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

STELL

https://doi.org/10.1007/978-3-030-39663-3ndertaken (.), 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

出價(jià)

Strategies of Electron Probe Data Reduction,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

平淡而無(wú)味

Book 1998re debris cones and debris slopes, as well as mudflows and alluvial fans. In addition to the Ice Age glaciation history, as a preparatory, indirect factor, the Holocene to present glaciation history is, as a result of the danlming-up of glacier- and moraine lakes and their outbursts, a direct risk f

間諜活動(dòng)

0924-5499 ndirect factor, the Holocene to present glaciation history is, as a result of the danlming-up of glacier- and moraine lakes and their outbursts, a direct risk f978-94-010-6200-8978-94-011-5228-0Series ISSN 0924-5499 Series E-ISSN 2215-0072

爭(zhēng)吵

Sedimentology and Clast Orientation of Deposits Produced by Glacial-Lake Outburst Floods in the Moud geomorphic systems in mountainous environments, increasing the risk of geologic and hydrologic hazards such as glacial-lake outburst floods, landslides, and glacier avalanches (.; .). Glacial-lake outbursts are perhaps the most devastating of these processes because they can travel tens to hundred