Titlebook: Disaster Management and Risk Reduction: Multidisciplinary Perspectives and Approaches in the Indian ; Proceedings of NERC Sudip Mitra,Kaus

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Damage Detection Using Experimentally Obtained Frequency Response Data with an Application of Artifcy response (displacement mode shapes) is insufficient to localize the damage. Artificial neural network training processes are utilized to reduce measurement error from the measured frequency response data set. Using central difference approximation, the training data sets are then used to generate the mode forms curvatures.

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Thrombolysis

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Alan Forrest,Karen Hagemann,Michael Roweownslope .. The bedrock where this landslide occured comprised of shale belonging to the?Disang Group. To be able to decipher the causes of such kinds of slumping down of pieces of broken rocks . geological, structural and geotechnical investigations are carried out. It could be established that the

BOOM

War, Culture and Society, 1750–1850It swept away one residential building where seven families lived, and a link road between Saron Veng and Tuithiang Veng was blocked for more than a month. The improper drainage system, weak lithology, and high permeability also enhance the triggering factor for a landslide. The landslide covers an

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Alan Forrest,Karen Hagemann,Michael Rowey also occur in a fresh area. In the present study, a fresh landslide was observed during March 2022, at Pangthang, East Sikkim.?Analysis through Geospatial Technology, ground survey and soil investigation?were carried out for ?the?estimation of landslide susceptibility at concerned location, and it

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Alan Forrest,Karen Hagemann,Michael Rowe debris, rocks or a slope failure, which occurs due to heavy rainfall, snow melting, earthquakes, etc. So, it is most important to scrutinize and explore the landslide susceptible zones. Accurate Landslide Susceptibility Mapping (LSM) is a pre-requisite for the development of landslide mitigation st

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rty. Short duration high-intensity rainfall is one of the major factors driving these slope instabilities. Out of several such landslides, the Chanmari landslide has been susceptible to major mass movements for many years and rainfall infiltration is the triggering factor for these slope movements.

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Transfusion

able areas sharing similar geology in different parts of the town were selected for electrical resistivity study. Vertical Electrical Sounding (VES) was carried out to determine the subsurface conditions by analyzing variations in the resistivity values following the Schlumberger configuration. The