Nikkō Seamount
Nikko
성층화산 · Japan · 392m (해저)

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- 해발
- 392m (해저)
- 좌표
- 23.078, 142.326
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Crustal thickness unknown
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Nikko submarine volcano is a massive seamount that rises from nearly 3 km depth to within 392 m of the ocean surface near the N end of the Mariana Volcanic Arc. Two large cones at the basaltic-to-andesitic volcano have been constructed on the NW and NE rims of a roughly 3-km-wide, flat-floored submarine caldera, whose rim is prominently displayed on the southern side, but largely buried on the north. A smaller cone is present on the SE caldera floor. The larger NW cone lies within a partially buried crater and displays hydrothermal activity. Discolored water was observed in July 1979, but none has been observed during semi-regular seasonal reconnaissance flights since then. Hydrothermal venting was documented during a NOAA expedition.
Wikipedia 요약
영어 요약Nikkō Seamount is a submarine volcano in the Volcano Islands region of Japan. It is the southernmost volcano of Japan.
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분화 이력
상세 타임라인
- 1979년VEI 0지질학적 추정1979-07-12 ~ 진행 중
외부 링크
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