ジェイムズ・ロス島
Mount Haddington Volcanic Field
楯状火山 · Antarctica · 1544m

- タイプ
- 楯状火山
- 国
- Antarctica
- 地域
- 南極・スコシア / Antarctic Peninsula Volcanic Province
- 標高
- 1544m
- 座標
- -64.150, -57.750
- 最終噴火
- 不明
- テクトニクス環境
- Intraplate / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The glacier-covered Mount Haddington shield volcano forms the high point of James Ross Island along the Larsen Rift near the northern tip of the Antarctic Peninsula. Effusive eruptions fed large lava deltas with basal hyalocalstite breccias overlain by subaerial lava flows. Well-preserved tuff cones and pyroclastic cones on the eastern flank below the summit icecap were considered to be only a few thousand years old (Smellie et al., 2008).
Wikipedia の要約
英語版の要約James Ross Island is a large island off the southeast side and near the northeastern extremity of the Antarctic Peninsula, from which it is separated by Prince Gustav Channel. Rising to 1,630 metres (5,350 ft), it is irregularly shaped and extends 40 nautical miles in a north–south direction.
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噴火履歴
詳細タイムライン
噴火記録はありません。
外部リンク
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