부베섬
Bouvet
순상화산 · Norway · 741m

- 화산 유형
- 순상화산
- 국가
- Norway
- 지역
- 대서양 / Southern Atlantic Volcano Group
- 해발
- 741m
- 좌표
- -54.408, 3.351
- 마지막 분화
- -50년
- 판구조 환경
- Rift zone / Oceanic crust (< 15 km)
- 화산 지형
- Shield
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The solitary ice-covered shield volcano of Bouvet Island is located just off the Southwest Indian Ridge, east of the triple junction between the African, South American, and Antarctic plates. This basaltic-to-rhyolitic island, also referred to as Bouvetoya, was discovered by and later named for Captain Lozier-Bouvet during his 1739 search for the "great southern continent." About 95% of the uninhabited 10-km-wide island is covered by glaciers. The most prominent feature is the 3.5-km-wide Wilhelmplataet caldera, which is breached to the sea on the NW side. A late-stage rhyolitic lava dome forms the Cape Valdivia peninsula on the N flank. A paleomagnetic investigation was made by Lovlie and Furnes (1978) of a massive basaltic lava flow unit at Cape Meteor; based on oriented drill cores they tentatively inferred a minimum age of 2000 years.
Wikipedia 요약
영어 요약Bouvet Island is an uninhabited subantarctic volcanic island and dependency of Norway. A protected nature reserve situated in the South Atlantic Ocean at the southern end of the Mid-Atlantic Ridge, it is the world's most remote island. Located north of 60°S latitude, Bouvet Island is not part of the southern region covered by the Antarctic Treaty System.
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분화 이력
상세 타임라인
- 기원전 50년VEI 0지질학적 추정BCE 50 ~ 진행 중
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