Gileican Islands: Difference between revisions
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The '''Gileican Islands''' {{IPA|[dʒɪ'li:kən]}} (lit. "winter islands"; [[Dethric language|Dethric]] '''''Gileicuno Eidis''''' {{IPA|[ʒi'li:kɯnə 'i:ðis]}}) are a chain of volcanic islands east of [[Dethria]] at the divergent plate boundary between the [[Canthauresian plate|Canthauresian]] and [[Marcasian plate|Marcasian]] plates | The '''Gileican Islands''' {{IPA|[dʒɪ'li:kən]}} (lit. "winter islands"; [[Dethric language|Dethric]] '''''Gileicuno Eidis''''' {{IPA|[ʒi'li:kɯnə 'i:ðis]}}) are a chain of volcanic islands east of [[Dethria]] and belonging thereto, at the divergent plate boundary between the [[Canthauresian plate|Canthauresian]] and [[Marcasian plate|Marcasian]] plates. While geologically young, the islands are already densely settled by wildlife; since discovery in 1946 [[CIE]], the area has been off-limits to human settlement and activity other than scientific research. | ||
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Latest revision as of 21:27, 21 December 2006
The Gileican Islands [dʒɪ'li:kən] (lit. "winter islands"; Dethric Gileicuno Eidis [ʒi'li:kɯnə 'i:ðis]) are a chain of volcanic islands east of Dethria and belonging thereto, at the divergent plate boundary between the Canthauresian and Marcasian plates. While geologically young, the islands are already densely settled by wildlife; since discovery in 1946 CIE, the area has been off-limits to human settlement and activity other than scientific research.
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