Horsham Stone
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Horsham Stone
Horsham Stone is a type of calcareous, flaggy sandstone containing millions of minute sand grains and occurring naturally in the Weald Clay of south-east England.Roger Birch, Sussex Stone, The Story of Horsham Stone and Sussex Marble, 2006, It is also high in mica and quartz. The rock extends in an arc-like formation for several kilometres around the town of Horsham from which it takes its name, and lies just below the Weald Clay surface in bands thick. Horsham Stone is significant for its ripple-marked appearance, formed by the action of the sea similar to the ripples on the sandbanks and beaches of Sussex. Formation Sussex Stone and its limestone equivalent Sussex Marble were formed around 130 million years ago in the Lower Cretaceous period when Britain was quite different from the shape it is today. It is estimated that the latitude for Britain was approximately 30 degrees north of the equator. The fossil evidence in Horsham Stone and Sussex Marble indicate a diversity of l ...
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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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Stane Street (Chichester)
Stane Street is the modern name of the Roman road in southern England that linked ''Londinium'' (London) to ''Noviomagus Reginorum'' (Chichester). The exact date of construction is uncertain; however, on the basis of archaeological artefacts discovered along the route, it was in use by 70 AD and may have been built in the first decade of the Roman occupation of Britain (as early as 43–53 AD). Stane Street shows clearly the engineering principles that the Romans used when building roads. A straight-line alignment from London Bridge to Chichester would have required steep crossings of the North Downs, Greensand Ridge and South Downs. The road was therefore designed to exploit a natural gap in the North Downs cut by the River Mole and to pass to the east of the high ground of Leith Hill, before following flatter land in the River Arun valley to Pulborough. The direct survey line was followed only for the northernmost from London to Ewell. At no point does the roa ...
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Stone (material)
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. M ...
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Sandstone In The United Kingdom
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 tec ...
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List Of Sandstones
This is a list of types of sandstone that have been or are used economically as natural stone for building and other commercial or artistic purposes. Trans-regional (across state borders) *'' Cornbrash Sandstone'': North Rhine-Westphalia, Lower Saxony *'' Elbe Sandstone'': Germany (Saxony) and the Czech Republic *''Red Main Sandstone'': Hesse, Baden-Württemberg, Bavaria *'' Wealden Sandstone'': Lower Saxony, North Rhine-Westphalia Australia * ''Hawkesbury Sandstone'': Sydney Basin, Gosford Belgium * '' Balegem Sandstone'': Balegem in Oosterzele * '' Ledian Sandstone'': Lede * '' Gobertange Sandstone'': Gobertange in Jodoigne Canada * Nepean Sandstone: Ottawa, Ontario * Paskapoo Sandstone: Calgary, Alberta Czech Republic * ''Božanov Sandstone'': near Božanov * ''Niedergrund Sandstone'': near Dolní Žleb * Libná Sandstone: near Libná * ''Zdoňov Sandstone'': near Zdoňov * ''Mšené Sandstone''; near Mšené-lázně * ''Podhorní Sandstone'': near Podhorn ...
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Purbeck Stone
Purbeck stone refers to building stone taken from a series of limestone beds found in the Upper Jurassic to Lower Cretaceous Purbeck Group, found on the Isle of Purbeck, Dorset in southern England. The best known variety of this stone is Purbeck Marble. The stone has been quarried since at least Roman times up to the present day. Geology The Purbeck Group is a sequence of sedimentary rocks that were deposited in a shallow freshwater to brackish lagoonal setting. It ranges in age from Tithonian to Berriasian. Limestone beds are developed at various levels throughout the sequence, each with a different character, which led to them being quarried for specific uses. Towards the top of the Lulworth Formation is the 'New Vein'. In the lower part of the Durlston Formation are the 'Downs vein, 'Freestone Vein' and the 'Laning Vein'. Towards the top of the Durlston are the 'Burr' (or Broken Shell Limestone) with up to three beds of the 'Purbeck Marble' above that. Occurrence The Purbeck Gr ...
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Cottage In Nuthurst Village, West Sussex England 2
A cottage, during Feudalism in England, England's feudal period, was the holding by a cottager (known as a cotter or ''bordar'') of a small house with enough garden to feed a family and in return for the cottage, the cottager had to provide some form of service to the manorial lord.Daniel D. McGarry, ''Medieval history and civilization'' (1976) p 242 However, in time cottage just became the general term for a small house. In modern usage, a cottage is usually a modest, often cosy dwelling, typically in a rural or semi-rural location and not necessarily in England. The cottage orné, often quite large and grand residences built by the nobility, dates back to a movement of "rustic" stylised cottages of the late 18th and early 19th century during the Romantic movement. In British English the term now denotes a small dwelling of traditional build, although it can also be applied to modern construction designed to resemble traditional houses (" mock cottages"). Cottages may be d ...
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Southwater
Southwater is a large village and civil parish in the Horsham District of West Sussex, England, with a population of roughly 10,000. It is administered within Horsham District Council and West Sussex County Council. History One of the oldest buildings in the parish is Great House Farmhouse, a listed building at Grade II* built in 1462 from a late medieval structure in the Tudor period just west of the town. In the early 19th century Southwater was predominately a collection of large estates divided into leased farms. Whilst mixed agriculture provided a lucrative industry for centuries, much of the population of Southwater originated from the workforce of the brick industry and the arrival of the railway, which opened in 1866. At the peak of production, the Southwater brickworks manufactured 18 million bricks a year, and employed 100 men. It was reported that Southwater bricks were used in the building of Christ’s Hospital, Victoria Station, RAAF Woomera Range Complex, London ...
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Nuthurst
Nuthurst is a village and civil parish in the Horsham district of West Sussex, England. The north of the parish borders Horsham town, with Nuthurst village south from the border. Within the parish is the estate and largely 19th-century country house of Sedgwick Park. History Nuthurst does not appear in the ''Domesday Book''. According to ''A Dictionary of British Place Names'', the place is recorded in 1228 as 'Nothurst', meaning "wooded hill where nut-trees grow", from the Old English ''hnutu'' + ''hyrst''. Nuthurst manor, and later parish, since before the Norman conquest of England has been part of the Singlegross Hundred of the Rape of Bramber. In 1855 the parish was of . The 1841 population was listed as 768; the 1851 population as 727. Nuthurst occupations in 1855 included 21 farmers, one of whom was a grocer at Mannings Heath, a charcoal burner, a carpenter, a blacksmith, a shoemaker, a baker, a shopkeeper who held the post office, two wheelwrights, one of whom operated ...
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Itchingfield
Itchingfield is a small village and civil parish in the Horsham district of West Sussex, England. It lies on the Barns Green to Broadbridge Heath road southwest of Horsham Horsham is a market town on the upper reaches of the River Arun on the fringe of the Weald in West Sussex, England. The town is south south-west of London, north-west of Brighton and north-east of the county town of Chichester. Nearby to .... The main settlement in the parish is Barns Green. The village's origins may lie with the Romans. This is suggested by the discovery of tiles in the parish. Gallery File:Itchingfield Church print.jpg, St. Nicolas c. 1830 File:St. Nicolas, Itchingfield.jpg, St. Nicolas 2017 File:Itchingfield Church interior - geograph.org.uk - 1588319.jpg, St. Nicolas Interior File:Itchingfield School - geograph.org.uk - 1071438.jpg, Itchingfield School References External links Horsham District Villages in West Sussex {{WestSussex-geo-stub ...
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Shipley, West Sussex
Shipley is a village and civil parish in the Horsham District of West Sussex, England. It lies just off the A272 road north-east of Storrington. The parish includes the village of Coolham and the hamlets of Dragon's Green, Brooks Green and Broomer's Corner. Shipley is first mentioned in a charter of 1073 as ''Scapeleia'', and in the Domesday Book of 1086 as ''Sepelei''. The name derives from the Old English ''scēap'' ('sheep') and ''lēah'' ('open ground, such as meadow, pasture, or arable land'). Thus it means 'sheep-clearing' or 'sheep-pasture'. The western River Adur flows through the village, where it meets a significant tributary, Lancing Brook. The parish has a land area of . In the 2001 census 1075 people lived in 448 households of whom 596 were economically active. At the 2011 Census the population included the hamlet of Coolham and increased to a total of 1,147. Shipley was home to Hilaire Belloc who in 1906 purchased Kings Land, with a house, and Shipley Windmi ...
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Manor House
A manor house was historically the main residence of the lord of the manor. The house formed the administrative centre of a manor in the European feudal system; within its great hall were held the lord's manorial courts, communal meals with manorial tenants and great banquets. The term is today loosely applied to various country houses, frequently dating from the Late Middle Ages, which formerly housed the landed gentry. Manor houses were sometimes fortified, albeit not as fortified as castles, and were intended more for show than for defencibility. They existed in most European countries where feudalism was present. Function The lord of the manor may have held several properties within a county or, for example in the case of a feudal baron, spread across a kingdom, which he occupied only on occasional visits. Even so, the business of the manor was directed and controlled by regular manorial courts, which appointed manorial officials such as the bailiff, granted ...
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