Mount Rendu is a mountain

Mountain

Image:Himalaya_annotated.jpg|thumb|right|The Himalayan mountain range with Mount Everestrect 58 14 160 49 Chomo Lonzorect 200 28 335 52 Makalurect 378 24 566 45 Mount Everestrect 188 581 920 656 Tibetan Plateaurect 250 406 340 427 Rong River...

 between Reid Glacier

Reid Glacier

Reid Glacier is an 11-mile-long glacier in the U.S. state of Alaska. It trends north to Reid Inlet in Glacier Bay National Park and Preserve, two miles south of Glacier Bay and 72 miles northwest of Hoonah. It was named by members of the Harriman Alaska Expedition for Harry Fielding Reid....

 and Heim Glacier

Heim Glacier

Heim Glacier is a glacier 8 nautical miles long in the southeast part of Arrowsmith Peninsula, which flows south to merge with the ice in Jones Channel, on the west coast of Graham Land. With Antevs Glacier, to the north, it forms a transverse depression extending to the southwest part of...

 on Arrowsmith Peninsula

Arrowsmith Peninsula

Arrowsmith Peninsula is a cape about long on the west coast of Graham Land, west of Forel Glacier, Sharp Glacier and Lallemand Fjord, and northwest of Bourgeois Fjord, with Hanusse Bay lying to the northwest. It was surveyed by the Falkland Islands Dependencies Survey in 1955-58 and named for...

 in Graham Land

Graham Land

Graham Land is that portion of the Antarctic Peninsula which lies north of a line joining Cape Jeremy and Cape Agassiz. This description of Graham Land is consistent with the 1964 agreement between the British Antarctic Place-names Committee and the US Advisory Committee on Antarctic Names, in...

. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948-59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Louis Rendu

Louis Rendu

Louis Rendu was French Roman Catholic bishop of Annecy and a scientist. He was the author of Theorie des glaciers de la Savoie, an important book on the mechanisms of glacial motion....

 (1789–1859), French Bishop and scientist, author of Theorie des glaciers de la Savoie, an important book on the mechanism of glacier

Glacier

A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

flow.