メネンガイ
Menengai
楯状火山 · Kenya · 2278m

- タイプ
- 楯状火山
- 国
- Kenya
- 地域
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- 標高
- 2278m
- 座標
- -0.200, 36.070
- 最終噴火
- -6050年
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Trachyte / Trachydacite
地質学的概要
The massive Menengai shield volcano occupies the floor of the East African Rift. Construction of a 30 km3 shield volcano beginning about 200,000 years ago was followed by the eruption of two voluminous ash-flow tuffs, each preceded by major pumice falls. The first took place about 29,000 years ago and produced a large caldera. The second, producing about 30 km3 of compositionally zoned peralkaline trachytic magma about 8000 years ago, was associated with formation of the present-day 8 x 12 km summit caldera. More than 70 post-caldera lava flows cover the caldera floor, the youngest of which may be only a few hundred years old. No historical eruptions are known. Fumarolic activity is restricted to the caldera.
Wikipedia の要約
英語版の要約Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley. The volcano formed about 200,000 years ago and the prominent 12 x 8 km caldera formed about 8000 years ago. The caldera floor is covered with numerous post caldera lava flows. The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world. Menengai has very little sediment in the caldera which is a thick mass of lava boulders and inaccessible ridges. Volcanic activity continues and a current project under the GDC is at an advanced stage towards geothermal power generation.
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噴火履歴
詳細タイムライン
- 紀元前 6050年VEI 6地質学的推定BCE 6050 ~ 進行中
- 紀元前 7350年 (±500年)VEI ?地質学的推定BCE 7350 ~ 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。