Italy · Caldera
Mount Olibano
Campi Flegrei
- Type
- Caldera
- Elevation
- 458m
- Last eruption
- 1538
- Type
- Caldera
- Country
- Italy
- Region
- Europe / Italian Peninsula Volcanic Provinces
- Elevation
- 458m
- Coordinates
- 40.827, 14.139
- Last eruption
- 1538
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Trachyte / Trachydacite
Geological summary
Campi Flegrei is a 13-km-wide caldera that encompasses part of Naples and extends to the south beneath the Gulf of Pozzuoli. Episodes of significant uplift and subsidence within the dominantly trachytic caldera have occurred since Roman times. The earliest known eruptive products are dated 47,000 years BP. The caldera formed following two large explosive eruptions, the massive Campanian ignimbrite about 36,000 BP, and the over 40 km3 Neapolitan Yellow Tuff (NYT) about 15,000 BP. Following eruption of the NYT a large number of eruptions originated from widely scattered subaerial and submarine vents. Most activity occurred during three intervals: 15,000-9,500, 8,600-8,200, and 4,800-3,800 BP. The latest eruptions were in 1158 CE at Solfatara and in 1538 CE when the Monte Nuovo cinder cone was built.
From Wikipedia
The Phlegraean Fields is a large volcanic caldera west of Naples, Italy. The Neapolitan Yellow Tuff eruption produced just 50 cubic kilometers. It is, however, one of relatively few volcanoes large enough to form a caldera. It is part of the Campanian volcanic arc, which includes Mount Vesuvius, about 9 km east of Naples. The Phlegraean Fields is monitored by the Vesuvius Observatory. Part of the city of Naples is built over it. The Phlegraean Fields' largest known eruptions have an estimated volcanic explosivity index (VEI) of 7. It is often called a supervolcano in popular media, although the accepted definition for that term is a volcano that has had an eruption with a VEI of 8, the highest level.
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Eruption history
20 recordedGlossaryDetailed timeline
- 1538VEI 3Observed1538-09-29 – 1538-10-06Monte Nuovo
- 1198VEI 1Observed1198 – end unknownSolfatara
- 1650 BCEVEI 4Geological estimate1650 BCE – end unknownFossa Lupara (Monte Senga)
- 1870 BCE (±50 yrs)VEI 4Geological estimate1870 BCE – end unknownAstroni
- 2000 BCE (±150 yrs)VEI 4Geological estimate2000 BCE – end unknownAverno
- 2040 BCEVEI 3Geological estimate2040 BCE – end unknownSolfatara
- 2080 BCE (±75 yrs)VEI 2Geological estimate2080 BCE – end unknownMonte Olibano-Accademia
- 2150 BCE (±500 yrs)VEI 5Geological estimate2150 BCE – end unknownAgnano Monte Spina
- 2220 BCE (±50 yrs)VEI ?Geological estimate2220 BCE – end unknownEastern NYT caldera
- 2330 BCE (±150 yrs)VEI 3Geological estimate2330 BCE – end unknown
- 2440 BCEVEI ?Geological estimate2440 BCE – end unknownAgnano-Monte Sant'Angelo
- 2500 BCEVEI 4Geological estimate2500 BCE – end unknownCigliano
- 2580 BCE (±50 yrs)VEI ?Geological estimate2580 BCE – end unknown
- 2890 BCE (±50 yrs)VEI ?Geological estimate2890 BCE – end unknownEast part of NYT caldera
- 6300 BCE (±50 yrs)VEI ?Geological estimate6300 BCE – end unknownN part of NYT caldera (San Martino)
- 6490 BCEVEI 3Geological estimate6490 BCE – end unknownEastern part of NYT caldera
- 6650 BCE (±100 yrs)VEI 4Geological estimate6650 BCE – end unknownFondi di Baia, Sartania
- 7590 BCE (±50 yrs)VEI ?Geological estimate7590 BCE – end unknownNE part of NYT caldera
- 7980 BCE (±500 yrs)VEI 3Geological estimate7980 BCE – end unknownSoccavo, Minapoli, Pisani & other vents
- 8480 BCE (±100 yrs)VEI 4Geological estimate8480 BCE – end unknown
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.