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Caniapiscau Reservoir
The Caniapiscau Reservoir () is a reservoir on the upper Caniapiscau River in the Côte-Nord administrative region of the Canadian province of Quebec. It is the largest body of water in Quebec and the second largest reservoir in Canada. The Caniapiscau Reservoir, formed by two dams and forty-three dikes, is the largest reservoir in surface area of the James Bay Project. As headpond, it feeds the power plants of the La Grande complex in the winter and provides up to 35% of their production. Its total catchment area is about . The reservoir was named after Lake Caniapiscau that was flooded during the formation of the reservoir. The name is an adaptation of the Cree or Innu toponym ''kâ-neyâpiskâw'', which means "rocky point". Albert Peter Low had noted in 1895 that "a high rocky headland jutts into the lake." He probably referred to the northwest facing peninsula that gives the reservoir the shape of an arc as we current know it. The Caniapiscau Reservoir is accessible by b ...
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Caniapiscau, Quebec
Caniapiscau () is a vast unorganized territory in the Côte-Nord region of Quebec, Canada, part of Caniapiscau Regional County Municipality. The territory is home to the huge Caniapiscau Reservoir, the largest body of water in Quebec. The reservoir was named after Lake Caniapiscau that was flooded in 1981 during the formation of the reservoir. The name comes from the Cree or Innu term ''kaniapiskau'' or ''kaneapiskak'' which means "rocky point" or "place where there is a rocky point". Albert Peter Low had noted in 1895 that "a high rocky headland jutts into the lake." He probably referred to the northwest facing peninsula that gives the reservoir the shape of an arc as we know it now. In the 19th century, Lake Caniapiscau was frequented by hunters and fur traders. In 1834, the Hudson's Bay Company opened there an outpost to link its facilities in the James Bay region with those of Ungava Bay. The Kaniapiskau Post closed in 1870. Community Caniapiscau () is a small community ...
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Hydro-Québec
Hydro-Québec is a public utility that manages the generation, transmission and distribution of electricity in the Canadian province of Quebec, as well as the export of power to portions of the Northeast United States. It was established by the Government of Quebec in 1944 from the expropriation of private firms. This was followed by massive investment in hydro-electric projects like the James Bay Project. Today, with 63 hydroelectric power stations, the combined output capacity is 37,370 megawatts. Extra power is exported from the province and Hydro-Québec supplies 10 per cent of New England's power requirements. Hydro-Québec is a Crown corporation (state-owned enterprise) based in Montreal. In 2018, it paid CAD$2.39 billion in dividends to its sole shareholder, the Government of Québec. Its residential power rates are among the lowest in North America. More than 40 percent of Canada’s water resources are in Québec and Hydro-Québec is the fourth largest hydropower produ ...
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James Bay Energy
The Société d'énergie de la Baie James is the company in charge of building the hydroelectric development known as the James Bay Project in northern Quebec. It was established in December 1971 by the ''Société de développement de la Baie James'' (SDBJ), a Crown corporation of the province of Quebec and became a wholly owned subsididiary of Hydro-Québec in 1978. Origins In the summer of 1971, the National Assembly of Quebec passed Bill 50, an Act establishing the Société de développement de la Baie James (SDBJ), a Crown corporation tasked with the development of natural resources as well as the general administration of the James Bay territory. The development of the hydroelectric potential was the focus of a newly created subsidiary (the SEBJ) with Hydro-Québec as a majority shareholder along with the SDBJ. Both corporations would be chaired by Pierre A. Nadeau, an insurance executive recruited by Robert Bourassa's money man, Paul Desrochers. The passage of Bill 50 wa ...
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James Bay
James Bay (french: Baie James; cr, ᐐᓂᐯᒄ, Wînipekw, dirty water) is a large body of water located on the southern end of Hudson Bay in Canada. Both bodies of water extend from the Arctic Ocean, of which James Bay is the southernmost part. Despite bordering the Canadian provinces of Quebec and Ontario, the bay and the islands within it, the largest of which is Akimiski Island, are politically part of Nunavut. Numerous waterways of the James Bay watershed have been modified with dams or diversion for several major hydroelectric projects. These waterways are also destinations for river-based recreation. Several communities are located near or alongside James Bay, including a number of Aboriginal Canadian communities, such as the Kashechewan First Nation and nine communities affiliated with the Cree of northern Quebec. As with the rest of Hudson Bay, the waters of James Bay routinely freeze over in winter. It is the last part of Hudson Bay to freeze over in winter, and the ...
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Hudson's Bay Company
The Hudson's Bay Company (HBC; french: Compagnie de la Baie d'Hudson) is a Canadian retail business group. A fur trading business for much of its existence, HBC now owns and operates retail stores in Canada. The company's namesake business division is Hudson's Bay, commonly referred to as The Bay ( in French). After incorporation by English royal charter in 1670, the company functioned as the ''de facto'' government in parts of North America for nearly 200 years until the HBC sold the land it owned (the entire Hudson Bay drainage basin, known as Rupert's Land) to Canada in 1869 as part of the Deed of Surrender, authorized by the Rupert's Land Act 1868. At its peak, the company controlled the fur trade throughout much of the English- and later British-controlled North America. By the mid-19th century, the company evolved into a mercantile business selling a wide variety of products from furs to fine homeware in a small number of sales shops (as opposed to trading posts) acros ...
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Ungava Bay
Ungava Bay (french: baie d'Ungava, ; iu, ᐅᖓᕙ ᑲᖏᖅᓗᒃ/) is a bay in northeastern Canada separating Nunavik (far northern Quebec) from Baffin Island. Although not geographically apparent, it is considered to be a marginal sea of the Arctic Ocean for climatic reasons. The bay is roughly oval-shaped, about at its widest point and about in length; it has an area of approximately . It is generally fairly shallow, under , though at its border with the Atlantic Ocean depths of almost are reached. Geography Although it is quite close to the open Atlantic (separated only by Hudson Strait), Ungava Bay is part of the Arctic Ocean. Ungava Bay is separated from Hudson Bay by the Ungava Peninsula. Akpatok Island is largest of the many islands in Ungava Bay. Bathymetric studies suggest that Ungava Bay may be the remnant of an impact crater (age unknown) approximately in diameter. The southwestern corner of Ungava Bay vies with the Bay of Fundy for the highest tidal range in t ...
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Koksoak River
__NOTOC__ The Koksoak River (french: rivière Koksoak) is a river in northern Quebec, Canada, the largest river in the Nunavik region. The Inuit village and region's administrative centre Kuujjuaq lies on the shores of the Koksoak, about south from its mouth. The name ''Koksoak'' is believed to originate from Moravian missionaries who evangelized among the Inuit of the area at the beginning of British rule and incorrectly spelled the Inuktitut word ''Kuujjuaq'', meaning "great river." In the 19th century, the river was also known as Big or South River, taken from South Bay which was the name of Ungava Bay at that time. In 1916, the name Koksoak was officially adopted. The Koksoak River arises at the confluence of its two main tributaries, the Rivière aux Mélèzes to the west and the Caniapiscau River to the south. The Koksoak River flows for about in an east-northeasterly direction into Ungava Bay, and passes by the village of Kuujjuaq, from where it flows northwards for abo ...
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Post-glacial Rebound
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution. The direct raising effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through the processes of ''ocean siphoning'' and ''continental levering'', the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.Milne, G.A., and J.X. Mitrovica (2008) ''Searching for eustasy in deglacial sea-level histories.'' Quaternary Science Reviews. 27:2292–2302. Overview During the last glacial period, much of northern Eu ...
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Nunavik
Nunavik (; ; iu, ᓄᓇᕕᒃ) comprises the northern third of the province of Quebec, part of the Nord-du-Québec region and nearly coterminous with Kativik. Covering a land area of north of the 55th parallel, it is the homeland of the Inuit of Quebec and part of the wider Inuit Nunangat. Almost all of the 14,045 inhabitants ( 2021 census) of the region, of whom 90% are Inuit, live in fourteen northern villages on the coast of Nunavik and in the Cree reserved land (TC) of Whapmagoostui, near the northern village of Kuujjuarapik. means "great land" in the local dialect of Inuktitut and the Inuit inhabitants of the region call themselves . Until 1912, the region was part of the District of Ungava of the Northwest Territories. Negotiations for regional autonomy and resolution of outstanding land claims took place in the 2000s. The seat of government would be Kuujjuaq. Negotiations on better empowering Inuit political rights in their land are still ongoing. A flag for N ...
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Gulf Of Saint Lawrence
, image = Baie de la Tour.jpg , alt = , caption = Gulf of St. Lawrence from Anticosti National Park, Quebec , image_bathymetry = Golfe Saint-Laurent Depths fr.svg , alt_bathymetry = Bathymetry of the Gulf of St. Lawrence , caption_bathymetry = Bathymetry of the Gulf of St. Lawrence , location = , group = , coordinates = , type = Gulf , etymology = , part_of = , inflow = , rivers = , outflow = , oceans = , catchment = , basin_countries = CanadaSaint Pierre and Miquelon (France) , agency = , designation = , date-built = , engineer = , date-flooded = , length = , width = , area = , depth = , max-depth = , volume = , residence_time = , salinity ...
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Proglacial Lake
In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around the ice. At the end of the last ice age about 10,000 years ago, large proglacial lakes were a widespread feature in the northern hemisphere. Moraine-dammed The receding glaciers of the tropical Andes have formed a number of proglacial lakes, especially in the Cordillera Blanca of Peru, where 70% of all tropical glaciers are. Several such lakes have formed rapidly during the 20th century. These lakes may burst, creating a hazard for zones below. Many natural dams (usually moraines) containing the lake water have been reinforced with safety dams. Some 34 such dams have been built in the Cordillera Blanca to contain proglacial lakes. Several proglacial lakes have also formed in recent decades at the end of glaciers on the eastern side of Ne ...
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