Mount LeSchack (Antarctica)

Mount LeSchack () is a distinctive flat-topped mountain, 2,265 m, standing on the north side of Perkins Canyon in the Wisconsin Range, Horlick Mountains. Mapped by United States Geological Survey (USGS) from surveys and U.

Quonset Glacier (Antarctica)

Quonset Glacier () is a glacier about 20 miles (32 km) long which drains the north slopes of Wisconsin Range between Mount LeSchack and Ruseski Buttress and trends west-northwest to enter the north side of Davisville Glacier. Mapped by United States Geological Survey (USGS) from surveys and U.

Quartz Pebble Hill (Antarctica)

Quartz Pebble Hill () is a flat-topped elevation on the north escarpment of Buckeye Table, Ohio Range, in the Horlick Mountains. The hill is located where Discovery Ridge joins the main escarpment.

Quartz Hills (Antarctica)

Quartz Hills () is an arcuate group of mainly ice-free hills and peaks standing immediately south of Colorado Glacier along the west side of Reedy Glacier. Mapped by United States Geological Survey (USGS) from surveys and U.

Reedy Glacier (Antarctica)

The Reedy Glacier () is a major glacier, over 160 km (100 mi) long and from 10 to 19 km (6 to 12 mi) wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range, and marking the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east.

Ohio Range (Antarctica)

The Ohio Range () is a mountain range in the Transantarctic Mountains of Antarctica. It is about 48 km (30 mi) long and 16 km (10 mi) wide, extending WSW-ENE from Eldridge Peak to Mirsky Ledge.

Wisconsin Range (Antarctica)

The Wisconsin Range ( ) is a major mountain range of the Horlick Mountains in Antarctica, comprising the Wisconsin Plateau and numerous glaciers, ridges and peaks bounded by the Reedy Glacier, Shimizu Ice Stream, Horlick Ice Stream and the interior ice plateau. Mapped by the USGS from surveys and US Navy air photos, 1959-64.

Rockefeller Plateau (Antarctica)

Rockefeller Plateau () is that portion of the interior ice plateau of Marie Byrd Land lying eastward of Shirase Coast and Siple Coast and southward of the Ford Ranges, Flood Range and Executive Committee Range, centering near the coordinates given above. Much of its extensive, ice-covered surface is from 1,000 to 1,500 m above sea level.

Horlick Mountains (Antarctica)

The Horlick Mountains () are a mountain range in the Transantarctic Mountains of Antarctica, lying eastward of Reedy Glacier and including the Wisconsin Range, Long Hills and Ohio Range. The mountains were discovered in two observations by the Byrd Antarctic Expedition, 1933-35, one by Kennett L.