LE NOSTRE ULTIME NEWS
The final programme of TEPHRA 2026 – International School of Volcanology, taking...
a cura di Gianfilippo De AstisSotto il cielo stellato delle Eolie, la serata sociale...
Si è conclusa a Torino la 19ª edizione delle International Earth Science...
a cura di Roberto ScandoneCome altre volte, alcuni giorni fa ho tentato di contattare...
Si è chiusa con uno straordinario successo di partecipazione e contenuti la...
A cura di Marco Viccaro Il prologo dell’eruzioneL’eruzione dell’Etna...
A cura di Lisetta GiacomelliLa formazione di aggregati, detti pisoliti o lapilli...
Siamo lieti pubblicare il programma del Festival Vulcani – Etna 2026, che si...
Care Socie e cari Soci, è stato pubblicato il programma definitvo...
International School of Volcanology 2026TEPHRA (Training in Eruptive Processes, Hazards...
PUBAIV
LE ULTIME PUBBLICAZIONI DEI NOSTRI SOCI
Recurrent evacuation of mantle mush in ocean islands revealed by clinopyroxene from La Palma
Caracciolo A., Ubide T., Ágreda-López M., Herrera R., Marquez A., González-García D., Huertas M. J., Ancochea E., Chicharro N., Coello-Bravo J. J., Petrelli M.
Temporal variations in magma plumbing influence eruption priming and the interpretation of unrest signals, yet remain poorly constrained in low-flux ocean island volcanoes. Here, we examine temporal changes in the active volcanic system beneath La Palma,...
Volcaniclastic deposit failure as a source of pyroclastic density currents during the 1944 eruption of Vesuvius
Natale J., Falasconi A., Grillo T. O., Bevilacqua A., Buono G., Favalli M., Fornaciai A., Frontoni A., Giordano G., Intrieri E., Nave R., Pappalardo L., Vona A., Di Traglia F.
Pyroclastic density currents (PDCs) are among the most lethal volcanic phenomena and are mainly generated by column collapse, lateral blasts, or dome failure. An additional but still poorly constrained hazard is represented by PDCs produced by the collapse...
Reappraisal of Holocene Caldera Resurgence at Campi Flegrei (Southern Italy): A Long-Lived Magma-Driven Resurgent Dome System
Natale J., Vitale S.
Caldera systems commonly experience inner resurgence, which shapes patterns of volcanic activity. However, incomplete reconstructions of past ground deformation can lead to incorrect recognition of precursory signals. The Campi Flegrei caldera (Italy)...
Unravelling the gap between the probabilistic volcanic hazard and risk perception: A comparative study of tephra fallout at Etna and Vesuvius volcanoes
Mele D., Lanciano T., Caporale D., Bellucci Sessa E., Massaro S., Nave R., Patimo R., Piazza R., Puglisi G., Rainò S., Rinaldi A., Scollo S., Sulpizio R.
Volcanic risk management frequently encounters a significant gap between Probabilistic Volcanic Hazard Assessment and subjective risk perception. This study addresses this issue by comparing communities exposed to tephra fallout from two contrasting volcanoes...
Mafic-ultramafic igneous rocks as a source of reactive phosphorus for the origin of life
Baidya A.S., Walton C.R., Kalita J., Szilas K., Viccaro M., Savage P.S., Allison S., Nisbet E.G., Schönbächler M., Mikhail S., Stüeken E.E.
Phosphite and pyrophosphate - reduced and polymerized forms of phosphorus - may have played a central role in prebiotic chemistry owing to their higher reactivity and solubility, yet their geological sources remain uncertain. Here we show that mafic–ultramafic...