Royal Society Range

The Royal Society Range (78°10′S 162°40′E) is a mountain range in Victoria Land, Antarctica. With its summit at 4,025 metres (13,205 ft), the massive Mount Lister forms the highest point in this range. Mount Lister is located along the western shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar glaciers. Other notable local terrain features include Allison Glacier, which descends from the west slopes of the Royal Society Range into Skelton Glacier.

Royal Society Range
View of the Royal Society Range from the Ross Sea
Highest point
PeakMount Lister
Elevation13,205 ft (4,025 m)
Coordinates78°10′00″S 162°40′00″E
Geography
Map depicting the location of the Royal Society Range in Victoria Land, Antarctica
ContinentAntarctica
RegionVictoria Land, Antarctica
Parent rangeTransantarctic Mountains
Mount Lister, tallest peak in range seen from McMurdo Station, March 2015
Royal Society Range seen from South, November 2011

Discovery and naming
Royal Society Range is located in Antarctica
Royal Society Range
Royal Society Range
Map depicting the location of the Royal Society Range in Victoria Land, Antarctica

The range was probably first seen by Captain James Clark Ross in 1841.[1]

The range was explored by the British National Antarctic Expedition (BrNAE) under Robert Falcon Scott, who named the range after the Royal Society and applied names of its members to many of its peaks. For example, Mount Lister was named for Lord Joseph Lister, President of the Royal Society, 1895–1900.[2] The Royal Society provided financial support to the expedition and its members had assisted on the committee which organized the expedition.[1]

Geology

The Royal Society Range consists of a Precambrian igneous and meta-igneous basement complex overlain by Devonian- to Triassic-age sandstones, siltstones and conglomerates of the Beacon Supergroup which dip shallowly westward away from the Ross Sea coast.[3] The entire region is cut by north–south trending longitudinal faults, east–west trending transverse faults, and structurally related dike swarms.[4]

Tectonic and fluvial activity have featured very heavily in the recent geologic history of the Royal Society Range. Following the extension of the Ross Sea Basin (c. 55 million years ago), an episode of uplift drove the creation of the Royal Society Range rift flank. At this time a tectonic (though not accretionary) wedge, up to 6 km thick on the coast, was present, though it quickly began to erode due primarily to fluvial processes, and the Royal Society Range was cut down near to its present appearance by the mid-Miocene. Relatively limited glacial action since that time has preserved much of the fluvial architecture of the Range, and though uplift did not cease, its magnitude is such that it has not drastically affected the landscape, having progressed only 67 meters in the last 8 million years.[3]

Koettlitz Glacier Alkaline Province

Neoproterozoic tectonic extension along the edge of the East Antarctic Craton between the Skelton and Koettlitz Glaciers resulted in the emplacement of coarse grained alkaline igneous intrusive rocks (ranging from gabbro to A-type granite). This area of alkaline intrusives is referred to as the Koettlitz Glacier Alkaline Province[5]

Ross Orogeny

Cambrian tectonic convergence, continental collision and plate subduction led to the emplacement of calc-alkaline and adakitic granitoids. This period of mountain building is referred to as the Ross Orogeny.

Volcanic history

The Royal Society Range contains over 50 basaltic vents, ranging in size from tiny mounds to cinder cones up to 300 meters (985 feet) high. Dating of surface material indicates they were active earlier than 15 million years ago (e.g. Heald Island)[6] and as recently as 80,000 years ago, with glacier-bound tephra layers suggesting even more recent Holocene activity.[7] The vast majority of vents are located in the foothills of the Royal Society mountains just north of Koettlitz Glacier, and most are Quaternary in age. Most emanating flows are 3–10 meters thick and less than 4 kilometers long. The composition, with very few exceptions, is porphyritic basanite with primarily olivine and clinopyroxene phenocrysts, though some phenocrystic plagioclase is also present.[8]

Features

See also

References
  1. "Royal Society Range". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2004-11-13.
  2. "Mount Lister". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2010-02-09.
  3. Sugden, D.E., Summerfield, M.A., Denton, G.H., Wilch, T.I., McIntosh, W.C., Marchant, D.R., and Rutford, R.H., 1999, Landscape development in the Royal Society Range, southern Victoria Land, Antarctica: stability since the mid-Miocene: Geomorphology, v. 28, p. 181-200.
  4. Wilson, T.J., 1995, Cenozoic transtension along the Transantarctic Mountains–West Antarctic rift boundary, southern Victoria Land, Antarctica: Tectonics, v. 14, 531–545.
  5. Read, S. E. (2010). Koettlitz Glacier Alkaline Province : Late Neoproterozoic extensional magmatism in southern Victoria Land, Antarctica (Thesis, Doctor of Philosophy). http://hdl.handle.net/10523/5428
  6. Wilch, T.I., 1991, The surficial geology and geochronology of middle Taylor Valley Antarctica: Implications for Plio-Pleistocene Antarctic glacial history [M.S. thesis]: Orono, The University of Maine, 363 p.,
  7. Armstrong, R.L., 1978, K-Ar dating: Late Cenozoic McMurdo Volcanic Group and Dry Valley glacial history, Victoria Land, Antarctica: New Zealand Journal of Geology and Geophysics, v. 21, p. 685-698.
  8. Wright, A.C., and Kyle, P.R., 1990, Royal Society Range Summary, in LeMasurier, W.E., and Thomson, J.W., eds., Volcanoes of the Antarctic Plate and Southern Oceans: Washington, DC, American Geophysical Union, Antarctic Research Series, v. 48, p. 81-88.
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