Mount Morning
Morning
楯状火山 · Antarctica · 2723m

- タイプ
- 楯状火山
- 国
- Antarctica
- 地域
- 南極・スコシア / McMurdo Volcanic Province
- 標高
- 2723m
- 座標
- -78.500, 163.530
- 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
- Phonolite
地質学的概要
Mount Morning is a glaciated, undissected, alkalic shield volcano in the Erebus volcanic province SE of the south end of the Royal Society Range. An elongated 4.9 x 4.1 km caldera lies at the summit, and numerous lava domes and cinder cones formed on fissures on the N, NE, and SE flanks. The latest volcanism associated with growth of the phonolitic central volcano was Potassium-Argon dated at about 1.2 to 1 million years, and late-Pleistocene to zero-age Argon-Argon dates were obtained for some of the volumetrically dominant basanitic fissure vents. More than 50 morphologically youthful vents occur on the flanks.
Wikipedia の要約
英語版の要約Mount Morning is a shield volcano at the foot of the Transantarctic Mountains in Victoria Land, Antarctica. It lies 100 kilometres (62 mi) from Ross Island. Mount Morning rises to an elevation of 2,723 metres (8,934 ft) and is almost entirely mantled with snow and ice. A 4.1-by-4.9-kilometre-wide summit caldera lies at the top of the volcano, and several ice-free ridges such as Hurricane Ridge and Riviera Ridge emanate from the summit. A number of parasitic vents mainly in the form of cinder cones dot the mountain.
Wikipedia · CC BY-SA · 記事全文を読む →
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
⚠ 参考情報です。緊急対応には使用しないでください。