マシュー島
Matthew Island
成層火山 · France - claimed by Vanuatu · 177m
- タイプ
- 成層火山
- 国
- France - claimed by Vanuatu
- 地域
- Southwestern Pacific Volcanic Regions / Vanuatu Volcanic Arc
- 標高
- 177m
- 座標
- -22.330, 171.320
- 最終噴火
- 1956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
Matthew Island is composed of two low andesitic-to-dacitic cones separated by a narrow isthmus. The Matthew name originates from an English mariner who sighted the island in 1788. Only the triangular eastern portion of the 0.6 x 1.2 km island was present prior to the 1940s, when construction of the larger western segment began; it consists primarily of lava flows. The western cone contains a crater that is breached to the NW and is filled by a lava flow whose terminus forms the NW coast.
Wikipedia の要約
英語版の要約Matthew Island and Hunter Island are two uninhabited volcanic islands in the South Pacific, 300 kilometres (190 mi) east of New Caledonia and south-east of Vanuatu. The pair, which lie 70 km (43 mi) apart, are claimed by Vanuatu as part of Tafea Province, and considered by the people of Aneityum part of their custom ownership, but also claimed by France as part of New Caledonia.
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噴火履歴
詳細タイムライン
- 1976年VEI 1地質学的推定1976-11-27 ~ 進行中
- 1966年VEI ?地質学的推定1966-08-16 ~ 進行中
- 1963年VEI 0観測記録1963-09-11 ~ 1964-07-02Norfolk Island Ridge
- 1956年 (±2年)VEI 0観測記録1956-07-02 ~ 進行中West-Matthew
- 1954年VEI 2観測記録1954-10-16 ~ 進行中West-Matthew (October 1954, not 1953)
- 1949年VEI 2観測記録1949 ~ 進行中West-Matthew
- 1828年VEI ?地質学的推定1828-01 ~ 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。