Based on in-situ observing,high resolution remote sensing data(WorldView-1,QuickBird and SPOT5/6),glacier distribution of Daxueshan in 2004,2008and 2015were interpreted.Glacier change of Daxueshan was analyzed from 2004to 2015.The results indicate that:(1)totally,there are 226glaciers with total area of 131.07km~2 in Daxueshan in 2015.It includes 81valley glaciers with area of 106.5km~2,128 hanging glaciers with area of 14.68km~2 and 17cirque glaciers with area of 9.89km~2.From 2004 to 2015,the glacier in Daxueshan is decreasing with a rate of 4.9%/10a,while summer average air temperature and yearly precipitation have no significant change at the same time.The glacier retreating can be attributed to the temperature increasing in previous decades of years and keep high temperature in these year.The retreating rate of valley glaciers,hanging glaciers and cirque glaciers are 0.45km~2/year、0.18km~2/year and 0.06km~2/year respectively from 2004to 2015;(2)By analyzing the elevation of glaciers,the minimum elevation of glaciers is increasing and the maximum elevation of glacier is decreasing.The elevation range of glacier distribution was reducing in the past 10years.Glaciers with small area change faster than Glacier with large area,because small glaciers are more sensitive to climate change.The analyzing of glaciers slope indicates that the glacier retreating is mainly distributed in the area with slope greater than 15degree.According to glacier aspect statistic,the majority of glacier in Daxueshan is North oriented.Comparing with other aspect orientation,glacier in aspect range 22.5°~45°,0°~22.5°and 337.5°~360°changed faster.