Gotley Glacier
Body of ice on Heard Island
53°10′S 73°27′E / 53.167°S 73.450°E / -53.167; 73.450
Gotley Glacier is a well-defined glacier, 5 nautical miles (9 km) long, descending from the ice-covered slopes of the Big Ben massif to the southwest side of Heard Island in the southern Indian Ocean. Its terminus is located between Cape Arkona and Cape Labuan.[6][7] To the east of Gotley Glacier is Deacock Glacier, whose terminus is located between Cape Labuan and Long Beach. To the northwest of Gotley Glacier is Lied Glacier, whose terminus is located between Cape Arkona and Cape Pillar. Cape Arkona separates Gotley Glacier from Lied Glacier.
Discovery and naming
Gotley Glacier was surveyed in 1948 by the Australian National Antarctic Research Expeditions, and named by them for Aubrey V. Gotley, meteorologist and officer-in-charge of the party.[6][7]
References
- ^ a b c Andrew Ruddell (25 May 2010). "Our subantarctic glaciers: why are they retreating?". Glaciology Program, Antarctic CRC and AAD. Archived from the original on 2 October 2009. Retrieved 5 June 2010.
- ^ Ian F. Allison; Peter L. Keage (1986). "Recent changes in the glaciers of Heard Island". Polar Record. 23 (144): 255–272. doi:10.1017/S0032247400007099. S2CID 130086301.
- ^ Quilty, P.G.; Wheller, G. (2000). "Heard Island and the McDonald Islands: A window into the Kerguelen Plateau (Heard Island Papers)". Pap. Proc. R. Soc. Tasm. 133 (2): 1–12.
- ^ Budd, G.M. (2000). "Changes in Heard Island glaciers, king penguins and fur seals since 1947 (Heard Island Papers)". Pap. Proc. R. Soc. Tasm. 133 (2): 47–60.
- ^ Douglas E. Thost; Martin Truffer (February 2008). "Glacier Recession on Heard Island, Southern Indian Ocean". Arctic, Antarctic, and Alpine Research. 40 (1): 199–214. doi:10.1657/1523-0430(06-084)[THOST]2.0.CO;2. S2CID 130245283. Archived from the original on 4 December 2012. Retrieved 7 June 2010.
- ^ a b "Gotley Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 5 June 2010.
- ^ a b "Gotley Glacier". Australian Antarctic Data Centre. Retrieved 5 June 2010.
Further reading
- U. Radok; D. Watts (1975). "A synoptic background to glacier variations of Heard Island" (PDF). Snow and Ice (Proceedings of the Moscow Symposium, August 1971) (104 ed.). Wallingford, Oxfordshire, UK: International Association of Hydrological Sciences. pp. 42–56. Retrieved 7 June 2010.
- Truffer, M., Thost, D. and Ruddell, A. (2001). "The Brown Glacier, Heard Island: its morphology, dynamics, mass balance and climate setting". Antarctic CRC Research Report No. 24. Hobart, Tasmania: Cooperative Research Centre for the Antarctic and Southern Ocean Environment, University of Tasmania. pp. 1–27.
{{cite book}}: CS1 maint: multiple names: authors list (link) - Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at Stephenson Glacier, Heard Island World Heritage Area" (PDF). Polar Record. 38 (207): 297–308. doi:10.1017/S0032247400017988. S2CID 37333655. Retrieved 7 June 2010.
External links
- Click here Archived 11 February 2014 at the Wayback Machine to see a map of Heard Island and McDonald Islands, including all major topographical features
- Australian Antarctic Division
- Australian Antarctic Gazetteer
- Composite Gazetteer of Antarctica
- Australian Antarctic Names and Medals Committee (AANMC)
- United States Geological Survey, Geographic Names Information System (GNIS)
- Scientific Committee on Antarctic Research (SCAR)
This article incorporates public domain material from "Gotley Glacier". Geographic Names Information System. United States Geological Survey.
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