Japan · Lava dome
Nii-jima
Niijima
- Type
- Lava dome
- Elevation
- 432m
- Last eruption
- 886

- Type
- Lava dome
- Country
- Japan
- Region
- Northwestern Pacific / Izu Volcanic Arc
- Elevation
- 432m
- Coordinates
- 34.397, 139.270
- Last eruption
- 886
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Minor (silicic)
- Major rock type
- Rhyolite
Geological summary
The elongated island of Niijima, SSW of Oshima, is 11 km long and only 2.5 km wide. Eight low rhyolitic lava domes are clustered in two groups at the northern and southern ends of the island, separated by an area of flat-topped domes and a low isthmus of pyroclastic deposits.
Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →
From Wikipedia
Nii-jima (新島) is a volcanic Japanese island administered by the Tokyo Metropolitan Government. It is one of the Izu Seven Islands, group of the seven northern islands of the Izu archipelago, and is located approximately 163 kilometres (101 mi) south of Tōkyō and 36 kilometres (22 mi) south of Shimoda Shizuoka Prefecture. The island is the larger inhabited component of the village of Niijima Village, Ōshima Subprefecture of Tokyo Metropolis, which also contains the neighboring island of Shikine-jima and the smaller, uninhabited Jinai-tō. Nii-jima is also within the boundaries of the Fuji-Hakone-Izu National Park.
Wikipedia · CC BY-SA · Read full article →
Eruption history
5 recordedGlossaryRecord summary
- Confirmed eruptions
- 5
- Uncertain eruptions
- 0
- Span of confirmed record
- 5950 BCE – 886
- Largest confirmed eruption
- VEI 4 (886)
- Confirmed eruptions since 1900
- 0
Detailed timeline
- 886VEI 4Observed886-06-29 – end unknownMukai-yama
- 856VEI 2Observed856 – 857Achi-yama
- 1250 BCEVEI ?Geological estimate1250 BCE – end unknown
- 4350 BCEVEI ?Geological estimate4350 BCE – end unknownNiijima-yama
- 5950 BCEVEI ?Geological estimate5950 BCE – end unknown
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.