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/10.1007/978-1-4613-2901-5ntion of natural scientists. The territory of the Tatras National Park in the Slovak Republic (Fig. 1) displays a unique natural environment in Central Europe both by its geomorphological evolution history and unique biosphere complex. The topic of this paper is to emphasize the natural hazards of t

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Conduit

Chaos Theory of Slides/Mud Flows in Mountain Areas,dom perturbations can send the system from one branch of the process-response curve to another: a natural disaster occurs. Thus, anytime the “equilibrium” in a landscape is disturbed, humans experience this as a disaster.

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Late Holocene Sturzstroms in Glacier National Park, Montana, U.S.A.,ndertaken (.), but few studies have focused on the distribution and age of rock-avalanche deposits in Montana, a state where the western third is seismically active and mountainous. Exceptions include works by (.), who described the rockslide avalanche produced by the Madison Canyon earthquake of 19

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Fluvial Hazards in a Steepland Mountain Environment, Southern Bolivia,n mountain environments, are not fully understood or adequately incorporated into development planning. Possibly the most important contribution of fluvial geomorphology to flood hazard assessment in mountain environments is in recognising the relationships between control of flood waters and the co

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Ablation