| Toby Glacier | |
|---|---|
 | |
| Highest point | |
| Peak | Mount Hamill |
| Elevation | 3,274 m (10,741 ft) |
| Coordinates | 50°13′18″N116°36′30″W / 50.22167°N 116.60833°W |
| Geography | |
| Country | Canada |
| Province | British Columbia |
| Parent range | Purcell Mountains |
Toby Glacier is a glacier in the Purcell Mountains of southeastern British Columbia, Canada. It covers an area of 123 square kilometres (47 sq mi). Its main drainage basin is Toby Creek. It is located within Purcell Wilderness Conservancy Provincial Park and Protected Area.
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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.
Kootenay Lake is a lake located in British Columbia, Canada. It is part of the Kootenay River. The lake has been raised by the Corra Linn Dam and has a dike system at the southern end, which, along with industry in the 1950s–70s, has changed the ecosystem in and around the water. The Kootenay Lake ferry is a year-round toll-free ferry that crosses between Kootenay Bay and Balfour. The lake is a popular summer tourist destination.
Glacier National Park is part of a system of 43 parks and park reserves across Canada, and one of seven national parks in British Columbia. Established in 1886, the park encompasses 1,349 km2 (521 sq mi), and includes a portion of the Selkirk Mountains which are part of the larger grouping of mountains, the Columbia Mountains. It also contains the Rogers Pass National Historic Site.
The Bugaboos are a mountain range in the Purcell Mountains of eastern British Columbia, Canada. The granite spires of the group are a popular mountaineering destination. The Bugaboos are protected within Bugaboo Provincial Park.
Panorama Mountain Resort is a ski and golf resort in Canada, located in the Purcell Mountains of southeastern British Columbia. Part of the Columbia Valley sub-region of the East Kootenay region, it is a tourist destination known for its rolling cliffs and views of the Rocky Mountains. It is privately owned by Panorama Mountain Village Inc.
The Purcell Mountains are a mountain range in southeastern British Columbia, Canada. They are a subrange of the Columbia Mountains, which includes the Selkirk, Monashee, and Cariboo Mountains. They are located on the west side of the Rocky Mountain Trench in the area of the Columbia Valley, and on the east side of the valley of Kootenay Lake and the Duncan River. The only large settlements in the mountains are the Panorama Ski Resort and Kicking Horse Resort, adjacent to the Columbia Valley towns of Invermere and Golden, though there are small settlements, such as Yahk and Moyie along the Crowsnest Highway, and residential rural areas dependent on the cities of Creston, Kimberley and Cranbrook, which are located adjacent to the 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).
Kokanee Glacier Provincial Park is one of the oldest provincial parks in British Columbia, established in 1922. The park has an area of 320.35 km2 (123.69 sq mi) and is located in the Selkirk Mountains in the West Kootenays region of BC. The park has three glaciers that feed over 30 alpine lakes which are the headwaters of many creeks.
Bugaboo Provincial Park is a provincial park in British Columbia, Canada, located in the central Purcell Mountains.
The Purcell Wilderness Conservancy is a provincial park in British Columbia, Canada. It was established in 1974, and encompasses six large drainages in the Purcell Mountains in the southeast of the province. It contains high peaks, alpine meadows and ridges, deep creek and river valleys, and hot springs at Dewar Creek.
Pigeon Spire is a peak in the Purcell Mountains of the Columbia Mountains in southeastern British Columbia, Canada. It may be one of the most climbed of the spires in The Bugaboos owing to its relatively low prominence from the Vowell Glacier and the existence of an easy route. It is not uncommon to have a couple dozen people on this route on a busy weekend. There are longer, harder routes on the spire's North and East faces.
Kluane / Wrangell–St. Elias / Glacier Bay / Tatshenshini-Alsek is an international park system located in Canada and the United States, at the border of Yukon, Alaska and British Columbia.
The Beaver River, also known as the Beavermouth Creek or Beaver Creek, is a tributary of the Columbia River in British Columbia, Canada, joining that river in the Rocky Mountain Trench northwest of the town of Golden. It enters the Columbia via Kinbasket Lake.
Howser Spire, or Howser Spire Massif, is a group of three distinct granite peaks, and the highest mountain of the Canadian Bugaboo Spires. The mountain is located at the southwest corner of the Vowell Glacier, within the Bugaboo mountain range in the Purcell Mountains, a subrange of British Columbia's Columbia Mountains, The highest of the three spires is the North Tower at 3,412 m (11,194 ft), the Central Tower the lowest, and the South Tower is slightly lower than the North at 3,292 m (10,801 ft).
Jumbo Glacier, also known as Jumbo, was a mountain resort municipality within the Regional District of East Kootenay in southeast British Columbia, Canada between 2013 and 2021. It was approximately 55 km (34 mi) west of Invermere near the Commander Glacier and around the headwaters of Jumbo Creek in the Purcell Range of the Columbia Mountains.
The Purcell Trench, also known as the Kootenay River Valley is a large valley on the western side of the northern part of North America's Rocky Mountains. The trench extends approximately 179 miles (288 km) from Lake Pend Oreille, Idaho, down the Kootenay River (north) to Kootenay Lake, up the north arm to Duncan Lake. It joins the Rocky Mountain Trench another 50 miles (80 km) northward at the south tip of Kinbasket Lake, in British Columbia. The trench bottom is 1 to 7 miles wide and is 1,750 to 2,100 feet above sea level. The trench is nearly a straight north or south line. Some of its topography has been carved into U-shaped glacial valleys, it is primarily a product of geologic faulting. The trench splits the Columbia Mountains between the Purcell Mountains on the east and the Selkirk Mountains on the west.
The Purcell Supergroup is composed primarily of argillites, carbonate rocks, quartzites, and mafic igneous rocks of late Precambrian (Mesoproterozoic) age. It is present in an area of about 15,000 km2 (5,800 sq mi) in southwestern Alberta and southeastern British Columbia, Canada, and it extends into the northwestern United States where it is called the Belt Supergroup. It was named for the Purcell Mountains of British Columbia by R.A. Daly in 1912. Fossil stromatolites and algal structures are common in some of the Purcell Supergroup rocks, and the Sullivan ore body at Kimberley, British Columbia, a world-class deposit of lead, zinc, and silver, lies within the Alderidge Formation in the lower part of the Purcell.
Archduke Mountain is a 3,135-metre (10,285-foot) mountain summit located in the Purcell Mountains of British Columbia, Canada. It is situated 43 km (27 mi) north of Kaslo, on the northern boundary of Purcell Wilderness Conservancy Provincial Park and Protected Area. The nearest peak is Emperor Peak, 1 km (0.62 mi) to the west. These two peaks make up the double summit of the Archduke-Emperor massif. The mountain's name was officially adopted June 20, 1972, when approved by the Geographical Names Board of Canada. The mountain's name was submitted by climber Dr. Curt Wagner for Beethoven's Archduke Trio, which was dedicated to Archduke Rudolf of Austria.
Jumbo Mountain, sometimes called Mount Jumbo, is a 3,437 meter elevation mountain summit located 42 km (26 mi) west-southwest of Invermere in the Purcell Mountains of southeast British Columbia, Canada. The nearest higher peak is Mount Farnham, 11 km (6.8 mi) to the north-northeast, and Karnak Mountain is set 0.79 km (0.49 mi) to the west. Jumbo and Karnak form a double summit massif which is the second-highest mountain in the Purcells, and fourth-highest in the Columbia Mountains. The first ascent of Jumbo Mountain was made August 4, 1915, by H.O. Frind, A.H. & E.L. MacCarthy, M & W.E. Stone, B. Shultz, and Conrad Kain via the North/Northeast Slopes. March 5, 1919, Conrad made a solo ascent of Jumbo Mtn on snowshoes - credited as the first winter ascent of an 11,000-ft peak in Canada. The peak was named by Edward Warren Harnden after the 1892 Jumbo Mineral Claim on nearby Toby Creek, which in turn was named for Jumbo the elephant. The mountain's toponym was officially adopted March 31, 1924, when approved by the Geographical Names Board of Canada.