Corcovado Volcano
Corcovado
成層火山 · Chile · 1826m

- タイプ
- 成層火山
- 国
- Chile
- 地域
- South America Volcanic Regions / Southern Andean Volcanic Arc
- 標高
- 1826m
- 座標
- -43.189, -72.794
- 最終噴火
- -4920年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
Little is known of this isolated volcano that was seen in eruption by Darwin in 1834, and an eruption was reported to have occurred in November 1835. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. A series of lakes flank the eastern side of the basaltic to basaltic andesite structure. Eruptions in historical time were considered likely from these postglacial volcanoes (Moreno 1985, pers. comm.).
Wikipedia の要約
英語版の要約Corcovado Volcano is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. The glacially eroded volcano is flanked by Holocene cinder cones. The volcano's base has likely prehistoric lava flows that are densely vegetated. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. At its foot lies a series of lakes. Corcovado dominates the landscape of the Gulf of Corcovado area and is visible from Chiloé Island, weather permitting.
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噴火履歴
詳細タイムライン
- 1835年VEI 2地質学的推定1835-11-11 ~ 進行中
- 1834年VEI 2地質学的推定1834-11 ~ 進行中
- 紀元前 4920年 (±100年)VEI ?地質学的推定BCE 4920 ~ 進行中
- 紀元前 6030年 (±100年)VEI ?地質学的推定BCE 6030 ~ 進行中
- 紀元前 6640年 (±770年)VEI ?地質学的推定BCE 6640 ~ 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。