Many of the world's great civilizations have grown up around mighty rivers—Egypt on the Nile, the Mound-builder civilization on the Mississippi, the Indus Valley Civilization on the Indus River. China has had the good fortune to have two great rivers: the Yangtze and the Yellow River (or Huang He). The Yellow River is also known as the "cradle of Chinese civilization" or the "Mother River." Usually a source of rich fertile soil and irrigation water, the Yellow River has transformed itself more than 1,500 times in recorded history into a raging torrent that has swept away entire villages. As a result, the river has several less-positive nicknames as well, such as "China's Sorrow" and the "Scourge of the Han People." Over the centuries, the Chinese people have used it not only for agriculture but also as a transportation route and even as a weapon. The Yellow River springs up in the Bayan Har Mountain Range of west-central China's Qinghai Province and makes its way through nine provinces before it pours its silt out into the Yellow Sea off the coast of Shandong Province. It is the world's sixth-longest river, with a length of about 3,395 miles. The river runs across central China's loess plains, picking up an immense load of silt, which colors the water and gives the river its name. The recorded history of Chinese civilization begins on the banks of the Yellow River with the Xia Dynasty, which lasted from 2100 to 1600 BCE. According to Sima Qian's "Records of the Grand Historian" and the "Classic of Rites," a number of different tribes originally united into the Xia Kingdom in order to combat devastating floods on the river. When a series of breakwaters failed to stop the flooding, the Xia instead dug a series of canals to channel excess water out into the countryside and then down to the sea. Unified behind strong leaders and able to produce bountiful harvests since Yellow River floods no longer destroyed their crops so often, the Xia Kingdom ruled central China for several centuries. The Shang Dynasty succeeded the Xia around 1600 BCE and also centered itself on the Yellow River valley. Fed by the riches of the fertile river-bottom land, the Shang developed an elaborate culture featuring powerful emperors, divination using oracle bones, and artwork including beautiful jade carvings. During China's Spring and Autumn Period (771 to 478 BCE), the great philosopher Confucius was born in the village of Tsou on the Yellow River in Shandong. He was almost as powerful an influence on Chinese culture as the river itself. In 221 BCE, Emperor Qin Shi Huangdi conquered the other warring states and established the unified Qin Dynasty. The Qin kings relied on the Cheng-Kuo Canal, finished in 246 BCE, to provide irrigation water and increased crop yields, leading to a growing population and the manpower to defeat rival kingdoms. However, the Yellow River's silt-laden water quickly clogged the canal. After Qin Shi Huangdi's death in 210 BCE, the Cheng-Kuo silted up entirely and became useless. In 923 CE, China was embroiled in the chaotic Five Dynasties and Ten Kingdoms Period. Among those kingdoms were the Later Liang and the Later Tang dynasties. As Tang armies approached the Liang capital, a general named Tuan Ning decided to breach the Yellow River dikes and flood 1,000 square miles of the Liang Kingdom in a desperate effort to stave off the Tang. Tuan's gambit did not succeed; despite the raging floodwaters, the Tang conquered the Liang. Over the following centuries, the Yellow River silted up and changed its course several times, breaking its banks and drowning surrounding farms and villages. Major re-routings took place in 1034 when the river split into three parts. The river jumped south again in 1344 during the waning days of the Yuan Dynasty. In 1642, another attempt to use the river against an enemy backfired badly. Kaifeng city had been under siege by Li Zicheng's peasant rebel army for six months. The city's governor decided to break the dikes in hopes of washing away the besieging army. Instead, the river engulfed the city, killing almost 300,000 of Kaifeng's 378,000 citizens and leaving the survivors vulnerable to famine and disease. The city was abandoned for years following this devastating mistake. The Ming Dynasty fell to Manchu invaders, who founded the Qing Dynasty just two years later. A northward course-change in the river in the early 1850s helped fuel the Taiping Rebellion, one of China's deadliest peasant revolts. As populations grew ever larger along the treacherous river's banks, so too did the death tolls from flooding. In 1887, a major Yellow River flood killed an estimated 900,000 to 2 million people, making it the third-worst natural disaster in history. This disaster helped convince the Chinese people that the Qing Dynasty had lost the Mandate of Heaven. After the Qing fell in 1911, China plunged into chaos with the Chinese Civil War and the Second Sino-Japanese War, after which the Yellow River struck again, this time even harder. The 1931 Yellow River flood killed between 3.7 million and 4 million people, making it the deadliest flood in all of human history. In the aftermath, with war raging and the crops destroyed, survivors reportedly sold their children into prostitution and even resorted to cannibalism to survive. Memories of this catastrophe would later inspire Mao Zedong's government to invest in massive flood-control projects, including the Three Gorges Dam on the Yangtze River. Another flood in 1943 washed away the crops in Henan Province, leaving 3 million people to starve to death. When the Chinese Communist Party took power in 1949, it began building new dikes and levees to hold back the Yellow and Yangtze Rivers. Since that time, floods along the Yellow River have still posed a threat, but they no longer kill millions of villagers or bring down governments. The Yellow River is the surging heart of Chinese civilization. Its waters and the rich soil it carries bring the agricultural abundance needed to support China's enormous population. However, this "Mother River" has always had a dark side to it as well. When the rains are heavy or silt blocks up the river channel, she has the power to jump her banks and spread death and destruction across central China.
The Mandarin Chinese word huang (“yellow”) is a reference to the fine loess sediments that the Yellow River carries to the sea. The Yellow River (Huang He), with a length of 3,395 miles (5,464 kilometres), is China’s second longest river—surpassed only by the Yangtze River (Chang Jiang). Its drainage basin is the third largest in China, with an area of some 290,000 square miles (750,000 square kilometres). The Yellow River originates in the Bayan Har Mountains, in the eastern Plateau of Tibet, at an elevation above 15,000 feet (4,600 meters). The Yellow River and its tributaries flow past some of China’s oldest cities, including Lanzhou, Baotou, Xi’an (Sian), Taiyuan, Luoyang, Zhengzhou, Kaifeng, and Jinan. Yellow River, Chinese (Pinyin) Huang He or (Wade-Giles romanization) Huang Ho, also spelled Hwang Ho, English Yellow River, principal river of northern China, east-central and eastern Asia. The Yellow River is often called the cradle of Chinese civilization. With a length of 3,395 miles (5,464 km), it is the country’s second longest river—surpassed only by the Yangtze River (Chang Jiang)—and its drainage basin is the third largest in China, with an area of some 290,000 square miles (750,000 square km). The river rises in southern Qinghai province on the Plateau of Tibet and crosses six other provinces and two autonomous regions in its course to the Bo Hai (Gulf of Chihli), an embayment of the Yellow Sea of the North Pacific Ocean. In its lower reaches it is a shifting, turbulent, silt-laden stream that often overflows its banks and sends floodwaters across the North China Plain. For that reason, it has been given such names as “China’s Sorrow” and “The Ungovernable.” The Mandarin Chinese word huang (“yellow”) is a reference to the fine loess sediments that the river carries to the sea. The Yellow River basin has an enormous population—exceeded by only a small number of countries—and the river and its tributaries flow past some of China’s oldest cities, including Lanzhou, Baotou, Xi’an (Sian), Taiyuan, Luoyang, Zhengzhou, Kaifeng, and Jinan.
A River Runs Through It: Fact or Fiction? Does Delhi, India, lie far from any river? Do many large rivers empty into the Bay of Bengal? Keep your head above water, and sort through the facts while floating through the questions in this quiz. The Yellow River is divided into three distinct parts: the mountainous upper course, the middle course across a plateau, and the lower course across a low plain. The Yellow River originates at an elevation above 15,000 feet (4,600 metres) in the Bayan Har Mountains, in the eastern Plateau of Tibet. In its upper reaches the river crosses two large bodies of water, Lakes Ngoring and Gyaring. Those shallow lakes, each covering an area of about 400 square miles (1,000 square km), are rich in fish and freeze over in winter. The Yellow River in that region flows generally from west to east. The broad highlands of the upper course rise 1,000 to 1,700 feet (300 to 500 metres) above the river and its tributaries. The highlands consist of crystalline rocks that are sometimes visible as eroded outcroppings on the surface. The river enters a region of deep gorges, winding its way first southeast, then northwest around the A’nyêmaqên (Amne Machin) Mountains, where its fall exceeds 10 feet per mile (2 metres per km), and then east again between the Xiqing and Laji mountains. Past the gorges, near the city of Lanzhou in southeastern Gansu province, it leaves the Plateau of Tibet. That transition marks the end of the upper Yellow River, which is some 725 miles (1,165 km) from its source. The upper course drains a basin covering about 48,000 square miles (124,000 square km), consisting chiefly of inaccessible, highly mountainous, sparsely populated terrain with a cold climate. The middle course of the Yellow River, extending more than 1,800 miles (2,900 km), consists of a great loop and drains an area of about 23,000 square miles (60,000 square km). The river at first flows northeast for about 550 miles (880 km) through the sandy soils of the northern Hui Autonomous Region of Ningxia and of the western Ordos Plateau. It has many rapids there, and in a number of places it narrows. The river then turns eastward and flows for another 500 miles (800 km) through alluvial plains in the Inner Mongolia Autonomous Region, in places branching into numerous distributary channels. In that stretch its fall is less than half a foot per mile (9 cm per km), and many of the channels have been developed over the millennia for irrigated agriculture. Lanzhou Portion of the Huang He (Yellow River) at Lanzhou, Gansu province, northwestern China. The Yellow River then turns sharply to the south and flows for about 445 miles (715 km), forming the border between Shaanxi and Shanxi provinces. The river’s width usually does not exceed 150 to 200 feet (45 to 60 metres) in that section, as it cuts through narrow gorges with steep slopes several hundred feet (above 100 metres) in height. The river then gradually widens, notably after receiving the waters of its two longest tributaries—first the Fen River of Shanxi province and then the Wei River of Shaanxi. At the confluence with the Wei, the Yellow River turns sharply to the east for another 300 miles (480 km) as it flows through inaccessible gorges between the Zhongtiao and eastern Qin (Tsinling) mountains. The average fall in that stretch is slightly more than 1 foot per mile (20 cm per km) and becomes increasingly rapid in the last 100 miles (160 km) before the river reaches the North China Plain at the city of Zhengzhou in Henan province. Most of the middle course is cut through the Loess Plateau, which extends eastward from the Plateau of Tibet to the North China Plain at elevations ranging between 3,000 and 7,000 feet (900 and 2,100 metres). The plateau contains terraced slopes as well as alluvial plains and a scattering of peaks sometimes rising more than 1,500 feet (450 metres) above the plateau. The river has cut at least six terraces across the plateau, which rise to more than 1,600 feet (500 metres) above the present river level. The terraces, formed over the past 2.5 million years, provide an important record of landscape evolution and ancient environmental change in the region. The underlying rock systems are covered with thick layers of loose soils, consisting mainly of wind-deposited sand and loess. The loess strata reach thicknesses of 160 to 200 feet (50 to 60 metres) and in some places as much as 500 feet (150 metres). Through those loose deposits the river has cut deep valleys, carrying away with it huge quantities of surface material, making that region one of the most highly eroded landscapes in the world. The easily eroded loess soil accounts for the instability of the riverbed both in the middle basin, where the erosion is considerable, and on the plain, where deposition builds up the channel bed. |
Why was the Huang He or Yellow River known as Chinas Sorrow
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