The core attractions of Siguniang Mountain Scenic Area are Shuangqiaogou, Changping Valley, Haizigou, Moguniang Mountain (Momei Peak), Sanguniang Mountain, Erguniang Mountain and Daguuniang Mountain. Siguniang Mountain is steep and modern glaciers are developed.
There are 52 snow peaks above 5000 meters above sea level, which are covered with snow all year round and developed with modern mountain glaciers. Siguniang Mountain, the main peak, is 6250 meters above sea level, which is the highest peak in Qionglai Mountain, the second peak in Sichuan and the third peak in Hengduan Mountain.
Extended data
Geomorphological features of Siguniang Mountain: Siguniang Mountain is located at the eastern edge of Qinghai-Tibet Plateau, the first step of China landform, and belongs to the transition zone from Sichuan Basin to Qinghai-Tibet Plateau. The geotectonic structure belongs to Songpan-Ganzi fold belt in China geosyncline, and the landform is divided into western Sichuan alpine plateau, alpine canyon subregion and alpine canyon belt in the middle reaches of Dadu River.
The main landform types are: dry and warm valley (semi-arid valley) landform, alpine landform and extremely high mountain landform. The surface of Siguniang Mountain is mainly composed of sandstone, slate, marble, limestone and crystalline limestone in Mesozoic and Paleozoic.
Baidu encyclopedia-siguniang mountain scenic spot