Qianling park is a national AAAA tourist area. It is located in thenorthwest of the Central District of Guiyang. It is adjacent to Zaoshan road inthe south, bageyan road in the East, Shibei road in the northeast, guandaoyanand Xiaoguan reservoir in the north, changpoling forest farm, qichongling,Sanqiao village and Shengquan in the West. It is 1.5 km away from the citycenter and covers an area of 426 hectares. It is one of the few largecomprehensive urban parks in China. It is famous for Mingshan, Xiushui, Youlin,Gusi, Shengquan and Linghou. The park was built in 1957. It is a bright pearl ofGuizhou Plateau since ancient times, and has the reputation of "the firstmountain in Southern Guizhou".
Because the climate background of Qianling mountain is located in theplateau, the climate conditions of Qianling mountain are quite consistent, andit has different plateau subtropical climate characteristics from the typicalmiddle subtropical region. There is no severe cold in winter, no severe heat insummer, abundant heat and long growth period. The annual average temperature is15.3 ℃, the monthly average temperature is 4.9 ℃, the maximum temperature is33-34 ℃, the minimum temperature is 4? 5 ℃, and the frost free period is 270days.
Qianling park is a collection of mountains, forests, springs, lakes, caves,temples and animals. It is known as "value in the city, beauty in nature".
Qianling mountain is a part of the central part of Qianzhong mountain. Thepark has continuous mountains and alternate valleys, and the terrain is full ofchanges. The altitude ranges from 1100 m to 1396 m, with undulating terrain andsmall relative elevation difference, about 200 m. The mountains are:baixiangling, bajiaoyan, daluoling, xiangwangshan, qichongling, Tanshan andzhangboshan. Among them, the altitude of daluoling is 1396 meters, which is thehighest peak in the park and the northwest of Guiyang central area.
Due to the complex geological structure, more strata are exposed in a smallrange in qianlingshan area, including Maokou Formation of Lower Permian,Wujiaping formation and Changxing Formation of Upper Permian, Daye Formation andAnshun formation of Lower Triassic, Guiyang formation of Middle Triassic,Sanqiao formation and Erqiao formation of Upper Triassic and Ziliujing group ofmiddle lower Jurassic.
In April 1944, Li Siguang, a famous geologist in China, inspected the siteof Hongfu temple in Qianling mountain, which belongs to the Quaternary glacialrelic "ice kiln".