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This type of measure is used in cases of smaller landslides. The effectiveness of micropiles is linked to the insertion of micropiles over the entire landslide area. In the case of rotational landslides in soft clay, the piles contribute to increasing the resisting moment by friction on the upper part of the pile shaft found in the landslide.
A landslide in which the sliding surface is located within the soil mantle or weathered bedrock (typically to a depth from few decimeters to some meters) is called a shallow landslide. Debris slides and debris flows are usually shallow. Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low ...
The difference between these two concepts is subtle but important. The landslide causes are the reasons that a landslide occurred in that location and at that time and may be considered to be factors that made the slope vulnerable to failure, that predispose the slope to becoming unstable. The trigger is the single event that finally initiated ...
In the wake of Hurricane Helene, more than 2,000 landslides displaced families in western North Carolina. They are waiting to find out if rebuilding is even possible or safe.
Pages in category "Landslide analysis, prevention and mitigation" The following 11 pages are in this category, out of 11 total. This list may not reflect recent changes .
The International Consortium on Landslides is a non-governmental organization created in 2002 to promote landslide research, education, and risk evaluation and reduction. It is located in Kyoto, Japan. The organization has consultative status with UNESCO. [1] [2] The ICL's journal is Landslides. It holds regular symposiums, including the World ...
Haunting memories of past landslides. Forecasters don’t expect the kind of rainfall that led to some of the region’s most destructive recent land flows.
Real-life landslide on a slope. Slope stability refers to the condition of inclined soil or rock slopes to withstand or undergo movement; the opposite condition is called slope instability or slope failure. The stability condition of slopes is a subject of study and research in soil mechanics, geotechnical engineering, and engineering geology.
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