Difference between revisions of "Template:POTD protected"

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The '''[[Beardmore Glacier]]''' in [[Antarctica]] is one of the largest valley [[glacier]]s 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]].
The '''[[Amundsen–Scott South Pole Station]]''' is a United States scientific research station at the [[South Pole]], the southernmost place on the Earth. The station is located on the high plateau of [[Antarctica]] at an elevation of 2,835 meters (9,301 feet) above sea level and is administered by the Division of Polar Programs within the National Science Foundation under the United States Antarctic Program (USAP).


The glacier is one of the main passages through the Transantarctic Mountains to the great polar plateau beyond, and was one of the early routes to the [[South Pole]] despite its steep upward incline. 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.


<p><small>Image credit: University of Maine </small></p>
 
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<p><small>Photo Credit: Daniel Leussler</small></p>
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Latest revision as of 05:09, 11 July 2026

SouthPoleStationDestinationAlpha.jpg

The Amundsen–Scott South Pole Station is a United States scientific research station at the South Pole, the southernmost place on the Earth. The station is located on the high plateau of Antarctica at an elevation of 2,835 meters (9,301 feet) above sea level and is administered by the Division of Polar Programs within the National Science Foundation under the United States Antarctic Program (USAP).


Photo Credit: Daniel Leussler

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