Lithofacies and eruptive conditions of the southernmost volcanoes in the world (87° S)

• Published in: Bulletin of Volcanology
• Main Authors: Smellie, J. L., Panter, K. S.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2021
• Subjects: Geochemistry and Petrology; Antarctic; Sheridan Bluff; South Pole; Transantarctic Mountains; Antarc*; Ice Sheet; South pole
• Online Access: http://dx.doi.org/10.1007/s00445-021-01475-y; https://link.springer.com/content/pdf/10.1007/s00445-021-01475-y.pdf; https://link.springer.com/article/10.1007/s00445-021-01475-y/fulltext.html

Abstract Neogene volcanic centres are uncommon in the Transantarctic Mountains but at least three basaltic examples occur within 300 km of South Pole, above 2200 m asl and inland of the margin of the West Antarctic Rift System. They are the southernmost volcanoes on Earth and have yielded Early—mid Miocene isotopic ages. Two of the centres, at Mt Early and Sheridan Bluff, have been examined. The centre at Mt Early is unequivocally glaciovolcanic. It formed a tall monogenetic volcanic edifice at least 1 km high and > 1.5 km in diameter. It erupted under significantly thicker-than-modern ice, which was probably a fast-moving ice stream at the eruptive site and resulted in a distinctive constructive architecture and lithofacies. It is the first described example of a glaciovolcano erupted beneath an ice stream. The characteristics of the second centre at Sheridan Bluff indicate that it was also a monogenetic volcano but with a shield-like profile, originally c. 6 km in basal diameter but just c. 400 m high. It probably erupted in a substantial pluvial lake in an ice-poor or ice-free environment. The strongly contrasting eruptive settings now identified by the volcanic sequences at both centres examined testify to a highly dynamic Antarctic Ice Sheet during the Early—mid Miocene.