Difference between revisions of "Template:Westarctica.wiki:Today's featured article"

 
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The '''Holy Order of The Cross''' is a [[Westarctica|Westarctican]] [[Orders of Westarctica|Order of Chivalry]] that recognizes exceptional Christian achievement. Citizens of Westarctica and foreigners who exemplify Christian values may receive the honor in all three of its classes. The order is bestowed irrespective of denominations of Christianity and has been awarded to Protestants and Catholics. It is the only Westarctican order that may be bestowed posthumously as a symbol of the eternal nature of the soul and the faith of the holder continuing in the afterlife.
'''[[Drift ice]]''' is the sea ice of the [[Southern Ocean]]. It extends far north in winter and retreats almost to the coastline each summer. Sea ice is frozen seawater that is usually less than a few meters thick. This is in contrast to [[Ice shelf|ice shelves]], which are formed by glaciers, float in the sea, and are up to a kilometer thick. There are two subdivisions of sea ice: fast ice, which is attached to land; and ice floes, which are not.


At the time the Holy Order was created, [[Grand Duke Travis]] had been a born-again Christian for less than a year. He wanted to find a way to publicly celebrate the [[Religion in Westarctica|national religion]] of [[Westarctica]] as well as recognize fellow Christians for their religious achievements. The "the" in front of the word "cross" is always capitalized to recognize the sanctity of The Cross on which Jesus was crucified.  '''([[Holy Order of The Cross|Full Article...]])'''
Sea ice in the Southern Ocean melts from the bottom instead of from the surface like Arctic ice because it is covered in snow. As a result, melt ponds are rarely observed. On average, [[Antarctica|Antarctic]] sea ice is younger, thinner, warmer, saltier, and more mobile than Arctic sea ice. Due to its inaccessibility, it is not as well-studied as Arctic ice.
 
'''([[Drift ice|Full Article...]])'''

Latest revision as of 16:39, 25 October 2024

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Drift ice is the sea ice of the Southern Ocean. It extends far north in winter and retreats almost to the coastline each summer. Sea ice is frozen seawater that is usually less than a few meters thick. This is in contrast to ice shelves, which are formed by glaciers, float in the sea, and are up to a kilometer thick. There are two subdivisions of sea ice: fast ice, which is attached to land; and ice floes, which are not.

Sea ice in the Southern Ocean melts from the bottom instead of from the surface like Arctic ice because it is covered in snow. As a result, melt ponds are rarely observed. On average, Antarctic sea ice is younger, thinner, warmer, saltier, and more mobile than Arctic sea ice. Due to its inaccessibility, it is not as well-studied as Arctic ice.

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