It is controversial whether Quaternary glaciers has existed in the middle and low mountains of eastern China, but the glacial erosion landforms must be formed through ice erosion. In order to analyze whether the mountain geomorphology has the characteristics of the ice erosion in these areas. The Himalayas where develops widespreadly modern glaciers is selected as the research object. Through macro analysis, the glacial cirque system composed of necking, triangular ridge, residual arc as well as some particular characters in the process of ice erosion like valley avoidance, swallowing ridge, cutting wall and penetrating beam. It is considered that ice erosion process is mainly controlled by three factors: snow line elevation, snowpack elevation and slop direction and angle. On this basis, It is found that the mountain landforms in eastern China including Lushan in Jiangxi province, Mengshan in Shandong province, Huanggangliang, the main peak of Greater Khingan are consistent with the ice erosion landforms of the Himalayas using comparative analysis. From the glacial erosion process, It can be confirmed that Quaternary glaciers exist in the middle and low mountains of eastern China.