Caracua: Difference between revisions

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 ==Geography==
-Caracua primarily consists of hilly seasonal tundras, with population centers primarily orbiting the [[Ashuk River|Ashuk]] and Copehe rivers. Of these two, the Ashuk leads to Mera Bay, while the Copehe is a tributary of Lake _____'s {{wp|endorheic basin}}. The Ashuk and Copehe have distinct fish breeds and chemical differences, with the Copehe being more saline and less ecologically dense due to drawing salt off of flats in its northernmost reaches that see regular thaws during deep summer.
+Caracua primarily consists of hilly seasonal tundras, with population centers primarily orbiting the [[Ashuk River|Ashuk]], Kilmer, and Copehe rivers. Of these two, the Ashuk land Kilmer feed into [[Mera Bay]], while the Copehe is a tributary of Lake _____'s {{wp|endorheic basin}}. The Copehe has distinct fish breeds and chemical differences from the other water systems in the country, as well as being more saline and less ecologically dense due to drawing salt off of flats in its northernmost reaches that see regular thaws during deep summer.
+The coast of Caracua is defined by the Malho Peninsula, which extends from arctic permafrost to the country's southernmost point. The Peninsula is only marginally arable, and contains few natural resources other than timber. The interior of the country centers on the Ashuk River, which forms the primary agricultural basin of the country as well as its largest population centers.
 ==History==