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Cona , also Cuona Lake or Tsonag Lake ( simplified Chinese : 错那湖 ; traditional Chinese : 錯那湖 ; pinyin : Cuònà Hú ), is a major lake of northern Tibet Autonomous Region , China. It is located in Amdo County , Nagqu , west of the road between Nagqu Town and Pana Town . The lake is considered holy to the Tibetans especially in the Bon religion, as it is seen as the "soul lake" of the Razheng Living Buddha. The smaller Ganong Lake lies almost adjacent to the southeast.

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132-581: Its area is approximately 300 square kilometres (120 sq mi), and it is at 4,594 metres (15,072 ft) above sea level making it one of the world's higher freshwater lakes. The lake is the source of the Gyalmo Nagqu, the headwater of the Salween River . Tsonag Lake can be observed on the right (west) as the train passes Cuonahu railway station on Qingzang Railway , going south toward Lhasa . This Nagqu Prefecture , Tibet location article

264-701: A 2010 peace agreement signed between ethnic militias and the Myanmar Union Government, commercial logging was able to increase dramatically in Karenni State. The Burmese government has banned the cutting of teak, but illegal logging for teak has persisted, driven by strong demand abroad. On the Thai side of the river, illegal logging has been ongoing since the 1990s in Salawin National Park. In Karen State, limestone quarrying for cement production along

396-806: A 50-foot granite pyramidal obelisk was erected in Xintan, on the site of Captain Plant's home, in a Chinese community of pilots and junk owners. One face of the monument is inscribed in Chinese and another in English. Though recently relocated to higher ground ahead of the Three Gorges Dam, the monument still stands overlooking the Upper Yangtze River near Yichang, a rare collective tribute to a westerner in China. Standard Oil ran

528-434: A diversity of habitats for freshwater, brackish and marine fishes. Subsistence fishing is predominant along the inland channels and bays, while a large commercial fishery is supported offshore. The most important commercial species include Nga pone na ( Paradise threadfin ) and Nga pyat (Coitor croaker). Prawns and shrimps are important in the local diet. Villages further upstream also depend on Salween fish, with Inle Lake being

660-716: A large fleet of warships appeared on the China coast, and with the first cannonball fired at a British ship, the Royal Saxon , the British started the first of the Opium Wars . Royal Navy warships destroyed numerous shore batteries and Chinese warships, laying waste to several coastal forts along the way. Eventually, they pushed their way up north close enough to threaten the Imperial Palace in Beijing itself. The China Navigation Company

792-716: A launching point for several invasions of Siam, which led to the collapse of the Ayutthaya Kingdom. The Burmese were unable to maintain lasting control over territories east of the river, although Burma regained the Tenasserim coast from Siam in a 1793 treaty. After the First Anglo-Burmese War in 1824, the Konbaung dynasty ceded coastal areas of Burma to the British Empire , including the whole Tenasserim coast south of

924-540: A major role in the history , culture , and economy of China . For thousands of years, the river has been used for water, irrigation, sanitation, transportation, industry, boundary-marking, and war. The Yangtze Delta generates as much as 20% of China's GDP , and the Three Gorges Dam on the Yangtze is the largest hydro-electric power station in the world that is in use . In mid-2014, the Chinese government announced it

1056-428: A particularly rich fishery. Overfishing combined with lack of regulation has become an issue in the 21st century, with catches in the lower Salween declining as much as 60 percent at some villages. The use of large "bag nets" that result in excessive bycatch , as well as the use of illegal poisons by commercial fishermen, have also contributed to the decline. Increased sedimentation from upstream logging has made

1188-774: A productive rice industry. The river flows for a further 100 km (62 mi) before terminating at a modestly sized delta and estuary in Mawlamyine in Mon State . The Salween is tidally influenced up to 75 km (47 mi) inland. Here it is joined by the Gyaing River from the east and the Ataran river from the southeast. The Thanlwin Bridge , the second longest bridge in Burma, connects Mawlamyine to Mottama . The combined river then breaks into

1320-614: A significant floral and faunal barrier as well as a rain shadow , and has been regarded as a major driver of plant speciation in the region. Around the Burma–China border, the Salween flows through the Northern Indochina subtropical forests ecoregion, which consists largely of subtropical broad-leaved evergreen forests, with pine forests at higher elevations and tropical forests at the lower margins. Further south in Burma and Thailand,

1452-420: A swimming craze through party propaganda. In 2002, Danish adventurer and sailor Troels Kløvedal sailed up the Yangtze, from Shanghai to past the Three Gorges Dam, in the collectively owned "Nordkaperen" sailing ship . Kløvedal had spent 12 years preparing and gathering the required permissions, and with a crew of Danes, his family members, a Chinese interpreter and several local maritime pilots , he became

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1584-581: Is a stub . You can help Misplaced Pages by expanding it . Salween River The Salween is a Southeast Asian river, about 3,289 km (2,044 mi) long, flowing from the Tibetan Plateau south into the Andaman Sea . The Salween flows primarily within southwest China and eastern Myanmar (Burma), with a short section forming the border of Burma and Thailand . Throughout most of its course, it runs swiftly through rugged mountain canyons. Despite

1716-529: Is an anglicisation of the Burmese name dating from 19th-century British maps. Due to its great range of elevation and latitude coupled with geographic isolation, the Salween basin is considered one of the most ecologically diverse regions in the world, containing an estimated 25 percent of the world's terrestrial animal species and thousands of plant species . Along its course the Salween provides water for agriculture and supports abundant fisheries, especially in

1848-470: Is delivered to the ocean during the monsoon season. The Salween delta is physically contiguous with the Irrawaddy and Sittaung deltas. The Irrawaddy–Sittaung–Salween delta is relatively stable, with the coastline advancing an average of 3.4 m (11 ft) per year between 1925 and 2006. Sediment accumulation is largely balanced out by subsidence and transport by ocean currents. However, proposed dams along

1980-518: Is found at 33°25′44″N 91°10′57″E  /  33.42889°N 91.18250°E  / 33.42889; 91.18250 and while not the furthest source of the Yangtze, it is the highest source at 5,342 m (17,526 ft) above sea level. The true source of the Yangtze, hydrologically the longest river distance from the sea, is at Jari Hill at the head of the Dam Qu tributary, approximately 325 km (202 mi) southeast of Geladandong. This source

2112-554: Is from the Sanskrit root gáṅgā . By the Han dynasty , Jiāng had come to mean any river in Chinese, and this river was distinguished as the "Great River" 大江 ( Dàjiāng ). The epithet 長 ( simplified version 长 ), meaning "long", was first formally applied to the river during the Six Dynasties period. Various sections of the Yangtze have local names. From Yibin to Yichang ,

2244-513: Is irrigated with surface water, and the rest with groundwater . Total water withdrawals amount to less than 3 percent of the river flow at 5.1 km (4,100,000 acre⋅ft). In recent years rubber, sugarcane and corn have become major cash crops, with the majority of this production exported to China. From 1998 to 2010, the area cultivated for rubber in Mon State increased fivefold, accompanied by significant deforestation. Further upstream,

2376-567: Is joined by the Ka, Suo and Ga rivers, all flowing from the southern slope of the Tanggula Mountains. In Biru County , the river begins a series of turns south and southeast, passing through Nyingchi prefecture. Shortly before entering Yunnan , it is joined from the east by the Yu River, its longest tributary within China. The Tibetan portion of the Salween basin is lightly populated, especially in

2508-583: Is only a homophone , due to Chinese having no phonetic script.) For more than 1,000 km (620 mi) the Salween runs parallel to, and west of the headwaters of the Mekong and Yangtze , separated by high mountain ridges of the Hengduan Mountains . The Gaoligong Mountains west of the Salween form the border between China and Burma. Between the Salween and Mekong rivers around the Tibet–Yunnan boundary are

2640-569: Is the first city on the Yangtze Plain . After entering Hubei province, the Yangtze receives water from a number of lakes. The largest of these lakes is Dongting Lake , which is located on the border of Hunan and Hubei provinces, and is the outlet for most of the rivers in Hunan. At Wuhan , it receives its biggest tributary, the Han River , bringing water from its northern basin as far as Shaanxi . At

2772-471: Is transported via waterways during the rainy season. In China, some forests in western Yunnan were intensively logged until the 1990s, when logging was banned there due to environmental impacts. The rate of deforestation has increased sharply in the 21st century, particularly in Shan, Karenni and Karen states. Before 2010, armed conflicts made it difficult for logging companies to access many of these areas. After

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2904-499: The Beijing dialect instead of Nanjing's and first published in 1867. The spellings Yangtze and Yangtze Kiang was a compromise between the two methods adopted at the 1906 Imperial Postal Conference in Shanghai, which established postal romanization . Hanyu Pinyin was adopted by the PRC's First Congress in 1958, but it was not widely employed in English outside mainland China prior to

3036-583: The Han dynasty , the region of the Yangtze River grew ever more important to China's economy. The establishment of irrigation systems (the most famous one is Dujiangyan , northwest of Chengdu, built during the Warring States period) made agriculture very stable and productive, eventually exceeding even the Yellow River region. The Qin and Han empires were actively engaged in the agricultural colonization of

3168-607: The Irrawaddy and Brahmaputra river systems on the west and the Mekong system on the east, and sharing a shorter boundary with the Yangtze system to the north. With a mean elevation of 3,515 m (11,532 ft), the Salween basin includes numerous glaciated mountain ranges, and the river flows for much of its length at high elevation. In China, the Salween basin is situated in Tibet Autonomous Region and Yunnan . In Burma

3300-703: The Jiangnan region south of the river ( Wuxi , Suzhou , Hangzhou ) and with northern China (all the way from Yangzhou to Beijing). The less well known ancient Lingqu Canal , connecting the upper Xiang River with the headwaters of the Guijiang , allowed a direct water connection from the Yangtze Basin to the Pearl River Delta . Historically, the Yangtze was the political boundary between north China and south China several times (see History of China ) because crossing

3432-553: The Longshan peoples of the North China Plain . What is now thought of as Chinese culture developed along the more fertile Yellow River basin; the " Yue " people of the lower Yangtze possessed very different traditions – blackening their teeth , cutting their hair short , tattooing their bodies, and living in small settlements among bamboo groves – and were considered barbarous by the northerners. The Central Yangtze valley

3564-619: The Meili Xue Shan , which include Kawagarbo , the highest peak in the Salween basin at 6,740 m (22,110 ft). Much of the river within Yunnan is part of the Three Parallel Rivers of Yunnan Protected Areas , a World Heritage Site . Forming canyons up to 4,500 m (14,800 ft) deep, this section is often called the "Grand Canyon of the East". Continuing south, the river crosses

3696-508: The Nanding River and Hka River from the east, and the Pang , Teng , and Pawn Rivers from the west. The Pang River is noted for its extensive limestone formations near the confluence with the Salween, where it breaks into a myriad of cataracts, channels and islets known as Kun Heng , "Thousand Islands". Inle Lake , the second largest lake in Burma and a World Biosphere Reserve , drains into

3828-503: The Shandong peninsula within the historical record, the Yangtze has remained largely static. Based on studies of sedimentation rates , however, it is unlikely that the present discharge site predates the late Miocene ( c.  11 Ma ). Prior to this, its headwaters drained south into the Gulf of Tonkin along or near the course of the present Red River . The Yangtze River is important to

3960-547: The Spring and Autumn period 's Five Hegemons and one of the Warring States ' Four Lords . They fell in against themselves, however. Chu's growing power led its rival Jin to support Wu as a counter. Wu successfully sacked Chu's capital Ying in 506 BC, but Chu subsequently supported Yue in its attacks against Wu's southern flank. In 473 BC, King Goujian of Yue fully annexed Wu and moved his court to its eponymous capital at modern Suzhou. In 333 BC, Chu finally united

4092-618: The Sunda pangolin . Limestone caves along the Salween in Thailand are home to numerous bat species, including the endemic Kitti's hog-nosed bat , the smallest known bat species in the world. The Nam San Valley along the Shan reach of the river provides habitat for the critically endangered white-rumped vulture and the slender-billed vulture . In the Salween delta, wetlands provide habitat for fishing cat , Asian small-clawed otter and Siamese crocodile , among other species. Along its lower course

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4224-541: The Three Parallel Rivers of Yunnan Protected Areas , a UNESCO World Heritage Site . Cháng Jiāng ( 长江 ; 長江 ) or " Long River " is the official name for the Yangtze in Mandarin Chinese . However, the Chinese have given different names to the upstream sections of the river up to its confluence with the Min River at Yibin , Sichuan. Jinsha River ("Gold Sands River") refers to the 2,308 km (1,434 mi) of

4356-408: The Yangtze sturgeon , which is extinct in the wild . In recent years, the river has suffered from industrial pollution, plastic pollution , agricultural runoff , siltation , and loss of wetland and lakes, which exacerbates seasonal flooding. Some sections of the river are now protected as nature reserves . A stretch of the upstream Yangtze flowing through deep gorges in western Yunnan is part of

4488-622: The Yellow River 's principal ports between the floods of 1344 and the 1850s, during which time the Yellow River ran well south of Shandong and discharged into the ocean a mere few hundred kilometers from the mouth of the Yangtze. ) By 1800, English cartographers such as Aaron Arrowsmith had adopted the French style of the name as Yang-tse or Yang-tse Kiang . The British diplomat Thomas Wade emended this to Yang-tzu Chiang as part of his formerly popular romanization of Chinese , based on

4620-618: The Yunnan-Guizhou Plateau via a series of deep canyons broken by wider valleys. In Longling County it is joined by the Kuke River and turns west, entering Burma. The total length of the river in China is 1,948 km (1,210 mi), not including a short 25 km (16 mi) segment along the China–Burma border. By the time it leaves China the Salween has descended more than 4,000 m (13,000 ft) from its source. In Burma

4752-613: The third-longest in the world. It rises at Jari Hill in the Tanggula Mountains of the Tibetan Plateau and flows 6,300 km (3,915 mi) in a generally easterly direction to the East China Sea . It is the fifth-largest primary river by discharge volume in the world . Its drainage basin comprises one-fifth of the land area of China , and is home to nearly one-third of the country's population . The Yangtze has played

4884-626: The "Yangzi River", from which the English name Yangtze is derived, is the local name for the Lower Yangtze in the region of Yangzhou . The name likely comes from an ancient ferry crossing called Yángzǐ or Yángzǐjīn ( 揚子 / 揚子津 ). Europeans who arrived in the Yangtze River Delta region applied this local name to the whole river. The dividing site between upstream and midstream is considered to be at Yichang and that between midstream and downstream at Hukou ( Jiujiang ). The river

5016-525: The 1060s King Anawrahta expanded the boundaries of the Pagan Kingdom (First Burmese Empire) from its origins in the Irrawaddy valley, conquering Thaton and the other Mon kingdoms in the Salween delta. In the late 1100s King Narapatisithu (Sithu II) conquered most of the Shan States, extending Burmese rule to the western bank of the Salween river from the delta as far north as Yunnan. For almost 500 years,

5148-458: The 1890s. Contemporary British maps labeled the river as "Salween", an anglicization of the Burmese name Thanlwin . Yangtze Yangtze or Yangzi ( English: / ˈ j æ ŋ t s i / or / ˈ j ɑː ŋ t s i / simplified Chinese : 长江 ; traditional Chinese : 長江 ; pinyin : Cháng Jiāng ; lit. 'long river') is the longest river in Eurasia and

5280-557: The 9th century BC. Traditional accounts credit these changes to northern refugees ( Taibo and Zhongyong in Wu and Wuyi in Yue) who assumed power over the local tribes, though these are generally assumed to be myths invented to legitimate them to other Zhou rulers. As the kingdoms of Wu and Yue , they were famed as fishers, shipwrights, and sword-smiths. Adopting Chinese characters , political institutions, and military technology, they were among

5412-507: The Burma–Thailand border south of this point. In Karen State, the river flows through karst limestone hills where numerous caves and unusual rock formations line the banks, particularly around the city of Hpa-An . The Salween emerges from the mountains into the coastal plain near Hlaingbwe Township . Near the coast, annual rainfall is as high as 4,000 to 5,000 mm (160 to 200 in), supporting dense tropical rainforest as well as

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5544-475: The Burmese military and local ethnic militias. The Salween is one of the least fragmented large river systems in Asia, with only a few small dams in the headwaters of the river and on tributaries. The river has extremely high hydropower potential, with a fall of more than 5,000 m (16,000 ft) from its source. Since the 1970s, the Burmese and Thai governments have sought to build massive hydroelectric dams along

5676-600: The Chinese government to make the river safer in 1917 by removing some of the most difficult obstacles and threats with explosives. In August 1917, British Asiatic Petroleum became the first foreign merchant steamship on the Upper Yangtze. Commercial firms, Robert Dollar Company, Jardine Matheson , Butterfield and Swire and Standard Oil added their own steamers on the river between 1917 and 1919. Between 1918 and 1919, Sichuan warlord violence and escalating civil war put Sichuan Steam Navigational Company out of business. Shutung

5808-499: The Chinese term for the mouth of the Yangtze ( 江口 , p   Jiāngkǒu ) as the name of the river itself. The name Blue River began to be applied in the 18th century, apparently owing to a former name of the Dam Chu or Min and to analogy with the Yellow River , but it was frequently explained in early English references as a 'translation' of Jiang , Jiangkou , or Yangzijiang . Very common in 18th- and 19th-century sources,

5940-597: The Dayebauk (north) and Mawlamyine (south) channels, forming Bilugyun Island before emptying into the Gulf of Martaban . Major tributaries by average flow (1971–2000): Flow regime at Hpa-an Station of Thanlwin River: Monthly flow pattern Thanlwin river at Hpa-an during 2009 to 2013: The present course of the Salween began to form about 5 million years ago as the Indian subcontinent collided with Asia, resulting in

6072-434: The Female Yak "; transliterated into Chinese : 直曲 ; pinyin : Zhíqū ). The river originates from several tributaries in the eastern part of the Tibetan Plateau , two of which are commonly referred to as the "source." Traditionally, the Chinese government has recognized the source as the Tuotuo tributary at the base of a glacier lying on the west of Geladandong Mountain in the Tanggula Mountains . This source

6204-450: The Nu River in western Yunnan, span elevations of 1,000 to 6,000 m (3,300 to 19,700 ft) and range from subtropical broadleaf evergreen to subalpine conifer forests. The rare Taiwania , one of the largest conifers in Asia, is found here along with more than twenty other conifer species. Due to its rugged and inaccessible terrain, this is considered one of the most intact large forest regions in China. The Mekong–Salween divide forms

6336-424: The Salween River. Due to its strategic location, Mawlamyine (anglicized as Moulmein) served as the capital of British Burma from 1826 until 1852 and as a gateway for overland trade into Yunnan. It became the center of a lucrative timber industry, particularly in teak . Logs were floated down the Salween River to meet oceangoing ships in Mawlamyine port. Forests in the lower Salween basin were extensively logged until

6468-412: The Salween are prime sources of tropical hardwoods including teak, pyinkadoe (red ironwood) and padauk (Burmese rosewood). Logging in the Burmese part of the basin first occurred on a large scale during the British colonial period in the 19th century. Clearcutting has destabilized soils along the river and raised sediment loads. Due to the lack of good roads across most of the basin, the majority of timber

6600-426: The Salween as more Han people settled in Yunnan. Martaban (now Mottama ) in the Salween Delta was a major trading port on the Maritime Silk Road as early as 200 BCE. By the 6th century CE, the Thaton Kingdom (one of the early Mon kingdoms ) ruled the Salween Delta and surrounding coasts from the capital of Thaton . From 738–902 CE, the kingdom of Nanzhao controlled Yunnan and parts of northern Burma, with

6732-516: The Salween basin includes the Kayah-Karen montane rain forests , where the karst limestone landscape of cliffs, sinkholes and caverns lends itself to a multitude of forest types. Limestone soils host drought deciduous forests, while dipterocarp –dominant tropical forests occur on granitic soils. Montane deciduous forests are widespread in the Shan Hills. Mangrove forests occur in the Salween delta, especially on Bilugyun Island. The basin supports about 151 fish species, with 77 of those found in

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6864-408: The Salween basin on both sides of the China–Burma border, migrated south along the river from Tibet around 500–300 BCE. The Lisu people , also originating in Tibet, arrived in Yunnan sometime before 1000 CE. Chinese records begin to mention Lisu in the late Tang dynasty (618–907 CE). The Lisu originally inhabited areas further east in Yunnan, but over centuries they were pushed north and west towards

6996-442: The Salween by way of the Pawn River. Further south, the river enters Karen State (Kayin State) and forms the border between Burma and Thailand for about 120 km (75 mi). In Thailand the river is known as Salawin ; much of the Thai side of the border is part of Salawin National Park and the Salawin Wildlife Sanctuary . At the south end of the border section it is joined by the northwest-flowing Moei River , which forms

7128-428: The Salween flows south and descends in elevation, it travels from temperate to subtropical and finally tropical climate zones, with yearly precipitation ranging from 1,200 to 2,000 mm (47 to 79 in) in the Shan Hills area. The total length of the river in Burma and Thailand is 1,316 km (818 mi). In Shan State and Karenni State (Kayah State) the river is joined by several large tributaries, including

7260-464: The Salween flows through Shan State , Karenni State , Karen State and Mon State . In Thailand the Salween borders only on Mae Hong Son Province , with tributaries extending into Chiang Mai , Tak and Kanchanaburi Province . The average flow rate at the China–Burma border is 68.74 km /a (2,178 m /s). Along the Burma–Thailand border the Salween carries an average annual flow of 200 km /a (6,300 m /s). The estimated flow rate at

7392-441: The Salween forming its southwestern boundary with the Burmese Pyu city-states . Tang China had several overland trade routes with Burma via Nanzhao, which it was allied with at times. One route started from Yinsheng (around present-day Jingdong , Yunnan) and headed west then south along the Salween River, reaching the Indian Ocean at Martaban. Another crossed the Salween around present day Baoshan , heading west towards India. In

7524-435: The Salween in and around Nujiang Prefecture . Although China had been expanding into the area since Ming times, the greatest influx of settlers was around 1700 to 1850. At the same time, Tibet was expanding its influence into western Yunnan. Tibetan parties raided down the Salween valley and took slaves from the indigenous Nu and Derung populations, which were not well politically organized and unable to offer much resistance. On

7656-411: The Salween in eastern Burma are home to dozens of medicinal plants crucial to the production of traditional herbal medicines. Some medicinal plants are cultivated, while others are harvested wild in the forest. Many wild species are threatened by deforestation and agricultural conversion. The Salween estuary and delta is a particularly rich fishery, with the complex network of tidal channels providing

7788-439: The Salween river is officially known as Thanlwin ; in Shan State , which the river enters immediately upon leaving China, it is also known as Nam Khone . Turning south, the river slices a winding course through the vast upland region known as the Shan Hills . This area is characterized by a complex, broken topography of small mountain ranges, plateaus and cliffs, through which the Salween has cut an extensive series of gorges. As

7920-429: The Salween river. Subsequently, Bayinnaung moved north up the Salween, subjugating all the independent Shan states by 1557. These victories were enabled in part by the acquisition of firearms from Dutch and Portuguese traders who first reached these coasts around 1511. European mercenaries also fought in some of these battles. At Martaban the Portuguese established a trading post, one of the first European settlements in

8052-483: The Salween sustains both flood and irrigated agriculture. The Salween delta is a major rice-growing area; it is the single most productive agricultural region in the Salween basin and home to over 500,000 people. Rice paddies are highly dependent on the river's annual flooding, bringing deposits of rich sediment. Other crops grown in the Salween basin include maize, wheat, chili, cotton, potatoes, groundnut, sesame, pulses, betel, tea, and various vegetables. Certain areas of

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8184-530: The Salween would trap much of the sediment with potential detrimental impacts to coastal erosion. The Salween basin is home to thousands of species of plants, with the highest plant diversity found in Yunnan's Three Parallel Rivers region. The Three Parallel Rivers protected areas include the Gaoligongshan National Nature Reserve and the Nu Jiang Reserve within the Salween basin; the Gaoligongshan reserve has more than 4,300 plant species. The Nujiang Langcang Gorge alpine conifer and mixed forests , situated along

8316-490: The Tibetan Plateau and northwest China starting around 1000 BCE. Tai peoples , ancestors of the Shan , began moving into the Shan Hills area of the middle Salween from Yunnan around 1000 CE and established multiple independent kingdoms, often known as the Shan States . The Nu people , originating in the Tibetan Plateau, may have inhabited the areas of the Salween (Nu) and Mekong (Lancang) in modern day China as early as 2000 BCE. The Wa people , who today inhabit parts of

8448-487: The Upper Yangtze on Leechuan at the end of 1898. With Plant's design input, Little had SS Pioneer built with Plant in command. In June 1900, Plant was the first to successfully pilot a merchant steamer on the Upper Yangtze from Yichang to Chongqing. Pioneer was sold to Royal Navy after its first run due to threat from the Boxer Rebellion and renamed HMS Kinsha . Germany's steamship effort that same year on SS Suixing ended in catastrophe. On Suixing's maiden voyage,

8580-458: The Yangtze River refers to the section from Yibin to Yichang; the middle part refers to the section from Yichang to Hukou County , where Lake Poyang meets the river; the downstream part is from Hukou to Shanghai. The origin of the Yangtze River has been dated by some geologists to about 45 million years ago in the Eocene , but this dating has been disputed. Although the mouth of the Yellow River has fluctuated widely north and south of

8712-411: The Yangtze from Yibin upstream to the confluence with the Batang River near Yushu in Qinghai, while the Tongtian River ("River that leads to Heaven") describes the 813 km (505 mi) section from Yushu up to the confluence of the Tuotuo River and the Dangqu River . In Old Chinese , the Yangtze was simply called Jiang/Kiang 江 , a character of phono-semantic compound origin, combining

8844-415: The Yangtze lowlands, maintaining a system of dikes to protect farmland from seasonal floods. By the Song dynasty, the area along the Yangtze had become among the wealthiest and most developed parts of the country, especially in the lower reaches of the river. Early in the Qing dynasty, the region called Jiangnan (that includes the southern part of Jiangsu , the northern part of Zhejiang and Jiangxi , and

8976-426: The ancestral Red into different drainage systems, with the Yangtze heading east towards the Pacific, and the Mekong and Salween flowing south into what is now Thailand's Chao Phraya River . About 1.5 million years ago, volcanic activity diverted the Salween west towards the Andaman Sea, roughly creating the modern path of the river. The parallel modern courses of the upper Salween, Mekong and Yangtze are located where

9108-433: The area. In the 1640s, the last years of the Ming dynasty, geographer Xu Xiake explored the Salween River country and determined that the upper Salween, Mekong and Red rivers (previously believed to be part of the same river system) were in fact separate. After the rise of the Qing dynasty China entered a new period of western expansion. In 1717 the Dzungar Khanate conquered Tibet, and China sought to expel them from

9240-423: The cultural origins of southern China and Japan. Human activity has been verified in the Three Gorges area as far back as 27,000 years ago, and by the 5th millennium BC, the lower Yangtze was a major population center occupied by the Hemudu and Majiabang cultures , both among the earliest cultivators of rice. By the 3rd millennium BC, the successor Liangzhu culture showed evidence of influence from

9372-549: The deadliest natural disasters ever recorded, and almost certainly the deadliest of the 20th century (when pandemics and famines are discounted). Estimates of the total death toll range from 145,000 to between 3.7 million and 4 million. The Yangtze flooded again in 1935 , causing great loss of life. From June to September 1954, the Yangtze River Floods were a series of catastrophic floodings that occurred mostly in Hubei Province. Due to unusually high volume of precipitation as well as an extraordinarily long rainy season in

9504-517: The delta region. The Salween basin is home to numerous ethnic minority groups, whose ancestors largely originated in the Tibetan Plateau and northwest China. Starting about 5,000 years ago, people began migrating south along the river, establishing small kingdoms and city-states . During the last 1,000 years, the Salween has defined various frontiers of the Burmese empires to the west, the Kingdom of Siam to

9636-454: The eastern Tibetan Plateau intersects the uplands of the Yunnan-Guizhou Plateau . The mountain ranges separating these rivers are individual terranes (crustal fragments) that accreted separately to the Asian continent – forming a basin and range landscape with drainage running from north to south – then compressed together such that the rivers flow only 20 km (12 mi) apart in places. As

9768-487: The estuary shallower and reduced its productivity, in turn reducing the rate of fish migration and spawning. The Burmese government has made efforts to address the issues, including seasonal fishing bans first implemented in 2012, but these laws have been rarely enforced. An alternative approach, using small, self-enforced community-based reserves where fishing is not allowed, has successfully protected fish populations and species diversity in northern Thailand. Forests along

9900-523: The first 2,600 km (1,600 mi) of its length, the river has fallen more than 5,200 m (17,100 ft). It enters the basin of Sichuan at Yibin . While in the Sichuan basin, it receives several large tributaries, increasing its water volume significantly. It then cuts through Mount Wushan bordering Chongqing and Hubei to create the famous Three Gorges . Eastward of the Three Gorges, Yichang

10032-475: The first foreigner since 1949 to navigate the Yangtze. His months-long journey was documented both in his 2004 book "Kineserne syr med lang tråd" and the TV show "Kløvedal i Kina" by DR . In August 2019, Welsh adventurer Ash Dykes became the first person to complete the 4,000-mile (6,400 km) trek along the course of the river, walking for 352 days from its source to its mouth. Tens of millions of people live in

10164-457: The floodplain are suitable for both farming and fishing, such as the seasonal Daw Lar Lake upstream of Hpa-An, where crops are grown on islands in the lake during the dry season. Following the annual harvest, the land is used for grazing livestock. In the rainy season fish migrate from the Salween River to spawn in the lake, and are caught in large numbers as the water level recedes at the end of

10296-489: The floodplain of the Yangtze valley, an area that naturally floods every summer and is habitable only because it is protected by river dikes. The floods large enough to overflow the dikes have caused great distress to those who live and farm there. Floods of note include those of 1931, 1954, and 1998. The 1931 Central China floods or the Central China floods of 1931 were a series of floods that are generally considered among

10428-474: The frigid headwater regions where precipitation is scarce and river flow depends almost entirely on glacier melt. The upper Salween basin includes more than 12,000 km (4,600 sq mi) of glaciers. In Yunnan, the Salween is known as the Nujiang ( Chinese : 怒江 ; pinyin : Nujiang ) or Nu River , after the indigenous Nu people , but also translating literally to "angry river". (The character

10560-587: The lake, the Tibetan section of the river is called Gyalmo Nagqu , "black river". In Tibet the river flows mostly within Nagqu prefecture. From Cona Lake, the river flows south and turns east near Nagqu Town , where the Chalong hydroelectric station is situated. Further east, the river is dammed at the smaller Jiquan hydroelectric station. As of 2017, these are the only two dams on the Salween River proper. Continuing east, it

10692-741: The lower Salween defined the frontier between Burma and the Ayutthaya Kingdom (Siam). In the late 1200s, the Pagan Kingdom collapsed after invasions of the Mongol Empire . The Mongols had also conquered the Dali Kingdom (Nanzhao's successor). In 1287 the Hanthawaddy Kingdom emerged in the Salween and Irrawaddy deltas. Martaban served as the Hanthawaddy capital between 1287 and 1364. Along

10824-519: The lower Yangtze by annexing Yue, whose royal family was said to have fled south and established the Minyue kingdom in Fujian . Qin was able to unite China by first subduing Ba and Shu on the upper Yangtze in modern Sichuan , giving them a strong base to attack Chu's settlements along the river. The state of Qin conquered the central Yangtze region, the previous heartland of Chu, in 278 BC, and incorporated

10956-568: The lowest population density is in Tibet (5 people/km ). The Salween originates in the Tanggula Mountains in the central Tibetan Plateau. The headwaters are located near Dengka Peak, east of Tanggula Pass . The highest source is Jiangmeiergang Galou glacier, 5,432 m (17,822 ft) above sea level. The various headwater streams flow southwest through high mountain valleys and accumulate in Cona Lake , at 4,594 m (15,072 ft). Downstream of

11088-549: The middle stretch of the Yangtze River late in the spring of 1954, the river started to rise above its usual level in around late June. Despite efforts to open three important flood gates to alleviate the rising water by diverting it, the flood level continued to rise until it hit the historic high of 44.67 m in Jingzhou, Hubei and 29.73 m in Wuhan. The number of dead from this flood was estimated at 33,000, including those who died of plague in

11220-442: The most powerful states during the later Zhou . In the middle Yangtze, the state of Jing seems to have begun in the upper Han River valley a minor Zhou polity, but it adapted to native culture as it expanded south and east into the Yangtze valley. In the process, it changed its name to Chu . Whether native or nativizing, the Yangtze states held their own against the northern Chinese homeland: some lists credit them with three of

11352-562: The most risky and deadly sections of the three gorges. Archibald John Little took an interest in Upper Yangtze navigation when in 1876, the Chefoo Convention opened Chongqing to consular residence but stipulated that foreign trade might only commence once steamships had succeeded in ascending the river to that point. Little formed the Upper Yangtze Steam Navigation Co., Ltd. and built Kuling but his attempts to take

11484-553: The mountainous middle reaches of the Salween River, former Shan vassal states regained their independence. Starting around 1380, Ming China annexed Yunnan and conquered some of the eastern Shan states. From 1436-49, Chinese armies crossed the Salween to wage the Luchuan–Pingmian campaigns against the Shan state of Mong Mao . These wars were an expensive failure for the Ming, and triggered tribal uprisings that fragmented Chinese power in

11616-548: The mountains continued to rise, the rivers incised into the landscape along parallel fault zones, creating the deep canyons of the present day. The Nujiang fault zone stretches over 600 km (370 mi) along the river in Yunnan. The formation of the Himalayas blocked drainage from the Tibetan Plateau south towards the Indian Ocean, forcing drainage north of the mountains east towards the Yangtze river. This east-flowing river,

11748-499: The mouth is 6,600 m /s (230,000 cu ft/s). About 89 percent of the annual flow occurs in the monsoon season (mid-May through November), and only 11 percent in the remainder of the year. The average volume of sediment in the Salween Delta is around 180 million tonnes per year. The population of the Salween basin is estimated at 24 million, or 76 persons/km . About 10 million people live adjacent or close to

11880-457: The name fell out of favor due to growing awareness of its lack of any connection to the river's Chinese names and to the irony of its application to such a muddy waterway. Matteo Ricci 's 1615 Latin account included descriptions of the "Ianſu" and "Ianſuchian." The posthumous account's translation of the name as Fils de la Mer ("Son of the Ocean") shows that Ricci, who by the end of his life

12012-423: The nearby Irrawaddy and Sittaung Rivers . The river also hosts a number of invasive exotic fish which were introduced for commercial purposes. In addition to fish, the Salween provides habitat for 92 amphibian species. The Salween has the greatest diversity of turtles of any river in the world. The endangered Giant Asian pond turtle and Big-headed turtle are found here. The Salween basin includes up to 25% of

12144-637: The normalization of diplomatic relations between the United States and the PRC in 1979; since that time, the spelling Yangzi has also been used. The source and upper reaches of the Yangtze are located in ethnic Tibetan areas of Qinghai . In Tibetan, the Tuotuo headwaters are the Machu ( Tibetan : རྨ་ཆུ་ , Wylie : rma-chu , lit. "Red Water"). The Tongtian is the Drichu ( འབྲི་ཆུ་ , ‘Bri Chu’), literally "Water of

12276-409: The northern tip of Jiangxi province, Lake Poyang , the biggest freshwater lake in China, merges into the river. The river then runs through Anhui and Jiangsu , receiving more water from innumerable smaller lakes and rivers, and finally reaches the East China Sea at Shanghai. Four of China's five main freshwater lakes contribute their waters to the Yangtze River. Traditionally, the upstream part of

12408-551: The other hand, the Lisu fiercely resisted efforts to take slaves and land. In the 1590s Siam had captured the Tenasserim coast, and the Salween delta again became the border with Burma. For more than a hundred years this remained a disputed area, changing hands several times between the Burmese and Siamese. Burmese rule returned to the Salween delta in the 1750s with the expansion of the Konbaung dynasty . Starting in 1759, Martaban served as

12540-616: The periods 1911–12, 1927–37, and 1945–49. The Jardine , the first steamship to sail the river, was built for Jardine, Matheson & Co. in 1835. This small vessel was to carry passengers and mail between Lintin Island , Macao , and Huangpu . However, the Chinese, draconian in their application of the rules relating to foreign vessels, were unhappy about a "fire-ship" steaming up the Canton River. The acting Viceroy of Liangguang issued an edict warning that she would be fired on if she attempted

12672-513: The predecessor of the modern Yarlung Tsangpo river, was repeatedly captured into drainages to the south, finding various routes to the sea via the Red, Mekong, Salween and Irrawaddy rivers. The combined Salween–Yarlung Tsangpo drainage would have been much longer than the modern Salween, stretching an additional 1,500 km (930 mi) west across the Tibetan Plateau. Ultimately the Yarlung Tsangpo

12804-516: The region into its expanding empire. Qin then used its connections along the Xiang River to expand into Hunan , Jiangxi and Guangdong , setting up military commanderies along the main lines of communication. At the collapse of the Qin Dynasty , these southern commanderies became the independent Nanyue Empire under Zhao Tuo while Chu and Han vied with each other for control of the north. Since

12936-472: The region. The Toungoo dynasty emerged in Burma during the 1500s, conquering much of Southeast Asia by 1565 to create the First Toungoo Empire (Second Burmese Empire). King Tabinshwehti captured and destroyed Martaban in 1541. Under the subsequent rule of Bayinnaung , an 800,000-strong army crossed the Salween in 1548 and invaded Siam. This was the first time Burmese rule had been extended east of

13068-591: The region. In 1718 the Qing sent an army but were unsuccessful in reaching Tibet, reaching only as far as the Salween River where they were defeated by Dzungar troops in the Battle of the Salween River . In response, the Qing sent a larger force to Tibet in 1720 , driving out the Dzungars and establishing Qing rule of Tibet . As the Qing pushed into Yunnan, the indigenous Lisu people were driven further west, eventually settling along

13200-455: The river bank in the southeastern Tibetan Plateau. The Mon are some of the earliest inhabitants of the Salween basin within Burma, migrating south from China around 3000 BCE, and settling in the Salween delta and adjacent coastal areas. Agriculture was first practiced in the Salween and Irrawaddy basins around the first century BCE. Ancestors of the Karen migrated down the Salween River area from

13332-465: The river has increased in the 21st century. There is also increasing sand and gravel mining in the lower river. As of 2015 the Burmese government was seeking international investment in the mining sector, and new policies could lead to considerable increase in mining activity along the river. Human presence along the upper Salween River dates to at least 31,000–39,000 years ago. Archeological evidence includes stone tools and animal remains discovered along

13464-463: The river proper. People of the Salween basin represent a large diversity of ethnic groups. In China, the Salween basin is home to Blang , Derung , Lisu , Nu , Palaung (De'ang), Shan , Tibetan and Wa . In Burma and Myanmar, the major ethnic groups include Akha , Lahu , Lisu, Hmong , Kachin , Karen , Karenni , Kokang , Pa'O , Shan and Yao . The highest population densities are in Mon State (300 people/km ) and Yunnan (100 people/km ), while

13596-466: The river provides a water source for numerous remote villages. With arable land limited by mountainous terrain, farming occurs primarily on the seasonally flooded river banks and islands. However, forest land has been increasingly converted to agriculture, which has led to sedimentation and other water quality issues. The higher elevation valleys are used for grazing, particularly in Tibet, where yaks, sheep, goats, horses and cattle are raised. Forests along

13728-580: The river through Sichuan and Chongqing Municipality is also known as the Chuān Jiāng ( 川江 ) or " Sichuan River ". In Hubei , the river is also called the Jīng Jiāng ( 荆江 ; 荊江 ) or the "Jing River" after Jingzhou , one of the Nine Provinces of ancient China. In Anhui , the river takes on the local name Wǎn Jiāng after the shorthand name for Anhui, wǎn (皖). Yángzǐ Jiāng ( 揚子江 ; 扬子江 ) or

13860-664: The river was difficult. This occurred notably during the Southern and Northern Dynasties , and the Southern Song . Many battles took place along the river, the most famous being the Battle of Red Cliffs in 208 AD during the Three Kingdoms period. The Yangtze was the site of naval battles between the Song dynasty and Jurchen Jin during the Jin–Song wars . In the Battle of Caishi of 1161,

13992-510: The river's great length, only the last 90 km (56 mi) are navigable, where it forms a modest estuary and delta at Mawlamyine . The river is known by various names along its course, including the Thanlwin (named after Elaeocarpus sp., an olive-like plant that grows on its banks ) in Burma and the Nu Jiang (or Nu River, named after Nu people ) in China. The commonly used spelling "Salween"

14124-488: The river. China also planned to dam the upper Salween, but in 2016 these plans were dropped in favor of establishing a national park. The future of dam projects in Myanmar and Thailand remains uncertain. The Salween basin includes about 283,500 km (109,500 sq mi), of which 48 percent is in China, 44 percent in Burma, and 8 percent in Thailand. The basin is extremely long and narrow, situated between

14256-691: The run and by 1915, foreign ships expressed their interest too. Plant was appointed by Chinese Maritime Customs Service as First Senior River Inspector in 1915. In this role, Plant installed navigational marks and established signaling systems. He also wrote Handbook for the Guidance of Shipmasters on the Ichang-Chungking Section of the Yangtze River , a detailed and illustrated account of the Upper Yangtze's currents, rocks, and other hazards with navigational instruction. Plant trained hundreds of Chinese and foreign pilots and issued licenses and worked with

14388-533: The season. The Salween generally floods in July–September and reaches its lowest around October–December. Compared to Burma's principal rice growing region, the Irrawaddy delta, the Salween delta floods more erratically, and is prone to drought for 1–2 years out of five. Approximately 380,000 ha (940,000 acres) of land are irrigated in the Salween basin, with 50 percent in Burma, 42 percent in China and 8 percent in Thailand. About 97 percent

14520-502: The ships of the Jin emperor Wanyan Liang clashed with the Song fleet on the Yangtze. Song soldiers fired bombs of lime and sulfur using trebuchets at the Jurchen warships. The battle was a Song victory that halted the invasion by the Jin. The Battle of Tangdao was another Yangtze naval battle in the same year. Politically, Nanjing was the capital of China several times, although most of

14652-470: The source of the Yangtze since the discovery of the Jari Hill source. These tributaries join and the river then runs eastward through Qinghai (Tsinghai), turning southward down a deep valley at the border of Sichuan (Szechwan) and Tibet to reach Yunnan . In the course of this valley, the river's elevation drops from above 5,000 m (16,000 ft) to less than 1,000 m (3,300 ft). Thus, over

14784-669: The south, and Imperial China to the east, with the Shan States along the middle Salween being a frequently contested area. In the 19th century, the British Empire invaded Burma with Mawlamyine serving as the colonial capital for many decades. Since Burmese independence in 1948, the Salween basin has been a battleground for several fronts of the Burmese Civil War , with large areas in Shan State and Karen State ( Kayin State ) contested between

14916-408: The southeastern part of Anhui ) provided 1 ⁄ 3 – 1 ⁄ 2 of the nation's revenues. The Yangtze has long been the backbone of China's inland water transportation system, which remained particularly important for almost two thousand years, until the construction of the national railway network during the 20th century. The Grand Canal connects the lower Yangtze with the major cities of

15048-536: The tankers Mei Ping, Mei An and Mei Hsia, which were collectively destroyed on December 12, 1937, when Japanese warplanes bombed and sank the U.S.S. Panay. One of the Standard Oil captains who survived this attack had served on the Upper River for 14 years. Chinese Communist Party chairman Mao Zedong took staged swims in the river in 1956 and 1966 at Wuhan in publicity stunts to demonstrate his health, also starting

15180-672: The time its territory only covered the southeastern part of China, such as the Wu kingdom in the Three Kingdoms period, the Eastern Jin Dynasty , and during the Southern and Northern Dynasties and Five Dynasties and Ten Kingdoms periods. Only the Ming occupied most parts of China from their capital at Nanjing , though it later moved the capital to Beijing. The ROC capital was located in Nanjing in

15312-623: The trip. On the Jardine's first trial run from Lintin Island the forts on both sides of the Bogue opened fire and she was forced to turn back. The Chinese authorities issued a further warning insisting that the ship leave Chinese waters. The Jardine in any case needed repairs and was sent to Singapore . Subsequently, Lord Palmerston , the Foreign Secretary decided mainly on the "suggestions" of William Jardine to declare war on China. In mid-1840,

15444-595: The uplift of the Himalaya mountains and the Tibetan Plateau. Prior to the Himalaya orogeny , what are now the upper Irrawaddy, Salween, Mekong and Yangtze rivers may have all flowed into the Red River , emptying into the South China Sea . The landscape was hilly but not particularly rugged, with average elevations of 1,000 m (3,300 ft) or less. As the continents converged, a complex jumble of mountains arose, breaking

15576-626: The upper Salween. The Salween has numerous cyprinid species, including the endangered Garra cryptonema and Akrokolioplax bicornis which are endemic to the basin. Inle Lake in Shan State, designated a UNESCO Biosphere Reserve in 2015, provides habitat for numerous endemic fish species. The Thousand Islands area at the Salween–Pang confluence, as well as the confluence of the Salween and Moei rivers, are also identified as critical fish habitat. The Salween shares most of its fish species with

15708-420: The vessel further upriver than Yichang were thwarted by the Chinese authorities who were concerned about the potential loss of transit duties, competition to their native junk trade and physical damage to their crafts caused by steamship wakes. Kuling was sold to China Merchants Steam Navigation Company for lower river service. In 1890, the Chinese government agreed to open Chongqing to foreign trade as long as it

15840-445: The vessel hit a rock and sunk, killing its captain and ending realistic hopes of regular commercial steam service on the Upper Yangtze. In 1908, local Sichuan merchants and their government partnered with Captain Plant to form Sichuan Steam Navigation Company becoming the first successful service between Yichang and Chongqing. Captain Plant designed and commanded its two ships, SS Shutung and SS Shuhun . Other Chinese vessels came onto

15972-706: The water radical 氵 with the homophone 工 (now pronounced gōng , but *kˤoŋ in Old Chinese ). Kong was probably a word in the Austroasiatic language of local peoples such as the Yue . Similar to *krong in Proto-Vietnamese and krung in Mon , all meaning "river", it is related to modern Vietnamese sông (river) and Khmer krung (city on riverside), whence Thai krung (กรุง capital city), not kôngkea (water) which

16104-592: The world's terrestrial animal species. About one-half of all animal species in China can be found in the upper Salween, which provides habitat for endangered species including the snow leopard and black snub-nosed monkey . The remote jungles of the Salween basin in Burma and Thailand, particularly in Kayin and Shan states, are home to dozens of large mammal species including the Indochinese tiger , clouded leopard , Asiatic black bear , sun bear , eastern hoolock gibbon , and

16236-475: Was an early shipping company founded in 1876 in London, initially to trade up the Yangtze River from their Shanghai base with passengers and cargo. Chinese coastal trade started shortly after, and in 1883 a regular service to Australia was initiated. Steamers came late to the upper river, the section stretching from Yichang to Chongqing. Freshets from Himalayan snowmelt created treacherous seasonal currents. But summer

16368-509: Was better navigationally and the three gorges , described as a "150-mile passage which is like the narrow throat of an hourglass," posed hazardous threats of crosscurrents, whirlpools and eddies, creating significant challenges to steamship efforts. Furthermore, Chongqing is 700 – 800 feet above sea level, requiring powerful engines to make the upriver climb. Junk travel accomplished the upriver feat by employing 70–80 trackers, men hitched to hawsers who physically pulled ships upriver through some of

16500-490: Was building a multi-tier transport network , comprising railways, roads and airports to create a new economic belt alongside the river. The Yangtze flows through a wide array of ecosystems and is habitat to several endemic and threatened species, including the Chinese alligator , the narrow-ridged finless porpoise , and also was the home of the now extinct Yangtze river dolphin (or baiji ) and Chinese paddlefish , as well as

16632-494: Was called Quian ( 江 ) and Quianshui ( 江水 ) by Marco Polo and appeared on the earliest English maps as Kian or Kiam , all recording dialects which preserved forms of the Middle Chinese pronunciation of 江 as Kæwng . By the mid-19th century, these romanizations had standardized as Kiang ; Dajiang , e.g., was rendered as "Ta-Kiang." "Keeang-Koo," "Kyang Kew," "Kian-ku," and related names derived from mistaking

16764-494: Was captured by the Brahmaputra River in present-day India. The Salween may once have had additional tributaries above its present source, but due to the uplift of the Himalaya blocking moisture from the Indian Ocean, these tributaries dried up, leaving the numerous terminal lakes scattered across Nagqu today. The Salween carries an estimated 108 to 237 million tonnes of sediment per year. About 92 percent of sediment

16896-568: Was commandeered by warlords and Shuhun was brought down river to Shanghai for safekeeping. In 1921, when Captain Plant died at sea while returning home to England, a Plant Memorial Fund was established to perpetuate Plant's name and contributions to Upper Yangtze navigation. The largest shipping companies in service, Butterfield & Swire, Jardine Matheson, Standard Oil, Mackenzie & Co., Asiatic Petroleum, Robert Dollar, China Merchants S.N. Co. and British-American Tobacco Co., contributed alongside international friends and Chinese pilots. In 1924,

17028-588: Was fluent in literary Chinese, was introduced to it as the homophonic 洋子江 rather than the usual 揚子江 . Further, although railroads and the Shanghai concessions subsequently turned it into a backwater, Yangzhou was the lower river's principal port for much of the Qing dynasty , directing Liangjiang 's important salt monopoly and connecting the Yangtze with the Grand Canal to Beijing. (That connection also made it one of

17160-611: Was home to sophisticated Neolithic cultures. Later it became the earliest part of the Yangtze valley to be integrated into the North Chinese cultural sphere. (Northern Chinese were active there since the Bronze Age ). In the lower Yangtze, two Yue tribes, the Gouwu in southern Jiangsu and the Yuyue in northern Zhejiang , display increasing Zhou (i.e., North Chinese) influence starting in

17292-421: Was only discovered in the late 20th century and lies in wetlands at 32°36′14″N 94°30′44″E  /  32.60389°N 94.51222°E  / 32.60389; 94.51222 and 5,170 m (16,960 ft) above sea level just southeast of Chadan Township in Zadoi County , Yushu Prefecture , Qinghai. As the historical spiritual source of the Yangtze, the Geladandong source is still commonly referred to as

17424-694: Was restricted to native crafts. In 1895, the Treaty of Shimonoseki provided a provision which opened Chongqing fully to foreign trade. Little took up residence in Chongqing and built Leechuan , to tackle the gorges in 1898. In March Leechuan completed the upriver journey to Chongqing but not without the assistance of trackers. Leechuan was not designed for cargo or passengers and if Little wanted to take his vision one step further, he required an expert pilot. In 1898, Little persuaded Captain Samuel Cornell Plant to come out to China to lend his expertise. Captain Plant had just completed navigation of Persia 's Upper Karun River and took up Little's offer to assess

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