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Zagime Anishinabek

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The Zagime Anishinabek (formerly known as the Sakimay First Nation ) are a Saulteaux band government in southern Saskatchewan , Canada.

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57-492: Their reserves include: Chief: Chief Lynn Acoose Councillors: This Saskatchewan -related article is a stub . You can help Misplaced Pages by expanding it . This First Nations in Canada –related article is a stub . You can help Misplaced Pages by expanding it . Indian reserve In Canada, an Indian reserve ( French : réserve indienne ) or First Nations reserve ( French : réserve des premières nations )

114-584: A colony in 1858, also worked to establish many reserves on the mainland during his tenure, though most of these were overturned by successor colonial governments and later royal commissions once the province joined Confederation in 1871. In 1867, legislative jurisdiction over "Indians and Lands reserved for the Indians" was assigned to the Parliament of Canada through the Constitution Act, 1867 ,

171-420: A fact which has led many to be abandoned, or used only seasonally (as a trapping territory , for example). Statistics Canada counts only those reserves which are populated (or potentially populated) as "subdivisions" for the purpose of the national census . For the 2011 census, of the more than 3,100 Indian reserves across Canada, there were only 961 Indian reserves classified as census subdivisions (including

228-659: A major part of Canada's Constitution (originally known as the British North America Act ), which acknowledged that First Nations had special status. Separate powers covered "status and civil rights on the one hand and Indian lands on the other." In 1870, the newly formed Dominion government acquired Rupert's Land , a vast territory in British North America consisting mostly of the Hudson Bay drainage basin that had been controlled by

285-691: A navigable stream". His trip down the river convinced him that Fort Langley could not replace Fort Vancouver as the company's main depot on the Pacific coast. Much of British Columbia's history has been bound to the Fraser, partly because it was the essential route between the Interior and the Lower Coast after the loss of the lands south of the 49th Parallel with the Oregon Treaty of 1846. It

342-612: A regional position within the Canadian Heraldic Authority is named after the river. The Fraser River is known for the fishing of white sturgeon , all five species of Pacific salmon ( chinook , coho , chum , pink , sockeye ), as well as steelhead trout . The Fraser River is also the largest producer of salmon in Canada. A typical white sturgeon catch can average about 500 pounds (230 kg). A white sturgeon weighing an estimated 500 kilograms (1,100 lb) and measuring 3.76 metres (12 ft 4 in)

399-715: A short dam lifespan, but mostly because of strong opposition from fisheries and other environmental concerns. In 1858, the Fraser River and surrounding areas were occupied when the gold rush came to the Fraser Canyon and the Fraser River. It is also a popular fishing location for residents of the Lower Mainland. The delta of the river, especially in the Boundary Bay area, is an important stopover location for migrating shorebirds . The Fraser Herald ,

456-442: A significant spring freshet , primarily impacting regions around Prince George , Kamloops , Hope and Surrey . Due to record snowpacks on the mountains in the Fraser River catch basin which began melting, combined with heavy rainfall, water levels on the Fraser River rose in 2007 to a level not reached since 1972. Low-lying land in areas upriver such as Prince George suffered minor flooding. Evacuation alerts were given for

513-405: A single government is responsible for more than one reserve. In 2003, 60 percent of status Indians lived on reserves. Of the 637,660 First Nations people who reported being Registered Indians, nearly one-half (49.3%) lived on an Indian reserve. This proportion varies across the country. Many reserves have no resident population; typically they are small, remote, non-contiguous pieces of land,

570-426: A trust agreement with CMHC, and lenders can receive loans to build or repair houses. In other programs, loans to residents of reserves are guaranteed by the federal government. Provinces and municipalities may expropriate reserve land if specifically authorized by a provincial or federal law. Few reserves have any economic advantages, such as resource revenues. The revenues of those reserves that do are held in trust by

627-845: A very important role in public policy stakeholder consultations, particularly when reserves are located in areas that have valuable natural resources with potential for economic development. Beginning in the 1970s, First Nations gained "recognition of their constitutionally protected rights." First Nations' rights are protected by section 35 of the Constitution Act, 1982 . By 2002, (Valiente) First Nations had already "finalised 14 comprehensive land claims and self-government agreements, with numerous others, primarily in northern Canada and British Columbia, at different stages of negotiations." Land claims and self-government agreements are "modern treaties" and therefore hold constitutional status. The Canadian Environmental Protection Act, 1999 (CEPA), "places aboriginal participation on par with federal ministers and

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684-521: A year. These are "public water systems managed by the federal government". There were also 18 communities that had "water issues for between two and 12 months." According to statistics gathered by Health Canada and the First Nations Health Authority , in 2015, there were "162 drinking water advisories in 118 First Nation communities". In October 2015, Neskantaga First Nation reported that its "20-year boil-water advisory"

741-939: Is an example of a reserve created in modern times. Another multi-band reserve of the Sto:lo peoples is Grass Indian Reserve No. 15 , which is located in the City of Chilliwack and is shared by nine bands. After the Royal Proclamation of 1763 but before Confederation in 1867, the Upper Canada Treaties (1764–1862 Ontario) and the Douglas Treaties (1850–1854 British Columbia) were signed. "Some of these pre-confederation and post-confederation treaties addressed reserve lands, hunting, fishing, trapping rights, annuities and other benefits." Governor James Douglas of British Columbia, which formally became

798-831: Is defined by the Indian Act as a "tract of land, the legal title to which is vested in Her Majesty , that has been set apart by Her Majesty for the use and benefit of a band ." Reserves are areas set aside for First Nations , one of the major groupings of Indigenous peoples in Canada , after a contract with the Canadian state (" the Crown "), and are not to be confused with Indigenous peoples' claims to ancestral lands under Aboriginal title . A single "band" (First Nations government) may control one reserve or several, while other reserves are shared between multiple bands. In 2003,

855-718: Is joined by the Bridge and Seton Rivers at the town of Lillooet , then by the Thompson River at Lytton , where it proceeds south until it is approximately 64 kilometres (40 mi) north of the 49th parallel , which is Canada's border with the United States . From Lytton southwards it runs through a progressively deeper canyon between the Lillooet Ranges of the Coast Mountains on its west and

912-412: Is named Queensborough and is part of the City of New Westminster. Also in the lowermost Fraser, among other smaller islands, is Annacis Island , an important industrial and port area, which lies to the southeast of the eastern end of Lulu Island. Other notable islands in the lower Fraser are Barnston Island , Matsqui Island , Nicomen Island and Sea Bird Island . Other islands lie on the outer side of

969-622: Is part of the Fraser Lowland and was formed also by sediment deposited from the Fraser, though most of the county is not in the Fraser drainage basin. Similar to the Columbia River Gorge east of Portland, Oregon , the Fraser exploits a topographic cleft between two mountain ranges separating a more continental climate (in this case, that of the British Columbia Interior ) from a milder climate near

1026-744: The Anishinaabe and the Swampy Cree tribes. Treaty 1 First Nations comprise the Brokenhead Ojibway Nation , Fort Alexander ( Sagkeeng First Nation ), Long Plain First Nation , Peguis First Nation , Roseau River Anishinabe First Nation , Sandy Bay First Nation and Swan Lake First Nation . The rights and freedoms of Canada's First Nations people have been governed by the Indian Act since its enactment in 1876 by

1083-471: The Cascade Range on its east. Hell's Gate , located immediately downstream of the town of Boston Bar , is a famous portion of the canyon where the walls narrow dramatically, forcing the entire volume of the river through a gap only 35 metres (115 feet) wide. An aerial tramway takes visitors out over the river. Hells Gate is visible from Trans-Canada Highway 1 about 2 km (1.2 mi) south of

1140-688: The Department of Indian and Northern Affairs stated there were 2,300 reserves in Canada, comprising 28,000 km (11,000 sq mi). According to Statistics Canada in 2011, there are more than 600 First Nations/Indian bands in Canada and 3,100 Indian reserves/First Nations reserves across Canada. Examples include the Driftpile First Nation , which like many bands, has only one reserve, Driftpile River 150 . The Bear River First Nation , who govern Bear River 6 , Bear River 6A and Bear River 6B , are one of many examples where

1197-555: The Hudson's Bay Company under its Charter with the British Crown from 1670 to 1870. Numerous aboriginal groups lived in the same territory and disputed the sovereignty of the area. The Dominion of Canada promised Britain to honour the provisions of the Royal Proclamation of 1763 to "negotiate with its Amerindians for the extinguishment of their title and the setting aside of reserves for their exclusive use." This promise led to

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1254-520: The Hudson's Bay Company 's main Pacific depot. Simpson had believed the Fraser River might be navigable throughout its length, even though Simon Fraser had described it as non-navigable. Simpson journeyed down the river and through the Fraser Canyon and afterwards wrote "I should consider the passage down, to be certain Death, in nine attempts out of Ten. I shall therefore no longer talk about it as

1311-586: The Kashechewan First Nation reserve's drinking water and chlorine levels had to be increased to 'shock' levels, causing skin problems and eventually resulting in an evacuation of hundreds of people from the reserve and costing approximately $ 16 million." Fraser River The Fraser River ( / ˈ f r eɪ z ər / ) is the longest river within British Columbia , Canada, rising at Fraser Pass near Blackrock Mountain in

1368-593: The Lower Mainland ( Fraser Valley and Metro Vancouver ) occurred in 1894. With no protection against the rising waters of the Fraser River, Fraser Valley and Metro Vancouver communities from Chilliwack downstream were inundated with water. In the 1894 floods, the water mark at Mission reached 7.85 metres (25.75 ft). After the 1894 flood, a dyking system was constructed throughout the Fraser Valley. The dyking and drainage projects greatly improved

1425-543: The Minister of Crown–Indigenous Relations the right to "determine whether any purpose for which lands in a reserve are used is for the use and benefit of the band." Title to land within the reserve may be transferred to only the band or to individual band members. Reserve lands may not be seized legally, nor is the personal property of a band or a band member living on a reserve subject to "charge, pledge, mortgage, attachment, levy, seizure distress or execution in favour or at

1482-543: The Mount Robson Provincial Park , to Steveston in Vancouver at the river mouth. With an average flow at the mouth of about 3,475 cubic metres per second (122,700 cu ft/s), the Fraser is the largest river by discharge flowing into the Pacific seaboard of Canada and the fifth largest in the country. The average flow is highly seasonal; summer discharge rates can be ten times larger than

1539-686: The North West Company from the site of present-day Prince George almost to the mouth of the river. The river's name in the Halqemeylem (Upriver Halkomelem) language is Sto:lo , often seen archaically as Staulo , and has been adopted by the Halkomelem-speaking peoples of the Lower Mainland as their collective name, Sto:lo . The river's name in the Dakelh language is Lhtakoh . The Tsilhqot'in name for

1596-721: The Numbered Treaties . Between 1871 and 1921, through Numbered Treaties with First Nations, the Canadian government gained large areas of land for settlers and for industry in Northwestern Ontario , Northern Canada and in the Prairies . The treaties were also called the Land Cession or Post-Confederation Treaties. Treaty 1 is an agreement established August 3, 1871, between the Crown and various First Nations in southeastern Manitoba , including

1653-757: The Rocky Mountain Trench and the Robson Valley near Valemount . After running northwest past 54° north, it makes a sharp turn to the south at Giscome Portage , meeting the Nechako River at the city of Prince George , then continues south, progressively cutting deeper into the Fraser Plateau to form the Fraser Canyon from roughly the confluence of the Chilcotin River , near the city of Williams Lake , southwards. It

1710-619: The Rocky Mountains and flowing for 1,375 kilometres (854 mi), into the Strait of Georgia just south of the City of Vancouver . The river's annual discharge at its mouth is 112 cubic kilometres (27 cu mi) or 3,550 cubic metres per second (125,000 cu ft/s), and each year it discharges about 20 million tons of sediment into the ocean. The river is named after Simon Fraser , who led an expedition in 1808 on behalf of

1767-589: The San Juan Islands , gaining strength over the open water of the Strait of Juan de Fuca . The estuary at the river's mouth is a site of hemispheric importance in the Western Hemisphere Shorebird Reserve Network . The Water Survey of Canada currently operates 17 gauge stations that measure discharge and water level along the majority of the mainstem from Red Pass just downstream of Moose Lake in

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1824-663: The Chippewas of the Thames First Nation 42 near Muncey, Ontario , which was formerly shared between them and the Chippewas of the Thames First Nation as a single parcel of land. Some reserves are shared by multiple bands, whether as fishing camps or educational facilities such as Pekw'Xe:yles , a reserve on the Fraser River used by 21 Indian bands that was formerly St. Mary's Indian Residential School and

1881-593: The North Arm, which is the southern boundary of the City of Vancouver , and the South Arm, which divides the City of Richmond from the City of Delta to the south. Richmond is on the largest island in the Fraser, Lulu Island and also on Sea Island , which is the location of Vancouver International Airport , where the Middle Arm branches off to the south from the North Arm. The far eastern end of Lulu Island

1938-482: The Parliament of Canada. The provisions of Section 91(24) of the Constitution Act, 1867 , provided Canada's federal government exclusive authority to legislate in relation to "Indians and Lands Reserved for Indians". Wikwemikong Unceded Reserve on Manitoulin Island is subject to the Indian Act provisions governing reserves even though its lands were never ceded to the Crown by treaty. The Indian Act gives

1995-540: The coast. When an Arctic high-pressure area moves into the British Columbia Interior and a relatively low-pressure area builds over the general Puget Sound and Strait of Georgia region, the cold Arctic air accelerates southwest through the Fraser Canyon . These outflow winds can gust up to 97 to 129 kilometres per hour (60 to 80 mph) and have at times exceeded 160 kilometres per hour (100 mph). Such winds frequently reach Bellingham and

2052-408: The estuary, most notably Westham Island , a wildfowl preserve, and Iona Island , the location of the main sewage plant for the City of Vancouver. After 100 kilometres (about 60 mi), the Fraser forms a delta where it empties into the Strait of Georgia between the mainland and Vancouver Island . The lands south of the City of Vancouver , including the cities of Richmond and Delta , sit on

2109-476: The first Europeans to find and enter it. The existence of the river, but not its location, had been deduced during the 1791 voyage of José María Narváez , under Francisco de Eliza . The upper reaches of the Fraser River were first explored by Sir Alexander Mackenzie in 1793, and fully traced by Simon Fraser in 1808, who confirmed that it was not connected with the Columbia River . The lower Fraser

2166-648: The flat flood plain . The islands of the delta include Iona Island, Sea Island, Lulu Island, Annacis Island, and a number of smaller islands. While the vast majority of the river's drainage basin lies within British Columbia, a small portion in the drainage basin lies across the international border in Washington in the United States, namely the upper reaches of the tributary Chilliwack and Sumas rivers. Most of lowland Whatcom County, Washington

2223-523: The flood problems, but over time, the dykes were allowed to fall into disrepair and became overgrown with brush and trees. With some dykes constructed of a wooden frame, they gave way in 1948 in several locations, marking the second disastrous flood. Flooding since 1948 has been minor in comparison. 1948 saw massive flooding in Chilliwack and other areas along the Fraser River. The high-water mark at Mission rose to 7.5 metres (24.7 ft). The peak flow

2280-563: The flow during the winter. The Fraser's highest recorded flow, in June 1894, is estimated to have been 17,000 cubic metres per second (600,000 cu ft/s) at Hope . It was calculated using high-water marks near the hydrometric station at Hope and various statistical methods. In 1948 the Fraser River Board adopted the estimate for the 1894 flood. It remains the value specified by regulatory agencies for all flood control work on

2337-464: The instance of any person other than an Indian or a band". While the act was intended to protect the Indian holdings, the limitations make it difficult for the reserves and their residents to obtain financing for development and construction, or renovation. To answer this need, Canada Mortgage and Housing Corporation (CMHC) has created an on-reserve housing loan program. Members of bands may enter into

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2394-489: The minister of Crown–Indigenous Relations and Northern Affairs Canada . Reserve lands and the personal property of bands and resident band members are exempt from all forms of taxation except local taxation. Corporations owned by members of First Nations are not exempt, however. This exemption has allowed band members operating in proprietorships or partnerships to sell heavily taxed goods, such as cigarettes, on their reserves at prices considerably lower than those at stores off

2451-437: The poorly maintained dyke systems failed to contain the water. At the height of the 1948 flood, 200 square kilometres (50,000 acres) stood under water. Dykes broke at Agassiz, Chiliwack, Nicomen Island, Glen Valley and Matsqui. When the flood waters receded a month later, 16,000 people had been evacuated, with damages totaling $ 20 million, about $ 225 million in 2020 dollars. Major flooding occurred once again in 1972 due to

2508-605: The provinces in the National Advisory Committee." Among other things, CEPA clarified the term "aboriginal land" in 3 (1): "The definitions in this subsection apply in this Act. "aboriginal land" means (a) reserves, surrendered lands and any other lands that are set apart for the use and benefit of a band and that are subject to the Indian Act ." Under sections 46–50 of the CEPA, Environment and Climate Change Canada 's National Pollutant Release Inventory (NPRI)

2565-591: The reserves. Most reserves are self-governed, within the limits already described, under guidelines established by the Indian Act . Due to treaty settlements, some Indian reserves are now incorporated as villages, such as Gitlaxt'aamiks , British Columbia, which like other Nisga'a reserves was relieved of that status by the Nisga'a Treaty . Similarly, the Indian reserves of the Sechelt Indian Band are now Indian government districts. Indian reserves play

2622-476: The river was designated as a Canadian Heritage River for its natural and human heritage. It remains the longest river with that designation. The Fraser is heavily exploited by human activities, especially in its lower reaches. Its banks are rich farmland, its water is used by pulp mills , and a few dams on some tributaries provide hydroelectric power . The main flow of the Fraser has never been dammed partly because its high level of sediment flows would result in

2679-555: The river, not dissimilar to the Dakelh name, is ʔElhdaqox , meaning Sturgeon ( ʔElhda-chugh ) River ( Yeqox ) . The Fraser drains a 220,000-square-kilometre (85,000 sq mi) area. Its source is a dripping spring at Fraser Pass in the Canadian Rocky Mountains near the border with Alberta . The river then flows north to the Yellowhead Highway and west past Mount Robson to

2736-459: The river. Further studies and hydraulic models have estimated the maximum discharge of the Fraser River, at Hope during the 1894 flood, as within a range of about 16,000 to 18,000 cubic metres per second (570,000 to 640,000 cu ft/s). On June 14, 1792, the Spanish explorers Dionisio Alcalá Galiano and Cayetano Valdés entered and anchored in the North Arm of the Fraser River, becoming

2793-775: The six reserves added for 2011). Some reserves that were originally rural were gradually surrounded by urban development. Montreal, Vancouver and Calgary are examples of cities with urban Indian reserves . One band Chief and Council commonly administer more than one reserve, such as the Beaver Lake Cree Nation with two reserves or the Lenape people (in Canada incorporated as the Munsee-Delaware Nation ), who occupy Munsee-Delaware Nation Indian Reserve No. 1. This consists of three non-contiguous parcels of land totalling 1,054 ha (2,600 acres) within

2850-772: The tramway. Simon Fraser was forced to portage the gorge on his trip through the canyon in June 1808. At Yale , at the head of navigation on the river, the canyon opens up and the river widens, though without much adjoining lowland until Hope , where the river then turns west and southwest into the Fraser Valley , a lush lowland valley, and runs past Chilliwack and the confluence of the Harrison and Sumas Rivers , bending northwest at Abbotsford and Mission . The Fraser then flows past Maple Ridge , Pitt Meadows , Port Coquitlam , and north Surrey . It turns southwest again just east of New Westminster , where it splits into

2907-407: Was "the longest running drinking water advisory in Canada." Shoal Lake 40 First Nation was under an 18-year boil water advisory. By 2006, nearly 100 Indian reserves had boil-water advisories and many others had substandard water. Ḵwiḵwa̱sut'inux̱w Ha̱xwa'mis First Nation , on Vancouver Island , had a boil-water advisory beginning in 1997. In October 2005, "high E. coli levels were found in

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2964-406: Was about 15,600 cubic meters per second. Cool temperatures in March, April, and early May had delayed the melting of the heavy snowpack that had accumulated over the winter season. Several days of hot weather and warm rains over the holiday weekend in late May hastened the thawing of the snowpack. Rivers and streams quickly swelled with spring runoff, reaching heights surpassed only in 1894. Finally,

3021-421: Was caught and released on the Fraser River in July 2012. In 2021, a white sturgeon was caught on the river weighing 890 pounds (400 kg), with a length of 352 cm (11.55 ft). It was estimated to be over 100 years old. The fish was tagged and released. The most significant Fraser river floods in recorded history occurred in 1894 and 1948. After European settlement, the first disastrous flood in

3078-507: Was initiated. NPRI is the inventory of "pollutants released, disposed of and sent for recycling by facilities across the country". The NPRI is used by First Nation administrations on reserves, along with other research tools, to monitor pollution. For example, NPRI data showed the Aamjiwnaang First Nation in Sarnia, Ontario, was "ground zero for Ontario's heaviest load of air pollution." By December 21, 2017, there were 67 long-term boil-water advisories that had been in effect for longer than

3135-411: Was revisited in 1824 when the Hudson's Bay Company sent a crew across Puget Sound from its Fort George southern post on the Columbia River . The expedition was led by James McMillan . The Fraser was reached via the Nicomekl River and the Salmon River reachable after a portage. Friendly tribes met earlier on by the Simon Fraser crew were reacquainted with. A trading post with agricultural potential

3192-421: Was the site of its first recorded settlements of Aboriginal people ( see Musqueam , Sto:lo , St'at'imc , Secwepemc and Nlaka'pamŭ ), the site of the first European-Indigenous mixed ancestry settlement in southern British-Columbia ( see Fort Langley ), the route of multitudes of prospectors during the Fraser Canyon Gold Rush and the main vehicle of the province's early commerce and industry. In 1998,

3249-462: Was to be located. By 1827, a crew was sent back via the mouth of the Fraser to build and operate the original Fort Langley . McMillan also led the undertaking. The trading post original location would soon become the first ever mixed ancestry and agricultural settlement in southern British Columbia on the Fraser (Sto:lo) river. In 1828 George Simpson visited the river, mainly to examine Fort Langley and determine whether it would be suitable as

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