Needless to say, the direction of the Yellow River is north-south.
Fenhe River originates from the jellyfish cave at the foot of Guancen Mountain in Dongzhai Town, ningwu county, Xinzhou, and the surrounding longan springs and strange rocks of Zhiguo flow through six villages including Dongzhai, Sanmaying, Gongjiazhuang, Ermaying, Toumaying, Huabei Tun, Shanzhai, Beitun, Kuaiguan, Ninghua, Bamen, Nantun, Zizi Temple and Chuanhutun, and then through Ningwu. There is a square pond of 25 square meters at the exit. The water is crystal clear and deep. The pool water gushed out from the underground tunnel cut by stones and flowed into a wide river. Above Longkou, there is the stone carving of "Fenyuan Zhao Ling", the source of Fenhe River, which is known as "the root of Jin land". It is said that in the past, the water flow in Fenyuan was very large, and the wood cut from Guancen Mountain was transported by the water in Fenyuan. Even in the forties and fifties of this century, wood can still be unloaded. Nowadays, due to various reasons, the amount of water is greatly reduced, and the incoming water from Fenyuan is only 0.2 seconds/cubic meter, which restricts the development of industry and agriculture and is in urgent need of protection.
Hutuo River originates from Gushan Village, Taixi Mountain, Fan Shi, Xinzhou, Shanxi Province, flows southwest between Hengshan Mountain and Wutai Mountain, eastward to Jiehe River, passes through Zhoushan and Taihang Mountain, eastward to Zangqiao, xian county, Hebei Province, and joins Fuyang River, another tributary of Ziya River. It has a total length of 587 kilometers and a drainage area of 27,300 square kilometers. The main tributaries are Wu Yang River, Yunzhong River, Muma River, Qingshui River, Nanping River and Yehe River. Feather arrangement, mainly concentrated above Huangbizhuang, with no tributaries below. The land potential in the basin is stepped from west to east, and the west is located in the mountains and basins on the eastern edge of Shanxi Plateau, with high terrain and thick loess distribution. The central part is a mountain range formed by Taihang anticline, which is rich in coal mines; The east is a plain. Natural vegetation is scarce in the basin, and soil erosion is serious. The area flowing through mountains, mountains and hills accounts for about 86% of the total basin area, and the total river drop is more than 1800 meters. Above Yaochi, it is upstream and flows southwest along Wutai Mountain in a banded basin. The width of the river varies from 100 m to 1000 m, and the water flow is slow. Yaochi to Gangnan is the middle reaches, flowing through Taihang Mountain area. The valley is deep, V-shaped, with a width of less than 200 meters, a big drop and a fast current. Below Huangbizhuang is the downstream, which flows through the plain. The river is very wide, with a maximum width of 6000 meters. The water flow is slow and the sediment is deposited, and it gradually becomes an overground river or a semi-overground river, with dikes built on both sides. The basin has a temperate continental monsoon climate, and the temperature decreases with the elevation of the terrain from east to west. The annual precipitation is 400 ~ 700 mm, which is concentrated in summer. Surface runoff is mainly replenished by rainfall. The average annual runoff is about 2.2 billion cubic meters, which is unevenly distributed. The runoff at the eastern foot of Taihang Mountain is larger, and it decreases as it goes upstream. The annual distribution of runoff is also uneven and varies greatly during the year. The amount of water in rainy years is 10 times that in dry years. The flood peak caused by heavy rain is high and steep, mainly from the main stream and Yehe River, which mostly occurs in July and August. Sediment concentration 1 1.4 kg/m3, with an annual sediment discharge of 2,920 tons. There are large and medium-sized reservoirs such as Gangnan, Huangbizhuang (see Gangnan Reservoir and Huangbizhuang Water Control Project), Gushan, Xiaruyue, Guanguan, Shuangrushan, Shiban, Xiaguan, Dashimen and Guo Zhuang 10, and there are many small reservoirs and ponds. The flood disaster has been basically controlled, and the benefits of irrigation and power generation are remarkable. The basin is rich in mineral resources, especially coal. There are also economically developed cities such as Shijiazhuang and Yangquan. Xibaipo (see Pingshan County), Cangyan Mountain Scenic Area and longxing temple can all go. Hutuo River has many different historical names. The Book of Rites is called evil pool or fire pool. Zhou Li is called the back pool. During the Warring States Period, it was called Lunshui (Hu Chi Water). Qin called Houchi River. The Eastern Han Dynasty called Hutuo River. Historical records call it running, also known as Yalun. It is said that Zhu is human. Cao Wei called Tuohe River. The Western Jin Dynasty was called Hutuo River. The Northern Wei Dynasty was renamed Qingninghe River.
Sanggan River is an important tributary of Haihe River, and there are two rivers in its upper reaches: Hezi River and Hui River. The main stream Hui River originates from Fenshuiling Village, Guancenshan, Ningwu County, Xinzhou, Shanxi Province, and Zi Yuan originates from Jiekou Mountain, Zuoyun County, Shanxi Province. These two rivers are called Sanggan River only after they meet in Shuo County and Yi Village. Sanggan River flows through Shuoxian, Yin Shan, Yingxian, Huairen, Datong and Weijiabao villages in Yanggao County and enters Hebei Province. The total length of Sanggan River in Shanxi is 252km, and the drainage area is17142km2. The main tributaries of Sanggan River are Huangshui River, Hunhe River and Yu He. Sanggan River is also an ancient river in Saibei, which flows through Yangyuan, Yuxian and Zhuolu in Zhangjiakou from west to east.
Muma River is a tributary of Hutuo River, which originates from the foot of Wutai Mountain, a famous Buddhist holy place, flows through Wutai, Beihu, Fan Shi and other counties, flows through the south of Xinzhou City, and tends to be flat when it reaches Xinzhou. The geographical position of high in the east and low in the west makes the river sand rolled by the Muma River go down all the way, and when it reaches the Ding Xin Plain, it begins to precipitate and accumulate over time, forming a thick sandy land. The water of Muma River is very clear, which originates from the good natural ecological environment of Wutai Mountain. Due to the construction of reservoirs in the upper reaches, the surface water in Shanxi has dropped seriously, and the lower reaches of Muma River have dried up.
Rivers in the clouds pass through the northern part of Xinzhou, Boming and other towns and join the Hutuo River, which is also a tributary of the Hutuo River.
Qingshui River originates from Xiazi Valley and Dongtai Valley in Wutai Mountain, flows through Jingangku, Shizui, Gengzhen, Shipenkou and Hu Jiazhuang, and joins the Hutuo River in Pingping. The total length is 104 km, the river width is 50-100 m, the water width is 5 m at ordinary times, the water depth is 0.5 m, the flow rate is 1.2 m per second, and the annual runoff is 255 million cubic meters. The flood season is from July to September, and there are 3 to 7 major floods every year, each lasting 5 to 7 days. The water surface is wide120m, the water depth is 2.5m, the flow rate is 2.5m per second, and the maximum flood peak in a hundred years is 2800m3 per second. The riverbed is steep, full of gravel, backed by mountains on both banks, and the lower reaches are mostly broken ridges and steep cliffs. The ice age is1February to March of the following year, and the ice thickness is 0.7 meters. In spring and autumn, most river beds are cut off, and water can be diverted for irrigation in summer. There are five bridges on the river: Threshold Stone Bridge, Gengzhen Bridge, Gaohongkou Bridge, Hekou Bridge and Gengjiazhuang Bridge.
Linxi River, also known as Minghe River, originated from Lingdi Village in Yangling South, with a total length of 30 kilometers. The riverbed is 50 to 100 meters wide, the water is 3 meters wide and 0.3 meters deep, the flow rate is 0.3 meters per second, and the total runoff is 2/kloc-0.0 million cubic meters. To the south of Taicheng, there are seasonal rivers such as Chengxigou, Dadaogou and Wang Jiagou, which flow through Dong Lei, Wangxiao, Taicheng and Liujiazhuang and join Qingshui River at Huamuping.
Xiaoyang River originates from Xiaobai Village, and borders Lingjie River with Xiaobeigou, Zhicungou, Chechanggou, Weidigou, Dongguigou and other streams. Arriving at Xiaodou Village18km, it is a low-water riverbed, and there is no water until the rainy season. The riverbed is wide, generally more than 500 meters. From the riverside to Xiaodou Village, there was water at first. On the small south slope, there was the intersection of Liuyuangou and Heilongchigou, which flowed into Qingshui River at the estuary through Xixia and Dianjun. The total length is 20 kilometers, the river is 30-50 meters wide, the water is 4 meters wide and 0.4 meters deep at ordinary times, the flow rate is 0.4 meters per second, the annual total runoff is 56.27 million cubic meters, the water is 80 meters wide and 0.9 meters deep in flood season, and the flow rate is l. l meters per second. The sand bed above the canyon is flat, and the flood season is mostly in the third quarter.
This small galaxy, which originated in Diantou Village, reached the intersection of probe and Sangyuangou, reached the intersection of Shanwen and Jinshangou, and reached the place 500 meters south of Bai Yang, namely Guojiazhuang, which is out of the water, with Lingjie River in the north. After Guojiazhuang, Guojiazhai, Beidaxing, to the south of Huaiyin Village, it flows into the Hutuo River. The total length is 30 kilometers, the water width is 15 meters, the depth is 0.2 meters, the flow rate is 0.3 meters per second, and the annual total runoff is 1774 cubic meters. The flood season lasts for three to six hours from July to September. Irrigation along the banks of the river has a long history, and there is a small river diversion bridge in Huaiyin.
You can go to Baidu Encyclopedia, which has the names of every river. If you have both, you won't post them.