Noble Peak ( 64°48′S63°25′W / 64.800°S 63.417°W ) is a peak in the Comer Range, 720 m, standing 1 nautical mile (1.9 km) southwest of Lockley Point and marking the northeast end of a prominent ridge on the northwest side of Wiencke Island, in the Palmer Archipelago. Discovered by the Belgian Antarctic Expedition, 1897–99, under Gerlache. The name appears on a chart based on a 1927 survey by DI personnel on the Discovery, but may reflect on earlier naming.
This article incorporates public domain material from "Noble Peak". Geographic Names Information System . United States Geological Survey.
Hope Bay is a bay 3 nautical miles long and 2 nautical miles wide, indenting the tip of the Antarctic Peninsula and opening on Antarctic Sound.
The Prince Olav Mountains is a mountain group in the Queen Maud Mountains in Antarctica stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf.
Tucker Glacier is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.
The Prince Charles Mountains are a major group of mountains in Mac. Robertson Land in Antarctica, including the Athos Range, the Porthos Range, and the Aramis Range. The highest peak is Mount Menzies, with a height of 3,228 m (10,591 ft). Other prominent peaks are Mount Izabelle and Mount Stinear. These mountains, together with other scattered peaks, form an arc about 420 km (260 mi) long, extending from the vicinity of Mount Starlight in the north to Goodspeed Nunataks in the south.
The Arctowski Peninsula is a peninsula, 15 nautical miles long in a north-south direction, lying between Andvord Bay and Wilhelmina Bay on the west coast of Graham Land, Antarctica.
The Scott Glacier is a major glacier, 120 nautical miles long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east.
Drygalski Glacier is a broad glacier, 18 nautical miles long which flows southeast from Herbert Plateau through a rectangular re-entrant to a point immediately north of Sentinel Nunatak on the east coast of Graham Land, Antarctica.
Ulu Peninsula is that portion of James Ross Island northwest of the narrow neck of land between Rohss Bay and Croft Bay, extending from Cape Obelisk to Cape Lachman, in Antarctica.
Achaean Range is a mountain range rising to 2,577 metres (8,455 ft) in the central part of Anvers Island in the Palmer Archipelago. It is bounded on the east by Iliad Glacier and Trojan Range and on the west by Marr Ice Piedmont, and extends northwest from Mount Agamemnon for 10 kilometres (6 mi), curving northeast for a further 19 km (12 mi) to Mount Nestor. Surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1955 and named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for the Achaeans, one of the opposing forces of the Trojan War in Homer's Iliad.
The Anderson Hills are an irregular group of hills, ridges and peaks between Mackin Table and the Thomas Hills in the Patuxent Range, Pensacola Mountains, Antarctica.
The Werner Mountains are a group of mountains located just west-southwest of New Bedford Inlet and between the Meinardus Glacier and Bryan Glacier, in Palmer Land, Antarctica.
The Dana Mountains are a group of mountains just northwest of New Bedford Inlet, bounded by Mosby Glacier on the north and Haines Glacier and Meinardus Glacier on the south, in Palmer Land, Antarctica.
The Gutenko Mountains are a large, scattered group of hills, nunataks and small mountains at the south end of Dyer Plateau in central Palmer Land, Antarctica. The feature includes the Elliott Hills, the Rathbone Hills, the Guthridge Nunataks and the Blanchard Nunataks.
Paradise Harbour is a wide embayment behind Lemaire Island and Bryde Island, indenting the west coast of Graham Land, Antarctica, between Duthiers Point and Leniz Point. The name was first applied by whalers operating in the vicinity and was in use by 1920.
Harbour Glacier is a through glacier 3 nautical miles (6 km) long and 1.5 nautical miles (3 km) wide, lying on the northwest side of Wiencke Island and extending in a northeast direction from Port Lockroy to the cove 1 nautical mile (2 km) east of Noble Peak, in the Palmer Archipelago, Antarctica. It was probably first seen by the Belgian Antarctic Expedition, 1897–99, under Gerlache. The glacier was charted in 1944 by the Falkland Islands Dependencies Survey, who so named it because of its proximity to the harbour of Port Lockroy.
The Harold Byrd Mountains are a group of exposed mountains and nunataks which extend in an east–west direction between the lower part of Leverett Glacier and the head of the Ross Ice Shelf in Antarctica. They were discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named by Rear Admiral Richard E. Byrd for D. Harold Byrd, a cousin of his and a contributor towards the purchase of furs for the expedition.
Victory Glacier is a gently sloping glacier, 8 nautical miles long, flowing east-southeast from the north end of Detroit Plateau on Trinity Peninsula to Prince Gustav Channel immediately north of Pitt Point. It is bounded by Trakiya Heights to the north and Kondofrey Heights to the south.
The La Gorce Mountains are a group of mountains, 20 nautical miles long, standing between the tributary Robison Glacier and Klein Glacier at the east side of the upper reaches of the Scott Glacier, in the Queen Maud Mountains of Antarctica.
The James Ross Island group is a group of islands located close to the northeastern tip of the Antarctic Peninsula. The largest islands in the group are James Ross Island, Snow Hill Island, Vega Island, and Seymour Island. The islands lie to the south of the Joinville Island group. The groups contains several scientific bases, notably Marambio Base, and numerous important palaeontological sites.