Report on Stromboli (Italy) — 15 October-21 October 2014
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 15 October-21 October 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, 15 October-21 October 2014. Smithsonian Institution and US Geological Survey.
38.789°N, 15.213°E; summit elev. 924 m
All times are local (unless otherwise noted)
On 16 October INGV reported that during the previous two months effusive activity continued at Stromboli from a vent at 650 m elevation. Lava flows traveled as far as the lower part of the Sciara del Fuoco. During the previous few weeks there were sporadic ash emissions from summit vents that were sometimes accompanied by ejected incandescent pyroclastic material.
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.