Xing'an County Tourist Attractions

Xing'an is quite rich in cultural relics and monuments, there are 3 national key cultural relics protection units, 8 provincial key cultural relics protection units, county-level key cultural relics protection units 32.

National key cultural relics protection unit that is the world's oldest canal - Lingquan, provincial key cultural relics protection unit "Guibei the first male pass" Gu Yanguan, the Qin city ruins, Shimaping Han Dynasty tomb complex, Jieshou Red Army The provincial-level important cultural relics protection units are "the first majestic pass in north Gui" ancient Yan pass, Qin city ruins, Shimaping Han Dynasty tomb complex, Jieshou Red Army Hall, etc.

Folding activity, the second, the tectonic movement after the geological structure of the area finalized. The folds and rupture structures formed by the three tectonic movements are spreading regularly along the north-east direction, and the identity of the development direction of different tectonic structures at the same time reflects that the cover structure inherits the direction of the base structure and the controlling effect of the base structure on the cover structure.

Geological structure:

Xing'an County is located in the southeast edge of the western section of the Jiangnan Paleocontinent, the northern part of the Xianggui fold belt. Geological development through the pre-Devonian trough (about 2.5 to 400 million years ago), the late Paleozoic plateau (about 4 to 230 million years ago) and the Middle Cenozoic land margin activity zone (200 to 300 million years ago to the present) three stages of development. The Xing'an area has gone through three strong nature of fold and rupture movements of the Garidong, Indo-Chinese and Yanshan.

The Caledonian movement was dominated by the formation of folded tectonics, followed by rupture, accompanied by the intrusion of granite basement, and the tectonic movement led to the return of the earth trough, which ended the stage of development of the earth trough. The Indo-Chinese movement was dominated by folding and fracturing activities, which led to the formation of the terrace cover structure and the end of marine sedimentation. The Yanshan movement was dominated by fracture tectonic activity.