Japan · Lava dome
Kōzu-shima
Kozushima
- Type
- Lava dome
- Elevation
- 572m
- Last eruption
- 838

- Type
- Lava dome
- Country
- Japan
- Region
- Northwestern Pacific / Izu Volcanic Arc
- Elevation
- 572m
- Coordinates
- 34.219, 139.153
- Last eruption
- 838
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Rhyolite
Geological summary
A cluster of rhyolitic lava domes and associated pyroclastic deposits form the 4 x 6 km island of Kozushima in the northern Izu Islands.
Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →
From Wikipedia
Kōzu-shima (神津島) is a volcanic Japanese island in the Philippine Sea. The island is administered by Tōkyō and is located approximately 30 kilometres (19 mi) northwest of the Miyake-jima and 14 kilometres (8.7 mi) southwest of the Nii-jima. It is one of the Izu Seven Islands, a group of the seven northern islands of the Izu archipelago. Kōzushima is administratively part of Kōzushima Village, under Ōshima Subprefecture of Tokyo Metropolis. As of 2017, the island's population was 1,952. Kōzushima is within the boundaries of the Fuji-Hakone-Izu National Park.
Wikipedia · CC BY-SA · Read full article →
Eruption history
5 recordedGlossaryRecord summary
- Confirmed eruptions
- 4
- Uncertain eruptions
- 1
- Span of confirmed record
- 8050 BCE – 838
- Largest confirmed eruption
- VEI 4 (838)
- Confirmed eruptions since 1900
- 0
Detailed timeline
- 838VEI 4Observed838-08-02 – end unknownTenjo-san
- 832VEI ?Method not stated832 – end unknown
- 100 BCE (±950 yrs)VEI ?Geological estimate100 BCE – end unknownNW tip of island (Kobe-yama)
- 750 BCE (±700 yrs)VEI ?Geological estimate750 BCE – end unknownN tip of island (Anano-yama, Hanatabe)
- 8050 BCEVEI ?Geological estimate8050 BCE – end unknownJogo-yama
Nearby volcanoes
External links
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