The source of the Yellow River is, where the Yellow River originates

It originates in Qumalai County, Yushu Prefecture, and its source is in the Goshkoya Snow Mountain at the northern foot of Bayan Kala Mountain in Maduo Township.

Qinghai Bayan Kala Mountain at the northern foot of the Occupy Zonglie Canal.

The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain on the Qinghai-Tibet Plateau, and flows through 9 provinces (autonomous regions) of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shanxi, Shaanxi, Henan and Shandong from west to east.

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 Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province.

Therefore, the birthplace of the Yellow River is in Qinghai Province, in the shape of "several", flowing through 9 provinces and regions such as Qinghai and Sichuan, and finally flowing into the Bohai Sea, with a total length of about 5,464 kilometers and a basin area of about 10,000 square kilometers.

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 accumulation in the lower reaches of the Yellow River have been going on since prehistoric geological times, and the impact 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.

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.

The south branch became the mainstream, and the north branch became the retreat canal in the rear irrigation area. The swing of the Longmen Tongguan river is also larger. However, the evolution of these sections has little impact on the development of the Yellow River as a whole. The course change of the Yellow River mainly occurs in the lower reaches.

1. The source of the Yellow River is in the ancient Zonglie Basin, which is located at the northern foot of Bayan Kala Mountain on the Qinghai-Tibet Plateau, which is about 40 kilometers long from east to west and about 60 kilometers wide from north to south.

2. In the southwest of the ancient Zonglie Basin, there is a small spring with an area of less than four square meters, from which clear spring water continues to gush, thus forming countless trickles in the basin. The original channel of the Yellow River was called "Maqu" by the Tibetan people, and Maqu was formed by the confluence of Yougu Zonglie Qu and Kari Qu in the Yugu Zonglie Basin.

3. In addition to the two sources of the ancient Zongliequ and the Kariqu, there is also a source called Zha Qu, which is also known as the "Three Sources of the Yellow River". After the ancient Zongliequ and the Kari song merged into the Maqu, they merged into the Sea of Stars. According to the surveys of geographers, Kariqu is 25 kilometers long than the ancient Legzong.

The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain 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 precipitation in the basin is small, mainly dryland agriculture, dry in winter and dry in spring, and the precipitation is concentrated in summer, autumn, July and August.