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Santorini

Volcán en escudo · 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
Tipo
Volcán en escudo
País
Greece
Región
European Volcanic Regions / Hellenic Volcanic Arc
Altitud
367 m
Coordenadas
36.404, 25.396
Última erupción
1950
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Shield
Roca principal
Dacite
Resumen geológico

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.

Resumen de Wikipedia

La caldera Santorini es una gran caldera volcánica, gran parte de la cual se encuentra sumergida, que se encuentra en la zona sur del mar Egeo, a 120 kilómetros de Creta en Grecia. Por encima de la superficie del mar está el grupo circular de las islas de Santorini, que se compone de Santorini, que es la isla principal, Therasia y Aspronisi en la periferia, y las dos islas Kameni en el centro del grupo.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1610 BCE~1412 BCE · 1 erupciones · VEI máx. 7226 BCE~28 BCE · 1 erupciones · VEI máx. 328 BCE~170 · 1 erupciones · VEI máx. 3566~763 · 1 erupciones · VEI máx. 41554~1752 · 2 erupciones · VEI máx. 31752~1950 · 5 erupciones · VEI máx. 21610 BCE819 BCE1709611752

Línea de tiempo detallada

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

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.