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Articles relating to landslides, several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, shallow or deep-seated slope failures, mudflows, and debris flows.
Seismic microzonation is defined as the process of subdividing a potential seismic or earthquake prone area into zones with respect to some geological and geophysical characteristics of the sites such as ground shaking, liquefaction susceptibility, landslide and rock fall hazard, earthquake-related flooding, so that seismic hazards at different locations within the area can correctly be ...
Animation of a landslide in San Mateo County, California Landslips Noire River (Rivière Noire), Saint-Alban landslide 1894, Quebec, Canada [1] [2] Landslides , also known as landslips , or rockslides , [ 3 ] [ 4 ] [ 5 ] are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls , mudflows , shallow ...
Huge landslide at La Conchita, 1995. A geologic hazard or geohazard is an adverse geologic condition capable of causing widespread damage or loss of property and life. [1] These hazards are geological and environmental conditions and involve long-term or short-term geological processes.
A large landslide entered Sullorsuaq Strait, generating a megatsunami which struck Alluttoq Island, where it had a run-up height of 45 to 70 metres (148 to 230 ft). [15] ~2800 BCE Zion Canyon, Utah, US: 0.286 km 3: Landslide created the currently level floor of Zion Canyon inside Zion National Park. [21] ~1920 BCE Jishi Gorge, Qinghai Province ...
Landslides occur around the world and have helped shape the Earth as we know it. The landslide that destroyed a rural neighborhood and claimed 43 lives in Oso, northeast of Seattle, 10 years ago ...
the free length: the non-concreted length. Positioning of anchors and nails in an unstable rocky hillside When the anchorage acts over a short length it is defined as a bolt, which is not structurally connected to the free length, made up of an element resistant to traction (normally a steel bar of less than 12 m protected against corrosion by ...
The knowledge of the landslide frequency is a fundamental element for any kind of probabilistic evaluation. Furthermore, the evaluation of the age of the landslide permits to correlate the trigger to specific conditions, as earthquakes or periods of intense rains. It is possible that phenomena could be occurred in past geological times, under ...
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