Mt Etna

Mount Etna, also known as Muncibe??u (beautiful mountain) in Sicilian and Mongibello in Italian (from the Latin mons and the Arabic gibel, both meaning mountain is an active stratovolcano on the east coast of Sicily, close to Messina and Catania. Its Arabic name was Jebel Utlamat (the Mountain of Fire). It is the largest active volcano in Europe,
currently standing 3,329 metres (10,922 ft) high, though this varies with summit eruptions; the mountain is 21 m (69 ft) lower now than it was in 1981. It is the highest mountain in Italy south of the Alps. Etna covers an area of 1,190 km² (460 sq mi) with a basal circumference of 140 km. This makes it by far the largest of the three active volcanoes in Italy, being about two and a half times the height of the next largest, Mount Vesuvius. Only Mount Teide in Tenerife surpasses it in the whole of the European region (though geographically Tenerife is an island of Africa). In Greek Mythology, the deadly monster Typhon was trapped under this mountain by Zeus, the god of the sky.
Mount Etna is one of the most active volcanoes in the world and is in an almost constant state of activity. The fertile volcanic soils support extensive agriculture, with vineyards and orchards spread across the lower slopes of the mountain and the broad Plain of Catania to the south. Due to its history of recent activity and nearby population, Mount Etna has been designated a Decade Volcano by the United Nations.

Mt Etna has the longest period of documented eruptions in the world. Etna is noted for the wide variety of eruption styles. The volcano is at its most spectacular when when both summit and flank eruptions occur simultaneously.

The structure of Mt Etna consists of a series of nested stratovolcanoes, characterised by summit calderas, the most important one being the Ellittico Caldera, which formed about 14,000-15,000 years ago.

Historically Mt Etna has produced effusive activity; however several pyroclastic deposits related to Plinian eruptions have been identified in the Holocene sequence. Under open vent conditions, ash emission only occurs during flank eruptions of Mt Etna volcano.

Structural and seismic data indicate that the regional deformation in the Etnean
area is generally dominated by N-S compression as the result of subduction of the African tectonic plate under the Eurasian plate.