Which mountain range does the Yangtze River originate in? Where does the Yangtze River originate?

The Yangtze River originates from the southwest side of Geladan Winter Peak in the Tanggula Mountains.

The well-known Yangtze River has three sources, namely the middle sourceTuotuo River, the south source of Dangqu, the north source of the Chumar River.

Among them, the core area of the headwaters of the Tuotuo River is located in the Geladan Winter Snow Mountain, Kunlun Mountain and Tanggula Mountain.

Between. Drops of water flow out of the cracks in the ice, between the layers of ice. Stay until there is a lot of meltwater.

By the time it came out of the ice, it was already raging.

The Tuotuo River, which flows from the trickle of glaciers, originates from the Jianggendiru Glacier on the southwest side of the Geladan Winter Snow Mountain, which is the most famous and largest glacier in the modern glaciers around the Geladan Winter Snow Mountain. ** Looks like the water is coming out of the world of ice.

The role of the Yangtze River:

Most of China's freshwater lakes.

It is distributed in the middle and lower reaches of the Yangtze River.

The larger area is Poyang Lake.

Dongting Lake, Taihu Lake and Chaohu Lake. The strategic significance of the Yangtze River is self-evident. Whether it is a battleship or a large type of ship, it can go straight up and down.

Jinsha River in the upper reaches of the Yangtze River.

This section of the water flow is very different, the water resources are extremely abundant, but the degree of availability is very low, there are the famous Three Gorges in the middle reach, it is a famous tourist attraction, and Nanjing in the lower reaches, the famous six ancient capitals.

One of them, Shanghai, the most prosperous city in China, is now the most prosperous city in China, and the entire Yangtze River is a magnificent and majestic epic.

The Yangtze River originates in the southwest of Qinghai Province and the main peak of the Tanggula Mountains on the Qinghai-Tibet Plateau.

In the summer of 1976 and the summer of 1978, the Yangtze River Basin Planning Office organized two Jiangyuan survey teams to conduct detailed field investigations in the Jiangyuan area to find out the water system and the source of the river. The upper source of the Yangtze River is located between Kunlun Mountain and Tanggula Mountain, where there are many rivers, the larger ones are Chumaer River, Tuotuo River and Dangqu 3. Among them, both the area and the amount of water in the basin are the largest in Dangqu, and according to the principle of "the source of the river is far away", the Tuotuo River is determined to be the positive source.

, the south source of Dangqu, the north source of the Chumar River. In the Jiangyuan area, there are more than 40 snow-capped mountains above 6,000 meters above sea level. The temperature is low, and the four seasons are like winter.

The annual precipitation is 200,400 mm, and the snowfall is predominant. The average temperature in July is lower than 0, and only during the day under the strong radiation of the sun, the temperature can reach more than 0, and the trickle formed by the melting water of ice and snow will become the initial water source of the Yangtze River.

Climatic characteristics of Gradandon.

The temperature difference is relatively large, and precipitation is scarce.

Gradandong is located in the territory of Tanggula Mountain Township, Golmud City, the highest peak of Tanggula Mountain Range. Gradandong Snow Mountain is the birthplace of the Yangtze River and one of the most distinctive glacial snow-capped mountains in China. At the same time, the expansion and contraction of the glacier in the East Snow Mountain of Gradandong clearly reveals the changes in the local climate, the Qinghai-Tibet Plateau and the world, which is of great scientific value.

The geological structure of the Gradandong area is complex, the glacier activity is frequent, and the cutting and fragmentation are the resulting terrain conditions. The climate is dry, with perennial low temperatures above 5,000 meters above sea level, and as low as below the coldest time. This area is not only rich in water, but also contains a large amount of precious minerals such as brass, iron, crystal, etc.

The above content refers to the Encyclopedia - Gradandon.

Encyclopedia - Tuotuo River.