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Hazard maps are created and used in conjunction with several natural disasters. [1] Different hazard maps have different uses. For instance, the hazard map created by the Rizal Geological Survey is used by Rizalian insurance agencies in order to properly adjust insurance for people living in hazardous areas. [2]
Founded in 1991, GHI is the first non-profit, nongovernmental organization dedicated to mitigating earthquake, tsunami, and landslide risks in the world's poorest and most at-risk regions. Its solutions emphasize preparedness, mitigation, and building local capacity in order to manage risk. [1]
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 ...
"Natural Disasters News".Ubyrisk. Archived from the original on 2018-11-01 Worldwide news site focused on natural disasters, mitigation and climate changes news "Global Risk Identification Program (GRIP)".
Landslide: 0 $70 million Aldercrest-Banyon landslide: Kelso, Washington: 1998 Blizzard: 30 $5 million North American ice storm of 1998: Canada and Northeast 1997 Flood: 0 $2 billion 1997 Red River flood: North Dakota, Minnesota, Southern Manitoba: 1996 Flood: 8 $500 million Willamette Valley flood of 1996: Washington, Oregon, Idaho, California ...
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 ...
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 ...
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 ...