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The Fen River is in Shanxi, and the Wei River is in Shaanxi.
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The Fen River originates from the foothills of Ningwu Guanshui Mountain in Shanxi Province, runs through the north and south of Shanxi Province, flows through Jingle County, Gujiao City, Taiyuan City, Qingxu County, Qi County, Jiexiu City, Huozhou City, Hongdong County, Linfen City, Houma City, and joins the Yellow River near Hejin.
The Fen River, known as Fen in ancient times, is also known as Fenshui, the second largest tributary of the Yellow River. The source tradition believes that it is the Leiming Temple Spring at the foot of Guanshui Mountain in Ningwu County, Shanxi Province, and the modern investigation believes that it is in Xiling Village, Taipingzhuang Township, Shenchi County.
The formation and evolution of the Fen River.
The Fen River system is influenced by meridional tectonic systems such as Luliang Mountain and Taihang Mountain, and develops into rivers in a series of graben basins. The ancient Fen River is longer and larger, in the late Pliocene, the Fen River has a long history, runs through the four major basins of Xinding, Taiyuan, Linfen and Yuncheng, flows through the south of Zhongtiao Mountain, and crosses the Yellow River in Maojin, Pinglu County.
Later, after the Himalayan movement, both the beginning and the end were attacked. Later, due to the uplift of Shilingguan and the rapid erosion rate of the river on the eastern side of Taihang Mountain, it attacked the east branch of the Fentuo River and became the upper reaches of the Hutuo River, leaving a very unnatural bend in the landform, while the Fen River retained its west branch and became the upper reaches of the Fen River.
The lower reaches of the Fen River still flowed into the Yellow River in the south through the Yuncheng Basin in the Pliocene, and then fell downward again due to the north-east-trending fault of the Lianshui River Valley, causing the Gufen River to turn around, running along the lower reaches of the Lianshui River Valley to join the Yellow River near Yongji County.
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The Wei River originates from the Bird and Mouse Mountain in Weiyuan County, Gansu Province, and its main stream flows from west to east, passing through Gansu and Shaanxi Provinces, and joins the Yellow River in Tongguan County, Weinan City, with a total length of 818 kilometers, which is the longest tributary of the Yellow River.
The south of the Wei River is the northern foot of the Qinling Mountains, the north is the Loess Plateau, the Wei River basin can be divided into east and west, the west is the loess hilly and gully area, and the east is the Guanzhong Plain (Weihe Plain).
The Guanzhong Plain starts from Baoji in the west, reaches Tongguan in the east, is more than 300 kilometers long from east to west, covers an area of about 10,000 square kilometers, and is known as "800 miles of Qinchuan". Guanzhong Plain is an alluvial plain and valley formed by the Wei River, Jing River, Luo River and other rivers, with fertile land, developed irrigation and abundant products, and is known as the "Land of Abundance" in history.
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The Wei River, the largest tributary of the Yellow River in China. The basin is mainly in the central part of Shaanxi Province. It originates from Bird and Mouse Mountain in Weiyuan County, Gansu Province, reaches Weinan City in Shaanxi Province in the east, and joins the Yellow River in Tongguan County.
There is the Qinling Mountains in the south, which runs east-west, and there is the Liupan Mountain barrier in the north. The Weihe River Basin can be divided into two parts: the loess hilly and gully area in the west, and the Guanzhong Plain in the east.
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The Fen River is in Shanxi Province. The Fen River flows through 29 counties (districts) of 6 cities in Shanxi Province, including Xinzhou City, Taiyuan City, Luliang City, Jinzhong City, Linfen City and Yuncheng City, with a total length of 713 kilometers and a basin area of 39,721 square kilometers, and joins the Yellow River in Miaoqian Village, Ronghe Town, Wanrong County. The Fen River, known as "Fen" in ancient times, is a tributary of the Yellow River in Shanxi Province and is the second largest tributary of the Yellow River.
The Fen River is the largest river in Shanxi and is known as the mother river by the people of Shanxi, which has a profound impact on the history and culture of Shanxi Province. <
The Fen River is in Shanxi Province. The Fen River flows through 29 counties (districts) of 6 cities in Shanxi Province, including Xinzhou City, Taiyuan City, Luliang City, Jinzhong City, Linfen City and Yuncheng City, with a total length of 713 kilometers and a basin area of 39,721 square kilometers, and joins the Yellow River in Miaoqian Village, Ronghe Town, Wanrong County. The Fen River, known as "Fen" in ancient times, is a tributary of the Yellow River in Shanxi Province and is the second largest tributary of the Yellow River.
The Fen River is the largest river in Shanxi and is known as the mother river by the people of Shanxi, which has a profound impact on the history and culture of Shanxi Province.
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Wei River in Shaanxi Province. The Wei River, known as Weishui in ancient times, is the largest tributary of the Yellow River. It originates from the Bird and Mouse Mountain in Weiyuan County, Dingxi City, Gansu Province, and mainly flows through Tianshui, Gansu Province, Baoji, Xianyang, Xi'an, Weinan and other places in the Guanzhong Plain of Shaanxi Province, and joins the Yellow River in Tongguan County, Weinan City.
The average annual runoff of the Wei River is 100 million cubic meters, and that of Shaanxi is 100 million cubic meters. The regional distribution of runoff was uneven, and the general trend was to decrease from south to north, with a high in the Qinling Mountains and Guanshan Mountains, and a low in the original and valley areas. The western part is larger than the eastern part of the country, and the midstream is richer than the downstream runoff. The runoff modulus of the northern slope of the Qinling Mountains is high, which is 9 15 liters per square kilometer, while the runoff modulus in the loess plain area is only one liter second per square kilometer, and only the runoff modulus of Qianhe is higher, and the runoff modulus of Qianyang Station is higher than that of liters per square kilometer.
The runoff modulus of the main stream of the Weihe River is litres per second square kilometer, and the Weijiapu and Xianyang stations are higher, which is caused by the addition of tributaries.
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The Wei River is in Gansu Province.
The Wei River originates from Bird and Mouse Mountain in Weiyuan County, Dingxi City, Gansu Province, spans eastern Gansu and central Shaanxi, and mainly flows through Tianshui, Gansu Province, Baoji, Xianyang, Xi'an, Weinan and other places in the Guanzhong Plain of Shaanxi Province, and joins the Yellow River in Tongguan County, Weinan City. The total length of the main stream is 818 kilometers, and the total area of the basin is 134766 square kilometers.
The main tributaries of Gansu Province include Qinqi River, Daxian River, Sandu River, Yilong River, Bangsha River, Sandu River, Hulu River, Borrowing River, Niutou River, etc. There are Qingjiang River, Qingshui River, Fayu River, Stone River, Xitangyu, Heihe, Liyu River, Xinhe, Fenghe, Soohe, Bahe, Linghe, Weihe, Chishui River, Yuxian Beiluo River, etc.
The Weihe River basin is crossed by the east-west Qinling Mountains in the south, and the Liupan Mountain barrier in the north. The Weihe River Basin can be divided into two parts: the loess hilly and gully area in the west, and the Guanzhong Plain in the east.
The water conservancy undertakings in the Weihe River Basin have a long history, and in Shaanxi, there are Longshou Canal and Zhengbai Canal, and the larger ancient water conservancy projects include Chengguo Canal and Cao Canal. By the time of liberation, in addition to the Luohui Canal and Jinghui Canal, the main irrigation projects in the Guanzhong area included the Weihui Canal, the Meihui Canal, the Heihui Canal, the Fenghui Canal, and the Shuhui Canal.
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The Wei River is in Gansu Province.
The largest tributary of the Yellow River is in the central part of Shaanxi Province. The Weihe River Basin is the origin of Xuanyuan Yellow Emperor and Shennong Yan Emperor, the first ancestors of the Chinese nation. The Weihe River Basin has a complex landform, including the northern slope of the Qinling Mountains across Shaanxi and Gansu, Liupan Mountain and Longshan Mountain, and the Weihe River is an asymmetrical water system.
The tributaries of the north bank have a long history, mainly flow through the Loess Plateau, the flood and dry flow is very different, the sediment content is large, and the suspended mass is the main tributary of the Wei River. The Weihe River Basin has a continental climate, and the water volume mainly comes from the right bank tributaries, while the amount of sediment mainly comes from the left bank tributaries. The average annual runoff of the Wei River is 100 million cubic meters, and that of Shaanxi is 100 million cubic meters.
The middle and lower reaches of the channel are vertical and horizontal, from the Han to the Tang Dynasty, all of which are the main roads of Guanzhong Caoyun. "The Classic of Mountains and Seas, the East Meridian of the Sea": "Weishui comes out of the birds and mice in the same cave mountain, the east injects the river, and enters the north of Huayin."
Northern Wei Dynasty Li Daoyuan's "Water Jing Note: Weishui": "Weishui out of Shouyang County, Shouyang Mountain, Weishouting Nangu Mountain, in the northwest of Bird and Mouse Mountain, this county has Gaocheng Ridge, there is a city number Weiyuan City on the ridge, and Weishui is out of Yan. Tang Zhang's poem "Dengxianyang North Temple Tower":
Weishui comes straight to the west, and Qinshan goes deep to the south. ”
More than 3,000 years ago, when the leader of the Zhou tribe, Gu Gong's father, led the people to transform the grassy and thorny Zhou Yuan under the Qishan Mountains into a center of civilization, the river gradually became difficult to assume its function of drinking and irrigating fields.
The above content reference:
Web Links. China National Geographic Network - Weihe, the nurturer of early civilization in Northwest China.
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The Wei River is in Gansu Province. The Wei River, the largest tributary of the Yellow River, is backed by the northern foothills of the Qinling Mountains and faces the Loess Plateau. Originating from central Gansu, she travels all the way to the east, carrying the largest population in Gansu with its tributaries; Out of Gansu, the Weihe River basin is as far as the south of Ningxia, radiating the entire northern Shaanxi and Guanzhong.
More than 65 percent of Shaanxi's population and gross domestic product, as well as more than 14 million acres of fertile land, are benefited by the Wei River.
Wherever the Wei River passes, many cities are named after "Wei". From the source of Weiyuan, Tongwei County, and then to Tianshui Weinan Town, into Shaanxi Weibin District, Weinan City.
Benefits of the Wei River:
1. The landscape along the Weihe River will be laid out in accordance with the landscape layout structure of "one belt, five sections, six districts, and six nodes", in which the landscape in the river beach is planned as "six areas", that is, from west to east, there are six distinctive landscape functional areas, such as the original ecological landscape area, the leisure landscape area, the sports landscape area, and the wetland landscape area.
2. Maintain the original appearance of the river.
3. Create a "wild interest" and water-friendly landscape.
4. Highlight the theme of rest and water sports.
5. Restore native vegetation, attract wild animals to inhabit, and maintain ecological balance.
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