What is the source and end point of the Fuyang River, and what is the source and end point of the Hu

The Fuyang River originates from the eastern foot of Taihang Mountain and the southern foot of Fushan in the Fengfeng Mining Area of Handan, and ends at the confluence of Xian County and Hutuo River in Cangzhou, which is called Ziya River. Fuyang River, belonging to the Ziya River system of the Haihe River Basin, flows through Handan, Xingtai, Hengshui and other areas, with a total length of about 413 kilometers. It is the backbone river of flood control, irrigation, drainage, navigation and other comprehensive utilization.

Where is the source of the Fuyang River?

Fuyang River, known as Fushui in ancient times, originates in Zhangdefu Mountain, flows through Cixian, Handan, Yongnian, Pingxiang, Julu, and then flows into Xingtai Daluze. The original concept referred to a stretch of river from the source to Oruzawa, which then dried up. After dredging the river, according to the contemporary river concept, the Fuyang River will be extended and connected.

Its source is located in the Fengfeng mining area and Jincun. There is also a theory that it originates from the Black Dragon Cave, which is divided into two layers, the upper cave is large and the lower cave is small. The hole underneath is blocked by vegetation and is not easy to see. Visitors can only find the hole below by looking at the hole above.

In addition, there are many tributaries of Fuyang River, located on the windward slope of Taihang Mountain, with short source, steep slope, rapid flow, large flood peak, large flow, and small river flow. The main rivers are Niu River, Hezhu River, Qin River, Suiyuan River, Zhangzhi River Spillway and Liu Lei River. Among them, the artificial river is the floodway of the Zhangzhi River and the Liu Lei River.

The flood storage and detention areas include the Huangliangmeng flood storage and detention area and the Yongnian depression flood storage and detention area.

The source of the Fuyang River is the southern foot of the Fushan Mountain in the Handan Fengfeng Mining Area at the eastern foot of Taihang Mountain, and the end point is the confluence of Xianxian County and the Hutuo River in the Cangzhou region, which is called the "Ziya River". Fuyang River, belonging to the Ziya River system of the Haihe River Basin, flows through Handan, Xingtai, Hengshui and other areas, with a total length of about 413 kilometers, is a backbone river for flood control, irrigation, drainage, navigation and other comprehensive utilization.

Where is the source of the Fuyang River?

Fuyang River, the ancient name of Fushui, originated in the Fushan of Ci County, Zhangde Prefecture, flows through Ci County, Handan, Yongnian, Pingxiang, Julu, and joins the Xingtai Continent, the original concept refers to a section of the river from the source to the Mainland, and later the Continent dries up, through the dredging of the river, and according to the contemporary river concept, the Fuyang River channel can be extended to an important river flowing through Handan, Xingtai, Hengshui.

Its source is located in the Fengfeng mining area and the village town of Jincun. There is also a saying that it originated from the Black Dragon Cave, and the Black Dragon Cave is divided into two layers, the upper hole is large, and the lower hole is small. The lower hole is blocked by grass and trees, it is not easy to see, and visitors generally look at the upper hole to find the lower hole.

In addition, there are many tributaries of Fuyang River, which are located on the windward slope of Taihang Mountain, with short sources, steep slopes, rapid flows, large flood peaks, and large river discharges. The main ones in Handan are the Yakniu River, the Zhu River, the Qin River, the Yuan River, the Zhizhang River Floodway, and the Liulei River. Among them, the artificial river channels are the Zhizhang River Floodway and the Liulei River.

The flood detention area projects include Huangliang Dream Flood Detention Area and Yongnian Depression Flood Detention Area.

The source of the Hutuo River is the area of Mapaoquan and Qiaoergou in Hengjian Township, Fanzhi County, North Plateau, Shanxi Province; The end point is in the northwest of Xian County, and it joins the Fuyang River from the south.

The Hutuo River is a large tributary of the Ziya River system in the Haihe River Basin. It originated from Mapaoquan and Qiaoergou in Hengjian Township, Fanzhi County, North Plateau, Shanxi Province. Fanzhi, Daixian, Xinzhou, Yuanping, Dingxiang, Wutai and Yuxian flow through Shanxi Province out of Shanxi Province, with a basin area of 11,936 square kilometers and a length of kilometers.

The Hutuo River flows into Pingshan County in Shijiazhuang area through Houjiao, passes through Lu, Lingshou, Zhengding, Gaocheng, Wuji, Jinzhou, and exits Zaoying in Shenze County, and then flows through Anping, Raoyang, Wuqiang, and Zhixian County Laohekou hub and Fuyang New River after confluence with the Ziya River.

History. The Shijiazhuang area, through which the Hutuo River flows, is an area where human civilization was developed earlier and has a very profound cultural heritage. As early as about 10,000 to 300,000 years ago, in the early, middle and late Paleolithic periods, human beings flourished in the Hutuo River basin in the Taihang Mountains.

Historically, the Hutuo River has had many different names. The "Classic of Mountains and Seas" is called Huchi, the "Book of Rites" is called the Evil Pond, the "Zhou Ji" is called Huchi and Huchi, the "Hejaz" is called Hutuo, the "Historical Records" is called Hutahe is also called Yatuo, and the "Notes on the Water Classic" is called Hutuo. The Hutuo River protrudes into the plain from the east of the Shanxi Plateau, with steep longitudinal slopes and turbulent currents, and often floods.

Therefore, in history, it is called the evil pool, the pond, and the pond, all of which mean that the water flow is fierce and fierce. The Hutuo River was called at least in the Han Dynasty. The Hutuo River originated in Shanxi and returned to Hebei, with turbulent water, sparse soil and good collapse, impermanence and unstable migration.

Although the upper reaches are dreviated, they are often silted. Walking through canyons in mountainous areas, confined to the terrain, rarely changing; Frequent diversions into the flat principle.

The source of the Fuyang River is the Great Wall Ridge of the Taihang Mountains and ends at Baiyangdian Lake on the Northern Plain of China. Here's a detailed introduction:

The Fuyang River originates from the Great Wall Ridge of the Taihang Mountains, and its main tributaries include Qingquan River, Luya River, Heigou River, etc. Due to the rugged terrain of the area, the water along the Fuyang River is relatively rapid, creating a series of waterfalls, canyons and cliffs, and the scenery is spectacular. As the river flows eastward, the Fuyang River passes through many cities and regions such as Zhangjiakou, Baoding, and Xingtai, and gradually enters the northern plain of China.

Here, the geomorphological features of the Fuyang River basin gradually become gentle, and the rivers become calmer.

The Fuyang River flows into Baiyangdian Lake on the plains of northern China. Baiyangdian Lake is one of the famous natural lake lakes in North China and an important wetland resource in the Fuyang River Basin. Here, the flow of the Fuyang River gradually becomes smoother, forming an attractive water town scenery.

At the same time, Baiyangdian is also an important fishery, aquaculture and group tourism base in North China.

The natural environment of the Fuyang River Basin is very rich and diverse. With a high forest cover and a wide variety of flora and fauna, it is a habitat and protected area for rare and endangered species. At the same time, the water resources of the Fuyang River Basin are also very abundant, and it has an important position in the whole of North China.

Due to the geographical location and the particularity of the climate and environment of the Fuyang River Basin, the water resources here are widely used in agricultural pure oranges, industrial and urban domestic water, etc.

However, with the continuous increase of human activities, the ecological environment of the Fuyang River Basin has been gradually destroyed. For example, a large number of development, construction, sewage and overfishing have all had a serious impact on the ecological environment of the Fuyang River Basin. In order to reverse this situation, the relevant authorities have taken a series of measures to protect the ecological environment of the Fuyang River basin, including strengthening environmental monitoring, establishing pollution prevention and control systems, restoring wetlands and planting trees.

In short, the Fuyang River is an important river in northern China, with its source in the Taihang Mountains and its end in Baiyangdian. The river runs through several cities and regions, and is blessed with abundant natural resources and a unique ecological environment. In order to protect the ecological environment and water resources of the Fuyang River Basin, we need to strengthen the awareness of environmental protection and take effective measures to jointly maintain this precious natural resource.

The source of the Hutuo River is the area of Mapaoquan and Qiaoergou in Taixi Mountain, Hengjian Township, Fanzhi County, North Plateau of Shanxi Province, and ends in the northwest of Xian County, where it joins the Fuyang River from the south.

Hutuo River is a river in the central part of Hebei Province, originating in the Taihang Mountains, the source is located in the Taixi Mountain, Fanzhi County, Xinzhou, Shanxi, passing through the middle of the continuous peaks of the Taihang Mountains, after entering Hebei Province, the river water resources converge to the Gangnan Reservoir and the Huangbizhuang Reservoir in Pingshan County, the river after the reservoir flows through the north of Shijiazhuang, all the way to the east and the Fuyang River converges into the Ziya River, and finally joins the Haihe River in Tianjin, and flows into the Bohai Sea.

Overview of Hutuo River:

The Hutuo River originates in Taixi Mountain, Fanzhi County, enters the territory of Yuanping from Dai County, and flows through 56 villages in 8 townships and towns such as Yangou, Sulongkou, Laoyang, Xizhen, Zhongyang, Zigan, Xinyuan and Wangjiazhuang, with a total length of kilometers in the territory.

The main tributaries are Yangwu River, Beiyunzhong River, Changle River, Yongxing River, Tonghe River, etc., and the smaller tributaries are Banqiao River, Wangdong River, Xiaoyi River, Shisi River, Beiqiao River, Nanqiao River, Shahe River, Beigang River, Groove River, Longwangtang River and other 29 rivers.

There are 2,703 small water conservancy projects in the Hutuo River Basin in Yuanping, including 16 reservoirs, 30 pond dams, 85 sluices and 53 pumping stations. There are 43 small artesian irrigation areas and 13 undercurrent interceptions.

The area of shelterbelts on both sides of the bank is hectares, the area of special purpose forests is hectares, the area of economic forests is 326 hectares, the area of charcoal forests is hectares, and the area of timber forests is hectares. In the area of woodland on both sides of the Hutuo River, the area of arbors is hectares.