Gunung berapi bawah laut Iriomote
Submarine Volcano NNE of Iriomotejima
Stratovolkan · Japan · 200 m (bawah laut)

- Tipe
- Stratovolkan
- Negara
- Japan
- Wilayah
- Pasifik Barat / Ryukyu Volcanic Arc
- Ketinggian
- 200 m (bawah laut)
- Koordinat
- 24.570, 123.930
- Letusan terakhir
- 1924
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Rhyolite
Ringkasan geologi
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.
Riwayat letusan
Ringkasan (VEI dari waktu ke waktu)
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Garis waktu rinci
- 1924VEI 4Teramati1924-10-31 – Berlangsung
Tautan eksternal
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