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Japón · Estratovolcán

Iriomote Submarine Volcano

Submarine Volcano NNE of Iriomotejima

Tipo
Estratovolcán
Altitud
200 m (submarino)
Última erupción
1924
Iriomote Submarine Volcano
Foto: User Darwinek on en.wikipedia · Public domain · Wikimedia Commons
Tipo
Estratovolcán
País
Japón
Región
Pacífico Occidental / Ryukyu Volcanic Arc
Altitud
200 m (submarino)
Coordenadas
24.570, 123.930
Última erupción
1924
Contexto tectónico
Zona de subducción / Corteza oceánica (< 15 km)
Forma volcánica
Compuesto
Roca principal
Riolita
Resumen geológico

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.

Resumen de Wikipedia

Resumen en inglés

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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Historial de erupciones

1 registradasGlosario
Resumen (VEI en el tiempo)
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1924~1924 · 1 erupciones · VEI máx. 419241924192519251925

Línea de tiempo detallada

  1. 1924VEI 4Observado
    1924-10-31 – fin desconocido

Volcanes cercanos

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.