Cavendish, Newfoundland And Labrador
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Cavendish, Newfoundland And Labrador
Cavendish is a local service district and designated place in the Canadian province of Newfoundland and Labrador. Geography Cavendish is in Newfoundland within Subdivision E of Division No. 1. Cavendish is located on Route 80, off the Route 1 (Trans Canada Highway) exit at Whitbourne. It lies on an area of Cambrian Period shale, slate, and limestone; a significant limestone prospect lies about south of the settlement. Soils are mapped as stony loam podzols of the Cochrane and Turk's Cove series. Demographics As a designated place in the 2016 Census of Population conducted by Statistics Canada, Cavendish recorded a population of 301 living in 120 of its 138 total private dwellings, a change of from its 2011 population of 363. With a land area of , it had a population density of in 2016. Government Cavendish is a local service district (LSD) that is governed by a committee responsible for the provision of certain services to the community. The chair of the LSD ...
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Newfoundland And Labrador
Newfoundland and Labrador (; french: Terre-Neuve-et-Labrador; frequently abbreviated as NL) is the easternmost province of Canada, in the country's Atlantic region. The province comprises the island of Newfoundland and the continental region of Labrador, having a total size of 405,212 square kilometres (156,500 sq mi). In 2021, the population of Newfoundland and Labrador was estimated to be 521,758. The island of Newfoundland (and its smaller neighbouring islands) is home to around 94 per cent of the province's population, with more than half residing in the Avalon Peninsula. Labrador borders the province of Quebec, and the French overseas collectivity of Saint Pierre and Miquelon lies about 20 km west of the Burin Peninsula. According to the 2016 census, 97.0 per cent of residents reported English as their native language, making Newfoundland and Labrador Canada's most linguistically homogeneous province. A majority of the population is descended from English and Irish s ...
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ...
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List Of Local Service Districts In Newfoundland And Labrador
The Canadian province of Newfoundland and Labrador has 175 unincorporated communities that are designated as local service districts (LSDs) for the purpose of providing water, sewer, fire, garbage, street lighting, animal control, and/or road maintenance services to ratepayers within a defined area. The services in an LSD are overseen by a committee of five to seven elected officials and delivered by hired staff. The costs are recovered by the LSD committee through taxes levied upon residents and other benefitting parties in the defined area. The ''Local Service District Regulations'' of the province's ''Municipalities Act'' is the legislation that provides the authority to designate an LSD. Upon receiving a petition led by a permanent resident of a certain area that is signed by the majority of permanent residents of that area, the provincial minister responsible for the ''Municipalities Act'' may issue an order to incorporate an LSD for the area. The order assigns the official na ...
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List Of Designated Places In Newfoundland And Labrador
A designated place is a type of geographic unit used by Statistics Canada to disseminate census data. It is usually "a small community that does not meet the criteria used to define incorporated municipalities or Statistics Canada population centres (areas with a population of at least 1,000 and no fewer than 400 persons per square kilometre)." Provincial and territorial authorities collaborate with Statistics Canada in the creation of designated places so that data can be published for sub-areas within municipalities. Starting in 2016, Statistics Canada allowed the overlapping of designated places with population centres. In the 2021 Census of Population, Newfoundland and Labrador had 207 designated places, an increase from 199 in 2016. Among these designated places are 5 retired population centres. In 2021, the 207 designated places had a cumulative population of 44,012 and an average population of . Newfoundland and Labrador's largest designated place is Goulds with a popul ...
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List Of Communities In Newfoundland And Labrador
This article lists unincorporated communities of the province of Newfoundland and Labrador, Canada. Incorporated towns and cities are incorporated municipalities and can be found on List of municipalities in Newfoundland and Labrador. Newfoundland and Labrador at Confederation in 1949 had nearly 1,450 communities. Today it has fewer than 700. A listing of abandoned communities is found at the List of ghost towns in Newfoundland and Labrador. __NOTOC__ A * Aaron Arm, Burgeo (Newfoundland) * Allan's Island, Lamaline (Newfoundland) * Amherst Cove (Newfoundland) * Angels Cove (Newfoundland) * Angelbrook, Glovertown (Newfoundland) * Apsey Beach (Newfoundland) * Apsey Brook (Newfoundland) * Argentia, Placentia (Newfoundland) * Arnold's Cove Station (Newfoundland) * Aspen Cove (Newfoundland) B * Back Cove, Fogo (Newfoundland) *Back Harbour, Twillingate (Newfoundland) * Bacon Cove, Conception Harbour (Newfoundland) *Badger's Quay, New-Wes-Valley (Newfoundland) * Bailey's Co ...
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Canada 2016 Census
The 2016 Canadian census was an enumeration of Canadian residents, which counted a population of 35,151,728, a change from its 2011 population of 33,476,688. The census, conducted by Statistics Canada, was Canada's seventh quinquennial census. The official census day was May 10, 2016. Census web access codes began arriving in the mail on May 2, 2016. The 2016 census marked the reinstatement of the mandatory long-form census, which had been dropped in favour of the voluntary National Household Survey for the 2011 census. With a response rate of 98.4%, this census is said to be the best one ever recorded since the 1666 census of New France. This census was succeeded by Canada's 2021 census. Planning Consultation with census data users, clients, stakeholders and other interested parties closed in November 2012. Qualitative content testing, which involved soliciting feedback regarding the questionnaire and tests responses to its questions, was scheduled for the fall of 2013, ...
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Podzol
In soil science, podzols are the typical soils of coniferous or boreal forests and also the typical soils of eucalypt forests and heathlands in southern Australia. In Western Europe, podzols develop on heathland, which is often a construct of human interference through grazing and burning. In some British moorlands with podzolic soils, cambisols are preserved under Bronze Age barrows (Dimbleby, 1962). Term Podzol means "under-ash" and is derived from the Russian под (pod) + зола́ (zola); the full form is "подзо́листая по́чва" (podzolistaya pochva, "under-ashed soil"). The term was first given in middle of 1875 by Vasily Dokuchaev. It refers to the common experience of Russian peasants of plowing up an apparent under-layer of ash (leached or E horizon) during first plowing of a virgin soil of this type. Characteristics Podzols can occur on almost any parent material but generally derive from either quartz-rich sands and sandstone or sedimentary debri ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ...
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Whitbourne, Newfoundland And Labrador
Whitbourne is a town on the Avalon Peninsula in Newfoundland and Labrador, Canada in Division 1. History Whitbourne, Newfoundland's first inland town, is named after Sir Richard Whitbourne, one of the most colourful early settlers of Newfoundland and Labrador who wrote a book about Newfoundland that was published in 1620. Sir Richard was appointed by the High Court of the Admiralty to set up the first English law court in the New World in 1615 in Trinity. He was kidnapped and held by the notorious Pirate Peter Easton in Harbour Grace. He also described a mermaid that he saw in St. John's harbour. Later, he became governor of Renews on the Southern Shore. Whitbourne, unlike most communities on the Island of Newfoundland is inland. It was founded in about 1880 during the construction of the Newfoundland Railway. The railway continued to be an important employer in the Town until its abandonment in 1988, although its economic significance declined gradually throughout the twe ...
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