The source of the Yellow River, what is the source of the Yellow River called?

Yellow River: With a total length of 5,464 kilometers and a basin area of 752,443 square kilometers, it is the second largest river in China after the Yangtze River. 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.

However, in Chinese history, human civilization along the Yellow River basin has had a great impact and is one of the most important birthplaces of the Chinese nation, so the Chinese generally call it the "mother river". The Yellow River is the second longest river in China, the fifth longest river in the world, and the river with the highest sediment content in the world. Introduction Portrait of the Yellow River Mother (Lanzhou, Gansu).

The Yellow River, the mother river of China, if the motherland is compared to a rooster standing tall, the Yellow River is the artery of the rooster's heart, which has witnessed the great development history of the Chinese nation. The Yellow River is 5,464 kilometers long, with a basin area of nearly 752443 square kilometers, connected to thousands of tributaries and streams, like countless capillaries, continuously delivering vitality and vitality to the motherland. Giving birth to generations of outstanding Chinese sons and daughters, the descendants of Yan and Huang are like the surging water of the Yellow River leading the trend of the times in different fields, telling the glory of the Yellow River in different ways, and influencing the historical process of Chinese civilization.

For example, in modern times, Wei Yuan, Sun Yat-sen, He Ziyuan, Liang Qichao, etc. are like a wave of the surging Yellow River, but they are all ordinary members of the Chinese nation......The Yellow River (2 photos) The Yellow River flows through 9 provinces and meanders in northern China. Looking down from the sky, it is very much like a huge "several" character, and faintly like the unique totem --- dragon of our nation. The source is located in the Yaradazai Peak of the Bayan Kala Mountains in Qinghai, with a main stream length of 4,675 kilometers and an average flow of cubic meters per second, which flows into the Bohai Sea in Kenli County, Dongying City, Shandong Province.

The dividing point between the upper and middle reaches is Hekou Town in the Inner Mongolia Autonomous Region, and the boundary point between the middle and lower reaches is Jiumengjin in Henan Province. The estuary of the Yellow River is 1,500 meters wide, generally 500 meters, only 50 meters in the narrower places, the water depth is generally meters, and the depth in some places is only meters.

It originates from the Bayankala Mountains in Qinghai.

Later, after in-depth investigation, three sources were found: one is Zha Qu, the other is about the ancient Zonglie Canal, and the third is Kari Qu. Zha Qu dries up most of the year, while Kariqu is the longest, the largest basin area, and does not dry up in the dry season, which is the source of the Yellow River.

Where is the source of the Yellow River?

The source of the Yellow River is located in the ancient Zonglie Basin at the northern foot of the Bayankala Mountains on the Qinghai-Tibet Plateau. The Yellow River runs from the Tibetan Plateau through nine provinces, including Qinghai and Sichuan, and finally flows into the Bohai Sea in Dongying City, Shandong Province. The Yellow River is the second longest river in China, the most important birthplace of Chinese civilization, and the river with the highest sediment content in the world.

The Yellow River is one of the longest rivers in the world, and the second longest river in China. The total length of the Yellow River is about 5,464 kilometers, and its basin area is about 752443 square kilometers according to the People's Daily Online, and the Ministry of Water Resources's "Yellow River Network" records that the total area of the basin is 10,000 square kilometers. The basin has long winters and short summers, and the temperature difference between winter and summer is huge, and the seasonal temperature changes are distinct.

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 area 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.

The northern source of the Yellow River originates from the Zhaqu at the southern foot of the Chahasila Mountain, a branch of the Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province, the southern source originates from the Kariqu at the northern foot of the Gezigoya Mountain, the branch of the Bayan Kala Mountains, and the western source originates from the Yougu Zongliequ in the western part of the Xingzhu Haixi.

With a total length of about 5,464 kilometers, the Yellow River is the fifth longest river in the world and the second longest river in China. The Yellow River flows through 9 provinces: Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong. Finally, it flows into the Bohai Sea.

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 of the Houtao irrigation area, and the Longmen Tongguan river channel also swung greatly. The course change of the Yellow River mainly occurred in the lower reaches of the Yellow River, and the range of channel changes in the lower reaches of the Yellow River in history was roughly from the Haihe River in the north to the Jianghuai River in the south.

The above content refers to the Encyclopedia - Yellow River.

The source of the Yellow River is located in the hinterland of Qinghai, and there are three main sources, the source of Zhaqu, the source of the ancient Zongliequ, and the source of the Kariqu, each of which plays a different role. Zhaqu dries up most of the year, while Kariqu is the longest with five springs, and the basin area is also the largest, and it does not dry up in the dry season, which is the source of the Yellow River.

Kariqu originated from the northern foot of the Bayan Kala Mountain branch of the various Zikoya Mountains, the altitude reached 4830 meters, the basin area of Kariqu reached square kilometers at that time, and later several springs at the foot of the mountain also overflowed a lot of clear water, increasing the basin of Kariqu, resulting in the current source of the Yellow River.

The Yellow River is more than 5 kilometers long, flows through 9 provinces and finally converges on the Bohai Sea. Beginning with the first Chinese dynasties, many dynasties have established their capitals along the Yellow River for thousands of years, and the Yellow River has played an important role. The Yellow River has a large volume of water and never breaks its flow.

The Yellow River is the mother river of the Chinese nation, she not only fed hundreds of millions of sons and daughters of China, in the Yellow River basin thousands of years ago, but also produced the initial fire of Chinese civilization, China's historical and cultural ancient cities, more than half of them are in the Yellow River Basin, such as Xi'an, Luoyang, Kaifeng, Qufu, etc., it is enough to see that the Yellow River has a major role in promoting the process of Chinese civilization and a major impact on the daily life of modern people.

The source of the Yellow River is in the hinterland of Qinghai Province in China.

The source of the Yellow River is in the hinterland of Qinghai Province in China, and the source is divided into three river sources: Zhaqu, about Guzong Liequ and Kariqu, and the multiple sources of the Yellow River are also the views of most people at present.

The main tributaries of the Yellow River include the Bai River, the Hei River, the Huangshui River, the Zuli River, the Qingshui River, the Dahei River, the Kuye River, the Wuding River, the Fen River, the Wei River, the Luo River, the Qin River, the Dawen River, etc. Among them, the Wei River is the largest tributary of the Yellow River.

The main lakes on the Yellow River are Zhaling Lake, Ngoling Lake, Wuliangsuhai Lake, and Dongping Lake.

The Yellow River Basin is vast, with many mountain ranges, a huge difference in elevation between the east and the west, and great differences in the landform of each region. In addition, because the basin is located in the mid-latitude zone, the influence of atmospheric circulation and monsoon circulation is relatively complex, so the climate in different regions of the basin is significantly different, and the annual and seasonal changes of climate elements are large.

During the period from 3000 to 2000 B.C. (from Yangshao culture period to Yinxu in Anyang) in the Yellow River Basin, the geographical environment was suitable for the growth of vegetation and the development of human production and living activities, and the climatic environment was about 2 years higher than that of the Yellow River Basin, which created excellent conditions for the development of crops and vegetation. During this period, there were a large number of lakes in the middle and lower reaches of the Yellow River, such as Leixiaze and Onozawa. "Mencius Teng Wen Gong I" once recorded that the Yellow River Valley "lush vegetation, birds and beasts breed", and the Guanzhong Plain still had "beautiful mountains, forests, rivers and valleys, and many genius powers" until the Warring States Period of China.

After the Warring States period, with the widespread use of iron farming tools and the migration of the economic center of the Qin State to Guanzhong, the vegetation of the Yellow River Basin and the Loess Plateau began to be destroyed. Because the Yellow River Basin has been the center of Chinese civilization for a long time, coupled with the phenomenon of ancient China's emphasis on agriculture and light animal husbandry, the destruction of vegetation in the Yellow River Basin has become a long-term and large-scale phenomenon.

With the beginning of the global cooling in the thirties of the 15th century AD and the southward migration of China's economic center, the ecological damage in the Yellow River basin began to decrease, but the forest cover has been difficult to recover to the state of the 3rd century BC. With the destruction of vegetation, the Loess Plateau began to be eroded by the Yellow River and swept away a large amount of soil, forming a surface form of thousands of ravines.