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River Doe Lea
The River Doe Lea is a river which flows near Glapwell and Doe Lea in Derbyshire, England. The river eventually joins the River Rother near Renishaw. The river contained 1,000 times the safe level of dioxins in 1991, according to a statement made by Dennis Skinner, (MP) in the House of Commons in 1992. The river flows through the site of the former Coalite plant near Bolsover, where coke, tar and industrial chemicals were manufactured until the plant closed in 2004. The stream section is designated an SSSI for its geological interest. Hydrology The river flows in a generally south to north direction through a region where the underlying geology is predominantly Carboniferous coal measures. To the east of its catchment there is a band of Permian Magnesian Limestone, which forms an escarpment. Magnesian Limestone is so called because it contains quantities of the mineral dolomite, which is rich in magnesium. The river and its tributary streams drain an area of about . During i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Doe Lea
Doe Lea is a small, linear village in the English county of Derbyshire. It is in the Bolsover district of the county and falls in the Ault Hucknall civil parish. The village runs along the old A617 road. A newer dual carriageway (currently the A617) runs parallel to it. The village is also immediately adjacent to junction 29 of the M1 motorway, like its neighbouring village Heath. Hardwick Hall is nearby. In 2005 the river and banks were given a makeover. A new path was put down, about 30 new trees were planted, the path was called Willow Walk and was opened by Dennis Skinner, MP. The work was carried out by The Doe Lea Valley Community Partnership, a group of volunteers from Doe Lea and surrounding areas. Work is still being carried out and is still being maintained by the group. The village has a public house and a community centre. The River Doe Lea runs through the village, and Doe Lea local nature reserve is located nearby. Doe Lea is near the villages of Bramley Vale, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scarcliffe
Scarcliffe is a village and civil parish in the Bolsover district of Derbyshire, England. It is sometimes called Scarcliffe with Palterton. The population of the parish (including the hamlets of Palterton, Rylah, Stockley, and parts of Stony Houghton and Hillstown (Bolsover)) at the 2001 UK Census was 5,211, increasing to 5,288 at the 2011 Census. Location About two miles (3 km) SSE of Bolsover, the village's main street is the B6417 road between Clowne and New Houghton, which connects at Scarcliffe to the A617 between Mansfield and Chesterfield. Other nearby settlements include Clay Cross, Matlock, Shirebrook, Warsop, North Wingfield, Tupton, Pilsley and Ashover.Scarcliffe, Derbyshire – home page of scarcliffeweb.co.uk (accessed 14 November 2007) Scarcliffe is within a few miles of Junction 29 of the |
Stainsby Mill
Stainsby Mill is a 19th-century flour watermill in Doe Lea, Chesterfield, Derbyshire, England. The mill, which has been restored to full working order, is a Grade II listed building and is under the ownership of the National Trust. The mill is part of the Hardwick Hall estate. History A mill on this site appears to have existed from the early 13th century. Originally all the water for the mill came from the River Doe Lea which fed the Miller's Pond on the Hardwick estate. By 1762 the Stainsby Pond, fed by the Stainsby Brook, had been constructed and the water also fed into the Mill Pond which was situated on the other side of the road from the mill. Water was allowed into the mill race by sluice gates under the road. The current mill By the 1840s the mill had become dilapidated and William Cavendish, 6th Duke of Devonshire decided it needed rebuilding and re-equipping. The mill was substantially rebuilt in dressed stone from the Hardwick Estate and fitted with modern machinery, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Trust For Places Of Historic Interest Or Natural Beauty
The National Trust, formally the National Trust for Places of Historic Interest or Natural Beauty, is a charity and membership organisation for heritage conservation in England, Wales and Northern Ireland. In Scotland, there is a separate and independent National Trust for Scotland. The Trust was founded in 1895 by Octavia Hill, Sir Robert Hunter and Hardwicke Rawnsley to "promote the permanent preservation for the benefit of the Nation of lands and tenements (including buildings) of beauty or historic interest". It was given statutory powers, starting with the National Trust Act 1907. Historically, the Trust acquired land by gift and sometimes by public subscription and appeal, but after World War II the loss of country houses resulted in many such properties being acquired either by gift from the former owners or through the National Land Fund. Country houses and estates still make up a significant part of its holdings, but it is also known for its protection of wild lands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Country House
An English country house is a large house or mansion in the English countryside. Such houses were often owned by individuals who also owned a town house. This allowed them to spend time in the country and in the city—hence, for these people, the term distinguished between town and country. However, the term also encompasses houses that were, and often still are, the full-time residence for the landed gentry who ruled rural Britain until the Reform Act 1832. Frequently, the formal business of the counties was transacted in these country houses, having functional antecedents in manor houses. With large numbers of indoor and outdoor staff, country houses were important as places of employment for many rural communities. In turn, until the agricultural depressions of the 1870s, the estates, of which country houses were the hub, provided their owners with incomes. However, the late 19th and early 20th centuries were the swansong of the traditional English country house lifest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grade I Listed
In the United Kingdom, a listed building or listed structure is one that has been placed on one of the four statutory lists maintained by Historic England in England, Historic Environment Scotland in Scotland, in Wales, and the Northern Ireland Environment Agency in Northern Ireland. The term has also been used in the Republic of Ireland, where buildings are protected under the Planning and Development Act 2000. The statutory term in Ireland is " protected structure". A listed building may not be demolished, extended, or altered without special permission from the local planning authority, which typically consults the relevant central government agency, particularly for significant alterations to the more notable listed buildings. In England and Wales, a national amenity society must be notified of any work to a listed building which involves any element of demolition. Exemption from secular listed building control is provided for some buildings in current use for worship, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hardstoft
Hardstoft is a hamlet in Derbyshire, England. It is located four miles east of Clay Cross, on the B6039 road. The Mexican Eagle Petroleum Company found small quantities of oil near Hardstoft in 1919 under encouragement from the British government. R. W. Ferrier, accessed 28 December 2008 See also *Listed buildings in Ault Hucknall
Ault Hucknall is a civil parish in the Bolsover district of Derbyshire, England. The parish co ...
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M1 Motorway
The M1 motorway connects London to Leeds, where it joins the A1(M) near Aberford, to connect to Newcastle. It was the first inter-urban motorway to be completed in the UK; the first motorway in the country was the Preston By-pass, which later became part of the M6. The motorway is long and was constructed in four phases. Most of the motorway was opened between 1959 and 1968. The southern end was extended in 1977 and the northern end was extended in 1999. History There had been plans before the Second World War for a motorway network in the United Kingdom. Lord Montagu formed a company to build a 'motorway like road' from London to Birmingham in 1923, but it was a further 26 years before the Special Roads Act 1949 was passed, which allowed for the construction of roads limited to specific vehicle classifications, and in the 1950s, the country's first motorways were given the government go-ahead. The first section of motorway was the Preston Bypass in Lancashire, now par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tibshelf
Tibshelf is a village and civil parish in the Bolsover District in Derbyshire, England. Located between the towns of Clay Cross, Shirebrook, Mansfield and Chesterfield. It had a population at the 2001 UK census of 3,548, increasing to 3,787 at the 2011 Census. Tibshelf shares its boundaries with the villages of Morton, Pilsley, Newton, Teversal and Hardstoft. The village was the site of the UK's first inland oil well. In the 19th century, coal was discovered, coal mining overtook agriculture as the primary industry in the area, and a local railway system was developed. Two deep mines were sunk, but were under threat of closure for a number of years after a partial cave-in. Culture and community Tibshelf has since redeveloped itself into a popular place to live, in part due to its location near the M1 motorway (Tibshelf services was originally named Chesterfield Services, but was rebranded due to being closer to Tibshelf, and after pressure from the local authorities) and its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magnesium
Magnesium is a chemical element with the symbol Mg and atomic number 12. It is a shiny gray metal having a low density, low melting point and high chemical reactivity. Like the other alkaline earth metals (group 2 of the periodic table) it occurs naturally only in combination with other elements and it almost always has an oxidation state of +2. It reacts readily with air to form a thin passivation coating of magnesium oxide that inhibits further corrosion of the metal. The free metal burns with a brilliant-white light. The metal is obtained mainly by electrolysis of magnesium salts obtained from brine. It is less dense than aluminium and is used primarily as a component in strong and lightweight alloys that contain aluminium. In the cosmos, magnesium is produced in large, aging stars by the sequential addition of three helium nuclei to a carbon nucleus. When such stars explode as supernovas, much of the magnesium is expelled into the interstellar medium where it ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (mineral)
Dolomite () is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite. An alternative name sometimes used for the dolomitic rock type is dolostone. History As stated by Nicolas-Théodore de Saussure the mineral dolomite was probably first described by Carl Linnaeus in 1768. In 1791, it was described as a rock by the French naturalist and geologist Déodat Gratet de Dolomieu (1750–1801), first in buildings of the old city of Rome, and later as samples collected in the mountains now known as the Dolomite Alps of northern Italy. Nicolas-Théodore de Saussure first named the mineral (after Dolomieu) in March 1792. Properties The mineral dolomite crystallizes in the trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. Unless it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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