A complete glacier system has developed in Fawangsi temple in Songshan in He'nan province. It is consisted of Junxi Ice Dipper, Songmen U Valley, Jushi Ice Ridge in Holocene Longma Ice Age, and Sangongshi Ice Ridge sequence. Junxi cirque has typical characteristics of cirque. The flatness index F is 1.93, and typical cirque flatness index F is 1.7~5.0. The Songmen U Valley has the characteristics of a typical ice eroded U-shaped trough valley, with a depth to width ratio of 0.28~0.36., while typical glacier U Valley depth to width ratio in the world is 0.24~0.45. A giant stone ridge developed in Lanma Ice Age at the lower end of Songmen U Valley. Ice stained ridges are formed by stacked giant stones of different gravel diameters. Interval develope well, and lack in mud and sand filling between the intervals. Various glacier scratches are developed on the surface of giant rock, and giant stone ridge has the same accumulation characteristics as tMengshan Lanmatou wall. At the end of the development, there is a sequence of Sangongshi glacial ridges and grooves, and glacial ridges are symmetrically distributed. Due to the influence of the terrain in the accumulation area, the left ridge is more developed than the right ridge. The left ridge is 750 m long and 50~80 m wide, with a steep inner side and a gentle outer side, and is 8~13 m higher than the bottom of ice melting trough. The glacial ridge is composed of non layered and mixed sized gravel, with glacier scratches and new moon shaped fractures developed on the surface of giant boulders. Through photoluminescence dating, the accumulation age of a row of glacial ridges was obtained to be (14.1±1.18) ka, corresponding to the cooling event of the new fairy tree