Simbo
성층화산 · Solomon Islands · 335m

- 화산 유형
- 성층화산
- 국가
- Solomon Islands
- 지역
- Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
- 해발
- 335m
- 좌표
- -8.292, 156.520
- 마지막 분화
- 1910년
- 판구조 환경
- Subduction zone / Crustal thickness unknown
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Simbo is a small island in the western Solomons with three truncated andesitic volcanic centers. The only Potassium-Argon date (2.3 +/- 1 million years ago from Mount Patukio) suggests a Pliocene-to-Pleistocene age for the island (Solomon Islands Geological Survey, 1982). The southern half of the island is thermally active. It contains fault-related fumarolic areas and hot springs near saltwater Lake Ove along the western coast and along the eastern coast near Mount Patukio, which has a steep-walled summit crater. Grover (1955) noted native accounts of the explosive enlargement of the Ngusunu explosion crater along the SW coast of the island one to two generations prior to 1955, probably after a visit by Guppy in 1882. Press reports mentioned an eruption in the early 1900s that forced the evacuation of villages beside Lake Ove, immediately adjacent to Ngusunu crater.
Wikipedia 요약
영어 요약Simbo is an island in Western Province, Solomon Islands. It was known to early Europeans as Eddystone Island. The islanders have their unique language spoken nowhere else.
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분화 이력
상세 타임라인
- 1910년 (±10년)VEI ?지질학적 추정1910 ~ 진행 중Ngusuna crater?
외부 링크
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