The origin of the Yellow River, where does the Yellow River originate

The Yellow River originates from the Zonglie Canal at the northern foot of Bayan Kala Mountain in Qinghai, with an altitude of more than 5,400 meters, and the surrounding high mountains are covered with snow all year round. The headwaters of the Yellow River include the Sea of Stars, a swamp of countless small lakes. After leaving the sea of stars, enter the Ngoling Lake and Zhaling Lake to Maduo, bypass the Jishi Mountain and the Xilian Mountain, and pass through the Longyang Gorge to reach Qinghai Guide, which is more than 1,900 kilometers long.

The upstream section is more than 1,500 kilometers long from Guide to Hekou Town, Suiyuan Province. The Yellow River is in Gansu, passing through many large canyons and gathering many tributaries. The middle section is more than 1,100 kilometers long from Hekou Town to Yujin, Henan.

The river bends and flows to the south, runs through the Loess Plateau, carries a large amount of sediment, surging down, reaches Hukou, the terrain falls steeply, forms Hukou Waterfall, and then flows through Longmen Gorge to Tongguan, the river channel widens, because of the tributaries such as Huiren Fenqin, Luohe River and Xiaoshui, the water volume increases greatly. The river water to Tongguan is blocked by Huashan, turns to the east, crosses Sanmenxia to Yuluo, and then enters the plain area. The downstream section flows into the Bohai Sea from Mengjin to Lijin County, Shandong, which is more than 870 kilometers long, because of the accumulation of sediment and the slow flow of water, there are embankments built on both banks, and it becomes higher than the ground"On the river on the ground"。

The Yellow River originates in the ancient Zonglie Basin at an altitude of 4,500 meters at the northern foot of Bayankala Mountain on the Qinghai-Tibet Plateau. Through Qinghai, Sichuan, Gansu on the Qinghai-Tibet Plateau, Ningxia, Inner Mongolia, Shaanxi, Shanxi on the Loess Plateau and Ordos Plateau, Henan and Shandong on the North China Plain, it flows into the Bohai Sea!

That's what everybody says!!

The northern foothills of the Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province.

Qinghai's ancient Zonglie Canal originated.

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, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea. 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 Yellow River originates in the ancient Zonglie Basin at the northern foot of the Bayankala Mountains on the Qinghai-Tibet Plateau.

The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain on the Qinghai-Tibet Plateau, and flows from west to east through nine provinces, including Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shanxi, Shaanxi, Henan and Shandong, and finally flows into the Bohai Sea. Precipitation in the basin.

It is small, mainly dryland agriculture, dry in winter and dry in spring, and precipitation is concentrated in summer, autumn, July and August.

Hydrological characteristics of the Yellow River:

Yellow river. The regional distribution of water resources is very uneven, showing a decreasing trend from south to north. Roughly west from Jimai, through the stone mountain, to the Daxia River, Tao River, along the Wei River.

The main stream reaches the Fen River.

To the south of the watershed line with the Qin River, it is mainly mountainous with good vegetation, the average annual precipitation is greater than 600 mm, and the annual runoff depth is more than 100 to 200 mm, which is the area with abundant water resources in the Yellow River Basin.

In the northern part of the basin, through Gaolan, Haiyuan, Tongxin, Dingbian.

To the north of the first line of Baotou, the climate is dry, the annual precipitation is less than 300 mm, and the annual runoff depth is less than 10 mm, which is the most water-poor area in the Yellow River Basin. The vast Loess Plateau between the above two lines.

In this area, the annual precipitation is generally 400 to 500 mm, the annual runoff depth is only 25 to 50 mm, and the soil erosion is serious, which is the main sediment area of the Yellow River.

The origin of the Yellow River is in the Bayan Karachabo Mountains on the Qinghai-Tibet Plateau.

The Yellow River is the second longest river in China, the most important birthplace of Chinese civilization, and the mother river of the Chinese.

It originates in the Bayankala Mountains of the Qinghai-Tibet Lost Fanxiang Plateau, is in the shape of several figures, flows through 9 provinces and regions such as Qinghai and Sichuan, and finally flows into the Bohai Sea, with a total length of about 5,464 kilometers and a basin area of about 10,000 square kilometers. It is also the river with the highest sediment content in the world because it flows through the Loess Plateau region in the middle section and carries a large amount of sediment.

The source of the Yellow River:

The soil plateau area carries a lot of sediment, so it is also the river with the highest sediment content in the world.

The source of the Yellow River is the ancient Zonglie Basin at the northern foot of the Bayan Kala Mountains on the Qinghai-Tibet Plateau. From west to east, it flows through 9 provinces (autonomous regions) of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea.

The Yellow River is one of the largest rivers in northern China and the longest river in the world.

1. China's second longest river. The total length is about 5,464 kilometers, and the basin area is about 752443 square kilometers. 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 called the river with the highest 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 origin of the Yellow River is in the ancient Zonglie Basin at the northern foot of the Bayankala Mountains on the Qinghai-Tibet Plateau, and its end is the Bohai Sea.

The Yellow River is a large river located in northern China, flowing from west to east through cities such as Qinghai, Inner Mongolia, Shanxi, Henan, Shandong, etc., with a total length of about 5,464 kilometers. According to the records of the People's Daily Online, the area of the Yellow River basin is almost 752443 square kilometers, and according to the records of the Yellow River Network, it is 10,000 square kilometers, including 10,000 square kilometers of the internal flow area.

The Yellow River is one of the most important birthplaces of Chinese civilization and is called the mother river by the Chinese. The Yellow River carries 1.6 billion tons of sediment every year, of which 1.2 billion tons will flow into the sea, and the remaining 400 million tons will be left in the lower reaches of the Yellow River all year round, forming an alluvial plain, which is very conducive to cultivation and nourishes a population.

The Yellow River is known as the mother river of the Chinese nation. His birthplace is on the Tibetan Plateau.