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Mount Morning

Morning

Gunung api perisai · Antarctica · 2723 m

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. · Foto: Photo by U.S. Navy. · Wikimedia Commons
Tipe
Gunung api perisai
Negara
Antarctica
Wilayah
Antarctic-Scotia Volcanic Regions / McMurdo Volcanic Province
Ketinggian
2723 m
Koordinat
-78.500, 163.530
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Phonolite
Ringkasan geologi

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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