The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being 200 km (125 mi) long and having a width of 40 km (25 mi). It descends about 2,200 m (7,200 ft) from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western.
Ben J. Bussey is an American planetary scientist.
Lambert Glacier is a major glacier in East Antarctica. At about 60 miles (100 km) wide, over 250 miles (400 km) long, and about 2,500 m deep, it holds the Guinness world record for the world's largest glacier. It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf. It flows in part of Lambert Graben and exits the continent at Prydz Bay.
Mertz Glacier is a heavily crevassed glacier in George V Coast of East Antarctica. It is the source of a glacial prominence that historically has extended northward into the Southern Ocean, the Mertz Glacial Tongue. It is named in honor of the Swiss explorer Xavier Mertz.
Murgash Glacier is the 3.4 km long and 3.2 km wide glacier on Greenwich Island in the South Shetland Islands, Antarctica situated southeast of Yakoruda Glacier, south of Teteven Glacier, southwest of Traub Glacier and west-northwest of Bravo Glacier. It is bounded by Lloyd Hill on the northwest, Tile Ridge on the east and Hebrizelm Hill on the southeast, and drains southwards into Kramolin Cove in McFarlane Strait between Yovkov Point and Kaspichan Point.
The Scott Glacier is a major glacier, 120 miles (190 km) long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east.
Schweitzer Glacier is a glacier which drains west along the north side of Littlewood Nunataks into Vahsel Bay. The Lerchenfeld Glacier, trending west-northwestward, coalesces with the lower portion of this glacier. Discovered by the German Antarctic Expedition, 1911–12, under Wilhelm Filchner. He named it for Major Schweitzer, first president of the German Antarctic Expedition Society.
Falkner Glacier, is an east-flowing valley glacier, 4 nautical miles long, located 2 nautical miles south of Oakley Glacier in the Mountaineer Range, Victoria Land, Antarctica. The glacier descends steeply to Lady Newnes Bay where it forms a floating glacier tongue. It was named by the Advisory Committee on Antarctic Names (2008) after Kelly K. Falkner, Professor of Chemical Oceanography at Oregon State University, who served from 2006 as the first Program Director for the Antarctic Integrated System Science Program in the Division of Antarctic Sciences, Office of Antarctic Programs, National Science Foundation.
Djerassi Glacier is a 2.8 km long and 1 km wide steep valley glacier situated south of Gorichane Glacier, west of the head of Malpighi Glacier, northwest of the head of Mackenzie Glacier, and north-northeast of Pirogov Glacier on Brabant Island in the Palmer Archipelago, Antarctica. It drains the west slopes of Harvey Heights and the north slopes of Mount Parry, and flows northwestwards into Lanusse Bay north of Venchan Peak.
Pirogov Glacier is a 5 km long and 1.5 km wide glacier situated south of Djerassi Glacier, west of the head of Mackenzie Glacier and northwest of Balanstra Glacier on Brabant Island in the Palmer Archipelago, Antarctica. It drains the south-southwest slopes of Mount Parry and flows westwards to enter Dallmann Bay south of Minot Point.
Rippon Glacier is a small glacier located in Kemp Land, East Antarctica. It is close east of Seaton Glacier, flowing southward into Edward VIII Ice Shelf.
Wilma Glacier is the western of two glaciers entering the southern part of Edward VIII Ice Shelf in Kemp Land, East Antarctica. The second, eastern glacier is Robert Glacier.
Gildea Glacier is a glacier 10 kilometres (6 mi) long and 5 kilometres (3 mi) wide flowing southwestward from Craddock Massif between Mount Slaughter and Mount Atkinson into Nimitz Glacier, in the Sentinel Range of the Ellsworth Mountains, Antarctica. The upper portion of the glacier also receives ice from Hammer Col and southern Vinson Massif.
Bally Glacier is a glacier 6 nautical miles (11 km) long which occupies the central part of the Carlstrom Foothills of the Churchill Mountains. It flows north along the east side of Mount Blick into Jorda Glacier. It was named by the Advisory Committee on Antarctic Names after John Bally of the University of Colorado Center for Astrophysics and Space Astronomy, Boulder, CO; he was a United States Antarctic Program principal investigator and field team member of the Advanced Telescope Project, South Pole Center for Astrophysical Research in Antarctica, 1992–95.
Bartley Glacier is a hanging glacier on the south wall of Wright Valley in the Asgard Range of Victoria Land, just west of Meserve Glacier. It was named by the Advisory Committee on Antarctic Names for construction driver Ollie B. Bartley, U.S. Navy, who was killed on January 14, 1957 when the vehicle (weasel) he was driving dropped through the sea ice at Hut Point, McMurdo Sound.
Butamya Glacier is the 6.9 km long and 2.5 km wide glacier on Barison Peninsula, Graham Coast on the west side of Antarctic Peninsula, situated northwest of Talev Glacier and north-northeast of Chernomen Glacier. It drains northwards, and flows into Beascochea Bay.
Bussey Glacier is a glacier flowing west from Mount Peary to the head of Waddington Bay on Kiev Peninsula on the west coast of Graham Land. It was first charted by the French Antarctic Expedition under Jean-Baptiste Charcot, 1908–10, and named by the UK Antarctic Place-Names Committee in 1959 for Group Captain John Bussey of the Directorate of Overseas Surveys.
Français Glacier is a glacier 4 nautical miles (7 km) wide and 12 nautical miles (22 km) long, flowing north-northeast from the continental ice to the Antarctic coast close west of Ravin Bay. Though no glaciers were noted on Captain Jules Dumont d'Urville's chart of this coast, the close correlation of his "Baie des Ravins" feature and narrative description with the indentation of the coast near the mouth of this glacier suggests first sighting of this feature by the French Antarctic Expedition, 1837–40. During December 1912 members of the Main Base Party of the Australasian Antarctic Expedition (AAE) camped on the upland slopes close east of the glacier, but no reference was made to the glacier in the AAE reports, though a clear view and unpublished sketch were obtained of the distant coast to the northwest.
Ashworth Glacier is an Antarctic glacier with sharply delineated sides, flowing west from Supporters Range into Mill Glacier, 5 kilometres (3 mi) north of Mount Iveagh. It was named by the Advisory Committee on Antarctic Names in 2007, after Allan C. Ashworth, Professor of Paleontology and Stratigraphy at North Dakota State University. He discovered the only yet known fly and beetle fossils in Antarctica in the nearby Dominion Range.
