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Kilikas Sea: Difference between revisions
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The '''Kilikas Sea''' is a {{wp|sea}} surrounded by the [[Kilikas_Sea#Extent|Kilikas Basin]] and is pass-through for waters from the [[Levantine Ocean]] to the [[Coscivian Sea]], and then onto the [[Sea of Odoneru]]. The sea is bound by the Arctic in the north and [[Levantia]] in the south. The northern 40% of the sea freezes over from January to March. This much colder water, moving southward, conflicting with the warmer winds moving up the western [[Levantia|Levantine]] coast from the equator in the southern [[Sea of Odoneru]] have caused a phenomenon known as the Kilikas Storm Belt, which encompasses the southwestern quadrant of the sea, particularly in the transitional waters of the Kilikas into the [[Coscivian Sea]]. | The '''Kilikas Sea''' is a {{wp|sea}} surrounded by the [[Kilikas_Sea#Extent|Kilikas Basin]] and is pass-through for waters from the [[Levantine Ocean]] to the [[Coscivian Sea]], and then onto the [[Sea of Odoneru]]. The sea is bound by the Arctic in the north and [[Levantia]] in the south. The northern 40% of the sea freezes over from January to March. This much colder water, moving southward, conflicting with the warmer winds moving up the western [[Levantia|Levantine]] coast from the equator in the southern [[Sea of Odoneru]] have caused a phenomenon known as the Kilikas Storm Belt, which encompasses the southwestern quadrant of the sea, particularly in the transitional waters of the Kilikas into the [[Coscivian Sea]]. | ||
The Kilikas Sea has an average depth of {{convert|1054|m|ft|abbr=on}} and the deepest recorded point is {{convert|6357|m|ft|abbr=on}} about 650 nm due east of [[Wintergen]], known as the Phistual Trench. Because of the Kilikas Storm Belt, the sea has only become an important route for merchants and travelers of in the last few centuries, following the development of safer maritime modes of transport. This has led to the development of slightly isolated cultures, like the [[Bergendii]] who otherwise would have been part of a larger Latinic civilization. The [[Kilikas_Sea#History|history of the Kilikas region]] is crucial to understanding the origins and development of [[Burgundie]], [[ | The Kilikas Sea has an average depth of {{convert|1054|m|ft|abbr=on}} and the deepest recorded point is {{convert|6357|m|ft|abbr=on}} about 650 nm due east of [[Wintergen]], known as the Phistual Trench. Because of the Kilikas Storm Belt, the sea has only become an important route for merchants and travelers of in the last few centuries, following the development of safer maritime modes of transport. This has led to the development of slightly isolated cultures, like the [[Bergendii]] who otherwise would have been part of a larger Latinic civilization. The [[Kilikas_Sea#History|history of the Kilikas region]] is crucial to understanding the origins and development of [[Burgundie]], [[Kiravia]], and the origins of globalization. | ||
The countries with coastlines on the Kilikas Sea are [[Burgundie]], [[Kiravia]], [[Fiannria]]. | The countries with coastlines on the Kilikas Sea are [[Burgundie]], [[Kiravia]], [[Fiannria]]. | ||
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*[[Islas Nubes]], [[Cartadania]] | *[[Islas Nubes]], [[Cartadania]] | ||
*[[Fiannria]] | *[[Fiannria]] | ||
*[[Meridia]], [[ | *[[Meridia]], [[Kiravia]] | ||
===Coastal cities=== | ===Coastal cities=== | ||
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===10 largest islands by area=== | ===10 largest islands by area=== | ||
*[[Meridia]], [[ | *[[Meridia]], [[Kiravia]] | ||
*[[Isle of Burgundie]], [[Burgundie]] | *[[Isle of Burgundie]], [[Burgundie]] | ||
*[[Wintergen]], [[Burgundie]] | *[[Wintergen]], [[Burgundie]] | ||