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Geological hazard: Difference between revisions

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'''Rather gradual or slow phenomena are e.g.:'''
'''Rather gradual or slow phenomena are e.g.:'''
* [[alluvial cone]]s (e.g. at the exit of [[cañon]]s or [[side valley]]s)
* [[alluvial cone]]s (e.g. at the exit of [[canyon]]s or [[side valley]]s)
* [[caldera]] development (volcanoes)
* [[caldera]] development (volcanoes)
[[Image:Norris_geyser_basin.jpg|thumb|right|Norris geyser at [[ National Park|Yellowstone NP]], Sept.2003]]
[[Image:Norris_geyser_basin.jpg|thumb|right|Norris geyser at [[ National Park|Yellowstone NP]], Sept.2003]]

Revision as of 21:51, 18 March 2006


A Geologic Hazard is one of several types of adverse geologic conditions capable of causing damage or loss of property and life. These hazards can consist of

Sudden or slow phenomena (alfabetic order)

Rather gradual or slow phenomena are e.g.:

Norris geyser at Yellowstone NP, Sept.2003

Geologic Hazard Evaluation

Geologic hazards are evaluated by an engineering geologist educated, trained and experienced in engineering geology for their recogition, investigation and analysis. Often in conjunction with a geotechnical engineer, the engineering geologist is qualified to formulate recommendations for the mitigation of the hazards. Mitigation can include avoidance of the hazards or relocation; construction of slope stabilization measures (earth buttress, retaining walls, diversion walls, shear pins, tiebacks, soil nails or soil anchors, revetments, injection of grout or concrete, deep foundations, tunnels, subdrains), and other measures.

See also: