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Cascapédia River
The Cascapédia River is a river in the Gaspé Peninsula of Quebec, Canada, which has its source at Lake Cascapedia, fed by streams of the Chic-Choc Mountains, and empties into Cascapedia Bay (''Baie de la Cascapédia''), a small bay of Chaleur Bay. The river is about long. At times, it is also called Grand Cascapédia River to differentiate it from the Little Cascapédia River which empties into the same bay just to the east. The Cascapedia is known for its Atlantic salmon (''salmo salar'') fishing. With average catches of and a record catch of , caught in 1886, the river has long been recognized as one of Quebec's richest salmon rivers. Already back in 1835, surveyor Joseph Hamel noted the abundance of fish, including trout, salmon, carp, and whitefish. Several Governors General of Canada, including The Marquess of Lansdowne and Lord Stanley, had summer homes along this river. The river is accessible via Quebec Route 299 that follows the river's course for . Almost its enti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bas-Saint-Laurent
The Bas-Saint-Laurent (Lower Saint-Lawrence), is an administrative region of Quebec located along the south shore of the lower Saint Lawrence River in Quebec. The river widens at this place, later becoming a bay that discharges into the Atlantic Ocean and is often nicknamed ''"Bas-du-Fleuve"'' (Lower-River). The region is formed by eight regional county municipalities and 114 municipalities. In the south, it borders Maine of the United States, and the Canadian New Brunswick and the regions of Chaudière-Appalaches and Gaspésie–Îles-de-la-Madeleine. It had a population of 197,385 and a land area of as of the 2016 Census. The territory has evidence of human occupation since the Pleistocene by successive indigenous peoples. The historic First Nations occupied it all until European colonisation started in the late 17th century; France made land concessions to settlers under the Seigneurial system of New France to encourage colonization. However, development of this region was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaspésie National Park
Gaspésie National Park (french: Parc national de la Gaspésie) is a provincial park located south of the town of Sainte-Anne-des-Monts, Quebec, Canada in the inland of the Gaspé peninsula. The park contains the highest peak of the Appalachian Mountains in Canada, Mont Jacques-Cartier, above sea level. In addition, the park contains the only population of Caribou found south of the Saint Lawrence River in Canada. Geology There are two major and geologically distinct mountain ranges in the park. The first one, to the west of the St-Anne's River, is the Chic-Choc Mountains, Chic-Choc Mountain range. This range is 600 million years old and was mainly formed from underwater volcanic activity. In contrast, the McGerrigle Mountains are much younger, only 380 million years. From the depths of the sea, magma oozed through cracks in the Earth's crust and then cooled, resulting in a large underground granite batholith. Over time, the softer sedimentary rocks above the batholith eroded ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rivers Of Quebec
This is a list of rivers of Quebec. Quebec has about: *one million lakes of which 62279 have a toponymic designation (a name), plus 218 artificial lakes; *15228 watercourses with an official toponymic designation, including 12094 streams and 3134 rivers. Quebec has 2% of all fresh water on the planet."''Du Québec à la Louisiane, sur les traces des Français d'Amérique'', Géo Histoire, Hors-série, Éditions Prisma, Paris, October 2006 James Bay watershed James Bay Rivers flowing into James Bay, listed from south to north * Rivière au Saumon (Baie James) * Rivière au Phoque (Baie James) * Désenclaves River * Roggan River **Corbin River ** Anistuwach River * Kapsaouis River * Piagochioui River =Tributaries of La Grande River= =Tributaries of Rupert River= =Tributaries of Broadback River= =Tributaries of Nottaway River= Tributaries of Waswanipi River (which empties in Nottaway River via Matagami Lake) Tributaries of Bell River Quebec rivers flowing in Ontario (o ... [...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] |
PH Level
In chemistry, pH (), historically denoting "potential of hydrogen" (or "power of hydrogen"), is a scale used to specify the acidity or basicity of an aqueous solution. Acidic solutions (solutions with higher concentrations of ions) are measured to have lower pH values than basic or alkaline solutions. The pH scale is logarithmic and inversely indicates the concentration of hydrogen ions in the solution.Bates, Roger G. ''Determination of pH: theory and practice''. Wiley, 1973. :\ce = - \log(a_\ce) = -\log( ce\ce M) where M = mol dm−3. At 25 °C (77 °F), solutions with a pH less than 7 are acidic, and solutions with a pH greater than 7 are basic. Solutions with a pH of 7 at this temperature are neutral (i.e. have the same concentration of H+ ions as OH− ions, i.e. pure water). The neutral value of the pH depends on the temperaturebeing lower than 7 if the temperature increases above 25 °C. The pH value can be less than 0 for very concentrated strong acids, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Electrical Conductivity
Electrical resistivity (also called specific electrical resistance or volume resistivity) is a fundamental property of a material that measures how strongly it resists electric current. A low resistivity indicates a material that readily allows electric current. Resistivity is commonly represented by the Greek letter (rho). The SI unit of electrical resistivity is the ohm-meter (Ω⋅m). For example, if a solid cube of material has sheet contacts on two opposite faces, and the resistance between these contacts is , then the resistivity of the material is . Electrical conductivity or specific conductance is the reciprocal of electrical resistivity. It represents a material's ability to conduct electric current. It is commonly signified by the Greek letter ( sigma), but ( kappa) (especially in electrical engineering) and ( gamma) are sometimes used. The SI unit of electrical conductivity is siemens per metre (S/m). Resistivity and conductivity are inte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chloride
The chloride ion is the anion (negatively charged ion) Cl−. It is formed when the element chlorine (a halogen) gains an electron or when a compound such as hydrogen chloride is dissolved in water or other polar solvents. Chloride salts such as sodium chloride are often very soluble in water.Green, John, and Sadru Damji. "Chapter 3." ''Chemistry''. Camberwell, Vic.: IBID, 2001. Print. It is an essential electrolyte located in all body fluids responsible for maintaining acid/base balance, transmitting nerve impulses and regulating liquid flow in and out of cells. Less frequently, the word ''chloride'' may also form part of the "common" name of chemical compounds in which one or more chlorine atoms are covalently bonded. For example, methyl chloride, with the standard name chloromethane (see IUPAC books) is an organic compound with a covalent C−Cl bond in which the chlorine is not an anion. Electronic properties A chloride ion (diameter 167 pm) is much larger tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sulfate
The sulfate or sulphate ion is a polyatomic anion with the empirical formula . Salts, acid derivatives, and peroxides of sulfate are widely used in industry. Sulfates occur widely in everyday life. Sulfates are salts of sulfuric acid and many are prepared from that acid. Spelling "Sulfate" is the spelling recommended by IUPAC, but "sulphate" was traditionally used in British English. Structure The sulfate anion consists of a central sulfur atom surrounded by four equivalent oxygen atoms in a tetrahedral arrangement. The symmetry is the same as that of methane. The sulfur atom is in the +6 oxidation state while the four oxygen atoms are each in the −2 state. The sulfate ion carries an overall charge of −2 and it is the conjugate base of the bisulfate (or hydrogensulfate) ion, , which is in turn the conjugate base of , sulfuric acid. Organic sulfate esters, such as dimethyl sulfate, are covalent compounds and esters of sulfuric acid. The tetrahedral molecular geometry of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonate
A carbonate is a salt of carbonic acid (H2CO3), characterized by the presence of the carbonate ion, a polyatomic ion with the formula . The word ''carbonate'' may also refer to a carbonate ester, an organic compound containing the carbonate group C(=O)(O–)2. The term is also used as a verb, to describe carbonation: the process of raising the concentrations of carbonate and bicarbonate ions in water to produce carbonated water and other carbonated beverageseither by the addition of carbon dioxide gas under pressure or by dissolving carbonate or bicarbonate salts into the water. In geology and mineralogy, the term "carbonate" can refer both to carbonate minerals and carbonate rock (which is made of chiefly carbonate minerals), and both are dominated by the carbonate ion, . Carbonate minerals are extremely varied and ubiquitous in chemically precipitated sedimentary rock. The most common are calcite or calcium carbonate, CaCO3, the chief constituent of limestone (as well a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jean-Baptiste-Louis Franquelin
Jean-Baptiste-Louis Franquelin (1650-c.1712) was a French trader who was appointed in the early 1670s as the first cartographer in '' Nouvelle France'' (Canada) by the colony's governor. He was appointed in 1688 as royal hydrographer by Louis XIV. Franquelin was born in the commune of Pallauau-sur-Indre in central France. He migrated to New France in 1671 where he was soon appointed as the colony's cartographer. He documented a decade of Louis Jolliet and René-Robert Cavelier de La Salle's explorations in North America. He also completed other projects for the Crown and served the king's military engineer. After returning to France in 1692, he never lived in Canada again. Biography Born at Saint-Michel de Villebernin, he grew up in the village in the small commune of Palluau-sur-Indre in central France. Having developed drawing and mapmaking skills, Franquelin migrated in 1671 from Indre department to ''Nouvelle France'' (Quebec) to work as a trader. New France Governor L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mi'kmaq Language
The Mi'kmaq (also ''Mi'gmaq'', ''Lnu'', ''Miꞌkmaw'' or ''Miꞌgmaw''; ; ) are a First Nations people of the Northeastern Woodlands, indigenous to the areas of Canada's Atlantic Provinces and the Gaspé Peninsula of Quebec as well as the northeastern region of Maine. The traditional national territory of the Mi'kmaq is named Miꞌkmaꞌki (or Miꞌgmaꞌgi). There are 170,000 Mi'kmaq people in the region, (including 18,044 members in the recently formed Qalipu First Nation in Newfoundland.) Nearly 11,000 members speak Miꞌkmaq, an Eastern Algonquian language. Once written in Miꞌkmaw hieroglyphic writing, it is now written using most letters of the Latin alphabet. The Mi'kmaq, Maliseet, and Pasamaquoddy nations signed a series of treaties known as the Covenant Chain of Peace and Friendship Treaties with the British Crown throughout the eighteenth century; the first was signed in 1725, and the last in 1779. The Miꞌkmaq maintain that they did not cede or give up their land t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
