Сульцбергер мұзжазығы және маңыздағы географиялық нысандар

Sulzberger Ice Shelf is an ice shelf about long and wide bordering the coast of Marie Byrd Land between Edward VII Peninsula and Guest Peninsula in Antarctica.

The Sulzberger Ice Shelf was observed and roughly mapped by the Byrd Antarctic Expedition (ByrdAE; 1928 30), which applied the name Sulzberger Bay to the open water indenting this feature. The United States Advisory Committee on Antarctic Names (US ACAN) extended the name Sulzberger to the adjacent ice shelf.

The landward side of the Sulzberger Ice Shelf extends southeast from Howard Heights and the mouth of the Stewart Glacier to McKinley Peak. From there it runs northeast past the Hershey Ridge and the Court Ridge, past the mouths of the Hammond Glacier, Swope Glacier, Boyd Glacier and Arthur Glacier to the Denfeld Mountains. It then runs north past the mouth of the Crevasse Valley Glacier and northwest along the southern edge of the Guest Peninsula. The seaward side extends in a generally northeast direction from the tip of the Reeves Peninsula to the tip of the Guest Peninsula. The seaward side forms the shore of Sulzberger Bay. The islands of the Marshall Archipelago are scattered throughout the ice shelf.

. A snow covered coastal promontory high between Stewart Glacier and Gerry Glacier on the north side of Edward VII Peninsula. Features in this area were explored by the ByrdAE, 1928 30 and 1933 35. These heights were mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photos, 1959 65. Named by US ACAN (at the suggestion of Admiral Richard E. Byrd) for Roy W. Howard of the ScrippsHoward newspapers, who made financial contributions to the ByrdAE, 1933 35.

. A glacier on the north side of Edward VII Peninsula, flowing northeast along, the east side of Howard Heights into Sulzberger Ice Shelf. Mapped by USGS from surveys and United States Navy air photos, 1959 65. Named by US ACAN for Lieutenant Commander Wayne B. Stewart, United States Navy, co pilot in LC 130F Hercules aircraft during Operation Deep Freeze 1968.

. A peak standing west of Hershey Ridge at the south end of the Ford Ranges. Discovered on the ByrdAE flight of December 5, 1929. Named by Byrd for Grace McKinley, wife of Captain Ashley C. McKinley, aerial photographer and third in command of the expedition.

. Glacier on the northeast side of the Haines Mountains, flowing northwest for about to Sulzberger Ice Shelf in the Ford Ranges. Discovered in 1934 by the ByrdAE, and named by Byrd for John Hays Hammond, American mining engineer and philanthropist.

. A glacier long, flowing eastward from the Haines Mountains along the south side of Keyser Nunatak to enter the Hammond Glacier. Mapped by USGS from surveys and United States Navy air photos, 1959 65. Named by US ACAN for Donald K. Reynolds, ionospheric physicist at Byrd Station, 1967 68 season.

. A glacier which drains westward from the Ford Ranges, between Mount Woodward and Mount West, into Sulzberger Ice Shelf. Features in these ranges were discovered and successively mapped by the ByrdAE (1928 30) and (1933 35) and by the USAS (1939 41) all led by R. Admiral R. E. Byrd. The glacier is named for Gerard Swope, president of General Electric, who contributed various types of electrical equipment to the ByrdAE (1933 35).

. Heavily crevassed glacier flowing west northwest for about to the Sulzberger Ice Shelf between Bailey Ridge and Mount Douglass in the Ford Ranges. Discovered on aerial flights of the ByrdAE in 1934, and named for Vernon D. Boyd, expedition machinist, and a member of West Base of the USAS (1939–41).

. Valley glacier about long, flowing west to Sulzberger Ice Shelf between the Swanson Mountains on the north and Mount Rea and Mount Cooper on the south, in the Ford Ranges. Discovered by members of West Base of the US AS, in aerial flights and from ground surveys in November December 1940. Named by US SCAN for R. Admiral Arthur C. Davis, United States Navy, a leader in aviation in the United States Navy.

. A broad glacier about long, flowing west southwest between Chester Mountains and Saunders Mountain. Discovered by a sledging party of the ByrdAE, which visited this area in November December 1934, and so named because of its extensively crevassed surface.