Lolobau Island
Lolobau
칼데라 · Papua New Guinea · 878m
- 화산 유형
- 칼데라
- 국가
- Papua New Guinea
- 지역
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- 해발
- 878m
- 좌표
- -4.916, 151.162
- 마지막 분화
- 1912년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Caldera
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Lolobau volcano has grown over the W rim of a 6-km-wide caldera which formed about 12,000 years ago. The 8 x 13 km island is located just off the coast of eastern New Britain. A small lake occupies the SW part of the caldera. A small lava dome (Hulu) caps Mount Lolobau, which has a 0.8 x 1.1 km summit crater breached to the NE. Flank cones are found along the coast of the largely submerged volcano. Several vents within the caldera, on the E flank of the main edifice, have been active during historical time. The latest eruptions took place during the early 20th century.
Wikipedia 요약
영어 요약Lolobau Island is an island in the Bismarck Sea, within the West New Britain Province of the Islands Region, in northern Papua New Guinea.
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분화 이력
상세 타임라인
- 1911년VEI 4관측 기록1911 ~ 1912East flank (Sili)
- 1908년VEI ?지질학적 추정1908 ~ 진행 중
- 1904년VEI 4관측 기록1904-08-09 ~ 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100년 (±30년)VEI 4지질학적 추정1100 ~ 진행 중Hulu
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