Fushun, located in the east and north of Liaoning Province, is a prefecture-level city and an important industrial base in Liaoning Province. It is adjacent to Jilin Province in the east, 45 kilometers away from the provincial capital Shenyang in the west, Tieling in the north and Benxi in the south.

Fushun has an ancient and long history. The Neolithic coal products unearthed here can prove that as early as 7000 years ago, our ancestors had been active in Fushun and reached a certain level of civilization. The appearance of the Great Wall in the Warring States and Qin and Han Dynasties and the establishment of Xuantu County in the Han Dynasty marked the profound accumulation of the early civilization history in Liaodong.

Fushun is a multi-ethnic area. Since ancient times, the ancestors of all ethnic groups living in the big family of the Chinese nation on both sides of the Hunhe River have jointly developed, which makes the culture here not only have internal relations with the Central Plains, but also have distinctive local ethnic characteristics. As a region where Han and ethnic minorities live together, many ethnic minorities such as Koguryo, Xianbei, Qidan, Nuzhen and Mongolia have experienced ups and downs in Fushun.

topography

Fushun area is located in the northern margin of North China platform and the west of Tieling-Jingyu ancient uplift. It is adjacent to the Taizihe ancient depression in the south and the western fold belt of the Black Sea in Mongolia in the north, and it is in a long-term uplift position in geological history.

The geological structure belongs to the east extension of the east-west complex structural belt of Yinshan Mountain, and the combination belt with the second giant uplift belt of Xinhua Xia, namely Changbai Mountain Range. The geological structure is complex, and the structures are divided into east-west structures, namely, Neocathaysian structure, yamagata structure, northwest structure and north-south structure.

Fushun belongs to the north China platform anticline, and Hunhe fault is the northern extension of the Tanlu fault, which runs across the city from east to west. Taking the Hunhe fault as the boundary, the northern part of Hunhe belongs to Tieling-Qingyuan uplift, and the southern part of Hunhe belongs to Fushun-Xinbin uplift. In addition, the southern part of Hunhe River has a large uplift and the basement rocks are widely exposed.

Therefore, Fushun's landform features are: based on mountains, with Hunhe Valley running through the whole region as the skeleton, with numerous valleys as the network, with natural landscapes intertwined with mountains, river beds and river valleys, and low hills and narrow valley plains with ups and downs in the middle.

Reference to the above content: Baidu Encyclopedia-Fushun City