Mount Etna

About

Mount Etna, or simply Etna, 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 (11,014 ft), but was then surpassed by the Voragine crater after the summer 2024 eruptions. Etna covers an area of 1,190 km2 (459 sq mi) with a basal circumference of 140 km (87 miles). This makes it by far the largest of the four 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. 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...

See also: Aetna (nymph) and King asleep in mountain One view is that the word Etna is from the Greek αἴθω ( aíthō ), meaning "to burn", through monophthongization of the Ancient Greek pronunciation as seen in Koine Greek phonology, or possibly from a Siculian (or Sicanian ?) dialect word ( *aith-na, "the fiery one"?) of the same Indo-European origin, namely the root *h₂eydʰ- "to burn; fire".

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.

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.

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. [ citation needed ] 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 c. 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.

See also: List of Mount Etna 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.

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.

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.

An eruption of Etna in 44 BCE was followed by famine in China (43 BCE) the Roman Republic and Egypt, with Plutarch (among others) suggesting a causal link ; however, an eruption of Mount Okmok early the following year is a more likely cause.

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.