Articles | Volume 67, issue 1
E&G Quaternary Sci. J., 67, 33–36, 2018
https://doi.org/10.5194/egqsj-67-33-2018
E&G Quaternary Sci. J., 67, 33–36, 2018
https://doi.org/10.5194/egqsj-67-33-2018

Thesis abstract 10 Sep 2018

Thesis abstract | 10 Sep 2018

Proglacial streams and their chronology in the glacier forefields of the Himalayas

Gerrit Tombrink

Cited articles

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Kuhle, M.: The maximum Ice Age (Würmian, Last Ice Age, LGM) glaciation of the Himalaya – a glaciogeomorphological investigation of glacier trim-lines, ice thicknesses and lowest former ice margin positions in the Mt. Everest–Makalu–Cho Oyu massifs (Khumbu and Khumbakarna Himal) including informations on late-glacial, neoglacial, and historical glacier stages, their snow-line depressions and ages, GeoJ., 62, 193–650, 2005. 
Kuhle, M.: The Uplift of High Asia above the Snowline and its Glaciation as an Albedo-Dependent Cause of the Quaternary Ice Ages, Earth sciences in the 21st Century, Nova science publ., New York, USA, 2013. 
Montgomery, D. R. and Buffington, J. M.: Channel-reach morphology in mountain drainage basins, Geol. Soc. Am. Bull., 109, 596–611, 1997. 
Racoviteanu, A. and Bajracharya, S.: GLIMS Glacier Database, Boulder, CO, USA, National Snow and Ice Data Center, https://doi.org/10.7265/N5V98602, 2008.