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{| role="presentation" style="margin:0 3px 3px; width:100%; text-align:left; background-color:transparent; border-collapse: collapse; "  | {| role="presentation" style="margin:0 3px 3px; width:100%; text-align:left; background-color:transparent; border-collapse: collapse; "  | ||
|style="padding:0 0.9em 0 0;" | [[File:  | |style="padding:0 0.9em 0 0;" | [[File:Beardmore Glacier - Antarctica.jpg|300px]]  | ||
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The '''[[  | 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   | 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>  | <p><small>Image credit: University of Maine </small></p>  | ||
[[:Category:Images|'''(More Featured Images)''']]  | [[:Category:Images|'''(More Featured Images)''']]  | ||
<div class="potd-recent" style="text-align:right;">  | <div class="potd-recent" style="text-align:right;">  | ||