Reclus
火砕丘 · Chile · 1403m
- タイプ
- 火砕丘
- 国
- Chile
- 地域
- South America Volcanic Regions / Austral Andean Volcanic Arc
- 標高
- 1403m
- 座標
- -50.940, -73.580
- 最終噴火
- 1908年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Dacite
地質学的概要
Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present. Research has also revealed evidence for eruptions in the 19th and early 20th centuries.
Wikipedia の要約
英語版の要約Reclus, also written as Reclús, is a cinder cone and stratovolcano located in the Southern Patagonian Ice Field, Chile. Part of the Austral Volcanic Zone of the Andes, its summit rises 1,000 metres (3,300 ft) above sea level and is capped by a crater about 1 kilometre (0.62 mi) wide. Close to the volcano lies the Amalia Glacier, which is actively eroding Reclus.
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噴火履歴
詳細タイムライン
- 1908年 (±1年)VEI 1観測記録1908 ~ 進行中
- 1879年VEI 2観測記録1879 ~ 進行中
- 1869年VEI 2観測記録1869 ~ 進行中
- 紀元前 1830年VEI ?地質学的推定BCE 1830 ~ 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。