The Canadian Rockies or Canadian Rocky Mountains comprise the Canadian segment of the North American Rocky Mountains. They are the eastern part of the Canadian Cordillera, which is a system of multiple ranges of mountains which runs from the Canadian Prairies to the Pacific Coast. The Canadian Rockies mountain system comprises the southeastern part of this system, lying between the Interior Plains of Alberta and Northeastern British Columbia on the east to the Rocky Mountain Trench of BC on the west. The southern end borders Idaho and Montana of the United States. In geographic terms the boundary is at the Canada/US border, but in geological terms it might be considered to be at Marias Pass in northern Montana. The northern end is at the Liard River in northern British Columbia.
The Kootenays or Kootenay is a region of southeastern British Columbia. It takes its name from the Kootenay River, which in turn was named for the Kutenai First Nations people.
Central Washington is a region of the U.S. state of Washington between the western and eastern parts of the state extending from the border with the Canadian province of British Columbia in the north to the border with the U.S. state of Oregon in the south. Generally, the western edge is the Cascade Range and the eastern edge is in the vicinity of the 119th meridian west.
Rogers Pass is a high mountain pass through the Selkirk Mountains of British Columbia used by the Canadian Pacific Railway and the Trans-Canada Highway. The pass is a shortcut across the "Big Bend" of the Columbia River from Revelstoke on the west to Donald, near Golden, on the east. The pass was discovered on May 29, 1881, by Major Albert Bowman Rogers, a surveyor working for the Canadian Pacific Railway. A second pass was named for Rogers in 1887 in Montana, c.373 miles to the south-east.
The Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to Bella Coola and Burke Channel, north of which are the Kitimat Ranges. The Coast Mountains lie between the Interior Plateau and the Coast of British Columbia.
The Chilcotin Ranges are a subdivision of the Pacific Ranges of the Coast Mountains. They lie on the inland lea of the Pacific Ranges, abutting the Interior Plateau of British Columbia. Their northwestern end is near the head of the Klinaklini River and their southeast end is the Fraser River just north of Lillooet; their northern flank is the edge of the Plateau while their southern is the north bank of the Bridge River. In some reckonings they do not go all the way to the Fraser but end at the Yalakom River, which is the North Fork of the Bridge.
The Shulaps Range is a subrange of the Chilcotin Ranges subset of the Pacific Ranges of the Coast Mountains in southwest-central British Columbia. The range is 55 km NW–SE and 15 km SW–NE and 2,970 km² (1150 mi²) in area.
The Big Bend Gold Rush was a gold rush on the upper Columbia River in the Colony of British Columbia in the mid-1860s.
The British Columbia Interior, BC Interior or Interior of British Columbia, usually referred to only as the Interior, is one of the three main regions of the Canadian province of British Columbia, the other two being the Lower Mainland, which comprises the overlapping areas of Greater Vancouver and the Fraser Valley, and the Coast, which includes Vancouver Island and also including the Lower Mainland.
Canoe River is the most northern tributary of the Columbia River in British Columbia, Canada. Its lower reach is flooded by Mica Dam. The lower Canoe River is called Canoe Reach, part of the Mica Dam's reservoir, Kinbasket Lake.
Columbia Country refers to the upper basin of the Columbia River in the Canadian province of British Columbia. It includes a smaller region known as the Columbia Valley, near the river's headwaters at Columbia Lake in the Rocky Mountain Trench, and the Big Bend of that river, now mostly inundated by Kinbasket Lake and Revelstoke Lake.
The Big Bend Highway is a 305 km (190 mi) former highway in the interior of British Columbia, was the original alignment of British Columbia Highway 1 which followed the Columbia River between Revelstoke and Golden through the Selkirk Mountains.
Big Bend Country is a term used in the Canadian province British Columbia to refer to the region around the northernmost bend of the Columbia River, where the river leaves its initial northwestward course along the Rocky Mountain Trench to curve around the northern end of the Selkirk Mountains to head southwest between that range and the Monashee Mountains, which lie to the west. The term is the namesake of the gold rush and associated gold mining district that flourished there in the 19th century. Long known to the indigenous peoples of the region, and in fact raided and at times occupied by the Blackfoot, the Big Bend is traditional territory of the Secwepemc (Shuswap) people, but also claimed by the Ktunaxa. Boat Encampment, near the Big Bend of the Columbia's most northerly point, is the historic site of a long-established fur trading cache and campsite on the annual York Factory Express.
The Sir Sandford Range is a subrange of the Big Bend Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located between Gold (river) and Palmer Creek just southwest of the Gold Arm of Kinbasket Lake.
The Adamant Range is a subrange of the Big Bend Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located on the west side of Columbia Reach, Kinbasket Lake, north of Glacier National Park.
The Windy Range is a subrange of the Big Bend Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located on the west side of Columbia Reach, Kinbasket Lake north of Windy Creek.
