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

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書目名稱Geomorphological Hazards in High Mountain Areas影響因子(影響力)




書目名稱Geomorphological Hazards in High Mountain Areas影響因子(影響力)學科排名




書目名稱Geomorphological Hazards in High Mountain Areas網(wǎng)絡公開度




書目名稱Geomorphological Hazards in High Mountain Areas網(wǎng)絡公開度學科排名




書目名稱Geomorphological Hazards in High Mountain Areas被引頻次




書目名稱Geomorphological Hazards in High Mountain Areas被引頻次學科排名




書目名稱Geomorphological Hazards in High Mountain Areas年度引用




書目名稱Geomorphological Hazards in High Mountain Areas年度引用學科排名




書目名稱Geomorphological Hazards in High Mountain Areas讀者反饋




書目名稱Geomorphological Hazards in High Mountain Areas讀者反饋學科排名

geometrician

https://doi.org/10.1007/978-3-642-66196-9attributed to lithology, the tectonic stress applied to the rocks and steep relief In addition the climatic conditions promote deep weathering and provide landslide triggering rainfall events, generally mainly during the monsoon (cf. ., .).

使增至最大

Electron Microscopy of the KidneyHarappan city of Mohenjo-Daro in Pakistan, the Pueblo Buildings of the American South west, the Islamic treasures of Uzbekistan, and a range of great Christian cathedrals from the Mediterranean lands — are disintegrating.

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Jacket

Sedimentology and Clast Orientation of Deposits Produced by Glacial-Lake Outburst Floods in the Mous of kilometers downstream dramatically modifying channel morphology and, in some cases, causing loss of human life and destruction of property. The devastating effects of glacial-lake outburst floods have been documented in the Andes (.), Himalayas (.; .; .; ., .), Canadian Rockies (.; .; .; .), Swiss Alps (.; .), and Cascades (.).

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CARK

Andean Landslide Hazards,er roads, dwellings, or people lie in the path of potential landslides. In many cases, human land use practices such as the cutting of roads and clearing of forest can also serve to increase the potential for landslides, and/or influence where they may happen (e.g., .; .).

habitat

Book 1998ards are inferred from the development of landscape during the Quaternary. The history of glaciers can be seen as of central importance for this. The Ice Age glacial erosion created V-shaped valleys, which with their steep flanks - as a consequence of the interglacial formation of V -valleys - have

bacteria

Geomorphological Hazards and Risks in the High Tatra Mountains,l Europe both by its geomorphological evolution history and unique biosphere complex. The topic of this paper is to emphasize the natural hazards of the alpine-type relief manifested mainly by different types of slope movements and anthropogenous share of geomorphological hazards and risks in the Tatras National Park.