Chilmark Stone
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Chilmark Stone
Chicksgrove Quarry () is a geological Site of Special Scientific Interest south of Upper Chicksgrove in Wiltshire, England notified in 1971. Chilmark stone, a form of limestone, is quarried at the site. Chicksgrove Quarry Ltd also operates Chilmark Mine, a site 1.5 miles to the northeast at Chilmark Quarries. Chilmark stone Chilmark stone is a fine quality building stone used extensively for construction and restoration projects throughout the South of England and nationally as a match for other stones such as Reigate Stone, Malmstone and Kentish rag. Thousands of tonnes of stone from Chicksgrove Quarry have been used in the restoration of Salisbury Cathedral. Other uses for the stone include restoration at Westminster Abbey Chapter House and Hampton Court Palace. Geological interest Strata at the quarry were first studied by Etheldred Benett in 1819. The geology exposed by the present and historical workings at Chicksgrove Quarry contribute heavily towards its classifica ...
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Geological Site Of Special Scientific Interest
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may b ...
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Salisbury Cathedral
Salisbury Cathedral, formally the Cathedral Church of the Blessed Virgin Mary, is an Anglican cathedral in Salisbury, England. The cathedral is the mother church of the Diocese of Salisbury and is the seat of the Bishop of Salisbury. The building is regarded as one of the leading examples of Early English Gothic architecture. Its main body was completed in 38 years, from 1220 to 1258. The spire, built in 1320, at , has been the tallest church spire in the United Kingdom since 1561. Visitors can take the "Tower Tour", in which the interior of the hollow spire, with its ancient wooden scaffolding, can be viewed. The cathedral has the largest cloister and the largest cathedral close in Britain at . It contains a clock which is among the oldest working examples in the world, and has one of the four surviving original copies of ''Magna Carta''. In 2008, the cathedral celebrated the 750th anniversary of its consecration. History As a response to deteriorating relations between ...
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Sites Of Special Scientific Interest In Wiltshire
__NOTOC__ The following is a list of Sites of Special Scientific Interest (SSSIs) in Wiltshire, England, United Kingdom. In England the body responsible for designating SSSIs is Natural England, which chooses a site because of its fauna, flora, geological or physiographical features. As of 2006, there are 134 sites designated in this Area of Search, of which the vast majority, 108, have been designated due to their biological interest, with just 21 due to their geological interest (and 5 for both). Natural England took over the role of designating and managing SSSIs from English Nature in October 2006 when it was formed from the amalgamation of English Nature, parts of the Countryside Agency and the Rural Development Service. Natural England, like its predecessor, uses the 1974–1996 county system and as such the same approach is followed here, rather than adopting the current local government or ceremonial county boundaries. The data in the table is taken from English Nature's ...
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Portland Stone
Portland stone is a limestone from the Tithonian stage of the Jurassic period quarried on the Isle of Portland, Dorset. The quarries are cut in beds of white-grey limestone separated by chert beds. It has been used extensively as a building stone throughout the British Isles, notably in major public buildings in London such as St Paul's Cathedral and Buckingham Palace. Portland Stone is also exported to many countries—being used for example in the United Nations headquarters in New York City. Geology Portland Stone formed in a marine environment, on the floor of a shallow, warm, sub-tropical sea probably near land (as evidenced by fossilized driftwood, which is not uncommon). When seawater is warmed by the sun, its capacity to hold dissolved gas is reduced; consequently, dissolved carbon dioxide (CO2) is released into the atmosphere as a gas. Calcium and bicarbonate ions within the water are then able to combine, to form calcium carbonate (CaCO3) as a precipitate. The proces ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ...
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Etheldred Benett
Etheldred Anna Maria Benett (22 July 1776 – 11 January 1845) was an early English geologist often credited with being the first female geologist, having devoted much of her life to collecting and studying fossils that she discovered in South West England. She worked closely with many principal geologists and her fossil collection, considered one of the largest at the time, played a part in the development of geology as a field of science. Early life Etheldred Anna Maria Benett was born in 1776 (or 1775) into a wealthy family as the second daughter of Thomas Benett (1729–1797) of Wiltshire and Catherine ''née'' Darell (d. 1790). Her maternal great grandfather was William Wake, Archbishop of Canterbury. Her elder brother John was member of Parliament for Wiltshire and later South Wiltshire from 1819 to 1852; his daughter married Lord Charles Spencer-Churchill. From 1802 she lived at Norton House in Norton Bavant, near Warminster, Wiltshire where she lived with he ...
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Hampton Court Palace
Hampton Court Palace is a Grade I listed royal palace in the London Borough of Richmond upon Thames, southwest and upstream of central London on the River Thames. The building of the palace began in 1514 for Cardinal Thomas Wolsey, the chief minister of Henry VIII. In 1529, as Wolsey fell from favour, the cardinal gave the palace to the king to check his disgrace. The palace went on to become one of Henry's most favoured residences; soon after acquiring the property, he arranged for it to be enlarged so that it might more easily accommodate his sizeable retinue of courtiers. Along with St James' Palace, it is one of only two surviving palaces out of the many the king owned. The palace is currently in the possession of King Charles III and the Crown. In the following century, King William III's massive rebuilding and expansion work, which was intended to rival the Palace of Versailles, destroyed much of the Tudor palace.Dynes, p. 90. His work ceased in 1694, leaving the pa ...
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Westminster Abbey
Westminster Abbey, formally titled the Collegiate Church of Saint Peter at Westminster, is an historic, mainly Gothic church in the City of Westminster, London, England, just to the west of the Palace of Westminster. It is one of the United Kingdom's most notable religious buildings and since Edward the Confessor, a burial site for English and, later, British monarchs. Since the coronation of William the Conqueror in 1066, all coronations of English and British monarchs have occurred in Westminster Abbey. Sixteen royal weddings have occurred at the abbey since 1100. According to a tradition first reported by Sulcard in about 1080, a church was founded at the site (then known as Thorney Island) in the seventh century, at the time of Mellitus, Bishop of London. Construction of the present church began in 1245 on the orders of Henry III. The church was originally part of a Catholic Benedictine abbey, which was dissolved in 1539. It then served as the cathedral of the Dioce ...
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Kentish Rag
Kentish may be used as a name: * Kentish Council is a local government area in Tasmania, Australia * Kentish Town is an area of north west London, England Kentish as a surname: * John Kentish (minister), 1768–1853 * John Kentish (tenor), 1910–2006, English opera singer Kentish may also be an adjective for things relating to the English county of Kent or the former Kingdom of Kent: * Kentish dialect, the dialect of Modern English spoken in Kent * Kentish dialect (Old English), a dialect of Old English * Kentish Man or Maid * Old Kentish Carol, a traditional Christmas carol from Kent See also * Kent (other) * Kentish plover {{disambig ...
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Upper Chicksgrove
Upper may refer to: * Shoe upper or ''vamp'', the part of a shoe on the top of the foot * Stimulant, drugs which induce temporary improvements in either mental or physical function or both * ''Upper'', the original film title for the 2013 found footage film ''The Upper Footage ''The Upper Footage'' (also known as ''Upper'') is a 2013 found footage film written and directed by Justin Cole. First released on January 31, 2013 to a limited run of midnight theatrical screenings at Landmark’s Sunshine Cinema in New York Cit ...'' See also

{{Disambiguation ...
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Malmstone
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil-rich, such as in the late-Cretaceous deposits of New Jersey. Occurrence Important exposures are known from both northern and western Europe, North America, southeastern Brazil and north Africa. Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware. Although greensand has ...
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Reigate Stone
Reigate Stone is a freestone that was mined from the Upper Greensand in north east Surrey. It was used in building work throughout the middle ages and early modern period. It is sometimes classified as a calcareous sandstone, although very little of the silica content is in the form of detrital sand grains. In addition to silicon dioxide, the stone also includes clay, fine-grained calcite, mica flakes and glauconite. Since exposure of Upper Greensand is rare, Reigate Stone was generally extracted from underground workings, although it may have been quarried from the surface at first. The stone was mined using the post-and-stall technique, in which adits (approximately wide and high) were cut into the beds, which dip downwards below the chalk above. Parallel grooves in the floors of these workings suggest that cut stone was brought to the surface on wooden sledges. Mines are thought to have existed along the base of the North Downs from Buckland in the west to Chaldon in th ...
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