The Rocky Mountains, also known as the Rockies, are a major mountain range in western North America. The Rocky Mountains stretch more than 4,800 kilometers (3,000 mi) from the northernmost part of British Columbia, in western Canada, to New Mexico in the Southwestern United States. Located within the North American Cordillera, the Rockies are somewhat distinct from the Pacific Coast Ranges, Cascade Range, and the Sierra Nevada, which all lie farther to the 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 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 latter term is also sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U.S. term, as in North Cascades National Park. 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 comprise the Canadian segment of the North American Rocky Mountains. They are the eastern part of the Canadian Cordillera, which is a system of multiple ranges of mountains which runs from the Canadian Prairies to the Pacific Coast. The Canadian Rockies mountain system comprises the southeastern part of this system, lying between the Interior Plains of Alberta and Northeastern British Columbia on the east to the Rocky Mountain Trench of BC on the west. The southern end borders Idaho and Montana of the United States. In geographic terms the boundary is at the Canada/US border, but in geological terms it might be considered to be at Marias Pass in northern Montana. The northern end is at the Liard River in northern British Columbia.
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 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 Columbia Mountains are a group of mountain ranges along the upper Columbia River in southeastern British Columbia, and also in 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 Kootenay 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).
The Palliser Range is a mountain range of the Canadian Rockies that lies in the extreme southeast corner of Banff National Park.
Chase Provincial Park is a provincial park in British Columbia, Canada, located around Carina and Tomias Lakes, 70km north of Germansen Landing in the Omineca Mountains just to the west of the Finlay Arm of Williston Lake. The park was in established 2001, comprising approximately 36,226 hectares.
Omineca River is a river in northern British Columbia, Canada. It flows into the Williston Lake, and is part of the Peace River basin. It was originally a tributary of the Finlay River before the creation of Lake Williston.
The Tuya Range is a rmountain range in the Stikine Ranges of the Cassiar Mountains in the far north of the Canadian province of British Columbia, near its border with the Yukon Territory and to the southwest of Watson Lake, Yukon, which is the nearest major settlement.
The Interior Mountains, also called the Northern Interior Mountains and Interior Ranges, are the semi-official names for a huge area that comprises much of the northern two thirds of the Canadian province of British Columbia and a large area of southern Yukon.
The Omineca Gold Rush was a gold rush in British Columbia, Canada in the Omineca region of the Northern Interior of the province. Gold was first discovered there in 1861, but the rush didn't begin until late in 1869 with the discovery at Vital Creek. There were several routes to the goldfields: two were from Fort St. James, one of which was a water route through the Stuart and Tachie Rivers to Trembleur Lake to Takla Lake and the other was overland, called the Baldy Mountain route. A third route came in overland from Hazelton on the Skeena River and a fourth route used the Fraser River and crossed over the Giscome Portage to Summit Lake, through McLeod Lake, and up the Finlay River to the Omineca River.
The Bulkley Ranges is mountain range in northern British Columbia, Canada, located between the Skeena and Bulkley Rivers south of Hazelton, north of the Morice River and Zymoetz River. It has an area of 7851 km2 and is a subrange of the Hazelton Mountains which in turn form part of the Interior Mountains.
The Babine Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Babine Lake, Babine River, Bulkey River and Skeena River in northern British Columbia, Canada.
The Lizard Range is a mountain range south-east of Fernie, British Columbia in the Canadian Rockies. This range is home to the Fernie Alpine Resort and parts of the Mount Fernie Provincial Park.
The Sustut River is a major tributary of the Skeena River in the north-central Interior of British Columbia, Canada. It forms the northwest boundary of the Hogem Ranges and flows southwest to meet the Skeena, north of Hazelton. Originally named the Bear Wallow River, its headwaters are at Sustut Lake, northwest of Germansen Landing.
Sustut Lake is a lake in the Omineca Mountains of the Northern Interior of British Columbia, Canada, located northwest of Germansen Landing in the Cassiar Land District. It is the source of the Sustut River, which flows roughly west and is a major tributary of the Skeena River. The lake's old, or alternate, name is Bear Wallow Lake. Sustut Peak is located to the west of the lake.
Germansen Landing is an unincorporated settlement on the Omineca River, at the confluence of that river and its tributary the Germansen, in the Northern Interior of British Columbia, Canada. The settlement was a focus of the Omineca Gold Rush of the 1860s. A Hudson Bay Supply post there supplied the miners and trappers. Placer mining continued into the 1930s, when the Depression created a market for gold. The area is very remote and required multiple lake and trail journeys to get to from Fort Saint James. Today, access is four hours by dirt logging road from Mackenzie along the west shore of Williston Lake.
The Germansen River, formerly Germansen Creek, is a major south tributary of the Omenica River in the Northern Interior of British Columbia, Canada. The settlement and former gold-rush centre of Germansens Landing is located at its confluence with the Omineca. Along its course is Germansen Lake at 55°41′45″N124°51′10″W, south of which is the Germansen Range and Mount Germansen.
