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Levantia: Difference between revisions
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==Topography and Climate== | ==Topography and Climate== | ||
Levantia runs the gamut from a tropical equatorial climate in the southern tip of [[Urcea]] to an arctic climate in the northern portions of [[Caergwynn]]. Northern Levantia is known for its infamous [[Kilikas Sea|Kilikas Storm Belt]], which encompasses the northern regions of [[Fiannria]], [[Faneria]], [[Caergwynn]], [[Hendalarsk]], [[Yytuskia-Helvana]], and [[Prevalia]], characterized by frequent and powerful temperate cyclones, thunderstorms, and blizzards that have historically made marine navigation extremely dangerous in the area. | Levantia runs the gamut from a tropical equatorial climate in the southern tip of [[Urcea]] to an arctic climate in the northern portions of [[Caergwynn]]. Northern Levantia is known for its infamous [[Kilikas Sea|Kilikas Storm Belt]], which encompasses the northern regions of [[Fiannria]], [[Faneria]], [[Caergwynn]], [[Hendalarsk]], [[Yytuskia-Helvana]], and [[Prevalia]], characterized by frequent and powerful temperate cyclones, thunderstorms, and blizzards that have historically made marine navigation extremely dangerous in the area. | ||
The [[Vandarch]] is a key topographical feature of Levantia. It is the world's largest inland sea and is connected to the oceans by the [[Grand Vandarch Canal]] to the north and by the [[Carolina Grand Canal]] to the south. The Vandarch has major effects on the climate of Levantia and has been described as a "thoroughfare of cold, Boreal air" which has the effect of cooling much of the southern part of the continent. | |||
==Human Geography== | ==Human Geography== | ||