| Airy Glacier | |
|---|---|
Location of Airy Glacier in Antarctica | |
| Location | Antarctic Peninsula |
| Coordinates | 69°13′S66°20′W / 69.217°S 66.333°W |
| Length | 20 nmi (37 km; 23 mi) |
| Width | 6 nmi (11 km; 7 mi) |
| Thickness | unknown |
| Terminus | Forster Ice Piedmont |
| Status | unknown |
The Airy Glacier ( 69°13′S66°20′W / 69.217°S 66.333°W Coordinates: 69°13′S66°20′W / 69.217°S 66.333°W ) is a glacier 20 nautical miles (37 km) long and 6 nautical miles (11 km) wide, flowing west to the northeast portion of Forster Ice Piedmont, near the west coast of the Antarctic Peninsula.
The glacier was first roughly surveyed by British Graham Land Expedition of 1936–37, then photographed from the air by the Ronne Antarctic Research Expedition in 1947, and surveyed by Falkland Islands Dependencies Survey in 1958. It was named by United Kingdom Antarctic Place-Names Committee for George Biddell Airy, British Astronomer Royal, who in 1839 introduced a method of correcting magnetic compasses for deviation.
The Prince Charles Mountains are a major group of mountains in Mac. Robertson Land in Antarctica, including the Athos Range, the Porthos Range, and the Aramis Range. The highest peak is Mount Menzies. Other prominent peaks are Mount Izabelle and Mount Stinear. These mountains together with other scattered peaks form an arc about 260 miles long, extending from the vicinity of Mount Starlight in the north to Goodspeed Nunataks in the south.
Shambles Glacier is a steep glacier 4 miles (6 km) long and 6 miles (10 km) wide, with very prominent hummocks and crevasses, flowing east between Mount Bouvier and Mount Mangin into Stonehouse Bay on the east side of Adelaide Island. It is the island's largest glacier, and provides an eastern outlet from the giant Fuchs Ice Piedmont which covers the entire western two-thirds of the island. In doing so, Shambles Glacier provides the largest 'gap' in Adelaide Island's north–south running mountain chain.
Mount Castro is a mountain, 1,630 metres (5,350 ft) high, on the north side of Seller Glacier, 5 nautical miles (9 km) southeast of Mount Gilbert, in the central Antarctic Peninsula. It was photographed from the air by the British Graham Land Expedition in 1937, and by the Ronne Antarctic Research Expedition in 1947. It was surveyed from the ground by the Falkland Islands Dependencies Survey in December 1958, and named by the UK Antarctic Place-Names Committee for João de Castro, a Portuguese navigator who made pioneer experimental investigations of the variation of the magnetic compass.
Wubbold Glacier is a steeply inclined glacier, 8 nautical miles (15 km) long, flowing south from the Havre Mountains, situated in the northern portion of Alexander Island, Antarctica. The glacier drains the north, west and southwest slopes of Mount Pontida, and flows into Lazarev Bay north of Mount Holt. It was photographed from the air by Ronne Antarctic Research Expedition in 1947 and was mapped from the photographs by Falkland Islands Dependencies Survey in 1960. Named by Advisory Committee on Antarctic Names for Commander J.H. Wubbold, USCG, commanding officer, USCGC Northwind, U.S. Navy Operation Deepfreeze, 1977.
Bartók Glacier is a glacier, 7 nautical miles (13 km) long and 3 nautical miles (6 km) wide, flowing southwest from the southern end of the Elgar Uplands in the northern part of Alexander Island. It was first photographed from the air and roughly mapped by the British Graham Land Expedition in 1937, and more accurately mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the Falkland Islands Dependencies Survey in 1960. It was named by the UK Antarctic Place-Names Committee after the Hungarian composer Béla Bartók.
Comrie Glacier is a glacier 13 nautical miles (24 km) long, flowing west to enter the head of Bigo Bay on the west coast of Graham Land. It was first sighted and roughly surveyed by the French Antarctic Expedition in 1909. It was resurveyed in 1935–36 by the British Graham Land Expedition (BGLE), and later named for Leslie J. Comrie, founder and first Director of the Scientific Computing Service Ltd, London, who, as Superintendent of HM Nautical Almanac Office in 1934, greatly assisted the BGLE, 1934–37, by providing advance copies of The Nautical Almanac up to 1937.
Norman Peak is a peak rising to 1,790 m on the north side of Airy Glacier, 4 nautical miles (7 km) north-northeast of Anchor Crag and 3.8 nautical miles (7 km) west of Peregrinus Peak, in southwest Graham Land. The peak was photographed from the air by Ronne Antarctic Research Expedition (RARE), 1947, and was surveyed by Falkland Islands Dependencies Survey (FIDS), 1958. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Robert Norman, English compass maker who fortuitously discovered magnetic dip in 1576.
Wakefield Highland is a snow-covered highland in the central region of the Antarctic Peninsula, bounded to the north by Hermes Glacier and the heads of Weyerhaeuser Glacier and Aphrodite Glacier, to the west by the heads of Airy Glacier, Rotz Glacier and Seller Glacier, to the south by Fleming Glacier and to the east by the heads of Lurabee Glacier, Sunfix Glacier and Grimley Glacier. Photographed from the air by Ronne Antarctic Research Expedition (RARE) on December 22, 1947. Surveyed by Falkland Islands Dependencies Survey (FIDS) in November 1960. Named after Viscount Wakefield of Hythe, a contributor to British Graham Land Expedition (BGLE), 1934–37. This toponym, concurred in by United Kingdom Antarctic Place-Names Committee (UK-APC) and Advisory Committee on Antarctic Names (US-ACAN), restores the name Wakefield in the vicinity of the BGLE's displaced "Mount Wakefield".
Whittle Glacier is a short channel glacier flowing northeast to Colvocoresses Bay and terminating in a small glacier tongue 6 nautical miles northwest of Williamson Glacier. Delineated from air photos taken by U.S. Navy Operation Highjump (1946–47), and named by Advisory Committee on Antarctic Names (US-ACAN) for Dr. J.S. Whittle, Assistant Surgeon on the sloop Vincennes of the United States Exploring Expedition (1838–42) under Lieutenant Charles Wilkes.
Coulter Glacier is a steeply inclined glacier, 5 nautical miles (9 km) long, flowing south from the Havre Mountains, northern Alexander Island, into Kolokita Cove in Lazarev Bay, Antarctica. The glacier was photographed from the air by the Ronne Antarctic Research Expedition in 1947 and mapped from the photographs by the Falkland Islands Dependencies Survey in 1960. It was named by the Advisory Committee on Antarctic Names for R.W. Coulter, Master of USNS Alatna during U.S. Navy Operation Deepfreeze, 1969.
Delius Glacier is a glacier, 6 nautical miles (11 km) long and 2 nautical miles (4 km) wide, flowing west from the Elgar Uplands into Nichols Snowfield, in the northern part of Alexander Island, Antarctica. It was first seen from the air and roughly mapped by the British Graham Land Expedition in 1937. It was more accurately mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the Falkland Islands Dependencies Survey in 1960, and from U.S. Landsat imagery of February 1975. It was named by the UK Antarctic Place-Names Committee after Frederick Delius, the British composer.
Tumble Glacier is a glacier extending along the east side of Alexander Island, Antarctica, 7 nautical miles (13 km) long and 3 nautical miles (6 km) wide, which flows east from the cliffs of Mount Egbert, Mount Ethelwulf and Mount Ethelred of the Douglas Range into the west side of the George VI Ice Shelf that occupies George VI Sound immediately south of Mount King. The glacier was first roughly surveyed in 1936 by the British Graham Land Expedition under Rymill. Resurveyed in 1948 by the Falkland Islands Dependencies Survey, and so named by them because of the extremely broken condition of the lower reaches of the glacier.
Fleming Glacier is a broad glacier 25 nautical miles (46 km) long on the west side of the Antarctic Peninsula, flowing west-northwest and terminating in Forster Ice Piedmont to the east of the Wordie Ice Shelf. The glacier was charted by the British Graham Land Expedition (BGLE) under John Rymill, 1934–37, and was photographed from the air by the United States Antarctic Service on September 29, 1940. This hitherto unnamed feature was named by the Advisory Committee on Antarctic Names in 1947 for Reverend W.L.S. Fleming, Dean of Trinity Hall, Cambridge University; also, chaplain, chief scientist, and geologist of the BGLE.
Hariot Glacier is a glacier flowing northwest along the south side of Morgan Upland before turning west into the northern portion of the Wordie Ice Shelf, along the west coast of the Antarctic Peninsula. It was roughly surveyed by the British Graham Land Expedition, 1936–37, and the upper reaches were photographed from the air by the Ronne Antarctic Research Expedition, 1947. The glacier was surveyed from the ground by members of the Falkland Islands Dependencies Survey who travelled along it in December 1958, and it was named by the UK Antarctic Place-Names Committee after Thomas Hariot, an English mathematician who pioneered new methods of navigation under the patronage of Sir Walter Raleigh.
Seller Glacier is a well-defined glacier, 20 nautical miles (37 km) long and 4 nautical miles (7 km) wide flowing westward into Forster Ice Piedmont, western Antarctic Peninsula, just north of Flinders Peak. Roughly surveyed by British Graham Land Expedition (BGLE), 1936–37, and resurveyed by Falkland Islands Dependencies Survey (FIDS) in December 1958.
Holtedahl Bay is a bay, 10 nautical miles (19 km) long in a northwest–southeast direction and averaging 6 nautical miles (11 km) wide, between Velingrad Peninsula and Stresher Peninsula along the west coast of Graham Land, Antarctica. The bay is entered southwest of Prospect Point and northeast of Black Head, and has its head fed by Hugi Glacier.
The Kelvin Crests are a line of steep-sided elevations with ice-covered cliffs 5 nautical miles (9 km) long, on the north side of Airy Glacier near its junction with Forster Ice Piedmont on the west side of the Antarctic Peninsula. Roughly surveyed by the British Graham Land Expedition in 1936–37, they were photographed from the air by the Ronne Antarctic Research Expedition in 1947. They were surveyed from the ground, from the southwest only, by members of the Falkland Islands Dependencies Survey, December 1958, and completely mapped by the United States Geological Survey, 1974. The feature was named by the UK Antarctic Place-Names Committee for William Thomson, 1st Baron Kelvin, a British physicist and engineer who made substantial improvements in the design of magnetic compasses, 1873–78, and invented the Thomson sounding machine in 1878.
Remus Glacier is a glacier, 8 nautical miles (15 km) long, which flows from the north slopes of Mount Lupa northwestward along the northeast side of the Blackwall Mountains into Providence Cove, Neny Fjord, on the west coast of Graham Land. The lower reaches of the glacier were first roughly surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 by the Falkland Islands Dependencies Survey (FIDS), who so named it for its association with Romulus Glacier, whose head lies near the head of this glacier.
Rotz Glacier is a tributary glacier 9 nautical miles (17 km) long and 2 nautical miles (3.7 km) wide. It flows west from Wakefield Highland, central Antarctic Peninsula, into Airy Glacier at a point due south of Mount Timosthenes. Photographed by Ronne Antarctic Research Expedition (RARE) on November 27, 1947. Surveyed by Falkland Islands Dependencies Survey (FIDS) in December 1958 and November 1960. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) after Jean Rotz, 16th century French chartmaker and writer on the principles of navigation, who designed an elaborate magnetic compass and became hydrographer to King Henry VIII in 1542.
This article incorporates public domain material from the United States Geological Survey document: "Airy Glacier".(content from the Geographic Names Information System )