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Divide Creek is a short creek near Kicking Horse Pass on the British Columbia/Alberta border (also the border between Yoho National Park and Banff National Park). After following the Continental Divide of the Americas for a short distance, the creek forks, with one side draining through the Bow River east to Hudson Bay and the Arctic Ocean, and the other side draining west to the Pacific Ocean by way of the Kicking Horse River.
Coordinates: 51°26′54.2″N116°17′05.4″W / 51.448389°N 116.284833°W
The Continental Divide of the Americas is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and Arctic oceans.
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.
Crowsnest Pass is a low mountain pass across the Continental Divide of the Canadian Rockies on the Alberta–British Columbia border.
Kootenay National Park is a national park of Canada in southeastern British Columbia. The park consists of 1,406 km2 (543 sq mi) of the Canadian Rockies, including parts of the Kootenay and Park mountain ranges, the Kootenay River and the entirety of the Vermilion River. While the Vermilion River is completely contained within the park, the Kootenay River has its headwaters just outside the park boundary, flowing through the park into the Rocky Mountain Trench and eventually joining the Columbia River. The park ranges in elevation from 918 m (3,012 ft) at the southwestern park entrance to 3,424 m (11,234 ft) at Deltaform Mountain.
The Big Hill on the Canadian Pacific Railway main line in British Columbia, Canada, was the most difficult piece of railway track on the Canadian Pacific Railway's route. It was situated in the rugged Canadian Rockies west of the Continental Divide of the Americas and Kicking Horse Pass. Even though the Big Hill was replaced by the Spiral Tunnels in 1909, the area has long been a challenge to the operation of trains and remains so to this day.
Kicking Horse Pass is a high mountain pass across the Continental Divide of the Americas of the Canadian Rockies on the Alberta–British Columbia border, and lying within Yoho and Banff national parks. Divide Creek forks onto both sides of the Continental Divide.
Triple Divide Peak is located in the Lewis Range, part of the Rocky Mountains in North America. The peak is a feature of Glacier National Park in the state of Montana in the United States. The summit of the peak, the hydrological apex of the North American continent, is the point where two of the principal continental divides in North America converge, the Continental Divide of the Americas and the Northern or Laurentian Divide.
Howse Pass is a pass through the Rocky Mountains in Canada. The pass is located in Banff National Park, between Mount Conway and Howse Peak. From here waters flow east via Conway Creek, Howse River, North Saskatchewan River to Lake Winnipeg and Hudson Bay. To the west it drains by the Blaeberry River to the Columbia River and on to the Pacific Ocean.
Athabasca Pass is a high mountain pass in the Canadian Rockies on the border between Alberta and British Columbia. In fur trade days it connected Jasper House on the Athabasca River with Boat Encampment on the Columbia River.
The Tonquin Valley is located in Jasper National Park, Alberta, Canada, next to the border of the provinces of Alberta and British Columbia, an area which is also the continental divide, running along the peaks of the South Jasper Range which rise above Amethyst Lake. Tonquin Creek drains Moat Lake and flows west into Mount Robson Provincial Park in British Columbia, and empties into the Fraser River. The Astoria River drains south and east into the Athabasca River.
Snow Dome is a mountain located on the Continental Divide in the Columbia Icefield, where the boundary of Banff National Park and Jasper National Park meets the border of Alberta and British Columbia in Canada. The summit's elevation is 3,456 m (11,339 ft).
The Waputik Icefield is located on the Continental divide in the Canadian Rocky Mountains, in the provinces of British Columbia and Alberta. It is developed on the heights of the Waputik Range in the Central Main Ranges.
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.
Alberta's Rockies comprise the Canadian Rocky Mountains in Alberta, Canada. On the southwestern part of the province along the British Columbia border, the region covers all but the south of Census Division 15.
A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not connected to the open sea. Every continent on earth except Antarctica has at least one continental drainage divide; islands, even small ones like Killiniq Island on the Labrador Sea in Canada, may also host part of a continental divide or have their own island-spanning divide. The endpoints of a continental divide may be coastlines of gulfs, seas or oceans, the boundary of an endorheic basin, or another continental divide. One case, the Great Basin Divide, is a closed loop around an endoreic basin. The endpoints where a continental divide meets the coast are not always definite since the exact border between adjacent bodies of water is usually not clearly defined. The International Hydrographic Organization's publication Limits of Oceans and Seas defines exact boundaries of oceans, but it is not universally recognized. Where a continental divide meets an endorheic basin, such as the Great Divide Basin of Wyoming, the continental divide splits and encircles the basin. Where two divides intersect, they form a triple divide, or a tripoint, a junction where three watersheds meet.
Simpson Pass, el. 2,107 m (6,913 ft), is a mountain pass on the border between the Canadian provinces of Alberta and British Columbia, in the area of the Ball Range. It is the prominence col for Mount Ball on the Continental Divide in the vicinity of Sunshine Village ski resort. Simpson River and Simpson Pass are named after Sir George Simpson who first explored the area in 1841.
The Banff-Windermere Highway, also known as the Banff-Windermere Parkway, is a 105 km (65 mi) highway which runs through the Canadian Rockies in British Columbia and Alberta in Canada. It runs from Radium Hot Springs, British Columbia to Castle Junction, Alberta, passing through Kootenay National Park and Banff National Park. It is designated as part of British Columbia Highway 93 and Alberta Highway 93.
A triple divide or triple watershed is a point on the Earth's surface where three drainage basins meet. A triple divide results from the intersection of two drainage divides. Triple divides range from prominent mountain peaks to minor side peaks, down to simple slope changes on a ridge which are otherwise unremarkable. The elevation of a triple divide can be thousands of meters to barely above sea level. Triple divides are a common hydrographic feature of any terrain that has rivers, streams and/or lakes.
The Committee's Punch Bowl is a small tarn on the continental divide straddling the border between the Canadian provinces of Alberta and British Columbia. George Simpson, governor of the Hudson's Bay Company, named the lake for the London-based managing committee of that company in 1824. While journeying on an important trade route in the company's trade area in what is now western Canada and parts of Alaska and the northwestern United States, he saw the lake at the summit of Athabasca Pass.