Mount Joyce is south of David Cauldron in the David Glacier and east of Hollingsworth Glacier.
The Ricker Hills lie to the west.
Nearby features include Burrage Dome to the northeast, Mount Mallis, Mount Howard, Mount Billing and Mount Bowen to the southeast, and Crash Nunatak and Ford Peak to the southwest.[1]
Geology
Mount Joyce, along with nearby nunataks, such as the Trio Nunataks, represents the remnants of a tableland of the Jurassic Ferrar Group, which consists of Kirkpatrick lavas and Ferrar doleritesills, alternating with rafts of sandstone of the Paleozoic and MesozoicBeacon Supergroup. The strata dip about 1-2 degrees (at most) to the west. On Mount Joyce only three major dolerite sills are observed, with two thin interleaving seams of Beacon sediments.[3]
75°40′S160°48′E / 75.667°S 160.800°E / -75.667; 160.800.
A mountain, 1,360 metres (4,460 ft) high, midway between Mount Joyce and Mount Billing in the Prince Albert Mountains, Victoria Land.
Mapped by USGS from surveys and United States Navy air photos, 1956-62.
Named by US-ACAN for Robert R. Mallis, geomagnetist/seismologist with the South Pole Station winter party, 1966.[5]
75°45′S161°03′E / 75.750°S 161.050°E / -75.750; 161.050.
A mountain of stratified sandstone capped by a sharp black peak, 1,875 metres (6,152 ft) high, standing 6 nautical miles (11 km; 6.9 mi) southwest of Mount Howard.
Discovered by the BrNAE, 1901-04, which named it for the Honorable C.C. Bowen, one of the men who gave the expedition much assistance in New Zealand.[8]
75°43′S160°27′E / 75.717°S 160.450°E / -75.717; 160.450.
A rock peak, 1,830 metres (6,000 ft) high, standing 6.5 nautical miles (12.0 km; 7.5 mi) west of Mount Billing.
Named by the Southern Party of NZGSAE, 1962-63, for M.R.J. Ford, asst. surveyor with that party, who had wintered over at Scott Base in 1962.[10]
Mount Joyce, USGS: United States Geographic Board, retrieved 2024-02-29
Worner, G. (1992), "Kirkpatrick Lavas, Exposure Hill Formation and Ferrar Sills in the Prince Albert Mountains, Victoria Land, Antarctica", Polarforschung, 60: 87–90