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Llangadfan
Llangadfan is a small village in Powys, Wales, based in the community of Banwy. The village lies on the A458 between Foel and Llanerfyl, from Llanwddyn. Dyfnant Forest is located nearby. The village is said to be known for its country dances. Geography Llangadfan is a village (area of ) and a parish, which lies on the banks of the River Vyrnwy and extends into the Banwy River and Nant-yn-Eira stream. Llanfyllin railway station (now closed) is to its north-east and Llanfair is away to its east-south-east. The pub here is known as "Cann Office Hotel". Climate The lowest average temperature recorded is in January and the average maximum is during August. The average annual rainfall is with a maximum monthly average of in December and lowest average of in June. Notable landmarks Llangadfan is home to St Cadfan's church, a medieval church whose original features have been obscured by a 19th century restoration. The church was originally said to have been established by ...
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Banwy
Banwy is a community in northwest Montgomeryshire, Powys, Wales, named after the River Banwy and also called ''Banw'' in Welsh. The community with the villages of Llangadfan and Foel, also called Garthbeibio. It is a sparsely populated area centred on the village of Llangadfan and extending west for some 10 km to the boundary with Gwynedd. It is located along the upper River Banwy valley, on either side of the A458 road between Llanfair Caereinion and Mallwyd. The population according to the 2011 UK census was 605. In 2005, the population was 534. Abernodwydd Farmhouse, a wooden-framed farmhouse built in 1678 from the Llangadfan was reassembled at the St Fagans National Museum of History St Fagans National Museum of History ( ; cy, Sain Ffagan: Amgueddfa Werin Cymru, links=no), commonly referred to as St Fagans after the village where it is located, is an open-air museum in Cardiff chronicling the historical lifestyle, cultur .... Banwy was the site of Ffridd y Cast ...
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Dyfnant Forest
Dyfnant Forest is a remote forest in northeastern-central Powys, Wales. Location Dyfnant Forest lies to the west of the B4395 road, a road which stems north from the A458 road and is between the valleys of the Afon Twrch to the west and the Afon Efyrnwy to the east, north of the village of Llangadfan. It is described by Lonely Planet as being "where a well-signposted maze of forestry tracks culminates in one enormous hill before descending rather spectacularly toward Lake Vyrnwy" (five miles away). Dyfnant Forest has an area of located at the periphery of the Cambrian Mountains, just south of Lake Vyrnwy. Geography The original forest was planted by the Forestry Commission. It is approached from a country road from Llangadfan, which branches into a foot track. It is well served by of forest tracks. The forest tracks include the Rainbow Trails, which were established by a partnership between Forestry Commission Wales and the Dyfnant and Fyrnwy Horse Riders' & Carriage Driv ...
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Saint Cadfan
Saint Cadfan ( la, Catamanus), sometimes Anglicized as Gideon, was the 6th century founder-abbot of Tywyn (whose church is dedicated to him) and Bardsey, both in Gwynedd, Wales. He was said to have received the island of Bardsey from Saint Einion Frenin, king of Llŷn, around 516 and to have served as its abbot until 542. Life and legacy Most of the information we have about Cadfan is from the awdl by Llywelyn the Bard in the 12th century. According to this he sailed from Brittany to Tywyn with 12 other saints, although some suggest that they came instead from Llanilltud Fawr. A Breton nobleman, he was said to be the son of Eneas Ledewig (Aeneas of Brittany) and Gwen Teirbron (Gwen Three Breasts), daughter of Budic II of Brittany. He journeyed to Britain accompanied by the children of Ithel Hael o Lydaw (of Brittany): Baglan, Flewyn, Gredifael, Tanwg, Twrog, Tegai, Trillo, Tecwyn and Llechid. Other reputed followers include Maël and Ilar. Wade-Evans thought ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Chancel
In church architecture, the chancel is the space around the altar, including the choir and the sanctuary (sometimes called the presbytery), at the liturgical east end of a traditional Christian church building. It may terminate in an apse. Overview The chancel is generally the area used by the clergy and choir during worship, while the congregation is in the nave. Direct access may be provided by a priest's door, usually on the south side of the church. This is one definition, sometimes called the "strict" one; in practice in churches where the eastern end contains other elements such as an ambulatory and side chapels, these are also often counted as part of the chancel, especially when discussing architecture. In smaller churches, where the altar is backed by the outside east wall and there is no distinct choir, the chancel and sanctuary may be the same area. In churches with a retroquire area behind the altar, this may only be included in the broader definition of chancel. I ...
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Vestry
A vestry was a committee for the local secular and ecclesiastical government for a parish in England, Wales and some English colonies which originally met in the vestry or sacristy of the parish church, and consequently became known colloquially as the "vestry". Overview For many centuries, in the absence of any other authority (which there would be in an incorporated city or town), the vestries were the sole ''de facto'' local government in most of the country, and presided over local, communal fundraising and expenditure until the mid or late 19th century using local established Church chairmanship. They were concerned for the spiritual but also the temporal as well as physical welfare of parishioners and its parish amenities, collecting local rates or taxes and taking responsibility for numerous functions such as the care of the poor, the maintaining of roads, and law enforcement, etc. More punitive matters were dealt with by the manorial court and hundred court, and latter ...
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Chancel Arch
In church architecture, the chancel is the space around the altar, including the choir and the sanctuary (sometimes called the presbytery), at the liturgical east end of a traditional Christian church building. It may terminate in an apse. Overview The chancel is generally the area used by the clergy and choir during worship, while the congregation is in the nave. Direct access may be provided by a priest's door, usually on the south side of the church. This is one definition, sometimes called the "strict" one; in practice in churches where the eastern end contains other elements such as an ambulatory and side chapels, these are also often counted as part of the chancel, especially when discussing architecture. In smaller churches, where the altar is backed by the outside east wall and there is no distinct choir, the chancel and sanctuary may be the same area. In churches with a retroquire area behind the altar, this may only be included in the broader definition of chancel. In ...
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Stoup
A holy water font or stoup is a vessel containing holy water which is generally placed near the entrance of a church. It is often placed at the base of a crucifix or religious representation. It is used in the Catholic Church, Anglican Churches, and some Lutheran churches to make the Sign of the Cross using the holy water upon entrance of the church. Holy water is blessed by a priest or a deacon, and many Christians believe it to be a reminder of the baptismal promises. See also *Baptismal font *''Nipson anomemata me monan opsin'' *Home stoup A home stoup is a small stoup with a small bowl and a decorated plaque that Christians in the Roman Catholic, Anglican and Lutheran traditions, hang inside homes, either at the house's entrance or, more commonly, on a bedroom wall at the head of ..., for usage and blessing at home References External links"Holy Water Fonts" Catholic Encyclopedia article
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Powys
Powys (; ) is a Local government in Wales#Principal areas, county and Preserved counties of Wales, preserved county in Wales. It is named after the Kingdom of Powys which was a Welsh succession of states, successor state, petty kingdom and principality that emerged during the Middle Ages following the end of Roman rule in Britain. Geography Powys covers the historic counties of Montgomeryshire and Radnorshire, most of Brecknockshire, and part of Denbighshire (historic), historic Denbighshire. With an area of about , it is now the largest administrative area in Wales by land and area (Dyfed was until 1996 before several Preserved counties of Wales, former counties created by the Local Government Act 1972 were abolished). It is bounded to the north by Gwynedd, Denbighshire and Wrexham County Borough; to the west by Ceredigion and Carmarthenshire; to the east by Shropshire and Herefordshire; and to the south by Rhondda Cynon Taf, Merthyr Tydfil County Borough, Caerphilly County Bor ...
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Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, pp.381-382 Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock ( clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined a ...
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Montgomeryshire
Montgomeryshire, also known as ''Maldwyn'' ( cy, Sir Drefaldwyn meaning "the Shire of Baldwin's town"), is one of thirteen historic counties of Wales, historic counties and a former administrative county of Wales. It is named after its county town, Montgomery, Powys, Montgomery, which in turn is named after one of William the Conqueror's main counsellors, Roger de Montgomerie, 1st Earl of Shrewsbury, Roger de Montgomerie, who was the 1st Earl of Shrewsbury. Montgomeryshire today constitutes the northern part of the Subdivisions of Wales#Principal areas of Wales, principal area of Powys. The population of Montgomeryshire was 63,779 according to the United Kingdom Census 2011, 2011 census, with a low population density of just 75 people per square mile (29 people per square km). The current area is 2,174 square km (839 square miles). The largest town is Newtown, Powys, Newtown, followed by Welshpool and Llanidloes. History The Treaty of Montgomery was signed on 29 September 1267, ...
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ...
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