Sumaco
成層火山 · Ecuador · 3990m
- タイプ
- 成層火山
- 国
- Ecuador
- 地域
- South America Volcanic Regions / Northern Andean Volcanic Arc
- 標高
- 3990m
- 座標
- -0.538, -77.626
- 最終噴火
- 1895年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Trachybasalt / Tephrite Basanite
地質学的概要
The forested Sumaco stratovolcano rises above the jungles of the western Amazon basin, east of Antisana volcano, and occupies an isolated position far to the east of the main Andes volcanic axis. Constructed over Cretaceous sedimentary rocks, it forms a relatively symmetrical cone in an area of heavy rainfall and erosion. Sumaco has produced alkaline tephritic, basanitic, and phonolitic rocks distinct from those of the main Andean chain. The volcano has a broad summit crater, 300 x 400 m wide, containing a central cone. Reports of historical eruptions are somewhat ambiguous; an eruption is inferred in the 18th or early-19th century on the basis of changes in crater morphology.
Wikipedia の要約
英語版の要約Sumaco is a symmetrical, isolated stratovolcano, that is set off from the main Ecuador volcanic axis. Its rocks are very distinct from those from most Andean volcanoes because of its lack of andesitic composition, in favour of basanite and phonolitic rock. Sumaco is heavily forested and contains a small cone in its broad summit crater. An historical eruption occurred around 1895.
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噴火履歴
詳細タイムライン
- 1933年VEI 2地質学的推定1933-02 ~ 進行中
- 1895年 (±30年)VEI 2観測記録1895 ~ 進行中
- 1650年 (±50年)VEI 3地質学的推定1650 ~ 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。