Difference between revisions of "Template:POTD protected"

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The '''[[Scott Glacier]]''' is a major [[glacier]], 120 miles (190 km) long, that drains the [[East Antarctic Ice Sheet]] through the [[Queen Maud Mountains]] to the [[Ross Ice Shelf]]. The Scott Glacier is one of a series of major glaciers flowing across the [[Transantarctic Mountains]], with the Amundsen Glacier to the west and the [[Leverett Glacier|Leverett]] and [[Reedy Glacier]]s to the east.
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 Scott Glacier originates on the Antarctic Plateau in the vicinity of [[D'Angelo Bluff]] and [[Mount Howe]], and descends between the Nilsen Plateau and the mountains of the [[Watson Escarpment]] to enter [[Ross Ice Shelf]] just west of the [[Tapley Mountains]]. The Scott Glacier is bisected by the 150° line of longitude putting roughly half the [[glacier]] in [[Westarctica]]'s territory while the westernmost half is located inside New Zealand's [[Ross Dependency]].


<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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