ロンゴノット山
Longonot
成層火山 · Kenya · 2776m

- タイプ
- 成層火山
- 国
- Kenya
- 地域
- 東アフリカ / Kenyan Rift Volcanic Province
- 標高
- 2776m
- 座標
- -0.914, 36.446
- 最終噴火
- 1863年
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Trachyte / Trachydacite
地質学的概要
The trachytic Longonot stratovolcano SE of Lake Naivasha in the Gregory Rift valley contains a 8 x 12 km caldera. Formation of the caldera accompanied large explosive eruptions about 21,000 years ago. A large central cone that was constructed within the caldera, which forms the summit, is truncated by a circular, 1.8-km-wide crater. Post-caldera lavas are found on the caldera floor and the volcano's flanks, marking a late stage of effusive eruptions. A well-preserved satellitic cone is located on the NE flank. Masai tradition records a lava flow on the N flank during the 19th century. Similarly youthful-looking lava flows occur on the SW flank.
Wikipedia の要約
英語版の要約Mount Longonot is a stratovolcano located southeast of Lake Naivasha in the Great Rift Valley of Kenya, Africa. It is thought to have last erupted in the 1860s. Its name is derived from the Maasai word Olongongot, meaning "mountains of many spurs" or "steep ridges".
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噴火履歴
詳細タイムライン
- 1863年 (±5年)VEI 0地質学的推定1863-07-02 ~ 進行中Northern flank
- 紀元前 1330年 (±100年)VEI ?地質学的推定BCE 1330 ~ 進行中
- 紀元前 7200年 (±100年)VEI ?地質学的推定BCE 7200 ~ 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。