Chilcotin River

The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This 19,200 km2 (7,400 sq mi) watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, 22 km (14 mi) upstream from Gang Ranch.

Chilcotin River
Chilcotin in Farwell Canyon
Native nameCheẑqox (Chilcotin)
Location
CountryCanada
ProvinceBritish Columbia
DistrictLillooet Land District
Physical characteristics
SourceItcha Lake
  locationNortheast of Itcha Mountain
  coordinates52°47′09″N 124°45′51″W
  elevation5,223 ft (1,592 m)
MouthFraser River
  location
Upstream from Gang Ranch
  coordinates
51°44′22″N 122°24′03″W
  elevation
1,152 ft (351 m)
Length241 km (150 mi)
Basin size19,300 km2 (7,500 sq mi)
Discharge 
  locationbelow Big Creek
  average102 m3/s (3,600 cu ft/s)
  minimum13.8 m3/s (490 cu ft/s)
  maximum1,100 m3/s (39,000 cu ft/s)

The geological processes that created this region support its diverse history, climate, and ecology. This diversity is also illustrated by the presence of biogeoclimatic zones and a rich population of fish. Canadian Fisheries and many communities within the region such as: Alexis Creek, Hanceville, and the Tŝilhqot’in Nation depend on the diversity of Chilcotin River. In recent years, its diverse history, climate, and ecology has been impacted by a number of environmental concerns such as: increases in flooding, changes in water quality, declines in steelhead trout populations, and an increase in mountain pine beetle outbreaks.

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