List of glaciers of James Ross Island and Graham Land

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Following is a list of glaciers of James Ross Island and Graham Land in Antarctica. This list may not reflect recently named glaciers in James Ross Island and Graham Land.

Contents

James Ross Island

Adelaide Island

Antarctic Peninsula

Palmer Archipelago

Trinity Peninsula

Related Research Articles

<span class="mw-page-title-main">Ross Island</span> Island in Ross Sea, Antarctica

Ross Island is an island in Antarctica lying on the east side of McMurdo Sound and extending 43 nautical miles from Cape Bird on the north to Cape Armitage on the south, and a like distance from Cape Royds on the west to Cape Crozier on the east. The island is entirely volcanic. Mount Erebus, 3,795 metres (12,451 ft), near the center, is an active volcano. Mount Terror, 3,230 metres (10,600 ft), about 20 nautical miles eastward, is an extinct volcano. Mount Bird rises to 1,765 metres (5,791 ft) just south of Cape Bird. Ross Island lies within the boundary of Ross Dependency, an area of Antarctica claimed by New Zealand.

<span class="mw-page-title-main">Antarctic Peninsula</span> Peninsula located in northern Antarctica

The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín 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 Churchill Mountains are a mountain range group of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. They border on the western side of the Ross Ice Shelf, between Byrd Glacier and Nimrod Glacier.

<span class="mw-page-title-main">Darwin Glacier (Antarctica)</span> Glacier in Antarctica

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 system, the Darwin–Hatherton.

<span class="mw-page-title-main">Terra Nova Bay</span>

Terra Nova Bay is a bay which is often ice free, about 40 nautical miles long, lying between Cape Washington and the Drygalski Ice Tongue along the coast of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition under Robert Falcon Scott, 1901–1904, and named by him after Terra Nova, one of the relief ships for the expedition.

Bertrand Ice Piedmont is an ice piedmont about 20 kilometres (11 nmi) long and from 6 to 9 kilometres wide, lying between Rymill Bay and Mikkelsen Bay on the Fallières Coast of Graham Land.

The Mulock Glacier is a large, heavily crevassed glacier which flows into the Ross Ice Shelf 40 kilometers south of the Skelton Glacier in the Ross Dependency, Antarctica.

<span class="mw-page-title-main">Swithinbank Glacier</span> Glacier in Graham Land, Antarctica

Swithinbank Glacier is a glacier on the west side of Hemimont Plateau flowing north to the southeast corner of Square Bay, in Graham Land. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1946–59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Charles Swithinbank, British glaciologist, a participant in several British, New Zealand and American expeditions to Antarctica, 1949–62.

<span class="mw-page-title-main">Jorum Glacier</span> Glacier in Antarctica

Jorum Glacier is a glacier draining the southeast slopes of Forbidden Plateau, and lowing east into Exasperation Inlet, just north of Caution Point, on the east coast of Graham Land, Antarctica. It was surveyed by the Falkland Islands Dependencies Survey in 1947 and 1955. The UK Antarctic Place-Names Committee name alludes to the punchbowl shape of the head of the glacier, a "jorum" being a large drinking bowl used for punch.

Toynbee Glacier is a glacier situated in the northeast portion of Alexander Island, Antarctica, extending 17 nautical miles (31 km) long and 5 nautical miles (9 km) wide, lying between Mount Huckle, Mount Spivey and Mount Stephenson of the northern portion of the Douglas Range on the west and Mount Tyrrell and Mount Tilley on the east. It flows north from the east face of Mount Stephenson into the George VI Ice Shelf that occupies George VI Sound. The glacier was first photographed from the air in 1937 by the British Graham Land Expedition under Rymill. Surveyed in 1948 by the Falkland Islands Dependencies Survey and named for Patrick A. Toynbee, FIDS air pilot at Stonington Island in 1948 and 1949.

Pluto Glacier is a glacier on the east coast of Alexander Island, Antarctica, 10 nautical miles (18 km) long and 4 nautical miles (7 km) wide, which flows east into George VI Sound to the north of Succession Cliffs. Although Pluto Glacier is not located within nearby Planet Heights, the glacier was named in association with the mountain range along with many other nearby glaciers that are named after planets of the Solar System. The glacier was first photographed from the air on November 23, 1935, by Lincoln Ellsworth and mapped from these photos by W.L.G. Joerg. Roughly surveyed in 1936 by the British Graham Land Expedition (BGLE). Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Pluto, then considered the ninth planet of the Solar System, following Falkland Islands Dependencies Survey (FIDS) surveys in 1948 and 1949.

<span class="mw-page-title-main">Evans Glacier (Graham Land)</span> Glacier in Antarctica

Evans Glacier is a gently-sloping glacier 15 nautical miles (28 km) long and 4 nautical miles (7 km) wide, draining the southeast slopes of Travnik Buttress eastwards between Rugate Ridge and Poibrene Heights to flow into Vaughan Inlet on the east coast of Graham Land, Antarctica. It was discovered by Sir Hubert Wilkins in an aerial flight, December 20, 1928, and named "Evans Inlet" by him for E.S. Evans of Detroit. A further survey by the Falkland Islands Dependencies Survey in 1955 reported that this low-lying area is not an inlet, but is formed by the lower reaches of Hektoria Glacier and the feature now described.

Remus Glacier is a glacier, 8 nautical miles (15 km) long, which flows from the north slopes of Mount Lupa northwestward along the northeast side of the Blackwall Mountains into Providence Cove, Neny Fjord, on the west coast of Graham Land. The lower reaches of the glacier were first roughly surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 by the Falkland Islands Dependencies Survey (FIDS), who so named it for its association with Romulus Glacier, whose head lies near the head of this glacier.

Vallot Glacier is a glacier flowing northwest to Laubeuf Fjord close south of Lewis Peaks, on Arrowsmith Peninsula in Graham Land. It was mapped by the Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948–59, and was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Joseph Vallot, a French naturalist and glaciologist who first measured the surface velocity of a glacier over a long period, in Switzerland, 1891–99.

<span class="mw-page-title-main">Index of Antarctica-related articles</span>

This is an alphabetical index of all articles related to the continent of Antarctica.

Charles Winthrop Molesworth Swithinbank, MBE was a British glaciologist and expert in the polar regions who has six places in the Antarctic named after him.