日光海山
Nikko
成層火山 · Japan · 392m (海底)

- タイプ
- 成層火山
- 国
- Japan
- 地域
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- 標高
- 392m (海底)
- 座標
- 23.078, 142.326
- 最終噴火
- 不明
- テクトニクス環境
- Subduction zone / Crustal thickness unknown
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Nikko submarine volcano is a massive seamount that rises from nearly 3 km depth to within 392 m of the ocean surface near the N end of the Mariana Volcanic Arc. Two large cones at the basaltic-to-andesitic volcano have been constructed on the NW and NE rims of a roughly 3-km-wide, flat-floored submarine caldera, whose rim is prominently displayed on the southern side, but largely buried on the north. A smaller cone is present on the SE caldera floor. The larger NW cone lies within a partially buried crater and displays hydrothermal activity. Discolored water was observed in July 1979, but none has been observed during semi-regular seasonal reconnaissance flights since then. Hydrothermal venting was documented during a NOAA expedition.
Wikipedia の要約
要約が短いです。詳細は記事全文をご覧ください。
日光海山(にっこうかいざん)は、硫黄島の南南東約210kmに位置する海底火山(海山)。別名、日光場。
Wikipedia · CC BY-SA · 記事全文を読む →
噴火履歴
詳細タイムライン
- 1979年VEI 0地質学的推定1979-07-12 ~ 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。