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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 Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).
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 Laurentian Mountains, also known as the Laurentians or Laurentides, are a mountain range in Canada. The range is 1,448 km long and ranges in height from 500 m with peaks over 1,000 m. The Laurentian Mountains extend across Labrador and Quebec within the Laurentian Upland, which contains foothills in northeastern Ontario. The range is located near the rivers of Ottawa, St. Lawrence, and Saguenay. The Laurentian Mountains primarily stretch across multiple regions in Quebec, with geologic formations such as the Jacques-Cartier Massif located within the range.
The Slate Range is a mountain range of the Canadian Rockies, located in Banff National Park, Canada. The range is named after slate, the primary composition of the mountains in the area.
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-inundated 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 Victoria Cross Ranges are a set of mountain ranges in the Canadian Rockies, located to the northwest of Jasper. Of the 19 peaks contained within this range, five are named after Canadian recipients of the Victoria Cross. The area of the ranges is 678 square kilometres (262 sq mi).
The Beaverfoot Range is a mountain range of the Canadian Rockies, located in southeastern British Columbia. The range extends from Cedared Creek near Spillimacheen north to the Kicking Horse River.
The Palliser Range is a mountain range of the Canadian Rockies that lies in the extreme southeast corner of Banff National Park, Alberta, Canada.
The Massive Range is a mountain range of the Canadian Rockies, located in the southwestern area of the Bow River valley in Banff National Park, Canada.
The Vermilion Range is a mountain range of the Canadian Rockies, in Banff National Park, Canada. The range is east of the Sawback Range and west of the Bare and Palliser Ranges.
The Waputik Range lies west of the upper Bow Valley, east of Bath Creek, and south of Balfour Creek in the Canadian Rockies. "Waputik" means "white goat" in Stoney. The range was named in 1884 by George Mercer Dawson of the Geological Survey of Canada. The President Range lies within the Waputik Range.
The Muskwa Ranges are a group of mountain ranges in northern British Columbia, Canada. They are part of the Northern Rockies section of the Rocky Mountains and are bounded on their west by the Rocky Mountain Trench and on their east by the Rocky Mountain Foothills. They are delimited on the north by the Liard River and on the south by the Peace Reach of the Lake Williston reservoir, south of which the next major grouping of the Rockies is the Hart Ranges.
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 High Rock Range is a mountain range of the Canadian Rockies in southwestern Alberta and southeastern British Columbia, Canada.
Crowsnest Range is a mountain range of the Rocky Mountains in southwestern Alberta and southeastern British Columbia, Canada.
The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeasternmost part of the Labrador Peninsula in northern Labrador and northern Quebec, Canada. It spans most of the eastern coast of Nunavut with high glaciated peaks rising through ice fields and some of Canada's largest ice caps, including the Penny Ice Cap on Baffin Island. It is bounded to the east by Baffin Bay, Davis Strait and the Labrador Sea while its northern portion is bounded by the Arctic Ocean.
Cirque Mountain is a mountain located 11 km (7 mi) northeast of Mount Caubvick, in Labrador, Canada. It is the third-highest mountain in Labrador, after Caubvick (1,652 m) and Torngarsoak Mountain (1,595 m), and lies in the Selamiut Range, which is a subrange of the Torngat Mountains. Before 1971, it was believed that Cirque Mountain was the highest peak in Canada east of the Rocky Mountains and south of Baffin Island; that distinction is now known to belong to Mount Caubvick.
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