| Junction Sheep Range Provincial Park | |
|---|---|
  Map of British Columbia | |
| Location | Lillooet Land District, British Columbia, Canada |
| Nearest city | 100 Mile House, BC |
| Coordinates | 51°47′59″N122°25′19″W / 51.79972°N 122.42194°W |
| Area | 4,774 ha. (47.74 km2) |
| Established | July 13, 1995 |
| Governing body | BC Parks |
Junction Sheep Range Provincial Park is a provincial park in British Columbia, Canada, located near the confluence of the Chilcotin and Fraser Rivers on the west bank of the latter river.
The Chilcotin Region began its history of agricultural settlements just as the Cariboo Gold Rush was waning in the 1860s. Two of the earliest ranches in this area were the Cotton and Deer Park Ranches, now amalgamated as Riske Creek Ranching. Settlement followed the accessible bunchgrass ranges along the terraces of the Chilcotin River between 1873 and 1893, and ranges have been used for livestock grazing since 1873. There is also historical evidence of mining in the area; remnants of old Chinese placer mining activities have been found at the confluence of the Fraser and Chilcotin Rivers. In 1973, a 4,573 hectare Wildlife Reserve, managed by the Fish and Wildlife Branch, was established to protect the bighorn sheep and their natural grassland habitat. This reserve was designated as the Junction Wildlife Management Area in 1987, and was designated a provincial park in 1995.
The area protects critical breeding, lambing, and winter range of the largest population of non-migratory California bighorn sheep in the world, a blue-listed species. Approximately 500 bighorn sheep live in the area, feeding on bunchgrass and other low growing plants, and finding refuge from predators in the steep breaks at the edges of grassland benches. In the past, the Junction California bighorn sheep have also provided a source of sheep for transplants to other areas of North America where the sheep had been extirpated.
The following recreational activities are available: horseback riding and hunting. There is no camping allowed within the park. The park is only open to the public during hunting season.
Located 60 kilometres south of Williams Lake, British Columbia. Access to the park is difficult, via rough 4 x 4 dirt roads through private ranchlands.
4,774 hectares in size.
51°48′00″N122°25′20″W / 51.8000°N 122.4222°W
Highway 20, also known as the Chilcotin Highway, and officially dubbed the Alexander MacKenzie Highway, is one of the two main east–west routes in the Central Interior of British Columbia (the other being Highway 16. The Chilcotin Highway runs 457 km from Williams Lake westward through the Chilcotin region to North Bentinck Arm, an inlet from the Pacific Ocean where the town of Bella Coola is located. As of 2019, all but 42 km has been paved, mostly for expediting the removal of timber from the region, which, like most of British Columbia, is afflicted with pine beetle infestations. Logging traffic and ranch-related traffic on the route can be expected.
The Bridge River is an approximately 120 kilometres (75 mi) long river in southern British Columbia. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of Lillooet; its flow, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project, with the water now entering the Fraser just south of Lillooet as a result.
The Chilcotin region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is also the name of the river draining that region. In the language of the Tsilhqot'in people, their name and the name of the river means "those of the red ochre river". The proper name of the Chilcotin Country, or Tsilhqotʼin territory, in their language is Tŝilhqotʼin Nen.
The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This 19,200 km2 (7,400 sq mi) watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, 22 km (14 mi) upstream from Gang Ranch.
The Chilcotin Ranges are a subdivision of the Pacific Ranges of the Coast Mountains. They lie on the inland lea of the Pacific Ranges, abutting the Interior Plateau of British Columbia. Their northwestern end is near the head of the Klinaklini River and their southeast end is the Fraser River just north of Lillooet; their northern flank is the edge of the Plateau while their southern is the north bank of the Bridge River. In some reckonings they do not go all the way to the Fraser but end at the Yalakom River, which is the North Fork of the Bridge.
The Camelsfoot Range is a sub-range of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains in British Columbia. The Fraser River forms its eastern boundary. The range is approximately 90 km at its maximum length and less than 30 km wide at its widest.
The Yalakom River is a tributary of the Bridge River, which is one of the principal tributaries of the Fraser River, entering it near the town of Lillooet, British Columbia. In frontier times it was also known as the North Fork of the Bridge River, and joins the Bridge River proper at Moha, a rural community with a history in ranching, farming and mining. The river is approximately 50km in length. The valley's climate is semi-arid in character and lodgepole pine predominates below treeline.
The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau that itself is a northward extension of the North American Plateau. The southern limit of the plateau is the Bonaparte River although some definitions include the Bonaparte Plateau between that river and the Thompson, but it properly is a subdivision of the Thompson Plateau. The portion of the Fraser Plateau west of the Fraser River is properly known as the Chilcotin Plateau but is often mistakenly considered to be part of the Cariboo Plateau, which is east of the Fraser.
Pink Mountain may refer to an unincorporated community on the Alaska Highway, a nearby mountain, or the hunting guiding territory west of the mountain.
Cathedral Provincial Park and Protected Area, usually known as Cathedral Provincial Park and also as Cathedral Park, is a provincial park in British Columbia, Canada. It is located east of E.C. Manning Provincial Park, south of BC Highway 3, and southeast of the town of Princeton, and southwest of Keremeos. Its southern boundary is the border with the United States. Much of the park is the basin of the Ashnola River. Cathedral Park is home to teal sub-alpine lakes, vast ridges and jarred peaks, old-growth forests, and rock formations of siltstone, granodiorite, and basalt. Hikers can scramble along various peaks such as the 8000-foot Grimface Mountain and Lakeview Mountain. Tourists flock to Smokey the Bear and Stone City because of their unique formations with incredible views formed by millennia of erosion, volcanic and tectonic activity, and glacial recession.
Tsʼilʔos Provincial Park is a provincial park in British Columbia, Canada. Tsʼilʔos is the official BC Parks designation for this provincial park, though sometimes it is written as "Tsʼil-os", "Tsʼyl-os", or "Tsylos". The "ʔ" in the name represents a glottal stop.
Itcha Ilgachuz Provincial Park is a provincial park in the Chilcotin Country of British Columbia, Canada. The park is 111,977 hectares in size and contains Far Mountain and Mount Downton, its two most prominent peaks.
The Spruce Lake Protected Area, formerly known variously as the Southern Chilcotin Mountains Provincial Park, Southern Chilcotins, and also as South Chilcotin Provincial Park, is a 71,347-hectare Protected Area in the British Columbia provincial parks system, approximately 200 km north of Vancouver. The area had been the subject of an ongoing preservationist controversy since the 1930s. In 2007, its status as a provincial park was downgraded to protected area.
Syringa Park is a provincial park on the east shore of Lower Arrow Lake in the West Kootenay region of southeastern British Columbia. At the foot of the Norns Range, Tulip Creek passes through the centre, and Syringa Creek is closer to the southeastern boundary. The park is about 19 kilometres (12 mi) west of Castlegar via Broadwater Rd.
Tyaughton Creek, formerly gazetted as the Tyaughton River, also historically known as Tyoax Creek, is a 50 kilometre tributary of British Columbia's Bridge River, flowing generally southeast to enter the main flow of that river about mid-way along the length of Carpenter Lake, a reservoir formed by Terzaghi Dam of the Bridge River Power Project.
Gold Bridge is an unincorporated community in the Bridge River Country of British Columbia, Canada. Although numbering only around 40 inhabitants, Gold Bridge is the service and supply centre for the upper basin of the Bridge River Valley, which includes recreation-residential areas at the Gun Lakes, Tyaughton Lake, Marshall Creek, and Bralorne; and the nearby ghost towns of Brexton and Pioneer Mine.
The Churn Creek Protected Area is a 36,747-hectare (90,800-acre) provincial protected area in British Columbia, Canada. It is a mix of dryland canyon and steppe and adjoining rangeland flanking the canyon of Churn Creek and that stream's confluence with the Fraser River at the northern apex of the Camelsfoot Range. The historic Gang Ranch is just north of the Churn Creek Protected Area. The Empire Valley Ranch ecological preserve was added to the Protected Area in an expansion.
Churn Creek is a tributary of the Fraser River in the Canadian province of British Columbia.
The Cascade Mountains leeward forests are a temperate coniferous forest ecoregion of North America, as defined by the World Wildlife Fund (WWF) categorization system.
South Chilcotin Mountains Provincial Park is a provincial park in British Columbia, Canada, located on Highway 40 northwest of Lillooet, British Columbia. The park, which is 56,796 ha. in size, was established on April 18, 2001, and It was created out of a portion of the Spruce Lake Protected Area. The park is located on three Indigenous Nations: The Tsilhqot’in, St’at’imc, and Secwepemc.
