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Xun County is located in the south of Henan Province, with a long history and profound cultural background. There are many tourist attractions here, which make people linger. Next, the author will introduce several scenic spots worth visiting.
Hongyunyan Scenic Area, located on the north bank of Huaihe River, is one of the four famous mountains in Henan Province. In the scenic area, the mountains are steep, the peaks are overlapping, the stone walls are steep, the ancient trees are towering, and the ravines are criss-crossing, which has unique natural scenery. In addition, there are many temples and historical sites such as Haifeng Temple, Beidou Pavilion and Bizhenyan in the scenic area, which allow visitors to appreciate the profoundness of Buddhist culture.
Zhoukoudian Tourist Area is located in the southeast of Xun County, with rich cultural relics. Here, visitors can visit the "Peking Man" site, Zhoukoudian stone factory, dragon fossils and so on. Understand the living conditions of early human beings and explore the evolution of human civilization.
Liyang County was established during the reign of Emperor Gaozu of the Western Han Dynasty and was subordinate to Wei County of Jizhou. This is the beginning of the establishment of Xunxian County, which is located in the northeast of Daishan Mountain. 1986 65438+1October 18 the State Council approved the transfer of Xun County to Hebi City. As of June, 2020, Xun County has jurisdiction over 4 streets and 7 towns, and the county people's government is located at No.62 Liyang Road.
There are no Archean and Ordovician outcrops in Xunxian County. CAMBRIAN is scattered in Xunxian hilly area, including Upper CAMBRIAN and Middle CAMBRIAN. Tertiary is distributed intermittently in the western part of China, showing Paleogene and Pliocene Hebi Formation. 83% of the territory is covered by Quaternary strata.
Xunxian county spans two structural units, Neihuang Uplift and Tangyin Graben, with east-west fault structure and northeast fault structure. According to its lithology, underground hydrology can be divided into tertiary sandstone fissure pore water-bearing strata and quaternary gravel pore water-bearing strata. Magmatic rocks are not developed in the area, and Yanshanian intrusive rocks are exposed sporadically.