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Bouvet
楯状火山 · Norway · 741m

- タイプ
- 楯状火山
- 国
- Norway
- 地域
- 大西洋 / 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
英語版の要約Bouvet Island is an uninhabited subantarctic volcanic island and dependency of Norway. A protected nature reserve situated in the South Atlantic Ocean at the southern end of the Mid-Atlantic Ridge, it is the world's most remote island. Located north of 60°S latitude, Bouvet Island is not part of the southern region covered by the Antarctic Treaty System.
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噴火履歴
詳細タイムライン
- 紀元前 50年VEI 0地質学的推定BCE 50 ~ 進行中
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。