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Riesgo sísmico en Guatemala

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Riesgo sísmico en Guatemala

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Desafío rápido sobre sismos y placas en Guatemala

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olga Recinos
olga Recinos
Guatemala

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Riesgo sísmico en Guatemala
 

Riesgo sísmico en GuatemalaOnline version

Desafío rápido sobre sismos y placas en Guatemala

by olga Recinos
1

El terremoto de 1976 en Guatemala fue causado por movimientos a lo largo de la falla de Motagua y alcanzó una magnitud de 7.5.

2

La falla de Motagua se localiza entre la placa de Cocos y la placa del Caribe.

3

El monitoreo de la actividad sísmica en Guatemala está a cargo principalmente del INSIVUMEH.

4

La actividad sísmica en Guatemala se genera únicamente por la interacción entre la placa del Caribe y la placa de Norteamérica.

5

La magnitud de un sismo se mide con la escala de Mercalli.

6

La falla de Motagua marca el límite entre la placa del Caribe y la placa de Norteamérica.

7

Los tsunamis en Guatemala pueden originarse a partir de terremotos en la zona de subducción frente a la costa del Atlántico guatemalteco.

8

INSIVUMEH es responsable únicamente de meteorología.

9

Guatemala está situada sobre tres placas tectónicas principales: la placa del Caribe, la placa de Cocos y la placa de Norteamérica.

10

El límite de subducción entre la placa de Cocos y la placa del Caribe se localiza frente a la costa del Pacífico guatemalteco.

 
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