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 número51Actividad Sísmica en Costa Rica Durante el 2013Nueva evidencia de un estadio juvenil de Pliometanastes protistus y su relación con ?Pliometanastes galushai Hirschfeld & Webb, 1968 (Xenarthra, Megalonychidae) para el Mioceno Superior de Costa Rica índice de autoresíndice de materiabúsqueda de artículos
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Revista Geológica de América Central

versión On-line ISSN 0256-7024versión impresa ISSN 0256-7024

Resumen

ALPIZAR, Yemerith et al. Activity of the Costa Rican Volcanoes During 2012-2013. Rev. Geol. Amér. Central [online]. 2014, n.51, pp.145-158. ISSN 0256-7024.

As part of the tasks of Red Sismológica Nacional of Costa Rica (RSN, UCR-ICE), volcanic monitoring is a topic that need all our attention. Likewise, the record of the results from this monitoring (field and laboratory work), is a useful tool for the research in short, middle and long term. This tecnic note comprises a synthesis of the results and observations of the last two years of volcanic surveillance at active volcanoes in Costa Rica (Rincón de la Vieja, Arenal, Poás, Barva, Irazú and Turrialba). These results enrich the RSN data base, covering four decades of experience in the implementation of advanced technologies in the area. In the beginning of 2012 all volcanoes manifested background behavior, representing low levels of phreatic and seismic activity. In September 2012, an increase in volcanic activity occurred following the Samara earthquake (Mw=7,6). This increased unrest was manifested mainly through the increase in temperature of fumaroles, some changes in crater lake dynamics and chemistry, increased seismic and phreatic activity. These higher activity conditions were maintained during the rest of the period.

Palabras clave : Volcano monitoring; Rincón de la Vieja; Arenal; Poás; Barva; Irazú; Turrialba.

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