일본 · 성층화산
Iriomote Submarine Volcano
Submarine Volcano NNE of Iriomotejima
- 화산 유형
- 성층화산
- 해발
- 200m (해저)
- 마지막 분화
- 1924년

- 화산 유형
- 성층화산
- 국가
- 일본
- 지역
- 서태평양 / Ryukyu Volcanic Arc
- 해발
- 200m (해저)
- 좌표
- 24.570, 123.930
- 마지막 분화
- 1924년
- 판구조 환경
- 섭입대 / 해양 지각 (< 15 km)
- 화산 지형
- 복성화산체
- 주요 암석
- 유문암
지질학적 요약
The southernmost Ryukyu Islands volcano is a shallow submarine volcano 20 km NNE of Iriomotejima island and 35 km WSW of the northern tip of the island of Ishigakishima in an area with an estimated depth of 200-300 m. A major submarine eruption on 31 October 1924 produced rhyolitic pumice rafts with an estimated volume of about 1 km3 that were carried by currents along both coasts of Japan as far north as Hokkaido. The largest pumice blocks exceeded 1 x 2 m in size, and the volume of ejecta places this poorly known eruption among the largest recorded in Japan.
Wikipedia 요약
영어 요약The Iriomote submarine volcano is an active submarine volcano located 20 km (12 mi) north of Iriomote Island, Japan. The volcano is also known as the Submarine Volcano NNE of Iriomotejima. Its only reported eruption occurred on October 31, 1924—measuring a Volcanic explosivity index (VEI) of 5, it is one of the largest historical eruptions in Japan. However, scientific knowledge about the eruption is sparse.
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분화 이력
1건 기록용어집상세 타임라인
- 1924년VEI 4관측 기록1924-10-31 ~ 종료일 미상
주변 화산
외부 링크
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