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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 (11,165 ft) Ranked 54th
Isolation	998.79 km (620.62 mi)
Listing	Ultra
Coordinates	37°45.3′N 14°59.7′E / 37.7550°N 14.9950°E / 37.7550; 14.9950
Naming
Native name	Muncibbeḍḍu (Sicilian)
Geography
Mount EtnaMetropolitan City of Catania, Sicily, ItalyShow map of SicilyMount EtnaMount Etna (Italy)Show map of Italy
Geology
Rock age	350,000 – 500,000 years
Mountain type	Stratovolcano
Last eruption	June 7th, 2024
UNESCO World Heritage Site
Criteria	Natural: viii
Reference	1427
Inscription	2013 (37th Session)
Area	19,237 ha
Buffer zone	26,220 ha

Mount Etna, or simply Etna (Italian: Etna [ˈɛtna] or Mongibello [mondʒiˈbɛllo]; Sicilian: Muncibbeḍḍu [mʊntʃɪbˈbɛɖɖʊ] or 'a Muntagna; Latin: Aetna; Ancient Greek: Αἴτνα and Αἴτνη), is an active stratovolcano on the east coast of Sicily, Italy, in the Metropolitan City of Catania, between the cities of Messina and Catania. It is located above the convergent plate margin between the African Plate and the Eurasian Plate. It is one of the tallest active volcanoes in Europe, and the tallest peak in Italy south of the Alps with a current height (September 2024) of 3,403 m (11,165 ft), though this varies with summit eruptions. For instance, in 2021 the southeastern crater reached a height of 3,357 m, but was then surpassed by the Voragine crater after the summer 2024 eruptions.

Etna covers an area of 1,190 km (459 sq mi) with a basal circumference of 140 km (87 miles). 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 on Tenerife in the Canary Islands surpasses it in the whole of the European–North-African region west of the Black Sea.

In Greek mythology, the deadly monster Typhon was trapped under this mountain by Zeus, the god of the sky and thunder and king of gods, and the forges of Hephaestus were said also to be underneath it.

Mount Etna is one of the world's most active volcanoes and is in an almost constant state of activity. The fertile volcanic soils produced from this activity 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. In June 2013, it was added to the list of UNESCO World Heritage Sites.

Etymology and mythology

One view is that the word Etna is from the Greek αἴθω (aíthō), meaning "I burn", through an iotacist pronunciation. Another view is that the name is derived from the Phoenician word attuna meaning 'furnace' or 'chimney'. In Classical Greek, it is called Αἴτνη (Aítnē), a name given also to Catania and the city originally known as Inessa. In Latin it is called Aetna. In Arabic, it is called Jabal al-Nār (جبل النار, 'the Mountain of Fire'). According to both Roman and Greek mythology, Vulcan/Hephaestus, the god of blacksmithing, had his forge under mount Etna.

The volcano is also known as Muncibbeḍḍu in Sicilian and Mongibello in Italian, generally regarded as deriving from the Romance word monte/munti plus the Arabic word jabal (جبل), both meaning 'mountain'. According to another hypothesis, the term comes from the Latin Mulciber (qui ignem mulcet, 'he who placates the fire'), one of the Latin names of the god Vulcan. Today, the name Mongibello is used for the area of Mount Etna containing the two central craters, and the craters located southeast and northeast of the volcanic cone.

The name Mongibel is found in Arthurian Romance, as the name of the otherworld castle (or realm) of Morgan le Fay and her half-brother, King Arthur, localised at Etna, according to traditions concerning them derived from the stories told by the Breton conteurs who accompanied the Norman occupiers of Sicily. What were originally Welsh conceptions concerning a dwarf king of a paradisal, Celtic underworld became attached to the quasi-historic figure of Arthur as "Ruler of the Antipodes" and were then transplanted into a Sicilian milieu, by Bretons impressed by the already otherworldly associations of the great, volcanic mountain of their new home. Mediaevalist Roger Sherman Loomis quotes passages from the works of Gervase of Tilbury and Caesarius of Heisterbach (dating from the late twelfth century) featuring accounts of Arthur's returning of a lost horse which had strayed into his subterranean kingdom beneath Etna. Caesarius quotes as his authority for the story a certain canon Godescalcus of Bonn, who considered it a matter of historical fact of the time of Emperor Henry's conquest of Sicily circa 1194. Caesarius employs in his account the Latin phrase in monte Gyber ('within Etna') to describe the location of Arthur's kingdom.

The Fada de Gibel of the Castle of Gibaldar (Fairy of Etna) appears in Jaufre, the only surviving Arthurian romance in the Occitan language, the composition of which is dated to between 1180 and 1230. However, in Jaufre, while it is clear from her name that the fairy queen in question is Morgan le Fay, the rich underworld queendom of which she is the mistress is accessed not through a fiery grotto on the slopes of Etna, but through a 'fountain' (i.e., a spring) – a circumstance more in keeping with Morgan's original watery, rather than fiery, associations, before her incorporation into the folklore of Sicily. Another Sicilian conception of the fairy realm or castle of Morgan le Fay is the Fata Morgana, an optical phenomenon common in the Strait of Messina.

History of volcanic eruptions

Eruptions of Etna follow multiple patterns. Most occur at the summit, where there are five distinct craters: the Northeast Crater, the Voragine, the Bocca Nuova, and two at the Southeast Crater Complex. Other eruptions occur on the flanks, which have more than 300 vents ranging in size from small holes in the ground to large craters hundreds of metres across. Summit eruptions can be highly explosive and spectacular but rarely threaten the inhabited areas around the volcano. In contrast, flank eruptions can occur down to a few hundred metres altitude, close to or even well within inhabited areas. Numerous villages and small towns lie around or on cones of past flank eruptions. Since the year AD 1600, at least 60 flank eruptions and countless summit eruptions have occurred; nearly half of these have happened since the start of the 20th century. Since 2000, Etna has had four flank eruptions – in 2001, 2002–2003, 2004–2005, and 2008–2009. Summit eruptions occurred in 2006, 2007–2008, January–April 2012, in July–October 2012, December 2018, and again in February 2021.

Geological history

Volcanic activity first took place at Etna about 500,000 years ago, with eruptions occurring beneath the sea off the ancient coastline of Sicily. About 300,000 years ago, volcanism began occurring to the southwest of the summit (centre top of the volcano), then activity moved towards the present centre 170,000 years ago. Eruptions at this time built up the first major volcanic edifice, forming a stratovolcano in alternating explosive and effusive eruptions. The growth of the mountain was occasionally interrupted by major eruptions, leading to the collapse of the summit to form calderas.

From about 35,000 to 15,000 years ago, Etna experienced some highly explosive eruptions, generating large pyroclastic flows, which left extensive ignimbrite deposits. Ash from these eruptions has been found as far away as south of Rome's border, 800 km (497 mi) to the north.

Thousands of years ago, the eastern flank of the mountain experienced a catastrophic collapse, generating an enormous landslide in an event similar to that seen in the 1980 eruption of Mount St. Helens. The landslide left a large depression in the side of the volcano, known as 'Valle del Bove' (Valley of the Ox). Research published in 2006 suggested this occurred around 8,000 years ago, and caused a huge tsunami, which left its mark in several places in the eastern Mediterranean.

The steep walls of the valley have suffered subsequent collapses on numerous occasions. The strata exposed in the valley walls provide an important and easily accessible record of Etna's eruptive history.

The most recent collapse event at the summit of Etna is thought to have occurred about 2,000 years ago, forming what is known as the Piano Caldera. This caldera has been almost entirely filled by subsequent lava eruptions but is still visible as a distinct break in the slope of the mountain near the base of the present-day summit cone.

Mount Etna is moving towards the Mediterranean Sea at an average rate of 14 mm (0.55 in) per year, the massif sliding on an unconsolidated layer above the older sloping terrain.

Historical eruptions

The first known record of eruption at Etna is that of Diodorus Siculus.

In 396 BCE, an eruption of Etna reportedly thwarted the Carthaginians in their attempt to advance on Syracuse during the Second Sicilian War.

A particularly violent explosive (Plinian) summit eruption occurred in 122 BCE, and caused heavy tephra falls to the southeast, including the town of Catania, where many roofs collapsed. To help with reconstruction after the devastating effects of the eruption, the Roman government exempted the population of Catania from paying taxes for ten years.

The Roman poet Virgil gave what was probably a first-hand description of an eruption in the Aeneid.

During the first 1500 years CE, many eruptions went unrecorded (or records have been lost); among the more significant are: (1) an eruption in about 1030 CE near Monte Ilice on the lower southeast flank, which produced a lava flow that travelled about 10 km, reaching the sea north of Acireale; the villages of Santa Tecla and Stazzo are built on the broad delta built by this lava flow into the sea; (2) an eruption in about 1160 (or 1224), from a fissure at only 350–450 m (1,148–1,476 ft) elevation on the south-southeast flank near the village of Mascalucia, whose lava flow reached the sea just to the north of Catania, in the area now occupied by the portion of the city named Ognina.

Rabban Bar Sauma, a Chinese traveller to the West, recorded the eruption of Etna on 18 June 1287.

The 1669 eruption, Etna's most destructive since 122 BCE, started on 11 March 1669 and produced lava flows that destroyed at least 10 villages on its southern flank before reaching the city walls of the town of Catania five weeks later, on 15 April. The lava was largely diverted by these walls into the sea to the south of the city, filling the harbour of Catania. A small portion of lava eventually broke through a fragile section of the city walls on the western side of Catania and destroyed a few buildings before stopping in the rear of the Benedictine monastery, without reaching the centre of the town. Contrary to widespread reports of up to 15,000 (or even 20,000) human fatalities caused by the lava, contemporaneous accounts written both in Italian and English mention no deaths related to the 1669 eruption (but give very precise figures of the number of buildings destroyed, the area of cultivated land lost, and the economic damage). Therefore, it is uncertain where the enormous number of fatalities can be attributed. One possibility is confusion between this eruption and an earthquake that devastated southeast Sicily (including Catania) 24 years later in 1693. A study on the damage and fatalities caused by eruptions of Etna in historical times reveals that only 77 human deaths are attributable with certainty to eruptions of Etna, most recently in 1987 when two tourists were killed by a sudden explosion near the summit.

Since 1750, seven of Etna's eruptions have had durations of more than 5 years, more than any other volcano except Vesuvius.

Modern-day eruptions (1923–present day)

As "Europe's most active volcano", eruptions occur frequently (with as many as 16 eruptions taking place in 2001). However, several eruptions of note have occurred over the last century.

A major eruption took place in June 1923, lasting from 6 June until 29 June. A large lava flow from an eruption in 1928 led to the destruction of a population centre for the first time since the 1669 eruption. The eruption started high on Etna's northeast flank on 2 November. Then new eruptive fissures opened at decreasing elevations down the flank of the volcano. The third and most vigorous of these fissures opened late on 4 November at an unusually low elevation, approximately 1,200 m (3,937 ft) above sea-level, in a zone known as Ripe della Naca. The village of Mascali, lying down-slope of the Ripe della Naca, was almost completely destroyed in two days. Only a church and a few surrounding buildings survived in the north part of the village, called Sant'Antonino or "il quartiere". During the last days of the eruption, the flow interrupted the Messina-Catania railway line and destroyed the train station of Mascali. The event was used by Benito Mussolini's fascist regime for propaganda purposes, with the evacuation, aid, and rebuilding operations being presented as models of fascist planning. Mascali was rebuilt on a new site, and its church contains the Italian fascist symbol of the torch, placed above the statue of Jesus Christ.

Other major 20th-century eruptions occurred in 1949, 1971, 1979, 1981, 1983 and 1991–1993. In 1971, lava buried the Etna Observatory (built in the late 19th century), destroyed the first generation of the Etna cable-car, and seriously threatened several small villages on Etna's east flank. In March 1981, the town of Randazzo on the northwestern flank of Etna narrowly escaped destruction by unusually fast-moving lava flows. That eruption was remarkably similar to one in 1928 that destroyed Mascali. The 1991–1993 eruption saw the town of Zafferana threatened by a lava flow, but successful diversion efforts saved the town with the loss of only one building a few hundred metres from the town's margin. Initially, such efforts consisted of the construction of earth barriers built perpendicularly to the flow direction; it was hoped that the eruption would stop before the artificial basins created behind the barriers would be completely filled. Instead, the eruption continued, and lava surmounted the barriers, heading directly toward Zafferana. Engineers then decided to use explosives near the source of the lava flow, to disrupt a very efficient lava tube system through which the lava travelled for up to 7 km (4 mi) without losing significant heat or fluidity. The main explosion on 23 May 1992 destroyed the tube and forced the lava into a new artificial channel, far from Zafferana, and it would have taken months to re-establish a long lava tube. Shortly after the blasting, the rate of lava emission dropped, and during the remainder of the eruption (until 30 March 1993) the lava never advanced close to the town again.

Following six years (1995–2001) of unusually intense activity at the four summit craters of Etna, the volcano produced its first flank eruption since 1991–1993 in July–August 2001. This eruption, which involved activity from seven distinct eruptive fissures mostly on the south slope of the volcano, was well covered by the mass-media because it occurred at the height of the tourist season and numerous reporters and journalists were already in Italy to cover the G8 summit in Genoa. It also occurred close to one of the tourist areas on the volcano, and thus was easily accessible. Part of the "Etna Sud" tourist area, including the arrival station of the Etna cable car, were damaged by this eruption, which otherwise was a rather modest-sized event by Etna standards.

In 2002–2003, a much larger eruption threw up a huge column of ash that could easily be seen from space and fell as far away as Libya, 600 km (370 mi) south across the Mediterranean Sea. Seismic activity in this eruption caused the eastern flanks of the volcano to slip by up to two metres, and many houses on the flanks of the volcano experienced structural damage. The eruption also completely destroyed the tourist station Piano Provenzana, on the northeastern flank of the volcano, and part of the tourist station "Etna Sud" around the Rifugio Sapienza on the south flank. Footage from the eruptions was recorded by Lucasfilm and integrated into the landscape of the planet Mustafar in the 2005 film Star Wars: Episode III – Revenge of the Sith. The Rifugio Sapienza is near the site of a cable car station which had previously been destroyed in the 1983 eruption; it has now been rebuilt. Following a slow and non-destructive lava outflow on the upper southeastern flank between September 2004 and March 2005, intense eruptions occurred at the Southeast Crater in July–December 2006. These were followed by four episodes of lava fountaining, again at the Southeast Crater, on 29 March, 11 April, 29 April and 7 May 2007. Ash emissions and Strombolian explosions started from a vent on the eastern side of the Southeast Crater in mid-August 2007.

On 4 September 2007, a major episode of lava fountaining occurred from the new vent on the east side of the Southeast Crater, also producing a plume of ash and scoriae which fell over the east flank of the volcano. A lava flow travelled about 4.5 km (2.8 mi) into the uninhabited Valle del Bove. This eruption was visible far into the plains of Sicily, ending the following morning between the hours of 5 to 7 a.m. local time. Catania-Fontanarossa Airport shut down operations during the night for safety precautions.

An eruption on the morning of 13 May 2008, immediately to the east of Etna's summit craters was accompanied by a swarm of more than 200 earthquakes and significant ground deformation in the summit area. The eruption continued at a slowly diminishing rate for 417 days, until 6 July 2009, making this the longest flank eruption of Etna since the 1991–1993 eruption that lasted 473 days. Previous eruptions, in 2001, 2002–2003, and 2004–2005 had lasted 3 weeks, 3 months, and 6 months, respectively. Lava flows advanced 6.5 km during the first few days of this eruption but thereafter stagnated at many minor distances from the vents; during the last months of the eruption lava rarely advanced more than 1 km downslope.

Through January 2011 to February 2012, the summit craters of Etna were the site of intense activity. Frequent eruptions and ash columns forced the authorities to shut down the Catania airport on several occasions. The July 2011 episode also endangered the Sapienza Refuge, the main tourist hub on the volcano, but the lava flow was successfully diverted. In 2014, a flank eruption started involving lava flows and strombolian eruptions. This was the first flank eruption since 2008–09.

On 3 December 2015, an eruption occurred which climaxed between 03:20 and 04:10 local time. The Voragine crater exhibited a lava fountain which reached 1 km (3,300 ft) in height, with an ash plume which reached 3 km (9,800 ft) in height. The activity continued on the following days, with an ash plume that reached 7 km (23,000 ft) in height that forced Catania airport to shut down for a few hours. Volcanic gas emissions from this volcano are measured by a multi-component gas analyzer system, which detects pre-eruptive degassing of rising magmas, improving prediction of volcanic activity.

An eruption on 16 March 2017 injured 10 people, including a BBC News television crew, after magma exploded upon contact with snow.

An eruption on 24 December 2018, following a dyke intrusion at shallow depth, spewed ash into the air, forcing the closure of airspace around Mount Etna. Two days later, a magnitude 4.9 earthquake shook the town of Fleri and surrounding towns and hamlets in the Province of Catania, damaging buildings and injuring four people.

Beginning in February 2021, Mount Etna began a series of explosive eruptions, which have had an impact on nearby villages and cities, with volcanic ash and rock falling as far away as Catania. As of 12 March 2021, the volcano has erupted 11 times in three weeks. The eruptions have consistently sent ash clouds over 10 km (33,000 ft) into the air, closing Sicilian airports. There have been no reports of injuries.

In February 2022 there were two eruptions. On 11 February 2022, at 6 pm, there were lava fountains from the Southeast Crater which became a single Strombolian eruption by 7 pm. Between 10 and 11 pm it had reached a height of almost 1,000 m and lava bombs were thrown at a considerable distance. Ash was blown west by the wind and then turned southeast. There was large lava flow in the western flank. On 19 February at 10.15 am there was an explosive eruption, again from the Southeast Crater, high lava fountains and lava flows, the longest of which went down the north-eastern flank towards the Bove Valley.

On 29 May 2022 a sudden collapse of the Southeast Crater created a fracture on its northern flank at an elevation of circa 2,800 m (9,186 ft). A small lava flow emerged and headed in the direction of the Leone Valley, just above the much larger Bove Valley. It continued for three days and was accompanied by small and sporadic eruptions from two of the many vents at the top of this crater.

Etna erupted once again on 4 July 2024 causing the Catania Airport to close due to volcanic ash in the air. The airport reopened the next day.

On August 14, 2024, Mt. Etna erupted violently sending an ash cloud 9.5km into the atmosphere. Catania Airport was forced to close the following day.

Volcanic explosivity index of recent eruptions

The Global Volcanism Program has assigned a Volcanic Explosivity Index (VEI) to all of Mount Etna's eruptions since January 1955:

Vortex rings

In the 1970s Etna erupted vortex rings, one of the first recorded events of this type, which are extremely rare. This happened again in 2000. Video footage of 8 June 2000 event was captured. Another event occurred on 11 April 2013. Other similar events occurred during the summer of 2023 (see photo) and 2024.

Geopolitical boundaries

The borders of ten municipalities (Adrano, Biancavilla, Belpasso, Bronte (from two sides), Castiglione di Sicilia, Maletto, Nicolosi, Randazzo, Sant'Alfio, Zafferana Etnea) meet on the summit of Mount Etna, making this a multipoint of elevenfold complexity.

Facilities

Etna is one of Sicily's main tourist attractions, with thousands of visitors every year. The most common route is through the road leading to Sapienza Refuge ski area, lying at the south of the crater at elevation of 1,910 m. From the Refuge, a cableway runs uphill to an elevation of 2,500 m, from where the crater area at 2,920 m is accessible.

Ferrovia Circumetnea – Round-Etna railway – is a narrow-gauge railway constructed between 1889 and 1895. It runs around the volcano in a 110-km long semi-circle starting in Catania and ending in Riposto 28 km north of Catania.

There are two ski resorts on Etna: one at the Sapienza Refuge, with a chairlift and three ski lifts, and a smaller one on the north, at Piano Provenzana near Linguaglossa, with three lifts and a chairlift.

Sapienza Refuge was the finish of Stage 9 of the 2011 Giro d'Italia and Stage 4 of the 2017 Giro.

See also

• Genista aetnensis, the Mount Etna broom
• List of Italian regions by highest point
• List of volcanoes in Italy
• Mount Vesuvius
• Sacred mountains
• Volcanic Seven Summits

Notes

1. ^ "Il cratere Voragine dell'Etna cresce, bordo supera 3.400 metri - Notizie - Ansa.it". Agenzia ANSA (in Italian). 18 September 2024. Retrieved 19 September 2024.
2. ^ The elevation varies with volcanic activity. The volcano last erupted 21 May 2023. It is frequently given as 3,350 m (10,990 ft), but many sources that support this concede that this is approximate. The coordinates given, which are consistent with SRTM data, are from a 2005 GPS survey. The elevation data are based on a LIDAR (Light Detection and Ranging) survey carried out in June 2007, see Neri, M.; et al. (2008), "The changing face of Mount Etna's summit area documented with Lidar technology", Geophysical Research Letters, 35 (9): L09305, Bibcode:2008GeoRL..35.9305N, doi:10.1029/2008GL033740
3. Pezzella, Francesca. "L'Etna si supera. Nuovo record di altezza a 3357 metri". www.ingv.it (in Italian). Archived from the original on 10 August 2021. Retrieved 10 August 2021.
4. "Mount Etna erupts dramatically, sending ash 4.5 kilometers high".
5. Suda, alphaiota, 375
6. "Etna & Aeolian Islands 2012 – Cambridge Volcanology". www.volcano.group.cam.ac.uk. October 2012.
7. Laura Geggel (16 August 2021). "Mount Etna is 100 feet taller than it was 6 months ago". Space.com.
8. "Italy volcanoes and Volcanics". USGS. Archived from the original on 1 July 2011.
9. Aelian, Hist. An. xi. 3, referenced under Aetnaeus in William Smith's Dictionary of Greek and Roman Biography and Mythology
10. Thomaidis, Konstantinos; Troll, Valentin R.; Deegan, Frances M.; Freda, Carmela; Corsaro, Rosa A.; Behncke, Boris; Rafailidis, Savvas (2021). "A message from the 'underground forge of the gods': history and current eruptions at Mt Etna". Geology Today. 37 (4): 141–149. Bibcode:2021GeolT..37..141T. doi:10.1111/gto.12362. ISSN 1365-2451. S2CID 238802288.
11. "Decade Volcanoes". United States Geological Survey.
12. Mount Etna Becomes a World Heritage Site, Italy Magazine, 4 May 2013
13. According to Adrian Room's book Place-names of the World. Room dismisses the hypothesis that 'Etna' has a Greek derivation. "Volcano – Podictionary Word of the Day". Blog.oup.com. 29 April 2010. Retrieved 2 June 2011.
14. "Woodhouse's English-Greek Dictionary Page Image". Artflx.uchicago.edu. Archived from the original on 24 August 2014. Retrieved 2 June 2011.
15. Chevedden, Paul E. (2010), "A Crusade from the First: The Norman Conquest of Islamic Sicily, 1060–1091", Al-Masaq: Islam and the Medieval Mediterranean, 22 (2): 191, doi:10.1080/09503110.2010.488891, S2CID 162316105
16. "mongibèllo". Vocabolario Treccani (in Italian). Istituto dell'Enciclopedia Italiana. Retrieved 22 April 2024.
17. Bruce, Christopher W. (1999). The Arthurian Name Dictionary. Taylor & Francis. ISBN 0-8153-2865-6.
18. Loomis, Roger Sherman Wales and the Arthurian Legend, pub. University of Wales Press, Cardiff 1956 and reprinted by Folcroft Press 1973, Chapter 5 King Arthur and the Antipodes, pp. 70–71.
19. Loomis, Roger Sherman, Arthurian Tradition And Chrétien de Troyes pub. Columbia University Press, New York 1948, pp. 66 & 306.
20. Arthurian Literature in the Middle Ages: A Collaborative History ed. Roger Sherman Loomis, pub. Oxford University Press 1959, special edition for Sandpiper Books Ltd. 2001, ISBN 0 19 811588 1
21. Martin-Schutz, Alicia. "Mt. Etna".
22. It has been suggested that this was the reason why the settlement of Atlit Yam (Israel), now below sea level, was suddenly abandoned around that time. See Pareschi, M. T.; Boschi, E. & Favalli, M. (2007), "Holocene tsunamis from Mount Etna and the fate of Israeli Neolithic communities", Geophysical Research Letters, 34 (16): L16317, Bibcode:2007GeoRL..3416317P, doi:10.1029/2007GL030717, S2CID 129407252. This claim has been contested, however, as "there is no evidence of tsunami deposits, nor of sudden and catastrophic changes such as damaged structures, whole animal carcases or evidence of traumatic injury, such as might be expected to result from a tsunami event" (Galili E., Rosen B., Evron M.W., Hershkovitz I., Eshed V., Horwitz L.K. (2020) Israel: Submerged Prehistoric Sites and Settlements on the Mediterranean Coastline—the Current State of the Art. In: Bailey G., Galanidou N., Peeters H., Jöns H., Mennenga M. (eds) The Archaeology of Europe’s Drowned Landscapes. Coastal Research Library, vol 35. Springer, Cham). See also, Galili, E., Horwitz, L. K., Hershkovitz, I., Eshed, V., Salamon, A., Zviely, D., Weinstein‐Evron, M., and Greenfield, H. (2008), Comment on "Holocene tsunamis from Mount Etna and the fate of Israeli Neolithic communities" by Maria Teresa Pareschi, Enzo Boschi, and Massimiliano Favalli, Geophysical Research Letters, 35, L08311.
23. Murray, J.B.; van Wyk de Vries, B.; Pitty, A. (April 2018). "Gravitational sliding of the Mt. Etna massif along a sloping basement" (PDF). Bulletin of Volcanology. 80 (4): 40. Bibcode:2018BVol...80...40M. doi:10.1007/s00445-018-1209-1. PMC 6560784. PMID 31258237.
24. Gravitational collapse of Mount Etna’s southeastern flank
25. Tanguy, J. C.; Condomines, M.; Goff, M.; Chillemi, V.; Delfa, S.; Patanè, G. (2007). "Mount Etna eruptions of the last 2,750 years: Revised chronology and location through archeomagnetic and 226Ra-230Th dating" (PDF). Bulletin of Volcanology. 70 (1): 55. Bibcode:2007BVol...70...55T. doi:10.1007/s00445-007-0121-x. S2CID 44241302.
26. Smith, William (1854). A Dictionary of Greek and Roman Geography. London: Walton and Maberly. p. 213.
27. Coltelli, M.; Del Carlo, P. & Vezzoli, L. (1998), "Discovery of a Plinian basaltic eruption of Roman age at Etna Volcano, Italy", Geology, 26 (12): 1095–1098, Bibcode:1998Geo....26.1095C, doi:10.1130/0091-7613(1998)026<1095:DOAPBE>2.3.CO;2
28. Chester, David K. (2001). "The 122 BCE Eruption of Mount Etna: Causes, Impacts, and Aftermath". Journal of Volcanology and Geothermal Research. 104 (1–4): 91–99.
29. Aeneid, edition of Theodore C. Williams, ca. 1908
30. Chester, David K. (2003). "Eruptions of Mount Etna from 1030 to 1224: Historical Records and Volcanological Implications". Journal of Volcanology and Geothermal Research. 125: 197–211.
31. Chester, David K. (2006). "Historical Eruptions of Mount Etna: 1160 to 1224". Journal of Volcanology and Geothermal Research. 150: 123–134.
32. The history of the life and travels of Rabban Sawma
33. "Mount Etna (volcano, Italy)". (the Encyclopædia Britannica has been wrongly cited as one source of this false information).
34. The Encyclopaedia Britannica 5th edition (1817) quotes from the eyewitness report of Lord Winchelsea, Ambassador to Constantinople, to the Court of England. It happens not to mention casualties. Encyclopaedia Britannica: Or, A Dictionary of Arts, Sciences, and Miscellaneous Literature, Enlarged and Improved. Vol. 1 (5th ed.). Edinburgh: A. Constable. 1823. pp. 248–249. See also: Charles Hutton; Georges Shaw; Richard Pearson (1809). The Philosophical Transactions of the Royal Society of London, from Their Commencement, in 1665, to the Year 1800; Abridged...: From 1665 to 1672. 1. London. pp. 357–358, 383–387, 637–638.
35. "Eruption of Snow-Covered Mt. Etna Kills 2 Tourists and Injures 7 Others". LA Times. Retrieved 2 June 2019.
36. "Etna and Man". Boris.vulcanoetna.it. Archived from the original on 22 July 2011. Retrieved 2 June 2011.
37. Venzke, E., ed. (10 December 2020). "What volcanoes have had the longest eruptions?". Global Volcanism Program — Volcanoes of the World (Version 4.9.2). Smithsonian Institution. doi:10.5479/si.GVP.VOTW4-2013. Retrieved 15 December 2020.
38. ^ "The Continuing Eruption of Mt. Etna". Earthobservatory.nasa.gov. 23 July 2001. Retrieved 15 February 2022.
39. Ponte, Gaetano (1923). "The Recent Eruption of Etna" (PDF). Nature. 112 (2815): 546–548. Bibcode:1923Natur.112..546P. doi:10.1038/112546a0. S2CID 6883748.
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References

• "Etna". Global Volcanism Program. Smithsonian Institution. Retrieved 25 December 2008.
• Chester, D. K.; Duncan, A. M.; Guest, J. E.; Kilburn, C. R. J. (1985). Mount Etna: The Anatomy of a Volcano. Chapman and Hall. pp. 412 pp. ISBN 978-0-8047-1308-5.

External links

• Mount Etna Nord Live Webcams by Linguaglossa H24
• "VONA bulletin".
• Mount Etna Regional Park
• Youtube video: eruption phases of Etna in 2018 (in Italian)
• Smithsonian Institution: Global Volcanism Program: Etna
• Footage of the 1971 eruption is featured in the 1979 film Days of Fury, hosted by Vincent Price

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