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Journal of Geophysical Research: Solid Earth(4)
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Chronology and phenomenology of the 1982 and 2015 Wolf volcano eruptions, Galápagos Archipelago
ArticleAbstract: The 1982 and 2015 eruptions were the first at Wolf volcano, Galápagos Archipelago, with eyewitness aPalabras claves:Eruption rate, GALAPAGOS, Lava fountain, Reticulite, WolfAutores:Bagnardi M., Coppola D., Gibson S., Gleeson M.L.M., Julien Bernard, Patricio A. Ramón, Silvana Hidalgo, Stephen Hernández, Stock M.J.Fuentes:scopusAutocorrelation Infrasound Interferometry
ArticleAbstract: Seismic and infrasound multistation ambient-noise interferometry has been widely used to infer grounPalabras claves:autocorrelations, infrasonic thermometer, infrasound, Interferometry, noise, Volcano infrasoundAutores:Hugo D. Ortiz, Johnson J.B., Juan Camilo Anzieta, Mario C. Ruiz, Matoza R.S., Stephen HernándezFuentes: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:googlescopusCrustal thickness and magma storage beneath the Ecuadorian arc
ArticleAbstract: The Northern Andes of Ecuador contain some of the most active volcanic systems in the Andes and extePalabras claves:Crustal Imaging, crustal structure, Joint inversion, SOUTH AMERICA, Volcanic structureAutores:Beck S.L., Delph J., Koch C.D., Lynner C., Mario C. Ruiz, Meltzer A., Pablo Samaniego Ponce, Patricia A. Mothes, Silvana Hidalgo, Stephen HernándezFuentes:scopusDrumbeat LP “Aftershocks” to a Failed Explosive Eruption at Tungurahua Volcano, Ecuador
ArticleAbstract: Highly periodic, repetitive long-period (LP) earthquakes, known as “drumbeats,” have been observed aPalabras claves:drumbeat earthquakes, long-period earthquakes, volcanic degassing, volcanic seismologyAutores:Bell A.F., Butcher S., Calder E., Mario C. Ruiz, Patricia A. Mothes, Stephen HernándezFuentes:googlescopusDynamic 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:scopusGeophysical 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:googlescopusGlobal ubiquity of dynamic earthquake triggering
ArticleAbstract: Earthquakes can be triggered by local changes in the stress field (static triggering) due to nearbyPalabras claves:Autores:Pankow K., Parsons T., Stephen Hernández, Velasco A.Fuentes:googlescopusForecasting and communicating the dispersion and fallout of ash during volcanic eruptions: lessons from the September 20, 2020 eruptive pulse at Sangay volcano, Ecuador
ArticleAbstract: Volcanic ash is a hazard to human health and activities. Accurate and timely forecasts coupled withPalabras claves:Ash3d, COMMUNICATION, eruption source parameters, forecasting, grain-size distribution, Sangay, violent StrombolianAutores:Gerardo Pino, Julien Bernard, Kibler J., Marjorie Encalada, Mastin L.G., Pablo Samaniego Ponce, Silvana Hidalgo, Stephen Hernández, Vizuete N.Fuentes:scopusEvolution 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:scopus