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Preliminary evaluation of the volcanic Hazard in the southern Valley of Mexico
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La ciudad de México está ubicada en el centro de un campo volcánico activo en la cuenca del Valle de México. Dejando de lado la actividad histórica del gran estratovolcán Popocatépetl, la última actividad de este campo volcánico fue la del volcán monogénico Xitle. Esta erupción ocurrió el año 2500 A.C. En este trabajo se calculo la tasa de erupción para el campo volcánico del sur del Valle de México por varios métodos diferentes. La tasa de erupción media se comprobó que es de 10-3 erupciones/año. La máxima probabilidad de erupción en el sur del Valle de México está situada en una banda E-0 que pasa a través de la Sierra de Chichinautzin. Por razones de seguridad, la expansión del área metropolitana de la ciudad de México deberá alejarse de la Sierra de Chichinautzin.
Title: Preliminary evaluation of the volcanic Hazard in the southern Valley of Mexico
Description:
La ciudad de México está ubicada en el centro de un campo volcánico activo en la cuenca del Valle de México.
Dejando de lado la actividad histórica del gran estratovolcán Popocatépetl, la última actividad de este campo volcánico fue la del volcán monogénico Xitle.
Esta erupción ocurrió el año 2500 A.
C.
En este trabajo se calculo la tasa de erupción para el campo volcánico del sur del Valle de México por varios métodos diferentes.
La tasa de erupción media se comprobó que es de 10-3 erupciones/año.
La máxima probabilidad de erupción en el sur del Valle de México está situada en una banda E-0 que pasa a través de la Sierra de Chichinautzin.
Por razones de seguridad, la expansión del área metropolitana de la ciudad de México deberá alejarse de la Sierra de Chichinautzin.
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