Pululagua
Pululahua
칼데라 · Ecuador · 3360m

- 화산 유형
- 칼데라
- 국가
- Ecuador
- 지역
- South America Volcanic Regions / Northern Andean Volcanic Arc
- 해발
- 3360m
- 좌표
- 0.046, -78.490
- 마지막 분화
- 290년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Caldera
- 주요 암석
- Dacite
지질학적 요약
Pululahua is a relatively low, forested volcano about 15 km N of Quito. The 5-km-wide summit caldera is narrowly breached to the west and partially filled by a group of dacitic lava domes. Pre-caldera lava domes of different ages are found outside the caldera to the E, SE, and S. Four post-caldera domes rise up to 450 m above the caldera floor. Large explosive eruptions producing pyroclastic flows took place during the late Pleistocene and Holocene. Caldera formation took place during a series of eruptions lasting 150-200 years beginning about 2,650 radiocarbon years ago. The latest dated eruption occurred from the post-caldera lava domes about 1,670 years ago and produced lava flows and pyroclastic flows.
Wikipedia 요약
영어 요약Pululahua is a dormant volcano in the north of Quito Canton, Pichincha Province, Ecuador. The volcano is in the Western Cordillera of the northern Ecuadorian Andes, approximately west-southwest of Mojanda and north of Casitahua volcanoes. Pululahua's caldera is approximately 5 km wide.The volcano is within an Ecuadorian national park known as Reserva Geobotánica Pululahua.
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분화 이력
상세 타임라인
- 290년VEI ?지질학적 추정290 ~ 진행 중
- 기원전 450년 (±150년)VEI 4지질학적 추정BCE 450 ~ 진행 중
- 기원전 690년 (±150년)VEI 5지질학적 추정BCE 690 ~ 진행 중
- 기원전 4800년VEI ?지질학적 추정BCE 4800 ~ 진행 중
외부 링크
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