Titlebook: Low-Dimensional Cooperative Phenomena; The Possibility of H H. J. Keller Book 1975 Springer Science+Business Media New York 1975 High-tempe

中世紀(jì)

Bernard C. Gersteinhen the two standing Buddhas, dating back to VI C. a.D. were destroyed. Not only was invaluable cultural heritage irremediably lost but also the consequences of the explosions, as well as the collapse of the giant statues, added greatly to the geological instability of the area. Traces of rocks rece

間諜活動

Peter M. Richardsion of the area, along with intensive fluvial erosion and tectonic disturbance of the rocks, has been significantly affecting the evolution of the landscape. Unknown triggering impulse for such huge slope deformation and presence of several younger generations of slope movements were reasons for com

Prostaglandins

Gerald F. Kokoszka as trenching and drilling are either difficult to employ or not allowed. This paper presents the results of DC resistivity, electromagnetic (EM ) and ground penetrating radar (GPR) surveys to map fractures and zones of weakness in crystalline bedrock at Machu Picchu, Peru. DC resistivity surveys we

Exterior

P. Day as trenching and drilling are either difficult to employ or not allowed. This paper presents the results of DC resistivity, electromagnetic (EM ) and ground penetrating radar (GPR) surveys to map fractures and zones of weakness in crystalline bedrock at Machu Picchu, Peru. DC resistivity surveys we

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征稅

B. Renker,R. Comèsetector of slope instability for individual use), a low-cost and simple monitoring method for early warning of landslides was proposed. A wireless sensor unit which is equipped with a MEMS (Micro Electro Mechanical Systems) tilt sensor and a volumetric water content sensor was developed and tested o

Matrimony

Huguette Launois,Halina Niedobaby the character and quality of the database used. The Peruvian DesInventar database is homogenous and, thus, serves as a useful tool for describing the significance of landslides and evaluating the role of the El Ni?o Effect among different causes of catastrophes. During the 1971–2009 period, the m

Lament

Klaus Krogmannotably in developing countries. To this end, a proposal was submitted to the IPL project committee by landslide researchers from the Geological Survey of Canada and the U.S. Geological Survey. The proposal is entitled IPL 106 “A Best Practices Handbook for Landslide Hazard Mitigation” and was accept

absolve

大洪水

L. V. Interrantemodel was based on the global datasets of climate, lithology, earthquake activity, and topography; and it was used to identify the areas with the highest hazard, or “hotspots”. The landslide hazard assessment model developed in the Natural Disaster Hotspots project was modified and improved to provi