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.

Southern Party of the CTAE (1956–58) and named for Charles M. Bowden, Chairman of the Ross Sea Committee which organized the N.Z.

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.

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