シンボ島
Simbo
成層火山 · Solomon Islands · 335m

- タイプ
- 成層火山
- 国
- Solomon Islands
- 地域
- Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
- 標高
- 335m
- 座標
- -8.292, 156.520
- 最終噴火
- 1910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
Simbo is a small island in the western Solomons with three truncated andesitic volcanic centers. The only Potassium-Argon date (2.3 +/- 1 million years ago from Mount Patukio) suggests a Pliocene-to-Pleistocene age for the island (Solomon Islands Geological Survey, 1982). The southern half of the island is thermally active. It contains fault-related fumarolic areas and hot springs near saltwater Lake Ove along the western coast and along the eastern coast near Mount Patukio, which has a steep-walled summit crater. Grover (1955) noted native accounts of the explosive enlargement of the Ngusunu explosion crater along the SW coast of the island one to two generations prior to 1955, probably after a visit by Guppy in 1882. Press reports mentioned an eruption in the early 1900s that forced the evacuation of villages beside Lake Ove, immediately adjacent to Ngusunu crater.
Wikipedia の要約
英語版の要約Simbo is an island in Western Province, Solomon Islands. It was known to early Europeans as Eddystone Island. The islanders have their unique language spoken nowhere else.
Wikipedia · CC BY-SA · 記事全文を読む →
噴火履歴
詳細タイムライン
- 1910年 (±10年)VEI ?地質学的推定1910 ~ 進行中Ngusuna crater?
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。