assam, India. Journal of Ecological Anthropology. 9: 20–34. doi:10.5038/2162-4593.9.1.2. ^ Gilfellon, George; Sarma, Jogendra; Gohain, K. (August 2003). Dogs and Bed Morphology in part of the Brahmaputra River in Assam. Journal of the Geologic Society of India. 62. ^ Flood Monsoon 2004: Post Flood Needed Summary Report (PDF). Bangladeshi Disaster and Emergency Sub-Group (BDER) (Report). Dhaka, Bangladeshi. 2004. Archive (PDF) from the original on 21 March 2016. Retrieved 25 February 2016. ^ China operationalized the largest bam on Brahmaputra in Tibet. The Times of India. October 13, 2015. Archived from the original on 22 April 2016. Retrieved July 26, 2016. ^ A former company with modern geography: for use at Eton School by Aaron Arrowsmith, page 56^ e.g. Rennell, 1776; Rennel, 1787^ a b China admits to Project Brahmaputra. Economic times. April 22, 2010. Archived from the original on April 26, 2010. Retrieved April 22, 2010. ^ MacArthur Foundation, Asian Security Initiative Archives 27 July 2011 in The Wayback Machine ^ Chinese bam will not impact the flow of Brahmaputra: Krishna. The Indian Express on April 22, 2010. Archived from the original on April 25, 2010. Retrieved April 22, 2010. ^ BBC (20 March 2014). Megadams: Battle over Brahmaputra A. BBC News. Archived from the original on 2 March 2017. Retrieved 10 June 2017. ^ Yeophantong, Pichamon (2017). Activists of the Euphrates River, political entrepreneurship and transboundary water discussions in Asia. International Water. 42 (2): 163–186. doi:10.1080/02508060.2017.1279041. ^ New Nation, Bangladeshi, January 17, 2010. Archived from the original on 14 June 2011. Retrieved 22 January 2010. ᘂ a c d e e gtin Gadkari flag cutting cargo movement on Brahmaputra Archived January 2, 2018 at the Wayback Machinery, Economic Times, December 29, 2017. A c c d e g Fencing to be on by December: Sonowal^ Chaturvedi, Amit, ed. (14 July 2020). Centers provide approval in principle for tunnels below Brahmaputra's amid tension with China: report. Hindustan Times. Retrieved 3 September 2020. ^ Archived Copy (PDF). Archived (PDF) from the original on 16 May 2018. Retrieved December 29, 2017.CS1 main: Archive copy as title (link) ^ Press Office Information. www.pib.nic.in government of India. Archived from the original on April 26, 2017. Retrieved 30 January 2017. Citation Rahaman, M. M.; Veins, O. (2009). Integrating Water Management into The Basin of Brahmaputra: Perspective and Hope for Regional Development. Natural Resources Forum. 33 (1): 60–75. doi:10.1111/j.1477-8947.2009.01209.x. Sarma, JN (2005). The process of Fluvial and Morphology in the Brahmaputra River in Assam, India. Geomorphology. 70 (3–4): 226–256. Bibcode: 2005Geomo.. 70..226S. Doi:10.1016/j.geomorph.2005.02.007. Ribhaba Bharali. Brahmaputra River Restoration Project. Published in Pratidin Assamese, Amar Assam in October 2012. Further reading Bibliography on Water Resources and International Law. Peace Palace River Library in Dhemaji and Dhakuakhana Background in Brahmaputra's Flood Scenario the Powerful River Bramaputra in the Assam Brahmaputra, a detailed study of the river by renowned writer Arup Dutta. by National Book Trust, New Delhi, India) Emilie Crémin. Between mobility and sedaning living: People in the river, face the contents of the Brahmaputra (Assam, north-eastern India). Global Settings and Changes. University of Paris 8 Vincennes Saint-Denis, 2014. French. Wikimedia Commons external links have media related to Brahmaputra. Wikisource contains the text of encyclopedia of Britannica Brahmaputra Articles. Retrieved from

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