Gaussberg

Gaussberg
Gaussberg in 1912
Highest point
Elevation373 m (1,224 ft)[1]
ListingList of volcanoes in Antarctica
Coordinates66°48′S 089°11′E / 66.800°S 89.183°E / -66.800; 89.183[2]
Geography
Gaussberg is located in Antarctica
Gaussberg
Gaussberg
Geology
Mountain typeVolcanic cone

Gaussberg (or Schwarzen Berg,[3] Mount Gauss) is an extinct, 370-metre-high (1,210-foot) high volcanic cone in East Antarctica fronting on Davis Sea immediately west of Posadowsky Glacier. It is ice-free and conical in nature, having formed subglacially about 55,000 years ago. The current edifice is thought to be the remains of a once-larger mountain that has been reduced by glacial and subaerial erosion. The volcano has produced lamproite magmas, and is the youngest volcano to have produced such magmas on Earth.

Research history

Discovered in February 1902 by the German Antarctic Expedition under Erich von Drygalski, who named it after his expedition ship[2] which in 1902 remained stuck in ice for a year.[4] The ship in turn was named in honour of the German mathematician Carl Friedrich Gauss.[2] Drygalski observed the volcano with the help of a tethered balloon.[5]

Owing to its peculiar composition, Gaussberg has been intensively researched.[6] The mountain was investigated in 1912 by the 1911-1914 Australasian Antarctic Expedition, by the Soviet Antarctic Expedition in 1956–1957,[4] by Australian expeditions in 1977, 1981,[7] 1987[8] and by an expedition linked to an entity "K.D.C" in 1997.[9] Regional krill stocks in turn were named after the mountain.[10] Owing to its peculiar composition and isolated location, the volcano has an importance out of proportion to its actual size.[11] The mineral gaussbergite is named after the volcano.[12]

Geography and geomorphology

The volcano lies in Kaiser Wilhelm II Land, Antarctica,[4] close to the West Ice Shelf and between the Australian Davis Station and Russian Mirny Station.[13] It lies on the Davis Sea immediately west of Posadowsky Glacier.[2] Gaussberg is within the Antarctic territory claimed by Australia,[14] and the only ice-free outcrop between Mirny Station and the Vestfold Hills.[15]

German map of Gaussberg

It consists of a 370-metre-high (1,210-foot), 1.5-kilometre-wide (0.93-mile)[1] cone located between the East Antarctic Ice Sheet on three sides and the sea on the fourth.[16] It is the only exposure of rock in the region,[16][17] with rocky outcrops at the summit and on the northern flank.[18] The edifice covers an area of about 10 square kilometres (3.9 sq mi)[19] and has a volume of 1 cubic kilometre (0.24 cu mi).[19] Most of the edifice is made out of pillow lavas with radii of 0.5–2 metres (1 ft 8 in – 6 ft 7 in) and 3–5 centimetres (1.2–2.0 in) thick crusts. The volcano is covered with lava fragments resembling lapilli which may have formed through erosion. Gaussberg has no volcanic crater,[4] rather having a ridge at the summit. The volcano has several terraces of undetermined origin[16] and may have formed as a shield volcano with multiple vents.[11] The rocks were probably emplaced subglacially, although the occurrence of pahoehoe lava is possible.[20] There are moraines on the southern, northwestern and northeastern foot of the volcano,[18] and erratic blocks and glacial striations are evidence that the volcano was formerly glaciated.[21]

Geology

Gaussberg is an extremely isolated volcano[22] although an ice rise a few kilometres southwest of Gaussberg[23] and aeromagnetic surveys suggest that within 30 kilometres (19 mi) there are other small volcanoes in the area.[11] It is the only Antarctic volcano situated on the Antarctic Shield, where the thickest crust of Antarctica is found.[24] Why it formed about 50,000 years ago on a stable continental margin is unclear; either a mantle plume, an instability of the East Antarctic continent[25][26][27] or lateral flow of mantle plume material are possible.[28] The basement underneath Gaussberg is formed by gneisses of Archean to Proterozoic age.[19] The lithosphere under Gaussberg is over 150 kilometres (93 mi) thick[26] and has an unusually high heat flow.[29]

Its activity has been related to the Kerguelen Plateau, but the Kerguelen volcanoes have yielded different magma compositions and there is no major geological structure linking the two other than the so-called "Kerguelen-Gaussberg Ridge",[22] thus a connection between the two is unproven.[17] A graben system in the region, which may have formed in Gondwana and may be correlated to tectonic structures on the Indian Peninsula, has been christened the "Gaussberg Rift";[30] the volcano rises on a horst on the rift but its relation to the rift is unclear.[31] Finally, the 90° E Fault that separates regional tectonic structures may have influenced volcanism at Gaussberg.[32]

Composition

The volcano has a uniform chemical composition[33] consisting of lamproite (originally identified as leucitite),[34] which defines a potassium-rich mafic rock suite.[4] The rocks are almost free of visible crystals[22] but contain numerous vesicles. Phenocrysts include clinopyroxene, leucite and olivine,[9] the latter containing spinel inclusions.[35] The Gaussberg suite is the youngest lamproite known on Earth.[36] The rocks are rich in volatiles[37] including carbon dioxide and water.[38] There are xenoliths, mostly granites coming from the Precambrian basement,[4] and zircons recovered from the rocks are up to several billion years old.[15] Palagonite,[4] salt[39] and native sulfur deposits have been found.[22]

The source of the Gaussberg lamproites is unclear, as the processes usually proposed for the formation of such magmas do not easily apply to the Gaussberg rocks.[40] The magma may have formed through the incomplete melting of phlogopite-rich mantle and further chemical processes such as crystal fractionation that raised the potassium/aluminium ratio above 1.[41] Deep mantle structures that formed through subduction billions of years ago and remained isolated since then have been proposed as the source of Gaussberg lamproites.[40] The Kerguelen plume may[42] or may not have played a role.[11]

Eruption history

Drastically different age estimates have been obtained on Gaussberg. Early research suggested a Pliocene or Miocene age based on a presumed history of the Antarctic Ice Sheet and comparisons between the appearance of Gaussberg with Kerguelen volcanoes.[33] Potassium-argon dating has yielded ages of 20 and 9 million years,[22] with younger dating efforts producing an age of 56,000±5,000 years.[43] Fission track dating produced ages of 25,000±12,000 years and geomorphologic considerations support a late Pleistocene age.[22] These disagreements between potassium-argon dating and other dating methods may indicate either contamination with older rocks or the presence of non-outgassed argon.[33] The 56,000±5,000 years age is considered to be more probable than the 20 and 9 million years ones.[44]

Gaussberg was probably constructed in a single eruptive episode[45] but there is evidence that the present-day edifice formed on an older, eroded volcano.[36] Gaussberg formed under much thicker ice than there is today in the area, and the ice deposited moraines on its summit.[22] There are different views on how erosion affected Gaussberg; some think that it was largely spared[46] and others that erosion wore down the initially much larger edifice to its current size;[47][9] the latter theory is the preferred view of the Global Volcanism Program[48] and is supported by aeromagnetic data which suggest an initial size of 10 kilometres (6.2 mi).[11] Dust layers in the Siple Dome ice core may come from wind-driven erosion of Gaussberg rocks.[49]

Biology

Several moss species were identified at Gaussberg,[50] as well as a protozoan fauna[51] such as rotifers inhabiting them.[52] Nematodes[53] and tardigrades have been found at Gaussberg.[54] It was the first place on the Antarctic mainland where lichens were reported.[50] Emperor penguin rookeries occur at the mountain[55] and snow petrels were observed to breed there,[56] but overall there is not much fauna at Gaussberg.[57]

See also

References

  1. ^ a b Mitchell & Bergman 1991, p. 131.
  2. ^ a b c d "Gaussberg". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2009-05-03.
  3. ^ Glaubrecht, Matthias; Maitas, Lothar; v. Salvini-Plawen, Luitfried (September 2005). "Aplacophoran Mollusca in the Natural History Museum Berlin. An annotated catalogue of Thiele's type specimens, with a brief review of "Aplacophora" classification". Mitteilungen aus dem Museum für Naturkunde in Berlin - Zoologische Reihe. 81 (2): 153. doi:10.1002/mmnz.200510009. ISSN 1435-1935.
  4. ^ a b c d e f g Sheraton & Cundari 1980, p. 417.
  5. ^ Doake, C. S. M. (23 April 1987). Antarctic Science. CUP Archive. p. 18. ISBN 978-0-521-26233-0.
  6. ^ LeMasurier et al. 1990, p. xviii.
  7. ^ LeMasurier et al. 1990, p. 448.
  8. ^ Migdisova et al. 2023, p. 913.
  9. ^ a b c Murphy 2002, p. 982.
  10. ^ Wright, Minturn T. (1987). "The Ownership of Antarctica, Its Living and Mineral Resources". Journal of Law and the Environment. 4 (2): 63 – via HeinOnline.
  11. ^ a b c d e Smellie, John L. (1 January 2021). "Chapter 1.2 Antarctic volcanism: volcanology and palaeoenvironmental overview". Geological Society, London, Memoirs. 55 (1): 33. doi:10.1144/M55-2020-1. ISSN 0435-4052. S2CID 234287036.
  12. ^ Aodha, Breandán S. Mac (1 June 1989). "Mineral Names from Toponyms". Names. 37 (1): 10. doi:10.1179/nam.1989.37.1.19. ISSN 0027-7738.
  13. ^ Tingey, McDougall & Gleadow 1983, p. 242.
  14. ^ Salvioli-Mariani, Toscani & Bersani 2004, p. 83.
  15. ^ a b Mikhalsky, E. V.; Belyatsky, B. V.; Presnyakov, S. L.; Skublov, S. G.; Kovach, V. P.; Rodionov, N. V.; Antonov, A. V.; Saltykova, A. K.; Sergeev, S. A. (1 March 2015). "The geological composition of the hidden Wilhelm II Land in East Antarctica: SHRIMP zircon, Nd isotopic and geochemical studies with implications for Proterozoic supercontinent reconstructions". Precambrian Research. 258: 180. Bibcode:2015PreR..258..171M. doi:10.1016/j.precamres.2014.12.011. ISSN 0301-9268.
  16. ^ a b c Vyalov & Sobolev 1959, p. 31.
  17. ^ a b Smellie & Collerson 2021, p. 615.
  18. ^ a b LeMasurier et al. 1990, p. 446.
  19. ^ a b c Mitchell & Bergman 1991, p. 87.
  20. ^ Williams, R. W.; Collerson, K. D.; Gill, J. B.; Deniel, C. (1 July 1992). "High Th/U ratios in subcontinental lithospheric mantle: mass spectrometric measurement of Th isotopes in Gaussberg lamproites". Earth and Planetary Science Letters. 111 (2): 257. Bibcode:1992E&PSL.111..257W. doi:10.1016/0012-821X(92)90183-V. ISSN 0012-821X.
  21. ^ Tingey, McDougall & Gleadow 1983, p. 245.
  22. ^ a b c d e f g Sheraton & Cundari 1980, p. 418.
  23. ^ Smellie & Collerson 2021, p. 617.
  24. ^ LeMasurier et al. 1990, p. 10.
  25. ^ Sushchevskaya et al. 2014, p. 1031.
  26. ^ a b Sleep 2006, p. 250.
  27. ^ Panter, Kurt Samuel (1 January 2021). "Chapter 1.3 Antarctic volcanism: petrology and tectonomagmatic overview". Geological Society, London, Memoirs. 55 (1): 46. doi:10.1144/M55-2020-10. ISSN 0435-4052. S2CID 234276184.
  28. ^ Sleep 2006, p. 252.
  29. ^ Reading, Anya M.; Stål, Tobias; Halpin, Jacqueline A.; Lösing, Mareen; Ebbing, Jörg; Shen, Weisen; McCormack, Felicity S.; Siddoway, Christine S.; Hasterok, Derrick (26 October 2022). "Antarctic geothermal heat flow and its implications for tectonics and ice sheets". Nature Reviews Earth & Environment. 3 (12): 12. Bibcode:2022NRvEE...3..814R. doi:10.1038/s43017-022-00348-y. ISSN 2662-138X. S2CID 253177825.
  30. ^ Golynsky, Dmitry; Golynsky, Alexander (1 May 2010). Rifts in the tectonic structure of East Antarctica. EGU General Assembly 2010. p. 11538. Bibcode:2010EGUGA..1211538G.
  31. ^ Smellie & Collerson 2021, p. 615-616.
  32. ^ Aitken, A. R. A.; Young, D. A.; Ferraccioli, F.; Betts, P. G.; Greenbaum, J. S.; Richter, T. G.; Roberts, J. L.; Blankenship, D. D.; Siegert, M. J. (14 April 2014). "The subglacial geology of Wilkes Land, East Antarctica". Geophysical Research Letters. 41 (7): 2396. Bibcode:2014GeoRL..41.2390A. doi:10.1002/2014gl059405. ISSN 0094-8276. S2CID 53971785.
  33. ^ a b c Tingey, McDougall & Gleadow 1983, p. 241.
  34. ^ Mitchell & Bergman 1991, p. 7.
  35. ^ Migdisova et al. 2023, p. 911.
  36. ^ a b Murphy 2002, p. 981.
  37. ^ Sushchevskaya et al. 2014, p. 1035.
  38. ^ Salvioli-Mariani, Toscani & Bersani 2004, p. 98.
  39. ^ Vyalov & Sobolev 1959, p. 33.
  40. ^ a b Murphy 2002, p. 999.
  41. ^ Sheraton & Cundari 1980, p. 426.
  42. ^ Sushchevskaya et al. 2014, p. 1046.
  43. ^ Tingey, McDougall & Gleadow 1983, p. 243.
  44. ^ Mitchell & Bergman 1991, p. 86.
  45. ^ Tingey, McDougall & Gleadow 1983, p. 244.
  46. ^ Grew, Edward S. (1982), Nairn, Alan E. M.; Stehli, Francis G. (eds.), "The Antarctic Margin", The Ocean Basins and Margins, Boston, MA: Springer US, p. 702, doi:10.1007/978-1-4615-8038-6_15, ISBN 978-1-4615-8040-9, retrieved 2022-03-19
  47. ^ LeMasurier et al. 1990, p. 447.
  48. ^ "Gaussberg". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-24.
  49. ^ Koffman, Bess G.; Goldstein, Steven L.; Winckler, Gisela; Kaplan, Michael R.; Kreutz, Karl J.; Bolge, Louise; Bory, Aloys; Biscaye, Pierre (15 December 2021). "Late Holocene dust provenance at Siple Dome, Antarctica". Quaternary Science Reviews. 274: 8. Bibcode:2021QSRv..27407271K. doi:10.1016/j.quascirev.2021.107271. ISSN 0277-3791. S2CID 244069283.
  50. ^ a b Gregory 1908, p. 33.
  51. ^ Gregory 1908, p. 35.
  52. ^ Murray, James (1907). "Antarctic Rotifera" (PDF). British Antarctic Expedition. 1909.1 (3): 41. Retrieved 18 March 2022.
  53. ^ Yeates, G. W. (December 1979). "Terrestrial nematodes from the Bunger Hills and Gaussberg, Antarctica". New Zealand Journal of Zoology. 6 (4): 641–643. doi:10.1080/03014223.1979.10428408.
  54. ^ Miller, W.R.; Miller, J.D.; Heatwole, H. (January 1996). "Tardigrades of the Australian Antarctic Territories: the Windmill Islands, East Antarctica". Zoological Journal of the Linnean Society. 116 (1–2): 181. doi:10.1111/j.1096-3642.1996.tb02342.x.
  55. ^ Fuchs, V. E. (January 1951). "The Falkland Islands Dependencies Survey, 1947–50". Polar Record. 6 (41): 16. Bibcode:1951PoRec...6....7F. doi:10.1017/S0032247400040894. ISSN 1475-3057. S2CID 251050677.
  56. ^ Croxall, J. P.; Steele, W. K.; McInness, S. J.; Prince, P. A. (1995-10-15). "Breeding Distribution of the Snow Petrel Pagodroma Nivea". Marine Ornithology. 23: 69–100. ISSN 1018-3337. Archived from the original on 2020-07-24. Retrieved 2022-03-20.
  57. ^ Vyalov & Sobolev 1959, p. 35.

Sources

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