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Chiles-Cerro Negro

成層火山 · Colombia-Ecuador · 4698m

Cerro Negro de Mayasquer (Ieft) and snow-capped Volcán Chiles (right), seen here from the south, are twin volcanoes that straddle the Colombia-Ecuador border.  Chiles volcano is of Pleistocene age, but has hot springs and an active hydrothermal system on its eastern flank.  Cerro Negro de Mayasquer is a stratovolcano with a caldera open to the west.  Andesitic and dacitic lava flows are of possible Holocene age.  Solfataras are found on the shore of a small crater lake.
Cerro Negro de Mayasquer (Ieft) and snow-capped Volcán Chiles (right), seen here from the south, are twin volcanoes that straddle the Colombia-Ecuador border. Chiles volcano is of Pleistocene age, but has hot springs and an active hydrothermal system on its eastern flank. Cerro Negro de Mayasquer is a stratovolcano with a caldera open to the west. Andesitic and dacitic lava flows are of possible Holocene age. Solfataras are found on the shore of a small crater lake. · 写真: Photo by Minard Hall, 1985 (Escuela Politécnica Nacional, Quito) · Wikimedia Commons
タイプ
成層火山
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

概要 (VEI時系列)
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1936~1936 · 1件 · 最大 VEI 219361936193719371937

詳細タイムライン

  1. 1936年VEI 2観測記録
    1936-07-17 ~ 進行中
    Volcano Uncertain: possibly Reventador

外部リンク

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