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Chiles-Cerro Negro

성층화산 · 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. · 사진: Photo by Minard Hall, 1985 (Escuela Politécnica Nacional, Quito) · Wikimedia Commons
화산 유형
성층화산
국가
Colombia-Ecuador
지역
South America Volcanic Regions / Northern Andean Volcanic Arc
해발
4698m
좌표
0.817, -77.938
마지막 분화
1936년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Dacite
지질학적 요약

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 요약

영어 요약

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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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1936~1936 · 1건 · 최고 VEI 219361936193719371937

상세 타임라인

  1. 1936년VEI 2관측 기록
    1936-07-17 ~ 진행 중
    Volcano Uncertain: possibly Reventador

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