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Seismic site effects information


Seismic site effects are related to the amplification of seismic waves in superficial geological layers.[1] The surface ground motion may be strongly amplified if the geological conditions are unfavorable (e.g. sediments). Therefore, the study of local site effects is an important part of the assessment of strong ground motions, seismic hazard and engineering seismology in general. Damage due to an earthquake may thus be aggravated as in the case of the 1985 Mexico City earthquake. For alluvial basins, we may shake a bowl of jelly to model the phenomenon at a small scale.

This article defines site effects first, presents the 1985 Mexico City earthquake, describes the theoretical analysis of the phenomenon (through mechanical waves) and details several research results on seismic site effects in Caracas.

  1. ^ Semblat J.F., Pecker A. (2009) Waves and vibrations in soils: earthquakes, traffic, shocks, construction works, IUSS Press, Pavia, Italy, 499p.

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Seismic site effects

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detection. A seismic array differs from a local network of seismic stations mainly by the techniques used for data analysis. The data from a seismic array is...

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as compared to the widespread effects of an earthquake. Due to lower-frequency vibrations of cryoseisms, some seismic monitoring stations may not record...

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Contra Dam

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on 2008-04-29. Retrieved 2007-05-24. Adams, R. D. (January 1968). "Seismic effects at Mangla Dam: Pakistan" (PDF). UNESCO. p. 5. Archived (PDF) from the...

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