The Skeena River is the second-longest river entirely within British Columbia, Canada. Since ancient times, the Skeena has been an important transportation artery, particularly for the Tsimshian and the Gitxsan—whose names mean "inside the River of Mist", and "people of the River of Mist," respectively. The river and its basin sustain a wide variety of fish, wildlife, and vegetation, and communities native to the area depend on the health of the river. The Tsimshian migrated to the Lower Skeena River, and the Gitxsan occupy territory of the Upper Skeena.
Thutade Lake is located in the Omineca Mountains of the Northern Interior of British Columbia, Canada. About 40 km (25 mi) in length, and no more than about 2 km (1.2 mi) wide, the lake is primarily significant as the ultimate source of the Mackenzie River. The lake is at the head of the Finlay River, which joins the Peace River via Williston Lake. The area is very remote, being located about 260 km (160 mi) north of Smithers, although several mining operations for ores containing copper, lead, zinc and silver have occurred around the lake. The largest of these is the Kemess Mine, an iron and copper property originally owned by Royal Oak Mines and now by Northgate Minerals, located in the valley of Kemess Creek, which is off the northeast end of Thutade Lake. The mine is accessed by the Omineca Resource Road and other resource routes, and is 400 km (250 mi) by road from Prince George. Just downstream from the outlet of Thutade Lake, the Finlay plunges over the 180-foot (55 m) Cascadero Falls, and then through a series of cataracts in a twisting course until it begins its main northeastward trend. Cascadero Falls is slated for hydroelectric development in connection with the power needs of the area's mines.
Kwadacha, also known as Fort Ware or simply Ware, is an aboriginal community in northern British Columbia, Canada, located in the Rocky Mountain Trench at the confluence of the Finlay, Kwadacha and Fox Rivers, in the Rocky Mountain Trench upstream from the end of the Finlay Reach of Williston Lake. The population is about 350. It is in the federal electoral riding of Prince George-Peace River.
The Omineca Mountains, also known as "the Ominecas", are a group of remote mountain ranges in the Boreal Cordillera of north-central British Columbia, Canada. They are bounded by the Finlay River on the north, the Rocky Mountain Trench on the east, the Nation Lakes on the south, and the upper reaches of the Omineca River on the west. They form a section of the Continental Divide, that, in this region, separates water drainage between the Arctic and Pacific Oceans. The lower course of the Omineca River flows through the heart of the range. To the south of the Ominecas is the Nechako Plateau, to the west the Skeena Mountains and Hazelton Mountains, to the north the Spatsizi Plateau and the Stikine Ranges, while east across the Rocky Mountain Trench are the Muskwa Ranges.
The Skeena Mountains, also known as the Skeenas, are a subrange of the Interior Mountains of northern British Columbia, Canada, essentially flanking the upper basin of the Skeena River. They lie just inland from the southern end of the Boundary Ranges of the Coast Mountains, and also of the northern end of the Kitimat Ranges. Their southern limit is described by the Bulkley River and the upper northwestern reaches of Babine and Takla Lakes, and on their northeast by the upper reaches of the Omineca River.
The Nechako Plateau is the northernmost subdivision of the Interior Plateau, one of the main geographic regions of the Canadian province of British Columbia. It spans the basin of the Nechako River and its tributaries the Stuart River and Endako Rivers, and is bounded on the south by the West Road River, south of which is the Chilcotin Plateau and on the north by the Nation River and the valleys of Babine and Takla Lakes, beyond which are the Omineca Mountains (N) and Skeena Mountains (NW). To the west, it abuts the various ranges of the Hazelton Mountains while on its east it is bounded by the pass between Prince George, British Columbia and the Parsnip Arm of Williston Lake, beyond which is the McGregor Plateau, which skirts the Northern Rockies. Some classification systems include the plateau area on the east bank of the Fraser River beyond the city of Prince George; this area neighbours the northernmost reaches of the Quesnel Highland and Cariboo Mountains.
The British Columbia Interior, popularly referred to as the BC Interior or simply the Interior, is a geographic region of the Canadian province of British Columbia. While the exact boundaries are variously defined, the British Columbia Interior is generally defined to include the 14 regional districts that do not have coastline along the Pacific Ocean or Salish Sea, and are not part of the Lower Mainland. Other boundaries may exclude parts of or even entire regional districts, or expand the definition to include the regional districts of Fraser Valley, Squamish–Lillooet, and Kitimat–Stikine.
Frank Cyril Swannell was one of British Columbia's most famous surveyors.
The Thumb is a mountain located 7 km (4 mi) south of Sitchiada Mountain on the east side of Bear Lake, on the divide between the upper Omineca River and the basin of the Bear River in the Omineca Country of the Central-North Interior of British Columbia, Canada. As the Omineca is part of the Arctic Ocean drainage, via the Peace and Mackenzie Rivers, and the Bear is in the basin of the Skeena River, which drains to the Pacific, The Thumb is located on the Continental Divide.
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 Metsantan Range are a mountain range between the upper Stikine and the Finlay River drainages in northern British Columbia, Canada. It has an area of 1116 km2 and is a subrange 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 Mitchell Range is a subrange of the Hogem Ranges of the Omineca Mountains, bounded by Takla Lake and the Nation River in northern British Columbia, Canada.
The Fishing Range is a subrange of the Swannell Ranges of the Omineca Mountains, located on the east side of Fishing Lakes and on the upper Finlay River in northern British Columbia, Canada.
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.
Bear Lake, formerly known as Fort Connelly or Fort Connolly, or Connolly's Lake, is an unincorporated settlement located on the northeast side of the lake of the same name, which lies to the north of Babine Lake and Takla Lake in the northwestern end of the Omineca Country in the North-Central Interior of British Columbia, Canada. At the same location is Takla Lake First Nation's Bear Lake Indian Reserve No. 4.
Bear Lake is a large lake in the northwestern Omineca Country of the North-Central Interior of British Columbia, Canada, located north of Babine and Takla Lakes. Unlike those two lakes, which are part of the Fraser River drainage, Bear Lake is a tributary to the Skeena River via the Bear River, which runs from its northern end. The community of Bear Lake, also known as Fort Connelly, is located on the lake's northeast side. The original Fort Connelly may have been, however, at the lake's northern end or on an island in Tsaytut Bay.
The Wolverine Range is a small subrange of the Swannell Ranges of the Omineca Mountains, located west of Williston Lake and south of Omineca Arm in northern British Columbia, Canada.
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.
Pelly Peak, is a 2,048-metre (6,719-foot) mountain summit in the Russel Range of the Omineca Mountains in northern British Columbia, Canada. The mountain is situated west of the head of Finlay Reach of Williston Lake, and a remote 67 km (42 mi) south of Fort Ware in the Cassiar Land District. It rises 1,250 m (4,100 ft) above the south shore of Pelly Lake. Its nearest higher peak is Barrier Peak, 5.0 km (3.1 mi) to the east. Precipitation runoff from the mountain drains into Pelly Creek, a tributary of the Ingenika River. Sir John Pelly (1777–1852) served as Governor of Hudson's Bay Company for three decades, and his name is attached to many geographic features in Canada, including but not limited to Pelly River, Pelly Mountains, Pelly Island, Pelly Bay, Mount Pelly, and Fort Pelly. The peak's name was officially adopted June 4, 1953, by the Geographical Names Board of Canada. Based on the Köppen climate classification, Pelly Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
