Vai al contenuto principale

Furnas

Stratovulcano · 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
Stratovulcano
Paese
Portugal
Regione
Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
Altitudine
805 m
Coordinate
37.770, -25.320
Ultima eruzione
1630
Contesto tettonico
Rift zone / Oceanic crust (< 15 km)
Forma vulcanica
Composite
Roccia principale
Trachyte / Trachydacite
Sintesi geologica

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.

Sintesi da Wikipedia

Furnas è una frazione (freguesia) di Povoação, città portoghese sull'isola di São Miguel, nelle Azzorre.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
4570 BCE~4363 BCE · 1 eruzioni · VEI max. ?1677 BCE~1470 BCE · 1 eruzioni · VEI max. ?437 BCE~230 BCE · 1 eruzioni · VEI max. ?23 BCE~183 · 1 eruzioni · VEI max. 5803~1010 · 1 eruzioni · VEI max. 41010~1217 · 1 eruzioni · VEI max. 41423~1630 · 3 eruzioni · VEI max. 54570 BCE3123 BCE1470 BCE23 BCE1423

Cronologia dettagliata

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

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.