Hameringham
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Hameringham
Hameringham is an extended village in the East Lindsey district of Lincolnshire, England. It is situated south-east from the town of Horncastle, and consists of High Hameringham and Low Hammeringham. It is in the civil parish of Lusby with Winceby. The parish church is dedicated to All Saints, and is a Grade II listed building dating from the year 1200, although heavily restored in 1893 by Hodgson Fowler after the nave collapsed. It is made from greenstone, brick, limestone and red sandstone. Hameringham belongs to the Fen and Hill Group of Parishes which also includes: * Mareham le Fen, St Helen * Mareham on the Hill, All Saints * Revesby, St Lawrence *Scrivelsby, St Benedict *Wilksby, All Saints The Thatched Cottage is a Grade II listed late 18th-century mud and stud thatched cottage. Dunsthorpe is a deserted medieval village In the United Kingdom, a deserted medieval village (DMV) is a former settlement which was abandoned during the Middle Ages, typically leaving ...
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Horncastle
Horncastle is a town and civil parish in the East Lindsey district in Lincolnshire, east of Lincoln. Its population was 6,815 at the 2011 census and estimated at 7,123 in 2019. A section of the ancient Roman walls remains. History Romans Although fortified, Horncastle was not on any important Roman roads, which suggests that the River Bain was the principal route of access to it. Roman Horncastle has become known recently as ''Banovallum'' (i. e. Wall on the River Bain). Although this Roman name has been adopted by some local businesses and the town's secondary modern school, it is not firmly known to be original. ''Banovallum'' was merely suggested in the 19th century through an interpretation of the '' Ravenna Cosmography'', a 7th-century list of Roman towns and road-stations, and may equally have meant Caistor. The Roman walls remain in places. One section is on display in the town's library, which was built over the top of the wall. The Saxons called the town ''Hyrne ...
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East Lindsey
East Lindsey is a local government district in Lincolnshire, England. The population of the district council was 136,401 at the 2011 census. The council is based in Manby. Other major settlements in the district include Alford, Wragby, Spilsby, Mablethorpe, Skegness, Horncastle, Chapel St Leonards and Louth. Skegness is the largest town in East Lindsey, followed by Louth, Mablethorpe and Horncastle. Political representation The political composition of East Lindsey District Council is as follows: With a total of 55 seats, the Conservatives hold a 7-seat majority, following the defection of two councillors (David Mangion and Sarah Parkin) to the Conservatives in 2020. Geography East Lindsey has an area of 1,760 km2, making it the fifth-largest district (and second-largest non-unitary district) in England. It was formed on 1 April 1974, under the Local Government Act 1972, from the south-eastern area of the former administrative county of Lindsey. It was a merger of th ...
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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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Villages In Lincolnshire
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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Deserted Medieval Village
In the United Kingdom, a deserted medieval village (DMV) is a former settlement which was abandoned during the Middle Ages, typically leaving no trace apart from earthworks or cropmarks. If there are fewer than three inhabited houses the convention is to regard the site as deserted; if there are more than three houses, it is regarded as a shrunken medieval village. There are estimated to be more than 3,000 DMVs in England alone. Other deserted settlements Not all sites are medieval: villages reduced in size or disappeared over a long period, from as early as Anglo-Saxon times to as late as the 1960s, due to numerous different causes. Reasons for desertion Over the centuries, settlements have been deserted as a result of natural events, such as rivers changing course or silting up, flooding (especially during the wet 13th and 14th centuries) as well as coastal and estuarine erosion or being overwhelmed by windblown sand. Many were thought to have been abandoned due to the de ...
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Mud And Stud
Wattle and daub is a composite building method used for making walls and buildings, in which a woven lattice of wooden strips called wattle is daubed with a sticky material usually made of some combination of wet soil, clay, sand, animal dung and straw. Wattle and daub has been used for at least 6,000 years and is still an important construction method in many parts of the world. Many historic buildings include wattle and daub construction. History The wattle and daub technique was used already in the Neolithic period. It was common for houses of Linear pottery and Rössen cultures of middle Europe, but is also found in Western Asia (Çatalhöyük, Shillourokambos) as well as in North America (Mississippian culture) and South America (Brazil). In Africa it is common in the architecture of traditional houses such as those of the Ashanti people. Its usage dates back at least 6,000 years. There are suggestions that construction techniques such as lath and plaster and even cob ...
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Wilksby
Wilksby is a hamlet in the civil parish of Wood Enderby, in the East Lindsey district of Lincolnshire. A former civil parish in itself, it was merged with the parish of Wood Enderby in 1936. History Wilksby was mentioned in ''Domesday Book'' of 1086 as "Wilchesbi", with the Lord of the Manor being William I. The name is derived from the Old Norse "Vilgeirr's/Vilgerth's" + "by", meaning the farmstead of Vilgeirr/Vilgerth. In 1931 the parish had a population of 30. On 1 April 1936 the parish was abolished and merged with Wood Enderby. Church The church is dedicated to All Saints, though it may once have been St Mary, and is Grade II listed. Built of greenstone and red brick, It was renovated in 1895. A church has known to have been on the site for at least 800 years, with the first recorded rector was Simon de Tynton in 1230. The stone font dates from the reign of King John (1166-1216), with the earliest written records from the church from 1563. Geography Wilksby lie ...
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Scrivelsby
Scrivelsby is a village and ecclesiastical parish in the East Lindsey district of the County of Lincolnshire, England. It is situated south of Horncastle and is on the B1183 road east from the A153 road. It is administered by the civil parish of Mareham on the Hill. Historically the manor was held by grand serjeanty, a form of feudal tenure which required the performance of a ceremonial service rather than a money payment – in this case as the King's Champion. History The manor of Scrivelsby is listed in the Domesday Book of 1086 as "Scrivelesbi" and was held in-chief from the king. It then comprised 89 households, 16 villagers, 11 smallholders and 30 freemen, with 8.5 ploughlands, a meadow of , woodland of , a mill and a church. In 1086 the manor was held by ''Robert Dispensator'' (Latin) ("Robert the Bursar"). Robert was succeeded by his brother Urse d'Abetot, feudal baron of Salwarpe in Worcestershire. Shortly thereafter the manor was in the possession of Roger ...
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Revesby, Lincolnshire
Revesby is a village and civil parish in the East Lindsey district of Lincolnshire, England. It is south-east from Horncastle, east from Woodhall Spa and north from Boston, and on the A155. The parish includes the hamlet of Moorhouses to the south of Revesby village. History The parish includes the site of the Cistercian abbey of SS Mary and Lawrence, founded in 1142 and colonised by monks from Rievaulx Abbey. The abbey was suppressed through the 1538 Dissolution of the Lesser Monasteries Act.Cox, J. Charles (1916) ''Lincolnshire'' pp. 249, 250; Methuen & Co. Ltd A post- restoration house was built close to the site of the abbey by Craven Howard. This house was rebuilt in 1849 as Revesby Abbey in Elizabethan style, to the 1843 design of William Burn, architect for Harlaxton Manor, with of deer park.''Kelly's Directory of Lincolnshire with the port of Hull'' 1885, p. 604Pevsner, Nikolaus; Harris, John: ''The Buildings of England: Lincolnshire'' p. 342 ...
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Mareham On The Hill
Mareham on the Hill is a village and civil parish about south-east from the town of Horncastle, Lincolnshire, England. Mareham on the Hill is listed in the 1086 ''Domesday Book'' as having one household and of woodland. The parish church is dedicated to All Saints and is a Grade II* listed building dating from the 15th century, although it was restored in 1780 and remodelled in 1804. It is built of green sandstone, limestone and red brick, and is colourwashed. The ecclesiastical parish is Mareham on the Hill, part of The Fen and Hill Group of the Deanery A deanery (or decanate) is an ecclesiastical entity in the Roman Catholic Church, the Eastern Orthodox Church, the Anglican Communion, the Evangelical Church in Germany, and the Church of Norway. A deanery is either the jurisdiction or residenc ... of Horncastle. The 2013 incumbent is Rev Canon Alec Boyd. Mareham Grange farmhouse is a Grade II listed 18th-century red-brick farmhouse with 20th-century alterations. Re ...
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Mareham Le Fen
Mareham le Fen (otherwise Mareham-le-Fen) is a village and civil parish about south from the town of Horncastle, Lincolnshire, England. The hamlet of Mareham Gate lies about south from the village, and it is believed that the deserted medieval village (DMV) of Birkwood is situated nearby. Mareham le Fen is listed in the 1086 ''Domesday Book'' as "Marun", with 33 households, of meadow, of woodland, and a church. The Lord of the Manor was William I. The parish church is dedicated to St Helen, and is a Grade II* listed building of greenstone and dating from the 13th century. It was partially rebuilt in 1879, and in 1974 the vestry was extended using stone from the demolished church of St Margaret at Woodhall. In the north aisle is a tomb to James Roberts who died 1826, and sailed in the ''Endeavour'' with Captain Cook and Sir Joseph Banks. In the churchyard is a medieval stone cross, which is both Grade II listed and a scheduled monument. Dating from the 14th century, it w ...
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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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