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Notre Dame Mountains
The Notre Dame Mountains are a portion of the Appalachian Mountains, extending from the Gaspé Peninsula of Quebec to the Green Mountains of Vermont. The range runs from northeast to southwest, forming the southern edge of the St. Lawrence River valley, and following the Canada–United States border between Quebec and Maine. The mountainous New Brunswick "panhandle" is located in the Notre Dame range as well as the uppermost reaches of the Connecticut River valley in New Hampshire. As the mountains are geologically old, they have eroded to an average height of around . Etymology ''Notre Dame'' is French for "Our Lady," a Catholic term referring to the Virgin Mary. While on an expedition on 15 August 1535, Jacques Cartier wrote: The ''jour Notre Dame d'aoust XVe'' refers to the feast of the Assumption of Mary, commemorated in the Catholic Church on 15 August. The following autumn, maps he authored carried the name "''haultes montaignes de Honguedo."'' However, it was the tit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chic-Choc Mountains
The Chic-Choc Mountains, also spelled Shick Shocks, is a mountain range in the central region of the Gaspe Peninsula in Quebec, Canada. It is a part of the Notre Dame Mountains, which is a continuation of the Appalachian Mountains. History The name ''Chic-Chocs'' comes from the Mi'kmaq word ''sigsôg'', meaning "crags" or "rocky mountains." It has undergone many different spellings over time, including Chikchâks (1836), Shick-shock (1857), and Chick-Saws (1863). Geography The Chic-Chocs run parallel to the St. Lawrence River and are located some 20 to 40 kilometers inland. They are a narrow band of mountains approximately long and wide. The Chic-Chocs are heavily eroded, with rounded, flattened tops and steep sides. Over 32 mountains in the range have peaks higher than ; the highest is Mount Jacques-Cartier at . Caribou can be found in the plateaus of this region. Tourism Although visited by just a few tourists, Chic-Choc Mountains became much more popular in the late 1990s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jean Alfonse
Jean Fonteneau, dit Alfonse de Saintonge (also spelled Jean Allefonsce) or João Afonso in Portuguese (also spelled João Alfonso) (, Portugal – December 1544 or 1549, off La Rochelle) was a Portuguese navigator, explorer and corsair, prominent in the European age of discovery. He had an early career in Portugal and later served the King of France. Early years and personal life Born João Afonso and later known in France as Jean Fonteneau or Alfonse of Saintonge, he married a woman named Valentine Alfonse (Valentina Alfonso). Taking to the sea at age 12, he joined the Portuguese India Armadas and the Portuguese commercial fleets as they sailed past the seven seas to the coasts of Brasil, Western Africa, and around the Cape to Madagascar and Asia. His writings talk of days lasting three months, and of a vast southern continent, the Terra Australis, and the Jave la Grande, which he claims to have seen south of Southeast Asia, possibly suggesting he had approached the Arctic ... [...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] |
Lake Témiscouata National Park
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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