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Journal of Geography (Chigaku Zasshi)
Late Quaternary glacier variation of the Ngojumba Glacier in the Khumbu Himal are determined by detailed field mapping of glacial landforms, stratigraphy of fossil soil, S-1, S-2, and S-3 in desending order, and 14C-dates of fossil soil horizon. The moraines of different ages indicate seven advance stages as follows ; the Gokyo stage, the Nah stage, the Machhermo stage, the Dole stage, the Phortse Drangka stage, the Phortse stage, and the Konar stage. The Gokyo and Nah stages, of which morainesdoi:10.5026/jgeography.99.3_270 fatcat:vhochwx325ebhcy6efyufz46g4