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일본 · 성층화산

Iriomote Submarine Volcano

Submarine Volcano NNE of Iriomotejima

화산 유형
성층화산
해발
200m (해저)
마지막 분화
1924년
Iriomote Submarine Volcano
사진: User Darwinek on en.wikipedia · Public domain · Wikimedia Commons
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 요약

The 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 기록용어집
요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다 · 화살표 키로 막대 이동, Enter로 열기
1924~1924 · 1건 · 최고 VEI 419241924192519251925

상세 타임라인

  1. 1924년VEI 4관측 기록
    1924-10-31 ~ 종료일 미상

주변 화산

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