래밍턴산
Lamington
성층화산 · Papua New Guinea · 1680m

- 화산 유형
- 성층화산
- 국가
- Papua New Guinea
- 지역
- 남서태평양 / Trobriand Volcanic Province
- 해발
- 1680m
- 좌표
- -8.950, 148.150
- 마지막 분화
- 1956년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Lamington is an andesitic stratovolcano with a 1.3-km-wide breached summit crater containing a lava dome that rises above the coastal plain of the Papuan Peninsula of New Guinea north of the Owen Stanley Range. A summit complex of lava domes and crater remnants tops a low-angle base of volcaniclastic deposits dissected by radial valleys. A prominent broad "avalanche valley" extends northward from the breached crater. Ash layers from two early Holocene eruptions have been identified. In 1951 a powerful explosive eruption produced pyroclastic flows and surges that swept all sides of the volcano, killing nearly 3,000 people. The eruption concluded with growth of a 560-m-high lava dome in the summit crater.
Wikipedia 요약
영어 요약Mount Lamington is an andesitic stratovolcano in the Oro Province of Papua New Guinea. The forested peak of the volcano had not been recognised as such until its devastating eruption in 1951 that caused about 3,000 deaths.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 1951년VEI 4관측 기록1951-01-17 ~ 1956-07-02
- 기원전 4850년 (±300년)VEI ?지질학적 추정BCE 4850 ~ 진행 중
- 기원전 5980년 (±300년)VEI ?지질학적 추정BCE 5980 ~ 진행 중
외부 링크
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