Ledger Stone
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Ledger Stone
A ledger stone or ledgerstone is an inscribed stone slab usually laid into the floor of a church to commemorate or mark the place of the burial of an important deceased person. The term "ledger" derives from the Middle English words ''lygger'', ''ligger'' or ''leger'', themselves derived from the root of the Old English verb ''liċġan'', meaning to lie (down). Ledger stones may also be found as slabs forming the tops of tomb chest monuments. Form and geology Ledger stones take the form of an inscribed stone slab, usually laid into the floor of a church to commemorate or mark the place of the burial of an important deceased person. Ledger stones may also be found as slabs forming the tops of chest tombs. An inscription is usually incised into the stone within a ledger line running around the edge of the stone. Such inscription may continue within the central area of the stone, which may be decorated with relief-sculpted or incised coats of arms, or other appropriate decorative ite ...
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Holy Trinity Church, Hull
Hull Minster is the Anglican minster and the parish church of Kingston upon Hull in the East Riding of Yorkshire, England. The church was called Holy Trinity Church until 13 May 2017 when it became Hull Minster. History It is the largest parish church in England by floor area. The church dates back to about 1300 and contains what is widely acknowledged to be some of the finest medieval brick-work in the country, particularly in the transepts. The Minster Church is a Grade I listed building. The Minster Church is a member of the Greater Churches Group. William Wilberforce, who led the parliamentary campaign against the slave trade, was baptised in Holy Trinity Church in 1759. In November 2014 plans were unveiled to reorder the church, creating an outstanding venue for performances, exhibitions and banquets, a visitor destination, and a place where those in need of help can find assistance. The aim was to create a place for the whole community, and a venue that would be ...
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Sussex Marble
Sussex Marble is a fossiliferous freshwater limestone material which is prevalent in the Weald Clay of parts of Kent, East Sussex and West Sussex in southeast England. It is also called Petworth Marble, Bethersden Marble or Laughton Stone in relation to villages where it was quarried, and another alternative name is winklestone. It is referred to as "marble" as it polishes very well, although it is not a true marble, geologically speaking, as it has not been subject to metamorphism. The matrix is made up of the shells of freshwater gastropods and ''viviparus'' winkles, similar to but larger than those making Purbeck Marble. The pale calcified remains of the shells are in a matrix of darker material. West Sussex has a good concentration of thin layers of Sussex Marble; beds typically measure no more than thick. There are often two beds—the lower formed of smaller-shelled gastropods than the upper—with a layer of calcareous clay between them. Historical use The Weald of ...
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Nijmegen
Nijmegen (;; Spanish and it, Nimega. Nijmeegs: ''Nimwèège'' ) is the largest city in the Dutch province of Gelderland and tenth largest of the Netherlands as a whole, located on the Waal river close to the German border. It is about 60 km south east of Utrecht and 50 km north east of Eindhoven. Nijmegen is the oldest city in the Netherlands, the second to be recognized as such in Roman times, and in 2005 celebrated 2,000 years of existence. Nijmegen became a free imperial city in 1230 and in 1402 a Hanseatic city. Since 1923 it has been a university city with the opening of a Catholic institution now known as the Radboud University Nijmegen. The city is well known for the International Four Days Marches Nijmegen event. Its population in 2022 was 179,000; the municipality is part of the Arnhem–Nijmegen metropolitan area, with 736,107 inhabitants in 2011. Population centres The municipality is formed by the city of Nijmegen, incorporating the former villages of Ha ...
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Haarlem
Haarlem (; predecessor of ''Harlem'' in English) is a city and municipality in the Netherlands. It is the capital of the province of North Holland. Haarlem is situated at the northern edge of the Randstad, one of the most populated metropolitan areas in Europe; it is also part of the Amsterdam metropolitan area, being located about 15 km to the west of the core city of Amsterdam. Haarlem had a population of in . Haarlem was granted city status or '' stadsrechten'' in 1245, although the first city walls were not built until 1270. The modern city encompasses the former municipality of Schoten as well as parts that previously belonged to Bloemendaal and Heemstede. Apart from the city, the municipality of Haarlem also includes the western part of the village of Spaarndam. Newer sections of Spaarndam lie within the neighbouring municipality of Haarlemmermeer. Geography Haarlem is located on the river Spaarne, giving it its nickname 'Spaarnestad' (Spaarne city). It is situated a ...
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Sir Richard Kaye, 6th Baronet
Sir Richard Kaye, 6th Baronet, , LL.D (1736–25 December 1809) was an English peer, churchman and scientist. He was Dean of Lincoln from 1783, and inherited the baronetcy from his elder brother Sir John Lister Kaye, 5th Baronet in 1789. Life He was educated at Brasenose College, Oxford graduating BCL in 1761. He was a patron of the artists Samuel Hieronymus Grimm, whom he commissioned for two decades to draw "everything curious", and Tilly Kettle. He was a friend of Joseph Banks whom he proposed for the Royal Society, and also Captain James Cook: Cook named after him the island now called Kayak Island. He was a member of the Madrigal Society, and also a Trustee of the British Museum. He married Ellen Fenton, daughter of William Fenton of Rothwell, West Yorkshire and widow of Thomas Mainwaring. In 1789 he was to inherit a baronetcy. He left no children, and the baronetcy came to an end with him. Clerical career Kaye was noted both for his piety but also as a great pluralist ...
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Mazy
Mazy ( wa, Mazi) is a village of Wallonia and a district of the municipality of Gembloux, located in the province of Namur, Belgium. Geography Mazy is crossed by the Orneau (a tributary of the Sambre). Heritage Falnuée Castle Falnuée Castle (french: Château-ferme de Falnuée is a ''château-ferme'' (castle farm) in Mazy, in the municipality of Gembloux, province of Namur, Wallonia, Belgium. It is now a golf clubhouse. See also *List of castles in Belgium A ''list' ..., currently a golf clubhouse, is located in Mazy. References External links * — picture of the castle. Former municipalities of Namur (province) Gembloux {{Namur-geo-stub ...
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Golzinne
Golzinne is a hamlet of the village of Bossière in Wallonia. It is administratively part of the city of Gembloux, located in the province of Namur, Belgium. It is notable as the only current producer of " Noir de Golzinne", a black marble. Marble from Golzinne was used in decorations of the Palace of Versailles The Palace of Versailles ( ; french: Château de Versailles ) is a former royal residence built by King Louis XIV located in Versailles, Yvelines, Versailles, about west of Paris, France. The palace is owned by the French Republic and since 19 .... See also * Noir Belge {{coord, 50, 31, 9.08, N, 4, 42, 55.91, E, type:city_scale:10000_region:BE, display=title Populated places in Namur (province) Gembloux ...
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Tournai Font
Tournai fonts are a type of baptismal font made from blue black limestone during the 12th and early 13th centuries in and around the Belgian town of Tournai by local masons. There are seven complete examples in England and a disputed number in Europe: eighty according to one source, or fifty in Northern France and Belgium and two in Germany according to another. A sculptural tradition, centred around Tournai, arose in the Scheldt valley from the 11th century onwards. This was characterised by its use of low relief (which was a useful feature when a sculpture was transported), hard lines and the depiction of minute detail, these features arising from the hardness of the material used from the 12th century; Tournai marble. As a sculptural style it is distinguished from the contemporary style of Mosan art, and it was used in sculpture in both Ghent and Bruges. The designation "Tournai font" is employed to identify fonts made by local masons who worked the stone, as opposed to at le ...
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Romanesque Architecture
Romanesque architecture is an architectural style of medieval Europe characterized by semi-circular arches. There is no consensus for the beginning date of the Romanesque style, with proposals ranging from the 6th to the 11th century, this later date being the most commonly held. In the 12th century it developed into the Gothic style, marked by pointed arches. Examples of Romanesque architecture can be found across the continent, making it the first pan-European architectural style since Imperial Roman architecture. The Romanesque style in England and Sicily is traditionally referred to as Norman architecture. Combining features of ancient Roman and Byzantine buildings and other local traditions, Romanesque architecture is known by its massive quality, thick walls, round arches, sturdy pillars, barrel vaults, large towers and decorative arcading. Each building has clearly defined forms, frequently of very regular, symmetrical plan; the overall appearance is one of simplic ...
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Tournaisian
The Tournaisian is in the ICS geologic timescale the lowest stage or oldest age of the Mississippian, the oldest subsystem of the Carboniferous. The Tournaisian age lasted from Ma to Ma. It is preceded by the Famennian (the uppermost stage of the Devonian) and is followed by the Viséan. Name and regional alternatives The Tournaisian was named after the Belgian city of Tournai. It was introduced in scientific literature by Belgian geologist André Hubert Dumont in 1832. Like many Devonian and lower Carboniferous stages, the Tournaisian is a unit from West European regional stratigraphy that is now used in the official international time scale. The Tournaisian correlates with the regional North American Kinderhookian and lower Osagean stages and the Chinese Tangbagouan regional stage. In British stratigraphy, the Tournaisian contains three substages: the Hastarian, Ivorian and lower part of the Chadian (the upper part falls in the Viséan). Stratigraphy The base of the ...
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Carboniferous Period
The Carboniferous ( ) is a Period (geology), geologic period and System (stratigraphy), system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Myr, Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin ''wikt:carbo#Latin, carbō'' ("coal") and ''wikt:fero#Latin, 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 (geologist), William Conybeare and William Phillips (geologist), 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 (geology), Mississippian and the later Pennsylvanian (geology), Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Stegocephalia, Tetrapods ( ...
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