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Iriomote Submarine Volcano

Submarine Volcano NNE of Iriomotejima

성층화산 · Japan · 200m (해저)

A submarine volcano is located approximately 20 km offshore NNE of Iriomotejima, shown in this bathymetric map by the Japan Coast Guard. On 31 October 1924 an eruption produced a pumice raft that eventually reached Japan.
A submarine volcano is located approximately 20 km offshore NNE of Iriomotejima, shown in this bathymetric map by the Japan Coast Guard. On 31 October 1924 an eruption produced a pumice raft that eventually reached Japan. · 사진: Courtesy of Japan Coast Guard. · Wikimedia Commons
화산 유형
성층화산
국가
Japan
지역
Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
해발
200m (해저)
좌표
24.570, 123.930
마지막 분화
1924년
판구조 환경
Subduction zone / Oceanic crust (< 15 km)
화산 지형
Composite
주요 암석
Rhyolite
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.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1924~1924 · 1건 · 최고 VEI 419241924192519251925

상세 타임라인

  1. 1924년VEI 4관측 기록
    1924-10-31 ~ 진행 중

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