The Horlick Mountains are a mountain range in the Transantarctic Mountains of Antarctica. Some sources indicate that the designation includes the Ohio Range, the Long Hills, and all of the Wisconsin Range, while others suggest that it includes only the eastern portion of the Queen Maud Mountains and the main body of the Wisconsin Range. At one point the designation also included the Thiel Mountains.
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.
El-Sayed Glacier is a glacier about 15 nautical miles long which drains the northeast slopes of Zuncich Hill in Marie Byrd Land. It flows northeast to enter Land Glacier at the south side of Mount Shirley. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1959–65, and was named by the Advisory Committee on Antarctic Names for Sayed Z. El-Sayed, a United States Antarctic Research Program oceanographer on the International Weddell Sea Oceanographic Expeditions, 1967–68 and 1969–70.
Albanus Glacier, also known as Phillips Glacier, is a 25-mile (40 km) long glacier flowing west along the south side of Tapley Mountains to enter Scott Glacier just north of Mount Zanuck, in the Queen Maud Mountains in Antarctica. It was discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. Byrd named it for Albanus Phillips, Jr., president of Phillips Packing in Cambridge, Maryland, a patron of, and supplier of provisions to, his Antarctic expeditions of 1928–30 and 1933–35.
Balchen Glacier is a crevassed glacier in Antarctica, flowing west to Block Bay between the Phillips Mountains and the Fosdick Mountains in Marie Byrd Land. It was discovered on December 5, 1929, by the Byrd Antarctic Expedition and named by Richard E. Byrd for Bernt Balchen, chief pilot of the expedition.
Mount Behling is an ice-covered, flat-topped mountain, 2,190 m, standing between the Steagall and Whitney Glaciers and 5 nautical miles (9 km) north of Mount Ellsworth in the Queen Maud Mountains. First mapped from ground surveys and air photos by the Byrd Antarctic Expedition, 1928-30. Named by Advisory Committee on Antarctic Names (US-ACAN) for Robert E. Behling, United States Antarctic Research Program (USARP) glaciologist on the South Pole—Queen Maud Land Traverse II, summer 1965-66.
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.
Cappellari Glacier is a glacier 11 nautical miles (20 km) long in the Hays Mountains, flowing west from the northwest shoulder of Mount Vaughan to enter Amundsen Glacier just north of Mount Dort. It was first roughly mapped by the Byrd Antarctic Expedition, 1928–30, and remapped by the United States Geological Survey from ground surveys and from U.S. Navy air photos, 1960–64. It was named by the Advisory Committee on Antarctic Names for Lewis K. Cappellari who made ionospheric studies at McMurdo Station in 1965.
The Chester Mountains are a group of mountains just north of the mouth of Crevasse Valley Glacier and 10 nautical miles (20 km) north of Saunders Mountain in the Ford Ranges of Marie Byrd Land. They were mapped by the Byrd Antarctic Expedition (1933–35) and named for Colby M. Chester, president of General Foods Corporation, who gave generous support to the Byrd expeditions.
DeGanahl Glacier is a narrow, steep-walled glacier about 10 nautical miles (20 km) long, flowing southeast from Jones Peak into the western side of Liv Glacier, opposite June Nunatak. It was discovered and photographed by Rear Admiral Byrd on the South Pole Flight in November 1929 and named for Joe deGanahl, a navigator and dog driver and a member of the Supporting Party for the Byrd Antarctic Expedition, 1928–30.
The Grosvenor Mountains are a group of widely scattered mountains and nunataks rising above the Antarctic polar plateau east of the head of Mill Glacier, extending from Mount Pratt in the north to the Mount Raymond area in the south, and from Otway Massif in the northwest to Larkman Nunatak in the southeast. They were discovered by Rear Admiral Richard E. Byrd on the Byrd Antarctic Expedition flight to the South Pole in November 1929, and named by him for Gilbert Hovey Grosvenor, President of the National Geographic Society, which helped finance the expedition. Several peaks near Mount Raymond were apparently observed by Ernest Shackleton in 1908, although they were then considered to be a continuation of the Dominion Range.
Drummond Glacier is a glacier 10 nautical miles (18 km) long and 2 nautical miles (4 km) wide, on the west coast of Graham Land, situated south of Hopkins Glacier and flowing west-northwest between Voit Peak and Sherba Ridge into Darbel Bay east of Sokol Point.
Goodale Glacier is a glacier which flows north from Mount Goodale and Mount Armstrong along the west side of the Medina Peaks, in the foothills of the Queen Maud Mountains of Antarctica. It was first seen and mapped by the Byrd Antarctic Expedition, 1928–30, and was named by the Advisory Committee on Antarctic Names in association with Mount Goodale.
McKinley Nunatak is the southernmost of three large nunataks in upper Liv Glacier, Antarctica, about 5 nautical miles (9 km) north-northeast of Barnum Peak. It was named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (1961–62) for Captain Ashley C. McKinley, a photographer with Rear Admiral Richard E. Byrd on his South Pole flight of 1929.
Hump Passage is a wide gap just southeast of Barnum Peak, through which Liv Glacier emerges from the polar plateau. It was originally referred to as the "Hump" by Rear Admiral Richard E. Byrd and is the pass over which he made his historic South Pole flight of 1929. The feature was observed by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (1961–62) who recommended the perpetuation of a form of the original name.
May Peak is a pyramidal peak rising to over 2,200 metres (7,200 ft) at the west side of Reedy Glacier, standing 1 nautical mile (2 km) west of Stich Peak in the Quartz Hills of Marie Byrd Land. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Robert L. May, a U.S. Navy helicopter pilot at McMurdo Station, 1962–63.
Sargent Glacier is a steep-walled tributary glacier, flowing southeast from the Herbert Range to enter Axel Heiberg Glacier just southeast of Bell Peak. Probably first seen by Roald Amundsen's polar party in 1911, the glacier was mapped by the Byrd Antarctic Expedition, 1928-30. Named by Advisory Committee on Antarctic Names (US-ACAN) for Howard H. Sargent III who made ionospheric studies at the South Pole Station in 1964.
The Howard Heights are a snow-covered coastal promontory, 515 metres (1,690 ft) high, between Stewart Glacier and Gerry Glacier on the north side of Edward VII Peninsula, Antarctica. Features in this area were explored by the Byrd Antarctic Expeditions, 1928–30 and 1933–35. These heights were mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1959–65, and were named by the Advisory Committee on Antarctic Names for Roy W. Howard of the Scripps-Howard newspapers, who made financial contributions to the 1933–35 Byrd expedition.
Mount Thorne is a prominent peak, 1,465 m, rising on the east flank of Amundsen Glacier, 6 nautical miles (11 km) northwest of Mount Goodale, in the Hays Mountains of the Queen Maud Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named for George A. Thorne, topographer and dog driver with that party.
Langford Peak is an isolated peak in Antarctica, 2 nautical miles (4 km) west of the lower part of Reedy Glacier and 5 nautical miles (9 km) northwest of Abbey Nunatak. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1960–63, and was named by the Advisory Committee on Antarctic Names for Lawrence G. Langford, Jr., a builder with the Byrd Station winter party, 1958.
