Mount Jacques-Cartier
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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 ...
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List Of The Most Isolated Major Summits Of North America
The following sortable table comprises the 230 mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland ( Kalaallit Nunaat), the islands of Canada, and the islands of Alaska. The Hawaiian Islands are not included because they are considered part of Oceania. with at least of topographic isolation and at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence. ...
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List Of Most Isolated Mountain Peaks Of Canada
The following sortable table comprises the 150 most topographically isolated mountain peaks of Canada with at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence. An ultra-prominent summit is a summit with at least of topographic prominence. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.If the elevation or prominence of a summit is calculated as a range of values, the arithmetic mean is shown. #The topographic prominence of a summit is a measure of how high the summit rises above its surroundings.The topographic prominence of a summit is the topographic elevation difference between the summit and its highest or key c ...
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Quebec 1000 Meter Peaks
This list of Quebec's 1000-meter peaks is a list of the highest summits in Quebec, used in the mountaineering sport of peak bagging. Ranked peaks have of clean prominence. (Includes map of peaks.) See also * Northeast 111 4000-footers ** New England Four-thousand footers ** Adirondack Forty-sixers * New England Fifty Finest References {{reflist Lists of mountains by prominence Lists of mountains by isolation Quebec Quebec * Peaks Peak or The Peak may refer to: Basic meanings Geology * Mountain peak ** Pyramidal peak, a mountaintop that has been sculpted by erosion to form a point Mathematics * Peak hour or rush hour, in traffic congestion * Peak (geometry), an (''n''-3)-d ...
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Mont-Albert, Quebec
Mont-Albert is an unorganized territory in the Gaspésie–Îles-de-la-Madeleine region of Quebec, Canada. The only population centre within the territory is Cap-Seize, located south of Sainte-Anne-des-Monts along Quebec Route 299. It was established circa 1940 as a forestry centre and named after the nearby Cap-Seize Creek, a tributary of the Sainte-Anne River. While the name literally means "Cape Sixteen", it is actually a transformation of the English word "capsize", the creek's original name. A post office operated there from 1946 to 1969. The ghost town of Saint-Octave-de-l'Avenir is about south-southeast of Cap-Chat, at an altitude of . It was formed in 1932 as part of the Vautrin Settlement Plan to encourage colonization of Gaspésie's interior and intended to bring relief during the Great Depression of the 1930s. The settlement was named after founding priest Louis-Octave Caron (1879–1942) and a hopeful outlook of the future (''avenir'' is French for "future"). It gr ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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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 ...
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National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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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, Quebec b ...
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Canadian Appalachians
The Appalachian Mountains, often called the Appalachians, (french: Appalaches), are a system of mountains in eastern to northeastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period. They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. The Appalachian chain is a barrier to east–west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the ''Appalachian Highlands'' physiographic division as consisting of 13 provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, St. Lawrence Valley, Appala ...
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Gaspé Peninsula
The Gaspé Peninsula, also known as Gaspesia (; ), is a peninsula along the south shore of the Saint Lawrence River that extends from the Matapedia Valley in Quebec, Canada, into the Gulf of Saint Lawrence. It is separated from New Brunswick on its southern side by Chaleur Bay and the Restigouche River. The name ''Gaspé'' comes from the Miꞌkmaq word , meaning "end", referring to the end of the land. The Gaspé Peninsula is slightly larger than Belgium, at . The population is 140,599 as of the 2011 census.The population of the Gaspe Peninsula is determined by adding the population of two federal electoral districts, Haute-Gaspésie—La Mitis—Matane—Matapédia and Gaspésie—Îles-de-la-Madeleine, while subtracting that of the Magdalen Islands. It is also noted as being the only region outside the Channel Islands to contain native speakers of Jersey Norman. Geography Sea cliffs dominate the peninsula's northern shore along the St. Lawrence River. Cap Gaspé, jutt ...
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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 ...
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