Pingyuan County, located in the northwest of Shandong Province, is a county on the Yellow River Plain, with a total area of 1.047 square kilometers and a population of about 447,000. The county seat is strategically located, with Mount Tai in the south and Beijing and Tianjin in the north. It is 2280km away from Tianjin Port, 0 km away from Huanghua Port 1 10km away from Jinan Yao Qiang Airport, and Pingyuan County is a plain. Beijing-shanghai railway-Beijing-Fuzhou Expressway runs through the north and south of the county, and Pingyuan Railway Station has 17 passenger and freight stops here every day, with an annual throughput of 500,000 tons.
Pingyuan County has a temperate monsoon climate with four distinct seasons and a pleasant climate. There are 7 towns, 3 townships, 2 sub-district offices, Longmen Economic and Technological Development Zone and 876 administrative villages in the county. Pingyuan County is an agricultural county, the main crops are wheat, corn, cotton and vegetables, among which the vegetable planting area is large and it is one of the important vegetable production bases in Shandong Province.
Geological environment of Pingyuan county
Pingyuan county is located in the golden zone of Beijing-Tianjin economic metropolis circle and Bohai economic circle, with Mount Tai in the south, Beijing-Tianjin in the north and 30 kilometers away from Dezhou City. It is 39 kilometers long from north to south and 48 kilometers wide from east to west, with a total area of 1047 square kilometers. Pingyuan county is located in the primary and secondary tectonic units of the earth and belongs to a part of Liaoning-Hebei-Taiwan syncline in North China. On the secondary structural unit, it is roughly zoned from the vicinity of Liutun Village in Tangsan Township to Fangsi Village in Fangsi Town, Yucheng City.
Its west is Aoduan District of Linqing City, and its east is Aoduan District of Jiyang District of Jinan City. The triangle extending from Liutun village to the northeast belongs to Chengning uplift area. There are faults between districts. Some of these faults have been cut into the lower strata of Neogene, some have cut the boundary between Tertiary and Quaternary, and some have Cenozoic basalts along the faults. For example, Tertiary basalts exist in the northeast faults passing through Wang Miao Town, Qiancao Town and Wangfenglou Town, and in the south of Encheng Town and Wangdagua Town.
The above contents refer to Baidu Encyclopedia-Pingyuan County.