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The Yellow River originates in the Bayankala Mountains of Qinghai Province, flows through nine provinces and regions of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea in Kenli County, Dongying, Shandong Province. With a total length of 5,464 kilometers, the main stream is the second longest river in China after the Yangtze River. The Yellow River is also the fifth longest river in the world.
The widest section of the Yellow River is from Baihe Town, Mengjin County, Henan Province to Gaocun Village, Dongming County, Shandong Province, with a width of 5 kilometers and 20 kilometers between the two banks. The widest part is the big car set in Changtan County, Henan, and the two sides are 20 kilometers apart. The narrowest part of the Yellow River is at the Aishan Pass in the downstream Dong'e territory, and due to the confrontation between the mountains on both sides, the narrowest part of the river channel is only 270 meters, and the water is high and surging.
Walking along the winding Yellow River to Aishan in Dong'e, you will find that the wide riverbed has narrowed sharply at the foot of Aishan. The opposite side of Aishan is the outer mountain, the two mountains hold hostage, forming a natural bayonet, the rapid yellow water swarms, squeezed in the narrow riverbed, roaring, roaring, galloping, forming a magnificent landscape that is not the mouth of the pot, but like the mouth of the pot. This is the narrowest point in the lower reaches of the Yellow River.
Aishan Kakou is not only a natural beauty in the lower reaches of the Yellow River, with high water and high waves; It is also a good place for local people to enjoy leisure and entertainment. "Autumn view of the waves and winter view of the ice, the sixteenth day of the first month put the river lantern. The carp of the Yellow River jumps the bayonet, and the dragon is locked at the foot of Aishan.
It is a true portrayal of the landscape that tourists come to see in different seasons.
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The total length of the Yellow River is 5,464 kilometers, the width is 5 kilometers, and the width is 20 kilometers.
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The distance between the embankments on both sides of the Yellow River is 5 kilometers wide and 20 kilometers wide. At its widest point, the two sides are 20 kilometers apart. Hehe.
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The widest part of the Yellow River is 1,500 meters.
The Yellow River 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 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 (autonomous regions) of Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Minxiang, Henan, and Shandong, and finally flows into the Bohai Sea. The precipitation in the basin section 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. 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.
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 to create a splendid and dazzling ancient culture in this vast land.
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With a total length of 5,464 kilometers, the Yellow River originates in the northern foothills of the Bayankala Mountains in Qinghai Province, and its main stream flows from west to east through nine provinces and autonomous regions and flows into the Bohai Sea.
Of course, the narrowest part is the two ends, and the bifurcation will become more and more detailed until there is no more, so the narrowest part is very small. Imagine it and you'll know.
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The width of the Yellow River is generally 500 meters, and the narrowest point is only 50 meters, and the width of Hukou Waterfall is the narrowest.
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The source of the Yellow River, the narrowest, 0m, or no width.
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The widest part of the Yellow River is the big car set in Changtan County, Henan, and the two banks are 20 kilometers apart from each other. It is a large river located in northern China, 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 the area of its basin is about 752443 square kilometers according to the People's Daily Online, and the Ministry of Water Resources ** "Yellow River Network" is recorded as: the total area of the basin is 10,000 square kilometers (including the area of the inflow area of 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.
Geological influence: 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 generated by the 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.
The above content reference: Encyclopedia - Yellow River.
Characteristics of the Yellow River: 1. Less water and more sand; 2. The spatial and temporal distribution of water and sand is uneven; 3. Hanging river on the ground; 4. Frequent flood disasters. >>>More
The main hazards of the Yellow River are flooding.
Most of the floods in the upper reaches of the Yellow River occurred in September, mainly from above Lanzhou, and the floods in Lanzhou mainly came from above Guide. Due to the long duration and low intensity of rainfall, coupled with the good vegetation above Lanzhou, the grassland and swamp have a strong effect on rainfall, resulting in a gentle flood rise and fall in the upper reaches of the Yellow River, with a long flood duration, low flood peak, and a short and fat flood process line. >>>More
The sayings about the Yellow River are as follows: >>>More
To harness the Yellow River, it is first necessary to maintain a comprehensive management of water and soil on the Loess Plateau in the middle reaches of the Yellow River, plant more trees, and reduce the amount of sediment flowing into the river. Next, the lower reaches of the Yellow River were to excavate the riverbed and reduce the height of the riverbed.
Uncle He, dear, you will have it in a moment.