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The Liard River of the North American boreal forest flows through Yukon, British Columbia and the Northwest Territories, Canada. Rising in the Saint Cyr Range of the Pelly Mountains in southeastern Yukon, it flows 1,115 km (693 2 (107,000 sq mi) of boreal forest and muskeg.
The Dease River flows through northwestern British Columbia, Canada and is a tributary of the Liard River. The river descends from Dease Lake, though its ultimate origin is in the headwaters of Little Dease Creek at Snow Peak, approximately 50 kilometres (31 mi) west of the lake. The river flows 265 kilometres (165 mi) generally north-eastward, draining into the Liard River near Lower Post, British Columbia. Large sections of the river parallel the Cassiar Highway, helping to make it a popular destination for canoeists, kayakers, and rafters.
Hyland River Provincial Park is a provincial park in British Columbia, Canada, located near the boundary with Yukon along the Alaska Highway just east of the community of Lower Post and north of the Liard River. Established in 1964, the park is 34 ha. in area.
Kluskoil Lake Provincial Park is a provincial park in British Columbia, Canada, located on the West Road River downstream from the Euchiniko Lakes.
Saltery Bay Provincial Park is a provincial park in British Columbia, Canada, located southeast of the city of Powell River, and on the north side of the entrance to Jervis Inlet in the central area of that province's Sunshine Coast region.
Hat Creek is a tributary of the Bonaparte River in British Columbia, Canada, joining that stream at Carquile, which is also known as Lower Hat Creek and is the site of the Hat Creek Ranch heritage museum and visitor centre. The Hat Creek basin includes a broad upper plateau area encircled by the gentle but high summits of the Clear Range and, to its east, the Cornwall Hills; this area is known as Upper Hat Creek. Adjacent to Upper Hat Creek is the gateway to Marble Canyon and a rancherie of the Pavilion First Nation, who are both a St'at'imc and Secwepemc people. During the Fraser Canyon and Cariboo Gold Rushes an important trail northwards from the lower Fraser Canyon led from Foster Bar on the Fraser via Laluwissen Creek into Upper Hat Creek, then via the creek to the Bonaparte River. The economy of the basin is ranching-based and includes some of the oldest ranches in the British Columbia Interior. On the northwest edge of the Upper Hat Creek basin there is a large lignite deposit and several exploratory pits, some dating back to the 19th century but some more recent, part of an intended, but now shelved Hat Creek coal-thermal proposal.
The Nicoamen River is a tributary of the Thompson River in the southern Interior of British Columbia, Canada, located 15 kilometres (9 mi) upstream from its confluence with the Thompson at Lytton.
The Stikine Plateau is a plateau in northern British Columbia, Canada. It lies between the Boundary Ranges of the Coast Mountains on the west and southwest and the Cassiar Mountains along its northeast, and between the Skeena Mountains on its south and southeast and the Jennings and Nakina Rivers on the north.
The Horseranch Range is a 40 km (25 mi) long north–south trending mountain range in northern British Columbia, Canada, located at the head of the Red River to the northwest of Deadwood Lake. Part of the Dease Plateau of either the Yukon Plateau or Cassiar Mountains system, it contains no glaciers and lies completely above tree line.
The Dease Plateau is a sub-plateau of the larger Yukon Plateau, and is located in far northern British Columbia, Canada, northwest from the Deadwood River to and beyond the Yukon-British Columbia boundary. The plateau is named in association with Dease Lake and the Dease River. Very mountainous in some of its vast area, it is in some classification systems it is included as a subarea of the Cassiar Mountains.
The Ashnola River is a tributary of the Similkameen River, rising in the northeastern part of the North Cascades in Washington, United States, and flowing north into British Columbia, Canada, to join the Similkameen River about halfway along that river's course between the towns of Princeton and Keremeos. The river crosses the international boundary at 49°00′00″N120°19′37″W and transits Cathedral Provincial Park. It has one main tributary, Ewart Creek, which is about 25 kilometres (16 mi) long and begins virtually at the border and is entirely within Cathedral Park.
Blue River 1 is the Statistics Canada census-area designation for what is properly termed the Blue River Indian Reserve No. 1, an Indian reserve in the Cassiar Country of the Northern Interior of British Columbia, Canada. It is located on the left bank of the river of the same name at that river's confluence with the Dease River and is under the administration of the Liard First Nation, a member of the Kaska Tribal Council.
The Blue River is a tributary of the Dease River in the Cassiar Country of the Northern Interior of British Columbia, Canada, flowing southeast into the latter river at the Blue River Indian Reserve No. 1 of the Liard First Nation.
The Whiting River is a stream, about 50 miles (80 km) long, in the U.S. state of Alaska and the Canadian province of British Columbia. It enters the waters of Stephens Passage at the Borough of Juneau in the Alaska Panhandle between the mouths of the Taku and Stikine Rivers. The main tributary of the Whiting is the South Whiting. The river's basin is at the northern end of the Stikine Icecap The river crosses the international boundary at 58°11′00″N133°13′00″W. Its origin is in the Chechidla Range, and its terminus is at Gilbert Bay, which empties into Stephens Passage. In 1888, Lieutenant Commander C. M. Thomas of the U.S. Navy (USN) named the river for assistant surgeon Robert Whiting, USN, a member of his surveying party.
The Skwawka River is a medium-sized river in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, flowing southeast 20 kilometers (12 mi) into the head of Queens Reach, which is the uppermost end of Jervis Inlet. The pass at the head of the river, which connects to the head of the Little Toba River, is the prominence col for Mount Alfred, which lies just west of the river's mouth and is the highest summit between Jervis and Toba Inlets. Above the river's lower reaches, on the east flank of Mount Alfred, is 700 meters (2,300 ft) Alfred Creek Falls, one of North America's highest.
Cascade Falls is a waterfall on the Kettle River in the Boundary Country of the Southern Interior of British Columbia. They are located just south of Christina Lake and just north of the Canada–United States border in a gorge 200-300 yards long and just below the railway bridge over the Kettle by the southern mainline of the Canadian Pacific Railway. The ghost town of Cascade City aka Cascade is nearby and was named for the falls, even though they were not officially named until 1977.
The Cottonwood River is a tributary of the Dease River in the Cassiar Country of the Northern Interior of British Columbia, Canada. Rising in the northern Stikine Ranges just east of Toozaza Peak, and just south of the origins of the Jennings and Little Rancheria River near the border with Yukon, it flows south along the east flank of the Tuya Range to meet the Dease just north of that river's source at Dease Lake, between the north end of that lake and McDame Creek and the former mining centre and community of McDame Post.
The Trout River is a tributary of the Liard River in far northern British Columbia, Canada, flowing northwest from headwaters at 58°44′N126°14′W, near Muncho Lake, to meet the Liard at the community of Liard River. It is at the upper end of the Grand Canyon of the Liard, which is part of Liard River Corridor Provincial Park and Protected Area.
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.
References
- "Deadwood River". Geographical Names Data Base . Natural Resources Canada.
- "Dease Plateau". BC Geographical Names .
59°24′00″N128°13′00″W / 59.40000°N 128.21667°W