The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 miles in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west.
Yoho National Park is a national park of Canada. It is located within the Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia, bordered by Kootenay National Park to the south and Banff National Park to the east in Alberta. The word Yoho is a Cree expression of amazement or awe, and it is an apt description for the park's spectacular landscape of massive ice fields and mountain peaks, which rank among the highest in the Canadian Rockies.
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.
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.
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 Robson Provincial Park is a provincial park in the Canadian Rockies with an area of 2,249 km2. The park is located entirely within British Columbia, bordering Jasper National Park in Alberta. The B.C. legislature created the park in 1913, the same year as the first ascent of Mount Robson by a party led by Conrad Kain. It is the second oldest park in the provincial system. The park is named for Mount Robson, which has the highest point in the Canadian Rockies and is located entirely within the park.
Mount Joffre is a mountain located on the Continental Divide, in Peter Lougheed Provincial Park, Alberta, and Elk Lakes and Height of the Rockies Provincial Parks in British Columbia. The mountain was named in 1918 by the Interprovincial Boundary Survey after Marshal Joseph Joffre, commander-in-chief of the French Army during World War I.
The Yellowhead Pass is a mountain pass across the Continental Divide of the Americas in the Canadian Rockies. It is located on the provincial boundary between the Canadian provinces of Alberta and British Columbia, and lies within Jasper National Park and Mount Robson Provincial Park.
The Great Divide Trail (GDT) is a wilderness hiking trail in the Canadian Rockies. The trail closely follows the Great Divide between Alberta and British Columbia, crossing the divide more than 30 times. Its southern terminus is in Waterton Lakes National Park at the Canada–US border and its northern terminus is at Kakwa Lake in Kakwa Provincial Park, north of Jasper National Park. The trail is 1,130 km (700 mi) long and ranges in elevation from 1,055 m (3,461 ft) at Old Fort Point trailhead near Jasper to 2,590 m (8,500 ft) at an unnamed pass above Michele Lakes just south of the White Goat Wilderness Area.
Laudonia is an extinct genus of trilobites that lived during the early part of the Botomian stage, which lasted from approximately 524 to 518.5 million years ago. This faunal stage was part of the Cambrian Period. There are currently two named species assigned to it.
The Lynx Formation or Lynx Group is a stratigraphic unit of Late Cambrian (Dresbachian) age in the Western Canada Sedimentary Basin. It is present in the Canadian Rockies of Alberta and British Columbia. It was originally described as the Lynx Formation by Charles Doolittle Walcott in 1913, based on and named for outcrops on the slopes of Lynx Mountain on the continental divide east of Mount Robson. It was subdivided into five formations and elevated to group status by J.D. Aitken and R.G. Greggs in 1967. The name Lynx Formation continues to be used in areas where some or all of the subdivisions cannot be distinguished. All of the formations in the Lynx Group include fossil trilobites and some contain the stromatolite Collenia.
Division Mountain is located on the Continental Divide along the Alberta - British Columbia border of Canada. It also straddles the shared boundary of Banff National Park with Kootenay National Park in the Canadian Rockies. It was named in 1919 by Charles D. Walcott since the mountain divides the Lyell Icefield from the Mons Icefield.
Quadra Mountain is located on the border of Alberta and British Columbia on the Continental Divide. It was named in 1910 by Arthur Oliver Wheeler. The name refers to the mountain's four pinnacles. However, in 1952 the form of the name was changed to Mount Quadra in the mistaken belief that it had been named after Juan Francisco de la Bodega y Quadra—mountains named for people taking the form "Mount Person's Name". In 1983 the form was changed back to Quadra Mountain by British Columbia and Alberta, and in 1984 by Parks Canada.
Wonder Peak is located on the border of Alberta and British Columbia in the Canadian Rockies. Situated on the Continental Divide, it also straddles the shared boundary of Banff National Park with Mount Assiniboine Provincial Park. It was named in 1913 by Arthur O. Wheeler and Conrad Kain.
Aye Mountain is located on the Canadian provincial boundary between Alberta and British Columbia on the Continental Divide. It was named in 1913 by the Interprovincial Boundary Survey.
Resplendent Mountain, or Mount Resplendent is a peak in the Canadian Rockies, located at the northern end of Mount Robson Provincial Park in British Columbia, Canada. It is a part of the Rainbow Range, and is a sister peak to the more famous Mount Robson, its nearest neighbour. Together they form a classic panorama seen by travellers from the VIA railway and Highway 16. The mountain was named by Arthur P. Coleman, and Arthur O. Wheeler wrote, "On the east side it is clad from top to bottom in pure white snow, and presents with the sun shining upon it a spectacle of such wonderful brilliance that the aptness of the name became immediately apparent." The first ascent was achieved on the same historic 1911 trip in which Conrad Kain first scouted the climbing routes later to be used on the first ascent of Mount Robson.
The Miette Group is an assemblage of metamorphosed sedimentary rocks of latest Precambrian (Neoproterozoic) age. It is present in the Canadian Cordillera from the Lake Louise area of Alberta to the Yukon. The Miette rocks include Ediacaran fossils, stromatolites, and trace fossils.
The Arctomys Formation is a stratigraphic unit of late Middle Cambrian age. It is present on the western edge of the Western Canada Sedimentary Basin in the Canadian Rockies of Alberta and British Columbia. It was named for Arctomys Peak near Mount Erasmus in Banff National Park by Charles Doolittle Walcott in 1920. Outcrops of the Arctomys can be seen in Banff and Jasper National Parks.
The Titkana Formation is a stratigraphic unit of Middle Cambrian age that is present on the western edge of the Western Canada Sedimentary Basin in the northern Canadian Rockies of Alberta and British Columbia. It was named for Titkana Peak near Mount Robson by Charles Doolittle Walcott in 1913. The Titkana Formation is generally unfossiliferous.
