Lewati ke konten utama

Kaldera Santorini

Santorini

Gunung api perisai · Greece · 367 m

The steep inner walls of Santorini drop steeply into the caldera bay. Pyroclastic flow deposits from four caldera-forming eruptions dating back to 100,000 years ago are exposed in the caldera walls in this N-looking view. The youngest caldera was formed about 3,500 years ago during the Minoan eruption of Santorini. The flat-topped peak on the left skyline is Skaros, a remnant of a shield volcano constructed within a previous caldera.
The steep inner walls of Santorini drop steeply into the caldera bay. Pyroclastic flow deposits from four caldera-forming eruptions dating back to 100,000 years ago are exposed in the caldera walls in this N-looking view. The youngest caldera was formed about 3,500 years ago during the Minoan eruption of Santorini. The flat-topped peak on the left skyline is Skaros, a remnant of a shield volcano constructed within a previous caldera. · Foto: Photo by Lee Siebert, 1994 (Smithsonian Institution). · Wikimedia Commons
Tipe
Gunung api perisai
Negara
Greece
Wilayah
European Volcanic Regions / Hellenic Volcanic Arc
Ketinggian
367 m
Koordinat
36.404, 25.396
Letusan terakhir
1950
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Dacite
Ringkasan geologi

Santorini (Thera), in the Aegean Sea, has steep-walled caldera rim with villages that overlook an active volcanic island in the center of a caldera bay. The circular island group is composed of overlapping shield volcanoes cut by at least four partially overlapping calderas. The oldest southern caldera was formed about 180,000 years before present (BP), followed by the Skaros caldera about 70,000 BP, and then the Cape Riva caldera about 21,000 BP. The youngest caldera formed about 3,600 BP (around 1600 BCE) during the Late-Bronze-Age Minoan eruption that forced abandonment of the island. Post-Minoan eruptions beginning in 197 BCE constructed a series of lava domes and flows that form two islands near the center of the caldera. The latest eruption produced a small lava dome and flow in 1950, accompanied by explosive activity.

Ringkasan Wikipedia

Kaldera Santorini adalah kaldera besar yang sudah tenggelam sebagian. Kaldera ini terletak di Laut Aegea selatan di Yunani, sekitar 120 km di sebelah utara pulau Kreta. Kaldera yang berada di atas permukaan laut membentuk Kepulauan Santorini yang kini merupakan tujuan wisata yang sangat populer. Di tengah kaldera ini juga terdapat dua pulau vulkanik kecil, yaitu pulau Nea Kameni dan Palea Kameni. Kedua pulau yang terbuat dari batu lava ini terbentuk dari sejumlah letusan bawah laut.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1610 BCE~1412 BCE · 1 letusan · VEI maks. 7226 BCE~28 BCE · 1 letusan · VEI maks. 328 BCE~170 · 1 letusan · VEI maks. 3566~763 · 1 letusan · VEI maks. 41554~1752 · 2 letusan · VEI maks. 31752~1950 · 5 letusan · VEI maks. 21610 BCE819 BCE1709611752

Garis waktu rinci

  1. 1950VEI 2Teramati
    1950-01-10 – 1950-02-02
    Nea Kameni (Liatsikas dome)
  2. 1939VEI 2Teramati
    1939-08-20 – 1941-07-02
    Nea Kameni (Triton, Ktenas, Fouque domes)
  3. 1928VEI 2Teramati
    1928-01-23 – 1928-03-17
    Nea Kameni (Naftilos dome)
  4. 1925VEI 2Teramati
    1925-08-11 – 1926-05
    Nea Kameni (Dafni dome)
  5. 1866VEI 2Teramati
    1866-01-26 – 1870-10-15
    Georgios, Afroessa and Reka domes
  6. 1707VEI 3Teramati
    1707-05-23 – 1711-09-14
    Nea Kameni
  7. 1570VEI 3Teramati
    1570 – 1573
    Mikri Kameni
  8. 726VEI 4Teramati
    726-07-15 – Berlangsung
    NE side of Thia Island
  9. 46VEI 3Teramati
    46-12-31 – 47-02-01
    Thia Island
  10. 197 SMVEI 3Teramati
    BCE 197 – Berlangsung
    Hiera Island
  11. 1610 SM (±14 tahun)VEI 7Perkiraan geologi
    BCE 1610 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.