The best place for a one-day tour in Du 'an.

The best place for a one-day tour in Du 'an: An Fu Temple in Du 'an.

Du 'an Anfu Temple is located in a small county in the southwest of China. Surrounded by mountains, the Lotus Pagoda is formed, and the three islands of Gu Song Island, which represent the three treasures of Buddhist monks, sit in it, just like a unique Buddhist country. Every spring and summer, the underground river overflows, and Gu Song Island is like a golden tile floating on the water. This is a miraculous sight. When the mainland falls, the water is rising. Everyone calls it a floating island. The island is spotless, noisy and quiet, just like a fairy island.

Du 'an Yao Autonomous County belongs to Hechi City, Guangxi Zhuang Autonomous Region, which is located on the transition slope from Yunnan-Guizhou Plateau to Guangxi Basin, in the east of Duyang Mountain. The terrain is high in the northwest and low in the southeast. It is one of the most typical karst landform areas in China. The county is famous for its peculiar peaks and caves and karst landforms. With a total area of 4095 square kilometers, it governs 10 towns, 9 townships and 248 villagers' committees. County People's Government is located in Anyang Town, 20 kilometers away from Nanning City and Hechi City/kloc-0.

geologic structure

The geological structural unit where Du 'an is located is Duyangshan Uplift in the east of Youjiang Reconstruction Geosyncline, adjacent to Laibin Fault Fold Belt in the middle of Gui Zhong Depression in the east, Damingshan Uplift Belt in the northwest, Jingxi-Tiandong Uplift Belt in the south and Xilin-Baise Fault Fold Belt in the west of Guixi Depression in the west. The geological structure system where Du 'an is located is the middle part of the Shanxi wing of Guangxi, and the folds and faults are distributed in the northwest direction, all over the country. The principal compressive stress is northeast-southwest, and the compressive structure is

The strata in China are exposed from Middle Devonian in Upper Paleozoic to Quaternary in Cenozoic, except Jurassic strata in the middle. Carboniferous and Permian strata are the most widely distributed, with a total thickness of 75 10/0m. Among them, the Middle Devonian to Upper Permian is a set of continuous shallow-sea carbonate rocks with a thickness of 5,300m, accounting for 70% of the total thickness of sedimentary rocks, and its distribution accounts for 965,438 of the total area of the county.

Reference to the above content: Baidu Encyclopedia-Du 'an