Western Boundary Mountain System: Difference between revisions
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Revision as of 19:17, 10 November 2006
The Western Boundary Mountain System (Arithide Iraphim Onoris Ryagia [i'ravim 'ɔnəris 'rja:gi.a]) is a chain of continuous crustal uplift from the Nikidi Islands north of Carabaea to the Tumides archipelago in the Thorfu, formed from the longest continuous destructive convergent plate boundary on Ilethes.
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