Midnight Plateau () is a prominent ice-covered plateau, over high, forming the central feature of the

Darwin Mountains The Darwin Mountains () are a group of mountains between the Darwin Glacier and Hatherton Glacier in Antarctica. They were discovered by the British National Antarctic Expedition (1901–04) and named for Major Leonard Darwin, at that time Honora ...

in Antarctica. It is the only area of snow accumulation in the Darwin Mountains.

Exploration and naming

The plateau was discovered by the

Victoria University of Wellington Antarctic Expedition The Antarctic Research Centre (ARC) is part of the School of Geography, Environment and Earth Sciences at Victoria University of Wellington. Its mission is to research " Antarctic climate history and processes, and their influence on the global cl ...

(VUWAE) of 1962–63 and so named because the feature was visited by expedition members at midnight on December 27, 1962.

Location

Midnight Plateau is in the center of the Darwin Mountains. Mount Ellis rises over the north of the plateau.

Haskell Ridge The Darwin Mountains () are a group of mountains between the Darwin Glacier and Hatherton Glacier in Antarctica. They were discovered by the British National Antarctic Expedition (1901–04) and named for Major Leonard Darwin, at that time Honora ...

and

Colosseum Ridge The Darwin Mountains () are a group of mountains between the Darwin Glacier and Hatherton Glacier in Antarctica. They were discovered by the British National Antarctic Expedition (1901–04) and named for Major Leonard Darwin, at that time Honora ...

runs north from the plateau to the Darwin Glacier. The plateau rises above the

Hatherton Glacier The Darwin Glacier () is a large glacier in Antarctica. It flows from the polar plateau eastward between the Darwin Mountains and the Cook Mountains to the Ross Ice Shelf. The Darwin and its major tributary the Hatherton are often treated as one s ...

to the south.

Northern features

Mount Ellis

. The highest point, high, surmounting the northern edge of Midnight Plateau. Mapped by the Darwin Glacier Party of the CTAE (1956-58). Named for M.R. Ellis, engineer with the CTAE, who accompanied Sir

Edmund Hillary Sir Edmund Percival Hillary (20 July 1919 – 11 January 2008) was a New Zealand mountaineering, mountaineer, explorer, and philanthropist. On 29 May 1953, Hillary and Sherpa people, Sherpa mountaineer Tenzing Norgay became the Timeline of M ...

to the South Pole.

Exodus Valley

. A steep moraine-filled valley which descends northward from Midnight Plateau between Colosseum Ridge and Exodus Glacier. So named by the VUWAE (1962-63) because the valley is virtually the only easy route of descent from Midnight Plateau.

Exodus Glacier

. A steep, smooth glacier northeast of Mount Ellis, flowing from the north edge of Midnight Plateau to the southwest side of Island Arena. Named by the VUWAE, 1962-63, in association with nearby Exodus Valley.

Kennett Ridge

. A rocky ridge, long, which descends eastward from the northeast end of Midnight Plateau. Mapped by the VUWAE (1962-63) and named for J.P. Kennett, geologist with the expedition.

Friedmann Peak

. A prominent peak rising to in the central part of Kennett Ridge. Named after Roseli Ocampo Friedmann, professor of microbiology, Florida A&M; University, Tallahassee, FL, who worked five austral summers in McMurdo Dry Valleys; co-discoverer there (with E. Imre Friedmann) of endolithic microorganisms in the Beacon sandstone, 1976.

Eastern features

Hale Valley

The north-most of three largely ice-free valleys that trend east from midnight Plateau in the Darwin Mountains. This valley is immediately south of Kennett Ridge. Named after Mason E. Hale (d.), lichenologist, National Museum of Natural History (Smithsonian), Washington, DC, who worked about six austral summers in the McMurdo Dry Valleys beginning c.1980.

McKay Valley

The central valley of three largely ice-free valleys that trend east from Midnight Plateau in the Darwin Mountains. Named after Christopher P. McKay, physicist, NASA Ames Research Center, Moffett Field, CA, who carried out investigations in McMurdo Dry Valleys (micrometeorology, thickness of ice in frozen lakes, stability of ground ice) in 15 austral summers beginning c.1980.

Wellman Valley

. A mainly ice-free valley lying just east of Midnight Plateau and north of Mount Ash. Explored by VUWAE, 1962-63, and named for H.W. Wellman, geologist of the Victoria University of Wellington, a participant in three Antarctic expeditions.

Southern features

Prebble Icefalls

. Icefalls on the southwestern side of Midnight Plateau. They occupy two large cirques south westward of Mount Ellis and fall about . Discovered by the VUWAE (1962-63) and named for W.M. Prebble, geologist with the expedition.

Polarmail Ledge

A relatively flat wedge-shaped platform that rises above Communication Heights in the south part of Midnight Plateau. At high, the feature is similar in elevation and aspect to Skilton Ledge, to the east. Named in association with Richard Chapman Johnson of Nazareth, PA, radio operator involved for 16 years (1985-2001) in coordinating MARSgrams and Polarmail which have enabled personnel in Antarctica to communicate with home.

Communication Heights

A group of highly eroded ice-free elevations to the south of Midnight Plateau. The feature rises to about high between Conant Valley and Grant Valley. So named because features in the area are named for communication workers.

Skilton Ledge

A relatively flat rectangular rock platform at the southeast margin of Midnight Plateau, Darwin Mountains. The upper surface high is ice covered but a rock cliff forms the south end. Named after Larry Skilton, Connecticut ham radio operator who made phone patches in the United States to complete radio communications from United States Antarctic Project (USAP) science stations including Palmer, McMurdo, Byrd surface station, and particularly South Pole. He worked a regular nightly schedule for 11 years (1990-2001) and arranged the completion of several thousand calls.

References

Sources

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