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ブーベ島

Bouvet

楯状火山 · Norway · 741m

The uninhabited shield volcano of Bouvet Island is depicted from the SE in this 26 November  1898 watercolor painting. About 95% of the 10-km-wide island is glaciated, and sampling on this basaltic-to-rhyolitic volcano has been restricted to coastal cliffs. A caldera on the opposite (NW) side of the island is breached to the sea. Bouvet, also referred to as Bouvetoya, is located just off the Southwest Indian Ridge, east of the triple junction between the African, South American, and Antarctic plates.
The uninhabited shield volcano of Bouvet Island is depicted from the SE in this 26 November 1898 watercolor painting. About 95% of the 10-km-wide island is glaciated, and sampling on this basaltic-to-rhyolitic volcano has been restricted to coastal cliffs. A caldera on the opposite (NW) side of the island is breached to the sea. Bouvet, also referred to as Bouvetoya, is located just off the Southwest Indian Ridge, east of the triple junction between the African, South American, and Antarctic plates. · 写真: Watercolor painting by F. Winter, 1898 (In: Chun, 1903; courtesy of NOAA Photo Library). · Wikimedia Commons
タイプ
楯状火山
Norway
地域
Atlantic Ocean Volcanic Regions / Southern Atlantic Volcano Group
標高
741m
座標
-54.408, 3.351
最終噴火
-50年
テクトニクス環境
Rift zone / Oceanic crust (< 15 km)
火山地形
Shield
主要岩石
Basalt / Picro-Basalt
地質学的概要

The solitary ice-covered shield volcano of Bouvet Island is located just off the Southwest Indian Ridge, east of the triple junction between the African, South American, and Antarctic plates. This basaltic-to-rhyolitic island, also referred to as Bouvetoya, was discovered by and later named for Captain Lozier-Bouvet during his 1739 search for the "great southern continent." About 95% of the uninhabited 10-km-wide island is covered by glaciers. The most prominent feature is the 3.5-km-wide Wilhelmplataet caldera, which is breached to the sea on the NW side. A late-stage rhyolitic lava dome forms the Cape Valdivia peninsula on the N flank. A paleomagnetic investigation was made by Lovlie and Furnes (1978) of a massive basaltic lava flow unit at Cape Meteor; based on oriented drill cores they tentatively inferred a minimum age of 2000 years.

Wikipedia の要約

ブーベ島 は、南大西洋の亜南極に浮かぶノルウェー領の火山島である。2022年現在、無人島である。ケープタウン(南アフリカ)の南南西約 2,500 km に位置する。最も近い陸地(南極大陸)との距離は 1,700 km であり、地理的に世界で最も隔絶した孤島である。島には無人の気象観測所がある。

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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
50 BCE~50 BCE · 1件 · 最大 VEI 050 BCE50 BCE49 BCE49 BCE49 BCE

詳細タイムライン

  1. 紀元前 50年VEI 0地質学的推定
    BCE 50 ~ 進行中

外部リンク

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