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Descoperirea, publicata in revista Science, demonteaza teoria conform careia comportamentul lui Stromboli, caraterizat de cel putin 2.500 ani de explozii care se repeta la fiecare 15-20 minute si de lansarea unor bucati de lava pana la 200 metri inaltime, s-ar datora formarii de bule de gaz la suprafata.
Studiul a fost realizat de Mike Burton si Filippo Muré de la Institutul national de geofizica si vulcanologie (Ingv) din Catania, Italia, impreuna cu Patrick Allard, cercetator in cadrul Grupului de Stiinte ale Pamantului din Franta si Alessandro La Spina, doctorand in geochimie la Universitatea din Palermo.
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