Tuya River
A tuya is a geologic term for a flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. The geologic term comes from Tuya Butte, which was named in association with Tuya Lake. The term may come from the Tahltan language.
The Tuya River is in the traditional territory of the Tahltan First Nation, of the Tahltan people, the Kaska Dena First Nation, and the Teslin Tlingit First Nation.
Geography
The Tuya River originates at High Tuya Lake in Tuya Mountains Provincial Park, just south of Ash Mountain, the highest peak of the Tuya Range. It flows south to Tuya Lake, southeast of Tuya Butte and east of Mount Josephine. The tributary Butte Creek, flowing south from Butte Lake in Tuya Mountains Provincial Park, empties into Tuya Lake. From the southern end of Tuya Lake the Tuya River continues south. It is joined by Josephine Creek and numerous unnamed tributaries.
Continuing south the Tuya River flows east of Tachilta Lakes, collecting more tributaries including Cody Creek, Tachilta Creek, Mckessock Creek, and Ross Creek. A few kilometres west of Cariboo Meadows the Tuya River is joined by its main tributary, the Little Tuya River. As the river nears the Stikine River it is joined by Classy Creek, then flows under Telegraph Creek Road. The Tuya River empties into the Stikine River near Days Ranch, the mouth of the Klastline River, and the Tahltan Indian reserve of "Tahltan 10", of the Tahltan First Nation,
Geology
Coal has been found in rocks exposed in the drainage of the Tuya River and its tributaries the Little Tuya River and Mansfield Creek, between the communities of Dease Lake and Telegraph Creek in northwestern BC. This coal field is called the Tuya River Coal Basin. The coal was first discovered in 1904, but the main exploration of its economic potential occurred in the late 1970s to 1990s by PetroCanada.
Natural history
The Tuya River drainage provides very high quality salmon spawning habitat, but fish passage is blocked by several barriers including an 11 m (36 ft) waterfall located about 3 km (1.9 mi) above the mouth of the Tuya and another significant barrier about 51 km (32 mi) upriver. In addition, a 2006 landslide created a barrier to fish passage near the mouth of the Tuya River. Chinook salmon spawn in the lowermost portion of the river, below the blockage.
In the 1950s the Alaska Department of Fish and Game assessed the Tuya River as having the highest level of potential salmon spawning habitat of any transboundary river, possibly capable of supporting more sockeye salmon than the entire Stikine River.
The Pacific Salmon Commission, a joint US-Canada transboundary river salmon protection regulatory body, has made the Tuya River a major component of its efforts to improve fish stocks in the Stikine River watershed.
In 2008 explosives were used to blast through the fish barrier created by the 2006 landslide. Field studies in 2009 indicated that the landslide barrier had been successfully breached. Salmonid species found in the Tuya River in 2009 included Chinook salmon, sockeye salmon, coho salmon, pink salmon, rainbow trout, and bull trout.