Iriomote Submarine Volcano
Submarine Volcano NNE of Iriomotejima
Estratovolcán · Japan · 200 m (submarino)

- Tipo
- Estratovolcán
- País
- Japan
- Región
- Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
- Altitud
- 200 m (submarino)
- Coordenadas
- 24.570, 123.930
- Última erupción
- 1924
- Contexto tectónico
- Subduction zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Rhyolite
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 inglésThe 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
Línea de tiempo detallada
- 1924VEI 4Observado1924-10-31 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.