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Monte Nuovo ("New Mountain") 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, during the most recent part of the Holocene, 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] The eruptive vent formed next to the medieval village of Tripergole on the shores of the then-much larger Lake Lucrino. The thermal bath village, which had been inhabited since ancient Roman times and was home to notable Roman-era buildings including Cicero's villa, was completely buried by ejecta from the new cinder cone. Tripergole's ruins and its important thermal springs completely disappeared under Monte Nuovo such that the exact location of the village can no longer be identified.[4]
| Monte Nuovo | |
|---|---|
 Monte Nuovo. View from Lucrine Lake. | |
| Highest point | |
| Elevation | 132 m (433 ft)[1] |
| Coordinates | 40°50′7″N 14°5′17″E |
| Geography | |
  Monte Nuovo Italy | |
| Location | Campania, Italy |
| Geology | |
| Mountain type | Cinder cone |
| Volcanic arc/belt | Campanian volcanic arc |
| Last eruption | 1538 |
Volcanologists feared another eruption[5] between 1969 and 1984, when there were again earthquakes and changes in land elevations in the area.[6][7]
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. S2CID 128745563.
- Scarth, pp. 43-56
- Il Villaggio di Tripergole - archeoFlegrei (in Italian)
- 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. S2CID 129177542.
- 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. S2CID 129810798.
- 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. S2CID 140656491.
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: Monte Nuovo, 1538". Vulcan's Fury: Man Against the Volcano. New Haven, Connecticut: Yale University Press. ISBN 0-300-07541-3.
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На других языках
[de] Monte Nuovo
Der Monte Nuovo (italienisch: „Neuer Berg“) ist ein westlich von Neapel auf dem Gemeindegebiet von Pozzuoli gelegener Vulkankegel.- [en] Monte Nuovo
[es] Monte Nuovo
El Monte Nuovo es un volcán que se encuentra en la zona de los Campos Flégreos cerca de Nápoles.[fr] Monte Nuovo
Le monte Nuovo est un volcan italien apparu en 1538 dans les champs Phlégréens au cours de son unique éruption, faisant de lui un volcan monogénique.[it] Monte Nuovo
Il monte Nuovo è un vulcano che fa parte dei Campi Flegrei. Si trova nel comune di Pozzuoli presso il Lago Lucrino. Si formò tra il 29 settembre e il 6 ottobre 1538 a seguito di un'eruzione che distrusse il villaggio medievale di Tripergole e mise in fuga la popolazione locale. La formazione del Monte Nuovo rappresenta una delle due eruzioni vulcaniche nei Campi Flegrei avvenute in epoca storica, insieme all'eruzione del 1158 alla solfatara (VEI 1)[1].Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.
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