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Saguenay Fjord National Park
Saguenay Fjord National Park (french: parc national du Fjord-du-Saguenay) is a provincial park located in Quebec, Canada. In the regions of Saguenay–Lac-Saint-Jean, Charlevoix, Côte-Nord, and Bas-Saint-Laurent, the park is situated along the eastern end of the Saguenay River and adjoins the Saguenay–St. Lawrence Marine Park for over 100 km (60 mi.). The park, originally named Saguenay National Park, was renamed on April 20, 2011.Le parc national du Saguenay devient le parc national du Fjord-du-Saguenay Ministère du Développement durable, de l’Environnement et des Parcs. Retrieved 11 May 2012. History Aborig ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebec
Quebec ( ; )According to the Canadian government, ''Québec'' (with the acute accent) is the official name in Canadian French and ''Quebec'' (without the accent) is the province's official name in Canadian English is one of the thirteen provinces and territories of Canada. It is the largest province by area and the second-largest by population. Much of the population lives in urban areas along the St. Lawrence River, between the most populous city, Montreal, and the provincial capital, Quebec City. Quebec is the home of the Québécois nation. Located in Central Canada, the province shares land borders with Ontario to the west, Newfoundland and Labrador to the northeast, New Brunswick to the southeast, and a coastal border with Nunavut; in the south it borders Maine, New Hampshire, Vermont, and New York in the United States. Between 1534 and 1763, Quebec was called ''Canada'' and was the most developed colony in New France. Following the Seven Years' War, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cévennes National Park
Cévennes National Park (french: Parc national des Cévennes) is a French national park located in Southern France, in the mountainous area of Cévennes. Created in 1970, the park has its administrative seat in Florac at Florac Castle. It is located mainly in the departments of Lozère and Gard; it also covers some parts of Ardèche and Aveyron, therefore stretching across a record number of departments for a national park. The Aven Armand cave is located in the park. In 2011, the Park was made a part of The Causses and the Cévennes, Mediterranean agro-pastoral Cultural Landscape UNESCO World Heritage Site. Geography frameless, Map of the Cévennes National Park, showing in red the central protected zone and, in green, the area encompassed by the park., 400px The park includes several mountains and plateaus, including: Mont Lozère, Mont Aigoual, Causse Méjean, France. Mont Lozère is the highest peak in the area, reaching 1,699 metres. History The Cévennes country ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurentian Mountains
The Laurentian Mountains (French: ''Laurentides'') are a mountain range in southern Quebec, Canada, north of the St. Lawrence River and Ottawa River, rising to a highest point of at Mont Raoul Blanchard, northeast of Quebec City in the Laurentides Wildlife Reserve. The Gatineau, L'Assomption, Lièvre, Montmorency, Nord and St. Maurice rivers rise in lakes in this mountain range. Background Although Laurentides is one of Quebec's official regions, the mountain range of the same name runs through six other regions: Capitale-Nationale, Outaouais, Lanaudière, Mauricie, Saguenay-Lac-Saint-Jean and Côte-Nord. Extending into central Ontario, the foothills of the Laurentian range are known as the Opeongo Hills, or the Madawaska Highlands. The Laurentian Mountain range is one of the oldest mountain ranges in the world. It contains rocks deposited before the Cambrian Period 540 million years ago. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fos ... [...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] |
Sand Dunes
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called '' ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tadoussac, Quebec
Tadoussac () is a village in Quebec, Canada, at the confluence of the Saguenay and Saint Lawrence rivers. The indigenous Innu call the place ''Totouskak'' (plural for ''totouswk'' or ''totochak'') meaning "bosom", probably in reference to the two round and sandy hills located on the west side of the village. According to other interpretations, it could also mean "place of lobsters", or "place where the ice is broken" (from the Innu ''shashuko''). Although located in Innu territory, the post was also frequented by the Mi'kmaq people in the second half of the 16th century, who called it ''Gtatosag'' ("among the rocks"). Alternate spellings of Tadoussac over the centuries included Tadousac (17th and 18th centuries), Tadoussak, and Thadoyzeau (1550). Tadoussac was first visited by Europeans in 1535 and was established in 1599 when the first trading post in Canada was formed there, in addition to a permanent settlement being placed in the same area that the Grand Hotel is located toda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beluga Whales
The beluga whale () (''Delphinapterus leucas'') is an Arctic and sub-Arctic cetacean. It is one of two members of the family Monodontidae, along with the narwhal, and the only member of the genus ''Delphinapterus''. It is also known as the white whale, as it is the only cetacean to regularly occur with this colour; the sea canary, due to its high-pitched calls; and the melonhead, though that more commonly refers to the melon-headed whale, which is an oceanic dolphin. The beluga is adapted to life in the Arctic, with anatomical and physiological characteristics that differentiate it from other cetaceans. Amongst these are its all-white colour and the absence of a dorsal fin, which allows it to swim under ice with ease. It possesses a distinctive protuberance at the front of its head which houses an echolocation organ called the melon, which in this species is large and deformable. The beluga's body size is between that of a dolphin and a true whale, with males growing up to l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
