Mount Homa
Homa Mountain
複成火山 · Kenya · 1751m

- タイプ
- 複成火山
- 国
- Kenya
- 地域
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- 標高
- 1751m
- 座標
- -0.380, 34.500
- 最終噴火
- 不明
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Foidite
地質学的概要
Homa Mountain is a large carbonatitic complex with a flat-topped summit that forms a broad peninsula on the E shore of Lake Victoria. This dominantly Miocene-to-Pleistocene complex contains numerous flank vents, including the carbonatitic and ultramafic Lake Simbi maar on the lower E flank. The Chiewo, Got Ojawa, and Got Oloo vents on the S and W sides of Homa Mountain were formed during the latest stage of carbonatitic activity. Legends of inhabitants near the Lake Simbi maar suggest that it may have been formed in historical time.
Wikipedia の要約
英語版の要約Mount Homa is a complex volcano located in western Kenya. It forms a broad peninsula on the southern shore of Winam Gulf, an extension of Lake Victoria. This peninsula defines Homa Bay and the mountaintop is about 20 kilometres (12 mi) north of the town of that name.
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