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One of the most important climatic events in the Iranian highlands during Quaternary era is remins and glacial geomorphology.
In this regard Alamkooh glacier must be concidered as the alone and most important glacier o area. This glacier has more than 14 small and larg glacier tongues which can be seen the activities life effects as well as them. The aim of this study is surveying of present geomorphological and also determinig the boundary extended them during the last and present glacier. The research methodology based on field work and measuring by using suitable indirect view and periodical.
The results show Alamkooh glaciers are gradually melting ,because of little feeding Avalanches fallen down the end-ward of cirques glacier can support their lives, the extending boundary toungues in the northern and southern slopes Alamkooh are 3800 and 4000 meter. Wheras the glacial morphology evidences indicat that the spread of these toungues has been 2800 and 3100m in the northern and southern slopes sides.