Shackleton Range

The Shackleton Range is a mountain range in Antarctica. Rising at Holmes Summit to 1,875 metres (6,152 ft), it extends in an east–west direction for about 160 kilometres (99 mi) between the Slessor and Recovery glaciers.[1]

Shackelton Range
The Shackleton Range, just out of the ice sheet between Slessor and Recovery glaciers.
Highest point
Elevation1,875 m (6,152 ft) 
Geography
Shackelton Range
Location in Antarctica

The range was named after Sir Ernest Shackleton, leader of the British Imperial Trans-Antarctic Expedition (or "Shackleton's Expedition") of 1914–16.[1]

Surveys

The Commonwealth Trans-Antarctic Expedition (CTAE), which in 1956 saw the range from the air, conducted a ground-level survey of its western part in 1957. The United States Navy photographed the range from the air in 1967. In 1968–69 and 1969–70, the British Antarctic Survey (based at Halley Station) conducted further ground surveys with support from US Navy C-130 Hercules aircraft.[1]

Geology

The Haskard Group and Turnpike Bluff Group rest unconformably on the Archean-Middle Proterozoic Shackleton Range Metamorphic Complex. The Ordovician-Early Devonian Blaiklock Glacier Group (475 Ma) also unconformably overlies the Shackleton Range Metamorphic Complex. This group is composed of sandstones and conglomerates, and is unconformably overlain by the Beacon Supergroup.[2]

Features

Geographical features include:

Herbert Mountains

Read Mountains

Du Toit Nunataks

Other features

La Grange Nunataks

Other features

gollark: Just make big companies backdoor it.
gollark: Well, I don't think they planned to *ban* E2E.
gollark: The UK has strict laws on political campaign maximum spend and whatnot.
gollark: A vote was won by a 4% margin several years ago before we knew what insanity would happen and which IIRC may actually have been affected by illegal campaigning.
gollark: Because "the will of the people".

References

  1. "Shackleton Range". Geographic Names Information System. United States Geological Survey. Retrieved 2004-10-31.
  2. Laird, M.G. (1991). Thomson, M.R.A.; Crame, J.A.; Thomson, J.W. (eds.). Lower-mid-Palaeozoic sedimentation and tectonic patterns on the palaeo-Pacific margin of Antarctica, in Geological Evolution of Antarctica. Cambridge: Cambridge University Press. pp. 178–179. ISBN 9780521372664.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.