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

 
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The '''[[Siple War]]''', also known as the '''Great Micronational Antarctic War''' was a [[micronation|micronational]] conflict between the [[Grand Duchy of Flandrensis]], Finismund, Marie State, and the Grand Duchy of [[Westarctica]] that began on 29 January 2009 and was officially ended by Flandrensis and Finismund on 1 June 2009. The conflict gained significant notoriety in the international community was even mentioned in a Dutch travel magazine.
'''[[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.


The conflict was sparked by a controversy over territorial claims, with both nations claiming sovereignty over [[Siple Island]] and [[Marie Byrd Land]] and neither being willing to recognize the other's claims. On 24 September 2010 Westarctica and the opposing nations signed an agreement called the [[West-Antarctic Treaty]]. The [[Duke of Waesche]] accepted the treaty on behalf of Westarctica and declared that Westarctica would recognize all Antarctic [[micronations]] and would join the [[Antarctic Micronational Union]].
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.


'''([[Siple War|Full Article...]])'''
'''([[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.

(Full Article...)