Aerial view of the Beardmore Glacier in 1956
|Length||200 km (125 mi)|
|Width||40 km (25 mi)|
|Terminus||Ross Ice Shelf|
The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being 200 km (125 mi) long and having a width of 40 km (25 mi). It descends about 2,200 m (7,200 ft) from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western.
The glacier was discovered and climbed by Ernest Shackleton during his Nimrod Expedition of 1908. Although Shackleton turned back before reaching the South Pole, he established the first proven route towards the pole and, in doing so, became the first person to set foot upon the polar plateau. In 1911–1912, Captain Scott and his Terra Nova Expedition team reached the South Pole by similarly climbing the Beardmore. However, they reached the pole a month after Roald Amundsen and his team, who had chosen a route up the previously unknown Axel Heiberg Glacier.
- "Beardmore Glacier". www.britannica.com. Encyclopædia Britannica, Inc. Retrieved 10 January 2014.
- "Beardmore Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 10 January 2014.
- "Rare Antarctic beetle find delights". BBC. 29 November 2016. Retrieved 29 November 2016.
|This glaciology article is a stub. You can help Wikipedia by expanding it.|