The Queen Elizabeth Range is a rugged mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica.
Alexandra Mountains is a group of low, separated mountains in the north portion of Edward VII Peninsula, just southwest of Sulzberger Bay in Marie Byrd Land, Antarctica. Discovered in January–February 1902 by the British National Antarctic Expedition during an exploratory cruise of the Discovery along the Ross Ice Shelf. Named for Alexandra, then Queen of the United Kingdom.
The Wisconsin Range is a major mountain range of the Horlick Mountains in Antarctica, comprising the Wisconsin Plateau and numerous glaciers, ridges and peaks bounded by the Reedy Glacier, Shimizu Ice Stream, Horlick Ice Stream and the interior ice plateau.
Marie Byrd Land is the portion of West Antarctica lying east of the Ross Ice Shelf and the Ross Sea and south of the Pacific Ocean, extending eastward approximately to a line between the head of the Ross Ice Shelf and Eights Coast. It stretches between 158°W and 103°24'W. The inclusion of the area between the Rockefeller Plateau and Eights Coast is based upon the leading role of the American Rear Admiral Richard E. Byrd in the exploration of this area. The name was originally applied by Admiral Byrd in 1929, in honor of his wife, to the northwestern part of the area, the part that was explored in that year.
The Prince Olav Mountains is a mountain range of the Queen Maud Mountains stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf.
The Ford Ranges is a grouping of mountain ranges standing east of Sulzberger Ice Shelf and Block Bay in the northwest part of Marie Byrd Land, Antarctica. Discovered by the Byrd Antarctic Expedition on December 5, 1929, and named by Byrd for Edsel Ford of the Ford Motor Company, who helped finance the expedition.
Barcus Glacier is a glacier in the Hutton Mountains that drains east-southeast, to the north of Mount Nash and Mount Light, into Keller Inlet in Palmer Land. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy air photos, 1961–67, and named by the Advisory Committee on Antarctic Names for James R. Barcus, ionospheric physics researcher at Byrd Station in the summers of 1966–67 and 1967–68.
Beck Peak is a peak, 2,650 metres (8,700 ft) high, on the east flank of Amundsen Glacier, standing 2 nautical miles (4 km) northwest of Mount Stubberud on the ridge descending from the northern Nilsen Plateau, Queen Maud Mountains. This peak appears to have been first mapped from air and ground photos taken by the Byrd Antarctic Expedition, 1928–30. It was mapped in greater detail by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–64. The peak was named by the Advisory Committee on Antarctic Names for Andreas Beck, a crew member and ice pilot on Amundsen's South Pole expedition of 1910–12. This naming preserves the spirit of Roald Amundsen's 1911 commemoration of "Mount A. Beck", a name applied by him for a mountain situated at 87°20′S148°0′E.
The Gothic Mountains is a group of mountains, 32 kilometres (20 mi) long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier, Albanus Glacier, and Griffith Glacier. The mountains were first visited in December 1934 by the Byrd Antarctic Expedition (ByrdAE) geological party led by Quin Blackburn. The name was proposed by Edmund Stump, leader of a U.S. Antarctic Research Program (USARP) - Arizona State University geological party which made investigations here in the 1980-81 season. The mountains are composed of granites which have weathered to produce a series of spires and peaks reminiscent of a Gothic cathedral.
Webber Island is the large central island of the White Islands in southern Sulzberger Bay. It is rudely delineated on the map of the Byrd Antarctic Expedition, 1928–30, and indicated as "low ice cliffs" that rise above the ice shelf in this part of the bay. Mapped in detail by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1959-65. Named for James Webber, United States Antarctic Research Program (USARP) ionospheric physicist at Byrd Station, 1968-69 season.
Crosswell Glacier is a glacier 10 nautical miles long, flowing north-northeast from Mount Shinn between Sullivan Heights and Bearskin Ridge, in the central part of the Sentinel Range, Ellsworth Mountains, Antarctica. Together with Patton and Pulpudeva Glaciers, it enters Ellen Glacier northwest of Mamarchev Peak and southeast of Mount Jumper.
Mount Kohler is a mountain, 480 metres (1,570 ft) high, on the south side of Boyd Glacier located 4 nautical miles (7 km) east of Mount Woodward in the Ford Ranges of Marie Byrd Land, Antarctica. It was mapped by a 1939–41 United States Antarctic Service expedition led by Richard Evelyn Byrd, and was named for Herbert V. Kohler, Jr. and Ruth DeYoung Kohler II, son and daughter of Herbert V. Kohler, a financial contributor to the Byrd Antarctic Expedition, 1933–35.
Mount Early is a solitary volcanic cone, 2,720 metres (8,920 ft) high, standing 13 nautical miles (24 km) north of D'Angelo Bluff, on the west side and near the head of Scott Glacier. It was discovered in December 1934 from nearby Mount Weaver by the Byrd Antarctic Expedition geological party led by Quin Blackburn. It was visited by the Ohio State University geological party led by George Doumani on November 21, 1962, and was named by the Advisory Committee on Antarctic Names after Captain Neal E. Early, US Army, a member of the aviation unit that supported the United States Geological Survey Topo East survey of this area, 1962–63.
Mount McCormick is a mountain 2 nautical miles (4 km) southeast of Mount Ralph in the Ford Ranges of Marie Byrd Land, Antarctica. It was discovered and mapped by the United States Antarctic Service (1939–41), and was named by the Advisory Committee on Antarctic Names for W.S. McCormick, an airplane pilot with the Byrd Antarctic Expedition (1933–35).
Mount Howe is an elongated mountain in Antarctica, 2,930 metres (9,600 ft) high, comprising low connecting ridges and gable-shaped nunataks. It rises at the east side of Scott Glacier, near the head, directly opposite Mount McIntyre. This mountain, including its small southern outlier, apparently is the southernmost mountain in the world. It was discovered in December 1934 by the Byrd Antarctic Expedition geological party led by Quin Blackburn, and was named by Admiral Byrd for Louis McHenry Howe, secretary to the President of the United States at that time, Franklin D. Roosevelt.
Hodgson Nunatak is a nunatak which lies 5 nautical miles (9 km) south of Teeters Nunatak and 20 nautical miles (37 km) northwest of Mount Moses in the Hudson Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–66, and named by the Advisory Committee on Antarctic Names for Ronald A. Hodgson, U.S. Navy, a builder with the Byrd Station party, 1966.
Mount Manger is a snow-covered mountain located 3 nautical miles (6 km) northwest of Mount Josephine in the Alexandra Mountains, on King Edward VII Peninsula, Antarctica. The mountain was photographed from the air and roughly mapped by the Byrd Antarctic Expedition, 1928–30, and was named by the Advisory Committee on Antarctic Names for William Manger, of the family that owned the Manger Hotel chain, who assisted Byrd expeditions by providing free room for office space and for expedition personnel.
Souchez Glacier is a tributary glacier about 17 nautical miles (31 km) long, flowing from Mount Crockett south along the east side of Faulkner Escarpment and then turning southeast to parallel the southwest side of Hays Mountains. It joins Bartlett Glacier just south of Mount Dietz, in the Queen Maud Mountains. Named by Advisory Committee on Antarctic Names (US-ACAN) for Roland A. Souchez, involved in geological studies at McMurdo Station during the season of 1965-66.
The La Gorce Mountains are a group of mountains, spanning 20 nautical miles (37 km), standing between the tributary Robison Glacier and Klein Glacier at the east side of the upper reaches of the Scott Glacier, in the Queen Maud Mountains of Antarctica. They were discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named by Richard E. Byrd for John Oliver La Gorce, Vice President of the National Geographic Society.
