バヌア・ウウー
Banua Wuhu
複成火山 · Indonesia · 5m (海底)

- タイプ
- 複成火山
- 国
- Indonesia
- 地域
- 西太平洋 / Sangihe Volcanic Arc
- 標高
- 5m (海底)
- 座標
- 3.146, 125.442
- 最終噴火
- 1919年
- テクトニクス環境
- Subduction zone / Oceanic crust (< 15 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
The submarine Banua Wuhu volcanic cone lies ~600 m off the western coast of Mahengatang Island, the emergent summit of a large submarine edifice, in the Sangihe Islands. Several ephemeral islands were constructed during the 19th and 20th centuries. An island 90 m high was formed in 1835, but had eroded to only a few rocks by 1848. Another island formed in 1889 was 50 m high in 1894. Five craters were reported during an eruption that built an island in 1904. An island that formed in 1919 had disappeared by 1935. Bathymetry shows shallow water over an area larger than Mahengatang Island towards the W (Haryanto, 2020). Satellite imagery frequently shows two sources of discolored water in the area, and it is a popular location for divers, who report sulfur odors and bubbling.
噴火履歴
詳細タイムライン
- 1968年VEI 0地質学的推定1968-09-05 ~ 1968-09-09
- 1918年VEI 3観測記録1918-07-18 ~ 1919-12-01
- 1904年VEI 2観測記録1904-04-17 ~ 1904-04-18
- 1904年VEI 2観測記録1904-08-27 ~ 進行中
- 1895年VEI 2観測記録1895-07-16 ~ 1895-12-26
- 1889年VEI 2観測記録1889-09-06 ~ 1889-09-09
- 1835年VEI 2観測記録1835-04-23 ~ 1835-04-26
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。