カリシンビ山
Karisimbi
成層火山 · DR Congo-Rwanda · 4490m

- タイプ
- 成層火山
- 国
- DR Congo-Rwanda
- 地域
- 東アフリカ / Albertine Rift Volcanic Province
- 標高
- 4490m
- 座標
- -1.506, 29.450
- 最終噴火
- -8050年
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Trachybasalt / Tephrite Basanite
地質学的概要
Karisimbi is a complex basanitic-to-trachytic volcano with a symmetrical sharp-peaked summit. The 2-km-wide Branca caldera, located SE of the summit, is filled by viscous lava flows and two explosion craters. The large 1.2-km-wide Muntango pit crater is located south of the summit. A broad lava plain, formed from lava flows erupted within the caldera and along a chain of cones, extends SW. More than 100 cones erupted along a NNE-SSW zone that extends to the shores of Lake Kivu. The youngest Potassium-Argon date obtained is about 10,000 years before present (de Mulder, 1985). The youngest eruptions produced a group of dome-shaped vents east of the caldera, which fed viscous lava flows that traveled as far as 12 km E, and lava flows from the SW-flank lava vents.
Wikipedia の要約
英語版の要約Mount Karisimbi is a stratovolcano in the Virunga Mountains on the border between Rwanda and the Democratic Republic of Congo. At 4,507 metres (14,787 ft), Karisimbi is the highest of the eight major mountains of the mountain range, which is a part of Albertine Rift, the western branch of the East African Rift. Karisimbi is flanked by Mikeno to the north, Bisoke to the east and Nyiragongo to the west, on the other side of the Rift Valley. Karisimbi is the 11th highest mountain of Africa and ranked 61st by prominence.
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噴火履歴
詳細タイムライン
- 紀元前 8050年VEI ?地質学的推定BCE 8050 ~ 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。