Ranking of the world s most sediment rich rivers

The Yellow River is the world's largest river with the largest sediment content, the second longest river in China and the fifth longest river in the world, and is known as China's "mother river". The length of the Yellow River is 5 464 km, and the basin area reaches 752 square km.

It flows through 9 provinces and regions and meanders in northern China. Looking down from the sky, it resembles a huge "few" character, and faintly resembles the unique totem of our nation - the dragon.

The middle reaches of the Yellow River flow through the Loess Plateau.

Due to soil erosion, tributaries bring in a lot of sediment, making the Yellow River the most sediment-laden river in the world. The maximum annual sediment discharge was 3.9 billion tons (1933), and the highest sediment content was 920 kilograms cubic meters (1977). The average sediment transport capacity of Sanmenxia Station is about 1.6 billion tons for many years, and the average sediment content is 35 kilograms of cubic meters, while the sediment content per cubic meter of water in the Yangtze River is less than 1 kilogram.

The sediment passes through the entrance of the Yellow River into the Bohai Sea and the Yellow Sea.

As far as the East China Sea there are 100 million tons, and the remaining 4200 million tonnes were deposited along the river.

The Yellow River uses an average of 1.6 billion tonnes of sediment annually to build a wall one meter wide and one meter high, which is equivalent to the length of the Earth and the Moon.

(38.)440,000 km), which is equivalent to 27 times the length of the equator.

A large amount of loess on the Loess Plateau is transported from the Yellow River to the plain and to the sea, accumulating over time, making the land continue to expand and the sea basin to continue to be shallow. In this way, not only the eastern part of the Loess Plateau formed a huge North China Plain.

Moreover, in the eastern edge of China, a shallow sea continental shelf has been reclaimed that is unparalleled in the world.

At present, most of the Bohai Sea, the Yellow Sea, and the East China Sea are within the scope of the shallow sea continental shelf.

The Yellow River has the highest sediment content in the world.

The river with the largest sediment content is the Yellow River in China!

The river with the largest sediment content in the world is the Yellow River.

At the same time, the Yellow River ranks second among all the long rivers in China, and ranks fifth among the world's long rivers, located in the north of China, once known as the mother river of China, the main reason for the large sediment content in the Yellow River is because the middle section of the Yellow River flows through the Loess Plateau region, the area does not have too much vegetation, it is easy to match the town to cause soil erosion, the Yellow River water flows, it will take away a large amount of sediment in the area, and these sediments will enter the Yellow River with the river.

The total length of the Yellow River is 5464 kilometers, the area has reached 752445 square kilometers, the Yellow River originates in the source of the three rivers in Qinghai, flows from west to east through Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan, Shandong and other 9 provinces, the end of the Yellow River is in the Bohai Sea, the Bohai Sea area is arid weather most of the time, the agriculture in the region is also dominated by dry land, the middle and upper reaches of the Yellow River are mainly mountainous and most of the middle and lower reaches are plains and hills.

Benefits of the Yellow River to Mankind:

The Ningxia Plain and the Hetao Plain are shaped by the Yellow River, and the Yellow River also participated in the shaping of the North China Plain, which is one of the three major plains in China, and the Yellow River contains very rich water energy resources, and a large number of water energy resources are provided to Li He in the middle and upper reaches of the Yellow River for industrial development.

Not only that, but the Yellow River also flows through arid or semi-arid areas where there is not enough precipitation all year round, and most of the water comes from the Yellow River, which also provides sufficient irrigation water for most areas. <>

The most sediment-laden river in the world is the Yellow River.

Further information is as follows:

The Yellow River is one of the longest rivers in the world and the second longest river in China (also known as the second largest river). The total length of the Yellow River is about 5,464 kilometers, and its basin area is about 752443 square kilometers in the "People's Daily Online", and the Ministry of Water Resources's "Yellow River Network" is recorded as:

The total area of the basin is 10,000 square kilometers (including the area of 10,000 square kilometers in the inflow area).

The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain on the Qinghai-Tibet Plateau, flows from west to east through nine provinces (autonomous regions) of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shanxi, Shaanxi, Henan and Shandong, and finally flows into the Bohai Sea. The precipitation in the basin is small, mainly dryland agriculture, dry in winter and dry in spring, and the precipitation is concentrated in summer, autumn, July and August.

The middle and upper reaches of the Yellow River are mainly mountainous, and the middle and lower reaches are dominated by plains and hills. Because the middle section of the river flows through the Loess Plateau region of China, it carries a large amount of sediment, so it is also known as the river with the most sediment content in the world. But in Chinese history, the diversion of the lower reaches of the Yellow River has had a huge impact on human civilization.

The Yellow River is the main birthplace of Chinese civilization, and the Chinese call it the "Mother River". Every year, 1.6 billion tons of sediment are carried, of which 1.2 billion tons flow into the sea, and the remaining 400 million tons remain in the lower reaches of the Yellow River for many years, forming an alluvial plain that is conducive to cultivation.

The Yellow River Basin is the earliest developed region in China. When most of the world was still in a state of ignorance, our industrious and brave ancestors cut thorns, cleared grass, and worked in this vast land, creating a splendid and dazzling ancient culture. At 12 o'clock on April 1, 2023, the entire Yellow River entered a fishing ban period.

The gestation, birth and development of the Yellow River are subject to the geological processes in the geohistorical period, with the tectonic movement caused by crustal changes as the external force, and the erosion, transport and accumulation under hydrological conditions as the internal force.

Yellow River.

The middle reaches of the Yellow River flow through the Loess Plateau, and its tributaries bring in a large amount of sediment, making the Yellow River the river with the highest sediment content in the world, with a maximum annual sediment discharge of 100 million tons (1933) and a maximum sediment content of 920 kilograms and cubic meters (1977). The average sediment transport capacity of Sanmenxia Station is about 1.6 billion tons for many years, and the average sediment content is 35 kilograms of cubic meters.

River course changes. During the historical period, the river course of the Yellow River in the upper and middle reaches of the plain has also evolved, and some of the changes are still great. For example, the Hetao section of Inner Mongolia, before 1850, it is mainly divided into two branches, the north branch is the main stream, the foot of the Yin Mountain is called the Wujia River, and the south branch is the Yellow River today.

In 1850, the lower reaches of the Wujia River north of Xishanzui were silted up and cut off for about 15 kilometers, and the south branch became the mainstream, and the north branch became the retreat canal in the Houtao irrigation area. The swing of the Longmen Tongguan river is also larger. However, the evolution of these sections has little impact on the development of the Yellow River as a whole.

The course change of the Yellow River mainly occurs in the lower reaches.

Historically, the range of river changes in the lower reaches of the Yellow River has roughly reached the Haihe River in the north and the Jianghuai River in the south. According to historical records, the lower reaches of the Yellow River have flooded more than 1,500 times, and there have been more than 20 major diversions.

What is the world's largest sandy river in Kaina?

a.The Yellow River is late.

b.Danube.

c.Nile.

d.Amazon.

Correct Answer: a