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Cayoosh Pass
Cayoosh Pass (1,275 m / 4,183 ft) is a mountain pass in the Lillooet Ranges of the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada. It lies just west of Duffey Lake on BC Highway 99 between the towns of Lillooet and Pemberton, formed by the headwaters of Cayoosh Creek to the east, flowing to the Fraser River at Lillooet, and Joffre Creek to the west, flowing steeply downhill to Lillooet Lake just southeast of the Mount Currie Indian Reserve. Cayoosh Pass and the valleys of Cayoosh and Joffre Creeks form the southern boundary of the Cayoosh Range, a subrange of the Lillooet Ranges. Long known to the St'at'imc and Lil'wat peoples whose territories include it, the pass was first traversed by a non-indigenous person when James Duffey, a.k.a. "Sapper Duffy" of the Royal Engineers, investigated the route in 1859–1860 during a resurvey and reconstruction of the Douglas Road, the route of which passed the Joffre Creek foot of the pass and followed th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Provincial Highway 99
Highway 99 is a provincial highway in British Columbia that serves Greater Vancouver and the Squamish–Lillooet corridor over a length of . It is a major north–south artery within Vancouver and connects the city to several suburbs as well as the U.S. border, where it continues south as Interstate 5. The central section of the route, also known as the Sea to Sky Highway, serves the communities of Squamish, Whistler, and Pemberton. Highway 99 continues through Lillooet and ends at a junction with Highway 97 near Cache Creek. The highway's number, assigned in 1940, was derived from former U.S. Route 99, the predecessor to Interstate 5 and a major route for the U.S. West Coast. Highway 99 originally comprised the King George Highway in Surrey, portions of Kingsway from New Westminster to Vancouver, and local streets. It was extended across the Lions Gate Bridge and to Horseshoe Bay in the 1950s along a new highway that would later be incorporated into Highway 1 (the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lil'wat
The Lil'wat First Nation ( lil, líl̓watǝmx), a.k.a. the Lil'wat Nation or the Mount Currie Indian Band, is a First Nations in Canada, First Nation band government located in the southern Coast Mountains region of the British Columbia Interior, Interior of the Canadian province of British Columbia. It is a member of the Lillooet Tribal Council, which is the largest grouping of band governments of the St'at'imc or Stl'atl'imx people (a.k.a. the Lillooet people). Other St'at'imc governments include the smaller In-SHUCK-ch Nation on the lower Lillooet River to the southwest, and the independent N'quatqua First Nation at the near end of Anderson Lake (British Columbia), Anderson Lake from Mount Currie, which is the main reserve of the Lil'wat First Nation, and also one of the largest Indian reserves by population in Canada. The Lil'wat First Nation's offices are located at Mount Currie, British Columbia, about 5 miles east of Pemberton, British Columbia, which is also located in t ... [...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] |
Joffre Lakes Provincial Park
Joffre Lakes Provincial Park is a class A provincial park located east of Pemberton in British Columbia, Canada. It was established in 1996, when Joffre Lakes Recreation Area (created 1988) was upgraded to park status. Three glacier-fed lakes are located in the park: Lower, Middle, and Upper Joffre Lakes. The rock flour in the water reflects blue and green waves, and gives the lakes a turquoise colour. Joffre Lakes is a popular destination for hikers in the summer and mountain climbers in the winter due to its scenic lakes, glaciers and challenging peaks. In recent years the park's popularity has increased dramatically, creating controversy due to the volume of litter in the park and drivers parking dangerously on the adjacent provincial highway. Recreation The recreation area is accessed from the parking lot along a trail. Upgrades have been made by the Parks Service in 2017 on this trail, and they hope to continue to upgrade the trail as far as the Middle Joffre Lake. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duffey Lake Provincial Park
Duffey Lake Provincial Park is a provincial park in British Columbia, Canada, located at the lake of the same name, which lies along BC Highway 99 just east of the summit of Cayoosh Pass. The lake's inflow and outflow are Cayoosh Creek. The park's highest point is Mount Rohr at the westernmost boundary. See also * Geography of British Columbia British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States ... References * External links * BC ParksDuffey Lake Provincial Park Provincial parks of British Columbia Lillooet Country Lillooet Ranges 1993 establishments in British Columbia Protected areas established in 1993 {{BritishColumbia-park-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian National Railway
The Canadian National Railway Company (french: Compagnie des chemins de fer nationaux du Canada) is a Canadian Class I freight railway headquartered in Montreal, Quebec, which serves Canada and the Midwestern and Southern United States. CN is Canada's largest railway, in terms of both revenue and the physical size of its rail network, spanning Canada from the Atlantic coast in Nova Scotia to the Pacific coast in British Columbia across approximately of track. In the late 20th century, CN gained extensive capacity in the United States by taking over such railroads as the Illinois Central. CN is a public company with 22,600 employees, and it has a market cap of approximately CA$90 billion. CN was government-owned, having been a Canadian Crown corporation from its founding in 1919 until being privatized in 1995. , Bill Gates is the largest single shareholder of CN stock, owning a 14.2% interest through Cascade Investment and his own Bill and Melinda Gates Foundation. Fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seton Lake
Seton Lake is a freshwater fjord draining east via the Seton River into the Fraser River at the town of Lillooet, about long, in area and lies at an elevation of . Its depth is . The lake is natural in origin but was raised slightly as part of the Bridge River Power Project, the two main powerhouses of which are on the north shore of the upper end of the lake near Shalalth. At the uppermost end of the lake is the community of Seton Portage and the mouth of the short Seton Portage River, which connects Anderson Lake on the farther side of the Portage to Seton Lake. The Seton Portage River is the main source of natural inflow to Seton Lake, and is primarily fed by Anderson Lake but also by Whitecap Creek, which has its origin on the east slopes of Whitecap Mountain, the highest in the Bendor Range, and by Spider Creek, which has its origin on the north slopes of an unnamed summit to the south of Seton Lake, which happens to be the highest of the Cayoosh Range which lines the sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anderson Lake (British Columbia)
Anderson Lake is located about 25 miles North of the town of Pemberton, British Columbia and is about 28.5 km2 (11 sq mi) in area and around 21 km (13 mi) in length. Its maximum depth is 215 meters (705 feet). It is drained by the Seton River, which feeds Seton Lake and so the Fraser River. It is fed by the Gates River, which drains from the Pemberton Pass divide with the Birkenhead River valley towards Pemberton- Mount Currie. It and Seton Lake were originally the same lake, which was cut in half between ten and twenty thousand years ago by a large landslide from the north face of the Cayoosh Range, which fronts Anderson Lake on the east. The slide created a locality known today as Seton Portage, which combined with the steamer ''Lady of The Lake'' played a key role on the route of the Douglas Road during the Fraser Canyon Gold Rush of 1858–59.http://www.library.ubc.ca/archives/pdfs/bchf/bchq_1946_1.pdf At its head, near the mouth of the Gates River, is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hurley River
The Hurley River is a major tributary of the Bridge River of west-central British Columbia that was earlier known as the South Fork of that larger river. It was for a while known as "Hamilton's River" after Danny Hamilton, an American who was among the first to settle in the goldfields region of the upper Bridge River. By the 1920s that name was changed to the Hurley River, commemorating one of the main pioneers of the Lillooet Country, Dan Hurley. The Hurley begins near Railroad Pass, a cleft in the mountains between the basins of the Bridge and upper Lillooet Rivers, and flows through a marshy upper valley eastwards before turning north just west of the famous gold-mining town of Bralorne. From that point the river goes over semi-hidden Hurley Falls into the Hurley Canyon, which makes up ten of the last twelve miles of the river before its confluence with the Bridge River near Gold Bridge, just below Lajoie Dam. An operating placer mine at the outlet of the canyon goes by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Railroad Pass (British Columbia)
Railroad Pass, 1385 m (4544 ft), usually known locally as Railway Pass, is a mountain pass in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Traversed by a seasonal dirt road known as the Hurley Main and sometimes also referred to therefore as Hurley Pass, the pass connects the Pemberton Meadows area of the upper valley of the Lillooet River, via Railroad Creek, to the uppermost reaches of the Hurley River, the main south fork of the Bridge River which the Hurley joins at the settlement of Gold Bridge. Railroad Pass gets its name from its potential as a possible route for a railway through the Coast Mountains although no formal record of such a survey exists. The Canadian Pacific Survey went through this area, but records only exist of survey parties attempting Ring Pass, at the head of the Lillooet River, and the divide between Meager Creek and Toba Inlet, as well as the southerly route since used by the Pacific Great Eastern, now a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Douglas Road
The Douglas Road, a.k.a. the Lillooet Trail, Harrison Trail or Lakes Route, was a goldrush-era transportation route from the British Columbia Coast to the Interior (NB another route known as the Lillooet Trail was the Lillooet Cattle Trail, which used some of the same route but was built 25 years later). Over 30,000 men are reckoned to have travelled the route in, although by the end of the 1860s it was virtually abandoned due to the construction of the Cariboo Wagon Road, which bypassed the region. History Originally traversed by Hudson's Bay Company employees in 1828 and charted by HBC explorer Alexander Caulfield Anderson in 1846, the route was heavily travelled by prospectors seeking to avoid the dangers of the Fraser Canyon to access the gold-bearing bars of the Fraser around today's Lillooet. Pressure for an alternative route to the Upper Fraser had mounted in the wake of the Fraser Canyon War of the winter of 1859, and miners were wary of travelling through the territory ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Royal Engineers
The Corps of Royal Engineers, usually called the Royal Engineers (RE), and commonly known as the ''Sappers'', is a corps of the British Army. It provides military engineering and other technical support to the British Armed Forces and is headed by the Chief Royal Engineer. The Regimental Headquarters and the Royal School of Military Engineering are in Chatham in Kent, England. The corps is divided into several regiments, barracked at various places in the United Kingdom and around the world. History The Royal Engineers trace their origins back to the military engineers brought to England by William the Conqueror, specifically Bishop Gundulf of Rochester Cathedral, and claim over 900 years of unbroken service to the crown. Engineers have always served in the armies of the Crown; however, the origins of the modern corps, along with those of the Royal Artillery, lie in the Board of Ordnance established in the 15th century. In Woolwich in 1716, the Board formed the Royal Regime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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