Chiles-Cerro Negro
성층화산 · Colombia-Ecuador · 4698m
- 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 요약Cerro 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
상세 타임라인
- 1936년VEI 2관측 기록1936-07-17 ~ 진행 중Volcano Uncertain: possibly Reventador
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