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Buckle Island
成層火山 · Antarctica · 1239m

- タイプ
- 成層火山
- 国
- Antarctica
- 地域
- Antarctic-Scotia Volcanic Regions / Balleny Hotspot Volcano Group
- 標高
- 1239m
- 座標
- -66.780, 163.250
- 最終噴火
- 1899年
- テクトニクス環境
- Rift zone / Oceanic crust (< 15 km)
- 火山地形
- Composite
- 主要岩石
- Trachybasalt / Tephrite Basanite
地質学的概要
Buckle Island is in the center of a 160-km-long chain of volcanic islands forming the Balleny Islands off the coast of Antarctica's Victoria Land. The islands are located at the southern end of a submarine ridge system that extends north to New Zealand, but is offset by the Indian-Antarctic ridge system. The elongated, 21-km-long island is capped by an gently sloping icecap that descends steeply to the sea between rocky cliffs. Dark eruption columns were reported during 1839 and 1899, but no detailed geological studies exist for the Balleny Islands volcanoes.
Wikipedia の要約
英語版の要約Buckle Island is one of the three main islands in the uninhabited Balleny Islands group located in the Southern Ocean. It lies 25 km (16 mi) north-west of Sturge Island and 8 km (5 mi) south-east of Young Island, some 110 km (68 mi) north-north-east of Belousov Point on the Antarctic mainland.
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噴火履歴
詳細タイムライン
- 1899年VEI 2観測記録1899-01-12 ~ 進行中
- 1839年VEI 2観測記録1839-02-09 ~ 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。