1995 Chiapas earthquake
http://dbpedia.org/resource/1995_Chiapas_earthquake an entity of type: Thing
The 1995 Chiapas earthquake occurred on October 20 at 20:38 local time. The epicenter was located in Ocozocoautla de Espinosa, in the state of Chiapas, Mexico, near Tuxtla Gutiérrez. It had a magnitude of Mw 7.2, or ML 6.5. Building damage was reported. Around 70 people were reported injured. In Tuxtla Gutiérrez, telephone and electricity services were momentarily interrupted. This earthquake could be felt strongly in Mexico City and in many parts of southern Mexico. It could also be felt in Guatemala and El Salvador. The centroid mechanism is of thrust faulting with a small strike-slip component. The rupture of this earthquake propagated from NW to SE over a distance of about 30 km. The duration of the rupture was about 17 seconds. The earthquake was resulted from the internal deformation
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El terremoto de Ocozocoautla de 1995 fue un movimiento ocurrido la noche del 20 de octubre de 1995 a las 20:38:58, hora local (GMT-5). Tuvo una magnitud de Mw 7.1 con epicentro a 12 km al noroeste de Ocozocoautla de Espinosa, Chiapas, a una profundidad de 160.0 km (según el Servicio Sismológico Nacional), y Mw 7.2 a 13 km al noroeste de Ocozocoautla y a 159.3 km de profundidad (según USGS).
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1995 Chiapas earthquake
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Terremoto de Ocozocoautla de 1995
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1995-10-21
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1995
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The 1995 Chiapas earthquake occurred on October 20 at 20:38 local time. The epicenter was located in Ocozocoautla de Espinosa, in the state of Chiapas, Mexico, near Tuxtla Gutiérrez. It had a magnitude of Mw 7.2, or ML 6.5. Building damage was reported. Around 70 people were reported injured. In Tuxtla Gutiérrez, telephone and electricity services were momentarily interrupted. This earthquake could be felt strongly in Mexico City and in many parts of southern Mexico. It could also be felt in Guatemala and El Salvador. The centroid mechanism is of thrust faulting with a small strike-slip component. The rupture of this earthquake propagated from NW to SE over a distance of about 30 km. The duration of the rupture was about 17 seconds. The earthquake was resulted from the internal deformation of the Cocos Plate, which is subducting beneath the North American Plate.
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El terremoto de Ocozocoautla de 1995 fue un movimiento ocurrido la noche del 20 de octubre de 1995 a las 20:38:58, hora local (GMT-5). Tuvo una magnitud de Mw 7.1 con epicentro a 12 km al noroeste de Ocozocoautla de Espinosa, Chiapas, a una profundidad de 160.0 km (según el Servicio Sismológico Nacional), y Mw 7.2 a 13 km al noroeste de Ocozocoautla y a 159.3 km de profundidad (según USGS). Este sismo ha tenido poca relevancia a nivel nacional a pesar de haber dejado graves daños en los municipios de Villaflores, Cintalapa, Ocozocoautla, Berriozábal y Tuxtla Gutiérrez, probablemente debido al anterior sismo ocurrido en Colima el 9 de octubre, además de contribuírsele información errónea como cambiar su epicentro a Cintalapa de Figueroa.
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