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Cutthorpe
Brampton is a civil parish in North East Derbyshire, England, with a population of 1,201 in 2011. Lying north west of London, north of Derby, and west of the market town of Chesterfield, Brampton encompasses part of the Peak District national park to the west, and shares a border with the Borough of Chesterfield, Barlow, Baslow and Bubnell, Beeley, and Holymoorside and Walton. The parish does not include the nearby built-up suburb of Brampton which is now within the Chesterfield unparished area. Geography Location Brampton is surrounded by the following local places: * Barlow, Moorhall and Wilday Green to the north * Holymoorside, Nether Loads and Upper Loads to the south * Chesterfield to the east * Baslow, Chatsworth and Robin Hood to the west. It is in area, in height and in width, spanning across all the western edge of the North East Derbyshire district, fitting between Chesterfield and the Derbyshire Dales districts. The parish lies in the north west of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brampton, Derbyshire
Brampton is a suburb in the west of Chesterfield, Derbyshire. Originally a village known as New Brampton and separate from the town, it became absorbed into it over time due to urban sprawl. It is centred on Chatsworth Road, the main arterial road (A619) that connects the town with the Peak District and Manchester. History The suburb has a historical association with the civil parish of Brampton in North East Derbyshire district, which is still outside the town. The civil parish includes the villages of Old Brampton (from which the suburb derives its name), Wadshelf and Cutthorpe which is a small village about north-west of Chesterfield with a village school, a butcher's shop and a small post office/grocery store, three public houses and two historic halls; the main road straggles through the village for three miles, reaching the Grange at its highest point, with commanding views all around. The suburb of Brampton until the late 19th century was a part of the ancient Bramp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holymoorside And Walton
Holymoorside and Walton is a civil parish within the North East Derbyshire district, which is in the county of Derbyshire, England. Named for its main settlements, with a mix of a number of villages and hamlets amongst a large rural area, it had a population of 2,223 residents in 2011. The parish is north west of London, north of the county city of Derby, and south west of the nearest market town of Chesterfield. It is adjacent with the Peak District national park to the west, and shares a border with the district of Chesterfield, along with the parishes of Ashover, Beeley, Brampton as well as Wingerworth. The parish paradoxically does not include the majority of the nearby built-up suburb of Walton, Chesterfield which is now within an adjacent unparished area of the borough. Geography Location Holymoorside and Walton is surrounded by the following local locations: * Chesterfield, Old Brampton and Wadshelf to the north * Alicehead, Harper Hill, Spitewinter and Upper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chesterfield, Derbyshire
Chesterfield is a market town and unparished area in the Borough of Chesterfield, Derbyshire, England, north of Derby and south of Sheffield at the confluence of the River Rother and River Hipper. In 2011 the built-up-area subdivision had a population of 88,483, making it the second-largest settlement in Derbyshire, after Derby. The wider borough had a population of 103,801 in 2011. In 2011, the town had a population of 76,753. It has been traced to a transitory Roman fort of the 1st century CE. The name of the later Anglo-Saxon village comes from the Old English ''ceaster'' (Roman fort) and ''feld'' (pasture). It has a sizeable street market three days a week. The town sits on an old coalfield, but little visual evidence of mining remains. The main landmark is the crooked spire of the Church of St Mary and All Saints. History Chesterfield was in the Hundred of Scarsdale. The town received its market charter in 1204 from King John, which constituted the town as a free boro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North East Derbyshire (UK Parliament Constituency)
North East Derbyshire is a constituency created in 1885 represented in the House of Commons of the UK Parliament since 2017 by Lee Rowley of the Conservative Party. This was the first time a Conservative candidate had been elected since 1935. The seat had been, relative to others, a marginal seat from 2005 to 2019 as its winner's majority had not exceeded 5.7% of the vote since the 23.2% majority won in that year. The seat has changed hands once since that year and is no longer marginal after the 26% majority won in 2019. History ;Summary of results The seat was created in the Redistribution of Seats Act 1885. Until 1910, the area was regularly represented by a Liberal MP. From the 1935 to the 2015 elections inclusive N.E. Derbyshire returned Labour candidates in succession. In 2010 and 2015 the results featured marginal majorities (a majority of relatively few percentage points between the winner's and the runner-up's tallies). The runner-up candidate from 1945 to 2015 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Derbyshire Moors
The Derbyshire moors are moorlands in the English county of Derbyshire, and form the southern part of the Peak District. They include: * Beeley Moor () * East Moor () * Brampton East Moor * Gibbet Moor () * Harewood Moor () References External links Morning on the Derbyshire Moors- a 1920 painting by Stanley Royle Stanley Royle RBA, (1888–1961) was an English post-impressionist landscape painter and illustrator who lived for most of his life in and around Sheffield (England), and in Canada, and was inspired by views of landscape, sea and snow. Early ... Geography of Derbyshire Peak District Moorlands of England {{Derbyshire-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bogland
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A baygall is another type of bog found in the forest of the Gulf Coast states in the United States.Watson, Geraldine Ellis (2000) ''Big Thicket Plant Ecology: An Introduction'', Third Edition (Temple Big Thicket Series #5). University of North Texas Press. Denton, Texas. 152 pp. Texas Parks and Wildlife. Ecological Mapping systems of Texas: West Gulf Coastal Plain Seepage Swamp and Baygall'. Retrieved 7 July 2020 They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink. Bogs occur where the water at the ground surface is acidic and low in nutrients. In contrast to fens, they derive most of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heath
A heath () is a shrubland habitat found mainly on free-draining infertile, acidic soils and characterised by open, low-growing woody vegetation. Moorland is generally related to high-ground heaths with—especially in Great Britain—a cooler and damper climate. Heaths are widespread worldwide but are fast disappearing and considered a rare habitat in Europe. They form extensive and highly diverse communities across Australia in humid and sub-humid areas where fire regimes with recurring burning are required for the maintenance of the heathlands.Specht, R.L. 'Heathlands' in 'Australian Vegetation' R.H. Groves ed. Cambridge University Press 1988 Even more diverse though less widespread heath communities occur in Southern Africa. Extensive heath communities can also be found in the Texas chaparral, New Caledonia, central Chile, and along the shores of the Mediterranean Sea. In addition to these extensive heath areas, the vegetation type is also found in scattered locations acro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moorland
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra (where the subsoil is permafros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forestry
Forestry is the science and craft of creating, managing, planting, using, conserving and repairing forests, woodlands, and associated resources for human and environmental benefits. Forestry is practiced in plantations and natural stands. The science of forestry has elements that belong to the biological, physical, social, political and managerial sciences. Forest management play essential role of creation and modification of habitats and affect ecosystem services provisioning. Modern forestry generally embraces a broad range of concerns, in what is known as multiple-use management, including: the provision of timber, fuel wood, wildlife habitat, natural water quality management, recreation, landscape and community protection, employment, aesthetically appealing landscapes, biodiversity management, watershed management, erosion control, and preserving forests as " sinks" for atmospheric carbon dioxide. Forest ecosystems have come to be seen as the most important componen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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