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Almolonga

성층화산 · Guatemala · 3173m

The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818.
The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818. · 사진: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
화산 유형
성층화산
국가
Guatemala
지역
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
해발
3173m
좌표
14.797, -91.519
마지막 분화
1818년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Dacite
지질학적 요약

Volcán de Almolonga is an andesitic stratovolcano with a 3.3-km-wide late-Pleistocene central caldera that is located along the Zunil fault zone. The caldera is surrounded by a ring-dike configuration of dacitic and rhyolitic lava domes. The youngest and only historically active dome complex is Cerro Quemado (whose name means Burned Peak), located immediately south of Guatemala's second largest city, Quezaltenango. About 1200 radiocarbon years ago, part of the andesitic-to-dacitic Cerro Quemado dome collapsed, producing a debris avalanche and an associated lateral explosion that swept across the valley to the west as far as the flanks of Siete Orejas volcano. The latest eruption in 1818 produced a blocky 2.5-km-long lava flow. Hot springs are located on the northern and eastern flanks of Cerro Quemado, and the Zuníl geothermal field, the site of a geothermal exploration project, lies on the SE flank of Cerro Quemado.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
800~902 · 1건 · 최고 VEI 31716~1818 · 2건 · 최고 VEI 28001004130915131716

상세 타임라인

  1. 1818년VEI 2관측 기록
    1818-01-16 ~ 1818-06-19
    East flank of Cerro Quemado
  2. 1765년VEI 2관측 기록
    1765-10-24 ~ 1765-10-25
    Cerro Quemado
  3. 800년 (±50년)VEI 3지질학적 추정
    800 ~ 진행 중
    Cerro Quemado

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