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Par Collection Par Auteur- KUHLE, M., (Editeur scientifique) (3)
- KUHLE, M. (1)
- KÖNIG, O. (1)
- MEINERS, S. (1)
- 1999 (3)
- Asia ; Fluvioglacial features ; Glacial features ; Glacial isostasy ; Glaciation ; High mountain ; Interglacial ; Kame ; Moraine ; Quaternary ; Roche moutonnée ; Tibet (1)
- Asie ; Fluvioglaciaire ; Glaciaire ; Glaciation ; Glacio-isostasie ; Haute montagne ; Interglaciaire ; Kame ; Moraine ; Quaternaire ; Roche moutonnée ; Tibet (1)
- Geochronology ; Glaciation ; Himalaya ; Lateglacial ; Moraine ; Nepal ; Postglacial ; Quaternary ; Snow line (1)
- Glaciation ; Géochronologie ; Himalaya ; Limite d'enneigement ; Moraine ; Népal ; Postglaciaire ; Quaternaire ; Tardiglaciaire (1)
- Glaciation ; Himalaya ; Lateglacial ; Moraine ; Nepal ; Palaeo-environment ; Quaternary ; Snow line (1)
- Glaciation ; Himalaya ; Limite d'enneigement ; Moraine ; Népal ; Paléo-environnement ; Quaternaire ; Tardiglaciaire (1)
- Tibet and High Asia (V) (3)
- Preliminary results on the last-high-glacial glaciation of the Rolwaling Himal and the Kangchenjunga Himal (Nepal, E- Himalaya) (1)
- Reconstruction of an approximately complete Quaternary Tibetan inland glaciation between the Mt. Everest- and Cho Oyu Massifs and the Aksai Chin. A new glaciogeomorphological SE-NW diagonal profile through Tibet and its consequences for the glacial isostasy and Ice Age cycle (1)
- The history of glaciation of the Rolwaling and Kangchenjunga Himalayas (1)
- Glaciation ; Himalaya ; Lateglacial ; Moraine ; Nepal ; Palaeo-environment ; Quaternary ; Snow line
- On the basis of empirical findings and inductive conclusions, the least extent of glaciation during the last ice age can be shown for 2 areas on the southern slopes of the Himalayas in Nepal. For the Rolwaling Himal, the snow line during the last
- ice age is calculated at 4000 m asl., i.e., 1500 m below the recent snow line. The last high-glacial snow line in the Kangchenjunga Himal is thought to be at 4350 m asl., the snow line depression here is 1150 m.
- Geochronology ; Glaciation ; Himalaya ; Lateglacial ; Moraine ; Nepal ; Postglacial ; Quaternary ; Snow line
- be carried out. Youngest historical to neoglacial ice margin positions could be recorded. Their mapping took place in a downward direction from the modern glacier margins. They confirm snow line (ELA) depressions from decameters up to ca. 100-250 m