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Mount Vesuvius (/ v ɪ ˈ s uː v i ə s / viss-OO-vee-əs) [a] is a somma–stratovolcano located on the Gulf of Naples in Campania, Italy, about 9 km (5.6 mi) east of Naples and a short distance from the shore. It is one of several volcanoes forming the Campanian volcanic arc.
The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. [2] The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the environment. When it condenses, it releases energy and warms the environment.
English: A map showing the cities and towns affected by the eruption of Mount Vesuvius in 79 AD. The general shape of the ash and cinder fall (see w:en:pyroclast) is shown by the dark area to the southeast of Mt Vesuvius. (P.S. It seems strange to show the modern day English names for the two bodies of water - I am open to suggestions).
Mount Vesuvius violently ejected a cloud of super-heated tephra and gases to a height of 33 km (21 mi), ejecting molten rock, pulverized pumice and hot ash at 1.5 million tons per second, ultimately releasing 100,000 times the thermal energy of the atomic bombings of Hiroshima and Nagasaki.
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A view of the ancient beach, with the skeletons of the fugitive victims of the eruption of Vesuvius in 79AD, open to the public for the first time.
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Image of Vesuvius Observatory and Mount Vesuvius(c. 19th Century) In 1841, around 200 years after the 1631 eruption, the Vesuvius Observatory was established. [ 11 ] This marked a huge milestone in the study of volcanology, as it was the first ever volcanological observatory.