Xingtang County, Shijiazhuang City, Hebei Province

Xingtang County, belonging to Shijiazhuang City, Hebei Province, is located in the southwest of Hebei Province, the east foot of Taihang Mountain and the North China Plain. It is located at 38 ° 20 ˊ 34 "~ 38 ° 42 ˊ 39" n and 114 ° 09 ˊ 56 "~ 114 ° 41 ˊ 52" E. In 2010, Xingtang County covers an area of 1025 square kilometers, with 4 towns and 11 townships and a population of 450000.

On October 22, 2018, Xingtang County was selected into the list of pilot areas for the integrated development of rural primary, secondary and tertiary industries in 2018.

On May 5, 2019, the Hebei provincial government issued a notice officially approving Xingtang County to withdraw from the poverty-stricken county sequence.

From 2005 to 2010, the total GDP of the whole county reached 41.495 billion yuan in five years.

History of construction

According to the research on the unearthed cultural relics of nanwangzhuang and nanjiasu, as early as the Neolithic age, there were human beings living and working here.

Yao from the Tang Dynasty (now Dingzhou Beitang Village) went to Pingyang, namely the throne (2357 BC), southbound calendar of the place, because of the name of the Southern Tang Dynasty. Xia, Shang and Zhou belong to Bingzhou and Jizhou respectively.

In the spring and Autumn period, it belonged to Xianyu state. At the beginning of the Warring States period, it belonged to the state of Zhongshan. After Zhao exterminated Zhongshan (296 BC), it belonged to the state of Zhao.

In the 24th year of King Nan of Zhou Dynasty (291 BC), the city of Tang Dynasty was built.

In the 26th year of the first emperor of Qin Dynasty (221 BC), it was divided into 36 counties. Gezhen county was located in the southbound Tang county. It is located in today's Gujun village and belongs to Julu County. In the first year of huhai (209 BC), Wuchen was established as the king of Zhao, belonging to Zhao. In the early Western Han Dynasty, it belonged to Hengshan County of Zhao state. In Emperor Wen's time, Hengshan was changed into Changshan County, belonging to Changshan.

In the summer of 154 BC, Changshan County was changed into Zhongshan state, belonging to Zhongshan.

This is the reason of the Eastern Han Dynasty. During the Three Kingdoms period, Wei changed to the South and Tang Dynasty belonged to Changshan state. The Jin Dynasty, the later Zhao Dynasty, the former Yan Dynasty, the former Qin Dynasty and the later Yan dynasty all belong to Changshan County. The word "south" in the Northern Wei Dynasty is Xingtang County, which belongs to Hengshan County.

In the eighth year of Qi Yongming's reign (490), Tang county was changed to Tang County, and the county government was moved to Madame city (now Shicheng area of Quyang County).

In the 21th year of Taihe in the Northern Wei Dynasty (497), the county was abolished and the county administration was restored. Xiping moved to duqian City, which is now Longzhou town.

Sui, Hengshan County.

Tang, because of it. Longevity two years (693), Zhou changed to Zhangwu County. In the first year of Shenlong (705), it was renamed Xingtang County. Dali three years (768), in the Tang Dynasty set slander state, jurisdiction Lingshou, Quyang, Xingtang. Dali nine years (774), state waste, county Hengzhou. In the fourth year of Tianyou (907), it was changed into Zhangwu County.

In 923, it was renamed Xingtang County. In the first year of Tianfu in the later Jin Dynasty (936), he was transferred to Yongchang County in the Tang Dynasty. In the first year of Qianyou in the later Han Dynasty (948), it was renamed Xingtang County.

In 1941, it belonged to Baoding road.

In 1928, the road was abandoned, under the jurisdiction of Hebei Province.

In 1938, the Shanxi Chahar Hebei border region was established, belonging to the Western Hebei region. In the autumn of the same year, it was assigned to the third special region of the Western Hebei region.

In the 29th year of the Republic of China (1940), it was transferred to the five special regions of Western Hebei.

In 1945, the fourth special area of Shanxi Chahar Hebei region.

In the 35th year of the Republic of China (1946), it was changed into the third special area of Jijin district.

In the 36th year of the Republic of China (1947), it was transferred to four special districts.

In 1949, after the founding of the people's Republic of China, it belongs to Dingxian District of Hebei Province. In 1954, Dingxian district was abolished and changed to Shijiazhuang district.

In 1958, it was incorporated into Xinle county.

In 1962, Xingtang County was restored.

In 1970, Shijiazhuang area was changed to Shijiazhuang area, which was under the jurisdiction of Tang Dynasty.

administrative division

At the end of 2009, Xingtang County covers an area of 1025 square kilometers, with jurisdiction over 4 towns and 11 townships. The county government is located at 17 Yucheng street, Longzhou town.

geographical environment

Location context

Xingtang County is located in the southwest of Hebei Province, at the junction of the hilly area and North China Plain. Located at 38 ° 20 ˊ 34 "- 38 ° 42 ˊ 39" n and 114 ° 09 ˊ 56 "- 114 ° 41 ˊ 52" E, it is an irregular rectangular shape from northwest to Southeast, 53 km long and 26 km wide, covering an area of 1025 square kilometers. It faces Quyang County of Baoding city across Shahe in the East, Zhengding County and Xinle County in the south, Lingshou County in the West and Fuping County of Baoding City in the north. It is 50 kilometers away from Shijiazhuang, the capital of Hebei Province, in the South and 240 kilometers away from Beijing in the north.

landforms

Xingtang County belongs to the Taihang shallow mountain area. The terrain in the county gradually inclines from northwest to Southeast, showing a ladder distribution, which is composed of low mountains, hills and plains. The highest point is the boundary mountain between jiukouzi Township and Fuping County, 960 meters above sea level; the lowest point is beigaoli village, 75 meters above sea level, 885 meters above sea level.

1. Low mountain area

The northwest part of Tuanshan huanglonggang Qintai beichengzhai line is a low mountainous area with an area of 379 square kilometers, including all villages in shangyanzhuang Township, jiukouzi Township and some villages in kouzi town. There are 39 peaks in the area, with an altitude of 960-225m. The mountain is nearly East-West trending and gradually converges gently to the East.

2. Hilly area

The northwest part of beilonggang zhaoyangguan Shangbei nanzhaiying line is hilly area, covering an area of 224 square kilometers, including all Beihe Township, Yuting, Shangbei, Zhaiying, most of Chengzhai Township and part of Nanqiao town. There are 6 peaks in the area, with an altitude of 225-150 meters. The terrain is gentle, the soil layer is 20-50 cm, and the valley is 2-3 m deep. The soil layer is thin, the texture is sticky and heavy, and the water storage capacity is poor.

3. Plain area

The southeastern part of beilonggang zhaoyangguan Shangbei nanzhaiying line is a plain area with an area of 422 square kilometers. It is a Cenozoic quaternary alluvial fan loess plain in front of Taihang Mountain. The altitude is between 75 and 150 meters. The texture is moderate.

rivers

Xingtang County belongs to the Daqing River system of Haihe River Basin. It is adjacent to Shahe River in the East and Cihe River in the West. There are Gaohe River and Quhe River in the territory, as well as six rivers (Gullies) with a drainage area of more than 30 square kilometers: Jianghe River, huanglonggang River, egong River, kuergou River, Longmen River and miaolinggou.

Gao river is a tributary of Shahe River, which is the largest river in the territory. Originating from Xiping Fengshan and Aoyu mountain in the northwest of the county, it flows southeast through the county city, turns east to beigaoli village, and joins Shahe River in the southeast. It passes through jiukouzi, kouzi, shangshangshang, Chengzhai, Shangbei, Shitong, Xingtang Town, Zhili and Duyanggang 9 townships and 71 villages. It has a total length of 69.4km, a riverbed width of 50-350m and a drainage area of 484.9km2. There is a reservoir in the upstream. There are three large tributaries 27.6 km below the reservoir, with large river slope, narrow riverbed, exposed rocks and fast water flow; there are four tributaries 38.8 km below the reservoir, with wide riverbed and many sandy beaches. The freezing period is from December to February of the next year, which is a seasonal river. There is a lot of flood in the flood season. In 1939, the flood discharge reached 1865 cubic meters per second.

Shahe River: it was called Paihe River in ancient times. It is a seasonal river and originated at the foot of Gushan Mountain in the northeast of Fanshi County, Shanxi Province.

Quhe River: once known as Haizi river. It originated from lujiazhuang and putashi in the north of Xingtang.

Cihe: formerly known as cishui, it is the boundary river of Xingtang, Lingshou and Zhengding counties.

climate

Xingtang County is located in warm temperate semi humid monsoon climate zone. Spring, autumn and winter are mainly affected by the cold air from Siberia and Mongolia, with clear weather and sufficient light; summer is affected by the warm climate in the south, with humid air and abundant precipitation. The annual average precipitation is 450.4 mm.

In spring (March to May), the temperature is changeable, with an average daily rise of 0.32 ℃. From 1970 to 1980, the wind frequency accounted for 41.6% of the annual wind frequency, most of which were northerly gales. The average precipitation (1954-1983) is 50.4 mm.

In summer (from June to August), the temperature increased sharply, with an average of 24.6 ℃, 26.6 ℃ and 24.3 ℃ in June, July and August respectively (1970-1983). There is more southeast wind. Precipitation accounts for 66-77% of the whole year.

It is dry in early summer, and the average precipitation is only 8.8 mm. The main disasters are rainstorm, hail and dry hot wind. During the 14 years from 1970 to 1983, there were 89 rainstorms and 65 hail, 12 dry hot wind and 6 drought.

In autumn (September to November), the temperature changes rapidly, from 10 ℃ to 0 ℃, generally 32-36 days, and the temperature difference between day and night is large. The precipitation accounts for 13-18% of the whole year, and the main disasters are low temperature, rain and frost. In the 14 years from 1970 to 1983, low temperature and continuous rain occurred 35 times.

In winter (December to February of the next year), it is dry and cold with little snow. It is often attacked by cold wave and strong wind from Siberia. From December to February of the next year, the average temperature is - 2.2 ℃, - 4.8 ℃, - 1.7 ℃. The extreme minimum values are - 19.7 ℃ (December 25, 1970), - 20.7 ℃ (February 12, 1978), and the precipitation only accounts for 2-3% of the whole year.

natural resources

mineral resources

Iron ore: it is mainly magnetite. The ore body is bedded and occurs in gneiss. The ore grade is 30-40%. After beneficiation, it can reach more than 60%. The total geological reserve is 1.145 million tons. It is mainly distributed in shangyanzhuang, mijiazhuang and jiangjiayu, gaojiazhuang and sibeigou in the north of Tongkou Town, shangnanzhuang in jiukouzi Township, etc.

Silica: mainly quartzite and vein quartz. It is mainly distributed in Zhangjiazhuang and Chengzhai of Chengzhai Township, liyanzhuang and xishiqiu of Kouzhen Town, etc.

Mica (white mica, broken mica): by the national building materials geological exploration team

Chinese PinYin : He Bei Sheng Shi Jia Zhuang Shi Hang Tang Xian