Qiaoxiang, Quyang

Quyangqiao township is located in the central Hebei Plain, 180 kilometers away from Beijing, 270 kilometers away from Huanghua port, 30 kilometers away from Shijiazhuang, the provincial capital, and 10 kilometers away from Shijiazhuang (Zhengding) International Civil Aviation Airport. It is subordinate to Zhengding, a famous historical city in China, and 8 kilometers away from Zhengding. Superior geographical location. Located at the junction of Zhengding County, Lingshou county and Huolu County, it has always been a must for merchants. All kinds of commodities gather here and flow to all parts of the country. Because of the shallow water level, the rich rice tastes delicious and is known as "Gongmi", which is also known as "the land of fish and rice". It is a good story that "a ladle can scoop fish and a bucket can draw water". Quyang: Take Beijing Shenzhen Expressway to the south, take Dingzhou Expressway to the west, take Dinglong highway to the west, 190km. Shijiazhuang Quyang: Take Beijing Shenzhen Expressway to the north, take Dingzhou Expressway to the west, take Dinglong highway to the west, 80 km. Baoding Quyang: (1) take national highway 107, pass Mancheng, Shunping, Wangdu and Dingzhou to Quyang, 90km. (2) Take jingzan Road, pass Shunping and Tang County, 80 km. Railway: take the train to Dingzhou station, get off and transfer to Quyang bus. Living in Quyang, Qiaoxiang, Quyang, you can not only find baijiawan Hotel (two-star) which is located by the lake, but also Quyang hotel which is clean, tidy and well served. The county can receive more than 5000 beds, including standard and standard beds. Some hotels also have senior suites, international long-distance service, etc. The warm and considerate service will satisfy you.

Qiaoxiang, Quyang

Quyangqiao town is located in the central Hebei Plain, with Taihang Mountain in the West and Hutuo River in the south. It is 180 km away from Beijing, 270 km away from Huanghua port, 30 km away from Shijiazhuang, the provincial capital, and 10 km away from Shijiazhuang (Zhengding) International Airport. It is subordinate to Zhengding, a famous historical city in China. The town is 8 km away from Zhengding. Superior geographical location. Quyangqiao town is one of the most developed and prosperous urban areas in Zhengding County, which is second only to Zhengding town. Located at the junction of Zhengding County, Lingshou county and Huolu County, it has always been a competitive place for merchants. All kinds of commodities gather here and flow to all parts of the country. Because of the shallow water level, the rich rice tastes delicious and is known as "Gongmi", which is also known as "the land of fish and rice". It is a good story that "a ladle can scoop fish and a bucket can draw water".

Quyang bridge belongs to warm temperate continental monsoon climate, with an average temperature of 15.8 ℃. The annual precipitation is 525.3 mm and the frost free period is 198 days on average. The four seasons are cold, warm, dry and wet, with more light, concentrated rainfall and frequent droughts and floods. Quyangqiao town is the best town of Fengshui in Zhengding. Wind is for transportation and water is for wealth. Quyangqiao town is in the northwest of Zhengding, which is the upwind direction of Zhengding. There are three rivers in quyangqiao town [Hutuo River, Zhouhe River and Hanhe River], and they are the birthplaces of two rivers [Zhouhe River and Hanhe River]. Zhouhe river originates from Zhoujiazhuang village in the town, and Hanhe river originates from Xihan village in the town. And Shijiazhuang's mother river Hutuo River transit. The town of Quyang bridge is really a treasure place to attract wind and gather water.

Evolution of organizational system

The town is located in Quyang bridge (1.5km to the north of the village), so it is named Quyang bridge town. Quyang bridge was originally the seat of the district and township government.

After the establishment of the people's commune in 1958, it was the site of Quyang bridge management area.

In 1961, the scale of the commune was adjusted and the management of Quyang bridge was divided into a commune,

On January 16, 1984, it was changed from commune to market town of Qiaoxiang, Quyang.

In December 1995, hanjialou township was incorporated into the city

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administrative division

It has jurisdiction over Quyang, Xikou village, Quyang bridge, dongquyang, nanquyang, Xixinzhuang village, Zhoujiazhuang village, donglizhai village

There are 20 village committees in xilizhai village, Hu Village, hanjialou village, Gaoping Village, qiantadi village, houtadi village, beibaidian village, nanbaidian village, Shaotong village, Xihan village, Donghan village and Xihe village.

Regional location

Quyangqiao town is located in the central Hebei Plain, with Taihang Mountain in the West and Hutuo River in the south. It is 180 km away from Beijing, 270 km away from Huanghua port, 30 km away from Shijiazhuang, the provincial capital, and 10 km away from Shijiazhuang Zhengding International Airport. It is subordinate to Zhengding, a famous historical city in China. The town is 8 km away from Zhengding City, with superior geographical location.

topographic features

1、 Geology

Quyangqiao town is located in the east of Taihang mountain uplift belt and the edge of Jizhong depression. In ancient times, the Hebei area where Quyang bridge is located was a sinking area, which was once a vast sea. Later, after the Fuping movement, Wutai movement and Luliang movement, the rocks were deposited in the ocean for a long time. These rocks not only produce fold faults, but also become ancient metamorphic rocks. Affected by the Caledonian movement between Silurian and Devonian in Paleozoic, this area is higher than the sea level. After about 100 million years, this area not only did not deposit, but also denuded all the Ordovician and Silurian strata. After the Variscan movement at the end of Permian, the area rose to land. Since the Mesozoic Jurassic Yanshanian movement, regional large faults have occurred along the edge of the plain, and synclinal basins have been formed in the part of the plain. At the end of the Cretaceous, the Yanshan movement ended, and the geomorphic outline of this area was roughly shaped. Since the Himalayan movement, the North China Plain has entered a relatively sinking stage, accompanied by rhythmic ascending and descending movements. From the tertiary to the early Quaternary, thick red rock series of fluvial and lacustrine facies were deposited in the plain area. Since the Quaternary, it has continued to decline and deposited thick loose sediments. This is the general process of crustal change in Quyang bridge and North China.

The loose sediments of Quaternary strata are about 450 meters thick in Zhengding County. The lower part is a set of purple red semi cemented strata of tertiary with unknown thickness. In the west of Yong'an village, no underlying bedrock is found.

The geotectonic position of quyangqiao area belongs to the North China fault depression in the middle Huaihe area. According to the analysis of geomechanics, the Taihang mountain area where the belt is located belongs to the Neocathaysian tectonic system.

The genetic types of land in the county are mainly clay and sandy soil formed by alluvial or siltation of riverbed facies. The soil layer less than 2 meters above the surface is generally compacted for a long time with good structure, and the shaft wall and slope sill are upright without collapse. Due to the different types of soil, its physical and mechanical properties are not consistent.

According to the experimental results, the bearing capacity of various types of foundation exposed on the surface is calculated and analyzed as follows: sand soil is generally between 14-24 T / m2, and sub sand soil is between 13-20 T / m2. The bearing capacity of the above natural foundation is generally more than 12 T / m2, which is suitable for general civil and industrial buildings.

2、 Geomorphology

Quyangqiao town is located in the eastern foot of Taihang Mountain, the middle and upper part of the piedmont alluvial fan, which is a Piedmont inclined plain. In the early glacial period of Dali 40000 years ago, the climate was cold and dry, with small precipitation and large precipitation variability. The river type is wide and shallow braided and straight, the river rises and falls suddenly, the flow is large, the flow rate is fast, and the river is easy to change. In the early stage, the river was mainly eroded to form erosion Valley, and then quickly accumulated to form piedmont alluvial fan composed of sand and gravel.

The Dali interglacial stage, which is 40000-25000 years ago, is a river interpenetrating between dahuapo. Although the climate of Dali main glacial stage, which is 25000-11000 years ago, became cold and dry, the river type was braided, the river rose and fell suddenly, and the flow rate was large and the flow rate was fast. The river course changes easily. In the early stage, deep erosion dominated, forming erosion surface and cutting Valley, and then rapid accumulation, forming a alluvial fan dominated by sand and gravel. In the later stage, the climate was drier, fluvial facies deposition played a secondary role, and aeolian deposition played an important role, covering a layer of loess on the sand and gravel.

During the early Holocene from 11000 to 75000000 years ago, the climate was mild and slightly wet, and the river type was still braided, but gradually came into a main channel. The river flow rate was large and the flow rate was rapid. In the early stage, it was mainly eroded and cut, and then mainly accumulated.

During the middle Holocene (7500-3000 years ago), the climate was warm and humid. The river was a curved or slightly curved river type dominated by suspended load sand transport. The flow rate was small, the river was stable, the sediment content was small, and there was medium and fine sand accumulation in the riverbed. In the middle Holocene, the river was active for a time, and began to be mainly eroded, forming an erosion surface, and then deposited silt with peat Sandy paleochannel, with thin thickness and small grain size, soon ended its active period and continued to accumulate in fluvial and lacustrine facies.

In the late Holocene since 3000 years ago, the climate was cool and dry, the variation rate of river flow increased, and the vitality began to strengthen. The river pattern gradually restored to braid. In the early stage, erosion was still the main cutting, and a terrace was formed in the valley cut by the alluvial fan. With the climate becoming colder and drier, the river pattern gradually changes from curved to straight or braided to straight, the sand carrying capacity of the river increases, the flow rate increases, and the change of diversion becomes more frequent. Therefore, the river accumulation landforms and the river differential accumulation landforms are formed under the alluvial fan.

Nowadays, the terrain of quyangqiao town is flat, the general trend is high in the north and low in the south, inclined from northwest to Southeast. The altitude is between 60-90 meters, and the natural gradient is 2%. The large landform of the town is relatively single, and the micro landform in some sections is relatively prominent. The town is divided into two parts by Zhouhan river. On both sides of the Hutuo River, there are scarps which are roughly the same as the flow direction of the river, generally 1 to 5 meters above the ground, and the highest is about 30 meters. These scarps are the second terrace of Hutuo River. On the north side of the river is Quyang, the steep ridge of Quyang bridge.

3、 Hydrology

（1） River quyangqiao town belongs to Haihe River Basin. There are Hutuo River and Zhouhan River in its territory, and lingzheng main canal in its north. In addition, according to historical records, history

Chinese PinYin : Qu Yang Qiao Xiang