Hadspen Quarry Ltd
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Hadspen Quarry Ltd
Hadspen Quarry is a stone quarry in Somerset, England. It is shown on Ordnance Survey maps for 1888–90, and may have been in operation for a considerable period before that. It supplies natural stone walling throughout the West Country. The products include coursed, coursed random and random rubble walling. The stone is still split and dressed at the quarry located close to Hadspen house and garden in the small village of Hadspen, within the parish of Pitcombe just outside Castle Cary. This golden colour limestone is seen in buildings in western Dorset and the surrounding areas, as can be seen at the Fleet Street site in Beaminster. Other products include name plaques, sawn ashlar quoins and capping stones. The stone is an Inferior Oolite of the Garantiana Beds, dating back to the Middle Jurassic.Weishampel, David B; et al. (2004). "Dinosaur distribution (Middle Jurassic, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, B ...
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Somerset
( en, All The People of Somerset) , locator_map = , coordinates = , region = South West England , established_date = Ancient , established_by = , preceded_by = , origin = , lord_lieutenant_office =Lord Lieutenant of Somerset , lord_lieutenant_name = Mohammed Saddiq , high_sheriff_office =High Sheriff of Somerset , high_sheriff_name = Mrs Mary-Clare Rodwell (2020–21) , area_total_km2 = 4171 , area_total_rank = 7th , ethnicity = 98.5% White , county_council = , unitary_council = , government = , joint_committees = , admin_hq = Taunton , area_council_km2 = 3451 , area_council_rank = 10th , iso_code = GB-SOM , ons_code = 40 , gss_code = , nuts_code = UKK23 , districts_map = , districts_list = County council area: , MPs = * Rebecca Pow (C) * Wera Hobhouse ( LD) * Liam Fox (C) * David Warburton (C) * Marcus Fysh (C) * Ian Liddell-Grainger (C) * James Heappey (C) * Jacob Rees-Mogg (C) * John Penrose (C) , police = Avon and Somerset Police ...
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Ordnance Survey
, nativename_a = , nativename_r = , logo = Ordnance Survey 2015 Logo.svg , logo_width = 240px , logo_caption = , seal = , seal_width = , seal_caption = , picture = , picture_width = , picture_caption = , formed = , preceding1 = , dissolved = , superseding = , jurisdiction = Great BritainThe Ordnance Survey deals only with maps of Great Britain, and, to an extent, the Isle of Man, but not Northern Ireland, which has its own, separate government agency, the Ordnance Survey of Northern Ireland. , headquarters = Southampton, England, UK , region_code = GB , coordinates = , employees = 1,244 , budget = , minister1_name = , minister1_pfo = , chief1_name = Steve Blair , chief1_position = CEO , agency_type = , parent_agency = , child1_agency = , keydocument1 = , website = , footnotes = , map = , map_width = , map_caption = Ordnance Survey (OS) is the national mapping agency for Great Britain. The agency's name indicates its original military purpose (se ...
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West Country
The West Country (occasionally Westcountry) is a loosely defined area of South West England, usually taken to include all, some, or parts of the counties of Cornwall, Devon, Dorset, Somerset, Bristol, and, less commonly, Wiltshire, Gloucestershire and Herefordshire. "Which counties make up the West Country?", ''YouGov.co.uk'', 23 October 2019
Retrieved 22 June 2021
The West Country has a distinctive regional English dialect and accent, and is also home to the .


Extent ...
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Hadspen House And Garden
Hadspen House of Hadspen, Somerset, England is built of Cary stone, mined from Hadspen Quarry. The stone is a soft limestone known for its deep burnt-orange colour. It is an inferior oolite of the Garantiana Beds and dates to the Middle Jurassic. The house has been designated by English Heritage as a grade II* listed building. House Hadspen House is said to have begun as a farmhouse, purchased by the London-lawyer William Player in 1687 on the Hadspen estate,[1 ] Player 'built the forefront of a gentleman's house in Byfleet Close, a barn two stables and ox house.' Player's expansion continued for 10–12 years. It included building walls around a court, adding a service wing, 'a stall for 24 cattle, a farm baliff's house, a brewhouse' and modern plumbing, with a leaded-pipe water supply. Player also begins the garden, planting extensively on both sides of the house and trees, behind, south and north of the house, that included beeches, elms, poplars, ashes and cherries. Hadspe ...
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Pitcombe
Pitcombe is a village and civil parish south-west of Bruton and from Wincanton in Somerset, England. It has a population of 532. The parish includes the hamlets of Cole and Godminster. The village lies on the River Pitt and other streams that flow into the River Brue. Godminster Lane Quarry and Railway Cutting is a geological Site of Special Scientific Interest important for study of the Inferior Oolite limestones of Middle Jurassic age. The rocks do contain the rich assemblage of fossil ammonites typical of the north Dorset/south Somerset area. It is also important as a reference site for three sub-divisions (zones) of the Inferior Oolite — the laeviscula, discites and concavum Zones. History The name Pitcombe means "the marshy valley". Evidence of prehistoric activity has been found near Godminster Farm, where a Roman coin hoard was also discovered. In the Domesday Book of 1086 the manor was held by Turstin FitzRolf and already had two watermills. Pitcombe wa ...
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Castle Cary
Castle Cary () is a market town and civil parish in south Somerset, England, north west of Wincanton and south of Shepton Mallet, at the foot of Lodge Hill and on the River Cary, a tributary of the Parrett. History The word Cary derives from the Celtic ''caer'' meaning rock, crag or castle, making the term Castle Cary a double-play. Castle Cary is said to take half its name from River Cary, itself an aporia. The first Cary Castle was besieged in 1138 and again in 1152. It was originally made of timber frame, as it would have been built by the Normans and inherited their building traditions in wood. Cary first appears in recorded history after the Norman invasion in the 11th century though according to Castle Cary history 'there is evidence the site was occupied and fortified before this. The second castle was abandoned by the mid-15th century in favour of a manor house and the stones pillaged for other buildings in the town. It would seem that the second castle was begun i ...
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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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Beaminster
Beaminster ( ) is a town and civil parish in Dorset, England, situated in the Dorset Council administrative area approximately northwest of the county town Dorchester. It is sited in a bowl-shaped valley near the source of the small River Brit. The 2013 mid-year estimate of the population of Beaminster parish is 3,100. Beaminster is the product of the Anglo-Saxon age, dating back to around the 7th century, when it was known as Bebingmynster, meaning the church of Bebbe although the date of origin of the town is unknown. The place name and historic evidence indicates that it was probably the site of a primary Saxon minster church and was at the centre of a large episcopal estate. These are likely to have acted as a focus for a settlement, but evidence of its formation is lacking. In its history Beaminster has been a centre of manufacture of linen and woollens, the raw materials for which were produced in the surrounding countryside. The town experienced three serious fires i ...
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Quoin (architecture)
Quoins ( or ) are masonry blocks at the corner of a wall. Some are structural, providing strength for a wall made with inferior stone or rubble, while others merely add aesthetic detail to a corner. According to one 19th century encyclopedia, these imply strength, permanence, and expense, all reinforcing the onlooker's sense of a structure's presence. Stone quoins are used on stone or brick buildings. Brick quoins may appear on brick buildings, extending from the facing brickwork in such a way as to give the appearance of generally uniformly cut ashlar blocks of stone larger than the bricks. Where quoins are decorative and non-load-bearing a wider variety of materials is used, including timber, stucco, or other cement render. Techniques Ashlar blocks In a traditional, often decorative use, large rectangular ashlar stone blocks or replicas are laid horizontally at the corners. This results in an alternate, quoining pattern. Alternate cornerstones Courses of large and small c ...
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Inferior Oolite
The Inferior Oolite is a sequence of Jurassic age sedimentary rocks in Europe. It was deposited during the Middle Jurassic.Weishampel, David B; et al. (2004). "Dinosaur distribution (Middle Jurassic, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 538–541. . The Inferior Oolite Group as more recently defined is a Jurassic lithostratigraphic group (a sequence of rock strata) in southern and eastern England . It has been variously known in the past as the Under Oolite (or Oolyte), the Inferior Oolite, the Inferior Oolite Series and the Redbourne Group. Outcrops The rocks are exposed from Dorset and Somerset eastwards and northwards through the English Midlands to Yorkshire. It is present at depth in the Wessex-Weald Basin, where it reaches its greatest thickness of 120 m. Lithology and stratigraphy The group consists of up to 120 m thickness of oolitic limestones and su ...
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Garantiana
''Garantiana'' is a genus of ammonites from the Bajocian In the geologic timescale, the Bajocian is an age and stage in the Middle Jurassic. It lasted from approximately 170.3 Ma to around 168.3 Ma (million years ago). The Bajocian Age succeeds the Aalenian Age and precedes the Bathonian Age. Stra ... stage at the beginning of the Middle Jurassic, included in the family Stephanoceratidae. Description ''Garantiana'' is strongly ribbed and generally evolute. The inner whorls are exposed in a wide and fairly deep umbilicus. Ribs arise at the umbilical margin and split in two (bifurcate) about midway up the sides and cross over the outer (ventral) rim. ''Garantiana'' was named by d'Orbigny, 1845. The type species is ''Garantiana garantiana'', which comes from France. Related genera include '' Orthogarantiana'' '' Pseudogarantiana'', and '' Strenoceras''. References External links ''Garantiana''in Hildoceras webpag''Garaniana''pictured in the Fossil Foru Jurassic ammon ...
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Middle Jurassic
The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 163.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations containing land animal fossils include the Forest Marble Formation in England, the Kilmaluag Formation in Scotland,British Geological Survey. 2011Stratigraphic framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf: research report RR/11/06 British Geological Survey, Keyworth, Nottingham. the Daohugou Beds in China, the Itat Formation in Russia, and the Isalo III Formation of western Madagascar. Paleogeography During the Middle Jurassic Epoch, Pangaea began to separate into Laurasia and Gondwana, and the Atlantic Ocean formed. Eastern Laurasia was tectonically active as the Cimmerian plate continued to collide with Laurasia's southern coast, completely closing the Paleo-Tethys Ocean. A subduction zone ...
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