Where is the source of the Yellow River, and where is the source of the Yellow River?

Where is the source of the Yellow River?

The source of the Yellow River is in the Kariqu River Valley and the Yugu Zonglie Basin at the foot of the Gezigoya Mountain at the northern foot of Bayan Kala Mountain, which is divided into two sources: north and south. The altitude of the two places is between 4,600 and more than 4,800 meters. According to ancient records, the Yellow River was called the river in ancient times, also known as the Turbid River, also known as the China River.

According to legend, as early as the time of Yaoshun, the Yellow River was a famous river.

Kariqu is located at the foot of the various mountains at the northern foot of Bayan Kala Mountain, with an altitude of 4,830 meters. It is sourced from five small springs that flow from a hillside cut ditch, and the original channel is nothing more than a babbling stream about 1 meter wide and less than 1 meter deep.

The stream flows from southwest to northeast from the flat and narrow valley of the Kariqu River, receiving many large and small tributaries along the way, gradually merging into a small river about 10 meters wide and more than 1 meter deep. The water of the Kariqu River is crystal clear, the swimming fish can be counted, there are countless large and small, different shapes of "Haizi" on both banks, the river water passes through the canyon of more than 100 kilometers, meets with the ancient Zonglie in Bayan Heqiao Mountain, and flows into the Maqu River.

Where is the source of the Yellow River?

The source of the Yellow River is the Yogu Liezong at the western end of the lake basin in Maduo County, Qinghai Province.

The Yellow River is also known as the Mother River of China, the River Water, the Turbid River, and the Hanging River.

The Yellow River, a large river located in northern China, 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 the basin area is about 752443 square kilometers. Belongs to the water system:

It flows into the Bohai Sea system. The average flow rate is 2571 cubic meters. 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 originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain on the Qinghai-Qinghai-Tibet Plateau, flows west and east through nine provinces (autonomous regions) of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, 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 and 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 passes 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"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, which is conducive to planting and planting.

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 source of the Yellow River, the area above the Duoshi Gorge in Maduo County, Qinghai Province, is the source area of the river, with an area of 10,000 square kilometers, which is a part of the Qinghai Plateau, belongs to the wide valley belt of the lake basin, and the elevation of the sea is more than 4,200 meters. Around the basin, the mountains are majestic, there are Yaradze Mountains in the west, Animaqing Mountains (also known as Jishi Mountain) in the east, Burhan Buda Mountains in the north, and Bayan Kala Mountains and the Yangtze River basin in the south.

At the western end of the lake basin, there is the ancient Zonglie, which is the birthplace of the Yellow River.

The source of the Yellow River is in the Bayankala Mountains of the Qinghai-Tibet Plateau.

The headwaters of the Yellow River are located in the hinterland of Qinghai. The source of the river is about the ancient sect of Liequ. 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.

There is only one spring, which is an oval basin that is 40 kilometers long from east to west and about 60 kilometers wide from north to south, and there are more than 100 small water pools in it, which are like stars and pearls.

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: Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shanxi, Shaanxi, Henan and Shandong, and finally flows into the Bohai Sea.

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The source of the Yellow River is located on the Tibetan Plateau in Qinghai Province in northwestern China. Originally named the "White River", it originated in the Qilian Mountains in the southeast of Motuo County, and was composed of two tributaries, the Heilongjiang River and the Nu River. The Heilongjiang River can be divided into upstream source stream and middle stream tributaries, of which the upstream source stream can be divided into two tributaries

Tibetan Antelope River and Xining River. The Tibetan Antelope River can be divided into two tributaries: the Rawa River in the upper reaches and the Tanggula River in the lower reaches.

The Rawa River is the earliest source of the Yellow River, and it can be divided into two tributaries: the Lhasa River in the upper reaches and the Jinsha River in the lower reaches. The source of the Lhasa River is located in Malkang County on the Qinghai-Tibet Plateau, starting with a glacial lake, flowing from the southwest, flowing through the city of Lhasa, and finally confluence with the Jinsha River to form the Yellow River.