. Bonner zoologische Monographien. Zoology. 30. : Transition of Outer and Inner Himalayas, alpine zone. Gorak Shep SW Mt. Everest, side moraine uith dwarf Salix 5200 m. Solukhumbu IX 1970. Horizontal structure - the threefold subdivision of the Himalayas The subdivision of the Himalayan system into the Outer. Inner and Tibetan Himalaxas (Schweinfurth 1982) is based on the amount of local precipitation (wet - moderate!} wet - dr}0. The Outer Himalayas () To the Outer Himalax as belong the south-facing macroslope of the main chain and the Ma- habharat and Siwalik rang


. Bonner zoologische Monographien. Zoology. 30. : Transition of Outer and Inner Himalayas, alpine zone. Gorak Shep SW Mt. Everest, side moraine uith dwarf Salix 5200 m. Solukhumbu IX 1970. Horizontal structure - the threefold subdivision of the Himalayas The subdivision of the Himalayan system into the Outer. Inner and Tibetan Himalaxas (Schweinfurth 1982) is based on the amount of local precipitation (wet - moderate!} wet - dr}0. The Outer Himalayas () To the Outer Himalax as belong the south-facing macroslope of the main chain and the Ma- habharat and Siwalik ranges to the south. It is the rainiest part of the Himalax as. which to a great extent creates its own climate, because of the monsoon precipitation it recei\ es. We have described it in the section "'Vertical stmcture: the forest belts". The Inner Himalayas () The Inner Himalayas, usualh' refeiTcd to as the Inner Valle\ s. ha\ e a special place in this system with regard to their ecology. They are forested, but the\- recei\"e distincth" less pre-. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Bonn, Zoologisches Forschungsinstitut und Museum Alexander Koenig


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