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Mount Morning

Morning

순상화산 · 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. · 사진: Photo by U.S. Navy. · Wikimedia Commons
화산 유형
순상화산
국가
Antarctica
지역
Antarctic-Scotia Volcanic Regions / McMurdo Volcanic Province
해발
2723m
좌표
-78.500, 163.530
마지막 분화
미확인
판구조 환경
Intraplate / Continental crust (> 25 km)
화산 지형
Shield
주요 암석
Phonolite
지질학적 요약

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.

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