| Big Bend Ranges | |
|---|---|
 Mount Sir Sandford from Gothics Glacier | |
| Highest point | |
| Peak | Mount Sir Sandford |
| Elevation | 3,519 m (11,545 ft) |
| Coordinates | 51°39′24″N117°52′03″W / 51.65667°N 117.86750°W |
| Geography | |
 | |
| Country | Canada |
| Province | British Columbia |
| Parent range | Selkirk Mountains |
The Big Bend Ranges are a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located in Big Bend of the Columbia River north of the Illecillewaet River.
The Canadian Rockies or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.
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.
The Selkirk Mountains are a mountain range spanning the northern portion of the Idaho Panhandle, eastern Washington, and southeastern British Columbia which are part of a larger grouping of mountains, the Columbia Mountains. They begin at Mica Peak and Krell Hill near Spokane and extend approximately 320 km north from the border to Kinbasket Lake, at the now-deserted location of the onetime fur company post, Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the Purcell Trench, which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River. The Selkirks are distinct from, and geologically older than, the Rocky Mountains. The neighboring Monashee and Purcell Mountains, and sometimes including the Cariboo Mountains to the northwest, are also part of the larger grouping of mountains known as the Columbia Mountains. A scenic highway loop, the International Selkirk Loop, encircles the southern portions of the mountain range.
The Columbia Mountains are a group of mountain ranges along the Upper Columbia River in British Columbia, Montana, Idaho and Washington. The mountain range covers 135,952 km². The range is bounded by the Rocky Mountain Trench on the east, and the Kootenai River on the south; their western boundary is the edge of the Interior Plateau. Seventy-five percent of the range is located in Canada and the remaining twenty-five percent in the United States; American geographic classifications place the Columbia Mountains as part of the Rocky Mountains complex, but this designation does not apply in Canada. Mount Sir Sandford is the highest mountain in the range, reaching 3,519 metres (11,545 ft).
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 Bendor Range is a small but once-famous subrange of the Pacific Ranges of the Coast Mountains, about It is approximately 7,000 square kilometres (2,700 sq mi) in area and about 40 km long and about 18 km at its widest. It lies between Anderson Lake on the southeast and the Carpenter Lake Reservoir or the Bridge River Power Project on the north, with the gold-rich valley of Cadwallader Creek on its southwest.
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 (1,150 sq mi) in area.
Hamber Provincial Park is a provincial park in British Columbia, Canada, located 130 kilometres (80.7 mi) north of Golden. Straddling the Great Divide on the provincial boundary with Alberta, the park is surrounded on three sides by Jasper National Park and protects the headwaters of the Wood River at Fortress Lake.
Big Bend generally refers to a major change in course or large meander in a river. It may refer to:
The British Columbia Interior, popularly referred to as the BC Interior or simply the Interior, is a geographic region of the Canadian province of British Columbia. While the exact boundaries are variously defined, the British Columbia Interior is generally defined to include the 14 regional districts that do not have coastline along the Pacific Ocean or Salish Sea, and are not part of the Lower Mainland. Other boundaries may exclude parts of or even entire regional districts, or expand the definition to include the regional districts of Fraser Valley, Squamish–Lillooet, and Kitimat–Stikine.
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, as well as the Big Bend of that river, now mostly inundated by Kinbasket Lake and Revelstoke Lake.
McGillivray Pass is a mountain pass in the Pacific Ranges of southwestern British Columbia, Canada, located about 30 miles west of the town of Lillooet and immediately west of the upper end of Anderson Lake, above the former resort community of McGillivray. The pass connects the head of McGillivray Creek with the head of Standard Creek, a tributary of Cadwallader Creek and was used as a route by prospectors, miners and hunters heading for the upper Bridge River Country beyond the pass. The pass was proposed at one time for a cog railway to connect the mines at Bralorne and Pioneer with the Pacific Great Eastern Railway (now part of CN but the project never went forward. There are private ski cabins near the summit area of the pass, which is the division between the Bendor Range to the east and the Cadwallader Range to the west.
The McGregor Plateau is a sub-plateau of the Nechako Plateau, the northernmost major subdivision of the Interior Plateau spanning the inland regions of the Pacific Northwest. Located in British Columbia, Canada, to the east of the city of Prince George, British Columbia, the McGregor Plateau lies between the main spine of the Northern Rocky Mountains on the east and the Fraser River on the west, beginning on its southeast at the confluence of the Torpy River with the Fraser and running northwest, parallel to the Fraser and the Rockies, to end in the area of the Arctic and Pacific Lakes to the north of the great bend in the Fraser River just upstream from and to the northeast of Prince George. The McGregor Plateau is very mountainous in character and includes several large rivers, the largest being the McGregor River and Herrick Creek. Included in the McGregor Plateau is the McGregor Range, which lies between the McGregor and Torpy Rivers and the Dezaiko Range, which lies between Herrick and McGregor Rivers.
The Rossland Range is a subrange of the Monashee Mountains of the Columbia Mountains, between the Columbia River and Big Sheep Creek in British Columbia, Canada. The highest point in the range is Old Glory Mountain, 2,376-metre (7,795-foot).
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.
The Cadwallader Range, originally named the Cadwallader Mountains, is a sub-range of the Pacific Ranges of the Coast Mountains in the Bridge River-Lillooet Country of the South-Central Interior of British Columbia, Canada, located between the south end of Anderson Lake (E) and the Hurley River. According to the provincial basemap, the precise alpine boundaries of the range are McGilliray Pass, at its eastern extremity and beyond which is the Bendor Range, and the pass between Noel and Sockeye Creeks on its west, which is immediately north of the lower end of Birkenhead Lake. The officially unnamed range west of that has been called the Noel Range, after its main peak Mount Noel. At the foot of the range along its northeast flank is Cadwallader Creek, scene of the historic and once-rich Bralorne and Pioneer Mines and the ghost town of Bralorne.
Tyoax Pass is a mountain pass in the Chilcotin Ranges of the Pacific Ranges, the southernmost main subdivision of the Coast Mountains of British Columbia, Canada. Located at the head of Tyaughton Creek, a north tributary of the Bridge River, it connects the basin of the Bridge River with that of Big Creek in the southern Chilcotin District, and is therefore at the boundary between the Spruce Lake Protected Area and Big Creek Provincial Park.
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