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Presqu'île Lake (Nord-du-Québec)
The Presqu'île Lake (French: ''Lac de la Presqu’île'') is a body of water forming a lake at South of the center of the village Chapais, in the regional County Municipality (RCM) of Eeyou Istchee Baie-James, in the administrative region of Nord-du-Quebec, in Quebec, in Canada. This body of water straddles the townships of Lévy, de Brongniart, and Brochant. The northern part of the lake is served by a forest road from the village of Chapais and stands out from route 113. The surface of the “Presqu’île Lake” is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Geography The Presqu'île lake took place inside the Presqu'île crater, crater impact of meteorite dating from Cambrian. The horseshoe-shaped lake measures of length by wide and covers an area of about . A moor of land advances on towards the South-West either towards the middle of the lake, since the Northeastern shore, forming a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baie-James
The Municipality of Baie-James (french: Municipalité de Baie-James) was a municipality in northern Quebec, Canada, which existed from 1971 to 2012. Located to the east of James Bay, Baie-James covered of land, making it the largest incorporated municipality in Canada — only eight Unorganized area (Canada), unorganized territories were larger. Its territory almost entirely (about 98%) covered the administrative region of Jamésie, although it contained less than five percent of the population. Essentially, it was the remainder of the Jamésie Territory's land after all of the major population centres were removed. On July 24, 2012, the Quebec government signed an accord with the Cree that would result in the abolition of Baie-James and the creation of a regional government known as Eeyou Istchee James Bay Territory. The hydroelectric power plants of the James Bay Project, La Grande Complex were all located within the municipal boundaries of Baie-James, making the municipalit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cosmic Impact
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Cosmic commonly refers to: * The cosmos, a concept of the universe Cosmic may also refer to: Media * ''Cosmic'' (album), an album by Bazzi * Afro/Cosmic music * "Cosmic", a song by Kylie Minogue from the album '' X'' * CosM.i.C, a member of the Swedish rap group Looptroop Rockers * Cosmic, an album by Thomas Anders Science * An electronic medical record software developed by Cambio * Constellation Observing System for Meteorology, Ionosphere, and Climate * COSMIC cancer database * COSMIC functional size measurement Other uses * Cosmic Top Secret, a category of classified information used by NATO * Cosmic ocean, a mythological motif See also * Cosmic background (other) * Cosmos (other) Cosmos generally refers to an orderly or harmonious system. Cosmos or Kosmos may also refer to: Space * ''Cosmos 1'', a privately funded solar sail spacecraft project * Cosmic Evolution Survey (COSMOS), a Hubble Space Telescope Treasury Project ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nottaway River Drainage Basin
The Nottoway are an Iroquoian Native American tribe in Virginia. The Nottoway spoke a Nottoway language in the Iroquoian language family. Names The term ''Nottoway'' may derive from ''Nadawa'' or ''Nadowessioux'' (widely translated as "poisonous snake"), an Algonquian-language term. Frank Siebert suggested that the term ''natowewa'' stems from Proto-Algonquian ''*na:tawe:wa'' and refers to the Massasauga, a pit viper of the Great Lakes region. The extension of the meaning as "Iroquoian speakers" is secondary. In Algonquian languages beyond the geographical range of the viper (i.e. Cree–Innu–Naskapi and Eastern Algonquian), the term's primary reference continues to focus on ''*na:t-'' 'close upon, mover towards, go after, seek out, fetch' and ''*-awe:'' 'condition of heat, state of warmth,' but no longer refers to the viper. A potential etymology in Virginia of ''*na:tawe:wa'' (Nottoway) refers to ''*na:t-'' 'seeker' + ''-awe:'' 'fur,' or literally 'traders' The earliest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Lakes In Canada
This is a partial list of lakes of Canada. Canada has an extremely large number of lakes, with the number of lakes larger than three square kilometres being estimated at close to 31,752 by the Atlas of Canada. Of these, 561 lakes have a surface area larger than 100 km2, including four of the Great Lakes. Almost 9% () of Canada's total area is covered by freshwater. There is no official estimate of the number of smaller lakes. This list covers lakes larger than . Canada's largest lakes This is a list of lakes of Canada with an area larger than . Alberta This is a list of lakes of Alberta with an area larger than . British Columbia This is a list of lakes of British Columbia with an area larger than . * Manitoba This is a list of lakes of Manitoba with an area larger than . New Brunswick Newfoundland and Labrador This is a list of lakes of Newfoundland and Labrador with an area larger than . Northwest Territories This is a list of lakes of the Northwest T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chibougamau River
The Chibougamau River flows west in the Chibougamau, then Eeyou Istchee James Bay (municipality) in the administrative region of Nord-du-Québec, Quebec, Canada. From the source, the course of the river successively crosses the townships of: Roy, McKenzie, O'Balski, Hauy, Scott, Barlow, Mckenzie, Blainlock, McKenzie, Barlow, Cuvier, Opemisca, Lamarck, Guettard, Saussure, Ribourde, Ronciere, Ribourde, Krieghoff and Gand. The surface of the Iserhoff North River is usually frozen from early November to mid-May, however, safe ice circulation is usually from mid-November to mid-April. Geography The surrounding hydrographic slopes of the Chibougamau River are: *North side: Maicasagi River, Caupichigau River, Comencho Lake and Opataca Lake; *East side: Chibougamau Lake, Obatogamau Lakes; *South side: Opawica River and Obatogamau River; *West side: Waswanipi River, Lake Waswanipi, Goéland Lake (Waswanipi River). The head of the Chibougamau River hydrographic slope is located ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waswanipi River
The Waswanipi River is a tributary of Matagami Lake. The Waswanipi River flows in the Municipality of Eeyou Istchee Baie-James in the administrative region of Nord-du-Québec, in Quebec, Canada. Geography The main hydrographic slopes adjacent to the Waswanipi River are: *North side: Nomans River, Inconnue River (Maicasagi River), Maicasagi River, La Trève River; *East side: Chibougamau River, Opawica River; *South side: Lake Waswanipi, O'Sullivan River, Wetetnagami River; *West side: Matagami Lake, Bell River, Nottaway River. The river originates in the village of Waswanipi, in the canton of Ghent, at the junction of the Chibougamau (coming from the east) and Opawica (coming from South). This start of the Waswanipi River is located at southwest of Chapais and about southwest of Chibougamau. A bridge spans the river at the village of Waswanipi. From its source, the course of the river flows over distributed as follows: * almost straight to the west up to a riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Matagami Lake
Lake Matagami is a lake in Jamésie, in Nord-du-Québec, in Quebec, in Canada. It is located just north-northeast of the town of Matagami. Geography Located in a marshy area of northern Quebec, the lake created by the meeting of the rivers Allard, Bell, Gouault, the Canet and Waswanipi. This lake is about wide, with a length of and an area of . History Matagami Lake has long been used as a transportation route in the fur trade from the 18th century to the 20th century by the Hudson's Bay Company. Toponymy In Cree, "matagami" means "meeting of waters", in reference to the large rivers that join. See also *Nottaway River, a watercourse * Gouault River, a watercourse *Allard River, a watercourse * Bell River, a watercourse *Waswanipi River, a watercourse *Canet River, a watercourse *James Bay *Matagami, Quebec Matagami (, ) is a small town in Quebec, Canada. It is located north of Amos, on Matagami Lake, at the northern terminus of Route 109 and the start of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nottaway River
The Nottaway River is a river in Quebec, Canada. The river drains Lake Matagami and travels north-west before emptying into Rupert Bay at the south end of James Bay. Its drainage basin is and has a mean discharge of 1190 m³/s (1556 yd³/s). Its source is the head of the Mégiscane River, which is from the mouth. Significant lakes along its course are Soscumica Lake () and Dusaux Lake (). The Nottaway, together with the Broadback and Rupert Rivers, was initially considered to be dammed and developed as part of the James Bay Project. But in 1972 hydro-electric development began on the more northerly La Grande and Eastmain Rivers, and the NBR Project was shelved. With the decision to divert the Rupert River to the La Grande, it is not likely that the Nottaway will be developed in the foreseeable future. Geography Nottaway means the lower course of Lake Matagami and a length of , of a watercourse which originates in the Mégiscane Lake. The whole is a long river of units flow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chibougamau
Chibougamau () is the largest town in Nord-du-Québec, central Quebec, Canada. Located on Lake Gilman it has a population of 7,504 people (2016 Canadian Census). Chibougamau is surrounded by, but not part of, the local municipality of Eeyou Istchee James Bay Regional Government. Due to its remoteness from Lac Saint-Jean (over south-east) and Abitibi-Témiscamingue (over south-west) areas, Chibougamau provides services for a few smaller communities surrounding it (Mistissini, Oujé-Bougoumou and Chapais) and for the regional resource-based industries. Despite Chibougamau's remoteness, it is only about as far north as Winnipeg, and is south of any part of the mainland of England. Nearby are Lake Aux Dorés, which is fed by the Chibougamau River from the larger Chibougamau Lake, after which the town was named. ''Chibougamau'' means "Gathering place" in the Cree language. The neighbouring Cree village of Oujé-Bougoumou has the same name with a more traditional Cree spelling. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Shield
The Canadian Shield (french: Bouclier canadien ), also called the Laurentian Plateau, is a geologic shield, a large area of exposed Precambrian igneous and high-grade metamorphic rocks. It forms the North American Craton (or Laurentia), the ancient geologic core of the North American continent. Glaciation has left the area with only a thin layer of soil, through which exposures of igneous bedrock resulting from its long volcanic history are frequently visible. As a deep, common, joined bedrock region in eastern and central Canada, the Shield stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada and most of Greenland; it also extends south into the northern reaches of the United States. Geographical extent The Canadian Shield is a physiographic division comprising four smaller physiographic provinces: the Laurentian Upland, Kazan Region, Davis and James. The shield extends into the United States as the Adirondack Mountains (connected by the Fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shatter Cone
Shatter cones are rare geological features that are only known to form in the bedrock beneath meteorite impact craters or underground nuclear explosions. They are evidence that the rock has been subjected to a shock with pressures in the range of . Morphology Shatter cones have a distinctively conical shape that radiates from the top (''apex'') of the cones repeating cone-on-cone in large and small scales in the same sample. Sometimes they have more of a spoon shape on the side of a larger cone. In finer-grained rocks such as limestone, they form an easily recognizable "horsetail" pattern with thin grooves (''striae''). However, the word "striae" should not be used to describe shatter cones, as that is considered misleading. Coarser grained rocks tend to yield less well developed shatter cones, which may be difficult to distinguish from other geological formations such as slickensides. Geologists have various theories of what causes shatter cones to form, including compress ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
