Yellow River (Huang He) | |
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Course of the Yellow River with major cities | |
Origin | Bayankala Mountains, Qinghai Province |
Mouth | Bohai Sea |
Basin countries | China |
Huang He, which is also known as the Yellow River because of the color of its silt, is the third longest river in Asia and the sixth longest river in the world. Located in China and measuring 5,464 kilometers (3,395 miles) in length, the river originates the Bayan Har Mountains in Qinghai province, western China.
Two great rivers run through China Proper: the Yellow River in the north, and the Yangtze (or Yangzi ) River to the south. In fact, most of China Proper belongs to the drainage-basins of these two rivers. Both originate to the far west in the Tibetan Plateau.
Yangtze River. The Yangtze River (or, "Changjiang" in Chinese, literally, the "long river"), is the longest river in China, running 6,300 kilometers (3915 miles). It is also the third longest river in the world.
Yellow RiverCountryChinaProvinceQinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan, ShandongPhysical characteristicsSourceBayan Har Mountains25 more rows
The Huang He (Yellow River) Valley is the birthplace of Chinese Civilization. The Yellow River is the second largest river in China and one of the longest river systems in the world.
This is because the sediment itself is in small, fine grains, meaning it can travel a long distance because its interaction with the water, banks and riverbed produces minimum friction. The large amount of sediment is what gives the river its yellow colour.
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.
The Yellow River is yellow because of the great amount of yellow silt suspended in the river. The yellow silt (loess) mainly comes from China's Loess Plateau.
The Yellow RiverThe Yellow River is called the "Mother River of China" and "the Cradle of Chinese Civilization" in China, as the Yellow River basin is the birth-place of the northern Chinese civilizations and the most prosperous region in the early Chinese history.
The Yellow River Basin is located between Qinghai and Shandong provinces, with a characteristic broad serpentine shape, taking it as far north as Inner Mongolia and as far south as Sichuan.
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 Ganges flows south and east from the Himalayas, forming a canyon as it leaves the mountain. It winds its way through northern India, eventually emptying into the Bay of Bengal. The Ganges' many tributaries originate from the nearby countries of Nepal, Bangladesh, and China (in an autonomous region called Tibet).
The name "Yellow River" comes from the huge amounts of "yellow" loess sediment it carries when flowing through the Loess Plateau. It is the world's...
Almost all Chinese agree that the Yellow River Basin was the cradle of Chinese Civilization. A great amount of archeological information proves tha...
Along the Yellow River, there are numerous historic and ancient attractions, and stunning scenery. Top attractions of the Yellow River include fore...
The Yellow River is the most important water resource for the dry north of China, playing an irreplaceable role in economic development, and agricu...
With global warming, decrease in rainfall in the Yellow River Basin, and increasing water demands for irrigation, industry, etc., the Yellow River...
Along the Yellow River, there are many worthwhile attractions and many tourist cities, such as Lanzhou, Zhongwei, Yinchuan, Baotou, Yan'an, Luoyang...
The Yellow River originates on the Qinghai-Tibet Plateau and flows through nine provinces from west to east, flowing into Bohai Sea. It is the "mother river of China": its basin was the center of Chinese politics, economy, and culture for over 2,000 years.
The Yellow River is yellow because of the great amount of yellow silt suspended in the river. The yellow silt (loess) mainly comes from China’s Loess Plateau.
The name "Yellow River" comes from the huge amounts of "yellow" loess sediment it carries, which are eroded when it flows through the Loess Plateau. It is the world's major river with the most excessive siltation.
The Yellow River carries an average of 1.6 billion tons of sediment a year. If the sediment were built into a wall one meter wide and one meter high, it would be three times as long as the distance between the Earth and the moon and 27 times as long as the equator.
Between 608 BC and 1938 AD, the Yellow River changed course 26 times, and flooded over 1,500 times .
When the Yellow River navigates Inner Mongolia, it mostly crosses grassy plains.
The Yellow River is the most important water resource for the dry north of China, playing an irreplaceable role in economic development, and agriculture. Since 1960 over 14 dams have been constructed on the river for hydroelectric power, which is vital to northern China's infrastructure.
The Yellow River is known for collecting enormous amounts of loess (a type of fine-grained sediment) from the Loess Plateau. 8. This sediment that the river collects gradually gets deposited in river bed, creating slow-accumulating subaqueous natural dam that remains undetectable and unpredictable.
The reason behind such names is its tendency of frequently creating devastating floods. Some of the floods it causes are so devastating that they kill millions of people.
Sometimes, the river would as far as 300 miles or 480 kilometers.
22. So, what makes the water of Yellow River yellow? It is the loess sediment that it picks up from Loess Plateau. The loess gives the typical yellow color to the river. The loess is extremely nutrient rich.
19. Because the levees were broken, the Yellow River flooded an area of 20,800 sq. mi. or 54,000 sq. km. The result was that anywhere between 500,000 to 900,000 Chinese people lost their lives. Yes, many Japanese soldiers were also killed.
First thing that happens is that the river bed rises slowly because of the vast amounts sediment deposit. This eventually leads to a situation where the water overflows and floods the surrounding regions, which stays low compared to the risen river bed. 10.
The Yellow River and the Yellow Sea are closely related because the river drains into the sea and is party responsible for the golden yellow color of the sea. Let us take a look at 30 facts about Yellow River and find out a few interesting things about it. Before we start with our list, let us take a quick look at some facts in a tabular format.
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 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.
The Yellow River (Hu ang He) basin and the Yangtze River (Chang Jiang) basin and their drainage networks. 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.
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.
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.
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 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. Yellow River (Huang He)