Prince Albert Mountains

The Prince Albert Mountains were discovered by Sir James Clark Ross, on February 17, 1841, and named by him for Prince Albert, the consort of the British Queen Victoria of England. The first exploration of the mountains was by British expeditions in the early 1900's. Detailed survey and mapping was accomplished by New Zealand and American expeditions in the 1950's and 1960's.^[1]

The northeastern section of the Prince Albert Mountains extends across the Reeves Glacier north to the Priestley Glacier. These two glacier converge into the Nansen Ice Sheet.^[2] Further south, they cross the David Glacier and Larsen Glacier.^[3] In the far south they extend to the Mawson Glacier.^[4] In the southwest the Reeves Névé extends to their west.^[5] The Ricker Hills are in the northwest of the range, between Hollingsworth Glacier and upper David Glacier.^[6]

This range include the following mountains:

Major glaciers, from north to south, include:

• Priestley Glacier is a major valley glacier, about 60 nautical miles (110 km; 69 mi) long, originating at the edge of the Polar Plateau. The glacier drains southeast between the Deep Freeze Range and Eisenhower Range to enter the northern end of the Nansen Ice Sheet.^[1]
• Reeves Glacier is a broad glacier originating on the interior upland and descending between Eisenhower Range and Mount Larsen to merge with the Nansen Ice Sheet.^[7]
• Larsen Glacier is a glacier flowing southeast from Reeves Névé, through the Prince Albert Mountains and entering the Ross Sea just south of Mount Crummer.^[8]
• David Glacier is a glacier over 60 nautical miles (110 km; 69 mi) long, flowing east from the polar plateau through the Prince Albert Mountains to the coast. It enters the Ross Sea between Cape Philippi and Cape Reynolds to form the floating Drygalski Ice Tongue.^[9]
• Mawson Glacier is a large glacier descending eastward from the Antarctic Plateau to the north of Trinity Nunatak and the Kirkwood Range, to enter the Ross Sea, where it forms the Nordenskjöld Ice Tongue.^[10]

Features or groups of features in the Prince Albert Mountains have been named by various survey groups and expeditions. From north to south they include:

• Eisenhower Range (74°15′S 162°15′E / 74.250°S 162.250°E / -74.250; 162.250 (Eisenhower Range)), a majestic mountain range, about 45 nautical miles (83 km; 52 mi) long and rising to 3,070 metres (10,070 ft), which rises between Reeves Névé on the west, Reeves Glacier on the south, and Priestley Glacier on the north and east.^[11]
• Mount Bellingshausen' (75°7′S 162°6′E / 75.117°S 162.100°E / -75.117; 162.100 (Mount Bellingshausen)), a conspicuous cone-shaped mountain, 1,380 metres (4,530 ft) high, standing 5 nautical miles (9.3 km; 5.8 mi) northeast of Mount Priestley between Larsen Glacier and David Glacier.^[12]
• Mount Joyce (75°36′S 160°49′E / 75.600°S 160.817°E / -75.600; 160.817 (Mount Joyce)), a prominent, dome-shaped mountain, 1,830 metres (6,000 ft) high, standing 8 nautical miles (15 km) northwest of Mount Howard.^[13]
• Ricker Hills (75°41′S 159°10′E / 75.683°S 159.167°E / -75.683; 159.167 (Ricker Hills)), a group of mainly ice-free hills, about 9 nautical miles (17 km; 10 mi) long, lying just west of Hollingsworth Glacier.^[14]
• Mount Armytage (76°02′S 160°45′E / 76.033°S 160.750°E / -76.033; 160.750 (Mount Armytage)), a dome-shaped mountain, 1,855 metres (6,086 ft) high, standing north of Mawson Glacier and 14 nautical miles (26 km; 16 mi) west of Mount Smith.^[15]
• Mount Murray (76°09′S 161°50′E / 76.150°S 161.833°E / -76.150; 161.833 (Mount Murrary)), a sharp granite peak, 1,005 metres (3,297 ft) high, standing 8 nautical miles (15 km; 9.2 mi) west of Bruce Point on the north side of Mawson Glacier.^[16]

  This article incorporates public domain material from websites or documents of the United States Geological Survey.

• Australian Antarctic Data Centre