Vital Creek is a creek located in the Omineca Country region of British Columbia, flowing eastward from its source in the Vital Range to meet Silver Creek, joining that creek from the west about 5 miles from its mouth into the Omineca River, about 41 km northeast of Takla Landing. [1] [2]
The Omineca Country, also called the Omineca District or the Omineca, is a historical geographic region of the Northern Interior of British Columbia, roughly defined by the basin of the Omineca River but including areas to the south which allowed access to the region during the Omineca Gold Rush of the 1860s. The term Omineca District also refers to the Omineca Mining District which referred to the same area but was a government administrative division. Today the name loosely refers to the region northwest of Prince George and north of Hwy 16 and occurs in the names of such entities as electoral districts, e.g. Prince George-Omineca.
British Columbia is the westernmost province of Canada, located between the Pacific Ocean and the Rocky Mountains. With an estimated population of 5.016 million as of 2018, it is Canada's third-most populous province.
The Vital Range is a subrange of the Hogem Ranges of the Omineca Mountains, bounded by Fall Creek, Silver Creek and Kenny Creek in northern British Columbia, Canada.
The gold deposits of Vital Creek were discovered in 1869 by Vital Laforce, who had also been among the four discoverers of gold along Williams Creek, which was the foundation of Barkerville. [3] This was the first creek mined in the Omineca. Late in the mining season of 1870, $7,000 was taken out by a party of 15 Chinese miners, giving some hope that significant gold might yet be found in the region. [4]
Williams Creek is an important historical gold mining creek in the Cariboo goldfields of the Central Interior of British Columbia, entering the Willow River between Barkerville and the town of Wells, which is at the headwaters of the Willow River.
The Omineca Gold Rush was a gold rush in British Columbia, Canada in the Omineca region of the Northern Interior of the province. Gold was first discovered there in 1861, but the rush didn't begin until late in 1869 with the discovery at Vital Creek. There were several routes to the goldfields: two were from Fort St. James, one of which was a water route through the Stuart and Tachie Rivers to Trembleur Lake to Takla Lake and the other was overland, called the Baldy Mountain route. A third route came in overland from Hazelton on the Skeena River and a fourth route used the Fraser River and crossed over the Giscome Portage to Summit Lake, through McLeod Lake, and up the Finlay River to the Omineca River.
The creek has been mined for gold and silver, which occurred simultaneously and were unusual to find in that way. [5] It has been hydraulicked and mined by Chinese syndicates like Gow Sing and Co. The bulk of the gold was obtained on bedrock and in crevices and cracks. [6]
Initial exploration and mining work was carried out by means of drift diggings, followed by ground sluicing and hydraulicking later. Drift mining and hydraulicking were both abandoned in the 1930s as there were no dumping facilities for mining waste. Later exploration to bedrock in pursuit of hard-rock ores met with little success. [7]
Total gold production from Vital Creek between 1876 and 1900 was 117,091 grams, and between 1926 and 1940 another 143,122 grams of gold were taken from the creek. Early takings were from the creek's present channel downstream from a waterfall 3 km upstream from the mouth of the creek. Gold was later found upstream from the waterfall in a pre-glacial channel, in the form of coarse well-worn flakes on the bedrock. [8]
Three jade boulders weighing 2267, 907 and 363 kilograms were reported as having been taken from the creek in 1963. [9]
Nephrite is a variety of the calcium, magnesium, and iron-rich amphibole minerals tremolite or actinolite (aggregates of which also make up one form of asbestos). The chemical formula for nephrite is Ca2(Mg, Fe)5Si8O22(OH)2. It is one of two different mineral species called jade. The other mineral species known as jade is jadeite, which is a variety of pyroxene. While nephrite jade possesses mainly grays and greens (and occasionally yellows, browns or whites), jadeite jade, which is rarer, can also contain blacks, reds, pinks and violets. Nephrite jade is an ornamental stone used in carvings, beads, or cabochon cut gemstones.
The area drained by the creek is underlain by a north-northwest striking, east-dipping metasedimentary/volcanic formation of the Carboniferous to Jurassic Cache Creek Complex. Phyllite, limestone and tuff are common. White quartz veins up to a metre in width were found within these rocks. [10]
Arquerite, a native amalgam of silver and mercury, is relatively abundant in the gold-bearing gravels of the creek. [11]
Thutade Lake is located in the Omineca Mountains of the Northern Interior of British Columbia, Canada. About 40 km in length, and no more than about 2 km wide, the lake is primarily significant as the ultimate source of the Mackenzie River. The lake is at the head of the Finlay River, which joins the Peace River via Williston Lake. The area is very remote, being located about 260 km north of Smithers, although several mining operations for ores containing copper, lead, zinc and silver have occurred around the lake. The largest of these is the Kemess Mine, an iron and copper property originally owned by Royal Oak Mines and now by Northgate Minerals, located in the valley of Kemess Creek, which is off the northeast end of Thutade Lake. The mine is accessed by the Omineca Resource Road and other resource routes, and is 400 km by road from Prince George. Just downstream from the outlet of Thutade Lake, the Finlay plunges over 180-foot (55 m) Cascadero Falls, and then through a series of cataracts in a twisting course until it begins its main northeastward trend. Cascadero Falls is slated for hydroelectric development in connection with the power needs of the area's mines.
Zeballos is a village located on the northwest coast of Vancouver Island in British Columbia, Canada. While legend suggests Spanish gold seekers may have explored the area in the late 16th century, Zeballos is now known for its ecotourism and sport fishing.
Minto City, often called just Minto, sometimes Minto Mines or Minto Mine, was a gold mining town in the Bridge River Valley of British Columbia from 1930 to 1936, located at the confluence of that river with Gun Creek, one of its larger tributaries. It was first called the Alpha group of claims in the 1920s, when underground miners were exploring the seams of Cadwallader Creek and the origins of the placer deposits downstream in the Bridge River. The mine prospect was never much successful although a model townsite was built by promoter "Big Bill" Davidson, who imported soil to build a specially-built rodeo ground and baseball diamond on the rocky site. The larger mine of Bralorne was nearby. The mine shut down in 1936 due to productivity issues, but restarted in 1940. The valley has since been significantly altered when most of the vestiges of the town were inundated by the waters of the Carpenter Lake reservoir following completion of the Bridge River Power Project. The town sat on the western end of the lake near the present Carpenter Lake Road, part of the road drove through a wooden Tudor arch built into the rock mill.
The Kemess Mine was an open-pit copper and gold mine, located just northeast of the foot of Thutade Lake, at the head of the Finlay River, in the Omineca Mountains of the Northern Interior of British Columbia, Canada. It was operated by Royal Oak Mines from 1998 to 1999, when it was bought by Northgate Minerals. Northgate operated the mine until its closure in 2011; that year Northgate was taken over by AuRico Gold. In 2014 AuRico Gold partitioned off its portion of Kemess Mine ownership creating a new company called AuRico Metals.
Tasu or Tassoo, also Old Tasu or Old Tasu Townsite, was an iron and copper open pit and underground mining operation and townsite located on the south shore of Tasu Sound in west-central Moresby Island in the Queen Charlotte Islands of the North Coast of British Columbia, Canada.
Gold Harbour, was a gold and silver mine and camp on Mitchell Inlet, part of Tasu Sound on Moresby Island in the Queen Charlotte Islands of the North Coast of British Columbia, Canada. It is notable as the location of the first lode mine worked in what is now British Columbia.
Copper Mountain was an important copper-mining company town in the Similkameen Country of the Southern Interior of British Columbia, Canada, just south of the town of Princeton.
McGillivray, formerly McGillivray Falls, is an unincorporated recreational community on the west shore of Anderson Lake, just east of midway between the towns of Pemberton and Lillooet, British Columbia, Canada, in that province's southwest Interior.
Cayoosh Creek is a northeast-flowing tributary of the Seton River in the Canadian province of British Columbia. The name Cayoosh Creek remains on the bridge-sign crossing the stream on BC Highway 99 and continues in use locally to refer to the final reaches of the Seton River, formerly Seton Creek, which prior to the renaming ending at the confluence with Cayoosh Creek. The creek is the namesake of Cayoosh Creek Indian Reserve No. 1, one of the main Indian reserves of the Cayoose Creek Indian Band, which lies adjacent to what was renamed the Seton River without local consultation.
Premier was a large gold mining camp in British Columbia, Canada some 18 miles from Stewart. It ran from the years 1918 to 1953 and was a large employer in the area. Huge bunkhouses, generators, concentrators, machine and cook houses sat on the hillside. A road provided access to the area, snowfall pending. Horses and cat tractors were used.
Henry "Harry" McDame was a Bahamas-born prospector in the California and British Columbia gold rushes.
The Germansen River, formerly Germansen Creek, is a major south tributary of the Omenica River in the Northern Interior of British Columbia, Canada. The settlement and former gold-rush centre of Germansens Landing is located at its confluence with the Omineca. Along its course is Germansen Lake at 55°41′45″N124°51′10″W, south of which is the Germansen Range and Mount Germansen.
Defot is a locality and former mining boomtown in the Cassiar Country of the Northern Interior of British Columbia, Canada, located west of Mount Defot.
Manson River is a river located in the Omineca Country region of British Columbia. It flows north into Manson Arm, Williston Lake. The river is located south of Germansen Landing. It was first known as Manson Creek and was discovered in 1871 by Robert Howell. The river has been mined using wing-damming, drifting and hydraulicking. Manson River has been mined by Europeans and Chinese.
Brexton, formerly known as Fish Lake, is a ghost town located in the Bridge River Country region of British Columbia. Although the provincial Gazetteer still lists the "settlement" of Brexton, which was situated between the southeast end of Gun Lake and Gold Bridge, and three and a half miles north of Bralorne, this once busy town has mostly vanished though a few buildings remain. The old town site now sits mainly on private property.
Jedway is a landing and erstwhile settlement and mining camp on Harriet Harbour, part of Skincuttle Inlet, on the east coast of Moresby Island in Haida Gwaii, British Columbia, Canada. Jedway was once a hub for mines in the area during a mining boom on South Moresby, including mines at Ikeda and Lockeport, though a mine at the Jedway iron-magnetite deposit, known as the Jessie showings, did not open until 1961. In the earlier period, Jedway had been the "capital" of the Queen Charlotte Islands until that (the headquarters of the provincial Gold Commissioner, E.M. Sandilands, whose position carried with it all the functions of and powers of government, to Queen Charlotte City in 1910. A 1908 in The Ledge, a mining newspaper based in Greenwood, said "there is room for another hotel in Jedway". Jedway remained a local service centre after that, however, with two Chinese sentenced to months-long imprisonment being relocated there from Queen Charlotte City in 1912 indicating the presence of jail facilities there.
Haylmore is a location in the Bridge River Country of the southwestern Interior of British Columbia, Canada, located near the town of Gold Bridge just below the confluence of the Bridge River and its south fork, the Hurley River.
Coordinates: 55°42′47″N125°28′04″W / 55.71306°N 125.46778°W