Mount Etna is the largest active volcano in Italy. Located near the east coast of the island of Sicily, it is 10,900 feet (3,329 meters) tall with a base circumference of about 93 miles (150 kilometers). It is also the volcano with the longest record of continuous eruption.
Mount Etna is a series of nested stratovolcanoes with four distinct summit craters. There are two central craters, called Bocca Nuova and Voragine; the Northeast crater; and the newest Southeast crater, which was formed by an eruption in 1978. Strombolian eruptions, which produce ash, tephra and lava fountains, are fairly common in these craters. The eruptions of early 2013 were mostly strombolian eruptions. The January 2013 eruption was from Bocca Nuova, and the February eruptions are most noticeable from the Southeast crater.
The mountain's largest feature is the Valle del Bove (Valley of the Ox), a large horseshoe-shaped caldera on the eastern slope. There are numerous fissures and vents on the flanks of the volcano that often produce slow-moving pyroclastic flows at low altitudes. These flows threaten agriculture, public utilities and transportation in the heavily populated towns surrounding the mountain.
History of eruptions
Mount Etna has a longer written record of eruptions than any other volcano. The first recorded observation of a Mount Etna eruption was written by Diodorus Siculus in 425 B.C. The mountain was also described by the Roman poet Virgil in the Aenid. Roman records from 122 B.C. indicate a large eruption blocked the sun for several days and caused widespread damage to the town of Catania on the coast. Roman taxes were cancelled for 10 years to help locals rebuild. Catania was in the path of destruction again in A.D. 40, 1169 and 1185.
Then, in 1669, in one of the mountains most destructive eruptions, 1,500 people were killed when the town of Nicoli was destroyed by an earthquake originating beneath Mount Etna. In Catania, the townspeople made one of the first known attempts at damage control by digging a trench to divert the lava slowly advancing upon the town. Unfortunately, the diverted lava then threatened the nearby town of Paterno, causing a brief battle that halted the attempt. Lava overtopped the Catania city wall and obliterated half the town again.
Mount Etna has almost continuous eruptive activity near the summit craters and in the Valle del Bove, but these vertical eruptions pose little threat to inhabitants. Flank eruptions cause more damage as vents and fissures can open at much lower, inhabited elevations. In 1928, the village of Mascali was obliterated in only two days when a fissure opened up near the foot of the mountain. In 1960, agricultural land was destroyed by ejected lava and ash fall.
In 1992, the town of Zafferana was endangered by lava flow and was saved by a more successful attempt at volcano control. Earthen dams were erected to try to contain the lava in the Valle del Bove but were shortly overtopped by the flowing lava. U.S. Marines were then called upon to help with “Operation Volcano Buster” by flying cargo helicopters to drop huge concrete blocks at the edge of the lava tunnel. Additional blocks, suspended underneath the helicopters were used like croquet mallets to knock the grounded blocks into the mouth of the tunnel. These efforts slowed the progression of the lava for the two weeks necessary to dig a diversionary channel for the lava, which was stopped just about half a mile (850m) from the city limit. Unfortunately several homes, fields, orchards and vineyards around the town were completely buried. [Countdown: History's Most Destructive Volcanoes]
Sitting on a fault
There are many theories as to why Mount Etna is so active. Mount Etna, like other Mediterranean volcanoes such as Stromboli and Vesuvius, rests on the subduction boundary where the African tectonic plate is being pushed under the Eurasian plate. Although they appear to be geographically close, Etna is actually quite different from the other volcanoes. It is actually part of a different volcanic arc. Etna, rather than sitting directly on the subduction zone, actually sits just in front of it.
Etna sits on the active fault between the African plate and the Ionian microplate, which are both being subducted together beneath the Eurasian plate. Current evidence suggests that the much lighter Ionian plate may have broken and part of it forced backwards by the much heavier African plate. Magma directly from Earth’s mantle layer is being sucked into the space created by the tilting Ionian slab. This phenomenon would account for the kinds of lava produced by eruptions of Mount Etna, which resemble the type of lava produced along deep sea trenches where mantle magma is forced through Earth’s crust. Lava from the other volcanoes is the type produced by the melting of existing crust rather than the upwelling of the mantle layer. There are other possible explanations for the unusual activity of Etna, such as existence of a hotspot or a window-like crack in the African plate.
In spite of the mystery and the danger, locals call Mount Etna “Mongibello,” the beautiful mountain. They grow olives, grapes and fruit in the soil enriched by the fallen ash. Tourism thrives as visitors come to ski or to marvel at the display of fire fountains during an eruption. One resident of Zafferana expressed the local’s love of their fiery mountain. As he left his home for the last time before it was engulfed by the lava, he set the table with a snow-white cloth and a bottle of his finest wine as a gift for Mongibello.