Traditional Culture Encyclopedia - Weather forecast - Which city in Henan does Fugou County belong to?
Which city in Henan does Fugou County belong to?
Fugou County belongs to Zhoukou City, Henan Province, and is located in the eastern plain of Henan Province. Fugou County is located in the eastern plain of Henan Province, which belongs to Zhoukou City, Henan Province, at the junction of Zhoukou, Xuchang and Kaifeng, and is located in the one-hour economic circle of Zhengzhou.
County-wide jurisdiction: Cuiqiao Town, Jiangcun Town, Baitan Town, Cao Li Township, Jiuyuan Town, Chaigang Township, Gucheng Town, Liansi Town, Biangang Town, Daxin Town, Lvtan Township, Baotun Town, Dalizhuang Township, Suburb Township, Futing Sub-district Office, Qiu Tong Sub-district Office, 16 townships and sub-district offices.
Daguang Expressway, Luo Yan Expressway and Luoan Expressway meet in China; Zhenghe high-speed rail transit, sanyo railway and Huangpu railways are under planning and construction, initially forming a large traffic pattern of "three high-speed rail transit and three railways extending in all directions".
Fugou was called Qiu Tong in ancient times. Because there was a pavilion in the east and a ditch in the west, it was changed to Fugou. County area 1 173 square kilometers, cultivated land 1 1400 mu, population 770,000. It has a warm temperate continental monsoon climate, with an annual average temperature of 14.4℃, annual precipitation of 6 1 1.4 mm and a frost-free period of 2 15 days.
topography
The geological foundation of Fugou County is the eastward expansion and downward inclination of the Qinling banded structural belt and Songshan fold belt, which is located in the middle of Tongxu Uplift and Zhoukou Depression. After Yanshan movement, it was uplifted for a long time and deposited only in the Late Tertiary. The upper tertiary to quaternary strata are 900-1200m thick. Hydrogeological exploration borehole records show that within 400 meters near the surface, all of them are loose deposits.
Fugou is located in the alluvial plain of the Yellow River, with a flat terrain, slightly inclined from northwest to southeast, with an altitude of 50-72 meters and an average surface slope of 1/6000. The ancient alluvial plain of the Yellow River has been cut by many floods, and many north-south residual hills have been formed on the plain.
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