Reclus
화쇄구 · Chile · 1403m
- 화산 유형
- 화쇄구
- 국가
- Chile
- 지역
- South America Volcanic Regions / Austral Andean Volcanic Arc
- 해발
- 1403m
- 좌표
- -50.940, -73.580
- 마지막 분화
- 1908년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Dacite
지질학적 요약
Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present. Research has also revealed evidence for eruptions in the 19th and early 20th centuries.
Wikipedia 요약
영어 요약Reclus, also written as Reclús, is a cinder cone and stratovolcano located in the Southern Patagonian Ice Field, Chile. Part of the Austral Volcanic Zone of the Andes, its summit rises 1,000 metres (3,300 ft) above sea level and is capped by a crater about 1 kilometre (0.62 mi) wide. Close to the volcano lies the Amalia Glacier, which is actively eroding Reclus.
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분화 이력
상세 타임라인
- 1908년 (±1년)VEI 1관측 기록1908 ~ 진행 중
- 1879년VEI 2관측 기록1879 ~ 진행 중
- 1869년VEI 2관측 기록1869 ~ 진행 중
- 기원전 1830년VEI ?지질학적 추정BCE 1830 ~ 진행 중
외부 링크
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