Valle de La Estrella earthquake: seismic analysis, disaster cascade and update of economic losses in present value (2020)
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| Autores: | , , |
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| Formáid: | artículo original |
| Stádas: | Versión publicada |
| Fecha de Publicación: | 2021 |
| Cur Síos: | Seismicity and focal mechanisms in the of North Panama Deformed Belt (NPDB) indicate a compressional environment associated with the overthrusting of the Panama Block (PB) on the Caribbean plate; crustal PB strike-slip focal mechanisms are observed in the Talamanca and Central Volcanic Cordillera. The hypocenters reach maximum depths between 50-60 km at the foot of the Talamanca mountain range and are shallow near the Caribbean coast. The 1991, Valle de la Estrella earthquake (Mw 7.6) triggered aftershocks in an area of ~140x70 km; landslides and liquefaction were the secondary events that caused most damage and losses in infrastructure (housing, bridges, railroad network, road network and aqueducts); its effects were concentrated in coastal cities, such as Limón and Bocas del Toro. The economic losses in present 2020 value correspond to $3 433 266 937.41. |
| País: | Portal de Revistas UCR |
| Institiúid: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| Teanga: | Español |
| OAI Identifier: | oai:portal.ucr.ac.cr:article/47079 |
| Rochtain Ar Líne: | https://revistas.ucr.ac.cr/index.php/geologica/article/view/47079 |
| Palabra clave: | Earthquake Limon 1991 Liquefaction Landslides Focal Mechanisms South Caribbean Terremoto Limón licuefacción deslizamientos mecanismos focales Caribe Sur |