A large ice-filled inlet at the mouth of Lennox-King Glacier, opening to the Ross Ice Shelf just southeast of Lewis Ridge.

Named by the NZGSAE (1959–60) for R. W. Richards, a member of the Ross Sea Party of the Imperial Trans-Antarctic Expedition (1914–17), who assisted in laying depots as far south as Mount Hope for Shackleton's proposed crossing of Antarctica.

A prominent wedge-shaped rock bluff on the west side of Lennox-King Glacier, 4 miles (6.4 km) southeast of Mount Allen Young.

Rock samples were collected at the bluff by John Gunner and Henry Brecher of the Ohio State University Geological Expedition, 1969-70.

A glacier about 10 miles (16 km) wide between the south end of Queen Elizabeth Range and the MacAlpine Hills, gradually descending east-north-east from the polar plateau to Bowden Névé.

A névé, about 350 square miles (910 km2) in area, bounded by the Marshall Mountains, Lewis Cliff and Mount Sirius.

A glacier, 9 miles (14 km) long, flowing westward from Mount Kirkpatrick in Queen Alexandra Range to enter Walcott Neve north of Fremouw Peak.

A glacier, 6 miles (9.7 km) long, flowing west from Grindley Plateau in Queen Alexandra Range, just north of Lamping Peak.

Named by US-ACAN for Lt. Charles E. Fegley, III, CEC, USN, officer in charge of the nuclear power unit at McMurdo Station during OpDFrz, 1964.

A glacier, 15 miles (24 km) long, descending the east slopes of Holland Range between Lewis Ridge and Mount Tripp to enter Richards Inlet.

A glacier, 15 miles (24 km) long, descending eastward from Holland Range between Vaughan Promontory and Lewis Ridge to the Ross Ice Shelf.

John A. Morton, officer in charge of USN Squadron VX-6 Detachment ALFA, which wintered at McMurdo Station, 1964.

So named by NZGSAE (1961–62) because it contains outcrops of ancient moraine (tillite), indicative of glacial action in remote Paleozoic times.