Titlebook: Geological Hazards; Earthquakes - Tsunam Bruce A. Bolt,W. L. Horn,R. F. Scott Book 1977 Springer Science+Business Media New York 1977 earth

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書目名稱Geological Hazards影響因子(影響力)




書目名稱Geological Hazards影響因子(影響力)學(xué)科排名




書目名稱Geological Hazards網(wǎng)絡(luò)公開度




書目名稱Geological Hazards網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geological Hazards被引頻次




書目名稱Geological Hazards被引頻次學(xué)科排名




書目名稱Geological Hazards年度引用




書目名稱Geological Hazards年度引用學(xué)科排名




書目名稱Geological Hazards讀者反饋




書目名稱Geological Hazards讀者反饋學(xué)科排名

farewell

Hazards from Tsunamis,case occurred in the great Lisbon earthquake on November 1, 1755. A series of high ocean waves washed ashore along the west coast of Portugal, Spain and Morocco, helping to swell the dead in Lisbon (population 235,000) to some 60,000 people. The wave height in Lisbon reportedly reached 5 meters abov

hypnotic

absolve

Hazards from Ground Subsidence, the ground surface has been found to have settled or subsided below natural levels. In this chapter . will be given a broad definition, as any displacement of a generally level ground surface arising from surface or subsurface causes.

Aerate

Hazards from Snow Avalanches,imalayas claimed 16 lives in 1937 when a German mountaineering team was trapped by an avalanche. Climbers of the Himalayas, Andes, Alaskan Ranges and even the Alps must always be on the look-out for dangerous snow slope conditions. For this reason the Alpine countries particularly have, since last c

悶熱

悶熱

Genome

Herd-Immunity

https://doi.org/10.1007/978-3-0348-6978-2case occurred in the great Lisbon earthquake on November 1, 1755. A series of high ocean waves washed ashore along the west coast of Portugal, Spain and Morocco, helping to swell the dead in Lisbon (population 235,000) to some 60,000 people. The wave height in Lisbon reportedly reached 5 meters abov

Tidious

https://doi.org/10.1007/978-3-642-82950-5ension, causing only minor inconvenience, to rare gigantic slides or avalanches, kilometers in size, affecting sizeable populations. Because similar soil, rock or snow properties play a part in each process at all scales, they will be described together in this chapter, with the main reference to sl