ペンギン島
Penguin Island
成層火山 · Antarctica · 180m
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- タイプ
- 成層火山
- 国
- Antarctica
- 地域
- 南極・スコシア / South Shetlands Volcanic Arc
- 標高
- 180m
- 座標
- -62.100, -57.930
- 最終噴火
- 1905年
- テクトニクス環境
- Intraplate / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The 1.4 x 1.7 km Penguin Island is located off the SE coast of King George Island in Antarctica's South Shetland Islands, west of the axis of the Bransfield Rift. The most prominent feature is Deacon Peak, a basaltic scoria cone with a 350-m-wide summit crater on the SW side of the island. A small plug of basaltic lava occupies the 75-m-deep crater. Petrel Crater, a 300-m-wide maar, is located near the east coast. The formation of Deacon Peak was dated by lichenometry at about 300 years ago, and the younger Petrel Crater maar was dated at about 100 years (Birkenmajer, 1979). Some reports of fumarolic activity on nearby Bridgeman Island are attributed to the more youthful Penguin Island.
Wikipedia の要約
英語版の要約Penguin Island is one of the smaller of the South Shetland Islands of Antarctica.
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噴火履歴
詳細タイムライン
- 1905年VEI ?地質学的推定1905-07-02 ~ 進行中NE flank (Petrel Crater)
- 1850年VEI ?観測記録1850-07-02 ~ 進行中Deacon Peak
- 1683年VEI ?地質学的推定1683 ~ 進行中Deacon Peak
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。