Report on Stromboli (Italy) — 18 June-24 June 2014

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 18 June-24 June 2014
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2014. Report on Stromboli (Italy). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 18 June-24 June 2014. 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)


INGV reported two episodes of effusive activity at Stromboli, one on 17 June and another on 22 June. Activity on 17 June occurred in the morning within the central part of the crater terrace (Bocca S2) and included explosive spattering. This activity lasted for a few hours and produced a small lava flow directed toward Pizzo Sopra la Fossa. A sharp increase in Strombolian activity began from all of the craters on 22 June, depositing voluminous material along the Sciara del Fuoco. A lava flow ~200 m long extended from the mouth of N2 (within the N part of the crater terrace). During the evening this flow slowed, and then stalled the following day when Strombolian activity decreased.

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.

Source: Sezione di Catania - Osservatorio Etneo (INGV)