カメルーン · 火山原
Oku Volcanic Field
- タイプ
- 火山原
- 標高
- 3011m
- 最終噴火
- 不明

- タイプ
- 火山原
- 国
- カメルーン
- 地域
- 北アフリカ / Western Africa Volcanic Province
- 標高
- 3011m
- 座標
- 6.250, 10.500
- 最終噴火
- 不明
- テクトニクス環境
- プレート内部 / 大陸地殻 (> 25 km)
- 火山地形
- 火山群
- 主要岩石
- 玄武岩 / ピクライト質玄武岩
地質学的概要
Numerous maars and basaltic cinder cones lie on or near the deeply dissected rhyolitic and trachytic Mount Oku massif along the Cameroon volcanic line. The Mount Oku stratovolcano is cut by a large caldera. The Oku volcanic field is noted for two crater lakes, Lake Nyos to the N and Lake Monoun to the S, that have produced catastrophic carbon-dioxide gas release events. The 15 August 1984 gas release at Lake Monoun was attributed to overturn of stratified lake water, triggered by an earthquake and landslide. The Lake Nyos event on 21 August 1986 caused at least 1,700 fatalities. The emission of ~1 km3 of magmatic carbon dioxide has been attributed either to overturn of stratified lake waters as a result of a non-volcanic process, or to phreatic explosions or injection of hot gas into the lake.
Wikipedia の要約
英語版の要約The Oku Volcanic Field or Oku Massif is a group of volcanoes based on a swell in the Cameroon Volcanic Line, located in the Oku region of the Western High Plateau of Cameroon. The Mount Oku stratovolcano rises to 3,011 m above sea level.
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噴火履歴
2件の記録用語集詳細タイムライン
- 1986年VEI ?根拠の記載なし1986-08-21 ~ 1986-12-30Lake Nyos
- 1550年 (±100年)VEI 3根拠の記載なし1550 ~ 終了日不明Lake Nyos
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。