[1] The Lexington Table was discovered and photographed on January 13, 1956 on a transcontinental nonstop flight by personnel of United States Navy Operation Deep Freeze I from McMurdo Sound to the vicinity of the Weddell Sea and return.

A mostly snow-covered escarpment that runs north–south for 4 nautical miles (7.4 km; 4.6 mi) and forms the northeast edge of Lexington Table.

A rock, 1,020 metres (3,350 ft) high, situated just off the east edge of Lexington Table, 6 nautical miles (11 km; 6.9 mi) north of Mount Zirzow.

Named by US-ACAN in 1979 after Keith D. Ritala, USARP geophysicist who conducted gravity research at South Pole Station, winter party 1972.

A mountain, 1,615 metres (5,299 ft) high, standing 4 nautical miles (7.4 km; 4.6 mi) north of Mount Mann on the east edge of Lexington Table.

A mountain, 1,680 metres (5,510 ft) high, standing on the southeast edge of Lexington Table, 4 nautical miles (7.4 km; 4.6 mi) south of Mount Zirzow.

Named in 1979 by US-ACAN after Raymond D. Watts, USGS geophysicist who worked in the Forrestal Range and Dufek Massif, 1978-79.

Rock crags on the ice slope between Henderson Bluff and Mount Lechner on the west side of Lexington Table.

A rock bluff, 1,660 metres (5,450 ft) high, along the west side of Lexington Table 9 nautical miles (17 km; 10 mi) north of Mount Lechner, in the Forrestal Range, Pensacola Mountains.

A prominent nunatak, 1,630 metres (5,350 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) southwest of Mount Lechner.

Discovered and photographed on January 13, 1956 during a United States Navy transcontinental nonstop plane flight from McMurdo Sound to Weddell Sea and return.

Named by US-ACAN for Hartford E. Blount, aviation machinists mate with United States Navy Squadron VX during Operation Deep Freeze, 1956.

Named by US-ACAN at the suggestion of Arthur B. Ford for Gunars Abele, civil engineer on the 1973-74 USARP-CRREL survey in this area.