Phlegraean Fields

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Phlegraean Fields
Pozzuoli NASA ISS004-E-5376 modified names.jpg
NASA Space Shuttle photo of Campi Flegrei, with main features labeled.
Elevation 458 m (1,503 ft)[1]
Location
Location Italy
Coordinates 40°49′37″N 14°08′20″E / 40.827°N 14.139°E / 40.827; 14.139Coordinates: 40°49′37″N 14°08′20″E / 40.827°N 14.139°E / 40.827; 14.139[1]
Geology
Type Caldera[1]
Age of rock 40,000 years
Volcanic arc/belt Campanian volcanic arc
Last eruption September to October 1538[1]
Sulfur at the Solfatara crater

The Phlegraean Fields (Italian: Campi Flegrei; from Greek φλέγω, "to burn")[citation needed] are a large volcanic area situated to the west of Naples, Italy. It was declared a regional park in 2003. Lying mostly underwater, the area of the caldera comprises 24 craters and volcanic edifices. Hydrothermal activity can be observed at Lucrino, Agnano and the town of Pozzuoli. There are also effusive gaseous manifestations in the Solfatara crater, which is known as the mythological home of the Roman god of fire, Vulcan. The area also features bradyseismic phenomena, which are most evident at the Macellum of Pozzuoli which in the 18th century was misidentified as a Temple of Serapis, as geologists puzzled over bands of boreholes (Gastrochaenolites) left by marine Lithophaga molluscs on three standing marble columns, showing that the level of the site in relation to sea level had varied. This area is monitored by the Vesuvius Observatory.[2]

Geological phases[edit]

Three geological phases or periods are recognised and distinguished.[3]

  • The First Phlegraean Period. It is thought that the eruption of the Archiflegreo volcano occurred about 39.28 ± 0.11 ka. The dating of the Campanian Ignimbrite (CI) eruption to ~37,000 calendar years B.P. draws attention to the coincidence of this volcanic catastrophe and the suite of coeval, Late Pleistocene biocultural changes that occurred within and outside the Mediterranean region. These included the Middle to Upper Paleolithic cultural transition and the replacement of Neanderthal populations by anatomically modern Homo sapiens, a subject of sustained debate. No less than 150 km3 of magma were extruded in the CI eruption, the signal of which can be detected in Greenland ice cores. As widespread discontinuities in archaeological sequences are observed at or following the CI event, a significant interference with ongoing human processes in Mediterranean Europe is hypothesized. Abstract [4] (older estimate ~37,000 years ago), erupting about 200 cubic kilometres (48 cu mi) of magma (500 cubic kilometres (120 cu mi) bulk volume)[5] to produce the Campanian Ignimbrite.[6] New research led by Liubov Vitalievna Golovanova and Vladimir Borisovich Doronichev of the ANO Laboratory of Prehistory in St. Petersburg, Russia, supports the hypothesis that these eruptions drove Neanderthals to extinction and cleared the way for modern humans to thrive in Europe and Asia.[7] The area is characterised by banks of piperno and pipernoid grey tuff at Camaldoli hill, like in the northern and western ridge of Mount Cumae; other referable deep products are those found at Monte di Procida, recognizable in the cliffs of its coast.
  • The Second Phlegraean Period. Between the 35,000-10,500 years ago,[3] it is characterized by the yellow tuff that constitutes the rests of an immense underwater volcano (having a diameter of ca. 15 kilometres (9.3 mi) and Pozzuoli to its center) Approximately 12,000 years ago the last major eruption occurred, forming a smaller caldera inside the main one, centered on the town of Pozzuoli. This event produced the Neapolitan yellow tuff, referring to the characteristic yellow rocks there.
  • The Third Phlegraean Period. Dated between 8,000 – 500 years ago,[3] it is characterized by white pozzolana, the material that forms the majority of volcanos in Flegrei Fields. Broadly speaking, it can be said there was an initial activity to the south-west in the zone of Bacoli and Baiae (10.000-8.000 years ago); an intermediate activity in an area centred between Pozzuoli, Spaccata Mountain and Agnano (8.000-3.900 years ago); and a more recent activity, moved towards the west to form Lake Avernus and Monte Nuovo (New Mountain) (3,800–500 years ago).

Volcanic deposit indicating possible eruption dated Ar at 315, 205, 157 and 18.0 kya[citation needed]

The caldera, which now is essentially at ground level, is accessible on foot. It contains a large number of fumaroles, from which steam can be seen issuing, and over 150 pools of boiling mud at last count. Several subsidiary cones and tuff craters lie within the caldera. One of these craters is filled by Lake Avernus. In 1538, an eight-day eruption in the area deposited enough material to create a new hill, Monte Nuovo. It has risen about 2 metres (7 ft) from ground level since 1970. It is a volcano capable of producing VEI 7 eruptions, as large as that of Tambora in 1815.[8] At present, the Campi Flegrei area comprises the Naples districts of Agnano and Fuorigrotta, the area of Pozzuoli, Bacoli, Monte di Procida, Quarto, the Phlegrean Islands (Ischia, Procida and Vivara).

A 2009 journal article stated that inflation of the caldera centre in the vicinity of Pozzuoli might presage an eruptive event within decades.[9] In 2012 the International Continental Scientific Drilling Programme planned to drill 3.5 km (2.2 miles) below the earth's surface near Pompeii intending to monitor the massive molten rock chamber below in order to provide early warning of any eruption. Local scientists are worried that such drilling itself could initiate an eruption or earthquake. In 2010 the Naples city council had prevented the drilling project. Programme scientists said the drilling was no different from industrial drilling in the area. The newly elected mayor allowed the project to go forward. A Reuters article emphasized that the area could produce a "super volcano" that might kill millions.[10]

Wine[edit]

Italian wine, both red and white, under the Campi Flegrei DOC appellation comes from this area. Grapes destined for DOC production must be harvested up to a maximum yield of 12 tonnes/hectare for red grape varieties and 13 tonnes/ha for white grape varieties. The finished wines need to be fermented to a minimum alcohol level of 11.5% for reds and 10.5% for whites. While most Campi Flegrei wines are blends, varietal wines can be made from individual varieties provided the variety used comprises at least 90% of the blend and the wine is fermented to at least 12% alcohol for reds and 11% for whites.[11]

Red Campi Flegrei is a blend of 50-70% Piedirosso, 10-30% Aglianico and/or Sciascinoso and up to 10% of other local (both red and white) grape varieties. The whites are composed of 50-70% Falanghina, 10-30% Biancolella and/or Coda di Volpe with up to 30% of other local white grape varieties.[11]

Cultural importance[edit]

Campi Flegrei has had strategical and cultural importance.

See also[edit]

Sources[edit]

This article has been completed with material from it:Campi Flegrei, Wikipedia in Italian and es:Campos Flegreos, Wikipedia in Spanish.

References[edit]

  1. ^ a b c d "Campi Flegrei". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=0101-01%3D. Retrieved 2008-09-20.
  2. ^ http://www.ov.ingv.it/OV/en/campi-flegrei.html
  3. ^ a b c Brand, Helen. "Volcanism and the Mantle: Campi Flegrei" (PDF). Retrieved 2008-06-18. 
  4. ^ De Vivo, B.; G. Rolandi, P. B. Gans, A. Calvert, W. A. Bohrson, F. J. Spera and H. E. Belkin (November 2001). "New constraints on the pyroclastic eruptive history of the Campanian volcanic Plain (Italy)". Mineralogy and Petrology (Springer Wien) 73 (1-3): p. 47–65. Bibcode:2001MinPe..73...47D. doi:10.1007/s007100170010. Retrieved 2008-09-20. 
  5. ^ Fisher, Richard V.; Giovanni Orsi; Michael Ort; Grant Heiken (June 1993). "Mobility of a large-volume pyroclastic flow — emplacement of the Campanian ignimbrite, Italy". Journal of Volcanology and Geothermal Research (Elsevier) 56 (3): pp. 205–220. Bibcode:1993JVGR...56..205F. doi:10.1016/0377-0273(93)90017-L. Retrieved 2008-09-20. 
  6. ^ Fedele, Francesco G.; et al. (2002). "Ecosystem Impact of the Campanian Ignimbrite Eruption in Late Pleistocene Europe". Quaternary Research 57 (3): 420–424. Bibcode:2002QuRes..57..420F. doi:10.1006/qres.2002.2331. Retrieved Oct 8, 2010. "Abstract" 
  7. ^ "Volcanoes Wiped out Neanderthals, New Study Suggests". ScienceDaily. Oct 7, 2010. Retrieved Oct 10, 2010. "The research is reported in the October issue of Current Anthropology" 
  8. ^ Newhall, Christopher G.; Self, Steve (1982). "The volcanic explosivity index (VEI): An estimate of explosive magnitude for historical volcanism". Journal of Geophysical Research 87 (C2): 1231–1238. Bibcode:1982JGR....87.1231N. doi:10.1029/JC087iC02p01231. 
  9. ^ Isaia, Roberto; Paola Marianelli; Alessandro Sbrana (2009). "Caldera unrest prior to intense volcanism in Campi Flegrei (Italy) at 4.0 ka B.P.: Implications for caldera dynamics and future eruptive scenarios". Geophysical Research Letters 36 (L21303): L21303. Bibcode:2009GeoRL..3621303I. doi:10.1029/2009GL040513. 
  10. ^ Antonio Denti, "Super volcano", global danger, lurks near Pompeii, Reuters, August 3, 2012.
  11. ^ a b P. Saunders Wine Label Language pg 132 Firefly Books 2004 ISBN 1-55297-720-X
  12. ^ "Pozzuoli:history,archeology,art,architecture,environment". 
  13. ^ Liubov Vitaliena Golovanova; Vladimir Borisovich Doronichev; Naomi Elancia Cleghorn; Marianna Alekseevna Koulkova; Tatiana Valentinovna Sapelko; M. Steven Shackley (2010; 51 (5): 655). "Volcanoes Wiped out Neanderthals, New Study Suggests" (news release). ScienceDaily (University of Chicago Press Journals). Journal Current Anthropology. doi:10.1086/656185. "Significance of Ecological Factors in the Middle to Upper Paleolithic Transition"  Check date values in: |date= (help)

External links[edit]