Mount Vesuvius

During the eruption of Mount Vesuvius in 79 AD, people tried to flee the area to escape the volcanic ash and debris. Some sought refuge in buildings or tried to shelter indoors. Many were ultimately overwhelmed by the pyroclastic flow and buried under the volcanic material.

well what would happen if it was a major eruption and if it was even bigger like then one back in 79 AD then a lot more destruction would happen towns would be whipped out, people would probably die (if they didn't have warning or did not evacuate in time) and it would just be chaos for them.

basically it is that they need to get the prediction very good and early because it will take a very long time to evacuate all of Naples.

if you have any probs email me at: billybob@hotmail.co.uk ! :)

Naples.

There were no recorded deaths from a Mount Vesuvius eruption in 1944. The last major eruption of Mount Vesuvius occurred in 1944 but casualties were minimal due to successful evacuations.

Mount Vesuvius is near the city of "Naples" in italy.

Pompeii and Herculaneum were completely buried in ash and pumice by the eruption of Mount Vesuvius in 79 AD, while Stabiae was also heavily damaged. The city of Naples, although affected by ashfall, did not suffer as much damage compared to the neighboring cities.

Stratovolcano (a composite volcano)

Today, Mount Vesuvius is a dormant volcano located near Naples, Italy. It is a popular tourist destination known for its scenic hiking trails and panoramic views of the Bay of Naples. The area is closely monitored for any signs of volcanic activity to ensure the safety of nearby residents and visitors.

Some people were able to escape the eruption of Mount Vesuvius in 79 AD by fleeing the area as soon as the volcano showed signs of activity. Others sought refuge indoors or in underground areas. Those who did not evacuate in time were unfortunately overwhelmed by the volcanic ash and pyroclastic flows.

Mount Vesuvius exists because of the African plate sliding under the Eurasian plate therefore the magma is then being disturbed and heating up so it is then starting a convection current and the magma is then breaking the weaker rock to reach the surface and Vesuvius is born.

They are sure trying since if it erupts 3 million people will be in the way. I just saw a Discovery program on it and they think they can map earthquakes to eruptions. By graphing the history of earthquakes in the area and when an eruption happened they were able to show a correlation. How strong it is is still the question. The volcano is one of the best watched in the world, but they still don't have all her secrets.

Mount Vesuvius is located on a continental plate, specifically the Eurasian Plate. It is within the boundaries of the subduction zone where the African Plate is being subducted beneath the Eurasian Plate, leading to volcanic activity in the region.

Some people may believe that Pompeii was overtaken by flowing lava, like the lava you see in the currently active Hawaiian volcanos. That did not happen. Pompeii was buried in a heavy rain of volcanic ash, and the people who died there were overcome in moments by an extremely hot pyroclastic flow, not by lava per se.

Here are some more myths:

One of the myths is that were disproved over time was that a completely intact city was rediscovered, which was wrong because the Pompeians, who had escaped, returned to their city when the ashes had cooled and removed some of the most precious treasures from the resort, but they left plenty behind to be uncovered at a later date and carted off to museums throughout Europe and America.

Another myth is that was disproved over time was that no body from Pompeii escaped, that everyone was either buried or they died when Mount Vesuvius erupted. The truth is that there were over 12,000 people and most Pompeians were able to escape before the final devastating eruption. There were only 1,100 bodies that had been uncovered which indicates that a portion of the residents were too slow or were unwilling to abandon the town during the first phase of the eruption.

Last two were from

:D GeniusGirlLives :D

they where slowly killed by raining rocks from the volcano, that soon weighed down roofs until they crushed people, and ash clouds. But they where soon finished off by a second pyroclastic shock. people died almost instantly

The eruption of Mount Vesuvius in 79 AD was extremely deadly, resulting in the destruction of Pompeii and Herculaneum, and causing the deaths of thousands of people. The event buried these cities under layers of ash and pumice, preserving them for centuries.

The boot-shaped country in the Mediterranean Sea where Mount Vesuvius and Mount Etna are found is Italy. Italy is known for its volcanic activity, with Mount Vesuvius near Naples and Mount Etna in Sicily being two of its most famous volcanoes.

The eruption of Mount Vesuvius in 79 AD lasted for about 18 hours, with the most violent phase occurring during the first 12 hours.

For the ad 79 eruption... people cant say exactly but the best estimate is 25,000 deaths for the ad 79 eruption. Hope I could help ;)

At Mount Vesuvius, you can hike to the crater rim where you can see stunning views of the Bay of Naples and the surrounding area. You can also learn about the history of the volcano and the destruction it caused to Pompeii and Herculaneum in 79 AD.

The eruption of Mount Vesuvius in 79 AD is estimated to have been around a magnitude 5 or 6 on the Richter scale. However, since the Richter scale was developed centuries later, modern seismologists use other methods to estimate the magnitude of historical earthquakes and volcanic eruptions.

Mount Vesuvius is located at a convergent boundary where the African plate is subducting beneath the Eurasian plate. This subduction process causes magma to rise from the Earth's mantle, leading to the formation of the volcano. The pressure and heat from the subduction zone contribute to the volcanic activity in the region, resulting in the formation and eruption of Mount Vesuvius.

Mount Vesuvius is located at a convergent plate boundary where the African Plate is subducting beneath the Eurasian Plate. This subduction leads to the build-up of pressure and the formation of magma that eventually erupts to create the volcano.

After the eruption of Mount Vesuvius in 79 AD, the cities of Pompeii and Herculaneum were buried under ash and pumice, preserving them for centuries. The area was abandoned and largely forgotten until their rediscovery in the 18th century, leading to significant archaeological excavations that have provided valuable insights into Roman daily life. Today, the ruins of Pompeii and Herculaneum are popular tourist destinations and UNESCO World Heritage sites.

Principal eruptions list
79 explosive Ash-fall, pomices and lahars

472 effusive-explosive Lava flow and lahars to north-western flank

512

26 February 685 effusive Imposing lava flow

787 effusive-explosive Lahars and imposing lava flow

968 Lava flow to sea

27 January 1037 Lava flow to sea

29 May 1139 explosive Ash-fall

1500 explosive Ash-fall

16 December 1631 effusive-explosive Cone collapse; lava flow to sea

3 July 1660 explosive Ash-fall to north-east flank

13 April 1694 effusive Lava toward Torre del Greco

25 May 1698 effusive-explosive Damage by ash-fall to south-east flank

28 July 1707 effusive-explosive

20 May 1737 effusive-explosive A lava flow invades T. del Greco; ash-fall and lahars

23 December 1760 effusive-explosive Opening of lateral vents on southern flank (150 m asl)

19 October 1767 effusive-explosive Two lava flows toward T.Annunziata. and S. Giorgio a Cremano

8 August 1779 explosive Ash and bombs over Ottaviano

15 June 1794 effusive-explosive Opening of lateral vents on south-western flank (470 m asl)
22 October 1822 effusive-explosive Two lava flows toward T. del Greco and Boscotrecase

23 August 1834 effusive-explosive A lava flow toward Poggiomarino

6 February 1850 effusive-explosive

1 May 1855 effusive A lava flow invades Massa and S.Sebastiano

8 December 1861 effusive-explosive Opening of lateral vents on south-western flank (290 m asl)

15 November 1868 effusive

24 April 1872 effusive-explosive A lava flow invades Massa and S.Sebastiano

4 April 1906 effusive-explosive A lava flow toward T.Annunziata, strong explosive activity

3 June 1929 effusive-explosive A lava flow toward Terzigno

18 March 1944 effusive-explosive A lava flow invades Massa and S.Sebastiano

source:http://www.vesuvioinrete.it/e_storia.htm