A mainly ice-free mountain, 1,420 metres (4,660 ft) high, at the east side of Amundsen Glacier, standing 5 nautical miles (9.3 km; 5.8 mi) west of Mount Goodale.

A prominent peak, 1,465 metres (4,806 ft) high, rising on the east flank of Amundsen Glacier, 6 nautical miles (11 km; 6.9 mi) northwest of Mount Goodale.

Mountain, 2,330 metres (7,640 ft) high, standing 5 nautical miles (9.3 km; 5.8 mi) south-southeast of Mount Goodale.

A massive mountain, 3,095 metres (10,154 ft) high, standing 4 nautical miles (7.4 km; 4.6 mi) north-northeast of Mount Vaughan.

First observed and roughly mapped in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould.

The name derives from granite samples collected on the wall at 100 metres (330 ft) high spacing for dating by the fission-track method.

A prominent peak, 3,140 metres (10,300 ft) high, standing 4 nautical miles (7.4 km; 4.6 mi) south-southwest of Mount Griffith on the ridge at the head of Vaughan Glacier.

Named for Norman D. Vaughan, dog driver with the Byrd Antarctic Expedition geological party under Laurence Gould which explored the mountains in this vicinity in December 1929.

The map resulting from the Byrd Antarctic Expedition, 1928–30, applied the name Mount Vaughan to the southern portion of Mount Goodale, but the US-ACAN has modified the original naming to apply to this larger peak which lies 15 nautical miles (28 km; 17 mi) southeastward.

So named by New Zealand Geological Survey Antarctic Expedition 1969–70; the summit is composed of vertical rock slabs, its strange appearance being reminiscent of a castle or citadel.

So named by members of New Zealand Geological Survey Antarctic Expedition who used this route in 1969-70 when the west side of the lower reaches of Scott Glacier were found to be impassable.

During November 1987, the névé was the camp site of the USARP-Arizona State University geological party, which suggested the name.

The name derives from the setting, surrounded by peaks, and from the appearance of Mount Pulitzer, the profile of which is remindful of a dragon.

A prominent mountain, 2,155 metres (7,070 ft) high, standing 7 nautical miles (13 km; 8.1 mi) northeast of Mount Griffith on the elevated platform between Koerwitz and Vaughan Glaciers.

A ridge 2 nautical miles (3.7 km; 2.3 mi) long, rising above the middle of the head of Koerwitz Glacier.

A mountain, 1,930 metres (6,330 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) northeast of Mount Pulitzer, near the west side of Scott Glacier.

Named by US-ACAN for Randy L. Nelson, who made satellite geodesy studies at McMurdo Station, winter party 1965.

A conspicuous rock peak surmounting Taylor Ridge on the west side of Scott Glacier, 4 nautical miles (7.4 km; 4.6 mi) northeast of Mount Pulitzer.

Named by US-ACAN for John H. Taylor, ionospheric physicist with the South Pole Station winter party, 1966.

The peak was climbed on Nov. 28, 1987, by four members of the US ARP-Arizona State University geological party led by Edmund Stump.

A prominent peak, 3,470 metres (11,380 ft) high, standing 2 nautical miles (3.7 km; 2.3 mi) east of Mount Astor in the Hays Mountains.

The application of this name has been shifted in accord with the position assigned on the maps resulting from the second Byrd Antarctic Expedition of 1933–35.

A mostly ice-free mountain rising to 2,490 metres (8,170 ft) high, located 1 nautical mile (1.9 km; 1.2 mi) north-northeast of Mount Colbert and 2 nautical miles (3.7 km; 2.3 mi) northeast of Mount Borcik in the southeast part of Hays Mountains.

A series of peaks on a ridge, located 5 nautical miles (9.3 km; 5.8 mi) southeast of Mount Crockett, extending eastward from Hays Mountains and terminating at Scott Glacier.

[30] This article incorporates public domain material from websites or documents of the United States Geological Survey.