Features of the glacier, its tributaries and the terrain through which they flow include:
Mount Kring . A sharply defined nunatak on the northern margin of the upper reaches of David Glacier, southwest of Mount Wood. Previously uncharted, it was used (with Mount Wood) as a reference for establishing a
United States Antarctic Research Program (USARP) field party on Nov. 6, 1962. Named by D.B.McC. Rainey of the Cartographic Branch of the New Zealand Dept. of Lands and Survey for Staff Sergeant Arthur L. Kring, USMC, navigator on many United States Navy VX-6 Squadron flights during the 1962–63 season when New Zealand field parties received logistic support by that squadron.
Mount Wood . An isolated nunatak lying northward of David Glacier and northeast of Mount Kring. Named by D.B. McC. Rainey of the Cartographic Branch of the New Zealand Dept. of Lands and Survey. Named after the foster parents of Staff Sgt. Arthur L. Kring, USMC, navigator with the United States Navy VX-6 Squadron which provided logistic support for the NZGSAE (1962–63).
Martin Nunataks . Two isolated nunataks situated along the northern margin of David Glacier, southeast of Mount Wood. Mapped by the
United States Geological Survey (USGS) from surveys and United States Navy air photos, 1956–62. Named by the United States
Advisory Committee on Antarctic Names (US-ACAN) for Robert D. Martin, USGS topographic engineer at McMurdo Station, 1961–62.
Hollingsworth Glacier . A broad glacier of low gradient, draining the vicinity east of the
Ricker Hills and flowing northeast to enter David Glacier just east of Trio Nunataks. Mapped by USGS from surveys and United States Navy air photos, 1956–62. Named by US-ACAN for Jerry L. Hollingsworth, meteorologist with the South Pole Station winter party, 1966.
David Cauldron . An icefall of turbulent iceblocks on the David Glacier. Named by the Southern Party of the NZGSAE, 1962–63, in association with David Glacier.
Woodberry Glacier . A small tributary glacier flowing south between Evans Heights and Mount Fearon to the north side of David Glacier. Mapped by USGS from surveys and United States Navy air photos, 1956–62. Named by US-ACAN for Barry D. Woodberry, ionospheric physicist with the South Pole Station winter party, 1966.
D'Urville Wall . A great glacier-cut wall of granite which rises to high and forms the north wall of David Glacier near its terminus. Discovered by the
British Antarctic Expedition, 1907–09, under Shackleton. He named this feature for Admiral Jules Dumont d'Urville.
Cape Philippi . A rock cape rising abruptly to high along the coast of Victoria Land, marking the north side of the terminus of David Glacier. Discovered by the British Antarctic Expedition, 1907–09, under Shackleton, who named this feature for Emil Philippi, distinguished geologist, who was a member of the GerAE, 1901–03, under Drygalski.
Hughes Bluff . A conspicuous rock and ice bluff, high, along the south side of David Glacier, west of Cape Reynolds. Mapped by USGS from surveys and United States Navy tricamera aerial photography, 1957–62. Named by US-ACAN for Garrett A. Hughes, USARP researcher (cosmic radiation) at McMurdo Station in 1966.
Cape Reynolds . A rocky cape marking the south side of the terminus of David Glacier. Discovered by the British Antarctic Expedition, 1907–09, under Shackleton, who probably named this feature for Jeremiah (John) N. Reynolds, an American who long agitated for exploration of the Antarctic, and who was one of the principal promoters of the United States Exploring Expedition, 1838–42.
Geikie Inlet . An inlet along the coast of Victoria Land, formed between the cliffs of the Drygalski Ice Tongue on the north and
Lamplugh Island and the seaward extension of
Clarke Glacier on the south. Discovered by the
British National Antarctic Expedition, 1901–04, under Scott, who named it after Sir Archibald Geikie, who gave much assistance in preparing the expedition. ==References==