Beardmore Glacier

From Wikipedia, the free encyclopedia

This is the current revision of Beardmore Glacier as edited by Hal8999 (Talk | contribs) at 14:48, 13 September 2007. This URL is a permanent link to this version of this page.
(diff) ← Older revision | current version (diff) | Newer revision → (diff)
Jump to: navigation, search
Image:Beardmore Glacier - Antarctica.JPG
Aerial view of the Beardmore Glacier in 1956.

The Beardmore Glacier (83°45′S, 171°00′E) in Antarctica is one of the largest glaciers in the world, with a length exceeding 160 km (100 mi). The glacier is one of the main passages from the Ross Ice Shelf through the Queen Alexandra and Commonwealth ranges of the Transantarctic Mountains to the Antarctic Plateau, and was one of the early routes to the South Pole.

The glacier was discovered by Ernest Shackleton during his Nimrod Antarctic expedition of 1908. Although Shackleton turned back before reaching the South Pole, he had discovered the first proven route to the pole, and in doing so, became the first person to set foot upon the great polar plateau. In 1911-1912, Captain Scott and his team successfully reached the South Pole by climbing the Beardmore. However, they reached the pole a month after Roald Amundsen and his team, who had climbed the previously unknown Axel Heiberg Glacier.

Beardmore Glacier is named after Sir William Beardmore, a Scottish industrialist and expedition sponsor born in 1856.

[edit] See also

[edit] References

fr:Glacier Beardmore it:Ghiacciaio Beardmore no:Beardmore Breen tr:Beardmore Buzulu

Views
Personal tools

Toolbox