Abstract:Glacier scratches are vitally important evidence to judge the relic of glacier. Scratches in rock face of trough valley and in ice gravel are very obvious. Scratches in rock face has the characteristics of long and thin, intensive and parallel; while scratches in ice gravel has the characteristics of short and thick, sparse and non-directional. There are also arc scratches, thrust scratches, crescent-shaped break, crescent-shaped crack and striation. Through comparative analysis, the scratches developed in Mengshan mountain are completely consistent with those in the modern glacial valley of Hailuogou in Sichuan province. Therefore, the glacial origin of the scratches in Mengshan mountain is further determined.