春日海山
Kasuga 1
成層火山 · United States · 598m (海底)

- タイプ
- 成層火山
- 国
- United States
- 地域
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- 標高
- 598m (海底)
- 座標
- 21.765, 143.710
- 最終噴火
- 1959年
- テクトニクス環境
- Subduction zone / Crustal thickness unknown
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
Kasuga 1, the northernmost of three seamounts in the the Kasuga seamount chain SE of Fukujin, rises from a depth of 3,000 m to within about 600 m of the ocean surface. A series of flank vents are located low on the southern side of the edifice. The summit does not have a caldera or display hydrothermal activity, and is largely covered by volcaniclastics. Altered basaltic and andesitic rocks dredged from the summit suggest that it is the oldest of the three seamounts, although delicately preserved lava flow lobes and toes from a flank eruption suggest a very youthful age. It is listed as an active volcano by the Japan Meteorological Agency, and floating pumice attributed to a submarine eruption was seen south of it in the summer of 1959. Water discoloration from a possible submarine eruption was reported near the seamount in November 1975.
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。
春日海山(かすがかいざん)または春日場(かすがば)とは、マリアナ諸島の北方、北緯21度46分、東経143度43分にある海底火山である。
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噴火履歴
詳細タイムライン
- 1975年VEI 0地質学的推定1975-11-16 ~ 進行中21.78 N 143.71 E
- 1959年VEI 0観測記録1959-07-15 ~ 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。