新島
Niijima
溶岩ドーム · Japan · 432m

- タイプ
- 溶岩ドーム
- 国
- Japan
- 地域
- 北西太平洋 / Izu Volcanic Arc
- 標高
- 432m
- 座標
- 34.397, 139.270
- 最終噴火
- 886年
- テクトニクス環境
- Subduction zone / Oceanic crust (< 15 km)
- 火山地形
- Minor (Silicic)
- 主要岩石
- Rhyolite
地質学的概要
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. The Mukaiyama complex on the south and the Atchiyama lava dome on the north were formed during eruptions in the 9th century CE, the last known activity. Shikineyama and Zinaito domes form small islands immediately to the SW and W, respectively, during earlier stages of volcanism. Earthquake swarms occurred during the 20th century.
Wikipedia の要約
英語版の要約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.
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噴火履歴
詳細タイムライン
- 886年VEI 4観測記録886-06-29 ~ 進行中Mukai-yama
- 856年VEI 2観測記録856 ~ 857Achi-yama
- 紀元前 1250年VEI ?地質学的推定BCE 1250 ~ 進行中
- 紀元前 4350年VEI ?地質学的推定BCE 4350 ~ 進行中Niijima-yama
- 紀元前 5950年VEI ?地質学的推定BCE 5950 ~ 進行中
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。