[1] The main trunk of the Mulock Glacier is about 60 kilometres (37 mi) long and drops about 800 metres (2,600 ft) from the edge of the East Antarctic Ice Sheet to its grounding line at its mouth.

[3] Hughes et al. (2017) consider that the East Antarctic outlet glaciers act as "nails" holding the Ross Ice Shelf in place.

It flows southeast past Mount Marvel to the north and the Henry Mesa to the south.

So named by the New Zealand party of the Commonwealth Trans-Antarctic Expedition (CTAE) (1956–58) because it appears to lead directly into Skelton Névé but instead drains south ward.

Glacier flowing from the southeast slopes of the Worcester Range to the Ross Ice Shelf, west of Cape Timberlake.

Named by US-ACAN in 1964 for Sveneld A. Evteev, glaciologist and Soviet exchange observer at McMurdo Station in 1960.

A conspicuous rock bluff along the south wall of Mulock Glacier, about 9 nautical miles (17 km; 10 mi) NW of Cape Lankester.

Alexander Anthony, USAF, in charge of science and publications on the staff of the U.S. Antarctic Projects Officer, 1963–65.

Prominent rock cliff 2 nautical miles (3.7 km; 2.3 mi) long, just northward of Cape Lankester at the mouth of Mulock Glacier.

A high, rounded, snow-covered cape at the south side of the entrance to Mulock Inlet, along the west edge of the Ross Ice Shelf.

Probably named for Sir Edwin Ray Lankester, Director of the Natural History Department of the British Museum (1898–1907) and founder of the Marine Biological Association in 1884.

The feature is occupied by lower Mulock Glacier which drains through it to the Ross Ice Shelf.