Land, people and culture 5
carries yellow (more accurately, brown) silt from the mountains down to the plains. The silt is deposited to contribute to a fi ne-grained, easily worked loess soil that has enabled China’s farmers to till the land for centuries.2
The waters of the Yellow River then irrigate this loess terrain. However, the silt that has been such a boon to rural China has also destroyed it periodically: the accumulation of silt deposits builds up over time and causes the river to burst its banks, fl ooding the farms and villages of the North China Plain and causing great loss of life as well as physical devastation and economic and social disruption. In one fateful year, 1851, the spectacular intensity of the fl ooding forced the river to change its course. Before the inundation, it fl owed into the ocean south of the Shandong Peninsula; afterwards it emerged to the north, at its present exit point. Not for nothing has the Yellow River been called ‘China’s sorrow’. The river that the world knows as the Yangzi (Yangtse) is known in China as the Changjiang, which simply means ‘Long River’, which it is – its total length is 3,964 miles. It fl ows from its source high on the Tibetan Plateau through spectacular gorges, passes through the very centre of China and spills out into the Yellow Sea just to the north of Shanghai. Its great breadth is as signifi cant as its great length. For centuries it was impossible to bridge the torrent for a distance of hundreds of miles and, in many places, it is still necessary to use a ferry to cross from one bank to the other. The construction of the great bridge at Nanjing, which was completed in 1969 during the Cultural Revolution, was proclaimed a major triumph for Chinese engineers and for the collective spirit of the People’s Republic. Because of the diffi culty that there has always been in crossing the Changjiang, the river was a major physical barrier and it is the natural boundary between northern and southern China – a separation which accounts in part for the pronounced cultural differences between the north and the south. The productive rice-growing areas of the south were traditionally known as Jiangnan (‘south of the river’, that is to the south of the Changjiang) and these areas have retained distinctive spoken languages and cultures which, especially in the rural areas, are quite unlike those of the northern, Mandarin-speaking part of China.
The Three Gorges hydroelectric project which dams the upper reaches of the river is a colossal and controversial feat of engineering which began in 1993, has submerged some 1,200 towns and villages and has displaced thousands of local residents. It has been criticised by environmental campaigners and many have blamed it for the increased pollution of the river. A more detailed consideration of the Three Gorges project can be found in Chapter 14.
Another important watercourse which is vital to the regional economy of south China is the Pearl River or Zhujiang. The Pearl River is China’s third longest and it is produced by the confl uence of three smaller rivers: the Xi Jiang (West River), the Bei Jiang (North River), and the Dong Jiang (East River). The river and its tributaries fl ow through the provinces of Hunan, Jiangxi, Guizhou, Yunnan, Guangxi and Guangdong before emptying into the South China Sea in the great Pearl River Delta.
The Pearl River Delta is home to some of the most dynamic and enterprising urban economies of contemporary China, including the pioneering Special
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