The Pleiades (volcano group)

The Pleiades are located at the crest of the Transantarctic Mountains,[3] 120 to 140 km (75 to 87 mi)[4][5] away from the coast of Lady Newnes Bay, Ross Sea.[6] The volcanoes are located between Evans Neve and the beginning of Mariner Glacier,[5] which drains Evans Neve[7] southeastwards towards the Ross Sea.[6] The volcanic group is named after the Pleiades star cluster in the constellation Taurus; the name was assigned to them by the New Zealand Geological Survey Antarctic Expedition.[8]

The volcanic group is formed by several steep,[9] small volcanic cones and lava domes that emerge from the ice of Evans Neve[10] over a 13 km (8.1 mi) long area. Most are nameless with the exception of the central Taygete Cone, Alcyone Cone just south of Taygete and the pair of c. 3,020 m (9,910 ft) high Mount Pleiones and c. 3,040 m (9,970 ft) high Mount Atlas in the southern sector.[11] Mount Atlas and Mount Pleiones form a compound stratovolcano[12] which is the principal volcano of The Pleiades.[3] Mount Atlas is formed by three separate cones that rise 0.5 km (0.31 mi) above the ice. Dykes, lava and scoria flows are found on these cones, the youngest of which has a semicircular crater.[13] and scoria cones dot its flanks.[10] At the foot of Mount Atlas are moraines with the form of ridges[13] and there are moraines within one of its craters as well.[14] The summit of Mount Pleiones features nested craters.[15]

Alcyone Cone lies 3.5 km (2.2 mi) north of Mount Atlas.[5] It is only slightly lower than Mount Atlas but is much smaller. It has two poorly defined craters and consists of lava flows covered with scree and volcanic bombs when not buried under snow.[13] Taygete Cone 6 km (3.7 mi) north of Mount Atlas[5] appears to be a lava dome bearing traces of hydrothermal alteration and of a small crater.[13] Apart from the lava flows which make up most of Mount Atlas,[16] pyroclastic rocks have been encountered at The Pleiades.[3] The other cones are partly buried by snow and some have breached or otherwise eroded craters.[17]

The volcanoes have alternatively been described as eroded[16] or uneroded.[3] The young appearance of the edifices indicates a young age of The Pleiades volcanoes.[3] The volcanoes have been prospected for the possibility to generate geothermal energy but the presence of a good heat source is unlikely.[18] An aeromagnetic anomaly has been correlated to the volcano group.[19] The cones form an arcuate alignment that might reflect the existence of a 6 kilometres (3.7 mi) wide caldera to their southeast.[20]

The Pleiades belong to the McMurdo Volcanic Group and more specifically to the Melbourne volcanic province, which extends from Mount Melbourne to The Pleiades and Malta Plateau.[3] These consist of the Cenozoic volcanoes of northern Victoria Land which form alignments and lineaments possibly controlled by deep fractures, and which are subdivided into a "Central Suite" consisting of large stratovolcanoes and a "Local Suite" consisting of other volcanic centres. Among the volcanoes of the McMurdo Volcanic Group are the large volcanoes Mount Overlord, Mount Melbourne[4] and in the area of The Pleiades the Malta Plateau.[9] Volcanic activity began about 10 – 7 million years ago.[21] Earlier volcanic activity began during the Cretaceous, when the West Antarctic Rift System became active.[22]

The basement underneath the volcanoes consists of Precambrian and Paleozoic sedimentary and intrusive rocks. The former are mostly represented by the Bowers Group/Bowers Supergroup and the Robertson Bay Group north of the volcanic complex and the latter by the Granite Harbour and Admiralty Intrusives mostly south of the volcanic complex. A major local fault system passes northeast of the volcanoes[6][23] and roughly follows the path of the Mariner Glacier,[23] while the Lanternman Fault passes southwest of them.[22] Some of these faults formed during the Ross Orogeny, when three terranes collided to form northern Victoria Land;[24] The Pleiades are located on the Bowers Terrane.[22] Faults may also govern the position of The Pleiades volcanoes.[25]

The oldest dated rocks are 847,000 ± 12,000 years old.[30] Eruptions took place about 825,000 years ago and emplaced trachytes in the central part of the field; even older eruptions may have occurred but are now buried underneath of snow and ice. Three more eruptions occurred in the subsequent 700,000 years before activity began to increase after 100,000 years.[31] Potassium-argon dating has yielded imprecise ages of 40,000 ± 50,000 for Mount Atlas and 20,000 ± 40,000 and 12,000 ± 40,000 for other volcanic cones.[11] Later argon-argon dating has yielded ages of less than 100,000 years for lavas on Mount Atlas[31] and for a lava east of Taygete, and ages of about 45,000 years for Alcyone and two more lava flows on Mount Atlas.[32] The Pleiones-Atlas complex may have last erupted 20,000 ± 7,000 years ago.[33]

Tephra deposits have been found in Antarctica which may originate at The Pleiades. These include:

• Eemian-age tephras in Taylor Glacier[34] and Talos Dome, although some of the latter may originate at Mount Rittmann instead.[35]
• One tephra layer emplaced about 50,000 years ago at a blue-ice area at Frontier Mountain.[36]
• Several tens of thousands of years old tephra layers at Lewis Cliff/Beardmore Glacier probably originate at The Pleiades.[37]
• 26,000 – 22,000 years old tephra in the Ross Sea, which was emplaced when part of the Ross Sea was ice-free.[38]
• 16,000 – 15,000 years old tephra layers in Talos Dome.[39]
• Tephra layers at Hercules Neve and Talos Dome, of probably Holocene age.[40]
• A volcanic glass layer at Siple Dome dated to 1286 – 1292 AD.[41] A tephra layer from 1254 AD was later correlated to Mount Rittmann.[42]
• Tephras in ice cores that date to 1776 – 1885 AD,[43] including one tephra layer at Siple Dome dated to about 1809.[44]
• Finally, a major eruption may have occurred either at The Pleiades or at Mount Melbourne between 1880–1980.[45]

The youngest ages of 6,000 ± 6,000[32] and 3,000 ± 14,000 years ago have been obtained on Taygete,[11] which together with the youthful texture of this dome[12] indicates a young age for The Pleiades, despite the imprecise dates.[13] The presence of pumice lapilli has been taken as evidence of very recent activity in the form of a moderate pumice eruption.[46] Presently, only minor fumarolic activity has been reported.[45] Future eruptions are possible[32] and The Pleiades are not monitored, but they are also remote from any research station.[47]

• List of volcanoes in Antarctica

• Esser, R.P.; Kyle, Philip (January 2002). "⁴⁰Ar/³⁹Ar chronology of the McMurdo Volcanic Group at The Pleiades, northern Victoria Land, Antarctica". Royal Society of New Zealand Bulletin. 35: 415–418. ISSN 1176-1865 – via ResearchGate.
• Faure, Gunter; Mensing, Teresa M. (2011). The Transantarctic Mountains. Dordrecht: Springer Netherlands. doi:10.1007/978-90-481-9390-5. ISBN 978-1-4020-8406-5.
• Kim, Jihyuk; Park, Jung-Woo; Lee, Mi Jung; Lee, Jong Ik; Kyle, Philip R. (2019-01-01). "Evolution of Alkalic Magma Systems: Insight from Coeval Evolution of Sodic and Potassic Fractionation Lineages at The Pleiades Volcanic Complex, Antarctica". Journal of Petrology. 60 (1): 117–150. Bibcode:2019JPet...60..117K. doi:10.1093/petrology/egy108. ISSN 0022-3530. S2CID 134730691.
• Kyle, Philip (January 1982). "Volcanic geology of the Pleiades, northern Victoria Land, Antarctica". In Craddock, C. (ed.). Antarctic Geoscience. Madison, WI: University of Wisconsin Press. pp. 747–754. ISBN 9780299084103 – via ResearchGate.
• Lee, Mi Jung; Kyle, Philip R.; Iverson, Nels A.; Lee, Jong Ik; Han, Yeongcheol (2019-09-01). "Rittmann volcano, Antarctica as the source of a widespread 1252 ± 2 CE tephra layer in Antarctica ice". Earth and Planetary Science Letters. 521: 169–176. Bibcode:2019E&PSL.521..169L. doi:10.1016/j.epsl.2019.06.002. ISSN 0012-821X. S2CID 198411649.
• LeMasurier, W.E.; Thomson, J.W.; Baker, P.E.; Kyle, P.R.; Rowley, P.D.; Smellie, J.L.; Verwoerd, W.J., eds. (1990). Volcanoes of the Antarctic Plate and Southern Oceans. Antarctic Research Series. Vol. 48. Washington, D. C.: American Geophysical Union. doi:10.1029/ar048. ISBN 978-0-87590-172-5.
• Riddolls, B. W.; Hancox, G. T. (1 November 1968). "The geology of the upper Mariner Glacier region, North Victoria Land, Antarctica". New Zealand Journal of Geology and Geophysics. 11 (4): 881–899. doi:10.1080/00288306.1968.10420758. ISSN 0028-8306.
• Smellie, John L.; Rocchi, Sergio (2021). "Chapter 5.1a Northern Victoria Land: volcanology". Geological Society, London, Memoirs. 55 (1): 347–381. doi:10.1144/M55-2018-60. ISSN 0435-4052. S2CID 233887403.
• Stump, Edmund, ed. (1986). Geological Investigations in Northern Victoria Land. Antarctic Research Series. Vol. 46. Washington, D. C.: American Geophysical Union. doi:10.1029/ar046. ISBN 978-0-87590-197-8.