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Stoke Sub Hamdon Priory
Stoke sub Hamdon Priory is a complex of buildings and ruins which initially formed a 14th-century college for the chantry chapel of St Nicholas, and later was the site of a farm in Stoke-sub-Hamdon, Somerset, England. The only building remaining from the college is a great hall and attached dwelling, dating from the late 15th century. The hall is designated by English Heritage as a Grade I listed building, while the outbuildings and gateway are Grade II listed. The whole site has been scheduled as an ancient monument. A number of the farm buildings are in poor condition, and have been added to the Heritage at Risk Register. The college was formed in 1304 as a chantry college, funded by John de Beauchamp, 1st Baron Beauchamp to serve the free chapel in his nearby manor house. Over the following 150 years, the college fell into disrepair and was rebuilt around 1460. During the dissolution, the land passed into the laity, and was a tenanted farm until the middle of the 20th centu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stoke-sub-Hamdon
Stoke-sub-Hamdon (or Stoke sub Hamdon), also known as Stoke under Ham, is a large village and civil parish in the South Somerset district of Somerset, England. It is situated west of Yeovil, with which it is linked by the A3088 road. The parish is located near the River Parrett, and includes the village of East Stoke. History The village stretches around Ham Hill which is a geological Site of Special Scientific Interest (SSSI), Iron Age hill fort, Roman site and country park. The hill has given its name to the distinctive quarried hamstone which is quarried from a ridge of sandy limestone rock that is elevated above the lower lying clay vales and nearby Somerset Levels. It is of particular importance to geologists because of the assemblages of fossils which it contains, the sedimentary features which it displays and the way it relates to other rocks of equivalent age in the close vicinity. The Bronze Age and Iron Age hill fort was occupied by the Durotriges tribe. A Roman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wells, Somerset
Wells () is a cathedral city and civil parish in the Mendip district of Somerset, located on the southern edge of the Mendip Hills, south-east of Weston-super-Mare, south-west of Bath and south of Bristol. Although the population recorded in the 2011 census was only 10,536, (increased to 12,000 by 2018) and with a built-up area of just , Wells has had city status since medieval times, because of the presence of Wells Cathedral. Often described as England's smallest city, it is actually second smallest to the City of London in area and population, but unlike London it is not part of a larger urban agglomeration. Wells takes its name from three wells dedicated to Saint Andrew, one in the market place and two within the grounds of the Bishop's Palace and cathedral. A small Roman settlement surrounded them, which grew in importance and size under the Anglo-Saxons when King Ine of Wessex founded a minster church there in 704. The community became a trading centre based on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thatching
Thatching is the craft of building a roof with dry vegetation such as straw, water reed, sedge (''Cladium mariscus''), rushes, heather, or palm branches, layering the vegetation so as to shed water away from the inner roof. Since the bulk of the vegetation stays dry and is densely packed—trapping air—thatching also functions as insulation. It is a very old roofing method and has been used in both tropical and temperate climates. Thatch is still employed by builders in developing countries, usually with low-cost local vegetation. By contrast, in some developed countries it is the choice of some affluent people who desire a rustic look for their home, would like a more ecologically friendly roof, or who have purchased an originally thatched abode. History Thatching methods have traditionally been passed down from generation to generation, and numerous descriptions of the materials and methods used in Europe over the past three centuries survive in archives and early publica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buttress
A buttress is an architectural structure built against or projecting from a wall which serves to support or reinforce the wall. Buttresses are fairly common on more ancient buildings, as a means of providing support to act against the lateral (sideways) forces arising out of inadequately braced roof structures. The term ''counterfort'' can be synonymous with buttress and is often used when referring to dams, retaining walls and other structures holding back earth. Early examples of buttresses are found on the Eanna Temple (ancient Uruk), dating to as early as the 4th millennium BC. Terminology In addition to flying and ordinary buttresses, brick and masonry buttresses that support wall corners can be classified according to their ground plan. A clasping or clamped buttress has an L shaped ground plan surrounding the corner, an angled buttress has two buttresses meeting at the corner, a setback buttress is similar to an angled buttress but the buttresses are set back from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ham Hill, Somerset
Ham Hill is a geological Site of Special Scientific Interest (SSSI), Scheduled Ancient Monument, Iron Age hill fort, Roman site, Local Nature Reserve and country park, to the west of Yeovil in Somerset, England. The hill has given its name to the distinctive quarried hamstone and also to two nearby villages: Stoke-sub-Hamdon and Norton Sub Hamdon, whose names mean "under-Ham-hill" (where "Ham" is Old English for a small settlement). The Mendip Hills, Blackdown Hills, Quantock Hills and Dorset Downs are all visible from Ham Hill, especially from its war memorial. It is popular for picnicking, walking and mountain biking in the grassy hollows of the old quarry workings. The geology supports a wide range of fauna including mammals, birds, invertebrates, reptiles and amphibians living on lichens, fungi, ferns and flowering plants. Geology The hill is part of a ridge of sandy limestone rock which is elevated above the lower lying clay vales and nearby Somerset Levels. The sedim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamstone
Hamstone is the name given to a honey-coloured building stone from Ham Hill, Somerset, England. It is a well-cemented medium to coarse grained limestone characterised by marked bedding planes of clay inclusions and less well-cemented material which weather differentially to give exposed blocks a characteristic furrowed appearance. In origin, Hamstone is a Jurassic limestone from the Toarcian, or Upper Lias, stage. History In the 19th century there were 24 small quarries operating on Ham Hill employing some 200 men. In later Victorian times industrial quarrying expanded significantly, with upwards of 200 small family-run quarries and masonry businesses operating on site. Modern quarrying Today hamstone is quarried in only two areas of Ham Hill. The North quarry, run by Ham & Doulting Stone, extracts stone from just beneath the surface and is the longest running hamstone quarry in existence. The Norton or South quarry, run by Harvey Stone, extracts its stone from some 20–3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Priory Gateway - Stoke Sub Hamdon - Geograph
A priory is a monastery of men or women under religious vows that is headed by a prior or prioress. Priories may be houses of mendicant friars or nuns (such as the Dominicans, Augustinians, Franciscans, and Carmelites), or monasteries of monks or nuns (as with the Benedictines). Houses of canons regular and canonesses regular also use this term, the alternative being "canonry". In pre-Reformation England, if an abbey church was raised to cathedral status, the abbey became a cathedral priory. The bishop, in effect, took the place of the abbot, and the monastery itself was headed by a prior. History Priories first came to existence as subsidiaries to the Abbey of Cluny. Many new houses were formed that were all subservient to the abbey of Cluny and called Priories. As such, the priory came to represent the Benedictine ideals espoused by the Cluniac reforms as smaller, lesser houses of Benedictines of Cluny. There were likewise many conventual priories in Germany and Italy dur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Monument
In British law, an ancient monument is an early historical structure or monument (e.g. an archaeological site) worthy of preservation and study due to archaeological or heritage interest. The '' Ancient Monuments and Archaeological Areas Act 1979'' classified ancient monuments as "scheduled monuments" or monuments that are considered by the Secretary of State of archaeological, historical or artistic importance. In addition, the term "ancient monument" can also refer to any early or historical manmade structure and/or architecture. Certain ancient monuments are of cultural importance for nations and become symbols of international recognition, including the ruins of Baalbek on Lebanese currency, the Angkor Wat on Cambodian currency and the Great Wall of China on the Chinese currency. There are some countries that display ancient buildings as symbols on their coats of arms as a way to affirm national identity. In this way, ancient monuments in the modern world are used as icons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Church Of St Mary The Virgin, East Stoke
The Church of St Mary the Virgin at East Stoke in Stoke-sub-Hamdon, Somerset, England dates from the 12th century. It has been designated as a Grade I listed building. It was previously dedicated to Saint Denis. Much of the church, including the nave and chancel with their stone carving are Norman, the structure being supported by pilaster buttresses. The north transept was added about 1225 and the south transept about 1300. The church has a tower with six bells. It shows various medieval carving including abstract corbels, an astrological tympanum, and St Michael slaying the dragon. Two of the carvings are thought to be Sheela na Gigs. The upper part of the tower was built in the 13th century with the parapet being added in the 15th. The church was restored in 1862, by Benjamin Ferrey. The parish is within the benefice of Stoke-sub-Hamdon, which is part of the Wells archdeaconry. Two of the Grade II* listed 17th-century monuments in the churchyard have suffered from su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapel Of Ease
A chapel of ease (or chapel-of-ease) is a church architecture, church building other than the parish church, built within the bounds of a parish for the attendance of those who cannot reach the parish church conveniently. Often a chapel of ease is deliberately built as such, being more accessible to some parishioners than the main church. Such a chapel may exist, for example, when a parish covers several dispersed villages, or a central village together with its satellite hamlet (place), hamlet or hamlets. In such a case the parish church will be in the main settlement, with one or more chapels of ease in the subordinate village(s) and/or hamlet(s). An example is the chapel belonging to All_Hallows_Church,_South_River, All Hallows' Parish in Maryland, US; the chapel was built in Davidsonville, Maryland, Davidsonville from 1860 to 1865 because the parish's "Brick Church" in South River was too far away at distant. A more extreme example is the Chapel-of-Ease built in 1818 on St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
