Top Attractions in Cariboo

Canim Falls

Canim Falls is a waterfall on the Canim River between Canim and Mahood Lakes in the Cariboo region of the Central Interior of British Columbia, Canada. It is 25 m high. The waterfall has eroded steadily upstream and created a 4 km long canyon cut into a lava plateau associated with the Wells Gray-Clearwater volcanic field. Canim Falls is inside the boundary of Wells Gray Provincial Park. A trail from Mahood Lake Road leads to Canim Falls and nearby Mahood Falls. "Canim" means a type of large canoe in the Chinook Jargon.

Canim Beach Provincial Park

Canim Beach Provincial Park is a provincial park in British Columbia, Canada, located at the southwest end of Canim Lake in the Interlakes District of the South Cariboo region, adjacent to the Secwepemc Indian reserve community of Canim Lake, British Columbia just northeast of 100 Mile House. The park was established by Order-in-Council in 1956 and expanded by later legislation in 2000 and 2004 to total a current approximate of 8.2 hectares . "Canim" means a type of large canoe in the Chinook Jargon.

Rainbow Range

The Rainbow Range, formerly known as the Rainbow Mountains, is a mountain range in British Columbia, Canada, located 40 kilometres northwest of Anahim Lake. Located on the western edge of the Chilcotin Plateau, the range adjoins the Coast Mountains Pacific Ranges to the south, and the Kitimat Ranges to the north. In some classification systems it is considered part of the Coast Mountains. It lies north of the Bella Coola and Atnarko Rivers and south and west of the Dean River, which curves around its north flank, and is relatively drier in climate and easier of terrain than more mountainous areas immediately west. Once called Tsitsutl, meaning "rainbow mountains" in the Ulkatcho dialect of the Carrier language, that name is now the name of the ranges highest peak.

Quesnel Lake

Quesnel Lake is a glacial lake or fjord in British Columbia, Canada, and is the origin of the Quesnel River. With a maximum depth of 506 meters, it is the deepest lake in British Columbia, though not the deepest lake in Canada, as is often claimed. That distinction belongs to Great Slave Lake. It is claimed to be the deepest fjord lake in the world. On August 4, 2014, the tailings pond of Mount Polley mine burst, spilling toxic effluent into Polley Lake and Quesnel Lake and temporarily depriving residents of Likely, British Columbia, of fresh water for household use.

Mahood Lake

Mahood Lake is a lake in the South Cariboo region of the Interior of British Columbia in Wells Gray Provincial Park. It is drained by the Mahood River, a tributary of the Clearwater River which has cut a deep canyon into Cambrian rocks and Pleistocene glacial moraines. Mahood Lake is fed by the short Canim River, which drains nearby Canim Lake to the west via Canim Falls and Mahood Falls. The lake is 629 metres in elevation, 197 metres deep at its deepest point, approximately 33.5 km² in area, 21 km in length and a maximum of 2.2 km in width. Mount Mahood is immediately south of the lake and rises to 1,812 m .

Chilko Lake

Chilko Lake is a 180 km² lake in west-central British Columbia, at the head of the Chilko River on the Chilcotin Plateau. The lake is about 65 km long, with a southwest arm 10 km long. It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation. It and Harrison Lake are the largest lakes in the southern Coast Mountains.

Barkerville

Barkerville was the main town of the Cariboo Gold Rush in British Columbia, Canada and is preserved as a historic town. It is located on the north slope of the Cariboo Plateau near the Cariboo Mountains 80 kilometres east of Quesnel along BC Highway 26, which follows the route of the original access to Barkerville, the Cariboo Wagon Road.

Alexandria

Alexandria or Fort Alexandria is a National Historic Site of Canada on the Fraser River in British Columbia, and was the end of the Old Cariboo Road and the Cariboo Wagon Road. It is located on Highway 97, 103 miles north of 100 Mile House and 28 miles south of Quesnel.

Wells

Wells is a small mining and tourist town in the Cariboo District of central British Columbia, located on BC Highway 26, 74 km from Quesnel and 8 km before the highway's terminus at Barkerville. It gains much of its revenue and jobs from tourists who pass through on their way to the Bowron Lake Provincial Park and to the historic museum town of Barkerville.

Williams Lake Indian Reserve No. 1

Williams Lake Indian Reserve, also called the Williams Lake Band Reservation and commonly referred to locally as the Sugarcane Reserve, aka Sugarcane or The Cane or SCB, is an Indian Reserve in British Columbia, Canada, located at the east end of Williams Lake and 12 km south of the city of the same name, on the right bank of the San Jose River. and is home to the Williams Lake Indian Band. The band is part of the Northern Shuswap Tribal Council, also known as the Cariboo Tribal Council, which is one of two tribal councils of the Secwepemc peoples. The Williams Lake Band has eight reserve landsites in British Columbia. The total area of Williams Lake Indian Band reserve land is 1,927.3, with the Williams Lake Reserve the largest at 1645.30 ha. The other reserve lands of the Williams Lake Band are: Asahal Lake Indian Reserve No. 2, at the head of Azahal Creek, 3 miles north of the east end of Williams Lake, 48.60 ha. Carpenter Mountain Indian Reserve No. 15, on the Old Cariboo Road, near the 156 Mile Post west of Cariboo Hill Lake, 68.30 ha. Chimney Creek Indian Reserve No. 5, on the left bank of the Fraser River at the mouth of Chimney Creek, 22.70 ha. Five Mile Indian Reserve No. 3, on Five Mile Creek 3.5 miles north of the mouth of the San Jose River, four miles north of 150 Mile House. 73.00 ha. James Louie Indian Reserve No. 3A, on Five Mile Creek, 4 miles north of 150 Mile House east of an adjoining Five Mile IR No. 3, 64.00 ha. San Jose Indian Reserve No. 6, on the west end of Williams Lake, north of its outlet, 2.60 ha. Tillion Indian Reserve No. 4, on the left bank of the Fraser River, at the mouth of Williams Lake River, 2.40 ha.

Cariboo River Provincial Park

Cariboo River Provincial Park is a provincial park in British Columbia, Canada, located between Barkerville and Likely in the upper Cariboo River basin. Located between Kimball and Cariboo Lakes, the park was established in 1995, comprising 3212 hectares. Its boundaries were revised in 2010, the total area now being 3211 hectares.

Horsefly Lake

Horsefly Lake is a lake in the eastern Cariboo region of the Central Interior of British Columbia, Canada. It lies at the head of the Horsefly River, a tributary of the Quesnel River, and is one of several large lakes at the verge of the Cariboo Plateau and the Cariboo Mountains; Quesnel Lake, the largest of those, is to its north and northwest. The lakes name first appeared on maps with Joseph Trutchs 1871 publication, and is credited with being so named because of the preponderance of horseflies in the area during summer. Horsefly Lake Provincial Park is located on its northwestern shore.

Far Mountain

Far Mountain is the highest of over 13 peaks in the Ilgachuz Range in the Anahim Volcanic Belt in British Columbia, Canada. The Ilgachuz Range is one of the three major shield volcanoes that formed the Anahim Volcanic Belt when the North American Plate moved over a hotspot . This is similar to the one which feeds the Hawaiian Islands. The mountain is located in the western part of Itcha Ilgachuz Provincial Park.

Mahood Falls

Mahood Falls is a waterfall in Wells Gray Provincial Park located on the Canim River between Canim Lake and Mahood Lake and northeast of 100 Mile House, British Columbia, Canada. The waterfall is 20 m high. Mahood Falls is also a small community spread out along 5 km of road east of Roserim Lake and south of Canim Lake. Population is about 50 people. There was a post office there until 1990, but presently there are no stores or services. Nearby Mahood Lake and, later, the Mahood Falls community were named after James Adam Mahood who was in charge of a Canadian Pacific Railway survey in this area in 1872. Joan Uhrig was born in 1935 at Canim Lake and grew up on the McNeil Ranch, now operated by the third generation of McNeils. According to her, the waterfall was unnamed during the familys early years at Canim Lake and considered to be part of nearby Canim Falls. When the post office was established in the 1950s and named Mahood Falls, tourists on the new road to Mahood Lake began asking for directions to see the waterfall. Answering repeatedly that there was no waterfall became so tiresome that the McNeils selected this waterfall to which they could send the curious tourists. Only the community, not the waterfall, is an official name in the British Columbia Gazetteer. Access to Mahood Falls is by a short trail off the Mahood Lake Road. Trail signage on the road says only Canim Falls. It is a 10-minute walk to see Mahood Falls first, then 10 minutes further to see Canim Falls. Both are on the Canim River, downstream from Canim Lake, where there is a large island; the north channel goes over Mahood Falls and the south channel over Canim Falls.

Chilcotin River

The Chilcotin River is a 241-kilometre long tributary of the Fraser River in southern British Columbia, Canada. It drains the Chilcotin Plateau, which lies between the Fraser River and the Coast Mountains. It starts northeast of Itcha Mountain and flows generally southeast to join the Fraser about 22 km upstream from Gang Ranch. Source elevation derived from Google Earth. Mouth elevation derived from Google Earth. Benke, Arthur C.; Cushing, Colbert E. . Field Guide to Rivers of North America. Academic Press. pp. 314–315. ISBN 978-0-12-378577-0. Retrieved 5 August 2013. "Archived Hydrometric Data Search". Water Survey of Canada. Retrieved 17 August 2013. Search for Station 08MB005 Chilcotin River below Big Creek "A Guide to Aboriginal Organizations and Services in British Columbia 2011 / 2012" . p. VII. Retrieved 17 November 2013. "Chilcotin River". BC Geographical Names.

Lava Canyon

Lava Canyon is a canyon on the Chilko River in the Chilcotin District of the Interior of British Columbia, Canada, located about 35 kilometres below the Chilkos outflow from the foot of Chilko Lake. Lava Canyon is named for the columnar basalt cliffs that form the canyon from former extensive volcanic activity of this region.

Anahim Peak

Anahim Peak, sometimes mistakenly called Anaheim, is a volcanic cone in the Anahim Volcanic Belt in British Columbia, Canada, located 39 km northwest of Anahim Lake and 11 km east of Tsitsutl Peak. It was formed when the North American Plate moved over a hotspot, similar to the one feeding the Hawaiian Islands, called the Anahim hotspot. It is one of the several volcanoes in the Anahim Volcanic Belt that stands out all by itself, rising from the Chilcotin Plateau, between the Rainbow Range and the Ilgachuz Range and near the headwaters of the Dean River.

Ilgachuz Range

The Ilgachuz Range is a name given to an extinct shield volcano in British Columbia, Canada. It is not a mountain range in the normal sense, because it was formed as a single volcano that has been eroded for the past 5 million years. It lies on the Chilcotin Plateau, located some 350 kilometres north-northwest of Vancouver and 30 km north of Anahim Lake. The highest peak of the range is Far Mountain. The range supports a unique grassland ecosystem. This type of grassland has not been seen anywhere else in central and southern British Columbia. The climate is cool and dry; typical of higher elevations of the Interior Plateau. The 280 kilometres long West Road River rises in the Ilgachuz Range and flows east to its confluence with the Fraser River between Prince George and Quesnel. It drains an area of approximately 12,000 km2, and dropping over 900 m before joining with the Fraser.

Itcha Range

The Itcha Range is a small isolated mountain range in the West-Central Interior of British Columbia, Canada. It is located 40 km northeast of Anahim Lake on the Chilcotin Plateau. With a maximum elevation of 2,375 m, it is the lowest of three mountain ranges extending east from the Coast Mountains. Two mountains are named in the Itcha Range; Mount Downton and Itcha Mountain. A large provincial park surrounds the Itcha Range and other features in its vicinity. More than 15 animal species are known to exist in the Itcha Range area, as well as a grassland community that is limited only to this location of British Columbia. The Itcha Range resides in the territory of aboriginal peoples who have occupied this region for centuries. This area has a relatively dry environment compared to the Coast Mountains in the west. In contrast to most mountain ranges in British Columbia, the Itcha Range represents an inactive shield volcano. This highly dissected volcanic edifice consists of a variety of rock types, including basanite, hawaiite, trachyte, rhyolite, phonolite and alkali olivine basalt. They were deposited by different types of volcanic eruptions characterized by passive lava flows and explosivity. Two stages of eruptive activity have been identified at the volcano along with three sub-phases that are limited only to the first stage of development. The main body of the Itcha Range is between 3.8 and 3.0 million years old and thus over two million years ago it passed the most active shield stage of life. A long period of dormancy lasting for almost a million years followed, which was interrupted by the post-shield stage of volcanism 2.2 to 0.8 million years ago. More recent volcanic activity in and around the Itcha Range might have occurred in the last 340,000 years to produce cinder cones. The Itcha Range is part of an east-west trending volcanic zone called the Anahim Volcanic Belt. This consists of large shield volcanoes, small cinder cones, lava domes and lava flows that become progressively younger from west to east. Several explanations have been made regarding the creation of this feature, each citing a different geologic process. If volcanic activity were to resume at the Itcha Range, Canadas Interagency Volcanic Event Notification Plan is prepared to notify people threatened by eruptions.

Canim Lake

Canim Lake is a lake in British Columbia, Canada. Its west end is 36 km northeast of 100 Mile House. "Canim" means a type of large canoe in the Chinook Jargon. Canim Lake is 26.5 km long. It is also part of the territory of the Shuswap First Nation where the ancestors are part of the Lake Division of the Shuswap Tribe of the Interior Nations of British Columbia. The Reilly Commission states that the 2,029 hectares region around Canim Lake are set aside for the Shuswap First Nation. In the summer of 1995, there was an archaeological evidence of an ancient civilization and evidence of carbon dated as 4,300 old.

Taseko Lakes

The Taseko Lakes are a pair of lakes, Upper Taseko Lake and Lower Taseko Lake, which are expansions of the upper Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada. Their name is based on the original in the Chilcotin language, Dasiqox Biny, where "Desiqox" means "Mosquito River" and is cognate to the name of the river as in English; the Chilcotin name refers to both lakes as one lake, which was also originally the case with the English usage until official designation of the separate lakes in 1954. The lakes are separated by the short Taseko Narrows, the name of which in Chilcotin is nanatsakash, and is an important crossing place for deer. The Tchaikazan River flows the area between the upper lower lake from the southwest, while the Taseko River feeds it from the southeast, while the equally large Lord River joins it from the south, at the head of the lake.

Tatlayoko Lake

Tatlayoko Lake is a lake on the Homathko River in the western Chilcotin District of the Central Interior of British Columbia, Canada, located on a north-south axis just upstream of the entrance of the series of canyons of the Homathko, including the Great Canyon of the Homathko, on its route to the sea at the head of Bute Inlet. The community of Tatlayoko Lake, British Columbia is located at its northern end.

Cottonwood House Historic Site

Cottonwood, including the Cottonwood Ranch and Cottonwood House, is an unincorporated settlement in the North Cariboo region of the Central Interior of British Columbia, Canada. Originally a ranch, it is located in the northern Cariboo Plateau, just 8 km northwest of Coldspring House, which is at the confluence of the Swift River and Lightning Creek, which is the beginning of the Cottonwood River. Lightning Creek was one of the more famous of the gold-bearing creeks of the Cariboo Gold Rush.

Fort Chilcotin

Fort Chilcotin was a short-lived trading post of the Hudson's Bay Company, located at the confluence of the Chilko and Chilcotin Rivers, British Columbia, Canada. It operated between the years 1836 and 1844. A commercial failure due to the lack of interest in the company merchandise shown by the Tsilhqot'in people, its operations were moved north to Fort Kluskus in Dakelh Territory. Today, the site where the fort used to stand is colloquially known as "Hudson's Bay Flats" - remembered particularly by the Tsilhqot'in (via oral history) as the site where, during the Chilcotin War, Lhats'as?in and the other Tsilhqot'in war chiefs were deceitfully lured and wrongfully arrested.

Quesnel Forks

Quesnel Forks, historically Quesnelle Forks, also simply known as "The Forks" or grandly known as "Quesnel City" is a ghost town in the Cariboo region of British Columbia, Canada. It is located the junction of the Quesnel and Cariboo Rivers and is 60 km southeast of Quesnel and only 11 km northwest of Likely.

Cottonwood River Provincial Park

Cottonwood River Provincial Park is a provincial park in British Columbia, Canada, located northeast of the confluence of the Quesnel and Cottonwood Rivers in that provinces North Cariboo region.

Itcha Ilgachuz Provincial Park

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.

Moose Valley Provincial Park

Moose Valley Provincial Park is a provincial park in British Columbia, Canada, located in the South Cariboo region 31 km west of 100 Mile House. Comprising approximately 2,322 ha, it is located to the north of Gustafsen Lake.

Nuntsi Provincial Park

Nuntsi Provincial Park, also known as Taseko Provincial Park, is a provincial park in British Columbia, Canada, located on the west side of the Taseko River in that provinces Chilcotin District, flanking both sides of Nuntsi Creek.

Mount Timothy Ski Area

Mount Timothy Ski Area is a small ski area located in the South Cariboo region of British Columbia, Canada, 30 km north of 100 Mile House and 18 km northeast of Lac La Hache The area has a triple chairlift, t-bar, platte lift and 2 Magic Carpet beginner lifts and has a vertical drop of 284m from a summit elevation of 1654m to a base elevation of 1370m. 35 runs range from Double black diamond to beginner terrain. This year Mt.Timothy will be opening with a brand new freestyle area geared towards the young and fearless. Mt.Timothy is visited by patrons from all across the world, as far away as Eastern Europe and Japan.

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Top Attractions in Cariboo

Canim Falls

Canim Beach Provincial Park

Rainbow Range

Quesnel Lake

Mahood Lake

Chilko Lake

Barkerville

Alexandria

Wells

Williams Lake Indian Reserve No. 1

Cariboo River Provincial Park

Horsefly Lake

Far Mountain

Mahood Falls

Chilcotin River

Lava Canyon

Anahim Peak

Ilgachuz Range

Itcha Range

Canim Lake

Taseko Lakes

Tatlayoko Lake

Cottonwood House Historic Site

Fort Chilcotin

Quesnel Forks

Cottonwood River Provincial Park

Itcha Ilgachuz Provincial Park

Moose Valley Provincial Park

Nuntsi Provincial Park

Mount Timothy Ski Area

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