Report on Stromboli (Italy) — 22 December-28 December 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 22 December-28 December 2010
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2010. Report on Stromboli (Italy). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 22 December-28 December 2010. Smithsonian Institution and US Geological Survey.
38.789°N, 15.213°E; summit elev. 924 m
All times are local (unless otherwise noted)
INGV-CT reported that a sequence of three explosions from Stromboli's "S" vent in the S part of the crater terrace were recorded on 19 December by thermal monitoring cameras in Vancori and Pizzo. The first explosion ejected coarse-grained pyroclastic material, followed by fine-grained tephra, more than 250 m above the crater terrace. A slightly less intense explosion occurred less than a minute later. The third and weakest explosion ejected material 180-200 m above the crater, generating an ash plume that dispersed over the W and NE parts of the island.
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.