外流湖
- 网络Outflow lake;exorheic lake
外流湖-
外流湖期湖面急剧下降，气温和湿度较现今略高；
During the outflow lake stage the lake level lowered sharply and the air temperature and humidity were slightly higher than the present ;
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外流湖期发育于末次冰期晚冰阶，以冰碛为主要特征，此时喜马拉雅山主脊带分水岭北移至现今荡拉山的位置；
The outflow lake stage , which is characterized by tills , occurred in the late glacial interval of the Last Glacial Maximum , when the watershed of the main ridge zone of the Himalayas shifted northward to the location of present Tangla Mountain .