Kirk Bramwith
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Kirk Bramwith
Kirk Bramwith is a village and civil parish in the Metropolitan Borough of Doncaster in South Yorkshire, England. It had a population of 200 in 2001, increasing to 320 at the 2011 Census. The village centre is located on a narrow strip of land, sandwiched between the River Don Navigation to the south east and the New Junction Canal to the north west. It is low-lying, with most of it close to the contour, and is almost surrounded by drainage ditches. Structures The Anglican church building is dedicated to St. Mary, and is grade II* listed. Most of the structure, which includes a square west tower, is fourteenth or fifteenth century, but the arch into the chancel and the south porch are much earlier, having been built in the twelfth century. It is built of ashlar magnesian limestone, with roofs of stone slate and Welsh slate. The old rectory was built in 1864 in a Tudor Revival style, using red brick with a Welsh slate roof. On Low Lane there is a late eighteenth-century bri ...
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Doncaster (borough)
The City of Doncaster is a metropolitan borough with city status in the United Kingdom, city status in South Yorkshire, England. It is named after its principal settlement, Doncaster, and includes the surrounding suburbs of Doncaster as well as numerous towns and villages. The district has large amounts of countryside. At 219 sq miles, it is the largest metropolitan borough by area in England. The largest settlement in the borough are Doncaster itself, followed by the towns of Thorne, South Yorkshire, Thorne, Hatfield, South Yorkshire, Hatfield and Mexborough (the latter of which is part of the Barnsley/Dearne Valley built-up area), and it additionally covers the towns of Conisbrough, Stainforth, South Yorkshire, Stainforth, Bawtry, Askern, Edlington and Tickhill. Doncaster borders the Selby District, Selby district of North Yorkshire to the north, the East Riding of Yorkshire to the north-east, North Lincolnshire to the east, Bassetlaw District, Bassetlaw in Nottinghamshire to ...
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South Yorkshire
South Yorkshire is a ceremonial and metropolitan county in the Yorkshire and Humber Region of England. The county has four council areas which are the cities of Doncaster and Sheffield as well as the boroughs of Barnsley and Rotherham. In Northern England, it is on the east side of the Pennines. Part of the Peak District national park is in the county. The River Don flows through most of the county, which is landlocked. The county had a population of 1.34 million in 2011. Sheffield largest urban centre in the county, it is the south west of the county. The built-up area around Sheffield and Rotherham, with over half the county's population living within it, is the tenth most populous in the United Kingdom. The majority of the county was formerly governed as part of the county of Yorkshire, the former county remains as a cultural region. The county was created on 1 April 1974, under the Local Government Act 1972. It was created from 32 local government districts of the ...
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Civil Parish
In England, a civil parish is a type of administrative parish used for local government. It is a territorial designation which is the lowest tier of local government below districts and counties, or their combined form, the unitary authority. Civil parishes can trace their origin to the ancient system of ecclesiastical parishes, which historically played a role in both secular and religious administration. Civil and religious parishes were formally differentiated in the 19th century and are now entirely separate. Civil parishes in their modern form came into being through the Local Government Act 1894, which established elected parish councils to take on the secular functions of the parish vestry. A civil parish can range in size from a sparsely populated rural area with fewer than a hundred inhabitants, to a large town with a population in the tens of thousands. This scope is similar to that of municipalities in Continental Europe, such as the communes of France. However, ...
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Metropolitan Borough Of Doncaster
The City of Doncaster is a metropolitan borough with city status in South Yorkshire, England. It is named after its principal settlement, Doncaster, and includes the surrounding suburbs of Doncaster as well as numerous towns and villages. The district has large amounts of countryside. At 219 sq miles, it is the largest metropolitan borough by area in England. The largest settlement in the borough are Doncaster itself, followed by the towns of Thorne, Hatfield and Mexborough (the latter of which is part of the Barnsley/Dearne Valley built-up area), and it additionally covers the towns of Conisbrough, Stainforth, Bawtry, Askern, Edlington and Tickhill. Doncaster borders the Selby district of North Yorkshire to the north, the East Riding of Yorkshire to the north-east, North Lincolnshire to the east, Bassetlaw in Nottinghamshire to the south-east, Rotherham to the south-west, Barnsley to the west, and Wakefield, West Yorkshire, to the north-west. It is part of the Yorkshire ...
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River Don Navigation
The River Don Navigation was the result of early efforts to make the River Don in South Yorkshire, England, navigable between Fishlake and Sheffield. The Dutch engineer Cornelius Vermuyden had re-routed the mouth of the river in 1626, to improve drainage, and the new works included provision for navigation, but the scheme did not solve the problem of flooding, and the Dutch River was cut in 1635 to link the new channel to Goole. The first Act of Parliament to improve navigation on the river was obtained in 1726, by a group of Cutlers based in Sheffield; the Corporation of Doncaster obtained an Act in the following year for improvements to the lower river. Locks and lock cuts were built and by 1751 the river was navigable to Tinsley. The network was expanded by the opening of the Stainforth and Keadby Canal in 1802, linking to the River Trent, the Dearne and Dove Canal in 1804, linking to Barnsley, and the Sheffield Canal in 1819, which provided better access to Sheffield. All ...
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New Junction Canal
The New Junction Canal is a canal in South Yorkshire, England. It is part of the Sheffield and South Yorkshire Navigation (S&SYN), although it was jointly funded by the Aire and Calder Navigation, and was opened in 1905. It links the River Don Navigation and the Stainforth and Keadby Canal with the Aire and Calder Navigation (Knottingley Canal). It is completely straight, and was the last canal built in England for commercial purposes. The canal has one lock, which was sized to allow the compartment boats of the Aire and Calder to use it, but the owning company failed to raise enough money to upgrade the River Don Navigation beyond, and Long Sandall lock prevented working of such boats through to Doncaster until it was rebuilt in 1959. There is still some commercial traffic on the canal, but most use is now by leisure boaters. One notable feature is the aqueduct over the River Don which is protected by large guillotine gates, which can be lowered when the Don is in spate, to p ...
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Kirk Bramwith Church - Geograph
Kirk is a Scottish and former Northern English word meaning "church". It is often used specifically of the Church of Scotland. Many place names and personal names are also derived from it. Basic meaning and etymology As a common noun, ''kirk'' (meaning 'church') is found in Scots, Scottish English, Ulster-Scots and some English dialects, attested as a noun from the 14th century onwards, but as an element in placenames much earlier. Both words, ''kirk'' and ''church'', derive from the Koine Greek κυριακόν (δωμα) (kyriakon (dōma)) meaning ''Lord's (house)'', which was borrowed into the Germanic languages in late antiquity, possibly in the course of the Gothic missions. (Only a connection with the idiosyncrasies of Gothic explains how a Greek neuter noun became a Germanic feminine). Whereas ''church'' displays Old English palatalisation, ''kirk'' is a loanword from Old Norse and thus retains the original mainland Germanic consonants. Compare cognates: Icelandic & ...
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Anglican
Anglicanism is a Western Christian tradition that has developed from the practices, liturgy, and identity of the Church of England following the English Reformation, in the context of the Protestant Reformation in Europe. It is one of the largest branches of Christianity, with around 110 million adherents worldwide . Adherents of Anglicanism are called ''Anglicans''; they are also called ''Episcopalians'' in some countries. The majority of Anglicans are members of national or regional ecclesiastical provinces of the international Anglican Communion, which forms the third-largest Christian communion in the world, after the Roman Catholic Church and the Eastern Orthodox Church. These provinces are in full communion with the See of Canterbury and thus with the Archbishop of Canterbury, whom the communion refers to as its '' primus inter pares'' (Latin, 'first among equals'). The Archbishop calls the decennial Lambeth Conference, chairs the meeting of primates, and is the ...
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Grade II* 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 "Record of Protected Structures, 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 buildin ...
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ...
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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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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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