Report on Stromboli (Italy) — 2 April-8 April 2003

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 2 April-8 April 2003
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2003. Report on Stromboli (Italy). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 2 April-8 April 2003. Smithsonian Institution and US Geological Survey.

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Stromboli

Italy

38.789°N, 15.213°E; summit elev. 924 m

All times are local (unless otherwise noted)


A strong explosion at Stromboli on 5 April around 0915 produced a mushroom-shaped ash cloud that rose several hundred meters above the volcano. Rocks ejected during the explosion damaged two homes and several roads in the town of Ginostra ~ 2 km SW of Stromboli's summit. There were no reports of injuries.

Geologic Background. Spectacular incandescent nighttime explosions at this volcano have long attracted visitors to the "Lighthouse of the Mediterranean." Stromboli, the NE-most of the Aeolian Islands, has lent its name to the frequent mild explosive activity that has characterized its eruptions throughout much of historical time. The small, 924-m-high island is the emergent summit of a volcano that grew in two main eruptive cycles, the last of which formed the western portion of the island. The Neostromboli eruptive period from about 13,000 to 5000 years ago was followed by formation of the modern Stromboli edifice. The active summit vents are located at the head of the Sciara del Fuoco, a prominent horseshoe-shaped scarp formed about 5000 years ago as a result of the most recent of a series of slope failures that extend to below sea level. The modern volcano has been constructed within this scarp, which funnels pyroclastic ejecta and lava flows to the NW. Essentially continuous mild strombolian explosions, sometimes accompanied by lava flows, have been recorded for more than a millennium.

Sources: Agence France-Presse (AFP), Associated Press, Stromboli On-Line