Stromboli is one of the most active volcanoes on Earth and has been erupting
almost continuously since 1932. Because it has been active for much of the
last 2,000 years and its eruptions are visible for long distances at night,
it is known as the "Lighthouse of the Mediterranean". It is among the
world's most visited volcanoes.
Stromboli is widely known for its spectacular eruptions which jet fountains
of molten rock from its lava-filled central crater. Because these eruptions
are so distinctive and well known, geologists use the word "Strombolian" to
clearly describe similar eruptive activity at other volcanoes.
Stromboli forms the northeastern-most of the Aeolian islands. Its base
begins over 1000 meters below the surface of the Tyrrhenian Sea and it rises
to an elevation of 924 meters above sea level.
|Map showing the location of Stromboli, in the Tyrrhenian Sea. Map by Geology.com and MapResources.
Nearby Volcanoes: Etna Vesuvius
Stromboli: Plate Tectonic Setting
Like Mount Etna on the island of Sicily, Stromboli is a part of the Calabrian volcanic arc. The volcanoes of the Calabrian arc are associated with the subduction of the African tectonic plate under the Eurasian plate. Stromboli is located on a NE-SW trending fault system, but the mechanisms which feed the volcano's magma chamber, and their relationship to the fault system, are poorly understood.
|Simplified plate tectonics cross section (A to B)
|Simplified plate tectonics cross-section showing how Stromboli is located above a subduction zone formed where the Eurasian and African plates collide. A three-dimensional view of this cross-section area is shown in
Figure 9 of Claudio Faccenna and others, 2007, Slab disruption, mantle circulation, and the opening of the Tyrrhenian basins, Geological Society of America, Special Paper 481, pages 153-169.
||Aeolian Islands, Italy
||924 m (3,031 ft)
Stromboli: Eruption History
Activity at Stromboli has been recorded by historians for more than 1,000 years, and varies from mild degassing to lava flows to violent explosive eruptions. Records from 1907 indicate that one explosion was strong enough to shatter windows in the island's villages, and strong explosions in 1930 were associated with an earthquake that also created a small tsunami. The most recent eruption began in 1932, and has continued essentially uninterrupted since then. Periodically, Stromboli's eruptive style transitions and vents near the summit produce lava flows that are funneled by the Sciara del Fuoco to the sea; the most recent of these occurred in 2002 and 2007. One theory that has been suggested to explain the transition is that the magma in Stromboli's summit conduit occasionally forces open dikes on the NW flank, and is erupted as lava flows rather than through gas-driven explosions.
|View of Stromboli erupting at sunset, jetting basaltic magma high in the air to form an incandescent "fountain". This is the type of eruption known as "Strombolian". Image © iStockphoto / lucamanieri.
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.
Find it on Geology.com
More from Geology.com
|Minerals: Information about ore minerals, gem materials and rock-forming minerals.|
A view of the island known as "Stromboli". A plume rises from the volcanic vent with the same name. The island has a population of a few hundred people. This view shows the northeast side of the island where most of their dwellings are located. Image © iStockphoto / miralex.
|Google Relief Map of Stromboli
|Google Maps terrain map of Stromboli. You can also use the "Sat" button in the upper right corner of the image to switch to a satellite image. View Larger Map
Stromboli Geology and Hazards
The island of Stromboli was built by a series of eruptions of potassium-rich basalt and basaltic andesite lavas. The first eruptions began about 200,000 years ago, and formed the now-eroded Strombolicchio volcano. Starting around 160,000 years ago, the island of Stromboli proper began forming. For the next 150,000 years, lava flows and pyroclastic deposits built a stratovolcano, which was eventually covered by pyroclastic deposits, lahars and lava flows. The Neostromboli period saw the formation of the modern volcanic edifice, which involved numerous flank and summit caldera collapses. The current eruptive vents are located at the top of the Sciara del Fuoco (Stream of Fire), a large collapse scar on the northwest side of the island which formed about 5,000 years ago.
Stromboli is the type location for the "Strombolian" style of eruptions. Strombolian eruptions are mild explosive events where "slugs" of gas periodically rise through a magma-filled volcanic conduit, burst at the surface, and throw bits of lava into the air. The lava falls as bombs (larger than about 3 inches in size) and scoria (smaller fragments), and eventually builds into a steep-sided volcanic cone.
The Sciara del Fuoco poses the most serious volcanic hazard on Stromboli. A catastrophic sector collapse would not only displace large volumes of material and possibly expose dike systems on the volcano's NW slope; it could also create a tsunami, which could cause much damage if it reached any of the other islands in the Aeolian archipelago or the Sicilian coast.
Stromboli venting steam. Stromboli is a stratovolcano that begins at the
bottom of the Tyrrhenian Sea and rises to an elevation of 924 meters (3031
feet) above sea level. This is a view of the eastern side of the island and
the Sciara del Fuoco (Stream of Fire) collapse scar, which funnels tephra
and lava flows to the sea. Image © iStockphoto / ToolX.
Did You Know?
In Jules Verne's novel Journey to the Center of the Earth (Voyage au Centre de la Terre), Axel and Otto Lidenbrock emerge from their subterranean journey from the volcano on Stromboli:
"Right above our heads, at a great height, opened the crater of a volcano from which escaped, from one quarter of an hour to the other, with a very loud expression, a lofty jet of flame mingled with pumice stone, cinders, and lava. I could feel the convulsions of Nature in the mountain, which breathed like a huge whale, throwing up from time to time fire and air through its enormous vents...
'Come si noma questa isola?' - 'What is the name of this island?'
'Stromboli,' replied the rickety little shepherd, dashing away from Hans and disappearing into the olive groves. We thought little enough about him.
"Stromboli! What effect on the imagination did these few words produce! We were in the center of the Mediterranean, amidst the eastern archipelago of mythological memory, in the ancient Strongylos, where Aeolus kept the wind and the tempest chained up. And those blue mountains, which rose toward the rising of the sun, were the mountains of Calabria."
Journey to the Center of the Earth, Chapter XLIII
|More Stromboli Information
Smithsonian Institution Global Volcanism Program Website:
USGS Cascades Volcano Observatory Website: Italy Volcanoes and Volcanics Italy Volcanoes and Volcanics
Gates, A.E. and Ritchie, D., 2007, Encyclopedia of Earthquakes and Volcanoes, Third Edition: New York, NY, Checkmark Books, 346 p.
Italy's Volcanoes: The Cradle of Volcanology Website.
Mattia et al., 2008, Geophysical investigations of the plumbing system of Stromboli volcano (Aeolian Islands, Italy). Journal of Volcanology and Geophysical Research, v. 176, n. 4, p. 529-540.
Verne, Jules, 1864, Journey to the Center of the Earth (Voyage au Centre de la Terre).