러시아 · 성층화산
라이코케섬
Raikoke
- 화산 유형
- 성층화산
- 해발
- 551m
- 마지막 분화
- 2019년

- 화산 유형
- 성층화산
- 국가
- 러시아
- 지역
- 북서태평양 / Kuril Volcanic Arc
- 해발
- 551m
- 좌표
- 48.292, 153.250
- 마지막 분화
- 2019년
- 판구조 환경
- 섭입대 / 중간 지각 (15-25 km)
- 화산 지형
- 복성화산체
- 주요 암석
- 현무암 / 피크로현무암
지질학적 요약
A low truncated volcano forms the small barren Raikoke Island, which lies 16 km across the Golovnin Strait from Matua Island in the central Kuriles. The oval-shaped basaltic island is only 2 x 2.5 km wide and rises above a submarine terrace. An eruption in 1778, during which the upper third of the island was said to have been destroyed, prompted the first volcanological investigation in the Kuril Islands two years later. Incorrect reports of eruptions in 1777 and 1780 were due to misprints and errors in descriptions of the 1778 event (Gorshkov, 1970). Another powerful eruption in 1924 greatly deepened the crater and changed the outline of the island. Prior to a 2019 eruption, the steep-walled crater, highest on the SE side, was 700 m wide and 200 m deep. Lava flows mantle the eastern side of the island.
Wikipedia 요약
영어 요약Raikoke or Raykoke is an uninhabited volcanic island near the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, 16 kilometres (9.9 mi) distant from the island of Matua. Its name is derived from the Ainu language, from the Hokkaido Ainu word "hellmouth".
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
4건 기록용어집상세 타임라인
- 2019년VEI 3관측 기록2019-06-22 ~ 2019-07-01
- 1924년VEI 4관측 기록1924-02-14 ~ 1924-02-15
- 1778년VEI 4관측 기록1778 ~ 종료일 미상
- 1765년 (±5년)VEI 2관측 기록1765 ~ 종료일 미상
주변 화산
외부 링크
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