Western Boundary Mountain System: Difference between revisions
From FrathWiki
Jump to navigationJump to search
No edit summary |
mNo edit summary |
||
| Line 1: | Line 1: | ||
The '''Western Boundary Mountain System''' ([[Arithide language|Arithide]] '''''Iraphim Onoris Ryagia''''' {{IPA|[ | The '''Western Boundary Mountain System''' ([[Arithide language|Arithide]] '''''Iraphim Onoris Ryagia''''' {{IPA|['irəvim '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]]. The system includes, from north to south, the [[Taza-a Lami]], the [[Iryagi]], the [[Alerryagi]], as well as several other subordinate mountain ranges such as the [[Hallaryagi]]. | ||
{{stub}} | {{stub}} | ||
Latest revision as of 01:45, 22 December 2006
The Western Boundary Mountain System (Arithide Iraphim Onoris Ryagia ['irəvim '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. The system includes, from north to south, the Taza-a Lami, the Iryagi, the Alerryagi, as well as several other subordinate mountain ranges such as the Hallaryagi.
This article is a stub. If you can contribute to its content, feel free to do so.
