Irovasdra: Difference between revisions
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Irovasdra occupies much of the western coast of the Far Northeastern peninsula. Its eastern border (with Fariva, Axonléga, and Rovidrea) is formed by the Aterandic Mountains and its western boundary is the bay of Rains, an arm of the Kilikas Sea (known abroad as the Coscivian Sea). The state's topography descends from the geologically ancient, heavily eroded Aterandics through a period of foothills and lower rolling hills to a relatively narrow (though wider in the north) coastal plain. The terrain is thickly forested with hemiboreal mixed forests of spruce, pine, maple, birch, and elm fed by the heavy rains that fall in Irovasdra year-round. | Irovasdra occupies much of the western coast of the Far Northeastern peninsula. Its eastern border (with Fariva, Axonléga, and Rovidrea) is formed by the Aterandic Mountains and its western boundary is the bay of Rains, an arm of the Kilikas Sea (known abroad as the Coscivian Sea). The state's topography descends from the geologically ancient, heavily eroded Aterandics through a period of foothills and lower rolling hills to a relatively narrow (though wider in the north) coastal plain. The terrain is thickly forested with hemiboreal mixed forests of spruce, pine, maple, birch, and elm fed by the heavy rains that fall in Irovasdra year-round. | ||
[[File:Tulach An T-Sionnaich Chambered Cairn from roadside - geograph.org.uk - 914951.jpg|thumb|align=left|500px|caption|If Irovasdra is still canon it probably looks like this] | [[File:Tulach An T-Sionnaich Chambered Cairn from roadside - geograph.org.uk - 914951.jpg|thumb|align=left|500px|caption|If Irovasdra is still canon it probably looks like this]] | ||
'''Major Settlements''' | '''Major Settlements''' | ||