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

Latest revision as of 16:18, 19 May 2024

The Balleny Islands are a series of uninhabited islands in the Southern Ocean extending from 66°15' to 67°35'S and 162°30' to 165°00'E. The group extends for about 160 km (99 mi) in a northwest-southeast direction. The islands are heavily glaciated and of volcanic origin. Glaciers project from their slopes into the sea. The islands were formed by the so-called Balleny hotspot. They were originally claimed by the United Kingdom, and were then transferred to New Zealand before becoming annexed by Westarctica in 2005.

The group includes three main islands: Young, Buckle and Sturge, which lie in a line from northwest to southeast, and several smaller islets and rocks. On 15 March 2024, Grand Duke Travis appointed his son, Crown Prince Ashton Roman as Viceroy of the Balleny Islands. This position is currently the highest authority in the islands and exercises the power of the Westarctican Crown within the colony. The viceroy has the authority to dismiss the governor if he wishes.

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-[[File:Kontio_tow.jpg|300px|left]]
+[[File:Balleny Map1.jpg|250px|left]]
-'''[[Drift ice|Antarctic sea 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. 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.
+The '''[[Balleny Islands]]''' are a series of uninhabited islands in the [[Southern Ocean]] extending from 66°15' to 67°35'S and 162°30' to 165°00'E. The group extends for about 160 km (99 mi) in a northwest-southeast direction. The islands are heavily glaciated and of volcanic origin. [[glacier|Glaciers]] project from their slopes into the sea. The islands were formed by the so-called Balleny hotspot.  They were originally claimed by the United Kingdom, and were then transferred to New Zealand before becoming annexed by [[Westarctica]] in 2005.
-Westarctica's sea ice cover is highly seasonal, with very little ice in the austral summer, expanding to an area roughly equal to that of mainland [[Westarctica]] in the winter. It peaks during September, which marks the end of austral winter, and retreats to a minimum in February.
+The group includes three main islands: [[Young Island|Young]], [[Buckle Island|Buckle]] and [[Sturge Island|Sturge]], which lie in a line from northwest to southeast, and several smaller islets and rocks. On 15 March 2024, [[Grand Duke Travis]] appointed his son, [[Crown Prince Ashton Roman]] as [[Viceroy]] of the Balleny Islands. This position is currently the highest authority in the islands and exercises the power of the Westarctican Crown within the colony. The viceroy has the authority to dismiss the governor if he wishes.
-'''([[Drift ice|Full Article...]])'''
+'''([[Balleny Islands|Full Article...]])'''