| Germansen Range | |
|---|---|
  Germansen Range Location in British Columbia | |
| Highest point | |
| Elevation | 1,644 m (5,394 ft)  |
| Geography | |
| Country | Canada |
| Province | British Columbia |
| Range coordinates | 55°37′N124°53′W / 55.617°N 124.883°W |
| Parent range | Swannell Ranges (Omineca Mountains) |
The Germansen Range is a small subrange of the Swannell Ranges of the Omineca Mountains, bounded by Germansen Lake and South Germansen River northern British Columbia, Canada.
The Bare Range is a mountain range of the Canadian Rockies, located south of the Red Deer River valley in Banff National Park, Canada. The range is named for the "bareness" of or lack of trees on the gentle slopes of the range.
The Beaverfoot Range is a mountain range in the Kootenay Ranges 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 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.
Omineca River is a river of the North American boreal forest, in northern British Columbia, Canada. It flows into 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. According to Father Adrien-Gabriel Morice the name is derived from a Sekani word meaning 'lake-like or sluggish river'.
The Thudaka Range is a mountain range located east of the Rocky Mountain Trench in British Columbia, Canada bounded by the Obo River on the east, the Frog River on the west, and on the south by the pass between Geese and Thudaka Creeks. The highest peak in the range is Thudaka Peak at 2,748 m (9,016 ft). The range is part of the Stikine Ranges.
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 did not 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 Swannell Ranges are a mountain range between the Finlay and Nation Rivers and between the Hogem Ranges and the Finlay Ranges of northern British Columbia, Canada. It has an area of 22932 km2 and is a subrange of the Omineca Mountains which in turn form part of the Interior Mountains. They are named in honour of legendary surveyor/explorer Frank Swannell.
The Hogem Ranges are a group of mountain ranges in the northwest part of the Omineca Country of the North-Central Interior of British Columbia, Canada, located between Takla Lake (W) and the Omineca River (E) and from the Nation Lakes (SE) to the Sustut River (NW). The ranges have a collective area of 8868 km2 and is a subgrouping of the Omineca Mountains which in turn form part of the Interior Mountains.
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.
The Bulkley Ranges are a 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.
Wedge Pass, also known as Billygoat Pass, 1430 m (4692 ft), is a mountain pass in the northern Garibaldi Ranges, the southwesternmost subdivisions of the Pacific Ranges of the Coast Mountains in British Columbia, Canada. Located immediately on the southern flank of Wedge Mountain and to the immediate north of the Spearhead Range, site of the Blackcomb half of the Whistler Blackcomb Ski Area, it connects the head of Wedge Creek (W), a tributary of the Green River with those of Billgoat Creek (E), a tributary of the Lillooet River. The pass is within Garibaldi Provincial Park and has no road access.
The Lizard Range is a mountain range southwest of Fernie, British Columbia in the Canadian Rockies. The 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.
The Germansen River is in the Omineca region of central British Columbia, Canada. Flowing through Germansen Lake, the river is a major tributary of the Omenica River, which in turn enters Williston Lake. Surrounded by the spread of the Swannell Ranges, the lake is south of Plughat Mountain and north of the Germansen Range, which contains Mount Germansen.
Manson River is a river located in the Omineca Country region of British Columbia. It flows north into Manson Arm, Williston Lake. The river is located south of Germansen Landing. It was first known as Manson Creek and was discovered in 1871 by Robert Howell. The river has been mined using wing-damming, drifting and hydraulicking. Manson River has been mined by Europeans and Chinese.
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