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The 1669 eruption of Mount Etna is the largest-recorded historical eruption of the volcano on the east coast of Sicily, Italy.After several weeks of increasing seismic activity that damaged the town of Nicolosi and other settlements, an eruption fissure opened on the southeastern flank of Etna during the night of 10–11 March.
This is an accepted version of this page This is the latest accepted revision, reviewed on 21 January 2025. Active volcano on the east coast of Sicily, Italy "Mongibello" redirects here. For the fictional location, see The Talented Mr. Ripley. Mount Etna Etna with the city of Catania in the foreground (December 2007) Highest point Elevation 3,403 m (11,165 ft)(varies) Prominence 3,403 m ...
September 2004 Stromboli eruption. Stromboli (/ ˈ s t r ɒ m b ə l i / STROM-bə-lee, Italian: [ˈstromboli]; Sicilian: Struògnuli [ˈʂː(ɽ)wɔɲɲʊlɪ]) is an island in the Tyrrhenian Sea, off the north coast of Sicily, containing Mount Stromboli, one of the four active volcanoes in Italy.
Articles relating to Mount Etna, its history, and its prominent depictions in classical mythology.It is an active stratovolcano on the east coast of Sicily, Italy, in the Metropolitan City of Catania, between the cities of Messina and Catania.
This is a list of active and extinct volcanoes in Italy. Name Elevation (m) Elevation (ft) Coordinates Most Recent Eruption Alicudi: 675: 2215 28,000 YBP: Amiata ...
The volcanism of Italy is due chiefly to the presence, a short distance to the south, of the boundary between the Eurasian Plate and the African Plate. Italy is a volcanically active country, containing the only active volcanoes in mainland Europe (while volcanic islands are also present in Greece, in the volcanic arc of the southern Aegean).
Eruptions at Italy's Mount Etna and the smaller Stromboli volcano spewed hot ash and lava, raising alert levels on the Mediterranean island of Sicily and forcing a temporary shutdown of Catania ...
The geology of Sicily (a large island located at Italy's southwestern end) records the collision of the Eurasian and the African plates during westward-dipping subduction of the African slab since late Oligocene. [1] [2] Major tectonic units are the Hyblean foreland, the Gela foredeep, the Apenninic-Maghrebian orogen, and the Calabrian Arc.
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