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The Chitina River (Ahtna Athabascan Tsedi Na’ [tʃɛ.diː.näʔ] < tsedi "copper" + na’ "river") [3] is a 274 km (170 mi) tributary of the Copper River in the U.S. state of Alaska. [1] It begins in the Saint Elias Mountains at the base of Chitina Glacier and flows generally northwest through the Wrangell–St. Elias National Park and ...
Sport fishing by contrast is open all year-long, [23] but peak season on the Copper River lasts from August to September, when the coho salmon runs. [ 24 ] [ 25 ] The fisheries are co-managed by the Alaska Department of Fish and Game (ADF&G) and the Department of the Interior Federal Subsistence Board.
Chitina (Ahtna Athabascan Tsedi Na ' [tʃɛ.diː.näʔ] < tsedi "copper" + na ' "river") [2] is a census-designated place (CDP) in Copper River Census Area, Alaska, United States. At the 2010 census the population was 126, up from 123 in 2000.
The McCarthy Road, within the Wrangell-Saint Elias National Park and Preserve, is a 58-mile (93 km) extension from Chitina to McCarthy. [1] The Edgerton Highway, named for U.S. Army Major General Glen Edgar Edgerton, a member of the Alaska Road Commission, follows an old pack trail along the Copper River, and is paved.
Fishing for white sturgeon will also be closed seasonally upstream of the Highway 50 bridge on the Sacramento River and Interstate 5 bridge on the San Joaquin River from January 1 to May 31, 2024.
North Fork East Fork Chandalar River – 54 miles (87 km) Wind River – 80 miles (130 km) Junjik River – 65 miles (105 km) Middle Fork Chandalar River – 102 miles (164 km) North Fork Chandalar River – 104 miles (167 km) Christian River – 140 miles (230 km) Porcupine River – 569 miles (916 km) Grass River – 39 miles (63 km)
Nizina River is the largest tributary of the Chitina River in the U.S. state of Alaska. It is located in the Wrangell–St. Elias National Park and Preserve . Geography
Kiagna River is a southern tributary of Chitina River, which it joins 30 miles (48 km) below the Chitina Glacier, heads in the high mountains between Chitina River and Granite Creek. It is formed by the union of three principal branches , which receive most of their water from melting snow and ice, and it occupies a typical glacial valley ...