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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.. Background Mount Morning is a glaciated, undissected alkalic shield volcano in the Erebus volcanic province located SE of the south end of the Royal Society Range. An elongated 4.9 x 4.1 km wide caldera lies at the 2723-m-high summit, and numerous parasitic lava domes and flank cinder cones formed on fissures on the north, NE, and SE flanks.

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Mount Morning is a shield volcano at the foot of the Transantarctic Mountains in Victoria Land, Antarctica. It lies 100 kilometres from Ross Island. Mount Morning rises to an elevation of 2,723 metres and is almost entirely mantled with snow and ice.. 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.