本文へスキップ
地図に戻る
比較

Mount Morning

Morning

楯状火山 · Antarctica · 2723m

Mount Morning is seen in this aerial view from the NE. The summit contains an ice-filled 4.1 x 4.9 km caldera. Numerous flank lava domes and scoria cones formed along fissures on Hurricane Ridge across the NE flank to the middle right, and on the Riviera Ridge beyond on the N flank.
Mount Morning is seen in this aerial view from the NE. The summit contains an ice-filled 4.1 x 4.9 km caldera. Numerous flank lava domes and scoria cones formed along fissures on Hurricane Ridge across the NE flank to the middle right, and on the Riviera Ridge beyond on the N flank. · 写真: Photo by U.S. Navy. · Wikimedia Commons
タイプ
楯状火山
Antarctica
地域
Antarctic-Scotia Volcanic Regions / 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.

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。