Lolobau Island
Lolobau
カルデラ · Papua New Guinea · 878m
- タイプ
- カルデラ
- 国
- Papua New Guinea
- 地域
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- 標高
- 878m
- 座標
- -4.916, 151.162
- 最終噴火
- 1912年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Caldera
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Lolobau volcano has grown over the W rim of a 6-km-wide caldera which formed about 12,000 years ago. The 8 x 13 km island is located just off the coast of eastern New Britain. A small lake occupies the SW part of the caldera. A small lava dome (Hulu) caps Mount Lolobau, which has a 0.8 x 1.1 km summit crater breached to the NE. Flank cones are found along the coast of the largely submerged volcano. Several vents within the caldera, on the E flank of the main edifice, have been active during historical time. The latest eruptions took place during the early 20th century.
Wikipedia の要約
英語版の要約Lolobau Island is an island in the Bismarck Sea, within the West New Britain Province of the Islands Region, in northern Papua New Guinea.
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噴火履歴
詳細タイムライン
- 1911年VEI 4観測記録1911 ~ 1912East flank (Sili)
- 1908年VEI ?地質学的推定1908 ~ 進行中
- 1904年VEI 4観測記録1904-08-09 ~ 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100年 (±30年)VEI 4地質学的推定1100 ~ 進行中Hulu
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。