Features of the southern part include, from west to east, Miller Crag, Sutley Peak, Walk Glacier, Forbidden Rocks and Christoffersen Heights.

[2] The charts of the United States Antarctic Service (USAS), 1939–41, show mountains in this approximate location and relationship to Dustin and Thurston Islands, indicating they were sighted in the flight from the ship Bear, February 27, 1940.

A bold and conspicuous outcropping of bare rock 1,450 metres (4,760 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) west-southwest of Sutley Peak in the west extremity of the Jones Mountains.

Two small rock exposures, visible from northward, situated near the crest of the ice-covered heights between Miller Crag and Sutley Peak.

South-facing cliffs with two prominent rock outcrops, located 2 nautical miles (3.7 km; 2.3 mi) south-southeast of Pillsbury Tower.

A small ridge with bare rock outcroppings located just north of Haskell Glacier and 2 nautical miles (3.7 km; 2.3 mi) south-southwest of Bonnabeau Dome.

They found a large block of ice in the shape of a square prism standing as an isolated feature at the south end of this ridge.

A small glacier descending from Christoffersen Heights and draining west between Prism Ridge and Forbidden Rocks.

Linear rock outcrops, 1 nautical mile (1.9 km; 1.2 mi) long, located on the west edge of Christoffersen Heights and between Haskell and Walk Glaciers.

Broad snow-covered heights which form the south-central portion of the Jones Mountains, southward of Bonnabeau and Anderson Domes.

Named by US-ACAN for Lieutenant Ernest H. Christoffersen, United States Navy Reserve, co-pilot of ski-equipped LC-47 Dakota aircraft on pioneering flights from Byrd Station to the Eights Coast area in November 1961.

So named by the party because the feature presented a right angle profile facing west when viewed from Camp Minnesota (from northward).

A short rock ridge with topographic highs of 1,180 and 1,141 metres (3,871 and 3,743 ft) at the ends, located just west of Pemmican Bluff.

So named by this party because the bluff is composed of complex volcanic rocks giving the north face a very mottled appearance similar to the pemmican eaten in the field.

A remnant volcanic cone, 1,295 metres (4,249 ft) high, with a shear north-facing rock cliff and a gradual slope at the south side, standing directly at the base of Avalanche Ridge.

With its dark rock rising 100 metres (330 ft) high above the surrounding area, it is clearly the most prominent landmark in these mountains.

A rock spur along the north front of the Jones Mountains, 1 nautical mile (1.9 km; 1.2 mi) west of Avalanche Ridge.

A rock spur along the north front of the Jones Mountains, 0.5 nautical miles (0.93 km; 0.58 mi) west of Avalanche Ridge.

Named by US-ACAN for Jerry W. Austin, aviation machinist's mate of United States Navy Squadron VX-6, a crew member on pioneering flights of LC-47 Dakota aircraft from Byrd Station to the Eights Coast area in November 1961.

High rock spur along the north front of the Jones Mountains, immediately east of Austin Valley.

Mapped by the University of MinnesotaJones Mountains Party, 1960-61, and named by them for Wayne B. Hughes, Assistant USARP Representative at McMurdo Station, 1960-61.

A low ice-covered peak lying 1 nautical mile (1.9 km; 1.2 mi) southwest of Anderson Dome.

Named by US-ACAN for David Snyder, aviation electronics technician with United States Navy Squadron VX-6, crew member on pioneer flights of LC-47 Dakota aircraft from Byrd Station to the Eights Coast area in November 1961.

A low ridge with rocky exposures, 1 nautical mile (1.9 km; 1.2 mi) long, which extends from the north side of Anderson Dome.

A point with steep ice-covered slopes which is marked by a rock exposure on the northeast face, located 2 nautical miles (3.7 km; 2.3 mi) west-southwest of the summit of Mount Loweth.

Named by US-ACAN for Staff Sergeant Leroy E. Eubanks, USMC, navigator with United States Navy Squadron VX-6, who participated in pioneering flights of LC-47 Dakota aircraft from Byrd Station to the Eights Coast area in November 1961.

Mapped by the University of Minnesota-Jones Mountains Party, 1960-61, and so named by them because the continual falling of rocks made examination of the area hazardous.

Named by US-ACAN for Hugh F. Loweth, Executive Offices of the President, who for some years was instrumental in the development and guidance of United States science policies and programs for Antarctica.