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Vesuvius has a long historic and literary tradition.It was considered a divinity of the Genius type at the time of the eruption of AD 79: it appears under the inscribed name Vesuvius as a serpent in the decorative frescos of many The historian Diodorus Siculus relates a tradition that Hercules, in the performance of his labors, passed through the country of nearby Cumae on his way to Sicily and found there a place called "the Phlegraean Plain" ( It was inhabited by bandits, "the sons of the Earth," who were giants.Layers of lava, ash, scoria and pumice make up the volcanic peak.Their mineralogy is variable, but generally silica-undersaturated and rich in potassium, with phonolite produced in the more explosive eruptions.Finding a weak spot at the Earth's surface, it broke through, thus forming the volcano.The volcano is one of several which form the Campanian volcanic arc.The Latins also competed for the occupation of Campania. Other peoples of unknown provenance are said to have been there at some time by various ancient authors. The caldera started forming during an eruption around 17,000 (or 18,300) years ago Monte Somma is 1,132 m (3,714 ft) high, separated from the main cone by the valley of Atrio di Cavallo, which is 5 km (3.1 mi) long.

Cores were dated by potassium–argon and argon–argon dating. Although the area has been subject to volcanic activity for at least 400,000 years, the lowest layer of eruption material from the Somma caldera lies on top of the 40,000 year‑old Campanian ignimbrite produced by the Campi Flegrei complex, and was the product of the Codola Plinian eruption 25,000 years ago.

Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.

Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman cities of Pompeii and Herculaneum, as well as several other settlements.

Others include Campi Flegrei, a large caldera a few kilometers to the north west, Mount Epomeo, 20 kilometres (12 mi) to the west on the island of Ischia, and several undersea volcanoes to the south.

The arc forms the southern end of a larger chain of volcanoes produced by the subduction process described above, which extends northwest along the length of Italy as far as Monte Amiata in Southern Tuscany.