Mount Vesuvius: Difference between revisions

From Citizendium
Jump to navigation Jump to search
imported>Richard Nevell
(Mention the AD79 eruption)
imported>Richard Nevell
(Add image)
Line 1: Line 1:
{{subpages}}
{{subpages}}
{{Image|Vesuvius, 2009.jpg|right|350px|Vesuvius as seen from the Bay of Naples}}
{{Image|Vesuvius and environs.jpg|right|350px|Aerial photograph showing the location of Mount Vesuvius}}
{{Image|Vesuvius and environs.jpg|right|350px|Aerial photograph showing the location of Mount Vesuvius}}
'''Mount Vesuvius''' (Italian: Monte Vesuvio, Latin: Mons Vesuvius) is an active volcano on the Bay of Naples, southern [[Italy]].  Its last eruption was in 1944, the most recent of any volcano on mainland Europe.
'''Mount Vesuvius''' (Italian: Monte Vesuvio, Latin: Mons Vesuvius) is an active volcano on the Bay of Naples, southern [[Italy]].  Its last eruption was in 1944, the most recent of any volcano on mainland Europe.


Mount Vesuvius is believed to be one of the remnants of a supervolcano which formed the Bay of Naples, Vesuvius and other volcanic areas nearby, such as Solfatara.  The original volcano was formed by a [[subduction zone]].  This was when the African plate was subducted underneath the larger Eurasian plate, causing it to melt into magma.  This magma was pushed upwards because it had a lower density than the rock above it, and reached the surface in the form of a volcano. The eruption of A.D. 79 buried the Roman towns of [[Pompeii]] and [[Herculaneum]] and their inhabitants. The settlements were preserved by the eruption are today are important [[archaeology|archaeological]] sites.
Mount Vesuvius is believed to be one of the remnants of a supervolcano which formed the [[Bay of Naples]], Vesuvius and other volcanic areas nearby, such as Solfatara.  The original volcano was formed by a [[subduction zone]].  This was when the African plate was subducted underneath the larger Eurasian plate, causing it to melt into magma.  This magma was pushed upwards because it had a lower density than the rock above it, and reached the surface in the form of a volcano. The eruption of A.D. 79 buried the Roman towns of [[Pompeii]] and [[Herculaneum]] and their inhabitants. The settlements were preserved by the eruption are today are important [[archaeology|archaeological]] sites.

Revision as of 13:44, 30 April 2013

This article is a stub and thus not approved.
Main Article
Discussion
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and subject to a disclaimer.
(CC [1]) Photo: J E Theriot
Vesuvius as seen from the Bay of Naples
(PD) Photo: Central Intelligence Agency
Aerial photograph showing the location of Mount Vesuvius

Mount Vesuvius (Italian: Monte Vesuvio, Latin: Mons Vesuvius) is an active volcano on the Bay of Naples, southern Italy. Its last eruption was in 1944, the most recent of any volcano on mainland Europe.

Mount Vesuvius is believed to be one of the remnants of a supervolcano which formed the Bay of Naples, Vesuvius and other volcanic areas nearby, such as Solfatara. The original volcano was formed by a subduction zone. This was when the African plate was subducted underneath the larger Eurasian plate, causing it to melt into magma. This magma was pushed upwards because it had a lower density than the rock above it, and reached the surface in the form of a volcano. The eruption of A.D. 79 buried the Roman towns of Pompeii and Herculaneum and their inhabitants. The settlements were preserved by the eruption are today are important archaeological sites.