Bishop River Provincial Park is a provincial park in the Pacific Ranges of the Coast Mountains on the Mainland of British Columbia, Canada, located southwest of and adjoining Ts'yl-os Provincial Park."Bishop River Park". BC Geographical Names. It lies along the upper course of the Bishop River, the main tributary of the Southgate River, from the Bishop's source at the western side of the Lillooet Icecap to midway along its course above its confluence with the Southgate. The park is 19,947 ha. in size. There are no roads or trails in the park although a forest service road from Waddington Harbour at the head of Bute Inlet leads up the Southgate to within a few miles of the park boundary.
Cariboo River Provincial Park is a provincial park in British Columbia, Canada, located between Barkerville and Likely in the upper Cariboo River basin.
Canal Flats Provincial Park was a provincial park in British Columbia, Canada, located at Canal Flats at the divide between Columbia Lake and the Kootenay River in the province's East Kootenay region. The park had been established in 1981 at approximately 6 hectares in size. In 2004, the park was converted from Order In Canada to Statute Designation and the size remained at approximately 6 hectares. The park status was cancelled in 2010 and the property is currently pending transfer to local government jurisdiction.
Columbia Lake Provincial Park is a provincial park in British Columbia, Canada, located on the northeast shore of Columbia Lake south of the town of Invermere. The park was established in 1988, comprising approximately 260 hectares. Its boundary was expanded in 2004, the total now comprising approximately 290 hectares, 275 hectares of which is upland, 15 hectares of which is foreshore.
Chilliwack Lake Provincial Park is a provincial park in British Columbia, Canada. Covering 92.58 km², the park is located 150 km east of Vancouver in the Chilliwack River Valley.
Denetiah Provincial Park is a provincial park in British Columbia, Canada. It is part of the larger Muskwa-Kechika Management Area. Established in 1999 and at 90,379 ha. in area, it is located west of the Kechika River between the Turnagain and Frog Rivers. The park includes Denetiah Lake and Dall Lake. Dune Za Keyih Provincial Park and Protected Area is to its east across the Kechika, while the Dall River Old Growth Provincial Park is on its northwest flank. Horneline Creek Provincial Park is 30 km to the north.
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.
Nimpkish Lake Provincial Park is a provincial park on northern Vancouver Island, British Columbia, Canada on Vancouver Island. The park is 3,949 ha. in area and was established on 1995. It is 32 km south of Port McNeill and on the southwest side of Nimpkish Lake. Primary access is by boat launch, though radio-controlled logging roads lead to the edge of the park. Western Forest Products in Woss, British Columbia should be contacted for road advisories. The park is in the traditional territory of the Namgis First Nation.
Tatlatui Provincial Park is a provincial park in British Columbia, Canada, located at the southern end of the Spatsizi Plateau and around the headwaters of the Firesteel River, part of the Finlay-Peace River basin and therefore in the Arctic drainage. Thutade Lake, at the head of the Firesteel and to the southeast of the park, is considered the ultimate source of the Mackenzie River.
The Turnagain River is a river in the Canadian province of British Columbia.
The Nahatlatch River is a tributary of the Fraser River in the Canadian province of British Columbia. It originates in the Lillooet Ranges of the Coast Mountains and empties into the Fraser River in the Fraser Canyon, north of Boston Bar.
The Cassiar River is a tributary of the Turnagain River in far northern British Columbia, flowing north to join the latter river southeast of Cry Lake. Its name is a reference to the Cassiar Land District, which it flows through the middle of and was the setting of the Cassiar Gold Rush of the 1870s.
Cornice Peak, 2093 m, is a mountain in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It is located on the west side of the Kimsquit River just northwest of the head of Dean Channel. The Kapella River, a tributary of the Kitlope, rises on the west side of Cornice Peak.
The Kispiox River is a river in the Skeena Country of British Columbia, Canada. It is a tributary of the Skeena River, flowing southeast to meet that river above its confluence with the Bulkley near Hazelton. It forms the eastern boundary of the Kispiox Range subdivision of the Hazelton Mountains.
The Nekite River is a river in the Central Coast region of British Columbia, Canada, flowing south to the head of Smith Inlet. Nekite Indian Reserve No. 2 is located at the mouth of the river and is one of the many reserves of the Gwa'sala-'Nakwaxda'xw Nations band government located in the area of Smith Sound, of which Smith Inlet is the uppermost part.
Drury inlet is an inlet in the Queen Charlotte Strait region of the Central Coast of British Columbia, Canada, extending west from Wells Passage to the northwest of North Broughton Island, northwest of the town of Port Hardy. Branching off to the northeast from the north side of the head of the inlet is Actaeon Sound.
The Bishop River is a river in the Pacific Ranges of the Coast Mountains, flowing west from the western edge of the Lillooet Icecap to join the Southgate River east of the Homathko Icefield. Bishop River Provincial Park surrounds the upper course of the river, from the source at the Lillooet Icecap to midway along its course above its confluence with the Southgate.
The Major Hart River is a river in northern British Columbia, Canada, flowing northeast into the Turnagain River, a tributary of the Kechika, southwest of the community of Liard River.
The Claud Elliott Creek Ecological Reserve is located southwest of the junction of Claud Elliott Creek and the Tsitsika River on northern Vancouver Island, southwest of the community of Sayward. The reserve, which was created to protect representative old-growth montane forests, was established in 1989, comprising approximately 231 hectares. It was expanded slightly in 2004 to a current total area of approximately 233 hectares.
The Nation River, formerly known as the Tribe River and originally in French as the Rivière au Nation, is a river in the Northern Interior of British Columbia, Canada, originally a tributary of the Parsnip River, it now feeds Lake Williston via Nation Arm of that lake, which is the reservoir formed by WAC Bennett Dam. The town of Mackenzie is to the southeast of the river's terminus at the lake.
