Marshall Mountains

A mountain, 2,650 metres (8,690 ft) high, standing between Swinford Glacier and Table Bay, in Queen Alexandra Range.

A peak 2.5 nautical miles (4.6 km; 2.9 mi) east of Mount Wild, at the south end of the Queen Alexandra Range.

The ridge is the site of the only known (1971) Permian peat deposit of Gondwanaland, discovered here by James M. Schopf of the Ohio State University Geological Expedition, 1969-70.

Named for Lieutenant Gerhard E. Skaar, United States Navy, who piloted the helicopter that took Schopf to the locality and subsequent discovery.

A peak 2.5 nautical miles (4.6 km; 2.9 mi) west of Mount Augusta at the southwest extremity of the Queen Alexandra Range.

A small group of isolated nunataks lying about 10 nautical miles (19 km; 12 mi) west of Marshall Mountains, at the south side of Walcott Névé.

So named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961-62) because a blizzard prevented them from reaching it for several days.

A high, elongate, flattish area in the Marshall Mountains, standing 2 nautical miles (3.7 km; 2.3 mi) northwest of Blizzard Peak, from which it is separated by a broad snow col.

The heights are about 2 nautical miles (3.7 km; 2.3 mi) long and rise 550 metres (1,800 ft) high above the surrounding snow surface.

A peak, 2,890 metres (9,480 ft) high, standing 4.5 nautical miles (8.3 km; 5.2 mi) north of Mount Marshall.

Named by US-ACAN for Fred H. Mayeda, United States ArmyRP meteorologist at South Pole Station, 1959.

Named by the Ohio State University Geological Expedition, 1969-70, for Donald N. Peterson, party member who collected basalt lavas from the ridge forpetrologic and paleomagnetic studies.

Marshall Mountains towards the southeast