[1] The Saratoga 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.

[1] Download coordinates as: The Saratoga Table is bounded by the Support Force Glacier to the east and the Median Snowfield to the southwest.

An ice-filled gap connecting the heads of May Valley and Chambers Glacier and marking the divide between Lexington and Saratoga Tables.

Named by US-ACAN for Lieutenant Commander Ronald E. Sorna, United States Navy, pilot on photographic flights in the Pensacola Mountains.

A mountainous snow-covered projection from the east side of Saratoga Table, 5 nautical miles (9.3 km; 5.8 mi) southeast of Sorna Bluff.

Named by US-ACAN in 1979 after Lieutenant Richard M. Hook, United States Navy, Medical Officer at South Pole Station, winter party 1969.

An irregular east-facing cliff, 4 nautical miles (7.4 km; 4.6 mi) long, located at the extremity of a spur trending eastward from Saratoga Table.

Named by US-ACAN in 1979 for Oscar C. Vigen, Budget and Planning Officer, Division of Polar Programs, National Science Foundation, 1968–85.

Named by US-ACAN in 1979 after Steven D. Sheriff, geologist, Western Washington State University, Bellingham, WA, who worked in this area, 1978–79.

A bluff 2 nautical miles (3.7 km; 2.3 mi) northeast of Mount Stephens on the west side of Saratoga Table.

A rock spur along the west side of Saratoga Table, 3 nautical miles (5.6 km; 3.5 mi) north of Mount Stephens.

At the suggestion of USGS party leader Arthur B. Ford, named by US-ACAN after Russell F. Burmester, geologist, Western Washington State University, Bellingham, WA, who worked in the Forrestal Range, 1978–79.

A linear group of hills with prominent rock outcrops, 11.5 nautical miles (21.3 km; 13.2 mi) long, at the southwest end of Saratoga Table.

Ford (1973–91) on the petrology of Antarctica and specifically on the Dufek intrusion of the northern Pensacola Mountains was critical for the understanding of the evolution of this major igneous complex.

An elongate nunatak, 1,710 metres (5,610 ft) high, standing 2.5 nautical miles (4.6 km; 2.9 mi) west of Dyrdal Peak in southern Forrestal Range.

A prominent nunatak lying 4 nautical miles (7.4 km; 4.6 mi) southeast of Fierle Peak at the south end of Forrestal Range, Pensacola Mountains.