Search results
Results from the WOW.Com Content Network
The Chilcotin River /tʃɪlˈkoʊtɪn/ [5] located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. [6] 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. [7]
Farwell Canyon (known to the local Tsilhqot'in First Nation as Nagwentled - 'place of landslides') is a canyon on the Chilcotin River in the Chilcotin District of British Columbia, Canada, located around the confluence of Farwell Creek and the Chilcotin, between the confluence of Big Creek and the Fraser River. This location has been ...
The Chilcotin Plateau is part of the Fraser Plateau, a major subdivision of the Interior Plateau of British Columbia.The Chilcotin Plateau is physically near-identical with the region of the same name, i.e. "the Chilcotin", which lies between the Fraser River and the southern Coast Mountains and is defined by the basin of the Chilcotin River and so includes montane areas beyond the plateau.
The Chilcotin (/ tʃ ɪ l ˈ k oʊ t ɪ n /) [2] region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River .
The Chilko is the Chilcotin River's main tributary. In fact at their confluence the Chilko River is much larger than the Chilcotin. It is also the main reason why the lower reaches of the Chilcotin are very silty. The Chilko gets most of its silt from the Taseko River, which joins it a few kilometers above the Chilko's mouth.
In a coastal Southern California city where multimillion-dollar estates teeter above the Pacific Ocean, power remained intentionally severed Tuesday to about 245 homes as worsening landslides have ...
The Lillooet Icecap is the source of several major rivers which radiate out from it in a wheel pattern. The Lillooet River is fed by the Lillooet Glacier on the icefield's southern flank and runs southeast via Pemberton to Harrison Lake. The Bridge River is fed by the Bridge Glacier on the icefield's eastern flank and runs east to the town of ...
The residual political impact of the Chilcotin War was one factor dissuading the CPR from using Bute Inlet; the other was the severe grades required in the canyon of the Homathko River in order to reach the elevation of the Chilcotin Plateau on the inland side of the Coast Range, as well as the cost of blasting along the inlet and the deep ...