Kigluaik Mountains
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| Kigluaik Mountains | |
|---|---|
Grand Central Valley, Kigluaik Mountains | |
| Highest point | |
| Peak | Mount Osborn |
| Elevation | 4,714 ft (1,437 m) |
| Coordinates | Lua error: callParserFunction: function "#coordinates" was not found.[1] |
| Naming | |
| Native name | Kiglawait (Inupiaq) |
| Geography | |
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| |
| Country | United States |
| State | Alaska |
| Subdivision | Seward Peninsula |
| Range coordinates | Lua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value).[2] |
The Kigluaik Mountains (Kiglawait in Inupiaq) are a 42-mile (68 km) mountain chain running east to west on western Alaska's Seward Peninsula.
Its highest point is the summit of Mount Osborn, at 4,714 feet (1,437 meters) above sea level. This remote range is home to numerous isolated mountain lakes which have been shown to contain unique subspecies of Arctic char.[3] Located in the Nome Census Area,[2] Kigluaik Mountains are noted as the location of Grand Union Glacier, the only remaining active glacier in western Alaska.[4]
References
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- ^ Parker E. Calkin, Darrell S. Kaufman, Bruce J. Przybyl, W. Brett Whitford, and Brian J. Peck Glacier Regimes, Periglacial Landforms, and Holocene Climate Change in the Kigluaik Mountains, Seward Peninsula, Alaska
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