History and controversy of the Three Gorges Dam

Also known as: The Sanxia

First discussed in the 1920s by Chinese Nationalist Party leaders, the idea for the Three Gorges Dam was given new impetus in 1953 when Chinese leader Mao Zedong ordered feasibility studies of a number of sites. Detailed planning for the project began in 1955. Its proponents insisted it would control disastrous flooding along the Yangtze, facilitate inland trade, and provide much-needed power for central China, but the dam was not without its detractors. Criticisms of the Three Gorges project began as soon as the plans were proposed and continued through its construction. Key problems included the danger of dam collapse, the displacement of some 1.3 million people (critics insisted the figure was actually 1.9 million) living in more than 1,500 cities, towns, and villages along the river, and the destruction of magnificent scenery and countless rare architectural and archaeological sites. There were also fears—some of which were borne out—that human and industrial waste from cities would pollute the reservoir and even that the huge amount of water impounded in the reservoir could trigger earthquakes and landslides. Some Chinese and foreign engineers argued that a number of smaller and far cheaper and less-problematic dams on the Yangtze tributaries could generate as much power as the Three Gorges Dam and control flooding equally well. Construction of those dams, they maintained, would enable the government to meet its main priorities without the risks.

Because of these problems, work on the Three Gorges Dam was delayed for nearly 40 years as the Chinese government struggled to reach a decision to carry through with plans for the project. In 1992 Premier Li Peng, who had himself trained as an engineer, was finally able to persuade the National People’s Congress to ratify the decision to build the dam, though almost a third of its members abstained or voted against the project—an unprecedented sign of resistance from a normally acquiescent body. Pres. Jiang Zemin did not accompany Li to the official inauguration of the dam in 1994, and the World Bank refused to advance China funds to help with the project, citing major environmental and other concerns.

Nevertheless, the Three Gorges project moved ahead. In 1993 work started on access roads and electricity to the site. Workers blocked and diverted the river in 1997, bringing to a close the first phase of construction. In 2003 the reservoir began to fill, the five-tier ship locks—which allowed vessels of up to 10,000 tons to navigate past the dam—were put into preliminary operation, and the first of the dam’s generators was connected to the grid, completing the second phase of construction. (Following completion of this second phase, some 1,200 sites of historical and archaeological importance that once lined the middle reaches of the Yangtze River vanished as floodwaters rose.) Construction of the main wall of the dam was completed in 2006. The remainder of the dam’s generators were operational by mid-2012, and a ship lift, which allowed vessels of up to 3,000 tons to bypass the five-tier ship locks and more quickly navigate past the dam, was completed in late 2015 and began officially operating in 2016.

The Editors of Encyclopaedia Britannica
This article was most recently revised and updated by Melissa Petruzzello.
Chinese (Pinyin):
Chang Jiang or
(Wade-Giles romanization):
Ch’ang Chiang
Top Questions

How long is the Yangtze River?

What is the source of the Yangtze River?

What are the principal tributaries of the Yangtze River?

What huge dam project was completed on the Yangtze River in 2006?

Yangtze River, longest river in both China and Asia and third longest river in the world, with a length of 3,915 miles (6,300 km). Its basin, extending for some 2,000 miles (3,200 km) from west to east and for more than 600 miles (1,000 km) from north to south, drains an area of 698,265 square miles (1,808,500 square km). From its source on the Plateau of Tibet to its mouth on the East China Sea, the river traverses or serves as the border between 10 provinces or regions. More than three-fourths of the river’s course runs through mountains. The Yangtze has eight principal tributaries. On its left bank, from source to mouth, these are the Yalung, Min, Jialing, and Han rivers; those on the right bank include the Wu, Yuan, Xiang, and Gan rivers.

The name Yangtze—derived from the name of the ancient fiefdom of Yang—has been applied to the river mainly by those in the West. Chang Jiang (“Long River”) is the name used in China, although it also is called Da Jiang (“Great River”) or, simply, Jiang (“[The] River”). The Yangtze is the most important river of China. It is the country’s principal waterway, and its basin is China’s great granary and contains nearly one-third of the national population.

Physical features

The upper course

The upper course of the Yangtze flows across the Plateau of Tibet and descends through deep valleys in the mountains east of the plateau, emerging onto the Yunnan-Guizhou (Yungui) Plateau. Summers there are warm, and the winters are cold. The source of the Yangtze is the Ulan Moron (Wulanmulun) River, which originates in glacial meltwaters on the slopes of the Tanggula Mountains in southern Qinghai province on the border with the Tibet Autonomous Region. From the confluence of this stream with several others, the river flows generally easterly through a shallow, spacious valley, the bottom of which is studded with lakes and small reservoirs. This part of its course lies in the higher regions of the Tibetan highlands.

The river’s character changes sharply upon reaching the eastern limits of the highlands. There the river—which in this stretch is called the Jinsha—descends from a high elevation, winding its way south of the high Bayan Har Mountains and forming a narrow valley up to 2 miles (3 km) in depth. Individual mountain peaks exceed elevations of 16,000 feet (4,900 metres) above sea level and are crowned with glaciers and perpetual snow. The steep, rocky slopes are cut with gorges and deep valleys. For several hundred miles the Yangtze flows in a southeasterly direction, before turning south to flow downward in rushing rapids. For a considerable distance the river flows through passes that are so steep that no room is left even for a narrow path. Villages, which are rarely found, are located high above the river. In this region the Yangtze runs close and parallel to both the Mekong and Salween rivers; all three rivers are within 15 to 30 miles (25 to 50 km) of one another and continue to flow in mutual proximity for a distance of more than 250 miles (400 km).

North of latitude 26° N these great rivers diverge, and the Yangtze turns east to pass through a winding valley with steep slopes. The river receives the waters of many tributaries, among which the Yalong River is the largest and contributes the most water. The Yangtze then widens to between 1,000 and 1,300 feet (300 and 400 metres), reaching depths often exceeding 30 feet (9 metres). In narrower gorges the water width decreases by almost half, but the depth increases sharply.

Tower Bridge over the Thames River in London, England. Opened in 1894. Remains an Important Traffic Route with 40,000 Crossings Every Day.
Britannica Quiz
Guess the City by Its River Quiz

Near the end of the upstream part of its course, the Yangtze descends to an elevation of 1,000 feet above sea level. Thus, over the first 1,600 miles (2,600 km) of its length, the river has fallen more than 17,000 feet (5,200 metres), or an average of more than 10 feet per mile (2 metres per km) of its course. In the mountains, however, there is a substantial stretch where the fall of the river is considerably greater.

The middle course

The middle course of the Yangtze stretches for about 630 miles (1,010 km) between the cities of Yibin in Sichuan province and Yichang in Hubei province. The climate is characterized by hot summers and relatively mild winters, as the high mountains to the west protect the region from the cold north and west winds. Annual precipitation measures between 40 and 60 inches (1,000 to 1,500 mm), a large part of it occurring in summer; the growing season lasts for more than six months. In most of this segment, the river crosses hilly Sichuan province, where the lower mountains and plateaus connect the highlands of southwestern China with the Qin (Tsinling) Mountains lying between the Yangtze and Huang He (Yellow River) basins. Located in this area is Chongqing, a major industrial centre and river port. The river’s width there is from about 1,000 to 1,600 feet (300 to 500 metres), and the depth in places exceeds 30 feet. The current is swift; the banks often are high and steep. The river falls some 820 feet (250 metres) in Sichuan, more than a foot per mile (0.2 metre per km) of flow.

Are you a student?
Get a special academic rate on Britannica Premium.

As the Yangtze flows through eastern Sichuan and into western Hubei, it traverses for a distance of 125 miles (200 km) the famous Three Gorges region before debouching onto the plains to the east. The gorges have steep, sheer slopes composed mainly of thick limestone rocks. Prior to the completion of the Three Gorges Dam in 2006, they rose some 1,300 to 2,000 feet (400 to 600 metres) above the river, although with the creation of the reservoir behind the dam their height has been diminished fairly significantly. Nonetheless, they still present the appearance of fantastic towers, pillars, or spears. Qutang, the first gorge—about 5 miles (8 km) long—is the shortest; prior to its inundation, the river there was considered the most dangerous for navigation, being extremely narrow with many rapids and eddies. Wu, the second gorge, stretches for about 30 miles (50 km); it is a narrow, steep corridor with almost vertical walls of heights up to 1,600 or even 2,000 feet above the river. The last gorge, Xiling, is located upstream of Yichang and extends for a distance of 21 miles; in places limestone cliffs rise directly out of the water, although with the rise of the reservoir to much lower heights than before. The gorges are rocky, and the walls are speckled with cracks, niches, and indentations. Even before the river was inundated, its depth in the gorges was considerable, increasing to between 500 and 600 feet (150 and 180 metres) and giving the Yangtze the greatest depths of any river in the world.