冰川湖主要分布在高山冰川作用的过程中,其中在念青唐古拉山和喜马拉雅山区较为普遍。它们分布的海拔一般较高,而湖体较小,多数是有出口的小湖,如藏南的八宿错,它是由扎拉弄巴和钟错弄巴两条古冰川汇合以后,因挖蚀作用加强所形成的冰川槽谷,后谷口被终碛封闭堵塞形成,湖面高3460m,面积26km2,最大 Glacial lakes are mainly distributed in the process of alpine glaciation, of which the Nyainqentanglha and Himalayas are more common. They are generally higher elevation distribution, and the smaller lake, most of them are exiting small lake, such as the Bazu fault in southern Tibet, which is due to Zara Alba and the clock after the collision of two ancient glaciers alley, due to Excavation to enhance the formation of the glacier valley, the valley after the end of moraine closed blocking the formation of the lake high 3460m, an area of ​​26km2, the largest