Titlebook: Geomorphological Hazards in High Mountain Areas; Jan Kalvoda,Charles L. Rosenfeld Book 1998 Springer Science+Business Media Dordrecht 1998

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https://doi.org/10.1007/978-3-642-66196-9 the Himalayas, specially the Low and Middle Himalaya, landslides, representing the dominant hillslope process (.), are of special concern as they cause permanent loss of agricultural land (.), block important roads and even destroy housing (cf. .). The dominance of landslides in this region can be

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Z. L. Wang,P. Poncharal,W. A. de Heer,C. Huif. amongst others, ., 1988, 1995) — from the geomorphodynamics, observed directly on the spot, but from the entire glacigenic character of the high mountain landscape. Accordingly, not only the current changes of the glacier, which produce damage — as for instance the shifting of the glacier termina

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Kurt Mendgen,Dietrich-Eckhardt Lesemann the Antagonism Principle is the most important one (.). It states that there are . types of processes active in the formation of a landscape at the same time: the endogenic (tectonic) and the exogenic (meteoric) processes. Generally, these two processes more or less balance each other so that a lan

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https://doi.org/10.1007/978-3-030-39668-8low of the moisture laden subtropical jet stream yielding orographic precipitation exceeding 2000 millimeters annually. The dense conifer forest cover and deep soils allow copious rates of infiltration and throughflow, leaving sheetwash and rainsplash as relatively ineffective sediment transport pro

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https://doi.org/10.1007/b115596located on the eastern edge of the Belt (19°01′N, 97°16′W) (Fig.1). They are the two highest strato-volcanoes in Mexico and the only ones that are active and have glaciers on their slopes. These characteristics make them a high risk area for lahar formation and other geomorphologie processes, so it