Antillanca Group
Antillanca Volcanic Complex
성층화산 · Chile · 1979m

- 화산 유형
- 성층화산
- 국가
- Chile
- 지역
- South America Volcanic Regions / Southern Andean Volcanic Arc
- 해발
- 1979m
- 좌표
- -40.783, -72.150
- 마지막 분화
- -230년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The Antillanca Volcanic Complex is a cluster of late-Pleistocene to Holocene basaltic-to-andesitic scoria cones, maars, and small stratovolcanoes covering an area of 380 km2 SE of Lago Puyehue and NE of Lago Rupanco. The most prominent edifice is the Holocene Casablanca stratovolcano, which has a truncated conical profile and produced major explosive eruptions about 2,910 and 2,260 radiocarbon years ago. Older late-Pleistocene stratovolcanoes, such as Sarnoso to the SW and Fiuchá to the NW, are extensively dissected by glaciers. Fissures oriented in four major directions influence the orientation of the cones. Thermal areas are found in scattered locations on the NW side of the complex.
Wikipedia 요약
영어 요약The Antillanca Group is a volcanic group of scoria cones, maars and small stratovolcanoes, in Chile. Casablanca stratovolcano is the tallest volcano of the group, which shelters the Antillanca ski resort on its west flank. Aguas Calientes and Puyehue Hot springs also form part of this volcanic group. The complex encompasses 380 km2 and to the west is bordered by the lakes Puyehue and Rupanco.
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분화 이력
상세 타임라인
- 기원전 230년 (±200년)VEI 5지질학적 추정BCE 230 ~ 진행 중Casablanca (Raihuén crater)
- 기원전 960년 (±150년)VEI 5지질학적 추정BCE 960 ~ 진행 중
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