| Turnpike Bluff | |
|---|---|
  | |
| Highest point | |
| Coordinates | 80°44′S 30°4′W / 80.733°S 30.067°W |
Turnpike Bluff ( 80°44′S 30°4′W / 80.733°S 30.067°W) is a conspicuous rock formation in the Shackleton Mountains of Antarctica. [1]
First mapped in 1957 by the Commonwealth Trans-Antarctic Expedition, and so named because it marks entry to a crevassed area of Recovery Glacier through which the Expedition's vehicles had difficulty in passing on their journey from Shackleton Base to the South Pole in 1957. [1]
Turnpike Bluff is in the south of the Otter Highlands, to the north of the Recovery Glacier. [2] It lies five nautical miles (9 km) southwest of Mount Homard, at the southwest extremity of the Shackleton Range. [1]
The Turnpike Bluff Group is a sedimentary sequence of rocks exposed on the south flank of the Shackleton Range. The sequence includes basal clastics and quartzite, followed by carbonate-bearing clastics with Riphean age stromatolite colonies, and capped by over 1 km of greywacke and quartzitic arenite, alternating with pelite. The sequence is underlain unconformably by an Archean granitoid basement (1400 Ma). Metamorphism occurred at 526 Ma. [3] The group contains four formations, named after Wyeth Heights, Stephenson Bastion, Flett Crags and Mount Wegener. [4] These are features along the southern margin of the Shackleton Mountains, from west to east. [2]
- ^ a b c Alberts 1995, p. 765.
- ^ a b Shackleton USGS map.
- ^ Paech, Hahne & Vogler 1991, pp. 123–128.
- ^ Clarkson 1983, p. 109.
- Alberts, Fred G., ed. (1995),
Geographic Names of the Antarctic (PDF) (2 ed.), United States Board on Geographic Names, retrieved 3 December 2023
This article incorporates
public domain material from websites or documents of the
United States Board on Geographic Names. - Clarkson, Peter D. (1983), "Geology of the Shackleton Range II The Turnpike Bluff Group" (PDF), British Antarctic Survey Bulletin, no. 52, pp. 109–124, retrieved 10 December 2023
- Paech, H.-J.; Hahne, K.; Vogler, P. (1991), Thomson, M.R.A.; Crame, J.A.; Thomson, J.W. (eds.), Crustal development: the Transantarctic Mountains, in Geological Evolution of Antarctica, Cambridge: Cambridge University Press, ISBN 9780521372664
-
Shackleton Range, United States Geological Survey, 1983, retrieved 4 December 2023 This article incorporates
public domain material from websites or documents of the
United States Geological Survey.
| Turnpike Bluff | |
|---|---|
| |
| Highest point | |
| Coordinates | 80°44′S 30°4′W / 80.733°S 30.067°W |
Turnpike Bluff ( 80°44′S 30°4′W / 80.733°S 30.067°W) is a conspicuous rock formation in the Shackleton Mountains of Antarctica. [1]
First mapped in 1957 by the Commonwealth Trans-Antarctic Expedition, and so named because it marks entry to a crevassed area of Recovery Glacier through which the Expedition's vehicles had difficulty in passing on their journey from Shackleton Base to the South Pole in 1957. [1]
Turnpike Bluff is in the south of the Otter Highlands, to the north of the Recovery Glacier. [2] It lies five nautical miles (9 km) southwest of Mount Homard, at the southwest extremity of the Shackleton Range. [1]
The Turnpike Bluff Group is a sedimentary sequence of rocks exposed on the south flank of the Shackleton Range. The sequence includes basal clastics and quartzite, followed by carbonate-bearing clastics with Riphean age stromatolite colonies, and capped by over 1 km of greywacke and quartzitic arenite, alternating with pelite. The sequence is underlain unconformably by an Archean granitoid basement (1400 Ma). Metamorphism occurred at 526 Ma. [3] The group contains four formations, named after Wyeth Heights, Stephenson Bastion, Flett Crags and Mount Wegener. [4] These are features along the southern margin of the Shackleton Mountains, from west to east. [2]
- ^ a b c Alberts 1995, p. 765.
- ^ a b Shackleton USGS map.
- ^ Paech, Hahne & Vogler 1991, pp. 123–128.
- ^ Clarkson 1983, p. 109.
- Alberts, Fred G., ed. (1995),
Geographic Names of the Antarctic (PDF) (2 ed.), United States Board on Geographic Names, retrieved 3 December 2023 This article incorporates
public domain material from websites or documents of the
United States Board on Geographic Names.
- Clarkson, Peter D. (1983), "Geology of the Shackleton Range II The Turnpike Bluff Group" (PDF), British Antarctic Survey Bulletin, no. 52, pp. 109–124, retrieved 10 December 2023
- Paech, H.-J.; Hahne, K.; Vogler, P. (1991), Thomson, M.R.A.; Crame, J.A.; Thomson, J.W. (eds.), Crustal development: the Transantarctic Mountains, in Geological Evolution of Antarctica, Cambridge: Cambridge University Press, ISBN 9780521372664
-
Shackleton Range, United States Geological Survey, 1983, retrieved 4 December 2023 This article incorporates
public domain material from websites or documents of the
United States Geological Survey.