Farr Bay is a bay 7 miles (11 km) wide on the coast of Antarctica, lying just east of Helen Glacier. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Mawson. In some early reports the feature was called "Depot Bay". It was later named by Mawson for Dr. C.C. Farr of New Zealand, a member of the Expedition Advisory Committee. [1]
Antarctica is Earth's southernmost continent. It contains the geographic South Pole and is situated in the Antarctic region of the Southern Hemisphere, almost entirely south of the Antarctic Circle, and is surrounded by the Southern Ocean. At 14,000,000 square kilometres, it is the fifth-largest continent. For comparison, Antarctica is nearly twice the size of Australia. About 98% of Antarctica is covered by ice that averages 1.9 km in thickness, which extends to all but the northernmost reaches of the Antarctic Peninsula.
The Western Base Party was a successful exploration party of the Australasian Antarctic Expedition. The eight-man Western Party was deposited by the Aurora on the Shackleton Ice Shelf at Queen Mary Land. The leader of the team was Frank Wild and the party included the geologist Charles Hoadley.
The Australasian Antarctic Expedition (AAE) was an Australasian scientific team that explored part of Antarctica between 1911 and 1914. It was led by the Australian geologist Douglas Mawson, who was knighted for his achievements in leading the expedition. In 1910 he began to plan an expedition to chart the 3,200-kilometre-long (2,000 mi) coastline of Antarctica to the south of Australia. The Australasian Association for the Advancement of Science approved of his plans and contributed substantial funds for the expedition.
Martin Glacier is a glacier, 3 nautical miles (6 km) wide and 9 nautical miles (17 km) long, which flows west and then northwest from the south side of Mount Lupa to the southeast corner of Rymill Bay where it joins Bertrand Ice Piedmont, on the west coast of Graham Land, Antarctica. It was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under John Riddoch Rymill, and was resurveyed in 1948–1949 by the Falkland Islands Dependencies Survey. The glacier was named for James H. Martin, a member of the British Australian and New Zealand Antarctic Research Expedition (1929–1931) under Sir Douglas Mawson, and first mate of the Penola during the BGLE.
Belgica Mountains is an isolated chain of mountains about 10 miles (16 km) long, standing 60 miles (97 km) east-southeast of the Sor Rondane Mountains in Queen Maud Land, in the Antarctic. The chain was discovered by the Belgian Antarctic Expedition (1957-1958) under Gaston de Gerlache, and named after the ship Belgica, commanded by his father, Lt. Adrien de Gerlache, leader of the Belgian Antarctic Expedition of 1897-99. The Prince de Ligne Mountains stand about 10 mi (16 km) north of the Belgica Mountains.
The Bay of Winds is a coastal embayment between Cape Dovers and Avalanche Rocks in Antarctica. It was discovered by the Western Base Party of the Australasian Antarctic Expedition, 1911–14, under Mawson, who so named it because of the almost constant outflow of cold dense air from the plateau into the bay.
Denman Glacier is a glacier 7 to 10 nautical miles wide, descending north some 70 nautical miles, which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Sir Douglas Mawson. Mawson named the glacier for Lord Denman, Governor-General of Australia in 1911, a patron of the expedition.
Cape Goodenough is an ice-covered cape marking the west side of the entrance to Porpoise Bay and forming the northernmost projection of Norths Highland in Antarctica. It was discovered by the British Australian New Zealand Antarctic Research Expedition under Douglas Mawson on an airplane flight in January 1931, and was named by Mawson for Admiral Sir William Goodenough, President of the Council of the Royal Geographical Society from 1930 to 1933.
Mawson Peninsula is a high, narrow, ice-covered peninsula on the George V Coast, on the west side of the Slava Ice Shelf, Antarctica, terminating in Cape Hudson. It extends for over 30 nautical miles (56 km) in a northwesterly direction. The peninsula was photographed from the air by U.S. Navy Operation Highjump, 1946–47, and was sketched and photographed by Phillip Law of the Australian National Antarctic Research Expeditions who flew along it to its northern end in February 1959. It was named by the Antarctic Names Committee of Australia for Sir Douglas Mawson.
Seaton Glacier is a glacier 17 miles (27 km) long, flowing southeast into Edward VIII Ice Shelf at the northwest part of Edward VIII Bay. It was mapped by Norwegian cartographers from aerial photos taken by the Lars Christensen Expedition, 1936–37, remapped, 1954–58, by ANARE and named by ANCA in 1958 for Flight Lt. John Seaton, RAAF, pilot with ANARE at Mawson in 1956.
The Scott Mountains are a large number of isolated peaks lying south of Amundsen Bay in Enderby Land of East Antarctica, Antarctica. Discovered on 13 January 1930 by the British Australian New Zealand Antarctic Research Expedition (BANZARE) under Sir Douglas Mawson. He named the feature Scott Range after Captain Robert Falcon Scott, Royal Navy. The term mountains is considered more appropriate because of the isolation of its individual features.
Mount Abbs is, at 7,005 feet (2,135 m), the most prominent peak in the central part of Aramis Range, Prince Charles Mountains, situated just west of Thomson Massif. Discovered by ANARE southern party led by W.G. Bewsher in December 1956. Named by ANCA after Gordon Abbs, radio operator at Mawson Station in 1956.
Commandant Charcot Glacier is a prominent glacier about 3 nautical miles (6 km) wide and 12 nautical miles (22 km) long, flowing north-northwest from the continental ice to its terminus at the head of Victor Bay. It was delineated from aerial photographs taken by U.S. Navy Operation Highjump, 1946–47. The French Antarctic Expedition, 1950–1952, under Mario Marret sledged west along the coast to Victor Bay, close east of this glacier, in December 1952, and it was named by them for the polar ship Commandant Charcot which transported French expeditions to this area, 1948–1952.
The Davis Peninsula is an elongated ice-covered peninsula, 3 nautical miles (6 km) wide, between Reid Glacier and Northcliffe Glacier. It was discovered in November 1912 by the Australasian Antarctic Expedition under Mawson, who named it for Captain John King Davis.
Junction Corner is the junction point of the mainland with the west side of Shackleton Ice Shelf. It was discovered and named by the Australasian Antarctic Expedition, 1911–14, under Mawson.
East Budd Island is the eastern of two larger islands at the north end of the Flat Islands in Holme Bay, Mac. Robertson Land. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, who named the northern islands "Flatoynalane". This island was named by the Antarctic Names Committee of Australia for Dr. G.M. Budd, a medical officer at Mawson Station in 1959.
Cape Gray is a rocky cape which forms the east side of the entrance to Commonwealth Bay, part of the George V Coast of Antarctica. The cape is actually a small rocky island which is joined to the icecap of the mainland by an ice ramp. It was discovered by the Australasian Antarctic Expedition (1911–14) under Douglas Mawson, who named it for Percival Gray, second officer on the expedition ship Aurora.
Cape Moyes is an ice-covered headland fronting on the Shackleton Ice Shelf, 18 nautical miles (33 km) west of Cape Dovers. It was discovered by the Australasian Antarctic Expedition (AAE) under Mawson, 1911–14, and named by him for Morton H. Moyes, meteorologist with the AAE Western Base party.
Melba Peninsula is a broad, ice-covered peninsula between Reid Glacier and the Bay of Winds, fronting on Shackleton Ice Shelf, Antarctica. It was discovered by the Australasian Antarctic Expedition under Mawson, 1911–14, who named it for Dame Nellie Melba of Melbourne, a patron of the expedition.
Helen Glacier Tongue is a glacier tongue which extends seaward from Helen Glacier on the coast of Antarctica. It was discovered in November 1912 by the Western Base Party of the Australasian Antarctic Expedition under Mawson, and is named after Helen Glacier.
Kista Strait is a strait between the Flat Islands and Jocelyn Islands in Holme Bay, Mac. Robertson Land, Antarctica. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37. The strait was first navigated by the site on which Australian National Antarctic Research Expeditions (ANARE) established Mawson Station.
Cape Margerie is a low, ice-covered cape in Antarctica, marked by prominent rock outcrops at its northern end, lying midway between Cape Mousse and Lacroix Nunatak and bounded on the north by numerous rocky islands. It was charted by the Australasian Antarctic Expedition under Mawson, 1911–14, who named this feature for Emmanuel de Margerie, a French geographer and geologist.
Mount Keyser is a mountain 3 nautical miles (6 km) east of Mount Ryder, in the eastern part of the Tula Mountains in Enderby Land, Antarctica. It was plotted from air photos taken from Australian National Antarctic Research Expeditions aircraft in 1957, and was named by the Antarctic Names Committee of Australia for D.O. Keyser, a radio officer at Mawson Station in 1961.
The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.
The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.
Coordinates: 66°35′S94°23′E / 66.583°S 94.383°E
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
This Queen Mary Land location article is a stub. You can help Wikipedia by expanding it. |