Mountain Ranges, Deserts and Landforms of Antarctica

East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying primarily in the Eastern Hemisphere south of the Indian Ocean, and separated from West Antarctica by the Transantarctic Mountains. It is generally greater in elevation than West Antarctica, and includes the Gamburtsev Mountain Range in the center. The geographic South Pole is located within East Antarctica.

Apart from small areas of the coast, East Antarctica is permanently covered by ice and it has relatively low biodiversity, with only a small number of species of terrestrial plants, animals, algae, and lichens. The coasts are the breeding ground for various seabirds and penguins, and the leopard seal, Weddell seal, elephant seal, crabeater seal and Ross seal breed on the surrounding pack ice in summer.

Adapted from Wikipedia: East Antarctica (CC BY-SA 4.0).

Queen Maud Land (Norwegian: Dronning Maud Land) is a roughly 2.7-million-square-kilometre (1.0-million-square-mile) region of Antarctica claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20° west, specifically the Caird Coast, Coats Land on the West, and the Australian Antarctic Territory 45° east, specifically Enderby Land on the East. In addition, a small unclaimed area from 1939 was annexed in June 2015. Positioned in East Antarctica, it makes out about one-fifth of the continent, and is named after the Norwegian Queen Maud (1869–1938).

In 1930, the Norwegian Hjalmar Riiser-Larsen was the first person known to have set foot in the territory. On 14 January 1939, the territory was claimed by Norway. On 23 June 1961, Queen Maud Land became part of the Antarctic Treaty System, making it a demilitarised zone. It is one of two Antarctic claims made by Norway, the other being Peter I Island. They are administered by the Polar Affairs Department of the Norwegian Ministry of Justice and Public Security in Oslo.

Most of the territory is covered by the east Antarctic ice sheet, and a tall ice wall stretches throughout its coast.

Adapted from Wikipedia: Queen Maud Land (CC BY-SA 4.0).

Ellsworth Land is a portion of the Antarctic continent bounded on the west by Marie Byrd Land, on the north by the Bellingshausen Sea, on the northeast by the base of the Antarctic Peninsula, and on the east by the western margin of the Filchner–Ronne Ice Shelf. It extends between 103°24'W and 79°45'W. The area west of 90°W is unclaimed, the area between 84°W and 90°W is claimed by Chile only, and the remainder by Chile and the United Kingdom as a part of the British Antarctic Territory. Eights Coast stretches between 103°24'W and 89°35'W, and Bryan Coast between 89°35'W and 79°45'W.

It is largely a high ice plateau, but includes the Ellsworth Mountains and a number of scattered mountain groups: Hudson, Jones, Behrendt, Hauberg, Merrick, Sweeney and Scaife Mountains.

This land lies near the center of the area traversed by American explorer Lincoln Ellsworth on an airplane flight during November–December 1935. It was named for him by the Advisory Committee on Antarctic Names in 1962 to commemorate that historic transcontinental flight from Dundee Island to the Ross Ice Shelf.

Adapted from Wikipedia: Ellsworth Land (CC BY-SA 4.0).

Kemp Land is a thin sliver of Antarctica including, and lying inland from, the Kemp Coast. Part of the Australian Antarctic claim, it is defined as lying between 56° 25' E and 59° 34' E, and, as with other sectors of the Antarctic, is deemed being limited by the 60° S parallel. It is bounded in the east by Mac. Robertson Land and in the west by Enderby Land. Kemp Land includes one major group of islands, the Øygarden Group.

It reaches a height of 3,346 feet above sea level.

Adapted from Wikipedia: Kemp Land (CC BY-SA 4.0).

Marie Byrd Land (MBL) is an unclaimed region of Antarctica. With an area of 1,610,000 km2 (620,000 sq mi), it is the largest unclaimed territory on Earth. It was named after the wife of American naval officer Richard E. Byrd, who explored the region in the early 20th century.

The territory lies in West Antarctica, east of the Ross Ice Shelf and the Ross Sea and south of the Pacific Ocean portion of the Antarctic or Southern Ocean, extending eastward approximately to a line between the head of the Ross Ice Shelf and Eights Coast. It stretches between 158°W and 103°24'W. The inclusion of the area between the Rockefeller Plateau and Eights Coast is based upon Byrd's exploration.

Adapted from Wikipedia: Marie Byrd Land (CC BY-SA 4.0).

Dome C, also known as dôme Circe, Dome Charlie (US) or dôme Concordia, is located at Antarctica at an elevation of 3,233 metres (10,607 ft) above sea level, on one of several domes of the Antarctic Ice Sheet. Dome C is located on the Antarctic Plateau, 1,100 kilometres (680 mi) inland from the French research station at Dumont D'Urville, 1,100 kilometres (680 mi) inland from the Australian Casey Station and 1,200 kilometres (750 mi) inland from the Italian Zucchelli Station at Terra Nova Bay. Russia's Vostok Station is 560 kilometres (350 mi) away. Dome C is the site of the Concordia Research Station, jointly operated by France and Italy.

Adapted from Wikipedia: Dome C (CC BY-SA 4.0).

Mac. Robertson Land is the portion of Antarctica lying southward of the coast between William Scoresby Bay and Cape Darnley. It is located at 70°00′S 65°00′E. In the east, Mac. Robertson Land includes the Prince Charles Mountains. It was named by the British Australian and New Zealand Antarctic Research Expedition (BANZARE) (1929–1931), under Sir Douglas Mawson, after Sir Macpherson Robertson of Melbourne, a patron of the expedition.

From 1965 onward, members of the SAE (Soviet Antarctic Expeditions) began undertaking geological fieldwork in the Prince Charles Mountains, eventually establishing a base, Soyuz Station, on the eastern shore of Beaver Lake in the northern Prince Charles Mountains.

Adapted from Wikipedia: Mac. Robertson Land (CC BY-SA 4.0).

Wilkes Land is a large district of land in eastern Antarctica, formally claimed by Australia as part of the Australian Antarctic Territory, though this claim has been held in abeyance for the period of the operation of the Antarctic Treaty, to which Australia is a signatory.

Adapted from Wikipedia: Wilkes Land (CC BY-SA 4.0).

The Ford Ranges (77°0′S 144°0′W) are a collection of mountain groups and ranges standing east of Sulzberger Ice Shelf and Block Bay in the northwest part of Marie Byrd Land, Antarctica.

Adapted from Wikipedia: Ford Ranges (CC BY-SA 4.0).

The Shackleton Range (80°30′S 25°00′W) is a mountain range in Antarctica that rises to 1,875 metres (6,152 ft) and extends in an east–west direction for about 100 miles (160 km) between the Slessor and Recovery Glaciers.

Adapted from Wikipedia: Shackleton Range (CC BY-SA 4.0).

Talos Dome (73°0′S 158°0′E; sometimes spelled Thalos Dome) is a large ice dome rising to 2,300 m (7,500 ft) to the southwest of the Usarp Mountains in Antarctica.

The dome overlies the east margin of the Wilkes Subglacial Basin. The feature was delineated by the Scott Polar Research Institute-National Science Foundation-Technical University of Denmark airborne radio echo sounding program, 1967–1979.

The dome was named after Talos of Greek mythology, who assisted Minos in the defense of Crete.

Adapted from Wikipedia: Talos Dome (CC BY-SA 4.0).

The Ellsworth Mountains are the highest mountain ranges in Antarctica, forming a 350 km (217 mi) long and 48 km (30 mi) wide chain of mountains in a north to south configuration on the western margin of the Ronne Ice Shelf in Marie Byrd Land. They are bisected by Minnesota Glacier to form the Sentinel Range to the north and the Heritage Range to the south. The former is by far the higher and more spectacular with Mount Vinson (4,892 meters (16,050 ft)) constituting the highest point on the continent. The mountains are located within the Chilean Antarctic territorial claim but outside of the Argentinian and British ones.

Adapted from Wikipedia: Ellsworth Mountains (CC BY-SA 4.0).

The Gould Coast (84°30′S 150°0′W) is a portion of the coast of Antarctica along the eastern margin of the Ross Ice Shelf at Amundsen Coast between the west side of Scott Glacier and the south end of the Siple Coast (83°30′S 153°0′W). It was named by the New Zealand Antarctic Place-Names Committee in 1961 for Laurence M. Gould, a geologist who was second-in-command of the Byrd Antarctic Expedition, 1928–30. Gould led the Geological Party which in 1929 mapped 175 miles (280 km) of this coast. While president of Carleton College, Northfield, Minnesota, he was appointed Chairman of the U.S. National Committee for the International Geophysical Year and took a prominent part in planning the United States research program for Antarctica.

Adapted from Wikipedia: Gould Coast (CC BY-SA 4.0).

The Prince Albert Mountains (76°00′S 161°30′E) are a major mountain group in Antarctica over 200 nautical miles (370 km; 230 mi) long.

Located in Victoria Land, they run north–south between the Priestley Glacier to the north and Ferrar Glacier to the south.

They are south of the Deep Freeze Range and north of the Kirkwood Range.

Adapted from Wikipedia: Prince Albert Mountains (CC BY-SA 4.0).

The Executive Committee Range (76°50′S 126°00′W) is a range consisting of five major volcanoes, which trends north-south for 50 nautical miles (93 km; 58 mi) along the 126th meridian west, in Marie Byrd Land, Antarctica.

Adapted from Wikipedia: Executive Committee Range (CC BY-SA 4.0).

Graham Land is the portion of the Antarctic Peninsula that 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 which the name "Antarctic Peninsula" was approved for the major peninsula of Antarctica, and the names Graham Land and Palmer Land for the northern and southern portions, respectively. The line dividing them is roughly 69 degrees south.

Graham Land is claimed by Argentina (as part of Argentine Antarctica), Britain (as part of the British Antarctic Territory) and Chile (as part of the Chilean Antarctic Territory).

Graham Land is the closest part of Antarctica to South America. Thus, it is the usual destination for small ships taking paying visitors on Antarctic trips from South America. (Larger ships are not allowed to disembark passengers.)

The mountains of Graham Land are the last range of the American Cordillera, the almost continuous sequence of mountain ranges forming the western "backbone" of North America, Central America, South America and the Antarctic Peninsula.

Adapted from Wikipedia: Graham Land (CC BY-SA 4.0).

The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martin in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctica.

The Antarctic Peninsula is part of the larger peninsula of West Antarctica, protruding 1,300 km (810 miles) from a line between Cape Adams (Weddell Sea) and a point on the mainland south of the Eklund Islands. Beneath the ice sheet that covers it, the Antarctic Peninsula consists of a string of bedrock islands; these are separated by deep channels whose bottoms lie at depths considerably below current sea level. They are joined by a grounded ice sheet. Tierra del Fuego, the southernmost tip of South America, is about 1,000 km (620 miles) away across the Drake Passage.

The Antarctic Peninsula is 522,000 square kilometres (202,000 sq mi) in area and 80% ice-covered.

The marine ecosystem around the western continental shelf of the Antarctic Peninsula (WAP) has been subjected to rapid climate change. Over the past 50 years, the warm, moist maritime climate of the northern WAP has shifted south.

Adapted from Wikipedia: Antarctic Peninsula (CC BY-SA 4.0).

Princess Ragnhild Coast (Norwegian: Prinsesse Ragnhild Kyst) is the portion of the coast of Queen Maud Land in Antarctica lying between 20° E and the Riiser-Larsen Peninsula, at 34° E. All but the eastern end of the coast is fringed by ice shelves. It was discovered by Capt. Hjalmar Riiser-Larsen and Capt. Nils Larsen in aerial flights from the ship Norvegia on February 16, 1931, and named for Princess Ragnhild of Norway. Vestvika Bay is a large bay on the west side of Riiser-Larsen Peninsula; it was mapped from air photos taken by the Lars Christensen Expedition, 1936–37, and named Vestvika, meaning "west bay."

Adapted from Wikipedia: Princess Ragnhild Coast (CC BY-SA 4.0).

Palmer Land (71°30′S 065°00′W) is the portion of the Antarctic Peninsula, Antarctica that lies south of a line joining Cape Jeremy and Cape Agassiz. This application of Palmer Land is consistent with the 1964 agreement between the Advisory Committee on Antarctic Names and the UK Antarctic Place-Names Committee, in which the name Antarctic Peninsula was approved for the major peninsula of Antarctica, and the names Graham Land and Palmer Land for the northern and southern portions, respectively. The line dividing them is roughly 69° S.

Adapted from Wikipedia: Palmer Land (CC BY-SA 4.0).

Queen Mary Land or the Queen Mary Coast (66°45′S 96°0′E) is the portion of the coast of Antarctica lying between Cape Filchner, in 91° 54' E, and Cape Hordern, at 100° 30' E. It is claimed by Australia as part of the Australian Antarctic Territory.

It was discovered in February 1912 by the Australasian Antarctic Expedition (1911–14) under the leadership of Douglas Mawson, who named it for Mary of Teck, queen consort of George V.

Adapted from Wikipedia: Queen Mary Land (CC BY-SA 4.0).

Sabrina Coast (67°20′S 119°0′E) is that portion of the coast of Wilkes Land, Antarctica, lying between Cape Waldron, at 115° 33' E, and Cape Southard, at 122° 05' E. John Balleny has long been credited with having seen land in March 1839 at about 117° E.

The United States Exploring Expedition under Lt. Charles Wilkes approached this coast in February 1840 and indicated its general configuration as shown in part by "Totten High Land" on his 1840 chart. In 1931 the British Australian New Zealand Antarctic Research Expedition (BANZARE) under Douglas Mawson saw what appeared to be land in this longitude about one degree farther south than that reported by Balleny and Wilkes. In recognition of Balleny's effort, Mawson retained the name of the cutter Sabrina, one of Balleny's ships which was lost in a storm at 95°E in the latter part of March 1839.

Adapted from Wikipedia: Sabrina Coast (CC BY-SA 4.0).

Kaiser Wilhelm II Land is a region of East Antarctica, situated between Cape Penck and Cape Filchner, within the sector claimed by Australia as part of the Australian Antarctic Territory. This claim, however, is not universally recognized due to the Antarctic Treaty System, which designates Antarctica for peaceful scientific research and prohibits new territorial assertions. The land was discovered in 1902 during the German Gauss expedition, which was funded by the German Emperor Wilhelm II and was subsequently named in his honor. It is geographically positioned between Princess Elizabeth Land to its west and Queen Mary Land to its east.

The topography of Kaiser Wilhelm II Land is predominantly characterized by the vast Antarctic ice sheet, with elevations gradually increasing towards the interior from the coast. The region's coastal areas support Antarctic wildlife, notably including Adélie penguins, which establish breeding colonies there, alongside various marine species adapted to the extreme polar environment.

Adapted from Wikipedia: Kaiser Wilhelm II Land (CC BY-SA 4.0).

The Walgreen Coast (75°30′S 107°0′W) is a portion of the coast of Antarctica between Cape Herlacher and Cape Waite, or between Eights Coast on the east and Bakutis Coast in the west. It is part of Marie Byrd Land. It extends from 103°24'W to 114°12'W. It was discovered by Richard E. Byrd and members of the US Antarctic Service (USAS) by flights from the USS Bear during February 1940.

The Walgreen Coast was named by Byrd after Charles R. Walgreen, president of the retail company Walgreens at the time, who was a funder of the Byrd Antarctic Expedition, 1933–1935, and assisted in equipping the Bear for the USAS, 1939–1941. This coast was mapped in detail by the United States Geological Survey from ground surveys and U.S. Navy air photographs, 1959–66.

It contains Thwaites Glacier, also known as the "Doomsday Glacier", for its major contributions to sea level rise as a result of climate change.

Adapted from Wikipedia: Walgreen Coast (CC BY-SA 4.0).

Banzare Coast (67°S 126°E), part of Wilkes Land, is that portion of the coast of Antarctica lying between Cape Southard, at 122°05′E, and Cape Morse, at 130°10′E.

This coast was spotted by the US Exploring Expedition in Feb. 1840.

It was seen from the air by the British-Australian-New Zealand Antarctic Research Expedition, in 1930–1931, led by Douglas Mawson. The name by Mawson is an acronym of the expedition title.

Adapted from Wikipedia: Banzare Coast (CC BY-SA 4.0).

Coats Land is a region in Antarctica which lies westward of Queen Maud Land and forms the eastern shore of the Weddell Sea, extending in a general northeast–southwest direction between 20°00′W and 36°00′W. The northeast part was discovered from the Scotia by William Speirs Bruce, leader of the Scottish National Antarctic Expedition, 1902–1904. He gave the name Coats Land for James Coats, Jr., and Major Andrew Coats, the two chief supporters of the expedition.

Adapted from Wikipedia: Coats Land (CC BY-SA 4.0).

Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south.

Adapted from Wikipedia: Victoria Land (CC BY-SA 4.0).

Knox Coast, part of Wilkes Land, is that portion of the coast of Antarctica lying between Cape Hordern, at 100°31′E, and the Hatch Islands, at 109°16′E.

Adapted from Wikipedia: Knox Coast (CC BY-SA 4.0).

Budd Coast (66°30′S 112°0′E), part of Wilkes Land, is that portion of the coast of Antarctica lying between the Hatch Islands, at 109°16'E, and Cape Waldron, at 115°33'E. It was discovered in February 1840 by the U.S. Exploring Expedition (1838–42) under the leadership of Lieutenant Charles Wilkes, and named by Wilkes for Thomas A. Budd, Acting Master of the sloop Peacock, one of the ships used on the expedition. A portion of the Puget Sound, Budd Inlet, is also named for Thomas Budd.

Adapted from Wikipedia: Budd Coast (CC BY-SA 4.0).

The Admiralty Mountains (alternatively Admiralty Range) is a large group of high mountains and individually named ranges and ridges in northeastern Victoria Land, Antarctica.

This mountain group is bounded by the sea (Ross Sea and Southern Ocean), and by the Dennistoun Glacier, Ebbe Glacier, and Tucker Glacier.

Adapted from Wikipedia: Admiralty Mountains (CC BY-SA 4.0).

King Edward VII Land or King Edward VII Peninsula is a large, ice-covered peninsula which forms the northwestern extremity of Marie Byrd Land in Antarctica. The peninsula projects into the Ross Sea between Sulzberger Bay and the northeast corner of the Ross Ice Shelf, and forms part of the Ross Dependency. Edward VII Peninsula is defined by the Ross Ice Shelf on the southwest, Okuma Bay on the west, and to the east by Sulzberger Bay and the Saunders Coast, all essentially on the Ross Sea / Southern Ocean in Antarctica. The northwest extremity of the peninsula is Cape Colbeck. Edward VII Peninsula is located at 77°40′S 155°00′W.

The western coast is Shirase Coast. In the north and east the Swinburne Ice Shelf is located.

Edward VII Peninsula was discovered on 30 January 1902 by the British National Antarctic Expedition (BrNAE) (1901–1904) under Robert Falcon Scott, who named it King Edward VII Land for King Edward VII of the United Kingdom. The coastline was further explored by the Nimrod Expedition under Ernest Shackleton in 1908–09, and the first landfall was made by a party of the Japanese Antarctic Expedition led by Shirase Nobu in 1912.

Adapted from Wikipedia: King Edward VII Land (CC BY-SA 4.0).

The Pensacola Mountains (82°37′S 52°49′W) are a large group of mountain ranges and peaks that extend 280 nautical miles (520 km; 320 mi) in a northeast–southwest direction in the Transantarctic Mountains System, Queen Elizabeth Land region of Antarctica.

They comprise the Argentina Range, Forrestal Range, Dufek Massif, Cordiner Peaks, Neptune Range, Patuxent Range, Rambo Nunataks and Pecora Escarpment.

These mountain units lie astride the extensive Foundation Ice Stream and Support Force Glacier which drain northward to the Ronne Ice Shelf.

Adapted from Wikipedia: Pensacola Mountains (CC BY-SA 4.0).

Shackleton Coast is the portion of the coast along the west side of the Ross Ice Shelf between Cape Selborne and Airdrop Peak at the east side of Beardmore Glacier in Antarctica.

It was named by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1961 after Sir Ernest Shackleton. He accompanied Scott on the southern journey during the Discovery expedition (1901–04) and subsequently led three Antarctic expeditions. On the British Antarctic Expedition (1907–09), Shackleton discovered the area beyond Shackleton Inlet to the Beardmore Glacier, and was the first to find a practicable route to the South Pole. Lack of food stopped him 97 miles (180 km) from his goal.

Adapted from Wikipedia: Shackleton Coast (CC BY-SA 4.0).

Clarie Coast, called Wilkes Coast by Australia, (66°30′S 133°0′E) is that portion of the coast of Wilkes Land lying between Cape Morse, at 130°10′E, and Pourquoi Pas Point, at 136°11′E. It was discovered in January 1840 by Captain Jules Dumont d'Urville, who recognized the existence of land lying south of the ice cliffs to which he applied the name Côte de Clarie, after the wife (Claire-Fortunée Roze) of Charles Jacquinot, the captain of his second ship, the Zélée.

It was also spotted by the US Exploring Expedition in February 1840.

Adapted from Wikipedia: Clarie Coast (CC BY-SA 4.0).

Princess Astrid Coast (Norwegian: Prinsesse Astrid Kyst) is a portion of the coast of Queen Maud Land, Antarctica, lying between 5° and 20° E. The entire coast is bordered by ice shelves. The region was discovered by Capt. H. Halvorsen of the Sevilla (ship) in March 1931 and in 1932 was named for Princess Astrid of Norway. The ice of the continental glacier is up to 4,000 meters thick in the interior. These thick glaciers are held in place by coastal mountain ranges. On the Princess Astrid Coast, some of the ice does flow through the mountains, spilling onto the relatively flat land on the Princess Astrid Coast. Also, the cold air spills over the mountains, creating very strong and persistent winds, which makes the snow scour off the tops of the glaciers leaving pale blue patches of bare ice. On top of the coastal line is the ice shelf, which is much smoother. The glacial ice floats on the sea surface which is beyond the chaotic surface of the sea ice which has been solidifying all winter long.

Off the Princess Astrid Coast are the Lazarev Sea and Riiser-Larsen Sea, both marginal seas of the Southern Ocean.

Adapted from Wikipedia: Princess Astrid Coast (CC BY-SA 4.0).

The Riiser-Larsen Peninsula (Norwegian: Riiser-Larsenhalvøya) is a large peninsula which forms the western portal to Lützow-Holm Bay and marks the separation of the Princess Ragnhild and Prince Harald Coasts. It was named after Captain Hjalmar Riiser-Larsen who discovered the peninsula in a flight from the Norvegia on 21 February 21 1931.

Adapted from Wikipedia: Riiser-Larsen Peninsula (CC BY-SA 4.0).

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 (1,950 m; 6,400 ft). 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.

These mountains were first observed and photographed from a distance by airmen of USN Operation Highjump, 1946–47. They were examined by several ANARE (Australian National Antarctic Research Expeditions) parties and mapped in the years 1954–61. They have been found to contain large deposits of iron ore. They were named by ANCA in 1956 for King Charles III, then the eight-year-old Prince Charles and son of Queen Elizabeth II.

Adapted from Wikipedia: Prince Charles Mountains (CC BY-SA 4.0).

Bear Peninsula (74°35′S 111°00′W) is a peninsula about 50 nautical miles (93 km; 58 mi) long and 25 nautical miles (46 km; 29 mi) wide which is ice-covered except for several isolated rock bluffs and outcrops along its margins, lying 3 nautical miles (5.6 km; 3.5 mi) east of Martin Peninsula on Walgreen Coast, Marie Byrd Land, Antarctica.

Adapted from Wikipedia: Bear Peninsula (CC BY-SA 4.0).