Report on Etna (Italy) — 11 June-17 June 2003
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
11 June-17 June 2003
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2003. Report on Etna (Italy). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 11 June-17 June 2003. Smithsonian Institution and US Geological Survey.
37.748°N, 14.999°E; summit elev. 3357 m
All times are local (unless otherwise noted)
The Toulouse VAAC reported that the Etna web video camera showed an ash plume below ~4 km a.s.l. drifting SE on 7 June. According to the Italy's Volcanoes website, in early June intense gas emissions took place from Northeast Crater, often feeding a plume that extended tens of kilometers. At Bocca Nuova crater strong gas emissions and occasional strong explosions occurred, but no fresh volcanic material was ejected beyond the pit. Gas was emitted from two pits in Voragine crater. There was a progressive increase in the number and activity of fumaroles near Southeast Crater's summit and the S flank.
Geological Summary. Mount Etna, towering above Catania on the island of Sicily, has one of the world's longest documented records of volcanism, dating back to 1500 BCE. Historical lava flows of basaltic composition cover much of the surface of this massive volcano, whose edifice is the highest and most voluminous in Italy. The Mongibello stratovolcano, truncated by several small calderas, was constructed during the late Pleistocene and Holocene over an older shield volcano. The most prominent morphological feature of Etna is the Valle del Bove, a 5 x 10 km caldera open to the east. Two styles of eruptive activity typically occur, sometimes simultaneously. Persistent explosive eruptions, sometimes with minor lava emissions, take place from one or more summit craters. Flank vents, typically with higher effusion rates, are less frequently active and originate from fissures that open progressively downward from near the summit (usually accompanied by Strombolian eruptions at the upper end). Cinder cones are commonly constructed over the vents of lower-flank lava flows. Lava flows extend to the foot of the volcano on all sides and have reached the sea over a broad area on the SE flank.