Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain on the Great Divide, on the British Columbia/Alberta border in Canada.
Mount Columbia is a mountain located in the Winston Churchill Range of the Rocky Mountains. It is the highest point in Alberta, Canada, and is second only to Mount Robson for height and topographical prominence in the Canadian Rockies. It is located on the border between Alberta and British Columbia on the northern edge of the Columbia Icefield. Its highest point, however, lies within Jasper National Park in Alberta.
Mount Garibaldi is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of 2,678 metres and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago. These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley.
Garibaldi Provincial Park, also called Garibaldi Park, is a wilderness park located on the coastal mainland of British Columbia, Canada, 70 kilometres (43.5 mi) north of Vancouver. It was established in 1920 and named a Class A Provincial Park of British Columbia in 1927. The park is a popular destination for outdoor recreation, with over 30,000 overnight campers and over 106,000 day users in the 2017/2018 season.
Tumbler Ridge is a district municipality in the foothills of the B.C. Rockies in northeastern British Columbia, Canada, and a member municipality of the Peace River Regional District. With a population of 2,399 (2021) living in a townsite, the municipality encompasses an area of 1,558 km2 (602 sq mi) of mostly Crown land. The townsite is located near the confluence of the Murray River and Flatbed Creek and the intersection of Highway 52 and Highway 29 and includes the site of the Tumbler Ridge Secondary School and Tumbler Ridge Airport. It is part of the Peace River South provincial electoral district and the Prince George—Peace River—Northern Rockies federal riding.
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).
Chetwynd is a district municipality located in the eastern foothills of the Rocky Mountains, in northeastern British Columbia, Canada. Situated on an ancient floodplain, it is the first town eastbound travellers encounter after emerging from the Rockies along Highway 97, and acts as the gateway to the Peace River Country. The town developed during the construction of infrastructure through the Rocky Mountains in the 1950s; additionally, it was used as a transshipment point during the building of hydroelectric dams, in the 1960s and 1970s, and the new town of Tumbler Ridge, in the early 1980s. Home to approximately 2,600 residents, the town’s population has increased little—if at all—since the 1980s, but is significantly younger than the provincial average.
The North Shore Mountains are a mountain range overlooking Vancouver in British Columbia, Canada. Their southernmost peaks are visible from most areas in Vancouver and form a distinctive backdrop for the city.
Wapiti Lake Provincial Park is a 16,837-hectare (41,610-acre) provincial park in British Columbia, Canada. It is 60 kilometres (37 mi) south of Tumbler Ridge, at the headwaters of Wapiti River, including its watershed from the Wapiti Pass to Wapiti Lake in the Canadian Rockies. The area contains significant amounts of fossils (ichthyosaurs) and fossil beds. There is habitat for grizzly bears, mountain goats, and bull trout. It was established as a Provincial Park on June 26, 2000. It is recognized by the provincial government as being an area traditionally used by First Nations people. Hunting and fishing are permitted in the park.
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.
The Hart Ranges are a major subrange of the Canadian Rockies located in northeastern British Columbia and western Alberta. The mountains constitute the southernmost portion of the Northern Rocky Mountains.
Sentinel Peak, is a 2,513-metre (8,245 ft) isolated, prominent limestone peak, west of the Continental Divide in British Columbia, Canada. It is highest summit in Misinchinka Ranges, a subdivision range of the Hart Ranges within the Northern Rocky Mountains.
The Northern Rocky Mountains, usually referred to as the Northern Rockies, are a subdivision of the Canadian Rockies comprising the northern half of the Canadian segment of the Rocky Mountains. While their northward limit is easily defined as the Liard River, which is the northward terminus of the whole Rockies, the southward limit is debatable, although the area of Mount Ovington and Monkman Pass is mentioned in some sources, as south from there are the Continental Ranges, which are the main spine of the Rockies forming the boundary between British Columbia and Alberta. Some use the term to mean only the area north of the Peace Arm of the Williston Reservoir, and in reference to Northern Rocky Mountains Provincial Park, while others consider the term to extend all the way south, beyond the limit of the Hart Ranges at Mount Ovington, to include the McBride area, the Sir Alexander Group and Mount Robson.
Nub Peak is a 2,746-metre (9,009-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Nestor Peak, 4.0 km (2.5 mi) to the west. The mountain is situated north of Sunburst Peaks, with Elizabeth Lake and Cerulean Lake in between. The Continental Divide and Assiniboine Pass are situated 3.5 km (2.2 mi) to the east. Nub Peak is famous for its panoramic view of Mount Assiniboine with its surrounding lakes and peaks. The mountain's descriptive name was officially adopted in 1924. An arm extending southwest from Nub is officially known as Chucks Ridge, and an arm extending southeast is officially called Nublet. Nub Peak is composed of sedimentary rock laid down during the Cambrian period and pushed east over the top of younger rock during the Laramide orogeny.
Mount King George is a prominent 3,413-metre (11,198-foot) mountain summit located in Height of the Rockies Provincial Park, in the Canadian Rockies of British Columbia, Canada. The mountain is the highest point of The Royal Group, a subset of the Rockies, which includes Mount Queen Mary, Mount Princess Mary, Mount Prince George, Mount Prince Albert, Mount Prince Henry, Mount Prince John, and Mount Prince Edward. Its nearest higher peak is Mount Joffre, 16.0 km (9.9 mi) to the east. Mount King George is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.
Gladsheim Peak is a prominent 2,830-metre (9,280-foot) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Gladsheim is the highest point in the Valhalla Ranges. It is situated in the southern part of Valhalla Provincial Park, 2.7 km (1.7 mi) northeast of Gimli Peak, and 12 km (7.5 mi) west of Slocan and Slocan Lake. The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. Gladsheim is the magnificent meeting hall containing thirteen council seats where, according to Norse mythology, Odin presided over all the realms. In keeping with the Valhalla theme, this peak's name was submitted in 1900 by R. W. Brock to the Geological Survey of Canada for consideration, and it was officially adopted March 31, 1924, by the Geographical Names Board of Canada.
Murray Range is a subdivision range of the Hart Ranges, of the Northern Rockies in British Columbia, Canada. The majority of the range lies within the Pine-Lemoray Provincial Park and is noted for its snowmobiling, hiking and ski touring opportunities. The boundaries of the Murray Range generally lie between the Misinchinka River to the west and Mountain Creek to the east; the Pine River to the north and Mount Reynolds to the south.
Mount Crysdale, is a 2,427-metre (7,963 ft) ultra-prominent, isolated peak in the Misinchinka Ranges, a subdivision range of the Hart Ranges, within the Northern Rocky Mountains.
Mount Morfee, is a 1,775 metre peak in the Misinchinka Ranges, a subdivision range of the Hart Ranges, within the Northern Rocky Mountains. The mountain is known locally as Morfee Mountain and features prominently over the town Mackenzie, BC.
