Stephenson Glacier (53°6′S73°42′E / 53.100°S 73.700°E / -53.100; 73.700) is a glacier close west of Dovers Moraine on the east side of Heard Island in the southern Indian Ocean.[6][7] Its terminus is between Dovers Moraine and Stephenson Lagoon, with part of the glacier flowing to Doppler Hill and Sealers Beach. To the north of Stephenson Glacier is Brown Glacier, whose terminus is located at Brown Lagoon. To the southwest of Stephenson Glacier is Winston Glacier, whose terminus is located at Winston Lagoon, between Cape Lockyer and Oatt Rocks.
^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.
^Andrew Ruddell (25 May 2010). "Our subantarctic glaciers: why are they retreating?". Glaciology Program, Antarctic CRC and AAD. Retrieved 5 June 2010.
^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.
^"Stephenson Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 5 June 2010.
^"Stephenson Glacier". Australian Antarctic Data Centre. Retrieved 5 June 2010.
and 27 Related for: Stephenson Glacier information
StephensonGlacier (53°6′S 73°42′E / 53.100°S 73.700°E / -53.100; 73.700) is a glacier close west of Dovers Moraine on the east side of Heard Island...
showed several glaciers had retreated further, including the Stephenson, Brown and Baudissin glaciers. Other studies have also shown the glaciers are retreating...
cliffs of Brown Glacier and StephensonGlacier, which in 1954 were over 50 feet (15 m) high, had disappeared by 1963 when the glaciers terminated as much...
Winston Glacier is StephensonGlacier, the terminus of which is located between Dovers Moraine and Stephenson Lagoon. To the southwest of Winston Glacier is...
off Brown and StephensonGlaciers by 1963. Glaciers terminated as much as 100 yards inland. Marked recession since 1955 of Baudissin Glacier on the north...
southeast of Brown Glacier is StephensonGlacier, whose terminus is located between Dovers Moraine and Stephenson Lagoon. Brown Glacier was surveyed by ANARE...
Mount Stephenson is a mountain in Antarctica. It is located within the central portion of the Douglas Range, standing at the heads of Toynbee Glacier and...
July 2013. "StephensonGlacier Retreat Heard Island". Glacierchange.wordpress. 4 November 2010. Retrieved 18 July 2013. "Heard Island glaciers melting away...
2000 found that the Stephenson, Brown and Baudissin glaciers, among others, had retreated even further. The terminus of Brown Glacier has retreated approximately...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
(link) Kevin Kiernan & Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
1–27. Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
1–27. Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
Mountains and the Stephenson Bastion into the Recovery Glacier, and small glaciers carry ice south from the Read Mountains and Stephenson Bastion. The high...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
1–27. Kevin Kiernan & Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
the east end of the main mass of Heard Island immediately east of StephensonGlacier. It was surveyed in 1948 by the Australian National Antarctic Research...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
(link) Kevin Kiernan; Anne McConnell (2002). "Glacier retreat and melt-lake expansion at StephensonGlacier, Heard Island World Heritage Area" (PDF). Polar...
north from the east face of Mount Stephenson into the George VI Ice Shelf that occupies George VI Sound. The glacier was first photographed from the air...
Bertram Glacier (70°50′S 67°28′W / 70.833°S 67.467°W / -70.833; -67.467) is a glacier, 15 nautical miles (28 km) long and 18 nautical miles (33 km)...
Shelby 20,990 657 Stark 5,400 288 Peoria, IL Metropolitan Statistical Area Stephenson 44,630 564 Freeport, IL Micropolitan Statistical Area Tazewell 131,343...
which flows east from the foot of Mount Stephenson into George VI Sound immediately north of Mount Huckle. The glacier was first roughly surveyed in 1936 by...
10 miles (16 km) southwest of Mount Stephenson in the northern portion of Alexander Island, Antarctica. The glacier was first sighted from the air by the...