Where is Xiangxian?

Elephant County is in Laibin City, Guangxi Zhuang Autonomous Region.

Xiangzhou County belongs to Laibin City, Guangxi Zhuang Autonomous Region. Located in central Guangxi, at the west foot of Dayao Mountain, it is connected to Xingbin District in the west, wuxuan county in the south, Jinxiu Yao Autonomous County in the east and Luzhai County and Liujiang District in Liuzhou City in the north. The total administrative area of Xiangzhou County 1898 square kilometers. By the end of 2065, 438+04 will have jurisdiction over 8 towns and 3 townships.

According to the data of the seventh census, as of 0: 00 1 1 in June 2020, the resident population of Xiangzhou County was 28 1846. Xiangzhou County is the hometown of Zheng Xianfu, a "Lingnan wizard" in Qing Dynasty, a "Guangdong master", Liao, a contemporary cartoonist in the world, and the former chairman of the government of Guangxi Zhuang Autonomous Region.

It has successively won the honorary titles of national advanced grain production county, national advanced unit in establishing activities in counties (cities, districts) ruled by law, national advanced area in the work of "two basics" and "hometown of longevity in China". 2065438+On February 2, 2009, it was rated as an advanced unit of traditional Chinese medicine at the county level by state administration of traditional chinese medicine.

Geographical environment of Xiang County:

Xiangzhou County is located in the inner side of the east wing of the front arc of "Guangxi Mountain Structure" mentioned by Li Siguang, and in the west of anticlinorium of Dayaoshan. The direction of the tectonic line is almost north-south, and it is partially offset to the east or west. The area around Crystal Temple Village is northwest; Dale-Baizhang in the east and Maping-Shilong in the west are NNE. The folds in the county are simple and the faults are well developed.

The folds are mostly short-axis anticlines and synclines, and there are interlaminar flexures or folds locally. There are more than 20 large and small faults, most of which belong to high-angle thrust faults, normal faults or gentle inference layers. All folds and most faults were formed by Indosinian movement. Xiangzhou-Wuxuan fault occurred many times in Devonian and Mesozoic-Cenozoic, and it is one of the famous rock-controlling and ore-controlling structures in Guangxi.