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Furnas

Stratovolkan · 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
Tipe
Stratovolkan
Negara
Portugal
Wilayah
Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
Ketinggian
805 m
Koordinat
37.770, -25.320
Letusan terakhir
1630
Kondisi tektonik
Rift zone / Oceanic crust (< 15 km)
Bentuk lahan
Composite
Batuan utama
Trachyte / Trachydacite
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

Furnas is a civil parish in the municipality of Povoação on the island of São Miguel in the Portuguese Azores. The population in 2011 was 1,439, in an area of 34.43 km2. The parish is one of the largest in the island and in the Azores. It is located east of Lagoa and Ponta Delgada, west of Povoação and southeast of Ribeira Grande.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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4570 BCE~4363 BCE · 1 letusan · VEI maks. ?1677 BCE~1470 BCE · 1 letusan · VEI maks. ?437 BCE~230 BCE · 1 letusan · VEI maks. ?23 BCE~183 · 1 letusan · VEI maks. 5803~1010 · 1 letusan · VEI maks. 41010~1217 · 1 letusan · VEI maks. 41423~1630 · 3 letusan · VEI maks. 54570 BCE3123 BCE1470 BCE23 BCE1423

Garis waktu rinci

  1. 1630VEI 5Teramati
    1630-09-03 – 1630-11-02
    South end of caldera (Pico da Areia)
  2. 1441 (±2 tahun)VEI 4Teramati
    1441 – Berlangsung
    Center of caldera (Gaspar)
  3. 1430 (±100 tahun)VEI 3Perkiraan geologi
    1430 – Berlangsung
    East caldera floor
  4. 1170 (±100 tahun)VEI 4Perkiraan geologi
    1170 – Berlangsung
    E caldera floor (Lake crater)
  5. 840 (±100 tahun)VEI 4Perkiraan geologi
    840 – Berlangsung
    Center of caldera (Gaspar)
  6. 80 (±100 tahun)VEI 5Perkiraan geologi
    80 – Berlangsung
    N floor of younger caldera
  7. 360 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 360 – Berlangsung
  8. 1670 SM (±1460 tahun)VEI ?Perkiraan geologi
    BCE 1670 – Berlangsung
  9. 4570 SMVEI ?Perkiraan geologi
    BCE 4570 – Berlangsung
    East rim of caldera (Pico do Canário)

Tautan eksternal

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