16 Oct landslide geography
Landslide Study Case-- Created using PowToon -- Free sign up at http://www.powtoon.com/join -- Create animated videos and animated presentations for free. Landslide in progress on Mars, 2008-02-19, Type of natural disasters involving ground movements, often caused by slope instability triggered by specific event, This article is about the geological phenomenon. Tsunami § Tsunami generated by landslides, https://pubs.usgs.gov/fs/2004/3072/fs-2004-3072.html, "Monitoring and analysis of an earthflow in tectonized clay shales and study of a remedial intervention by KCl wells", "Residual strength and creep behaviour on the slip surface of specimens of a landslide in marine origin clay shales: influence of pore fluid composition", "Two multi-temporal datasets that track the enhanced landsliding after the 2008 Wenchuan earthquake", "Internal erosion controls failure and runout of loose granular deposits: Evidence from flume tests and implications for post-seismic slope healing", "Shear Resistance Variations in Experimentally Sheared Mudstone Granules: A Possible Shear-Thinning and Thixotropic Mechanism", "Shear-Rate-Dependent Behavior of Clayey Bimaterial Interfaces at Landslide Stress Levels", "Ancient Volcano Collapse Caused A Tsunami With An 800-Foot Wave", "Landslide susceptibility assessment using Fuzzy Sets, Possibility Theory and Theory of Evidence. [28] The factors that have been used for landslide hazard analysis can usually be grouped into geomorphology, geology, land use/land cover, and hydrogeology. The planes may be broadly parallel to the surface ("translational slides") or spoon-shaped ("rotational slides"). Early predictions and warnings are essential for the reduction of property damage and loss of life. [16][17] These processes normally cause the first severe road interruptions, due not only to deposits accumulated on the road (from several cubic metres to hundreds of cubic metres), but in some cases to the complete removal of bridges or roadways or railways crossing the stream channel. Modelación no paramétrica de lluvias para la ciudad de Manizales, Colombia: una aplicación de modelos multinomiales de probabilidad y de probabilidades imprecisas", "Remote Sensing and GIS Technologies as Tools to Support Sustainable Management of Areas Devastated by Landslides", "Forecasting potential slope failure in open pit mines", Weitere Erkenntnisse und weitere Fragen zum Flimser Bergsturz, "Two large late quaternary rock slope failures and their geomorphic significance, Annapurna, Himalayas (Nepal)", "Large landslide in Gansu Zhouqu August 7", British Geological Survey landslides site, British Geological Survey National Landslide Database, https://en.wikipedia.org/w/index.php?title=Landslide&oldid=983122692, Creative Commons Attribution-ShareAlike License, Combination in time and/or space of two or more principal types of movement, saturation by rain water infiltration, snow melting, or.
Landslide Study Case-- Created using PowToon -- Free sign up at http://www.powtoon.com/join -- Create animated videos and animated presentations for free. [19][27], Landslide hazard analysis and mapping can provide useful information for catastrophic loss reduction, and assist in the development of guidelines for sustainable land-use planning. They can be visually identified by concave scarps at the top and steep areas at the toe. This massive landslide first occurred seven hundred years. Water then increases the pore-water pressure and reduces the shearing strength of the material.[18]. Debris avalanches can also travel well past the foot of the slope due to their tremendous speed. The task is complex, and all the attempts towards operational landslide forecasting have adopted, implicitly or explicitly, a number of simplifying assumptions to reduce to a manageable extent the complex, and not yet fully … Researchers need to know which variables are the most important factors that trigger landslides in any given location. significant rockfall or volcanic collapse into the sea,[26] can generate tsunamis. This is essentially due to a decrease in the shear strength of the slope material, to an increase in the shear stress borne by the material, or to a combination of the two.
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