Results 51 to 60 of about 1,766 (197)

Probabilistic source location of explosion quakes at Stromboli volcano estimated with double array data [PDF]

, 2004
Data from two dense arrays of short-period seismometers are used to retrieve source locations of the explosion quakes at Stromboli volcano. Slowness vectors stimated at both arrays with the zero-lag cross-correlation technique constitute the experimental
Saccorotti, G., Mario La Rocca, La Rocca, M., Ibanez, J., Gilberto Saccorotti, Del Pezzo, E., Edoardo Del Pezzo, Jesus Ibanez   +7 more
core   +1 more source

Slope Failures Induced by the December 2002 Eruption at Stromboli Volcano [PDF]

, 2008
We reconstruct the sequence of landslides that occurred soon after the beginning of the December 2002 eruption on the NW flank of Stromboli volcano. Landslides involved the northeastern part of the Sciara del Fuoco (SdF) slope, an old collapse scar ...
Marsella, M., Romagnoli, C., Tommasi, P., Coltelli, M., Chiocci, F. L., Baldi, P.   +5 more
core   +2 more sources

The Stromboli geophysical experiment. Preliminary report on wide angle refraction seismics and morphobathymetry of Stromboli island (Southern Tyrrhenian sea, Italy)based on integrated offshore-onshore data acquisition (cruise STRO-06 R/V Urania) [PDF]

, 2007
The Stromboli geophysical experiment, performed to acquire onshore and offshore seismic data through a combined on-land and marine network, was finalized to reconstruct the seismic tomography of the volcano and to investigate the deep structures and the
Ciampi, Maurizio, Ilinskyi, Dimitri, Aiello, Gemma, Marsella, Ennio, Contrafatto , Danilo, Ulivieri, Giacomo, Di Prima , Sergio, Passaro, Salvatore, Iavarone, Michele, Bortoluzzi , Giovanni, De Cesare, Walter, Govoni, Aladino, Sgroi , Tiziana, Genco, Riccardo, Ruggieri , Stefano, Platania , Raffaele, Moretti, Milena, Patanè, Domenico, Scotto di Vettimo, Paolo, Rinke, Norbert Ralf, Speciale , Stefano, Di Fiore, Vincenzo, Augusti , Vincenzo, Marchetti, Emanuele, Castellano, Mario, Ferrante, Valentina, La Rocca, Mario, Ligi , Marco, Rapisarda, Salvatore, Frugoni, Francesco, Favali , Paolo, La Canna, Giorgio, Mangano , Giorgio, Zuccarello, Luciano   +33 more
core  

Interaction between seismicity and deformation on different time scales in volcanic areas: Campi Flegrei and Stromboli [PDF]

Advances in Geosciences, 2019
We study oscillations recorded at Stromboli and Campi Flegrei by different sensors: seismometers, strainmeters and tiltmeters. We examine both the high-frequency (>0.5 Hz) portion of the spectrum and very long period signals up to tidal scales.
M. Falanga, E. De Lauro, S. Petrosino, S. De Martino   +3 more
doaj   +1 more source

Submarine Flank Collapses at Tagoro Volcano: Insights From Bathymetric Surveys and 3D Multiphase Simulations

Journal of Geophysical Research: Oceans, Volume 131, Issue 8, August 2026.
Abstract Volcanic islands are prone to flank instabilities that can generate tsunamis even when mobilized volumes are moderate. This study investigates submarine collapses during the 2011–2012 eruption south of El Hierro, which built the Tagoro submarine volcano.
E. P. Montellà, A. Romano, G. Barajas, J. A. Lozano, J. T. Vázquez, J. L. Lara, E. Fraile‐Nuez   +6 more
wiley   +1 more source

Gas slug ascent through changes in conduit diameter : Laboratory insights into a volcano-seismic source process in low-viscosity magmas. [PDF]

, 2006
Seismic signals generated during the flow and degassing of low-viscosity magmas include long-period (LP) and very-long-period (VLP) events, whose sources are often attributed to dynamic fluid processes within the conduit.We present the results of ...
Lane, Steve J., James, M. R., Chouet, B. A.   +2 more
core  

Broadband measurements of the sources of explosions at Stromboli Volcano, Italy

Geophysical Research Letters, 1999
During September–October 1997, 21 three‐component broadband seismometers were deployed on Stromboli Volcano at radial distances of 0.3–2.2 km from the active crater to investigate the source mechanisms of Strombolian explosions. In the 2–50 s band, the very‐long period (VLP) signals associated with explosions are consistent with two stationary sources ...
CHOUET B, SACCOROTTI G, DAWSON P, MARTINI M, SCARPA, Roberto, DE LUCA G, MILANA G, CATTANEO M.   +7 more
openaire   +2 more sources

A review of the supercritical state of eruption‐fed volcanic density currents in subaerial and subaqueous settings

Sedimentology, Volume 73, Issue 5, Page 1331-1351, August 2026.
ABSTRACT Subaerial Pyroclastic Density Currents (PDCs) and Subaqueous Eruption‐Fed Density Currents (SEFDCs) produced during volcanic eruptions can present major hazards to surrounding communities and ecosystems. The bedforms deposited by these volcanic density currents can provide insights into the nature of transport and depositional processes, which
Shannon E. Frey, Martin Jutzeler, Rebecca J. Carey   +2 more
wiley   +1 more source

Coupling UV Camera‐Derived SO2 Emission Rate and Thermal Output at Mount Etna: A Decadal Analysis Across Eruptive Phases

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
Abstract At persistently degassing open‐vent volcanoes, SO2 emissions are especially useful to capture the transition from quiescence to eruption, though accurate quantification is challenged by complex volcanic plume dynamics and limited resolution of observations. Here, we present an exceptionally long (∼10–year) record of SO2 emission rates from the
Giovanni Lo Bue Trisciuzzi, Alessandro Aiuppa, Marcello Bitetto, Mauro Coltelli, Francesco Ciancitto, Gaetana Ganci, Mimmo Palano, Giuseppe Bilotta, Emilio Pecora, Paolo Principato, Angelo Vitale, Dario Delle Donne   +11 more
wiley   +1 more source

Low-frequency seismic signals recorded by OBS at Stromboli volcano (Southern Tyrrhenian Sea) [PDF]

, 2009
Five three-component broadband ocean bottom seismometers (OBSs) were deployed on the seafloor around the Aeolian Islands (Southern Tyrrhenian Sea). By comparing OBSs digital seismograms, we found a low-frequency seismicity recorded only at OBS05, the
Montuori, C., Sgroi, T., Favali, P., Agrusta, R.   +3 more
core   +1 more source