타후물코산
Tajumulco
성층화산 · Guatemala · 4203m

- 화산 유형
- 성층화산
- 국가
- Guatemala
- 지역
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- 해발
- 4203m
- 좌표
- 15.043, -91.903
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Dacite
지질학적 요약
Tajumulco is Guatemala's highest peak and the highest volcano in Central America. Two summits, one with a 50-70 m wide crater, lie along a NW-SE line. A lava flow from the ~4200-m-high NW summit traveled down a deep valley on the NW flank. The andesitic-dacitic volcano was constructed over the NW end of a large arcuate SW-facing escarpment of uncertain origin. Tajumulco has had several unconfirmed reports of historical eruptions. Sapper (1917) considered it to have erupted during historical time, but without accurate dates. The volcano was reported to eject many rocks, destroying houses on 24 October 1765, but this may have been a rock avalanche. Juarros reported some eruptions before 1808, and there are unlikely reports of eruptions in 1821 (or 1822), 1863, and 1893 (Incer 1988, unpublished manuscript).
Wikipedia 요약
영어 요약Volcán Tajumulco is a large stratovolcano in the department of San Marcos in western Guatemala. It is the highest mountain in Central America at 4,203 metres (13,789 ft). It is part of the mountain range of the Sierra Madre de Chiapas, which begins in Mexico's southernmost state of Chiapas.
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분화 이력
상세 타임라인
- 1863년VEI 2지질학적 추정1863 ~ 진행 중
- 1821년VEI 2지질학적 추정1821 ~ 진행 중
외부 링크
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