イギリス · 成層火山
ナイチンゲール島
Nightingale Island
- タイプ
- 成層火山
- 標高
- 365m
- 最終噴火
- 2004年

- タイプ
- 成層火山
- 国
- イギリス
- 地域
- 大西洋 / Southern Atlantic Volcano Group
- 標高
- 365m
- 座標
- -37.420, -12.480
- 最終噴火
- 2004年
- テクトニクス環境
- リフト帯 / 海洋地殻 (< 15 km)
- 火山地形
- 複成火山
- 主要岩石
- 粗面岩 / 粗面デイサイト
地質学的概要
Nightingale Island, along with the adjacent smaller Middle (or Alex) and Stoltenhoff Islands and associated small islets, are the southernmost of the Tristan da Cunha island group. The heavily eroded island consists of ash and agglomerate units with intervening massive trachytic intrusions and lava flows. Volcanic rocks were K-Ar dated at between 400,000 and 150,000 years, and a radiocarbon date of about 39,000 years BP was obtained from an ash layer overlain by a lava flow. An earthquake swarm lasting 6 hours beginning on 29 July 2004 was followed by observation of large blocks of floating phonolitic pumice that washed up on Tristan da Cunha. The pumice was considered to be from an eruption associated with an earthquake swarm 37-53 km SSE of Tristan da Cunha on the submarine SE flank of Nightingale Island.
Wikipedia の要約
英語版の要約Nightingale Island is an active volcanic island in the South Atlantic Ocean, 3 square kilometres (1.2 sq mi) in area, part of the Tristan da Cunha group of islands. They are administered by the United Kingdom as part of the overseas territory of Saint Helena, Ascension and Tristan da Cunha.
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噴火履歴
1件の記録用語集詳細タイムライン
- 2004年VEI 0観測記録2004-07-29 ~ 2004-07-30Submarine SE flank
近くの火山
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。