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.
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.
The Winston Churchill Range is a mountain range in the central section of the Park Ranges of the Canadian Rockies located in Jasper National Park. The range was named after Sir Winston Churchill, former British prime minister.
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).
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.
The Premier Range is a group of mountains within the Cariboo Mountains of east-central British Columbia, Canada. The range is bounded by the Raush River and Kiwa Creek to the north, the North Thompson River on the south and west and the Fraser River and its tributaries to the east.
Mount Sir John Abbott is a 3,398-metre (11,148 ft) mountain located in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. It is located at the south end of the west wall of Kiwa Glacier, the source of Kiwa Creek.
Mount Sir John Thompson is a 3,349 m (10,988 ft) mountain located at co-ordinates 52°44′N119°44′W in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. The mountain is located between the David and North Canoe Glaciers.
Mount Stanley Baldwin is a mountain located in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. The mountain is located at the head of the Gilmour Glacier. It was originally named Mount Challenger by Allen Carpé during his 1924 ascent of the mountain.
Mount Sir MacKenzie Bowell is a 3,301 m (10,830 ft) mountain peak located at co-ordinates 52°49′54″N119°43′48″W in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. The mountain is located between the Kiwa and Tete glaciers.
Mount John Oliver is a 3,123-metre (10,246 ft) mountain in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. The mountain is located on the divide between the Kiwa and Tete Creeks and is covered by a glacier.
Mount Louis Saint Laurent is a 3,045 m (9,990 ft) mountain located at co-ordinates 52°45′34″N119°47′07″W in the Premier Range of the Cariboo Mountains in the east-central interior of British Columbia, Canada. The mountain is to the west of the David Glacier and overlooks the Raush River.
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.
The Spearhead Range is a short subrange of the Garibaldi Ranges of southwestern British Columbia, Canada, adjacent to the resort town of Whistler, British Columbia and ending at its northwestern apex in Blackcomb Mountain, one of two mountains forming the Whistler Blackcomb ski resort. Other notable summits are Tremor Mountain, The Spearhead, Mount Macbeth, Decker Mountain, Mount Trorey, Phalanx Mountain and Shatter, Shudder, Quiver and other similarly named peaks and glaciers. The range was named by Don and Phyllis Munday as the range's peaks resembled spearheads rising from the alpine fog. To the north of the range is Lone Goat Pass, formed by Wedge Creek and Lone Goat Creek, which is fed by the Spearhead Glacier, the largest glacier in the range. The valley of Fitzsimmons Creek is on the range's south side, and is the location of the Whistler Sliding Centre, which was built for the 2010 Winter Olympics.
The Dawson Range is a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located southeast of Rogers Pass in Glacier National Park. The highest point is Mount Dawson. Other peaks of the range include Mount Selwyn, Mount Donkin, and Mount Fox.
Asperity Mountain is a mountain located in British Columbia, Canada, rising to 3,716 metres (12,192 ft). It is located between Tellot and Tiedemann Glaciers on the north and south respectively, in the Waddington Range, a subrange of the Pacific Ranges. The gorge of the Homathko River runs north to south on the east side of the mountain, carrying runoff from the mountain and glaciers to the Pacific Ocean.
Mount McKenzie, Mount MacKenzie or Mount Mackenzie may refer to:
Chaos Glacier is part of the Waddington Range in the southern British Columbia Coast Mountains in Canada, located at 51°25′25″N125°15′5″W. It flows to the north from Mount Tiedemann for approximately four kilometers before joining the larger Scimitar Glacier. The name was officially adopted in 1978 from field sketches of the area by mountaineer Don Munday. The area's steep terrain makes this an excellent example of a continuous ice fall.
Franklin Glacier is a mountain glacier in the Waddington Range of the Pacific Ranges in southwestern British Columbia, Canada. It lies at the head of the Franklin River adjacent to Mount Waddington, the highest mountain entirely within British Columbia.
