Zhangguangcailing area is located in the south-central part of Heilongjiang Province and parts of eastern Jilin Province. Historically, it was under the jurisdiction of Bohai, Jin, Liao and Qing established by Su Shenren and Jurchen in northern China. The Qing dynasty was forbidden for a long time. It was the birthplace of Jin Dynasty and Qing Dynasty.
The elevation of Linhai Snowfield is mostly between 180-800 meters, with an average elevation of 400-500 meters. The annual average temperature is 1.9-3.6℃, the extreme maximum temperature is 36.3 degrees, the extreme minimum temperature is -38.8 degrees and the frost-free period is 85- 130 days.
Extended data:
Zhangguangcailing is the most prominent mountain in Heilongjiang Province, with high mountains and complex terrain, including cliffs and steep slopes. From the main ridge to both sides, from Zhongshan to low hills, it gradually declines, belonging to the mountainous area eroded by running water.
Erosion and denudation of Zhongshan Mountain: mainly distributed along the main ridges of Zhangguangcailing and Guokui Mountain. Most mountains are composed of Hercynian granite and Baigangshi granite. The main ridge in the north is Silurian sandstone and slate, and the south is intermediate-acid volcanic rock. The mountain is in the northeast, majestic, steep, deep valley, deep valley and steep slope.
Narrow ridge, high terrain and precipice are the main features of Zhongshan in Zhangguangcailing. There are many peaks above 1000 meters above sea level, and the highest peak is Dadu Dingzi Peak at the southern end of the main ridge, with an altitude of 1780 meters, which is the first peak in Heilongjiang Province. From southwest to east, there are more than 20 peaks with an altitude of 1000 meters.
Such as dam crest (elevation 1668.9 m), old dam crest (elevation 142 1 m), cauldron helmet (elevation 130 1 m) and earth crest (elevation/kloc-0) Most of the peaks distributed along the main ridge have gentle peaks, representing the ancient planation plane, which is a flat and steep terrain formed by crustal uplift since Quaternary.
Baidu Encyclopedia-Linhai Xueyuan Scenic Area
Baidu Encyclopedia-Changbai Mountain Range (a mountain range in the northeast and surrounding areas of China)