Ross Embayment

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Map of Antarctica showing outline of Ross Embayment

The Ross Embayment is a large region of Antarctica, comprising the Ross Ice Shelf and the Ross Sea, that lies between East and West Antarctica.

Extent[]

The continent of Antarctica has two major divisions; West Antarctica in mostly western longitudes and East Antarctica in mostly eastern longitudes. East Antarctica is the larger and has a higher average elevation. Separating the two subcontinents is a lower elevation topographic region occupied by the Ross Ice Shelf and the Ross Sea. This region is referred to as the Ross Embayment. The embayment comprises an area of approximately 1,137,000 square kilometres (439,000 sq mi). It includes the Ross Sea (637,000 square kilometres (246,000 sq mi))[1] and the Ross Ice Shelf (as of 2013, 500,809 square kilometres (193,363 sq mi)).[2] The name is most commonly used in the scientific literature,[3][4][5] at times along with the West Antarctic Rift System, which is of larger extent and has geologic meaning.[6] Because the rift system includes the embayment, the latter is considered to lie in West Antarctica.

The informal use of the name 'Ross Embayment' tends to denote a smaller region than the rift system. The embayment extends from Northern Victoria Land and the Transantarctic Mountains on the west (in East Antarctica) to the Edward VII Peninsula, Shirase Coast, and Siple Coast on the east (Marie Byrd Land in West Antarctica), and south to the grounding line of the Ross Ice Shelf.[1]

Formation[]

A view of the Ross Ice Shelf and Ross Sea in Antarctica from the Moderate Resolution Imaging Spectroradiometer (MODIS). North at top. A giant iceberg on the left (west) has broken off the front of the Ross Ice Shelf. The Transantarctic Mountains cross the image from left to lower right. Original file from Commons was image-enhanced.

The low elevation marine characteristic of the Ross Embayment formed since the Jurassic period.[7] Before that time and earlier East and West Antarctica had similar elevations and the Ross Embayment did not exist.[7][8][9] The breakup of the eastern sector of Gondwana in Cretaceous time resulted in crustal extension, thinning and subsidence to form the Ross Embayment.[10] The mechanism of crustal stretching and subsidence in the Ross Embayment has been attributed to detachment faulting.[11] Extension between East and West Antarctica totals about 500 kilometers.[12] Half of this occurred prior to sea floor spreading that separated the New Zealand microcontinents (Zealandia) from Antarctica beginning at 85 million years.[13] The remaining extension occurred in the , Northern Basin, and in the western Ross Sea before late Miocene time.[12][14] Subsidence continued as mantle under the Ross Embayment cooled.[12]

See also[]

References[]

  1. ^ Jump up to: a b "About the Ross Sea". NIWA. 2012-07-27. Retrieved 2018-02-23.
  2. ^ Rignot, E.; Jacobs, S.; Mouginot, J.; Scheuchl, B. (2013-07-19). "Ice-Shelf Melting Around Antarctica". Science. 341 (6143): 266–270. doi:10.1126/science.1235798. ISSN 0036-8075. PMID 23765278. S2CID 206548095.
  3. ^ Fitzgerald, Paul G.; Sandiford, Michael; Barrett, Peter J.; Gleadow, Andrew J.W. (1986). "Asymmetric extension associated with uplift and subsidence in the Transantarctic Mountains and Ross Embayment". Earth and Planetary Science Letters. 81 (1): 67–78. doi:10.1016/0012-821x(86)90101-9.
  4. ^ Webb, Peter-Noel; Harwood, David M. (1991). "Late Cenozoic glacial history of the Ross embayment, Antarctica". Quaternary Science Reviews. 10 (2–3): 215–223. doi:10.1016/0277-3791(91)90020-u.
  5. ^ McKay, Robert; Browne, Greg; Carter, Lionel; Cowan, Ellen; Dunbar, Gavin; Krissek, Lawrence; Naish, Tim; Powell, Ross; Reed, Josh (2009). "The stratigraphic signature of the late Cenozoic Antarctic Ice Sheets in the Ross Embayment". Geological Society of America Bulletin. 121 (11–12): 1537–1561. doi:10.1130/b26540.1.
  6. ^ Behrendt, J. C.; LeMasurier, W. E.; Cooper, A. K.; Tessensohn, F.; Tréhu, A.; Damaske, D. (1991-12-01). "Geophysical studies of the West Antarctic Rift System". Tectonics. 10 (6): 1257–1273. doi:10.1029/91tc00868. ISSN 1944-9194.
  7. ^ Jump up to: a b Barrett, P.J. (1981). "History of the Ross Sea region during the deposition of the Beacon Supergroup 400-180 million years ago". Journal of the Royal Society of New Zealand. 11 (4): 447–458. doi:10.1080/03036758.1981.10423334.
  8. ^ Barrett, P. J., D. H. Elliot, and J. F. Lindsay (2013), The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurrasic) in the Beardmore Glacier Area, Antarctica, in Geology of the Central Transantarctic Mountains, edited by M. D. Turner and J. E. Splettstoesser, pp. 339–428, American Geopysical Union, doi:10.1029/AR036p0339.
  9. ^ Bialas, Robert W.; Buck, W. Roger; Studinger, Michael; Fitzgerald, Paul G. (2007-08-01). "Plateau collapse model for the Transantarctic Mountains–West Antarctic Rift System: Insights from numerical experiments". Geology. 35 (8): 687–690. doi:10.1130/G23825A.1. ISSN 0091-7613.
  10. ^ Dalziel, I. W. D.; Lawver, L. A. (2001). Alley, Richard B.; Bindschadle, Robert A. (eds.). The West Antarctic Ice Sheet: Behavior and Environment. American Geophysical Union. pp. 29–44. doi:10.1029/ar077p0029. ISBN 9781118668320.
  11. ^ Fitzgerald, P.G. and Baldwin, S.L. (1997). "Detachment fault model for the evolution of the Ross Embayment". The Antarctic Region: Geological Evolution and Processes: 555–564.CS1 maint: multiple names: authors list (link)
  12. ^ Jump up to: a b c Wilson, Douglas S.; Luyendyk, Bruce P. (2009-08-01). "West Antarctic paleotopography estimated at the Eocene-Oligocene climate transition". Geophysical Research Letters. 36 (16): L16302. doi:10.1029/2009gl039297. ISSN 1944-8007. S2CID 163074.
  13. ^ Lawver, L.A. and Gahagan, L.M. (1994). "Constraints on timing of extension in the Ross Sea region". Terra Antartica. 1 (3): 545–552.CS1 maint: multiple names: authors list (link)
  14. ^ Henrys, S., T. Wilson, J.M. Whittaker, C. Fielding, J. Hall, and T. Naish (2007). "Tectonic History of Mid-Miocene to Present Southern Victoria Land Basin, Inferred from Seismic Stratigraphy in McMurdo Sound, Antarctica; USGS Open-File Report 2007-1047, Short Research Paper 049". Tectonic History of Mid-Miocene to Present Southern Victoria Land Basin, Inferred from Seismic Stratigraphy in Mcmurdo Sound, Antarctica. 2007 (1047srp049). doi:10.3133/of2007-1047.srp049.CS1 maint: multiple names: authors list (link)
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