Chiles-Cerro Negro
成層火山 · Colombia-Ecuador · 4698m
- タイプ
- 成層火山
- 国
- Colombia-Ecuador
- 地域
- South America Volcanic Regions / Northern Andean Volcanic Arc
- 標高
- 4698m
- 座標
- 0.817, -77.938
- 最終噴火
- 1936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
The Chiles-Cerro Negro volcanic complex includes both the Pleistocene Chiles and the Cerro Negro de Mayasquer stratovolcanoes astride the Colombia-Ecuador border. Cerro Negro has a caldera open to the west, with andesitic and dacitic lava flows of possible Holocene age (Hall 1992, pers. comm.) and solfataras on the shore of a small crater lake. An eruption reported in 1936 may have been from Reventador (Catalog of Active Volcanoes of the World). The higher, glacier-covered summit of Chiles, about 4 km ESE of Cerro Negro, last erupted about 160,000 years ago, but it has a caldera open to the north with hot springs and an active hydrothermal system on its eastern flank.
Wikipedia の要約
英語版の要約Cerro Negro de Mayasquer is a volcano on the border of Colombia and Ecuador. It lies 3 kilometres (2 mi) north-west of the volcano Chiles, and the two peaks are considered part of the same Chiles-Cerro Negro volcanic complex. These volcanoes, together with Cumbal are andesitic in rock type. A 1936 eruption reported by the Colombian government agency INGEOMINAS may have been from the Ecuadorean volcano Reventador, otherwise the volcano has not erupted for around 160,000 years.
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噴火履歴
詳細タイムライン
- 1936年VEI 2観測記録1936-07-17 ~ 進行中Volcano Uncertain: possibly Reventador
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。