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The Yellow River, a major river in northern China, has a total length of about 5,464 kilometers and a basin area of about 752443 square kilometers. It is the fifth longest river in the world and the second longest river in China.
The Yellow River originates from the Maqu of the ancient Zonglie Basin at the northern foot of the Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province. From west to east, it flows through nine provinces, municipalities and autonomous regions of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea.
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. But in Chinese history, the diversion of the lower reaches of the Yellow River has had a huge impact on human civilization.
It is the main birthplace of Chinese civilization, and the Chinese call it the "mother river". Almost 1.6 billion tonnes of sediment are produced every year, of which 1.2 billion tonnes flow into the sea, leaving the remaining 400 million tonnes in the lower reaches of the Yellow River for many years, forming an alluvial plain that is conducive to cultivation.
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Yellow River (yellow
River), with a total length of 5,464 kilometers and a basin area of square kilometers, is the second longest river in China after the Yangtze River, which originates in the Kariqu at the northern foot of the Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province.
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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.
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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 from the Bayankala Mountains of the Qinghai-Tibet Plateau, in the shape of "several", 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.
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The Yellow River originates in the Bayankala Mountains of Qinghai Province, flows eastward from Qinghai Province, and its main stream flows through Qinghai Province, Gansu Province, Sichuan Province, Ningxia Hui Autonomous Region, Inner Mongolia Autonomous Region, Shaanxi Province, Shanxi Province, Henan Province, and finally empties into the Bohai Sea in Shandong Province. The Yellow River is the cradle of the Chinese nation.
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The Yellow River is the second longest river in China. It originates in the ancient Zonglie Basin at the northern foot of Bayankala Mountain on the Qinghai-Tibet Plateau. The total length is 5464 km. The basin covers an area of 10,000 square kilometers. Eventually, the Bohai Sea will be injected into our country.
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The Yellow River originates on the Tibetan PlateauBayan Kala MountainThe northern foothills of the Yogu Zonglie Basin.
The Yellow River flows from west to east through nine provinces (autonomous regions) 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.
The middle and upper reaches of the Yellow River are mainly mountainous, and the middle and lower reaches are dominated by plains and hills. As the middle section of the river flows through the Loess Plateau of China.
area, so it carries a lot of sediment, so it is also known as the river with the most sediment content in the world. But in Chinese history, the lower reaches of the Yellow River were diverted to human civilization.
The impact has been huge.
Geological impact of the Yellow River.
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.
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The birthplace of the Yellow River: 1. The Yellow River originates from the Kariqu River Valley and the ancient 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.
2. 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 rolling he. 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 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.
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The source of the Yellow River is located in Zhiduo County, Yushu Tibetan Autonomous Prefecture, Qinghai Province, with an altitude of about 5,300 meters, and is the birthplace of the Yellow River, one of the five major rivers in China. It is part of the Tibetan Plateau and is surrounded by spectacular mountains. The source of the Yellow River is mainly fed by glacial meltwater and rainfall, and the water is clear and pure.
The climate here is cold and dry, with long winters and short summers, typical of the highlands.
The birthplace of the Yellow River.
Hello, dear, I'm honored to answer for you! <>
The source of the Yellow River is located in Zhiduo County, Yushu Tibetan Autonomous Prefecture, Qinghai Province, with an altitude of about 5,300 meters, and is the birthplace of the Yellow River, one of the five major rivers in China. It is part of the Tibetan Plateau and is surrounded by spectacular mountains. The source of the Yellow River is mainly fed by glacial meltwater and rainfall, and the water is clear and pure.
The climate here is cold and dry, with long winters and short summers, typical of the highlands.
The birthplace of the Yellow River is an important area of Chinese history and culture, with a rich cultural heritage and historical traditions. There are many ancient Tibetan villages and temples here, such as Zhaling Lake, Ta'er Monastery, etc., which is one of the tourist attractions. The protection of the birthplace of the Yellow River has always attracted much attention, and all sectors of society have been actively promoting the protection work to protect the ecological environment and cultural heritage of the birthplace of the Yellow River, so that this beautiful land will always maintain its original natural features and historical and cultural value.
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What is the birthplace of the Yellow River? 1. The Yellow River originates in the Bayankala Mountains of the Qinghai-Tibet Plateau in Qinghai Province, the Bayankala Mountains are 780 kilometers long, about 5,000 meters above sea level, there are many high mountains covered with snow all the year round, the glaciers hang everywhere, after each spring, under the strong sunlight, the alpine ice and snow gradually melt, and the meltwater merges into streams to supply water for the Yellow River.
2. The Yellow River has three specific sources, the northern source originates from the Zhaqu at the southern foot of the Chahassila Mountain, the southern source originates from the Kariqu at the northern foot of the Gezikoya Mountain, the branch of the Bayan Kala Mountain, and the western source originates from the ancient Zongliequ in the western part of the Xingzhu Haixi. Among the three rivers of Zhaqu, Kariqu and Yugu Zongliequ, Kariqu is the longest, the basin area is also the largest, and it does not dry up in the dry season, so it is recognized as the source of the Yellow River.
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There are three birthplaces of the Yellow River, namely the Zhaqu of the Chahara Xixiaozi Xiang Mountain in the north, the Kariqu of the Gezigoya Mountain in the south, and the Yuegu Zongliequ of the Xingzhu Haixi in the west, all of which are in Qinghai Province.
Like the Yangtze River, the Yellow River is the birthplace of ancient Chinese civilization and is often referred to as the "river" in ancient times, with a total length of about 5,464 kilometers, flowing through several provinces of Qixing and finally entering the ocean in Kenli County, Shandong.
In fact, the water quality of the upper reaches of the Yellow River is not yellow, but the middle reaches pass through the Loess Plateau, where soil erosion is serious, and a large amount of sediment flows into the water, so the water quality in the middle and lower reaches of the Yellow River turns yellow.
The Yellow River is the world's largest river with the highest sediment content, with about 1.6 billion tons of sediment flowing into the river each year, most of which flows into the Loess Plateau.
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Summary. The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayan Kala Mountain in Qumalai County, Qinghai Province. Generally, the area from the source of the Yellow River to Xinghai (Longyangxia Reservoir) in Qinghai is called the source area of the Yellow River.
The Yellow River originates in the ancient Zonglie Basin at the northern foot of Bayan Kala Mountain in Qumalai County, Qinghai Province. Generally, the area above the source of the Yellow River to Xinghai in Qinghai (Longyang Gorge is buried in Suichunku people) is called the source area of the Yellow River.
Huangzhi Ju Stupid River is a large river located in the northern region of China, which is one of the longest rivers in the world and the second longest river in China (also known as the second largest river). The total length of the Yellow River is about 5,464 kilometers, and its basin area is about 752443 square kilometers in the "People's Daily Online", and the Ministry of Water Resources's "Yellow River Network" is recorded as:
The total area of the basin is 10,000 square kilometers (including the area of the inflow area 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 Kariqu and Yougu Zongliequ at the northern foot of Bayankala Mountain are the main source of the Yellow River, which originates from Yaradaze Peak in Bayankala Mountains.
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