Tours privados en el volcán Etna
: Descubra el volcán activo más grande de Europa en privado, visitas guiadas tours de 1 día. Tours pueden personalizarse para diferentes intereses y niveles de condición física.
más en el volcán Etna ...
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
Etna webcams / datos en tiempo realEtna videos de volcán
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-ongoing(f)
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
Tuesday, Nov 15, 2011
The ongoing eruption at Etna, seen from Radiostudio 7 webcam (http://www.radiostudio7.it) located at Belvedere
A little bit later, the lava flow already has reached the slope into Valle del Bove and lava fountains are seen from the summit vent as well.
A new eruptive episode is in progress at the New SE crater of Etna today. Starting this morning, tremor has been rising steeply and at the time of writing, the first strombolian explosions, or even small lava fountains, and perhaps already a small lava flow can be seen emerging from the SE-trending fissure cutting through the cone. All signs point towards that this is going to be the long-awaited 18th paroxysm of the New SE crater in 2011, following the previous one on 23 Oct after 23 days, the longest-so-far interval since July. [leer todo
Sunday, Oct 23, 2011
Another paroxysmal eruption (the 17th in 2011) is in progress at Etna's New SE crater at the time of writing. The volcanic tremor recorded by INGV has risen sharply to 50 times above background levels, and strong strombolian activity and/or lava fountains, as well as a lava flow into the Valle del Bove are visible from various webcams. ...màs
Sunday, Oct 09, 2011
The lava fountains from the lower part of the SE fissure at the beginning of the 16th paroxysm of Etna's New SE crater, ca. 15h30, 8 Oct 2011
Following 10 days of quiet, a new paroxysmal eruption (nr 16 in 2011) took place from the New SE crater of Etna volcano during the afternoon of 8 October 2011. ...màs
Wednesday, Sep 28, 2011
lava flows from the 15th paroxysm of the New SE crater of Etna volcano (webcam image from http://www.radiostudio7.it/webcam.asp)
The 15th paroxysm of Etna's New SE crater occurred in the evening of 28 Sep, a few days earlier than what statistically had been expected (based on thze steady increasing intervals between the past similar events). ...màs
Monday, Sep 19, 2011
Tremor measured by INGV Catania during the 14th paroxysm
The 14th paroxysm of Etna's New SE crater is in progress at the time of writing. Bad weather conditions hide the eruption, but the seismic signals of INGV Catania show that a major eruptive episode is occurring. Since 9am, volcanic tremor has been gradually increasing to (at the moment) 30+ times background levels, and is still rising. Most likely, lava fountains are being ejected from vents inside the crater and lava flows descending into Valle del Bove if the new episode is similar to the previous ones. ...màs
Thursday, Sep 08, 2011
The 13th paroxysm from Etna's New SE crater occurred this morning between ca. 8 and 10am, following a steep increase in tremor and a short period of rapidply increasing strombolian activity from several vents inside the new crater. The eruption intensified into lava fountains generating a tall ash plume drifting SSE and showering a narrow sector south of Etna with ash. ...màs
Monday, Aug 29, 2011
Another powerful eruption with an intense peak activity of tall lava fountains - a so-called paroxysm - occurred at Etna volcano's New SE crater earlier today. This marks the 12th event of the series in 2011 so far. The main phase of the eruption lasted between around 5 and 7 am local time. ...màs
Saturday, Aug 20, 2011
Tremor amplitude at 9h40 local time...
The 11st paroxysm of Etna's New SE crater is taking place. Strombolian activity and increased degassing started late during the night and early morning. The activity increased into lava fountains producing a tall ash column probably between 8 and 9 am. A lava flow is emitted that descends into the Valle del Bove.
Friday, Aug 12, 2011
Beginning lava fountains at Etna (RadioStudio7 webcam)
View of Etna from distance (RadioStudio7 webcam)
The 10th paroxysm of the New SE crater at Etna volcano is in progress. Strombolian activity as well as tremor amplitude increased sharply at around 9am local time and are now (ca. 10 am local time) becoming lava fountains.
Strombolian activity has restarted at the "New SE crater" of Etna volcano, which means that, most likely, the 10th paroxysm is under way - IF the volcano behaves as during the past 9 episodes, where strombolian activity increased to violent lava fountain eruptions within 12-72 hours after the onset of such strombolian activity. ...màs
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: Una tercera configuración tectónica donde se produce la actividad volcánica se cree que es el resultado de plumas del manto y no están directamente relacionada a los límites de la placa. Llamado punto caliente los volcanes entran en esta categoría.