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 mi (4,800 km) 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 United States, 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 Basin 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 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 B.C. 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.
Kootenay National Park is a national park of Canada located 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.
Savona is a small community located at the west end of Kamloops Lake, where the Thompson River exits it. It is approximately halfway between Kamloops and Cache Creek along the Trans-Canada Highway. The countryside surrounding the community is semi-arid grasslands and hills, which support cattle ranching and agriculture. Savona has about 2000 hours of sunshine and less than 12 inches of precipitation a year. It has a population of approximately 650.
Yukon is in the northwestern corner of Canada and is bordered by Alaska and the Northwest Territories. The sparsely populated territory abounds with natural scenic beauty, with snowmelt lakes and perennial white-capped mountains, including many of Canada's highest mountains. The territory's climate is Arctic in territory north of Old Crow, subarctic in the region, between Whitehorse and Old Crow, and humid continental climate south of Whitehorse and in areas close to the British Columbia border. Most of the territory is boreal forest with tundra being the main vegetation zone only in the extreme north and at high elevations.
Bowron Lake Provincial Park is a provincial park located in northern British Columbia, Canada, roughly 117 km (73 mi) east of the city of Quesnel. Other nearby towns include Wells and the historic destination of Barkerville. Once a popular hunting and fishing destination, today the park is protected and known for its abundant wildlife, rugged glaciated mountains, and numerous freshwater lakes.
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.
Atlin/Áa Tlein Téix'i Provincial Park is a provincial park in British Columbia, Canada. Situated in the remote northwestern corner of the province, the park protects large tracts of boreal forest, alpine tundra and glaciated terrain. The southern third of Atlin Lake, the largest natural body of freshwater in the province, is within the park boundary. The park is very undeveloped; no roads traverse it and no facilities, supplies, developed campsites or maintained hiking trails are available inside the park. The area has become a focal point in controversies involving proposed hydroelectric projects affecting Atlin Lake and environmental groups who view these proposals as potentially damaging to the lake's environment and its surroundings.
Birkenhead Lake Provincial Park is a provincial park in British Columbia, Canada, located in the Lillooet Country region to the northeast of Pemberton and immediately northwest of Birkenhead Peak and Gates Lake at the community of Birken.
Height of the Rockies Provincial Park is a provincial park in the Canadian Rockies of south eastern British Columbia, Canada. It is located west of the Continental Divide, adjacent to Elk Lakes Provincial Park.
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.
Sugarbowl-Grizzly Den Provincial Park and Protected Area is a provincial park in British Columbia, Canada.
Divide Creek is a short creek near Kicking Horse Pass on the British Columbia/Alberta border. 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.
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.
The Tatlatui Range is a large and very alpine mountain range on the east flank of the upper Skeena River in northern British Columbia, Canada. It has an area of 2307 km2 and is a subrange of the Omineca Mountains which in turn form part of the Interior Mountains. The range features several lakes, the largest of which, Thutade Lake, is at the head of the Finlay River, and is considered the ultimate source of the Mackenzie River. Tatlatui Lake, the next largest lake in the range, to the northwest of Thutade Lake, is at the head of the Firesteel River, a tributary of the Finlay. Various summits of the range, which as described separates the Pacific and Arctic drainages, form part of the Continental Divide. Most of the range and its lakes are in Tatlatui Provincial Park.
Churn Creek is a tributary of the Fraser River in the Canadian province of British Columbia.
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.
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.
