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A simple and general methodology to calibrate seismic instruments for debris flow quantification: application to Cotopaxi and Tungurahua volcanoes (Ecuador)
ArticleAbstract: Debris flows are hazardous phenomena occurring at volcanoes, and monitoring them has proved as challPalabras claves:Buckingham Π-theorem, Debris flow monitoring, Peak-discharge rate, Seismic instrumentsAutores:Daniel Alejandro Pacheco, Emilia Saltos, S. Daniel Andrade, Stefanie Almeida, Stephen Hernández, Wilson AceroFuentes:scopusAreas prone to slow slip events impede earthquake rupture propagation and promote afterslip
ArticleAbstract: At subduction zones, transient aseismic slip occurs either as afterslip following a large earthquakePalabras claves:Autores:Cubas N., Jean Mathieu Nocquet, Patricia A. Mothes, Paul Jarrin, Plain M., Rolandone F., Sandro Vaca, Stephen Hernández, Vallée M., Yvonne FontFuentes:googlescopusGeophysical Footprints of Cotopaxi’s Unrest and Minor Eruptions in 2015: An Opportunity to Test Scientific and Community Preparedness
Book PartAbstract: Cotopaxi volcano, Ecuador, experienced notable restlessness in 2015 that was a major deviation fromPalabras claves:Cotopaxi volcano-Ecuador, Precursory geophysical patterns, Precursory LPs and VLPs, State of preparedness, volcanic unrest, Volcano MonitoringAutores:Edwin G. Viracucha, Elizabeth H. Gaunt, Espín P.A., Julien Bernard, Marco A. Yépez, Mario C. Ruiz, Patricia A. Mothes, Patricio A. Ramón, Paul Jarrin, Silvana Hidalgo, Stephen HernándezFuentes:googlescopusEvolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador
ArticleAbstract: Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the ePalabras claves:Long-period seismicity, volcanic monitoring, volcano-glacier interactions, volcano-seismic swarms, Volcano-tectonic interactionsAutores:Bell A.F., Butcher S., Mario C. Ruiz, Stephen HernándezFuentes:scopusDynamic earthquake triggering response tracks evolving unrest at Sierra Negra volcano, Galápagos Islands
ArticleAbstract: The propensity for dynamic earthquake triggering is thought to depend on the local stress state andPalabras claves:Autores:Bean C.J., Bell A.F., LaFemina P.C., Mario C. Ruiz, McCloskey J., Möllhoff M., Stephen HernándezFuentes:scopusLinking ground-based data and satellite monitoring to understand the last two decades of eruptive activity at Sangay volcano, Ecuador
ArticleAbstract: Sangay is one of the most active volcanoes in Ecuador, as it has been almost continuously erupting aPalabras claves:Episodic eruptions, Eruption frequency, Long-lasting activity, Sangay volcano, Size of the eruptionsAutores:Anais Vásconez Müller, Arellano S.R., Battaglia J., Coppola D., Francisco J. Vasconez, Jorge Córdova, Julien Bernard, Liorzou C., Marcelo Ortíz, Marco Almeida, Patricio A. Ramón, Silvana Hidalgo, Stephen Hernández, Valade S.Fuentes:scopusVolcanic event management in the Galápagos Islands, Ecuador
ArticleAbstract: The volcanoes of Galápagos, Ecuador, are among the most active in the world, with an average of fivePalabras claves:Autores:Francisco J. Vasconez, García L., Guillermo Viracucha, Julien Bernard, Patricio A. Ramón, Silvana Hidalgo, Stephen HernándezFuentes:scopusThe different characteristics of the recent eruptions of Fernandina and Sierra Negra volcanoes (Galápagos, Ecuador)
ArticleAbstract: After eight years of quiescence, Fernandina volcano experienced two short-lived eruptions, on 4 SeptPalabras claves:Autores:Alexandra P. Alvarado, Francisco J. Vasconez, Gorki A. Ruiz, Julien Bernard, LaFemina P.C., Mario C. Ruiz, Patricio A. Ramón, Silvana Hidalgo, Stephen HernándezFuentes:scopus