나이팅게일섬
Nightingale Island
성층화산 · United Kingdom · 365m

- 화산 유형
- 성층화산
- 국가
- United Kingdom
- 지역
- Atlantic Ocean Volcanic Regions / Southern Atlantic Volcano Group
- 해발
- 365m
- 좌표
- -37.420, -12.480
- 마지막 분화
- 2004년
- 판구조 환경
- Rift zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
Nightingale Island, along with the adjacent smaller Middle (or Alex) and Stoltenhoff Islands and associated small islets, are the southernmost of the Tristan da Cunha island group. The heavily eroded island consists of ash and agglomerate units with intervening massive trachytic intrusions and lava flows. Volcanic rocks were K-Ar dated at between 400,000 and 150,000 years, and a radiocarbon date of about 39,000 years BP was obtained from an ash layer overlain by a lava flow. An earthquake swarm lasting 6 hours beginning on 29 July 2004 was followed by observation of large blocks of floating phonolitic pumice that washed up on Tristan da Cunha. The pumice was considered to be from an eruption associated with an earthquake swarm 37-53 km SSE of Tristan da Cunha on the submarine SE flank of Nightingale Island.
Wikipedia 요약
나이팅게일섬(Nightingale Island)은 남대서양의 활화산섬으로, 면적은 3제곱킬로미터이며 트리스탄다쿠냐 제도의 일부이다. 영국이 세인트헬레나 어센션 트리스탄다쿠냐의 해외 영토의 일부로 관리하고 있다.
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분화 이력
상세 타임라인
- 2004년VEI 0관측 기록2004-07-29 ~ 2004-07-30Submarine SE flank
외부 링크
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