Resumen
The May 13, 1647 earthquake, the larger catastrophe in the colonial history of central Chile, is considered as the second event of the inter-plate earthquakes series that has occurred at regular intervals in this part of Chile. However, this historical analysis suggests this earthquake, besides generating a strong and widespread shaking in the central valley, did not produced a tsunami. Both features could imply it was an intra-plate event, sourced in the surface of the continental plate or deeper in the Nazca plate. The reported effects resemble those from the 1939 Chillan earthquake, a middle-depth intra-plate event that although it did not produce a tsunami it does generated large intensities in the central valley and a huge number of victims. If the 1647 earthquake was intra-plate, a problematic risk scenario is set for the most populated region of the country.
Título traducido de la contribución | The 1647 earthquake in central Chile as an intraplate event: another threat to metropolitan Chile |
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Idioma original | Español |
Páginas (desde-hasta) | 23-33 |
Número de páginas | 11 |
Publicación | Revista de Geografia Norte Grande |
N.º | 53 |
Estado | Publicada - 2012 |
Publicado de forma externa | Sí |
Palabras clave
- 1647 earthquake
- Central Chile
- Historical seismology
- Intra-plate earthquake