サウス・アイランド
Lake Turkana South Island
成層火山 · Kenya · 800m

- タイプ
- 成層火山
- 国
- Kenya
- 地域
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- 標高
- 800m
- 座標
- 2.636, 36.596
- 最終噴火
- 1888年
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The southernmost and largest of the three volcanic islands in Lake Turkana, South Island (sometimes referred to as Hohnel Island), contains numerous tuff cones. Early stage cone formation may have been associated with a high stand of Lake Turkana dated at about 10,000 years ago, and later subaerial activity postdates the last high stand of the lake about 3,200 years ago. The island is within a volcanic horst that extends 10 km to the N beneath the lake surface. Dominantly basaltic lava flows erupted from a N-S fissure extending the 11-km length of the island are morphologically similar to Holocene flows from The Barrier volcano at the S end of Lake Turkana. An eruption from a scoria cone on the island was witnessed during Count von Teliki's 1888 expedition.
Wikipedia の要約
英語版の要約South Island, or Hohnel Island, is a fissure-formed volcanic island and the largest one out of 3 other major islands in Lake Turkana, Kenya. This volcano was discovered in 1888 while it was erupting by Count Teleki, a Hungarian explorer who led the first expedition into the region. It is a part of the Lake Turkana National Parks, which is a UNESCO World Heritage Site.
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噴火履歴
詳細タイムライン
- 1888年VEI 1観測記録1888 ~ 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。