Stronger or longer: Discriminating between Hawaiian and Strombolian eruption styles [PDF]
The weakest explosive volcanic eruptions globally, Strombolian explosions and Hawaiian fountaining, are also the most common. Yet, despite over a hundred years of observations, no classifications have offered a convincing, quantitative way of demarcating
Andronico, D +11 more
core +13 more sources
Imaging of Erebus volcano using body wave seismic interferometry of Strombolian eruption coda [PDF]
Seismic interferometry is a recently developed theory that allows for the recovery of a medium's impulse response between two points should randomly distributed sources of white noise, or equivalently, a multiply scattered equipartioned wavefield, be present throughout the medium. We exploit the extremely scattering nature of volcanic media and seismic
Julien Chaput +4 more
semanticscholar +4 more sources
Anatomy of a Strombolian eruption: Inferences from particle data recorded with thermal video [PDF]
AbstractOver the past decade, a proliferation of new technologies has pushed forward our ability to measure the dynamics of volcanic emissions as they exit, and ascend above, the vent. Measuring parameters of all particles as they exit the vent during an explosive eruption is the best way to gather parameters such as size, shape, velocity, and mass for
Maxime Bombrun +4 more
semanticscholar +6 more sources
Petrologic and numerical modeling study of Strombolian eruption dynamics at Volcán Llaima (Chile)
Le volcan Llaima se situe dans la zone volcanique sud des Andes, ~700 km au sud de Santiago du Chili. C'est l'un des volcans les plus actifs du pays avec plus de 50 éruptions depuis 1640. Le dernier épisode éruptif a duré deux ans et s'est terminé au milieu de l'année 2009.
Caroline Bouvet de Maisonneuve
semanticscholar +4 more sources
An analytical model for gas overpressure in slug-driven explosions:insights into Strombolian volcanic eruptions [PDF]
Strombolian eruptions, common at basaltic volcanoes, are mildly explosive events that are driven by a large bubble of magmatic gas (a slug) rising up the conduit and bursting at the surface.
Del Bello, Elisabetta +4 more
core +3 more sources
Shallow magma‐mingling‐driven Strombolian eruptions at Mt. Yasur volcano, Vanuatu [PDF]
Mt. Yasur volcano (Vanuatu) has been increasingly recognized for its high‐frequency Strombolian eruptions. Strombolian activity is often regarded as a product of the rapid ascent of gas slugs originating from a deep magma, which mingle with a batch of shallow magma upon eruption.
Simon Kremers +6 more
openalex +5 more sources
Physical parameterization of Strombolian eruptions via experimentally‐validated modeling of high‐speed observations [PDF]
Pressurized gas drives explosive volcanic eruptions. Existing models can predict the amount and pressure of gas in erupting magma, but application and testing of such models is currently limited by the accuracy of input parameters from natural systems.
Jacopo Taddeucci +7 more
openalex +5 more sources
Strombolian eruptions and dynamics of magma degassing at Yasur Volcano (Vanuatu) [PDF]
Open vent basaltic volcanoes account for a substantial portion of the global atmospheric outgassing flux, largely through passive degassing and mild explosive activity. We present volcanic gas flux and composition data from Yasur Volcano, Vanuatu collected in July 2018. The average volcanic plume chemistry is characterised by a mean molar CO2/SO2 ratio
Julia Woitischek +8 more
openalex +6 more sources
Seismic Source Migration During Strombolian Eruptions Inferred by Very‐Near‐Field Broadband Seismic Network [PDF]
AbstractWe analyze seismic waves excited by small Strombolian explosions to understand the source process of volcanic explosions. We deployed five broadband seismometers at only 100–300 m away from the active craters of Stromboli volcano, Italy. Moment tensor inversion of the entire seismic signals in the 0.05–0.2 Hz band locates the source at a depth ...
Shunsuke Sugimura +5 more
openalex +3 more sources
Plate tephra: Preserved bubble walls from large slug bursts during violent Strombolian eruptions [PDF]
We describe unusual "plate tephra" particles that provide key information about rarely observed processes that occur during volcanic eruptions. The tephra formed during the 2008-2009 eruption of Llaima volcano, Chile, and dispersed as far as 9 km from the vent.
Dawn Ruth, Eliza S. Calder
openalex +4 more sources

