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Mount Etna - Italy
Article by Jessica Ball
|Mount Etna in Eruption at Night|
Mount Etna night eruption: A night photo of Mount Etna producing an eruption of glowing ejecta in 2008. These spectacular eruptions can be seen from many parts of Sicily. Image copyright iStockphoto / Frizi.
Mount Etna: Introduction
Mount Etna is the highest and most active volcano in Europe. Towering above the city of Catania on the island of Sicily, it has been growing for about 500,000 years and is in the midst of a series of eruptions that began in 2013.
Etna has displayed a variety of eruption styles, including violent explosions and voluminous lava flows. More than 25% of Sicily's population lives on Etna's slopes, and it is the main source of income for the island, both from agriculture (due to its rich volcanic soil) and tourism.
Where is Mount Etna? Map showing the location of Mount Etna on the east coast of Sicily. Map by Geology.com and MapResources.
Nearby Volcanoes: Stromboli, Vesuvius
Table of Contents
|Simplified plate tectonics cross section|
Simplified plate tectonics cross section showing how Mount Etna is located above a subduction zone formed where the Eurasian and African plates collide. In this subduction zone, a window has torn in the subducting slab.
Mt. Etna: A view of snowcapped Mount Etna. Image copyright iStockphoto / Domenico Pellegriti.
Mount Etna: Plate Tectonic Setting
Mount Etna is associated with the subduction of the African plate under the Eurasian plate, which also produced Vesuvius and Campi Flegrei, but is part of a different volcanic arc (the Calabrian rather than Campanian). A number of theories have been proposed to explain Etna's location and eruptive history, including rifting processes, a hot spot, and intersection of structural breaks in the crust. Scientists are still debating which best fits their data, and are using a variety of methods to build a better image of the Earth's crust below the volcano.
VEI: The Most Explosive Volcanic Eruptions
|Ruins: House buried by Etna|
Ruins of a small house partially buried by volcanic debris from Mount Etna. Image copyright iStockphoto / Peeter Viisimaa.
-- In 122 BC, when an explosive eruption rained so much ash and lapilli onto the town of Catania that many of its buildings were destroyed by roof collapses, the town's inhabitants were exempted from paying taxes to Rome for ten years.
-- There have been two attempts to control the path of lava flows threatening to destroy the town of Catania. The first was in 1669, and the second was in 1992. During the 1992 attempt, the United States Marines worked with Italian volcanologists to develop "Operation Volcano Buster", in which they used explosives to blast a hole in a lava tunnel on Etna's flank and then dropped large blocks of concrete into the hole to try and stem the flow of the lava. Like the 1669 attempt, however, this plan was ultimately unsuccessful.
Mount Etna Geology and Hazards
Mount Etna consists of two edifices: an ancient shield volcano at its base, and the younger Mongibello stratovolcano, which was built on top of the shield. The basaltic shield volcano eruptions began about 500,000 years ago, while the stratovolcano began forming about 35,000 years ago from more trachytic lavas. The volcano's slopes currently host several large calderas which formed when the roofs of magma chambers collapsed inward, including the east-facing, horseshoe-shaped Valle de Bove.
Etna's current activity consists of continuous summit degassing, explosive Strombolian eruptions, and frequent basaltic lava flows. Ash clouds from the explosive eruptions are especially hazardous to aircraft, since ash that is pulled into a jet engine can melt, coat moving parts with a layer of glass, and cause the engine to shut down. These dangerous ash clouds are often visible from space.
Facts About Mount Etna
||Island of Sicily, Italy
||3,330 m (10,925 ft)
Etna has also produced pyroclastic flows, ashfalls, and mudflows, but the lava flows are the most immediately hazardous type of activity, especially to the city of Catania.
The lava flows themselves usually do not move fast enough to threaten humans, they can cover large areas and destroy crops and buildings. In the event of a large flank (fissure) eruption, evacuating the inhabitants of towns and cities near the volcano would be a huge challenge.
|Mt. Etna Eruption (October 30, 2002)|
Mount Etna ash plume: An oblique photograph of Mount Etna looking to the southeast taken by astronauts onboard the International Space Station on October 30, 2002. The dark plume rising from the top of the volcano is an ash cloud. The broad white cloud streaming from areas of lower elevation is smoke produced by forest fires ignited as a hot lava flow moved through a pine forest. The ash and smoke caused air traffic to be diverted and forced the closing of roads, schools and businesses. Larger Image.
|Mt. Etna Eruption (October 30, 2002)|
Mount Etna ash plume: An oblique photograph of Mount Etna on the west coast of the island of Sicily. This photo is looking to the southeast with the Mediterranean Sea in the background and was taken by astronauts onboard the International Space Station on October 30, 2002. The scene shows the ash plume from the eruption being carried by wind across the Mediterranean Sea to Libya, over 350 miles away. Larger Image.
|Sicilian Vineyard in the shadow of Mt. Etna|
A Sicilian vineyard growing in the shadow of Mount Etna. The inhabitants of Sicily must balance the advantage of rich volcanic soil with the dangers of losing their crops and farms to an eruption from the still-active volcano. Image copyright iStockphoto / Domenico Pellegriti.
Mount Etna: Eruption History
Etna's eruptions have been documented since 1500 BC, when phreatomagmatic eruptions drove people living in the eastern part of the island to migrate to its western end. The volcano has experienced more than 200 eruptions since then, although most are moderately small. Etna's most powerful recorded eruption was in 1669, when explosions destroyed part of the summit and lava flows from a fissure on the volcano's flank reached the sea and the town of Catania, more than ten miles away. This eruption was also notable as one of the first attempts to control the path of flowing lava.
The Catanian townspeople dug a channel that drained lava away from their homes, but when the diverted lava threatened the village of Paterno, the inhabitants of that community drove away the Catanians and forced them to abandon their efforts.
An eruption in 1775 produced large lahars when hot material melted snow and ice on the summit, and an extremely violent eruption in 1852 produced more than 2 billion cubic feet of lava and covered more than three square miles of the volcano's flanks in lava flows. Etna's longest eruption began in 1979 and went on for thirteen years; its latest eruption began in September 2013, and is still ongoing.
|More Etna Information|
Smithsonian Institution Global Volcanism Program: Etna page.
Gates, A.E. and Ritchie, D., 2007, Encyclopedia of Earthquakes and Volcanoes, Third Edition: New York, NY, Checkmark Books, 346 p.
Chester, D.K., 1985, Mount Etna: The Anatomy of a Volcano: Stanford, CA, Stanford University Press, 404 p.
Instituto Nazionale di Geophisica e Vulcanologia, Sezione di Catania (National Institute of Geophysics and Volcanology, Catanian Section)
Italy's Volcanoes: The Cradle of Volcanology Website.
"Zafferana Etnea Journal: It's Plug Up Mt. Etna or Go the Way of Pompeii." New York Times article, April 25, 1992.
About the Author
Jessica Ball is a graduate student in the Department of Geology at the State University of New York at Buffalo. Her concentration is in volcanology, and she is currently researching lava dome collapses and pyroclastic flows. Jessica earned her Bachelor of Science degree from the College of William and Mary, and worked for a year at the American Geological Institute in the Education/Outreach Program. She also writes the Magma Cum Laude blog, and in what spare time she has left, she enjoys rock climbing and playing various stringed instruments.
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