Submarine Volcano NNE of Iriomotejima
Stratovolcano in Japan
Key Facts
Elevation
-200 m (-656 ft)
Type
Stratovolcano
Location
24.570°, 123.930°
Region
Ryukyu Volcanic Arc
Rock Type
Rhyolite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
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.
Volcanic Hazards & Risk Assessment
Primary Hazards
- Pyroclastic flows
- Lava flows
- Volcanic bombs and ballistics
- Lahars and mudflows
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 102 years ago | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in Western Pacific Volcanic Regions
Quick Info
- •Smithsonian ID: 282010
- •Evidence: Eruption Observed
- •Epoch: Holocene
About the Photo
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.
Courtesy of Japan Coast Guard.
Authority Sources
Related Volcanoes
Basic Information
This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.