Titlebook: Geomorphological Fluid Mechanics; N. J. Balmforth,A. Provenzale Book 2001 Springer-Verlag Berlin Heidelberg 2001 Geomorphology.Iceberg.con

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Václav Drchal,Václav Janiš,Josef Kudrnovskýhis massive amount of material is subsequently deposited on the ground, with much of the coarser fraction of the flow being deposited within a few hundred kilometres of the volcanic edifice. This may lead to a substantial regional change to the topography, with ash flow deposits being tens to hundre

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W. Dekeyser,L. Fiermans,J. Vennikplitudes of these disastrous events appear to have increased in recent years perhaps due to recent climate warming. The events endanger the personal property and infra-structure in mountainous regions. For example, from the winters 1940/41 to 1987/88 more than 7000 snow avalanches occurred in Switze

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https://doi.org/10.1007/978-1-4757-5099-7es subject to a free surface flow bounded by a granular medium. Flow of water also occurs very slowly through the interstices of the granular medium: however such a weak filtration process may be safely ignored. The interface between flowing mixture and granular medium can move as a result of a cont

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