Oku Volcanic Field
火山原 · Cameroon · 3011m

- タイプ
- 火山原
- 国
- Cameroon
- 地域
- Northern Africa Volcanic Regions / 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
- Intraplate / Continental crust (> 25 km)
- 火山地形
- Cluster
- 主要岩石
- Basalt / Picro-Basalt
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
詳細タイムライン
- 1986年VEI ?地質学的推定1986-08-21 ~ 1986-12-30Lake Nyos
- 1550年 (±100年)VEI 3地質学的推定1550 ~ 進行中Lake Nyos
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。