Gada Ale
成層火山 · Ethiopia · 287m

- タイプ
- 成層火山
- 国
- Ethiopia
- 地域
- Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
- 標高
- 287m
- 座標
- 13.975, 40.408
- 最終噴火
- 不明
- テクトニクス環境
- Rift zone / Intermediate crust (15-25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Gada Ale (also known as Kebrit Ale), the most prominent volcano at the northern end of the Erta Ale Range, is formed of interstratified lava flows and hyaloclastites. Fumarolic activity is continuing, and the summit crater contains a small lake with hot mud. Like other Erta Ale Range volcanoes, Gada Ale is considered to be of Holocene age (Barberi and Varet, 1970). A fissure on the SE flank has produced spatter cones and a cinder cone; the latter fed lava flows that reach to Lake Bakili. The symmetrical Catherine tuff ring is located along this same SE trend west of Lake Bakili, and other tuff rings occur on the east side of the lake. A 2-km-wide salt dome to the west has uplifted lava flows as much as 100 m, and the structure of Gada Ale itself appears to be related to salt diapir uplift.
Wikipedia の要約
英語版の要約Gada Ale is a stratovolcano located in the Afar Region, Ethiopia. It is the most prominent volcano at the northern end of the Erta Ale Range.
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噴火履歴
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噴火記録はありません。
外部リンク
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