Difference between revisions of "Template:POTD protected"

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The '''[[Flag of Westarctica]]''' has gone through many changes since the nation first declared itself a sovereign territory. Although the original flag of the [[Achaean Territory of Antarctica|Achaean Territory]] was generally considered to be an eyesore, subsequent flags were designed to be more aesthetically pleasing while also encompassing the values of [[Westarctica]].
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.


In late 2014, [[Grand Duke Travis]] decided it was time to bring back some of the old [[National Symbols of Westarctica|symbols of Westarctica]]. In a show of solidarity with the old regime, he created a new flag utilizing the old symbology of the "Cross and Crown" design. To make the flag more aesthetically pleasing, simple tinctures of blue and white were used instead of the original teal and forest green found on the 2004 - 2010 flags. The specific tincture of blue is called "Westarctica Blue" and is considered a protected official color of Westarctica.
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>Author: [[Grand Duke Travis]] </small></p>
<p><small>Image credit: University of Maine </small></p>
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Revision as of 04:57, 16 September 2019

Scott-Glacier.jpg

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 and Reedy Glaciers to the east.

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.

Image credit: University of Maine

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