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Campi Flegrei

Kaldera · Italy · 458 m

A Landsat satellite image shows the Campi Flegrei caldera north of the Bay of Naples. The 13-km-wide caldera, immediately west of the city of Naples (upper right), was created following massive explosive eruptions about 34,000 and 12,000 years ago. Subsequent eruptions formed numerous craters and cones within the caldera and along its margins. The most recent eruption created the Monte Nuovo tuff cone in 1538.
A Landsat satellite image shows the Campi Flegrei caldera north of the Bay of Naples. The 13-km-wide caldera, immediately west of the city of Naples (upper right), was created following massive explosive eruptions about 34,000 and 12,000 years ago. Subsequent eruptions formed numerous craters and cones within the caldera and along its margins. The most recent eruption created the Monte Nuovo tuff cone in 1538. · Foto: NASA Landsat image, 1984. · Wikimedia Commons
Tipe
Kaldera
Negara
Italy
Wilayah
European Volcanic Regions / Italian Peninsula Volcanic Provinces
Ketinggian
458 m
Koordinat
40.827, 14.139
Letusan terakhir
1538
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Caldera
Batuan utama
Trachyte / Trachydacite
Ringkasan geologi

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 eruption were in 1158 CE at Solfatara and activity in 1538 CE that formed the Monte Nuovo cinder cone.

Ringkasan Wikipedia

Campi Flegrei adalah kaldera besar yang terletak di sebelah barat Napoli, Italia. Kawasan gunung ini dinyatakan sebagai taman regional pada tahun 2003. Area kaldera terdiri dari 24 kepundan dan bangunan vulkanik; kebanyakan dari mereka berada di bawah air. Aktivitas hidrotermal dapat diamati di Lucrino, Agnano dan di kota Pozzuoli. Ada juga manifestasi gas efusif di kawah Solfatara, rumah mitologi dewa api Romawi, Vulcan. Kawasan ini dipantau oleh Observatorium Vesuvius.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
8480 BCE~8146 BCE · 1 letusan · VEI maks. 48146 BCE~7812 BCE · 1 letusan · VEI maks. 37812 BCE~7478 BCE · 1 letusan · VEI maks. ?6810 BCE~6476 BCE · 2 letusan · VEI maks. 46476 BCE~6142 BCE · 1 letusan · VEI maks. ?3137 BCE~2803 BCE · 1 letusan · VEI maks. ?2803 BCE~2469 BCE · 2 letusan · VEI maks. 42469 BCE~2135 BCE · 4 letusan · VEI maks. 52135 BCE~1801 BCE · 4 letusan · VEI maks. 41801 BCE~1467 BCE · 1 letusan · VEI maks. 4870~1204 · 1 letusan · VEI maks. 11204~1538 · 1 letusan · VEI maks. 38480 BCE6142 BCE3471 BCE1133 BCE1204

Garis waktu rinci

  1. 1538VEI 3Teramati
    1538-09-29 – 1538-10-06
    Monte Nuovo
  2. 1198VEI 1Teramati
    1198 – Berlangsung
    Solfatara
  3. 1650 SMVEI 4Perkiraan geologi
    BCE 1650 – Berlangsung
    Fossa Lupara (Monte Senga)
  4. 1870 SM (±50 tahun)VEI 4Perkiraan geologi
    BCE 1870 – Berlangsung
    Astroni
  5. 2000 SM (±150 tahun)VEI 4Perkiraan geologi
    BCE 2000 – Berlangsung
    Averno
  6. 2040 SMVEI 3Perkiraan geologi
    BCE 2040 – Berlangsung
    Solfatara
  7. 2080 SM (±75 tahun)VEI 2Perkiraan geologi
    BCE 2080 – Berlangsung
    Monte Olibano-Accademia
  8. 2150 SM (±500 tahun)VEI 5Perkiraan geologi
    BCE 2150 – Berlangsung
    Agnano Monte Spina
  9. 2220 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 2220 – Berlangsung
    Eastern NYT caldera
  10. 2330 SM (±150 tahun)VEI 3Perkiraan geologi
    BCE 2330 – Berlangsung
  11. 2440 SMVEI ?Perkiraan geologi
    BCE 2440 – Berlangsung
    Agnano-Monte Sant'Angelo
  12. 2500 SMVEI 4Perkiraan geologi
    BCE 2500 – Berlangsung
    Cigliano
  13. 2580 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 2580 – Berlangsung
  14. 2890 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 2890 – Berlangsung
    East part of NYT caldera
  15. 6300 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 6300 – Berlangsung
    N part of NYT caldera (San Martino)
  16. 6490 SMVEI 3Perkiraan geologi
    BCE 6490 – Berlangsung
    Eastern part of NYT caldera
  17. 6650 SM (±100 tahun)VEI 4Perkiraan geologi
    BCE 6650 – Berlangsung
    Fondi di Baia, Sartania
  18. 7590 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 7590 – Berlangsung
    NE part of NYT caldera
  19. 7980 SM (±500 tahun)VEI 3Perkiraan geologi
    BCE 7980 – Berlangsung
    Soccavo, Minapoli, Pisani & other vents
  20. 8480 SM (±100 tahun)VEI 4Perkiraan geologi
    BCE 8480 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.