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The South Pole–Queen Maud Land Traverse (SPQMLT) was a three-part scientific exploration of Antarctica undertaken by the United States in the 1960s. The three parts, referred to individually as South Pole–Queen Maud Land Traverse I, II, and III (SPQMLT-1, -2, and -3), traveled a zigzag route across nearly 4200 km of the Antarctic Plateau in ...
Queen Maud Mountains The Dominion Range ( 85°20′S 166°30′E / 85.333°S 166.500°E / -85.333; 166.500 ) is a broad mountain range , about 30 nautical miles (56 km; 35 mi) long, forming a prominent salient at the juncture of the Beardmore and Mill glaciers in Antarctica
Plateau Station is an inactive American research and South Pole—Queen Maud Land Traverse support base on the central Antarctic Plateau.Construction on the site started on December 13, 1965, and the first traverse team (named SPQML II) arrived in early 1966.
Queen Maud Land 3,937 feet (1,200 m) ... (serving Amundsen–Scott South Pole Station) ... Antarctic Digital Database Map Viewer—SCAR This page was last edited on ...
Queen Maud Land (Norwegian: Dronning Maud Land) [note 1] is a roughly 2.7-million-square-kilometre (1.0-million-square-mile) [5] region of Antarctica claimed by Norway as a dependent territory. [6] It borders the claimed British Antarctic Territory 20° west and the Australian Antarctic Territory 45° east .
Titan Dome is a large ice dome on the polar plateau, trending east–west and rising to 3,100 metres (10,200 ft) between the Queen Maud Mountains and the South Pole. The dome was first crossed by the sledge parties of Shackleton, Amundsen, and Scott on their journeys toward the South Pole, and was described as a major snow ridge.
The central of three nunataks in mid-stream of the upper Liv Glacier, standing about 4 nautical miles (7.4 km; 4.6 mi) southeast of Mount Wells, in the Queen Maud Mountains. Named by the Southern Party of the NZGSAE (1961-62) for Harold June, aviator and engineer on the South Pole flight of R. Admiral Richard E. Byrd in 1929. [9]
A rock peak, 760 metres (2,490 ft) high, in the northeast part of Collins Ridge, at the confluence of Bowman and Amundsen Glaciers in the Queen Maud Mountains. Discovered and mapped by the Byrd Antarctic Expedition, 1928-30. Named by US-ACAN for Ronald E. Witalis, meteorologist, South Pole Station winter party, 1961. [23]