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Hart Jaune River
The Hart Jaune River (french: Rivière Hart Jaune) is a river in Quebec, Canada. It flows from the Petit lac Manicouagan to the Manicouagan Reservoir. Location The Hart Jaune River is in the unorganized territory of Rivière-Mouchalagane in the Caniapiscau Regional County Municipality. It forms the outlet of the Petit lac Manicouagan at the Hart-Jaune Dam, which feeds the 45.5 MW Hart-Jaune generating station. The river flows southwest to the Manicouagan Reservoir. It is about long, and has a vertical drop of . The sources of the water are in the Uapishka Biodiversity Reserve, which also feeds the Toulnustouc and Manicouagan rivers. The Hart Jaune is one of the major inlets to the Manicouagan Reservoir, along with the Mouchalagane, Seignelay, Themines and Petite Riviere Manicouagan. The reservoir is drained by the Manicouagan River. Quebec Route 389 from Baie-Comeau to Labrador City crosses the river at Km 375 over a small wooden one-way bridge. In February 2017 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebec Route 389
Quebec's Route 389 connects Route 138 adjacent to Baie-Comeau with the Newfoundland and Labrador border, connecting with the Trans-Labrador Highway (Newfoundland and Labrador provincial route 500) to Wabush and Labrador City, and beyond to Goose Bay. On its way it skirts the eastern shore of Manicouagan Reservoir. Route description The Québec North Shore Company and Hydro-Québec completed portions from Route 389 to the Manic 5 hydroelectric project site (km 213), now known as the Daniel-Johnson Dam. From km 213, the highway follows a path traditionally used by aboriginal people and explorers, with access to the Hart Jaune Hydroelectric Complex at km 390. The town of Gagnon, now torn down, was at km 394. From km 317 (gas station and restaurant), the highway is now paved all the way to km 495. Starting at km 495, the "Fire Lake Mine Road" section was built by unemployed workers during a labour dispute, influenced by the presence of the railway owned by the Québec Cartier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petite Riviere Manicouagan
Vincent Aycocho, or better known as Petite is a Filipino actor, comedian, singer and TV show host. He is known for as a Filipino comedian in ''Comedy Bar (Philippine TV series), Comedy Bar'', Punch line and Clowns, together with their other celebrities; Boobay, Iyah, Donita Nose, Ate Gay, Allan K. and Wally Bayola. Petite had more projects on GMA Network, such as hosting ''CelebriTV'', which was co-hosted with Joey de Leon. Career After in comedy bar Petite has a numerous shows in GMA Network; Petite signed a contract on GMA Network in 2014 as an actor and comedian, Petite guesting in ''CelebriTV'', and joining the Bulaga Pa More! in ''Eat Bulaga!'' as a performer, Sunday PinaSaya guesting in ''Kalyeserye'' as a applicant role and in ''Vampire ang Daddy Ko'' as special guest. ;''Comedy Bar'' Petite is a singer and performer in a Philippine TV comedian series ''Comedy Bar (Philippine TV series), Comedy Bar'', hosting Boobay, Fabio Ide and others, he is a best notable work in ''C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allochthon
upright=1.6, Schematic overview of a thrust system. The hanging wall block is (when it has reasonable proportions) called a nappe. If an erosional hole is created in the nappe that is called a window (geology)">window. A klippe is a solitary outcrop of the nappe in the middle of autochthonous material. An allochthon, or an allochthonous block, is a large block of rock which has been moved from its original site of formation, usually by low angle thrust faulting. An allochthon which is isolated from the rock that pushed it into position is called a klippe. If an allochthon has a "hole" in it so that one can view the autochthon (geology), autochthon beneath the allochthon, the hole is called a "window" (or Fenster). Etymology: Greek; 'allo' = other, and 'chthon' = earth. In generalized terms, the term is applied to any geologic units that originated at a distance from their present location For comparison, see also Autochthon. In the United States there are three notable al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anorthosite
Anorthosite () is a phaneritic, intrusive igneous rock characterized by its composition: mostly plagioclase feldspar (90–100%), with a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minerals most commonly present. Anorthosites are of enormous geologic interest, because it is still not fully understood how they form. Most models involve separating plagioclase crystals based on their density. Plagioclase crystals are usually less dense than magma; so, as plagioclase crystallizes in a magma chamber, the plagioclase crystals float to the top, concentrating there. Anorthosite on Earth can be divided into five types: # Archean-age anorthosites # Proterozoic anorthosite (also known as massif or massif-type anorthosite) – the most abundant type of anorthosite on Earth # Layers within Layered Intrusions (e.g., Bushveld and Stillwater intrusions) # Mid-ocean ridge and transform fault anorthosites # Anorthosite xenoliths in other rocks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grenville Orogeny
The Grenville orogeny was a long-lived Mesoproterozoic mountain-building event associated with the assembly of the supercontinent Rodinia. Its record is a prominent orogenic belt which spans a significant portion of the North American continent, from Labrador to Mexico, as well as to Scotland. Grenville orogenic crust of mid-late Mesoproterozoic age (c. 1250–980 Ma) is found worldwide, but generally only events which occurred on the southern and eastern margins of Laurentia are recognized under the "Grenville" name. These orogenic events are also known as the Kibaran orogeny in Africa and the Dalslandian orogeny in Western Europe. Timescale The problem of timing the Grenville orogeny is an area of some contention today. The timescale outlined by Toby Rivers in 2008 is derived from the well-preserved Grenville Province and represents one of the most detailed records of the orogeny. This classification considers the classical Grenville designation to cover two separate oro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alnus Incana
''Alnus incana'', the grey alder or speckled alder, is a species of multi-stemmed, shrubby tree in the birch family, with a wide range across the cooler parts of the Northern Hemisphere. Tolerant of wetter soils, it can slowly spread with runners and is a common sight in swamps and wetlands. It is easily distinguished by its small cones, speckled bark and broad leaves. Description It is a small- to medium-sized tree tall with smooth grey bark even in old age, its life span being a maximum of 60 to 100 years. The leaves are matte green, ovoid, long and broad. The flowers are catkins, appearing early in spring before the leaves emerge, the male catkins pendulous and long, the female catkins long and one cm broad when mature in late autumn. The seeds are small, long, and light brown with a narrow encircling wing. The grey alder has a shallow root system, and is marked not only by vigorous production of stump suckers, but also by root suckers, especially in the northern par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Innu
The Innu / Ilnu ("man", "person") or Innut / Innuat / Ilnuatsh ("people"), formerly called Montagnais from the French colonial period ( French for "mountain people", English pronunciation: ), are the Indigenous inhabitants of territory in the northeastern portion of the present-day province of Labrador and some portions of Quebec. They refer to their traditional homeland as ''Nitassinan'' ("Our Land", ᓂᑕᔅᓯᓇᓐ) or ''Innu-assi'' ("Innu Land"). The Innu are divided into several bands, with the Montagnais being the southernmost group and the Naskapi being the northernmost. Their ancestors were known to have lived on these lands as hunter-gatherers for several thousand years. To support their seasonal hunting migrations, they created portable tents made of animal skins. Their subsistence activities were historically centred on hunting and trapping caribou, moose, deer, and small game. Their language, Ilnu-Aimun or Innu-Aimun (popularly known since the French colonia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labrador City
Labrador City is a town in western Labrador (part of the Canadian province of Newfoundland and Labrador), near the Quebec border. With a population of 7,412 as of 2021, it is the second-largest population centre in Labrador, behind Happy Valley-Goose Bay. Neighbouring Labrador City is Wabush, a smaller town with a population of approximately 1,964 as of 2021. Together, the "twin towns" are known as Labrador West. In the 1960s, Labrador City was founded to accommodate employees of the Iron Ore Company of Canada, and iron ore mining continues to be the primary industry in the town. The Labrador City town motto is ''Kamistiatusset'', a Naskapi word meaning "land of the hard-working people." The Labrador City town crest is that of a snowy owl holding a scroll atop a black spade on a mound of red earth. The symbol represents iron ore mining. The spade is flanked by two caribou. Both snowy owls and caribou are native to the Labrador City area. Government Belinda Adams was appointed as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baie-Comeau
Baie-Comeau (; 2021 city population 20,687; CA population 26,643) is a city located approximately north-east of Quebec City in the Côte-Nord region of the province of Quebec, Canada. It is located on the shores of the Saint Lawrence River near the mouth of the Manicouagan River, and is the seat of Manicouagan Regional County Municipality. There are two urban area population centres within the city limits: Baie-Comeau proper, with a population of 9,100, and Hauterive, with a population of 11,147, as of the 2021 Canadian Census. The city is named after the adjacent Comeau Bay, which is named in honour of Napoléon-Alexandre Comeau, a Québécois naturalist. Baie-Comeau is the birthplace of former Prime Minister of Canada Brian Mulroney. History The oldest part of Baie-Comeau is the area known as ''Vieux-Poste'' (Old Post) near the mouth of the Amédée River where in 1889, the Saint-Eugène-de-Manicouagan Mission was founded by Eudists. In 1898, the first sawmill in the Côt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_Labrador.jpg "Click for more on -> Anorthosite")
