Ellis Fjord ( 68°36′S78°5′E / 68.600°S 78.083°E ) is a long narrow fjord between Breidnes Peninsula and Mule Peninsula in the Vestfold Hills of Antarctica. It was photographed by the Lars Christensen Expedition (1936–37), and plotted by Norwegian cartographers as a bay and a remnant lake which were called "Mulvik" (snout bay) and "Langevatnet" (long lake) respectively. Analysis by John Roscoe of air photos taken by U.S. Navy Operation Highjump (1946–47) showed these two features to be connected. The feature was renamed Ellis Fjord by Roscoe after Edwin E. Ellis, aerial photographer on U.S. Navy Operation Highjump flights over this area. [1]
Davis Station, commonly called Davis, is one of three permanent bases and research outposts in Antarctica managed by the Australian Antarctic Division (AAD). Davis is situated on the coast of Cooperation Sea in Princess Elizabeth Land, Ingrid Christensen Coast in the Australian Antarctic Territory, a territory claimed by Australia. Davis lies in an Antarctic oasis, a mostly ice-free area known as the Vestfold Hills.
The Vestfold Hills are rounded, rocky, coastal hills, 512 square kilometres (198 sq mi) in extent, on the north side of Sorsdal Glacier on the Ingrid Christensen Coast of Princess Elizabeth Land, Antarctica. The hills are subdivided by three west-trending peninsulas bounded by narrow fjords. Most of the hills range between 30 and 90 metres in height, with the highest summit reaching nearly 160 metres (520 ft).
The Prince Gustav Channel was named in 1903 after Crown Prince Gustav of Sweden by Otto Nordenskiöld of the Swedish Antarctic Expedition.
Lake Zvezda is a large, irregular-shaped glacial lake 0.5 miles (0.80 km) southeast of Lake Cowan in the east part of Vestfold Hills of Princess Elizabeth Land in Antarctica.
Cosgrove Ice Shelf is a 35-mile (56 km) long by 25-mile (40 km) wide ice shelf, occupying the inner (east) part of the embayment between King Peninsula and Canisteo Peninsula, Antarctica. It was mapped from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named by the Advisory Committee on Antarctic Names for Lieutenant Jerome R. Cosgrove, U.S. Navy Reserve, assistant communications officer on the staff of the Commander, U.S. Navy Support Force, Antarctica, during U.S. Navy Operation Deep Freeze, 1967 and 1968.
Branchinecta gaini is a species of fairy shrimp from Antarctica and Patagonia. It is the largest freshwater invertebrate in Antarctica, at 16 mm (0.63 in) long. It lives on bacteria and other organisms, surviving the winter as resting eggs.
Nemesis Glacier is a large glacier which flows northeast through the center of the Aramis Range, Prince Charles Mountains. Discovered in January 1957 by ANARE southern party under W.G. Bewsher, and named after Homer's Nemesis because considerable difficulty was experienced in traversing the region due to the glacier.
Mule Peninsula is an irregularly shaped rocky peninsula between Ellis Fjord and Krok Fjord in the southern part of the Vestfold Hills of Princess Elizabeth Land, Antarctica. It was mapped from aerial photographs taken by the Lars Christensen Expedition of 1936–37 and named Breidnesmulen by Norwegian cartographers. Mule Peninsula is an adaptation of the original Norwegian name by the Antarctic Names Committee of Australia.
Tryne Crossing is a low but rough pass across Langnes Peninsula, Vestfold Hills, leading from the southwest arm of Tryne Fjord to Langnes Fjord. Used for portage and sledges and probably suitable for tracked vehicles. The area was mapped from air photos taken by the Lars Christensen Expedition (1936–37), and was photographed by U.S. Navy Operation Highjump (1946–47). First traversed by an ANARE party led by B.H. Stinear, May 13, 1957, and named for its association with Tryne Fjord.
Sørsdal Glacier is a heavily crevassed glacier on the Ingrid Christensen Coast of Princess Elizabeth Land in Antarctica, 15 nautical miles (28 km) long, flowing westward along the south side of Krok Fjord and the Vestfold Hills and terminating in a prominent glacier tongue at Prydz Bay. Discovered in February 1935 by a Norwegian expedition under Captain Klarius Mikkelsen and named for Lief Sørsdal, a Norwegian dentist and a member of the party from the whaling ship Thorshavn that landed at the northern end of the Vestfold Hills.
Tarbuck Crag is one of a group of three high points about 0.75 nautical miles (1.4 km) southwest of Club Lake in the Vestfold Hills, Antarctica. The feature is 140 m high and has steep sides to the south and east. The feature was the terminal tellurometer station of the 1969 ANARE Prince Chabroarles Mountains survey. Named by Antarctic Names Committee of Australia (ANCA) for J. Tarbuck, cook at Wilkes Station in 1965, cook at Davis Station in 1969, and expedition assistant with ANARE at Wilkes in 1967.
Taynaya Bay is a bay which is completely enclosed except for a very narrow entrance on the north side, lying within the northern part of Langnes Peninsula, Vestfold Hills. The feature was photographed by the Lars Christensen Expedition (1936–37), but was plotted on the subsequent maps as a lake. John Roscoe's 1952 study of air photographs taken by Operation Highjump (1946–47) showed that the bay is connected at the north to the sea. It was photographed by ANARE (1954–58) and the Soviet Antarctic Expedition (1956), the latter applying the name Bukhta Taynaya.
Topografov Island is an island just north of Partizan Island in the north part of the entrance to Langnes Fjord, Vestfold Hills in Antarctica. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37). Subsequently, photographed by U.S. Navy Operation Highjump (1946–47), ANARE (1954–58) and the Soviet Antarctic Expedition (1956). The latter named it Ostrov Topografov.
Luncke Ridge is a fairly prominent ridge on the northern side of the eastern extremity of Langnes Fjord in the Vestfold Hills of Antarctica. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37. The ridge was seen in 1957 by an Australian National Antarctic Research Expeditions party and named for Bernhard Luncke, a Norwegian cartographer who plotted the Vestfold Hills area for the Hansen Atlas.
Langnes Fjord is a narrow fjord, 10 nautical miles (19 km) long, between Langnes Peninsula and Breidnes Peninsula in the Vestfold Hills of Antarctica. It was mapped from air photos by the Lars Christensen Expedition (1936–37) and named after Langnes Peninsula. John Roscoe's 1952 study of air photos taken by U.S. Navy Operation Highjump (1946–47) revealed that this fjord continues farther east than was previously mapped, and that it includes what had been plotted as an isolated lake which the Norwegians had called "Breidvatnet."
Lake Burton, also known as Burton Lagoon, is a meromictic and saline lake in the Vestfold Hills of Princess Elizabeth Land in Eastern Antarctica. Princess Elizabeth Land, including the lake, is claimed by Australia as part of the Australian Antarctic Territory. The lake has a surface area of 1.35 km2 (0.52 sq mi), a volume of 9.69 million m3, a maximum depth of 18.3 metres (60 ft) and a mean depth of 7.16 metres (23.5 ft). The lake is named after H. R. Burton, a biologist working in the Vestfold Hills of Antarctica.
Barrier Island is an island, 0.5 nautical miles (0.9 km) long, at the north end of the Vestfold Hills, lying just north of the entrance to Tryne Fjord in Tryne Sound. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37. Visited in 1957 by an ANARE party and so named because the island appeared to form a barrier to the passage of icebergs up Tryne Fjord.
Camp Lake is a small lake lying 0.5 nautical miles west of the head of Weddell Arm on Breidnes Peninsula, Vestfold Hills. Mapped from air photos taken by U.S. Navy Operation Highjump, 1946-47. So named because when first visited by an ANARE party in January 1955, a camp was established near the northeast end of the lake.
Lake Washburn is a lake that formerly existed in the Taylor Valley, McMurdo Dry Valleys, Antarctica. It formed when climatic changes and an expansion of ice caused the flooding of the valley, between 23,000 and 8,340 radiocarbon years ago. Its extent and elevation are unclear but Lake Bonney and Lake Fryxell are considered to be its present-day remnant.
Deprez Basin is a nearly circular basin on the Ingrid Christensen Coast of Princess Elizabeth Land in East Antarctica.
This article incorporates public domain material from "Ellis Fjord". Geographic Names Information System . United States Geological Survey.