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Pompeii (/ p ɒ m ˈ p eɪ (i)/ ⓘ pom-PAY(-ee), Latin: [pɔmˈpei̯.iː]) was a city in what is now the municipality of Pompei, near Naples, in the Campania region of Italy.Along with Herculaneum, Stabiae, and many surrounding villas, the city was buried under 4 to 6 m (13 to 20 ft) of volcanic ash and pumice in the eruption of Mount Vesuvius in 79 AD.
Like the nearby city of Pompeii, Herculaneum is famous as one of the few ancient cities to be preserved nearly intact, as the solidified material from the volcano that blanketed the town protected it against looting and the elements. Although less known than Pompeii today, it was the first and, for a long time, the only discovered Vesuvian city ...
Considering the data for all the surge deposits arrived at a surge deposit estimate. The authors discovered that the city of Pompeii was a relatively cool spot within a much hotter field, which they attributed to the interaction of the surge with the "fabric" of the city. [27] The investigators reconstruct the sequence of volcanic events as ...
As ash and lava spewed out of Mount Vesuvius in 79 A.D., everything stopped for people in the ancient Roman city of Pompeii. The devastating volcanic eruption was visible to the occupants of ...
But in 79 A.D., in the Roman city of Pompeii at the foot of Mount Vesuvius, the guy holding the “THE END IS NEAR!” sign was right. When the volcano blew, the town was covered by boiling hot ...
An ancient beach that was destroyed by the eruption of Mount Vesuvius nearly 2,000 years ago has reopened to the public after restoration works.
Pompei (Italian:; Neapolitan: Pumpeje [pumˈbɛːjə]), in English also Pompeii (/ p ɒ m ˈ p eɪ (i)/ pom-PAY(-ee), as in the name of the ancient city) is a city and commune in the Metropolitan City of Naples, Italy, home of the ancient Roman ruins of Pompeii that are part of the UNESCO World Heritage Sites.
The volcano then entered a stage of more frequent, but less violent eruptions, until the most recent Plinian eruption, which destroyed Pompeii and Herculaneum. Evidence of these eruptions comes from badly preserved ashfall deposits that have been dubitatively assigned to either the Somma-Vesuvius complex, or the Phlegrean fields .