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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 Mount Jacques-Cartier (french: Mont Jacques-Cartier) is a mountain in the Chic-Choc Mountains range in eastern Quebec, Canada. At , it is the tallest mountain in souther ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Jacques-Cartier
Mount Jacques-Cartier (french: Mont Jacques-Cartier) is a mountain in the Chic-Choc Mountains range in eastern Quebec, Canada. At , it is the tallest mountain in southern Quebec, and the highest mountain in the Canadian Appalachians. Located in the Gaspé Peninsula, the mountain is protected within a Quebec provincial park called Gaspésie National Park, and is host to the last remaining population of reindeer, woodland caribou south of the Saint Lawrence River. The summit can be accessed by a hiking trail. References Landforms of Gaspésie–Îles-de-la-Madeleine, Mont Jacques One-thousanders of Quebec Notre Dame Mountains {{Quebec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Logan (Quebec)
Mount Logan is a mountain on the Gaspé Peninsula, in Quebec, Canada. Part of the Chic-Choc Mountains, Mount Logan rises above sea level, making it the highest point in the Bas-Saint-Laurent region and one of the few Quebec peaks over . The mountain's unusually steep northern flank is visible from Cap-Chat, Quebec, Cap-Chat, on the estuary of Saint Lawrence. The altitude and the summit's exposure to winds from the Gulf of St. Lawrence make it one of Quebec's most precipitated summits. The combination of the mountain's physiography and unusual climate make it the habitat of several rare animal and plant species, such as caribou and Arnica griscomii, griscom arnica. Mount Logan's topography, ancient geological composition, and remarkable flora and fauna aroused the scientific community's interest in the mid-19th century. Despite conditions favorable for mountain skiing, skiing, Mount Logan's remoteness has worked against efforts to develop recreational and tourist enterprises. Str ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Quebec
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Quebec
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mont Jacques-Cartier
Mount Jacques-Cartier (french: Mont Jacques-Cartier) is a mountain in the Chic-Choc Mountains range in eastern Quebec, Canada. At , it is the tallest mountain in southern Quebec, and the highest mountain in the Canadian Appalachians. Located in the Gaspé Peninsula, the mountain is protected within a Quebec provincial park called Gaspésie National Park, and is host to the last remaining population of woodland caribou south of the Saint Lawrence River The St. Lawrence River (french: Fleuve Saint-Laurent, ) is a large river in the middle latitudes of North America. Its headwaters begin flowing from Lake Ontario in a (roughly) northeasterly direction, into the Gulf of St. Lawrence, connectin .... The summit can be accessed by a hiking trail. References Mont Jacques One-thousanders of Quebec Notre Dame Mountains {{Quebec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mont Xalibu
Mount Xalibu is a mountain located in the unorganized territory of Mont-Albert, in Quebec. Culminating at above sea level, it is one of the highest peaks in the Notre Dame Mountains. It is located in Gaspésie National Park. Toponymy The mountain, without official designation until 2 February 1989, was given the Mi'gmaq name of an animal that inhabits its flanks, the woodland caribou. Geography Situation Mount Xalibu is located in eastern Canada, in the province of Quebec, on the northern flank of the Gaspé Peninsula. It is southeast of the town of Sainte-Anne-des-Monts, capital of La Haute-Gaspésie Regional County Municipality, and northeast of Quebec, provincial capital. The summit rises to of altitude in the McGerrigle Mountains, within the Chic-Choc Mountains of the Notre-Dame range. Topography Mount Xalibu is part of the McGerrigle Mountains, formerly called ''Tabletop'' (“table top”) because of their constitution in plateaus which surmount steep rock fac ... [...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] |
International Appalachian Trail
The International Appalachian Trail (IAT; french: Sentier international des Appalaches, SIA) was originally a hiking trail which ran from Katahdin Woods and Waters National Monument, in Maine, through New Brunswick, to the Gaspé Peninsula of Quebec, after which it followed a ferry route to Newfoundland, and then continued to the northern-easternmost point of the Appalachian Mountains at Belle Isle, Newfoundland and Labrador. As of July 2020, there are widely geographically dispersed IAT-branded walking trails in Greenland, Iceland, Norway, Sweden, Denmark, Scotland, Northern Ireland, Ireland, Isle of Man, Wales, England, Spain, Portugal, and Morocco. History The IAT was proposed in 1994 by Richard Anderson, a Maine fisheries biologist, with plans to traverse the portions of the Appalachian Mountains in Maine, New Brunswick, and Quebec that the Appalachian Trail did not cover. Following route selection, construction of the trail took place through the late 1990s. The first pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mont Albert, Quebec
Mont Albert ( en, Mount Albert) is a mountain in the Chic-Choc range in the Gaspésie National Park in the Gaspé Peninsula of eastern Quebec, Canada. At , it is one of the highest mountains in southern Quebec, and is popular for hiking. Mount Albert was named in honour of Prince Albert of Saxe-Coburg and Gotha, husband of Queen Victoria, because geologist Alexander Murray made the first recorded ascent of the mountain on the Prince's birthday, 26 Aug. 1845. Geography The summit of Mount Albert is a plateau across called ''La Table à Moïse'', or Moses's Table. It includes two summits, Albert North () and Albert South (). Each of the summits is situated at either side of the plateau. The principal component of Mont Albert is an unusual kind of bedrock called serpentine; this originated as oceanic crust and was then uplifted during the formation of the Appalachian Mountains about 480 million years ago. The nearly flat serpentine tableland on the mountain's summit is an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
