Mount Vesuvius, Campania, Italy

Mount Vesuvius, Campania, Italy

Mount Vesuvius is a somma–stratovolcano located on the Gulf of Naples in Campania, Italy, about 9 km east of Naples and a short distance from the shore. It is one of several volcanoes forming the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera, resulting from the collapse of an earlier, much higher structure.

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The eruption of Mount Vesuvius in 79 AD destroyed the Roman cities of Pompeii, Herculaneum, Oplontis, Stabiae and other settlements. The eruption ejected a cloud of stones, ash and volcanic gases to a height of 33 km, erupting molten rock and pulverized pumice at the rate of 6×105 cubic metres per second. More than 1,000 people are thought to have died in the eruption, though the exact toll is unknown. The only surviving witness account consists of two letters by Pliny the Younger to the historian Tacitus.
Vesuvius has erupted many times since. It is the only volcano on Europe’s mainland to have erupted in the last hundred years. It is regarded as one of the most dangerous volcanoes in the world, marked as one of the Decade Volcanoes, because 3,000,000 people live near enough to be affected by an eruption, with at least 600,000 in the danger zone. Eruptions tend to be violent and explosive; these are known as Plinian eruptions.

Vesuvius is a “humpbacked” peak, consisting of a large cone (Gran Cono) partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier (and originally much higher) structure called Mount Somma. The Gran Cono was produced during the A.D. 79 eruption. For this reason, the volcano is also called Somma-Vesuvius or Somma-Vesuvio.
The caldera started forming during an eruption around 17,000–18,000 years ago and was enlarged by later paroxysmal eruptions, ending in the one of AD 79. This structure has given its name to the term “somma volcano”, which describes any volcano with a summit caldera surrounding a newer cone.
The cliffs forming the northern ridge of Monte Somma’s caldera rim reach a maximum height of 1,132 m at Punta Nasone. The summit of the main cone of Vesuvius is 1,281 m above sea level and more than 400m above the 5 km long valley of Atrio di Cavallo (the northern floor of Monte Somma’s caldera).
The volcano’s slopes are scarred by lava flows, while the rest are heavily vegetated, with scrub and forests at higher altitudes and vineyards lower down.