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Furnas

Estratovolcán · Portugal · 805 m

Furnas volcano, at the eastern end of Sao Miguel Island, contains two nested calderas. The southern rim of the younger 6-km-wide caldera is seen here from the north, with Furnas Lake on the right foreground. At least 10 trachytic pumice layers, all erupted during the past 5,000 years, post-date the caldera. The dome with the semi-circle of trees in the center behind the lake is the site of the most recent eruption at Furnas, a sub-Plinian eruption in 1630 CE.
Furnas volcano, at the eastern end of Sao Miguel Island, contains two nested calderas. The southern rim of the younger 6-km-wide caldera is seen here from the north, with Furnas Lake on the right foreground. At least 10 trachytic pumice layers, all erupted during the past 5,000 years, post-date the caldera. The dome with the semi-circle of trees in the center behind the lake is the site of the most recent eruption at Furnas, a sub-Plinian eruption in 1630 CE. · Foto: Photo by Rick Wunderman, 1997 (Smithsonian Institution). · Wikimedia Commons
Tipo
Estratovolcán
País
Portugal
Región
Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
Altitud
805 m
Coordenadas
37.770, -25.320
Última erupción
1630
Contexto tectónico
Rift zone / Oceanic crust (< 15 km)
Forma volcánica
Composite
Roca principal
Trachyte / Trachydacite
Resumen geológico

Furnas volcano lies at the eastern end of Sao Miguel Island, immediately west of the older Nordeste shield volcano and its Povoaçao caldera. There are at least two calderas, a younger one that is 6-km wide and a larger older one that is less topographically distinct. The eastern wall of the 500-m-deep Furnas caldera overlaps the western wall of the Nordeste Povoaçao caldera. Volcanic activity dates back about 100,000 years. At least 11 trachytic pumice layers, all erupted during the past 5000 years, post-date the caldera. The most prominent post-caldera feature is the Pico do Gaspar lava dome, east of the Lagoa das Furnas caldera lake. A zone of late-Pleistocene to Holocene basaltic-to-trachytic cinder cones and lava domes is located between Furnas and Agua de Pau volcanoes. Two historical eruptions have occurred, one sometime between 1439 and 1443 and the other in 1630. The latter was one of the largest Holocene explosive eruptions in the Azores and caused significant damage and fatalities.

Resumen de Wikipedia

Furnas es una freguesia portuguesa perteneciente al municipio de Povoação, situado en la Isla de São Miguel, Región Autónoma de Azores.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
4570 BCE~4363 BCE · 1 erupciones · VEI máx. ?1677 BCE~1470 BCE · 1 erupciones · VEI máx. ?437 BCE~230 BCE · 1 erupciones · VEI máx. ?23 BCE~183 · 1 erupciones · VEI máx. 5803~1010 · 1 erupciones · VEI máx. 41010~1217 · 1 erupciones · VEI máx. 41423~1630 · 3 erupciones · VEI máx. 54570 BCE3123 BCE1470 BCE23 BCE1423

Línea de tiempo detallada

  1. 1630VEI 5Observado
    1630-09-03 – 1630-11-02
    South end of caldera (Pico da Areia)
  2. 1441 (±2 años)VEI 4Observado
    1441 – En curso
    Center of caldera (Gaspar)
  3. 1430 (±100 años)VEI 3Estimación geológica
    1430 – En curso
    East caldera floor
  4. 1170 (±100 años)VEI 4Estimación geológica
    1170 – En curso
    E caldera floor (Lake crater)
  5. 840 (±100 años)VEI 4Estimación geológica
    840 – En curso
    Center of caldera (Gaspar)
  6. 80 (±100 años)VEI 5Estimación geológica
    80 – En curso
    N floor of younger caldera
  7. 360 a. C. (±150 años)VEI ?Estimación geológica
    BCE 360 – En curso
  8. 1670 a. C. (±1460 años)VEI ?Estimación geológica
    BCE 1670 – En curso
  9. 4570 a. C.VEI ?Estimación geológica
    BCE 4570 – En curso
    East rim of caldera (Pico do Canário)

Enlaces externos

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