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Morning

Vulcano a scudo · 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
Tipo
Vulcano a scudo
Paese
Antarctica
Regione
Antartide e Scotia / McMurdo Volcanic Province
Altitudine
2723 m
Coordinate
-78.500, 163.530
Ultima eruzione
Sconosciuto
Contesto tettonico
Intraplate / Continental crust (> 25 km)
Forma vulcanica
Shield
Roccia principale
Phonolite
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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.

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