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The Kechika River is a tributary of the Liard River, about 300 kilometres (190 mi) long, in northern British Columbia, Canada. The Kechika flows generally northwest through the northernmost section of the Rocky Mountain Trench before turning east to join the Liard, a major branch of the Mackenzie River system. The river's 22,700 km2 (8,800 sq mi) drainage basin is characterized by high glaciated peaks, boreal forest, and open tundra. With no settlements, roads or dams along its course, the Kechika is considered "one of British Columbia's finest examples of wilderness and undisturbed wildlife habitat."
Liard River Hot Springs Provincial Park is a provincial park in British Columbia, Canada. It is home to the second largest natural hot springs in Canada, after Deer River Hot Springs 15 km to the north east. It is a natural river of hot water rather than a spring fed man made pool. The park is part of the larger Muskwa-Kechika Management Area. The community of Liard River, British Columbia is located nearby.
Dall River Old Growth Provincial Park is a provincial park in British Columbia, Canada. It is part of the larger Muskwa-Kechika Management Area and is located immediately northwest of Denetiah Provincial Park, northwest of the junction of the Gataga and Kechika Rivers. Established in 1999, the park is 642 ha. in area. The park protects areas of white spruce old growth.
Prophet River Hot Springs Provincial Park is a provincial park in British Columbia, Canada. Established high in the Muskwa Ranges, on the course of the Prophet River, it is part of the larger Muskwa-Kechika Management Area.
Redfern-Keily Provincial Park was a provincial park in British Columbia, Canada.
Tetsa River Provincial Park is a former provincial park in British Columbia, Canada. It is part of the larger Muskwa-Kechika Management Area. It is located on the north side of the Tetsa River at the confluence of Mill Creek, and is on the Alaska Highway.
The Stikine Ranges are a group of mountain ranges and mountainous plateaus in northwestern British Columbia, Canada. They are the northernmost subdivision of the Cassiar Mountains and among the least explored and most undeveloped parts of the province.
Strand Fiord Pass is a mountain pass on southern Axel Heiberg Island, Nunavut, Canada.
The Gataga River is a river in the Northern Rockies of British Columbia, Canada. It is a tributary of the Kechika River, which is a tributary of the Liard.
The Sikanni Chief River, is a river in the Northern Rocky Mountains region of the northern interior of British Columbia, Canada. Its headwaters are near Mount McCusker, northeast of the head of the Finlay Arm of Williston Lake. It joins the Fontas River to form the Fort Nelson River southeast of the town of Fort Nelson. However, among the local population the Fontas is viewed only as a tributary of the Sikinni Chief, in the view that the Sikanni continues to exist, flowing northwest to where it meets the larger Muskwa River where the Fort Nelson River is actually formed in the eyes of the indigenous Dene, Cree and European-descendant populations of Fort Nelson First Nation and Fort Nelson.
The Telkwa Range is a subrange of the Bulkley Ranges, located south of the junction of the Telkwa River and Bulkley River in northern British Columbia, Canada.
Fimbulheimen is a mountain range in Queen Maud Land, Antarctica. It stretches from Jutulstraumen by 1° west of Carsten Borchgrevink Ice at 18° east, about 200 km from the ice edge. Fimbulheimen is thus between Maudheim Plateau and Sør-Rondane.
The Koeye Range is a small mountain range in southwestern British Columbia, Canada, located between the Koeye River and Elizabeth Lake. It has an area of 68 square kilometres (26 sq mi) and is a subrange of the Pacific Ranges which in turn form part of the Coast Mountains.
The Rocky Mountain Foothills are an upland area flanking the eastern side of the Rocky Mountains, extending from the Liard River in British Columbia southward into Alberta. Bordering the Interior Plains system, they are part of the Rocky Mountain System or Eastern System of the Western Cordillera of North America.
The Frog Lakes are a group of lakes, drained eastward by an unnamed stream feeding the Frog River, a tributary of the Kechika River in the Stikine Ranges of the northern interior of British Columbia. Though not the hydrological source of the Frog River, the lakes are in an east–west aligned valley which forms the divide between the basins of the Stikine River and that of the Liard, and are therefore on the Continental Divide between the Pacific and Arctic drainages. Draining from their west is the Pitman River, a Stikine tributary, from an unnamed lake just to their west, while the Kechika is a major tributary of the Liard, which is a tributary of the Mackenzie. Frog Lakes Pass, at an elevation of 1015 m (3330 ft), is the prominence col for the 2668 m (8753 ft) Sharktooth Mountain, giving it a prominence of 1653 m.
Horneline Creek Provincial Park is a provincial park in far northern British Columbia, Canada. It is located west of the Kechika River about 130 km south of Lower Post and 30 km north of Denetiah Provincial Park and southwest of the community of Liard River.
The Red River is a tributary of the Kechika River in the far north of British Columbia, Canada, flowing east to meet the Kechika from headwaters in the Cassiar Mountains. In its middle reaches it forms the boundary between the Dease Plateau (N) and the Cassiar Mountains (S) and for its final stretch it crosses part of the Liard Plain. It is crossed by an unnamed road about 17.5 kilometres (10.9 mi) upstream from its confluence with the Kechika, and is just to the north of Aeroplane Lake.
The Liard Plain is a landform in far northern British Columbia, Canada. It is located between the Smith River and the Dease Plateau.
The Major Hart River is a river in northern British Columbia, Canada, flowing north-east into the Turnagain River, a tributary of the Kechika, south-west of the community of Liard River.
The Dall River is a river in northern British Columbia, Canada, flowing northwest into the Turnagain River, a tributary of the Kechika, to the west of Mount Skook Davidson. Originally named the Cold Fish River, it was renamed in 1944 to avoid confusion with another river of that name that is a tributary of the Spatsizi, and because of the presence of Dall's sheep in the area. Dall Lake is along its course, south of Dall River Old Growth Provincial Park, which lies between the lake and the confluence with the Turnagain. Denetiah Provincial Park, on the river's upper course, includes Dall Lake.
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58°45′00″N127°30′00″W / 58.75000°N 127.50000°W
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