What is the source of the Yellow River, and what is the source of the Yellow River

The source of the Yellow River is located in the hinterland of Qinghai. The source of the river is one for the Zha song, the second is about the ancient sect of the song, and the third is the Kari song. 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.

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

The Yellow River flows from west to east through nine provinces, including Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea.

The hydrological basin of the Yellow River. 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.

Every year, 1.6 billion tons of sediment are produced, 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 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 Yellow River originates in the Kariqu River Valley and the ancient Zonglie Basin in the Bayan Kala Mountains of Qinghai Province, and is divided into two sources: north and south.

The Yellow River is known as the mother river of China, giving birth to the 5,000-year-old civilization of the Chinese nation, so what is the source of the Yellow River? Let's find out.

01 Kariqu is located at the foot of the Khozi Khata Mountain 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.

02 It is an oval basin with a length of 40 kilometers from east to west and a width of about 60 kilometers from north to south. There are more than 100 small pools of water in the basin, and from a distance, it looks like countless sparkling pearls embedded in the basin. The water is surrounded by a natural pasture with green grass.

03 After the ancient sect was listed on the sea of stars and joined the Kariqu, the original channel of the source of the Yellow River was formed, Maqu. Maqu, the local Tibetan people call it the Peacock River. This section of the river is wide and shallow, and the flow rate is slow, resulting in large swamps and meadows and numerous water pools.

Maqu flows eastward through a 16-kilometre-long river valley into the famous Sea of Stars.

04 The Xingzhu Sea, which has historically been used to denote the entire headwaters of the Yellow River, is a basin-shaped wetland with a length of about 30 kilometers from east to west, and a short distance from north to south, only a few kilometers to more than a dozen kilometers.

05 In 1978, the state organized an expedition to the source of the river to conduct an on-the-spot investigation in the source area, and found that in the western part of the source area, there were three rivers that flow into the Xingzhu Sea, which are Zhaqu, Yougu Zongliequ and Kariqu. The flow of Zaqu is the shortest, and the amount of water is small, so it can only be counted as a tributary of the ancient Zongliequ. Compared with Kariqu, Kariqu is nearly 30 kilometers long, with a basin area of 700 square kilometers and more than twice the amount of water.

Therefore, the basis for determining that Kariqu is the source of the Yellow River is sufficient.

Maqu.

In 1952, the Yellow River Water Conservancy Committee organized a team to investigate the source of the Yellow River and the possibility of diverting water from the Tongtian River into the Yellow River. In 1978, the South-to-North Water Survey Team of the Yellow River Water Conservancy Commission, the Nanjing Institute of Geosis and the Lake Survey Team of the Department of Geography of Nanjing University conducted another investigation and study of the source area of the river.

At the same time, the Qinghai Provincial People** and the Qinghai Provincial Military Region invited relevant units to form an inspection group to conduct a one-month inspection and put forward a proposal that Kariqu be used as the source of the river to be sentenced to land. In 1985, the Yellow River Water Conservancy Commission was established in accordance with historical traditions and opinionsMaqu is confirmed to be the source of the Yellow River, and it is located in the southwest corner of the ancient Zonglie Basin, with an east longitude of 95°59'24", 35°01 N'18"place, set up the source of the river mark.

Geological influences

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. In the course of the history of Chenghe, the movement has been continuous and advancing with the times.

Soil erosion on the Loess Plateau and sediment excavation in the lower reaches of the Yellow River have been carried out since prehistoric geological times, and the influence of human activities has been increasing since then. According to various studies, the PaleoYellow River has three stages of development: the Early Pleistocene from the Tertiary to the Quaternary is the gestation period of the PaleoYellow River.

In the Middle Pleistocene of the Quaternary Period (1.15 million years ago and 100,000 years ago), the ancient Yellow River was born and grew in the period. In the Late Pleistocene (100,000 years ago, 10,000 years ago), the Yellow River formed an ocean system.