Monte Nuovo: Difference between revisions
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The event is important in the [[history of science]] because it was the first eruption in modern times to be described by a large number of witnesses.<ref name=Scarth1>Scarth, pp. 43-56</ref> |
The event is important in the [[history of science]] because it was the first eruption in modern times to be described by a large number of witnesses.<ref name=Scarth1>Scarth, pp. 43-56</ref> |
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Volcanologists feared another eruption<ref>{{cite journal | last1 = Barberi | first1 = F. | last2 = Corrado | first2 = G. | last3 = Innocenti | first3 = F. | last4 = Luongo | first4 = G. | year = 1984 | title = Phlegraean Fields 1982–1984: Brief chronicle of a volcano emergency in a densely populated area | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 175–185 }}</ref> between 1969 and 1984, |
Volcanologists feared another eruption<ref>{{cite journal | last1 = Barberi | first1 = F. | last2 = Corrado | first2 = G. | last3 = Innocenti | first3 = F. | last4 = Luongo | first4 = G. | year = 1984 | title = Phlegraean Fields 1982–1984: Brief chronicle of a volcano emergency in a densely populated area | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 175–185 | doi=10.1007/bf01961547}}</ref> between 1969 and 1984, |
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when there were again earthquakes and changes in land elevations in the area.<ref>{{cite journal | last1 = Del Pezzo | first1 = E. | last2 = De Natale | first2 = G. | last3 = Zoloo | first3 = A. | year = 1984 | title = Space-time distribution of small earthquakes at Phlegraean Fields, south-central Italy | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 201–207 }}</ref><ref>{{cite journal | last1 = Bianchi | first1 = R. | last2 = Coradini | first2 = A. | last3 = Federico | first3 = C. | last4 = Giberti | first4 = G. | last5 = Sartoris | first5 = G. | last6 = Scandone | first6 = R. | year = 1984 | title = Modelling of surface ground deformations in the Phlegraean Fields volcanic area, Italy | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 321–330 }}</ref> |
when there were again earthquakes and changes in land elevations in the area.<ref>{{cite journal | last1 = Del Pezzo | first1 = E. | last2 = De Natale | first2 = G. | last3 = Zoloo | first3 = A. | year = 1984 | title = Space-time distribution of small earthquakes at Phlegraean Fields, south-central Italy | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 201–207 | doi=10.1007/bf01961549}}</ref><ref>{{cite journal | last1 = Bianchi | first1 = R. | last2 = Coradini | first2 = A. | last3 = Federico | first3 = C. | last4 = Giberti | first4 = G. | last5 = Sartoris | first5 = G. | last6 = Scandone | first6 = R. | year = 1984 | title = Modelling of surface ground deformations in the Phlegraean Fields volcanic area, Italy | url = | journal = Bulletin of Volcanology | volume = 47 | issue = 2| pages = 321–330 | doi=10.1007/bf01961563}}</ref> |
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==Notes== |
==Notes== |
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Revision as of 11:27, 4 October 2014
| Monte Nuovo | |
|---|---|
 | |
| Highest point | |
| Elevation | 458 m (1,503 ft)[1] |
| Geography | |
  Monte Nuovo Italy | |
| Location | Campania, Italy |
| Region | IT |
| Geology | |
| Mountain type | Cinder cone |
| Volcanic arc/belt | Campanian volcanic arc |
| Last eruption | 1538 |
Monte Nuovo is a cinder cone volcano within the Campi Flegrei caldera, near Naples, southern Italy. A series of damaging earthquakes and changes in land elevation preceded its only eruption, which lasted from September 29 to October 6, 1538, when it was formed.[2] The event is important in the history of science because it was the first eruption in modern times to be described by a large number of witnesses.[3]
Volcanologists feared another eruption[4] between 1969 and 1984, when there were again earthquakes and changes in land elevations in the area.[5][6]
Notes
- ^ "Campi Flegrei". Global Volcanism Program. Smithsonian Institution. Retrieved 2014-01-01.
- ^ Di Vito, Mauro; et al. (1987). "The 1538 Monte Nuovo eruption (Campi Flegrei, Italy)". Bulletin of Volcanology. 49 (4): 608–15. doi:10.1007/bf01079966.
{{cite journal}}: Explicit use of et al. in:|author2=(help) - ^ Scarth, pp. 43-56
- ^ Barberi, F.; Corrado, G.; Innocenti, F.; Luongo, G. (1984). "Phlegraean Fields 1982–1984: Brief chronicle of a volcano emergency in a densely populated area". Bulletin of Volcanology. 47 (2): 175–185. doi:10.1007/bf01961547.
- ^ Del Pezzo, E.; De Natale, G.; Zoloo, A. (1984). "Space-time distribution of small earthquakes at Phlegraean Fields, south-central Italy". Bulletin of Volcanology. 47 (2): 201–207. doi:10.1007/bf01961549.
- ^ Bianchi, R.; Coradini, A.; Federico, C.; Giberti, G.; Sartoris, G.; Scandone, R. (1984). "Modelling of surface ground deformations in the Phlegraean Fields volcanic area, Italy". Bulletin of Volcanology. 47 (2): 321–330. doi:10.1007/bf01961563.
References
- Piero Giacomo da Toledo (1539) Ragionamento del terremoto, del Nvovo monte, del aprimento di terra in Pozvolo nel anno 1538; e dela significatione d'essi Napoli, Giouanni Sulztbah alemano
- Scarth, Alwyn (1999). "Chapter 4: Nonte Nuovo, 1538". Vulcan's Fury: Man Against the Volcano. New Haven, Connecticut: Yale University Press. ISBN 0-300-07541-3.
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