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Gyalmo Ngulchu : ウィキペディア英語版
Salween River

The Salween (, , also spelt Thanlwin; , ; , ''Gyalmo Ngulchu''; , literally "Angry River" in Chinese — the river is actually named after the Nu people living in the area, but Chinese having no phonetic script had to use a character with a similar sound as Nu which happens to be the character for rage; Thai , ''Mae Nam Salawin'' ((タイ語:แม่น้ำสาละวิน)); is a river, about long, that flows from the Tibetan Plateau into the Andaman Sea in Southeast Asia. It drains a narrow and mountainous watershed of that extends into the countries of China, Burma and Thailand. Steep canyon walls line the swift, powerful and undammed Salween, one of the longest free-flowing rivers in the world.〔 Its extensive drainage basin supports a biodiversity comparable with the Mekong and is home to about 7 million people. In 2003, key parts of the mid-region watershed of the river were included within the Three Parallel Rivers of Yunnan Protected Areas, a UNESCO World Heritage Site.〔
The people who live on the Salween are relatively isolated from the rest of the world. The river is only navigable up to from the mouth, and only in the rainy season.
The Burma Road was constructed between 1937 and 1938 during the Second Sino-Japanese War and crossed the river at the Huitong bridge. The Huitong bridge was blown by the retreating Chinese army and the river became the frontline from 1942 to 1944.
The Salween Campaign of World War II, was launched in order to liberate occupied China and open the Burma Road again and connect it to the Ledo Road.
Logging began on the mountains surrounding the Salween in the late 20th century, and has damaged the river's ecology. In recent years, there have been a number of proposals to dam the Salween river in China, prompting environmental concerns and wide opposition.〔 Construction of at least one dam on a tributary of the Salween is currently underway in China's Yunnan province, and more are expected to follow.
==Geography==

The Salween rises at in the Qinghai Mountains on the Tibetan Plateau, near the headwaters of the Mekong and Yangtze rivers. It initially flows west but then very shortly makes a great bend to the east, entering the Chinese province of Yunnan and the Three Parallel Rivers of Yunnan Protected Area, a World Heritage Site. Here, the Salween—called the Nu or Nujiang〔—has been proposed for a series of enormous dams that would theoretically generate more power than Three Gorges Dam, currently the world's largest hydroelectric station. It then makes a wide southward arc between the Tibetan and Yunnan-Guizhou Plateaus, dropping into what is often known as the "Grand Canyon of the East" or "China's Grand Canyon",〔 a -deep gorge that takes it past the Chinese border into northeastern Burma through Shan State and Kayah State,
A sharp bend west and another south takes the Salween between the great mountain ranges of eastern Burma, the Daen Lao Range, a subrange of the Shan Hills, followed by the Dawna Hills in the east and the Karen Hills in the west,〔(Burma -Geography )〕 the river then receives the Pai River also from the left and flows through Salawin National Park to join the Moei River from the east as it approaches Thailand, where it is called the ''Salawin'', forming the Burma-Thailand boundary for about , before re-entering Burma, passing through Karen State and Mon State.〔 The river finally breaks out of its gorge about from the mouth, and slows down dramatically as it courses through a series of agricultural valleys. About from the mouth the river finally widens and deepens enough to become navigable for large watercraft. In quick succession it receives Dontham River from the right and Gyaing River from the left, from where the river turns west, flowing under Thanlwin Bridge and widening into a small river delta at Mawlamyaing (formerly Moulmein). This region is the most heavily developed on the river and contains most of the basin's population.
Near the mouth the river has an average annual discharge of , although this varies widely. The river's base flow is provided by Tibetan glaciers, although it swells dramatically by the time it reaches the lowlands near the coast, especially in monsoon season.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Salween River」の詳細全文を読む



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