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120-581: Several sites on the Nelson River, with potential of millions of horsepower, had been identified as early as 1911, but transmission of power to population centres in the south was beyond the state of the art of electric power transmission at that time. Between 1955 and 1960, studies were carried out to determine what resources would be available for future hydraulic generation in Manitoba. The stations at Kelsey, Kettle, Long Spruce and Limestone were built on

240-461: A okimahkan . loosely translated as "war chief". This office was different from that of the "peace chief", a leader who had a role more like that of diplomat. In the run-up to the 1885 North-West Rebellion , Big Bear was the leader of his band, but once the fighting started Wandering Spirit became war leader. There have been several attempts to create a national political organization that would represent all Cree peoples, at least as far back as

360-549: A suture zone between these cratons and the Trans-Hudson Orogen . The Western Churchill and Superior cratons collided at about 1.9–1.8 Ga in the Trans-Hudson orogeny. Because of the irregular shapes of the colliding cratons, this collision trapped between them large fragments of juvenile crust, a sizable microcontinent , and island arc terranes , beneath what is now the centre of modern Hudson Bay as part of

480-898: A 1994 gathering at the Opaskwayak Cree First Nation reserve. The name "Cree" is derived from the Algonkian -language exonym Kirištino˙ , which the Ojibwa used for tribes around Hudson Bay . The French colonists and explorers, who spelled the term Kilistinon , Kiristinon , Knisteneaux , Cristenaux , and Cristinaux , used the term for numerous tribes which they encountered north of Lake Superior, in Manitoba, and west of there. The French used these terms to refer to various groups of peoples in Canada, some of which are now better distinguished as Severn Anishinaabe (Ojibwa), who speak dialects different from

600-593: A Métis as "a person who self-identifies as Métis, is distinct from other Aboriginal peoples, is of historic Métis Nation Ancestry and who is accepted by the Métis Nation". At one time the Cree lived in northern Minnesota, North Dakota and Montana. Today, American Cree are enrolled in the federally recognized Chippewa Cree tribe, located on the Rocky Boy's Indian Reservation , and in minority as "Landless Cree" on

720-525: A comparable position at 59°N on the Eurasian landmass in the Russian Far East and with a similar subarctic climate , has an annual average of −2.7 °C (27.1 °F). Vis-à-vis geographically closer Europe, contrasts stand much more extreme. Arkhangelsk at 64°N in northwestern Russia has an average of 2 °C (36 °F), while the mild continental coastline of Stockholm at 59°N on

840-753: A detailed history of the Hudson Bay basin has been reconstructed. During the majority of the Cambrian Period, this basin did not exist. Rather, this part of the Canadian Shield area was still topographically high and emergent. It was only during the later part of the Cambrian that the rising sea level of the Sauk marine transgression slowly submerged it. During the Ordovician, this part of

960-607: A dozen communities. Some of these were founded as trading posts in the 17th and 18th centuries by the Hudson's Bay Company, making them some of the oldest settlements in Western Canada . With the closure of the HBC posts and stores, although many are now run by The North West Company , in the second half of the 20th century, many coastal villages are now almost exclusively populated by Cree and Inuit . Two main historic sites along

1080-646: A few miles south of the Arctic Circle ) as being part of the Arctic Ocean, specifically "Arctic Ocean Subdivision 9.11". Other authorities include it in the Atlantic, in part because of its greater water budget connection with that ocean. The search for a western route to Cathay and the East Indies , which had been actively pursued since the days of Christopher Columbus and John Cabot , in

1200-618: A large increase in electric power exports, since Manitoba load growth will not require this capacity for a generation or more. All of these projects require additional HVDC transmission capacity from the North to the South. One such project, Bipole III, had been discussed with communities on the east side of Lake Winnipeg, but this area has been reserved by the provincial government, making transmission line construction infeasible. The government and Manitoba Hydro have currently rerouted Bipole III through

1320-601: A long time thereafter. In May 1612, Sir Thomas Button sailed from England with two ships to look for Henry Hudson, and to continue the search for the Northwest Passage to Asia. In 1668, Nonsuch reached the bay and traded for beaver pelts, leading to the creation of the Hudson's Bay Company (HBC), which still bears the historic name. The HBC negotiated a trading monopoly from the English Crown for

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1440-566: A minor amount of terrestrial fluvial sands and gravels of the Cretaceous period are preserved in the fill of a prominent ring-like depression about 325–650 km (202–404 mi) across created by the dissolution of Silurian evaporites during the Cretaceous period. From the large quantity of published geologic data that has been collected as the result of hydrocarbon exploration, academic research, and related geologic mapping ,

1560-483: A ring of subsided strata around the centre of this basin, strata representing this period of time are absent from the Hudson Bay basin and the surrounding Canadian Shield. The Precambrian Shield underlying Hudson Bay and in which Hudson Bay basin formed is composed of two Archean proto-continents, the Western Churchill and Superior cratons . These cratons are separated by a tectonic collage that forms

1680-622: A similar portion of the lowlands in Manitoba is contained in Wapusk National Park , the latter location being a significant maternity denning area for polar bears . In contrast, most of the eastern shores (the Quebec portion) form the western edge of the Canadian Shield in Quebec. The area is rocky and hilly. Its vegetation is typically boreal forest .The northern shores are tundra . Measured by shoreline, Hudson Bay

1800-412: A simplification of identity, and it has become "fashionable" for bands in many parts of Saskatchewan to identify as "Plains Cree" at the expense of a mixed Cree-Salteaux history. There is also a tendency for bands to recategorize themselves as "Plains Cree" instead of Woods Cree or Swampy Cree. Neal McLeod argues this is partly due to the dominant culture's fascination with Plains Indian culture as well as

1920-671: A surface area of 1,230,000 km (470,000 sq mi). It is located north of Ontario , west of Quebec , northeast of Manitoba , and southeast of Nunavut , but politically entirely part of Nunavut. It is an inland marginal sea of the Arctic Ocean . The Hudson Strait provides a connection between the Labrador Sea and the Atlantic Ocean in the northeast, while the Foxe Channel connects Hudson Bay with

2040-626: A tribal council of seven Swampy Cree First Nations across northern Manitoba and is based in The Pas . The Chemawawin Cree Nation (also Rocky Cree) are based on their reserve Chemawawin 2, adjacent to Easterville, Manitoba , 200 kilometres (120 mi) southeast of The Pas. Mathias Colomb First Nation (also Rocky Cree) is located in the community of Pukatawagan on the Pukatawagan 198 reserve. Misipawistik Cree Nation (also Rocky Cree)

2160-533: Is Wînipekw (southern dialect) or Wînipâkw (northern dialect), meaning muddy or brackish water. Lake Winnipeg is similarly named by the local Cree , as is the location for the city of Winnipeg . The bay is named after Henry Hudson , an Englishman sailing for the Dutch East India Company , and after whom the river that he explored in 1609 is also named . Hudson Bay encompasses 1,230,000 km (470,000 sq mi), making it

2280-745: Is 26 km northwest of Winnipeg , Manitoba. Download coordinates as: One of the key elements of the Nelson project was the diversion of much of the Churchill River into the Nelson watershed. The 1,600-kilometre-long (1,000 mi) Churchill River originates in northern Alberta and drains into Hudson Bay at Churchill, Manitoba . Currently the Missi Falls Control Structure ( 57°20′34″N 98°08′17″W  /  57.3427°N 98.1381°W  / 57.3427; -98.1381  ( Notigi Control Structure ) ) at

2400-1061: Is a combination of a Cree reserved land (TC) and a Cree village municipality (VC), both with the same name. Moose Cree ( Cree : Mōsonī or Ililiw ), also known as Moosonee are located in Northeastern Ontario . Constance Lake First Nation is the only Cree member of Matawa First Nations . They are located on their reserves, Constance Lake 92 and English River 66 , in the Cochrane District , Ontario. Mushkegowuk Council , based in Moose Factory, Ontario , represents chiefs from seven First Nations across Ontario. Moose Cree members are: Chapleau Cree First Nation , Kashechewan First Nation , Missanabie Cree First Nation , Moose Cree First Nation , and Taykwa Tagamou Nation . The Chapleau Cree First Nation and their two reserves, Chapleau Cree Fox Lake and Chapleau 75 , are located outside of Chapleau, Ontario in

2520-492: Is a group of people claiming descent from the same common ancestor; each clan would have a representative and a vote in all important councils held by the band (compare: Anishinaabe clan system ). Each band remained independent of each other. However, Cree-speaking bands tended to work together and with their neighbours against outside enemies. Those Cree who moved onto the Great Plains and adopted bison hunting , called

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2640-652: Is a privately owned port on Hudson Bay in Churchill, Manitoba , Canada. Routes from the port connect to the North Atlantic through the Hudson Strait . As of 2008, the port had four deep-sea berths capable of handling Panamax -size vessels for the loading and unloading of grain, bulk commodities, general cargo, and tanker vessels. The port is connected to the Hudson Bay Railway , which shares

2760-565: Is acknowledged by academics that all bands are ultimately of mixed heritage and multilingualism and multiculturalism was the norm. In the West, mixed bands of Cree, Saulteaux, Métis, and Assiniboine, all partners in the Iron Confederacy , are the norm. However, in recent years, as indigenous languages have declined across western Canada where there were once three languages spoken on a given reserve, there may now only be one. This has led to

2880-493: Is also a major difference in grammatical vocabulary (particles) between the groups. Within both groups, another set of variations has arisen around the pronunciation of the Proto-Algonquian phoneme *l , which can be realized as /l/, /r/, /y/, /n/, or /ð/ (th) by different groups. Yet in other dialects, the distinction between /eː/ (ē) and /iː/ (ī) has been lost, merging to the latter. In more western dialects,

3000-541: Is an enclave of Schefferville. The other, Lac-John , is 2 km (1.2 mi) outside the town. Première Nation des Innus de Nutashkuan is based on their reserve of Natashquan 1 or Nutashkuan. The reserve is located on the north shore of the Gulf of Saint Lawrence at the mouth of the Natashquan River . Montagnais de Pakua Shipi  [ fr ] located in the community of Pakuashipi , Quebec, on

3120-669: Is based in Gillam , 248 kilometres (154 mi) northeast of Thompson via Provincial Road 280 (PR 280) , and has several reserves along the Nelson River . Shamattawa First Nation is located on their reserve, Shamattawa 1, on the banks of the Gods River where the Echoing River joins. The community is very remote; only connected via air or via winter ice roads to other First Nation communities. The Tataskweyak Cree Nation

3240-469: Is based on the reserve of York Landing, 30 kilometres (19 mi) south of Split Lake via ferry. York Factory was a settlement and Hudson's Bay Company (HBC) trading post, established in 1684, on the shore of Hudson Bay, at the mouth of the Hayes River . In 1956, the trading post was closed and the community was moved inland to the current site. Swampy Cree Tribal Council is, as the name suggests,

3360-580: Is composed of three Atikamekw First Nations. The council is based in La Tuque, Quebec . The Atikamekw are inhabitants of the area they refer to as Nitaskinan ("Our Land"), in the upper Saint-Maurice River valley. The First Nations: Eeyou Istchee is a territory equivalent to a regional county municipality (TE) of Nord-du-Québec represented by the Grand Council of the Crees . On 24 July 2012,

3480-547: Is in the Missanabie , Ontario area. The Moose Cree First Nation is based in Moose Factory in the Cochrane District. Moose Factory was founded in 1672–1673 by Charles Bayly , the first overseas governor of the Hudson's Bay Company, and was the company's second post. It was the first English settlement in what is now Ontario. The Nation has two reserves: Factory Island 1 on Moose Factory Island , an island in

3600-778: Is located at Fort Albany, Ontario, on the southern shore of the Albany River at James Bay. The reserve, Fort Albany 67, is shared with the Kashechewan First Nation. The Attawapiskat First Nation is located at mouth of the Attawapiskat River on James Bay. The community is on the Attawapiskat 91A reserve. The Attawapiskat 91 reserve is 27,000 hectares (67,000 acres) on both shores of the Ekwan River , 165 kilometres (103 mi) upstream from

3720-527: Is located in the Naskapi village of Kawawachikamach, 15 km (9.3 mi) northeast of Schefferville , Quebec. The village is in the reserve of the same name . The Mushuau Innu First Nation , located in the community of Natuashish , Newfoundland and Labrador, is located in the Natuashish 2 reserve on the coast of Labrador . Innus of Ekuanitshit live on their reserve of Mingan, Quebec , at

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3840-535: Is located in the community of Split Lake, Manitoba within the Split Lake 171 reserve, 144 kilometres (89 mi) northeast of Thompson on PR 280, on the lake of the same name on the Nelson River system. War Lake First Nation possess several reserves but are located on the Mooseocoot reserve in the community of Ilford, Manitoba , 35 kilometres (22 mi) east of York Landing. York Factory First Nation

3960-491: Is located near Grand Rapids, Manitoba , 400 kilometres (250 mi) north of Winnipeg at the mouth of the Saskatchewan River as it runs into Lake Winnipeg. Mosakahiken Cree Nation (also Rocky Cree) is located around the community of Moose Lake about 63 kilometres (39 mi) southeast of The Pas on their main reserve, Moose Lake 31A. Opaskwayak Cree Nation (also Rocky Cree) has several reserves but most of

4080-484: Is located on the north shore of Reindeer Lake close to the Saskatchewan border. It has one reserve, Brochet 197, 256 kilometres (159 mi) northwest of Thompson, adjoining the village of Brochet . The Bunibonibee Cree Nation is located along the eastern shoreline of Oxford Lake at the headwaters of the Hayes River . The Nation controls several reserves with the main reserve being Oxford House 24 adjacent to

4200-471: Is not so much a language, as a chain of dialects, where speakers from one community can very easily understand their neighbours, but a Plains Cree speaker from Alberta would find a Quebec Cree speaker difficult to speak to without practice." One major division between the groups is that the Eastern group palatalizes the sound /k/ to either /ts/ (c) or to /tʃ/ (č) when it precedes front vowels . There

4320-484: Is now regulated by Manitoba Hydro as part of the energy generation operations. Some property owners on the southern edge of the lake feel that the levels are now maintained at a higher average level than would be natural, and attribute erosion of their property to the lake level. Manitoba Hydro has pointed out that the regulation project also allows lake level to be lowered, such as during the 1997 floods, thereby preventing significant property damage. Although development of

4440-611: Is owned by twelve First Nations of which three are Swampy Cree. Cumberland House Cree Nation is based in Cumberland House, Saskatchewan on the Cumberland House Cree Nation 20 reserve, 97 kilometres (60 mi) southwest of Flin Flon , Manitoba. Cumberland House , founded in 1774 by Samuel Hearne , was the site of the HBC's first inland fur-trading post. The Red Earth First Nation is located in

4560-529: Is safety in numbers, all families would want to be part of some band, and banishment was considered a very serious punishment. Bands would usually have strong ties to their neighbours through intermarriage and would assemble together at different parts of the year to hunt and socialize together. Besides these regional gatherings, there was no higher-level formal structure, and decisions of war and peace were made by consensus with allied bands meeting together in council. People could be identified by their clan , which

4680-629: Is the Belcher Islands . The Belcher Islands are located in the centre of the Nastapoka arc. Another group includes the Ottawa Islands which are located near the eastern shore of the Hudson Bay. Hudson Bay occupies a large structural basin , known as the Hudson Bay basin, that lies within the Canadian Shield . The collection and interpretation of outcrop, seismic and drillhole data for exploration for oil and gas reservoirs within

4800-649: Is the largest bay in the world (the largest in area being the Bay of Bengal). The distinctive arculate segment on the eastern shore of Hudson Bay is referred to as the Nastapoka arc . There are many islands in Hudson Bay, mostly near the eastern coast. All the islands, including those in James Bay, are part of Nunavut and lie in the Arctic Archipelago . Several are disputed by the Cree. One group of islands

4920-685: The 20th century . The HBC's trade monopoly was abolished in 1870, by a British Order in Council called the Deed of Surrender , ceded Rupert's Land to Canada, an area of approximately 3,900,000 km (1,500,000 sq mi), as part of the Northwest Territories . In 1912, the western shore south of 60° and, following the Quebec Boundaries Extension Act, 1912 , all the eastern shore were transferred to

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5040-532: The Canadian Arctic , estimated to consist of approximately 54,473 individuals. Hudson Bay has a lower average salinity level than that of ocean water. The main causes are the low rate of evaporation (the bay is ice-covered for much of the year), the large volume of terrestrial runoff entering the bay (about 700 km (170 cu mi) annually, the Hudson Bay watershed covering much of Canada, many rivers and streams discharging into

5160-895: The Fort Peck Indian Reservation and as "Landless Cree" and "Rocky Boy Cree" on the Fort Belknap Indian Reservation , all in Montana . The Chippewa Cree share the reservation with the Pembina Band of Chippewa Indians , who form the "Chippewa" ( Ojibwa ) half of the Chippewa Cree tribe. On the other Reservations, the Cree minority share the Reservation with the Assiniboine , Gros Ventre and Sioux tribes. Traditionally,

5280-652: The Moose River , about 16 kilometres (9.9 mi) from its mouth at James Bay; and Moose Factory 68 , a tract of land about 15 kilometres (9.3 mi) upstream on the Moose River. The Taykwa Tagamou Nation has two reserves, New Post 69, and their main reserve, New Post 69A outside Cochrane, Ontario along the Abitibi River . Wabun Tribal Council is a regional chief's council based in Timmins, Ontario representing Ojibway and Cree First Nations in northern Ontario. Moose Cree members are: Brunswick House First Nation and Matachewan First Nation . Brunswick House's reserves are Mountbatten 76A and Duck Lake 76B located in

5400-422: The Northwest Territories to Labrador . It is the most widely spoken aboriginal language in Canada. The only region where Cree has official status is in the Northwest Territories, together with eight other aboriginal languages, French and English. The two major groups: Nehiyaw and Innu, speak a mutually intelligible Cree dialect continuum , which can be divided by many criteria. In a dialect continuum, "It

5520-407: The Rocky Boy Indian Reservation with Ojibwe (Chippewa) people. The documented westward migration over time has been strongly associated with their roles as traders and hunters in the North American fur trade . The Cree are generally divided into eight groups based on dialect and region. These divisions do not necessarily represent ethnic sub-divisions within the larger ethnic group: Due to

5640-557: The Sudbury District . The Kashechewan First Nation community is located on the northern shore of the Albany River on James Bay. The Hudson's Bay Company established a post, Fort Albany , at this location between 1675 and 1679. Kashechewan First Nation is one of two communities that were established from Old Fort Albany, the other being Fort Albany First Nation . The two Nations share the Fort Albany 67 reserve. The Missanabie Cree First Nation signed Treaty 9 in 1906 but did not receive any reserved lands until 2018. The Missanabie reserve

5760-416: The Algonquin. Depending on the community, the Cree may call themselves by the following names: the nēhiyawak, nīhithaw, nēhilaw , and nēhinaw ; or ininiw, ililiw, iynu (innu) , or iyyu . These names are derived from the historical autonym nēhiraw (of uncertain meaning) or from the historical autonym iriniw (meaning "person"). Cree using the latter autonym tend to be those living in

5880-430: The American company OmniTRAX to run privately. In December 2015, OmniTRAX announced it was negotiating a sale of the port, and the associated Hudson Bay Railway, to a group of First Nations based in northern Manitoba. With no sale finalized by July 2016, OmniTRAX shut down the port and the major railroad freight operations in August 2016. The railway continued to carry cargo to supply the town of Churchill itself until

6000-429: The Arctic Ocean ( Davis Strait ) by Hudson Strait ; on the north, with the Arctic Ocean by Foxe Basin (which is not considered part of the bay), and Fury and Hecla Strait . Hudson Bay is often considered part of the Arctic Ocean: the International Hydrographic Organization , in its 2002 working draft of Limits of Oceans and Seas , defined Hudson Bay, with its outlet extending from 62.5 to 66.5 degrees north (just

6120-448: The Arctic Ocean in the north. The Hudson Bay drainage basin drains a very large area, about 3,861,400 km (1,490,900 sq mi), that includes parts of southeastern Nunavut, Alberta , Saskatchewan , Ontario , Quebec , all of Manitoba , and parts of the U.S. states of North Dakota , South Dakota , Minnesota , and Montana . Hudson Bay's southern arm is called James Bay . The Eastern Cree name for Hudson and James Bay

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6240-403: The Burntwood and subsequently Nelson River is controlled by the Notigi Control Structure.( 55°51′37″N 99°19′51″W  /  55.8604°N 99.3308°W  / 55.8604; -99.3308  ( Notigi Control Structure ) ) Before the construction of the diversion, the Manitoba portion of the Churchill River was estimated to have 3 gigawatts of hydroelectric potential. The river

6360-479: The Canadian Shield continued to be submerged by rising sea levels except for a brief middle Ordovician marine regression . Only starting in the Late Ordovician and continuing into the Silurian did the gradual regional subsidence of this part of the Canadian Shield form the Hudson Bay basin. The formation of this basin resulted in the accumulation of black bituminous oil shale and evaporite deposits within its centre, thick basin-margin limestone and dolomite , and

6480-497: The Canadian Shield. The similarity in areal extent of the free-air gravity anomaly with the perimeter of the former Laurentide ice sheet that covered this part of Laurentia led to a long-held conclusion that this perturbation in the Earth's gravity reflected still ongoing glacial isostatic adjustment to the melting and disappearance of this ice sheet. Data collected over Canada by the Gravity Recovery and Climate Experiment (GRACE) satellite mission allowed geophysicists to isolate

6600-424: The Fisher River 44 and 44A reserves. Marcel Colomb First Nation is located outside of Lynn Lake on the Black Sturgeon reserve on Hughes Lake, 289 kilometres (180 mi) northwest of Thompson via Provincial Road 391 . Norway House Cree Nation is located in Norway House which is located on the Playgreen Lake section of the Nelson River system on the north side of Lake Winnipeg. In 1821, Norway House became

6720-466: The HBC built several factories ( forts and trading posts ) along the coast at the mouth of the major rivers (such as Fort Severn ; York Factory , Churchill ; and the Prince of Wales Fort ). The strategic locations were bases for inland exploration. More importantly, they were trading posts with Indigenous peoples who came to them with furs from their trapping season. The HBC shipped the furs to Europe and continued to use some of these posts well into

6840-437: The Hudson Bay watershed , called Rupert's Land . In 1670, the English Crown granted a charter to facilitate fur trading within the Hudson Bay drainage basin . France contested this grant by sending several military expeditions to the region, but abandoned its claim in the Treaty of Utrecht (April 1713). The Treaty of Utrecht, signed on 11 April 1713, marked a significant agreement between Britain and France. The treaty

6960-413: The Hudson Bay basin found that it is filled by, at most, 2,500 m (8,200 ft) of Ordovician to Devonian limestone , dolomites, evaporites , black shales , and various clastic sedimentary rocks that overlie less than 60 m (200 ft) of Cambrian strata that consist of unfossiliferous quartz sandstones and conglomerates , overlain by sandy and stromatolitic dolomites. In addition,

7080-446: The Mainland. Northern Hudson Bay has a polar climate ( Köppen : ET ) being one of the few places in the world where this type of climate is found south of 60 °N, going farther south towards Quebec , where Inukjuak is still dominated by the tundra . From Arviat , Nunavut , to the west to the south and southeast prevails the subarctic climate (Köppen: Dfc ). This is because in the central summer months, heat waves can advance from

7200-441: The Monsoni, (a branch of the Ojibwe ). Both groups had donned war paint in preparation to an attack on the Dakota and another group of Ojibwe. After acquiring firearms from the HBC, the Cree moved as traders into the plains, acting as middlemen with the HBC. The Naskapi are the Innu First Nations inhabiting a region of northeastern Quebec and Labrador , Canada. The Naskapi are traditionally nomadic peoples, in contrast with

7320-429: The Nelson River system was intended to secure a reliable source of low-cost energy to promote industrial development in Manitoba, such development was not forthcoming. Concerns about the magnitude and cost of Hydro development led the provincial government to start an inquiry into the management of the company. The Commission of Inquiry into Manitoba Hydro reported in 1979 that Manitoba Hydro had not developed resources in

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7440-437: The Nelson hydroelectric system. The great distance between generating sites on the Nelson River and load centres in southern Manitoba required the use of high-voltage direct current (HVDC) electric power transmission lines to bring the energy to market. When these lines began operation as the Nelson River Bipole in 1972, they were the longest and highest-voltage direct current lines in the world. The Dorsey converter station

7560-427: The Plains Cree, were allied with the Assiniboine , the Metis Nation, and the Saulteaux in what was known as the " Iron Confederacy ", which was a major force in the North American fur trade from the 1730s to the 1870s. The Cree and the Assiniboine were important intermediaries in the Indian trading networks on the northern plains. When a band went to war, they would nominate a temporary military commander, called

7680-504: The Quebec government signed an accord with the Cree Nation that resulted in the abolition of the neighbouring municipality of Baie-James and the creation of the new Eeyou Istchee James Bay Regional Government , providing for the residents of surrounding Jamésie TE and Eeyou Istchee to jointly govern the territory formerly governed by the municipality of Baie-James. Eeyou Istchee is a territory of eight enclaves within Jamésie plus one enclave (Whapmagoostui) within Kativik TE. Each enclave

7800-435: The Russian port of Murmansk . The increase in ships traversing the proposed Arctic Bridge will result in an increase in accidents that will release pollutants into the environment, due to the freezing of the water in the winter cleanup will be harder and with a shorter window of time. The biggest port in the Hudson bay is the city of Churchill, which lies on the river with the same name, Churchill River. The Port of Churchill

7920-616: The Sudbury District near Chapleau, Ontario. The Matachewan First Nation is on the Matachewan 72 reserve near Matachewan township in the Timiskaming District . Fort Severn First Nation and their reserve, Fort Severn 89, located on the mouth of the Severn River on Hudson Bay, is the most northern community in Ontario. It is a member of Keewaytinook Okimakanak Council . Mushkegowuk Council , based in Moose Factory, Ontario , represents chiefs from seven First Nations across Ontario. Swampy Cree members are: Fort Albany First Nation and Attawapiskat First Nation . Fort Albany First Nation

8040-416: The Trans-Hudson Orogen. The Belcher Islands are the eroded surface of the Belcher Fold Belt, which formed as a result of the tectonic compression and folding of sediments that accumulated along the margin of the Superior Craton before its collision with the Western Churchill Craton. Hudson Bay and the associated structural basin lie within the centre of a large free-air gravity anomaly that lies within

8160-420: The adjacent provinces, but the bay and offshore islands remained part of the Northwest Territories. Starting in 1913, the bay was extensively charted by the Canadian government's CSS  Acadia to develop it for navigation. This mapping progress led to the establishment of Churchill, Manitoba, as a deep-sea port for wheat exports in 1929, after unsuccessful attempts at Port Nelson . The Port of Churchill

8280-452: The basic unit of organization for Cree peoples was the lodge , a group of perhaps eight or a dozen people, usually the families of two separate but related married couples, who lived together in the same wigwam (domed tent) or tipi (conical tent), and the band , a group of lodges who moved and hunted together. In the case of disagreement, lodges could leave bands and bands could be formed and dissolved with relative ease. However, as there

8400-400: The bay), and the limited connection with the Atlantic Ocean and its higher salinity. Sea ice is about three times the annual river flow into the bay, and its annual freezing and thawing significantly alters the salinity of the surface layer. Although its exact effects are not fully understood currently, the cyclonic storms in the bay are responsible for synoptic variability of salinity along

8520-445: The closure of an ancient ocean basin . The current general consensus is that it is an arcuate boundary of tectonic origin between the Belcher Fold Belt and undeformed basement of the Superior Craton created during the Trans-Hudson orogeny. This is because no credible evidence for such an impact structure has been found by regional magnetic, Bouguer gravity , or other geologic studies. However, other Earth scientists have proposed that

8640-670: The coast became part of the Mid-Canada Line , watching for a potential Soviet bomber attack over the North Pole. The only Arctic deep-water port in Canada is the Port of Churchill , located at Churchill, Manitoba. Cree The Cree or nehinaw ( Cree : néhinaw , néhiyaw , nihithaw , etc.; French: Cri ) are a North American Indigenous people . They live primarily in Canada , where they form one of

8760-510: The coast were York Factory and Prince of Wales Fort . Communities along the Hudson Bay coast or on islands in the bay are (all populations are as of 2016): The Hudson's Bay Company built forts as fur trade strongholds against the French or other possible invaders. One example is York Factory with angled walls to help defend the fort. In the 1950s, during the Cold War , a few sites along

8880-486: The coast. One consequence of the lower salinity of the bay is that the freezing point of the water is higher than in the rest of the world's oceans, thus decreasing the time that the bay remains ice-free. The increase of river inflows during the winter has decreased the season of sea ice by more than one month since the 1960s. The lower salinity of the bay also has effects on the distribution and prevalence of common marine life such as micro algae. Research has shown that

9000-570: The community of Oxford House, Manitoba , 160 kilometres (99 mi) southeast of Thompson. God's Lake First Nation is located in the God's Lake Narrows area on the shore of God's Lake . The main reserve is God's Lake 23, 240 kilometres (150 mi) southeast of Thompson. The Manto Sipi Cree Nation also live on God's Lake in the community of God's River on the God's River 86A reserve, about 42 kilometres (26 mi) northeast of God's Lake Narrows. All of

9120-615: The community of Sheshatshiu in Labrador and is located approximately 45 km (28 mi) north of Happy Valley-Goose Bay . Sheshatshiu is located adjacent to the Inuit community of North West River . The Sheshatshiu Nation has one reserve, Sheshatshiu 3. Pekuakamiulnuatsh First Nation is located on the reserve of Mashteuiatsh in the Saguenay–Lac-Saint-Jean region, 8 km (5.0 mi) north of Roberval, Quebec , on

9240-822: The community of Red Earth, on the banks of the Carrot River , on the Carrot River 29A reserve. Close by is the Red Earth 29 reserve, about 75 kilometres (47 mi) east of Nipawin . Shoal Lake Cree Nation is located in Pakwaw Lake, on the Shoal Lake 28A reserve, 92 kilometres (57 mi) east of Nipawin. The Keewatin Tribal Council, described under Swampy Cree, also represents Rocky Cree First Nations in Manitoba. The Barren Lands First Nation

9360-605: The country's largest First Nations . More than 350,000 Canadians are Cree or have Cree ancestry. The major proportion of Cree in Canada live north and west of Lake Superior , in Ontario , Manitoba , Saskatchewan , Alberta , and the Northwest Territories . About 27,000 live in Quebec . In the United States, Cree people historically lived from Lake Superior westward. Today, they live mostly in Montana , where they share

9480-524: The development of extensive reefs that ringed the basin margins that were tectonically uplifted as the basin subsided. During Middle Silurian times, subsidence ceased and this basin was uplifted. It generated an emergent arch, on which reefs grew, that divided the basin into eastern and western sub-basins. During the Devonian Period, this basin filled with terrestrial red beds that interfinger with marine limestone and dolomites. Before deposition

9600-481: The distinction between /s/ and /ʃ/ (š) has been lost, both merging to the former. "Cree is a not a typologically harmonic language. Cree has both prefixes and suffixes, both prepositions and postpositions, and both prenominal and postnominal modifiers (e.g. demonstratives can appear in both positions)." Golla counts Cree dialects as eight of 55 North American languages that have more than 1,000 speakers and which are being actively acquired by children. The Cree are

9720-430: The entire bay is around 0 °C (32 °F) or below. In the extreme northeast, winter temperatures average as low as −29 °C (−20 °F). The Hudson Bay region has very low year-round average temperatures. The average annual temperature for Churchill at 59°N is −6 °C (21 °F) and Inukjuak, facing cool westerlies in summer at 58°N , an even colder −7 °C (19 °F). By comparison, Magadan , in

9840-525: The evidence of an Archean impact might have been masked by deformation accompanying the later formation of the Trans-Hudson orogen and regard an impact origin as a plausible possibility. The longer periods of ice-free navigation and the reduction of Arctic Ocean ice coverage have led to Russian and Canadian interest in the potential for commercial trade routes across the Arctic and into Hudson Bay. The so-called Arctic Bridge would link Churchill, Manitoba, and

9960-419: The form ililiw , coastal East Cree and Naskapi use iyiyiw (variously spelled iiyiyiu , iiyiyuu , and eeyou ), inland East Cree use iyiniw (variously spelled iinuu and eenou ), and Montagnais use ilnu and innu , depending on dialect. The Cree use "Cree", "cri", "Naskapi, or "montagnais" to refer to their people only when speaking French or English. As hunter-gatherers ,

10080-549: The gravity signal associated with glacial isostatic adjustment from longer–time scale process of mantle convection occurring beneath the Canadian Shield. Based upon this data, geophysicists and other Earth scientists concluded that the Laurentide Ice Sheet was composed of two large domes to the west and east of Hudson Bay. Modelling glacial isostatic adjustment using the GRACE data, they concluded that ≈25 to ≈45% of

10200-614: The greater degree of written standardization and prestige Plains Cree enjoys over other Cree dialects. The Métis (from the French, Métis – of mixed ancestry) are people of mixed ancestry, such as Cree and French, English, or Scottish heritage. According to Aboriginal Affairs and Northern Development Canada , the Métis were historically the children of French fur traders and Cree women or, from unions of English or Scottish traders and Cree, Northwestern Ojibwe, or northern Dene women ( Anglo-Métis ). The Métis National Council defines

10320-544: The hot land and make the weather milder, with the result that the average temperature surpasses 10 °C (50 °F). The bay receives water from various surrounding rivers and currents originating from the Foxe Basin in the north, resulting in a counterclockwise overall flow. At the extreme southern tip of the extension known as James Bay arises a humid continental climate with a longer and generally hotter summer. (Köppen: Dfb ). The average annual temperature in almost

10440-473: The ice over the winter, and the crew survived onshore at the southern tip of James Bay . In the spring, as the ice receded, Henry Hudson expressed a desire to continue exploring the uncharted region. However, on 22 June 1611, the crew mutinied. They left Hudson and others adrift in a small boat. The fate of Hudson and the other men stranded with him remains undetermined. Nevertheless, there is little evidence in historical documents to suggest that they persisted for

10560-547: The largest group of First Nations in Canada, with 220,000 members and 135 registered bands. Together, their reserve lands are the largest of any First Nations group in the country. The largest Cree band and the second largest First Nations Band in Canada after the Six Nations Iroquois is the Lac La Ronge Band in northern Saskatchewan. Given the traditional Cree acceptance of mixed marriages, it

10680-471: The last 100 years has led to decreases in the extent of the sea ice in Hudson Bay by 19.5% per decade. As well as a lengthening of the ice-free period, which was as short as four months in the late 17th century. The polar climate of Hudson Bay means it is home for a variety of polar climate animals, in the Western Hudson Bay (WHB) beluga whale population is the most significant known group in

10800-430: The latter part of the 15th century, directly resulted in the first sighting of Hudson Bay by Europeans. English explorers and colonists named Hudson Bay after Sir Henry Hudson who explored the bay beginning 2 August 1610, on his ship Discovery . On his fourth voyage to North America, Hudson worked his way around Greenland 's west coast and into the bay, mapping much of its eastern coast. Discovery became trapped in

10920-518: The line was damaged by flooding on 23 May 2017. The Port and the Hudson Bay Railway were sold to Arctic Gateway Group —a consortium of First Nations, local governments, and corporate investors—in 2018. On 9 July 2019, ships resupplying Arctic communities began stopping at the port for additional cargo, and the port began shipping grain again on 7 September 2019. The coast of Hudson Bay is extremely sparsely populated; there are only about

11040-471: The lower Nelson River to support both Manitoba load growth and export plans. Limestone, the largest generating station in Manitoba, is on the Lower Nelson only 90 km from Hudson Bay . Long-term firm power sales contracts were signed with Northern States Power Company of Minneapolis, Minnesota . Control dams and excavated channels have transformed Lake Winnipeg into a 25,000 km reservoir for

11160-473: The lower salinity of the Hudson Bay limits the growth of micro algae, which causes a notable change in biomass along the bay's salinity gradient. The western shores of the bay are a lowland known as the Hudson Bay Lowlands , covering 370,000 km (140,000 sq mi), and are Canada's largest continuous peatland . Much of the landform has been shaped by the actions of glaciers and

11280-408: The lowest-cost and most efficient way, and made many recommendations for the governance of Manitoba Hydro. Download coordinates as: 56°02′26″N 96°32′20″W  /  56.04056°N 96.53889°W  / 56.04056; -96.53889 Hudson Bay Hudson Bay , sometimes called Hudson's Bay (usually historically), is a large body of saltwater in northeastern Canada with

11400-458: The many dialects of the Cree language , the people have no modern collective autonym . The Plains Cree and Attikamekw refer to themselves using modern forms of the historical nêhiraw , namely nêhiyaw and nêhirawisiw , respectively. Moose Cree, East Cree, Naskapi, and Montagnais all refer to themselves using modern dialectal forms of the historical iriniw , meaning 'man.' Moose Cree use

11520-468: The mouth of South Indian Lake reduces the flow of the Churchill River to 15% of its natural flow. This causes South Indian Lake to rise 3 metres (10 feet), as opposed to the 10.6 metres (35 feet) envisioned in the original plan. The diverted water flows through the 9.3 km (5.8 mi) South Bay Diversion Channel into the Rat River , which is in the Nelson River watershed. The outflow of Rat River into

11640-830: The mouth of the Mingan River of the Saint Lawrence River in the Côte-Nord (north shore) region. Innu Takuaikan Uashat Mak Mani-Utenam based in Sept-Îles, Quebec, in the Côte-Nord region on the Saint Lawrence River. They own two reserves: Maliotenam 27A, 16 kilometres (9.9 mi) east of Sept-Îles, and Uashat 27, within Sept-Îles. Innu Nation of Matimekush-Lac John is based out of Schefferville, Quebec. One reserve, Matimekosh ,

11760-860: The mouth on James Bay. Independent from a Tribal Council is the Weenusk First Nation located in Peawanuck in the Kenora District. The community was located on their reserve of Winisk 90 on the mouth of the Winisk River on James Bay but the community was destroyed in the 1986 Winisk flood and the community had to be relocated to Peawanuck. Keewatin Tribal Council is a Tribal Council based in Thompson, Manitoba that represents eleven First Nations, of which five are Swampy Cree, across northern Manitoba. Fox Lake Cree Nation

11880-582: The northern limit of Hudson Bay as follows: A line from Nuvuk Point ( 62°21′N 78°06′W  /  62.350°N 78.100°W  / 62.350; -78.100 ) to Leyson Point, the Southeastern extreme of Southampton Island , through the Southern and Western shores of Southampton Island to its Northern extremity, thence a line to Beach Point ( 66°03′N 86°06′W  /  66.050°N 86.100°W  / 66.050; -86.100 ) on

12000-428: The observed free-air gravity anomaly was due to ongoing glacial isostatic adjustment, and the remainder likely represents longer time-scale effects of mantle convection. Earth scientists have disagreed about what created the semicircular feature known as the Nastapoka arc that forms a section of the shoreline of southeastern Hudson Bay. The Nastapoka arc forms a 155 degree curve and appears to be very circular. Noting

12120-572: The paucity of impact structures on Earth in relation to the Moon and Mars, Carlyle S. Beals proposed that it is possibly part of a Precambrian extraterrestrial impact structure that is comparable in size to the Mare Crisium on the Moon. In the same volume, John Tuzo Wilson commented on Beals' interpretation and alternately proposed that the Nastapoka arc may have formed as part of an extensive Precambrian continental collisional orogen, linked to

12240-1000: The population lives on the Opaskwayak 21E reserve, immediately north of and across the Saskatchewan River from The Pas. The Sapotaweyak Cree Nation is located in the Shoal River 65A reserve adjacent to the community of Pelican Rapids , about 82 kilometres (51 mi) south of The Pas. Wuskwi Sipihk First Nation has several reserves but the main reserve is Swan Lake 65C which contains the settlement of Indian Birch, about 150 kilometres (93 mi) south of The Pas. Not affiliated with any Tribal Council: Fisher River Cree Nation , Marcel Colomb First Nation , and Norway House Cree Nation . Fisher River Cree Nation , located approximately 177 kilometres (110 mi) north of Winnipeg in Koostatak on Lake Winnipeg , control

12360-499: The principal inland fur trading depot for the Hudson's Bay Company. Norway House was also where Treaty 5 was signed. They control more than 80 reserves from less than 2 hectares (4.9 acres) to their largest, Norway House 17, at over 7,600 hectares (19,000 acres). The Nation is one of the most populous in Canada with 8,599 people as of November 2021 . Prince Albert Grand Council is based in Prince Albert, Saskatchewan and

12480-544: The same parent company, and cargo connections are made with the Canadian National Railway system at HBR's southern terminus in The Pas . It is the only port of its size and scope in Canada that does not connect directly to the country's road system; all goods shipped overland to and from the port must travel by rail. The port was originally owned by the Government of Canada but was sold in 1997 to

12600-641: The same year and finished in 1976. Diversion began 9 September 1976 with full planned potential reached on 20 August 1977. More than 5000 MW of hydroelectric potential could be developed in Manitoba, which includes 1380 MW at the Conawapa site, 630 MW at the Keeyask site, and 1000 MW at the Gillam Island site, all on the lower Nelson river. Other sites have been assessed but are not currently under study for development. All of these developments would require

12720-455: The second-largest water body using the term " bay " in the world (after the Bay of Bengal ). The bay is relatively shallow and is considered an epicontinental sea , with an average depth of about 100 m (330 ft) (compared to 2,600 m (8,500 ft) in the Bay of Bengal ). It is about 1,370 km (850 mi) long and 1,050 km (650 mi) wide. On the east it is connected with

12840-463: The shore of an analogous large hyposaline marine inlet – the Baltic Sea – has an annual average of 8 °C (46 °F). Water temperature peaks at 8–9 °C (46–48 °F) on the western side of the bay in late summer. It is largely frozen over from mid-December to mid-June, when it usually clears from its eastern end westwards and southwards. A steady increase in regional temperatures over

12960-515: The shrinkage of the bay over long periods of time. The coastal area, located in a region characterized by permanently frozen layers of soil, known as permafrost , is a low-lying wetland that receives water from lakes and fast-flowing rivers. Signs of numerous former beachfronts can be seen far inland from the current shore. A large portion of the lowlands in the province of Ontario is part of the Polar Bear Provincial Park , and

13080-688: The southern limits of the Cree territory in Montana were the Missouri River and the Milk River . In Manitoba, the Cree were first contacted by Europeans in 1682, at the mouth of the Nelson and Hayes rivers by a Hudson's Bay Company (HBC) party traveling about 100 miles (160 km) inland. In the south, in 1732; in what is now northwestern Ontario, Pierre Gaultier de Varennes, sieur de La Vérendrye , met with an assembled group of 200 Cree warriors near present-day Fort Frances , as well as with

13200-588: The territorial Montagnais, the other segment of Innu. The Naskapi language and culture is quite different from the Montagnais, in which the dialect changes from y to n as in "Iiyuu" versus "Innu". Iyuw Iyimuun is the Innu dialect spoken by the Naskapi. Today, the Naskapi are settled into two communities: Kawawachikamach Quebec and Natuashish , Newfoundland and Labrador. The Naskapi Nation of Kawawachikamach

13320-444: The territories of Quebec and Labrador. The Cree language (also known in the most broad classification as Cree-Montagnais, Cree-Montagnais-Naskapi, to show the groups included within it) is the name for a group of closely related Algonquian languages , the mother tongue (i.e. language first learned and still understood) of approximately 96,000 people, and the language most often spoken at home of about 65,000 people across Canada, from

13440-481: The village of Les Escoumins, Quebec . The community is on the north shore of the Saint Lawrence River at the mouth of the Escoumins River in the Côte-Nord region, 40 km (25 mi) northeast of Tadoussac and 250 km (160 mi) northeast of Québec . Conseil de la Nation Atikamekw , officially named Atikamekw Sipi – Conseil de la Nation Atikamekw, is a tribal council in Quebec, Canada. It

13560-503: The west side of Manitoba and construction has begun as of 2012. Like any other large-scale activity, the Nelson River Hydroelectric Project has not been without controversy. In 1976, the Churchill River diversion project was set into operation. Flow was diverted by a series of channels and control structures into the Nelson River. Instead of developing hydroelectric sites along the Churchill River, water

13680-578: The western shore of Lac Saint-Jean . Bande des Innus de Pessamit based in Pessamit , Quebec, is located about 58 km (36 mi) southwest of Baie-Comeau along the north shore of the Saint Lawrence River at the mouth of the Betsiamites River . It is across the river directly north of Rimouski, Quebec . Pessamit is 358 km (222 mi) northeast of Quebec City. Innue Essipit are based in their reserve of Essipit , adjacent to

13800-624: The western shore of the mouth of the Saint-Augustin River on the north shore of the Gulf of Saint Lawrence in the Côte-Nord region. The community is adjacent to the settlement of Saint-Augustin . Montagnais de Unamen Shipu  [ fr ] are located at La Romaine, Quebec at the mouth of the Olomane River on the Gulf of Saint Lawrence. They have one reserve; Romaine 2. Sheshatshiu Innu First Nation located in

13920-576: Was an important shipping link for trade with Europe and Russia until its closure in 2016 by owner OmniTRAX . The port and the Hudson Bay Railway were then sold to the Arctic Gateway Group —a consortium of First Nations , local governments, and corporate investors—in 2018. On 9 July 2019, ships resupplying Arctic communities began stopping at the port for additional cargo, and the port began shipping grain again on 7 September 2019. The International Hydrographic Organization defines

14040-487: Was diverted by control structures and an artificial channel into the Nelson, thereby increasing flow and saving cost of development. The effects of this diversion on pre-existing water levels and the indigenous Cree and Métis people continue to be felt to this day. Negotiations between the affected Northern communities and Manitoba Hydro continue, to discuss mitigation measures and compensation for loss of traditional resource areas and sites. The water level of Lake Winnipeg

14160-502: Was however 160 km (100 mi) further north than the Nelson River, thus further from the major users of power in southern Manitoba. Jointly harnessing the water increased the flow of the Nelson River by 40%, while the flow of the Burntwood River is now 9 times pre-diversion levels. In 1973 Manitoba Hydro was granted an interim licence to divert 850 m/s (30,000 cu ft/s ) of water from the Churchill River. Construction began

14280-710: Was negotiated in Utrecht, Netherlands, and marked a crucial stage in the conclusion of the War of the Spanish Succession . Its provisions had a significant impact in shaping the postwar landscape and establishing a new order in both Europe and North America. French concessions in North America as outlined in the Treaty of Utrecht included: Hudson Bay region, Nova Scotia , and Newfoundland . During this period,

14400-460: Was terminated by marine regression, Upper Devonian black bituminous shale accumulated in the south-east of the basin. The remaining history of the Hudson Bay basin is largely unknown as a major unconformity separates Upper Devonian strata from glacial deposits of the Pleistocene . Except for poorly known terrestrial Cretaceous fluvial sands and gravels that are preserved as the fills of

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