List of glaciers of Graham Land

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Following is a list of glaciers of Graham Land in Antarctica. This list may not reflects recently named glaciers in Graham Land.

Contents

Antarctic Peninsula

Adelaide Island

James Ross Island

Palmer Archipelago

Trinity Peninsula

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<span class="mw-page-title-main">Aoraki / Mount Cook</span> Mountain in New Zealand

Aoraki / Mount Cook is the highest mountain in New Zealand. Its height, as of 2014, is listed as 3,724 metres. It sits in the Southern Alps, the mountain range that runs the length of the South Island. A popular tourist destination, it is also a favourite challenge for mountain climbers. Aoraki / Mount Cook consists of three summits: from south to north, the Low Peak, the Middle Peak and the High Peak. The summits lie slightly south and east of the main divide of the Southern Alps, with the Tasman Glacier to the east and the Hooker Glacier to the southwest. Mount Cook is ranked 10th in the world by topographic isolation.

<span class="mw-page-title-main">Ice cap</span> Ice mass that covers less than 50,000 kmĀ² of land area

In glaciology, an ice cap is a mass of ice that covers less than 50,000 km2 (19,000 sq mi) of land area. Larger ice masses covering more than 50,000 km2 (19,000 sq mi) are termed ice sheets.

<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.

Martin Glacier is a glacier, 3 nautical miles (6 km) wide and 9 nautical miles (17 km) long, which flows west and then northwest from the south side of Mount Lupa to the southeast corner of Rymill Bay where it joins Bertrand Ice Piedmont, on the west coast of Graham Land, Antarctica. It was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under John Riddoch Rymill, and was resurveyed in 1948–1949 by the Falkland Islands Dependencies Survey. The glacier was named for James Hamilton Martin, a member of the British Australian and New Zealand Antarctic Research Expedition (1929–1931) under Sir Douglas Mawson, and first mate of the Penola during the BGLE.

The Airy Glacier is a glacier 20 nautical miles (37 km) long and 6 nautical miles (11 km) wide, flowing west to the northeast portion of Forster Ice Piedmont, near the west coast of the Antarctic Peninsula.

Sibelius Glacier is a glacier, 12 miles (19 km) long and 6 miles (10 km) wide, flowing south into the Mozart Ice Piedmont 10 miles (16 km) southwest of Mount Stephenson in the northern portion of Alexander Island, Antarctica. The glacier was first sighted from the air by the British Graham Land Expedition in 1937. Mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960. This feature was named by the United Kingdom Antarctic Place-Names Committee for Jean Sibelius (1865-1957), Finnish composer.

Ice Gate Glacier is a narrow hanging glacier, tributary to Astudillo Glacier, between rock spurs on the west slope of Dallmeyer Peak, Danco Coast, Antarctica. It was named by the Polish Antarctic Expedition in about 1992, probably from the gatelike appearance of the spurs at the junction of the two glaciers.

<span class="mw-page-title-main">Crane Glacier</span> Glacier in the Aristotle Mountains of the Antarctic Peninsula

Crane Glacier, is a narrow glacier which flows 30 miles (50 km) in an east-northeasterly direction along the northwest side of Aristotle Mountains to enter Spillane Fjord south of Devetaki Peak, on the east coast of the Antarctic Peninsula. Sir Hubert Wilkins photographed this feature from the air in 1928 and gave it the name "Crane Channel", after C.K. Crane of Los Angeles, reporting that it appeared to be a channel cutting in an east-west direction across the peninsula. The name was altered to "Crane Inlet" following explorations along the west coast of the peninsula in 1936 by the British Graham Land Expedition, which proved that no through channel from the east coast existed as indicated by Wilkins. Comparison of Wilkins' photograph of this feature with those taken in 1947 by the Falklands Islands Dependencies Survey shows that Wilkins' "Crane Channel" is this glacier, although it lies about 75 miles (120 km) northeast of the position originally reported by Wilkins.

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

Flask Glacier, is a gently-sloping glacier, 25 nautical miles long, flowing east from Bruce Plateau to enter Scar Inlet between Daggoo Peak and Spouter Peak in Graham Land, Antarctica. The lower reaches of this glacier were surveyed and photographed by the Falklands Islands Dependencies Survey (FIDS) in 1947. The entire glacier was photographed by the Falkland Islands and Dependencies Aerial Survey Expedition in 1955–56, and mapped by the FIDS in 1957. It was named by the UK Antarctic Place-names Committee after the third mate on the Pequod in Herman Melville's Moby-Dick; or, The White Whale.

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

Sestrimo Glacier is the 11 km long and 4 km wide glacier on the northwest side of Trinity Peninsula in Graham Land on the Antarctic Peninsula. Situated southwest of Ogoya Glacier, west-northwest of Broad Valley and north of Cugnot Ice Piedmont. Draining the north slopes of Windy Gap, and flowing northwards east of Mount D'Urville and west of Argentino (Guerrero) Peak to enter Lafond Bay in Bransfield Strait south of Cockerell Peninsula.

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

Antevs Glacier, also known as North Heim Glacier, is a glacier on Arrowsmith Peninsula, Graham Land, flowing north between Seue Peaks and Boyle Mountains into Muller Ice Shelf, Lallemand Fjord. It was named by the United Kingdom Antarctic Place-Names Committee in 1960 after Ernst V. Antevs, American glacial geologist.

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

Barnes Glacier is a glacier on the west side of Hemimont Plateau flowing west into Blind Bay on the west coast of Graham Land. It was named by the UK Antarctic Place-Names Committee in 1958 for Howard T. Barnes, Canadian physicist and pioneer of ice engineering.

<span class="mw-page-title-main">Belgun Peak</span>

Belgun Peak is the ice-covered peak with precipitous, partly ice-free west slopes, rising to 1205 m in the northwest extremity of Trakiya Heights on Trinity Peninsula in Graham Land, Antarctica. It is situated on the east side of Zlidol Gate, surmounting the head of Russell West Glacier to the north, and the upper course of Victory Glacier to the south.

<span class="mw-page-title-main">Lepitsa Peak</span>

Lepitsa Peak is the ice-covered peak rising to 1110 m in the northeast foothills of Detroit Plateau on Trinity Peninsula in Graham Land, Antarctica. It is situated on the west side of Zlidol Gate, surmounting the head of Russell West Glacier to the north, and the upper course of Victory Glacier to the southeast.

Clarke Glacier is a 2 miles (3.2 km)-wide, 20 miles (32 km)-long glacier, located on the west coast of Graham Land in Antarctica. It flows west, along the north side of Sickle Mountain and the Baudin Peaks, to Mikkelsen Bay.