Japan · Stratovolcano
Aogashima
- Type
- Stratovolcano
- Elevation
- 423m
- Last eruption
- 1785

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific / Izu Volcanic Arc
- Elevation
- 423m
- Coordinates
- 32.458, 139.759
- Last eruption
- 1785
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-basalt
Geological summary
The small 2.5 x 3.5 km dominantly basaltic island of Aogashima is surrounded by steep cliffs and contains a small 1.7 x 1.5-km-wide caldera.
Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →
From Wikipedia
Aogashima (青ヶ島) is a volcanic island to the south of Japan in northernmost Micronesia. It is the southernmost and most isolated inhabited island of the Izu Islands. The islands border the northeast Philippine Sea and lie north of the Ogasawara Islands. The island lies approximately 358 kilometres (222 mi) south of mainland Tokyo and 64 kilometres (40 mi) south of Hachijō-jima.
Wikipedia · CC BY-SA · Read full article →
Eruption history
7 recordedGlossaryRecord summary
- Confirmed eruptions
- 7
- Uncertain eruptions
- 0
- Span of confirmed record
- 1800 BCE (±100 yrs) – 1785
- Largest confirmed eruption
- VEI 4 (600 BCE)
- Confirmed eruptions since 1900
- 0
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
Detailed timeline
- 1780VEI 3Observed1780-07-27 – 1785-05Maru-yama, SW part of Ikenosawa crater
- 1670VEI 2Observed1670 – 1680Ikenosawa crater
- 1652VEI 3Observed1652 – end unknownIkenosawa crater
- 600 BCE (±200 yrs)VEI 4Geological estimate600 BCE – end unknownSE flank (Kintagaura)
- 1100 BCE (±300 yrs)VEI ?Geological estimate1100 BCE – end unknownNNW flank
- 1200 BCE (±50 yrs)VEI ?Geological estimate1200 BCE – end unknown
- 1800 BCE (±100 yrs)VEI 2Geological estimate1800 BCE – end unknownNorthwest flank
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.