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Beaver Pass (Cariboo)
Beaver Pass, elev. 1070 m (3510 ft), is a pass in the hillcountry of the northern Cariboo Plateau forming a divide between Lightning Creek (S) and Tregillus Creek, part of the Willow River drainage (N), located just northwest of Beaver Pass House, a locality along the route of BC Highway 26, which leads to Barkerville and Wells from its start at its junction with the Cariboo Highway Highway 97 is a major highway in the Canadian province of British Columbia. It is the longest continuously numbered route in the province, running and is the only route that runs the entire north–south length of the British Columbia, connec ... (97) at the city of Quesnel. References Mountain passes of British Columbia Landforms of the Cariboo {{cariboo-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cariboo Plateau
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. As a region and historical identity, the Cariboo is sometimes considered to extend to the Thompson River to the south of that, and to border on the city of Kamloops at its southeastern corner and even as far as Lytton, at the confluence of the Fraser and Thompson Rivers. The town of Lillooet is generally considered to be in the Cariboo, while the Bridge River Country to its west was sometimes ref ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lightning Creek (British Columbia)
Lightning Creek is a creek located in the Cariboo region of British Columbia British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, .... This creek flows into the Swift River and was discovered in 1861 by Cunningham, Bell and Hume. Lightning Creek was mined for gold. A problem mining this creek is the depth of the bedrock and the flooding of the deep diggings. In 1876 half a dozen companies were operating pumps twenty four hours a day and raising almost 20 million gallons per day in an effort to keep the ground drained. The total value of the gold yielded from the creek is about $15,000,000. The tributaries on the south side of this creek yielded gold, but those on the north side yielded little gold. References Rivers of British Columbia {{BritishColumbia-river-s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Willow River (British Columbia)
The Willow River is a tributary of the Fraser River in the north-central Interior of British Columbia, Canada. It enters the Fraser near the community of Willow River, just upstream from the city of Prince George, near the confluence of the Salmon River. Its source is in the Cariboo goldfields at Jack of Clubs Lake in the mining and arts community of Wells, British Columbia, near Barkerville. In 1974, the canyon of the Willow River, east of Prince George, was the scene of a tragic accident involving eight teenagers who died when their three canoes and kayak were broken in the raging waters and boulders of a narrow gorge. See also *List of British Columbia rivers The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes th ... References Tributaries of the Fraser River Rivers of the Caribo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beaver Pass House
Beaver Pass House is an unincorporated locality and former roadhouse on the Cariboo Wagon Road (now the Barkerville Highway) in the Cariboo Country of the Central Interior of British Columbia, Canada. Located on the north bank of Lightning Creek northwest of Coldspring House, another roadhouse, it still had a population of 17 in the 1961 Canadian census, in which it had been listed as Beaver Pass (the pass proper is just to its north). By that time, the original roadhouse had been destroyed by a fire, but a gas station and coffeehouse had been built near the original location. Between Beaver Pass House and Coldspring House are the localities of Wingdam and Pinegrove. Pinegrove is the location of the Troll Ski Resort, a small operation popular with skiers from Quesnel. See also *Cottonwood, British Columbia Cottonwood, including the Cottonwood Ranch and Cottonwood House, is an unincorporated settlement in the North Cariboo region of the Central Interior of British Colum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Provincial Highway 26
Highway 26, also known as the Barkerville Highway, is a minor east-west highway in the North Cariboo region of the Central Interior of British Columbia, Canada. First opened in 1967, it provides access to the community of Wells and the famous gold rush town of Barkerville at the foot of the Cariboo Mountains, respectively 75 and 81 km (47 and 51 mi) east of the highway's junction with Highway 97 at Quesnel. Also accessed by the route is Bowron Lakes Provincial Park, a popular canoeing expedition circuit, the cutoff for which is between Barkerville and Wells. Since Highway 26 is very lightly travelled, it has not needed any major improvements since its opening. Its route is approximately the same as that of the Cariboo Wagon Road. See also * Cottonwood House *Coldspring House *Beaver Pass House *Stanley, British Columbia Stanley was a gold rush town in the Cariboo region of British Columbia that began during the Cariboo Gold Rush. History Gold was found in near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barkerville, British Columbia
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 east of Quesnel. BC Highway 26, which follows the route of the Cariboo Wagon Road, the original access to Barkerville, goes through it. History Founding Barkerville is located on the western edge of the Cariboo Mountains in British Columbia. It was named after Billy Barker from Cambridgeshire, England, who was among those who first struck gold at the location in 1861. His claim was the richest and the most famous. Barkerville was built up almost overnight, and was a case of "growth via word of mouth". It grew as fast as the word of Barker's strike spread. His claim would eventually yield 37,500 ounces (1,065 kg/2,350 lb) of gold. Before the construction of the Cariboo Wagon Road, people hauled their own supplies to Barkerville, either on their backs or in a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wells, British Columbia
Wells is a small mining and tourist town in the Cariboo District of central British Columbia, located on BC Highway 26, from Quesnel and 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. History Originally a company town, it was managed by ''Cariboo Gold Quartz Mine''. Fred M. Wells, for whom the town was named, prospected in the area for 10 years before finding the minerals that built the company. At its heyday of the 1930s, Wells sported 4500 people. In 1942 it had a greater population than Quesnel or Prince George. The closure of the gold and other mineral mines in 1967 took its toll on the town and most of the population moved away. Today it has a listed population of just 250 which doubles during the summer months. Between May and September, Wells sees over 100,000 tourists pass through on their way to Bark ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cariboo Highway
Highway 97 is a major highway in the Canadian province of British Columbia. It is the longest continuously numbered route in the province, running and is the only route that runs the entire north–south length of the British Columbia, connecting the Canada–United States border near Osoyoos in the south to the British Columbia–Yukon boundary in the north at Watson Lake, Yukon. The highway connects several major cities in BC Interior, including Kelowna, Kamloops, Prince George, and Dawson Creek. Within and near these cities, Highway 97 varies from a two-lane highway to a freeway with as many as six lanes. Some remote sections also remain unpaved and gravelled. The route takes its number from U.S. Route 97, with which it connects at the international border. The highway was initially designated '97' in 1953. Route description The busiest section of Highway 97 is in West Kelowna, carrying almost 70,000 vehicles per day. Some sections in the northern regions of the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quesnel, British Columbia
Quesnel (Kee-nel in French) is a city located in the Cariboo Regional District of British Columbia, Canada. Located nearly evenly between the cities of Prince George and Williams Lake, it is on the main route to northern British Columbia and the Yukon. Quesnel is located at the confluence of the Fraser River and Quesnel River. Quesnel's metropolitan area has a population of 23,146 making it the largest urban center between Prince George and Kamloops. Quesnel is a sister city to Shiraoi, Japan. Quesnel hosted the 2000 British Columbia Winter Games, a biennial provincial amateur sports competition. To the east of Quesnel is Wells, Barkerville, and Bowron Lake Provincial Park, a popular canoeing destination in the Cariboo Mountains. History Long before the arrival of prospectors during the Cariboo Gold Rush of 1862, the Southern Carrier (Dakelh) people lived off the land around Quesnel, occupying the area from the Bowron Lakes in the east to the upper Blackwater River and Dean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of British Columbia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
