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Lake Bermen
Lake Bermen (french: Lac Bermen, formerly known as ''Lac Allemand'') is a lake in the province of Quebec, Canada. The lake is on ancient rocks of the Superior Province where gold mineralization has been found. It is named after Claude de Bermen de la Martinière (1636–1719), a senior official in New France. Location The Lake Bermen region ( NTS 23F) is in the centre of the province of Quebec near the border with Labrador. It is northwest of the town of Fermont and south of the Caniapiscau Reservoir. The region is accessible by float plane from Fermont or by helicopter from Wabush airport in Labrador. There are less than two inhabitants per . Lake Bermen is in the unorganized territory of Caniapiscau in the Côte-Nord region of Quebec. Hydrography Lake Bermen is long and wide, and has an area of . It is in a swampy area about southeast of Caniapiscau Reservoir. The lake is fed by several bodies of water further south, and drains to the north via lakes Rossignol and Guill ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pluton
In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and New Jersey; the Henry Mountains of Utah; the Bushveld Igneous Complex of South Africa; Shiprock in New Mexico; the Ardnamurchan intrusion in Scotland; and the Sierra Nevada Batholith of California. Because the solid country rock into which magma intrudes is an excellent insulator, cooling of the magma is extremely slow, and intrusive igneous rock is coarse-grained (phaneritic). Intrusive igneous rocks are classified separately from extrusive igneous rocks, generally on the basis of their mineral content. The relative amounts of quartz, alkali feldspar, plagioclase, and feldspathoid is particularly important in classifying intrusive igneous rocks. Intrusions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beauport, Quebec City
Beauport is a borough of Quebec City, Quebec, Canada on the Saint Lawrence River. Beauport is a northeastern suburb of Quebec City. Manufacturers include paint, construction materials, printers, and hospital supplies. Food transportation is important to the economy. Attractions include ''Parc de la Chute-Montmorency'' (Montmorency Falls Park), which contains a fortification built in 1759 by James Wolfe and Manoir Montmorency, the home from 1791 to 1794 of Prince Edward, Duke of Kent and Strathearn. The city's historic district contains many interesting churches and homes, including Bélanger-Girardin House, a National Historic Site of Canada where visitors can learn about Beauport's heritage. Annual events include the spring arts festival Salon de Mai and the summer Festival Folklorique des enfants du monde, a multicultural and international children's folklore festival. History Beauport was established in 1634, making it one of the oldest European-founded communities in Canad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebec City
Quebec City ( or ; french: Ville de Québec), officially Québec (), is the capital city of the Provinces and territories of Canada, Canadian province of Quebec. As of July 2021, the city had a population of 549,459, and the Communauté métropolitaine de Québec, metropolitan area had a population of 839,311. It is the eleventhList of the largest municipalities in Canada by population, -largest city and the seventhList of census metropolitan areas and agglomerations in Canada, -largest metropolitan area in Canada. It is also the List of towns in Quebec, second-largest city in the province after Montreal. It has a humid continental climate with warm summers coupled with cold and snowy winters. The Algonquian people had originally named the area , an Algonquin language, AlgonquinThe Algonquin language is a distinct language of the Algonquian languages, Algonquian language family, and is not a misspelling. word meaning "where the river narrows", because the Saint Lawrence River na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Louis De Rouvroy, Duc De Saint-Simon
Louis de Rouvroy, duc de Saint-Simon, GE (16 January 16752 March 1755), was a French soldier, diplomat, and memoirist. He was born in Paris at the Hôtel Selvois, 6 rue Taranne (demolished in 1876 to make way for the Boulevard Saint-Germain). The family's ducal peerage ('' duché-pairie''), granted in 1635 to his father Claude de Rouvroy (1608–1693), served as both perspective and theme in Saint-Simon's life and writings. He was the second and last Duke of Saint-Simon. His enormous memoirs are a classic of French literature, giving the fullest and most lively account of the court at Versailles of Louis XIV and the ''Régence'' at the start of Louis XV's reign. Peerage of France Men of the noblest blood (in Saint-Simon's view) might not be, and in most cases were not, peers in France. Derived at least traditionally and imaginatively from the ''douze pairs'' (twelve peers) of Charlemagne, the peerage of France was supposed to be, literally, the chosen of the ''noblesse'', d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perche
Perche () (French: ''le Perche'') is a former province of France, known historically for its forests and, for the past two centuries, for the Percheron draft horse breed. Until the French Revolution, Perche was bounded by four ancient territories of northwestern France: the provinces of Maine, Normandy, and Orléanais, and the region of Beauce. Afterwards it was absorbed into the present-day departments of Orne and Eure-et-Loir, with small parts in the neighboring departments of Eure, Loir-et-Cher, and Sarthe. Toponymy ''Perche'' is known by the following ancient Latin and French toponymic designations: ''saltus Particus'', ''silva Perticus'' before the 6th century, ''pagus quem Pert cnsem vocant'' and ''pagus pertensis'' in the 6th century, ''pagus Perticus'' no date and c. 815, ''Particus saltus'' in the 11th century, ''silva Perticus'' in 1045, '' ePerche'' in 1160 - 1174 and in 1308, ''Perche'' in1238, ''foresta de Pertico'' in1246,Nègre, Ernest (1990). ''Toponymie génér ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metasedimentary Rock
In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand an .... Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be used to identify the original sedimentary rock, even where they have been subject to high-grade metamorphism and intense deformation. Types of metasedimentary rocks See also * References Metamorphic petrology {{petrology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metavolcanic Rock
Metavolcanic rock is volcanic rock that shows signs of having experienced metamorphism. In other words, the rock was originally produced by a volcano, either as lava or tephra. The rock was then subjected to high pressure, high temperature or both, for example by burial under younger rocks, causing the original volcanic rock to recrystallization (geology), recrystallize. Metavolcanic rocks are sometimes described informally as ''metavolcanics''. When it is possible to determine the original volcanic rock type from the properties of the metavolcanic rock (particularly if the degree of metamorphism is slight), the rock is more precisely named by appylying the prefix ''meta-'' to the original rock type. For example, a weakly metamorphosed basalt would be described as a ''metabasalt'', or a weakly metamorphosed tuff as a ''metatuff''. Metavolcanic rock is commonly found in greenstone belts. See also * References {{petrology-stub Metamorphic rocks Volcanic rocks Metamorphic pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granitoid
A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites. As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms ''granite'' and ''granitic rock'' are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give a complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Felsic
In geology, felsic is a modifier describing igneous rocks that are relatively rich in elements that form feldspar and quartz.Marshak, Stephen, 2009, ''Essentials of Geology,'' W. W. Norton & Company, 3rd ed. It is contrasted with mafic rocks, which are relatively richer in magnesium and iron. Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. Felsic magma or lava is higher in viscosity than mafic magma/lava. Felsic rocks are usually light in color and have specific gravities less than 3. The most common felsic rock is granite. Common felsic minerals include quartz, muscovite, orthoclase, and the sodium-rich plagioclase feldspars (albite-rich). Terminology In modern usage, the term ''acid rock'', although sometimes used as a synonym, normally now refers specifically to a high-silica-content (greater than 63% SiO2 by weight) volcanic rock, such as rhyolite. Older, broader usage ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diatexite
Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian cratonic blocks. It consists of two or more constituents often layered repetitively: one layer is an older metamorphic rock that was reconstituted subsequently by partial melting ("paleosome"), while the alternate layer has a pegmatitic, aplitic, granitic or generally plutonic appearance ("neosome"). Commonly, migmatites occur below deformed metamorphic rocks that represent the base of eroded mountain chains. Migmatites form under extreme temperature and pressure conditions during prograde metamorphism, when partial melting occurs in metamorphic paleosome. Components exsolved by partial melting are called neosome (meaning ‘new body’), which may or may not be heterogeneous at the microscopic to macroscopic scale. Migmatites often appear as tightly, incoherently folded veins (ptygmatic folds).Recommendations by the IUGS Subcommission on the Systematics of Me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
