Gileican Islands: Difference between revisions
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The '''Gileican Islands''' ([[Dethric language|Dethric]] '''''Gileicuno Eidis''''' {{IPA|[ʒi'li:kɯnə 'i:ðis]}}) | 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, formed from a stationary mantle plume. 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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[[Category: Ilethes]] | |||
[[Category: Geography of Ilethes]] | |||
[[Category: Geology of Ilethes]] | |||
[[Category: Islands of Ilethes]] | |||
[[Category: Dethria]] | |||
Revision as of 08:21, 5 November 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 at the divergent plate boundary between the Canthauresian and Marcasian plates, formed from a stationary mantle plume. 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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