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Complejo estratovolcán Currently about 3329 m (changing due to eruptive activity and collapse of its crater rims)
Sicily, Italy, 37.75°N / 14.99°E
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Erupciones del volcán Etna:
Near continuously active; some major historic eruptions include 122 BC (large Plinian outbursts that created the small caldera of the "Cratere del Piano"), 1669 AD (devastating flank eruption that destroyed 15 villages and part of Catania), 1787 (Subplinian eruption and one of the most spectacular summit eruptions on record - lava fountains reportedly up to 3000 m high).Eruptions since 1950 (f: flank / s: summit activity):
1950 (s), 1950-51(f), 1955 (s), 1956 (s), 1956 (f), 1957 (s),1960 (s), 1961 (s), 1964 (f), 1964 (s), 1966 (s), 1966-1971(s), 1968 (f), 1971(f), 1972-1973 (s), 1974 (f), 1974-1975 (s), 1975-1977 (f), 1977-1978 (s), 1978 (f), 1979(s), 1979 (f), 1980 (s), 1981 (s), 1981 (f),1982-1983 (s), 1983(f), 1984(s), 1985(s), 1985(f), 1986(s), 1986-1987 (f), 1987(s), 1988(s), 1989(s), 1989(f), 1990 (s), 1991-93(f), 1995(s), 1996(s), 1997 (s), 1998 (s), 1999 (s), 2000 (s), 2001(s), 2001 (f), 2002(s), 2002-03(f), 2004-2005 (f), 2006 (s), 2007 (s), 2008-2009 (f), 2010(s), 2011-2013(s), 2014-18, 2018(f), 2019 (s)
Typical eruption style:
Efusivas (coladas de lava) y ligeramente explosivo (estromboliana) erupciones. Tanto cumbre y frecuentes erupciones de flanco, el último parece estar ocurriendo en racimos que duran unos pocos a unas pocas decenas de años.
Últimos terremotos cercanos
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The best place to stay near Mt Etna is no doubt the Corsaro hotel, located a few 100 m from the cable car station at La Sapienza cable car station on Etna South: Hotel Corsaro
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Etna volcano updates and eruption news:
Etna volcano (Italy): continuing ash emissions
lunes feb 18, 2019 10:57 | POR: T
Etna erupting ash from NE crater as seen last evening from Lipari (!) during extremely clear weather (image: Emanuela Carone / VolcanoDiscovery Italia)
For more than a month, sometimes intense ash emissions have been taking place from the NE crater and, to lesser extent, from Bocca Nuova.
These ashes are currently believed not to be formed by fresh magma rising in the conduits, but instead are composed of older material that is now being vented from the inner conduits. It can be interpreted as the surface expression of internal re-adjustments that followed the brief, but intense eruption at Christmas last year, which drained (some of the) magma from the conduits and reservoirs.
Another factor are likely the seismic events around the volcano in the days and weeks after, which also might have caused internal shifts in magma storage.
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