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Furnas

成層火山 · Portugal · 805m

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. · 写真: Photo by Rick Wunderman, 1997 (Smithsonian Institution). · Wikimedia Commons
タイプ
成層火山
Portugal
地域
Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
標高
805m
座標
37.770, -25.320
最終噴火
1630年
テクトニクス環境
Rift zone / Oceanic crust (< 15 km)
火山地形
Composite
主要岩石
Trachyte / Trachydacite
地質学的概要

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.

Wikipedia の要約

英語版の要約

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.

Wikipedia · CC BY-SA · 記事全文を読む

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
4570 BCE~4363 BCE · 1件 · 最大 VEI ?1677 BCE~1470 BCE · 1件 · 最大 VEI ?437 BCE~230 BCE · 1件 · 最大 VEI ?23 BCE~183 · 1件 · 最大 VEI 5803~1010 · 1件 · 最大 VEI 41010~1217 · 1件 · 最大 VEI 41423~1630 · 3件 · 最大 VEI 54570 BCE3123 BCE1470 BCE23 BCE1423

詳細タイムライン

  1. 1630年VEI 5観測記録
    1630-09-03 ~ 1630-11-02
    South end of caldera (Pico da Areia)
  2. 1441年 (±2年)VEI 4観測記録
    1441 ~ 進行中
    Center of caldera (Gaspar)
  3. 1430年 (±100年)VEI 3地質学的推定
    1430 ~ 進行中
    East caldera floor
  4. 1170年 (±100年)VEI 4地質学的推定
    1170 ~ 進行中
    E caldera floor (Lake crater)
  5. 840年 (±100年)VEI 4地質学的推定
    840 ~ 進行中
    Center of caldera (Gaspar)
  6. 80年 (±100年)VEI 5地質学的推定
    80 ~ 進行中
    N floor of younger caldera
  7. 紀元前 360年 (±150年)VEI ?地質学的推定
    BCE 360 ~ 進行中
  8. 紀元前 1670年 (±1460年)VEI ?地質学的推定
    BCE 1670 ~ 進行中
  9. 紀元前 4570年VEI ?地質学的推定
    BCE 4570 ~ 進行中
    East rim of caldera (Pico do Canário)

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。