Response of a hydrothermal system to escalating phreatic unrest: the case of Turrialba and Irazú in Costa Rica (2007–2012)
Open Access
- 12 July 2021
- journal article
- research article
- Published by Springer Science and Business Media LLC in Earth, Planets and Space
- Vol. 73 (1), 1-26
- https://doi.org/10.1186/s40623-021-01471-8
Abstract
No abstract availableKeywords
Funding Information
- Istituto Nazionale di Geofisica e Vulcanologia
- Universidad de Costa Rica
This publication has 68 references indexed in Scilit:
- SO2 degassing from Turrialba Volcano linked to seismic signatures during the period 2008–2012International Journal of Earth Sciences, 2013
- Space- and ground-based measurements of sulphur dioxide emissions from Turrialba Volcano (Costa Rica)Bulletin of Volcanology, 2012
- Rainfall and cloud water interception in mature and secondary lower montane cloud forests of central Veracruz, MexicoJournal of Hydrology, 2010
- Evolution of fluid geochemistry at the Turrialba volcano (Costa Rica) from 1998 to 2008Bulletin of Volcanology, 2010
- Naturally acid waters from Copahue volcano, ArgentinaApplied Geochemistry, 2009
- High water contents in basaltic magmas from Irazú Volcano, Costa RicaJournal of Volcanology and Geothermal Research, 2007
- Hydrogeochemistry and rare earth element behavior in a volcanically acidified watershed in Patagonia, ArgentinaChemical Geology, 2005
- New insight into the factors leading to the 1998 flank collapse and lahar disaster at Casita volcano, NicaraguaBulletin of Volcanology, 2003
- Hydrothermal element fluxes from Copahue, Argentina: A “beehive” volcano in turmoilGeology, 2001
- Failure of volcano slopesGéotechnique, 1997