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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, jut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Canada
The list of regions of Canada is a summary of geographical areas on a hierarchy that ranges from national (groups of provinces and territories) at the top to local regions and sub-regions of provinces at the bottom. Administrative regions that rank below a province and above a municipality are also included if they have a comprehensive range of functions compared to the limited functions of specialized government agencies. Some provinces and groups of provinces are also quasi-administrative regions at the federal level for purposes such as representation in the Senate of Canada. However regional municipalities (or regional districts in British Columbia) are included with local municipalities in the article List of municipalities in Canada. National regions The provinces and territories are sometimes grouped into regions, listed here from west to east by province, followed by the three territories. Seats in the Senate are equally divided among four regions: the West, Ontario, Que ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jèrriais
(french: Jersiais, also known as the Jersey Language, Jersey French and Jersey Norman French in English) is a Romance language and the traditional language of the Jersey people. It is a form of the Norman language spoken in Jersey, an island in the Channel Islands archipelago off the coast of France. Its closest relatives are the other Norman languages, such as , spoken in neighbouring Guernsey, and the other . Use of has been in decline over the past century, as English has increasingly become the language of education, commerce and administration on Jersey. There are very few people who speak as a mother tongue and, owing to the age of the remaining speakers, their numbers decrease annually. Despite this, efforts are being made to keep the language alive. The language of Sark, Sercquiais, is a descendant of the brought by the Jersey colonists who settled Sark in the 16th century, with mutual intelligibility with the Norman language of mainland Normandy. is often calle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Côte-Nord
Côte-Nord (, ; ; land area ) is the second-largest administrative region by land area in Quebec, Canada, after Nord-du-Québec. It covers much of the northern shore of the Saint Lawrence River estuary and the Gulf of Saint Lawrence past Tadoussac. While most of the region is in the same time zone as the rest of Quebec, the far eastern portion east of the 63rd meridian, excluding the Minganie Regional County Municipality, is officially in the Atlantic Time Zone and does not observe daylight saving time. Population At the 2016 Canadian Census, the population amounted to 92,518, approximately 1.1% of the province's population, spread across 33 municipalities, various Indian reserves and a Naskapi reserved land. The towns of Baie-Comeau and Sept-Îles combined amount to a little more than half of the population of the region. Geography and economy Côte-Nord was created as an administrative region in 1966. Important landmarks of Côte-Nord include Anticosti Island, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flora
Flora is all the plant life present in a particular region or time, generally the naturally occurring (indigenous (ecology), indigenous) native plant, native plants. Sometimes bacteria and fungi are also referred to as flora, as in the terms ''gut flora'' or ''skin flora''. Etymology The word "flora" comes from the Latin name of Flora (mythology), Flora, the goddess of plants, flowers, and fertility in Roman mythology. The technical term "flora" is then derived from a metonymy of this goddess at the end of the sixteenth century. It was first used in poetry to denote the natural vegetation of an area, but soon also assumed the meaning of a work cataloguing such vegetation. Moreover, "Flora" was used to refer to the flowers of an artificial garden in the seventeenth century. The distinction between vegetation (the general appearance of a community) and flora (the taxonomic composition of a community) was first made by Jules Thurmann (1849). Prior to this, the two terms were used ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serpentine Group
Serpentine subgroup (part of the kaolinite-serpentine group in the category of phyllosilicates) are greenish, brownish, or spotted minerals commonly found in serpentinite. They are used as a source of magnesium and asbestos, and as decorative stone. The name comes from the greenish colour and smooth or scaly appearance from the Latin , meaning "serpent rock". Serpentine subgroup is a set of common rock-forming hydrous magnesium iron Silicate minerals#Phyllosilicates, phyllosilicate () minerals, resulting from the metamorphism of the minerals that are contained in mafic to ultramafic rocks. They may contain minor amounts of other elements including chromium, manganese, cobalt or nickel. In mineralogy and gemology, serpentine may refer to any of the 20 varieties belonging to the serpentine subgroup. Owing to admixture, these varieties are not always easy to individualize, and distinctions are not usually made. There are three important mineral polymorphism (materials science), po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tree Line
The tree line is the edge of the habitat at which trees are capable of growing. It is found at high elevations and high latitudes. Beyond the tree line, trees cannot tolerate the environmental conditions (usually cold temperatures, extreme snowpack, or associated lack of available moisture). The tree line is sometimes distinguished from a lower timberline, which is the line below which trees form a forest with a closed canopy. At the tree line, tree growth is often sparse, stunted, and deformed by wind and cold. This is sometimes known as '' krummholz'' (German for "crooked wood"). The tree line often appears well-defined, but it can be a more gradual transition. Trees grow shorter and often at lower densities as they approach the tree line, above which they are unable to grow at all. Given a certain latitude, the tree line is approximately 300 to 1000 meters below the permanent snow line and roughly parallel to it. Causes Due to their vertical structure, trees are more sus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Tundra
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as '' Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Por ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount 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] |
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] |
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] |
Appalachian Mountains
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, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering (subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
