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St Oswald's Church, Thornton In Lonsdale
St Oswald's Church is in the village of Thornton in Lonsdale, North Yorkshire, England. It is an active Anglican parish church in the deanery of Ewecross, the archdeaconry of Craven and the Diocese of Leeds. Its benefice is united with that of All Saints, Burton in Lonsdale. The church is recorded in the National Heritage List for England as a designated Grade II* listed building. History The tower dates from the 15th century. In 1868–70 the church, other than the tower and three Norman arches, was rebuilt in Perpendicular style by the Lancaster architects Paley and Austin. This cost £5,000 (equivalent to £ as of ), and was paid for from the will of Felix Slade, after whom the Slade School of Fine Art was named, and who had lived in a house nearby. The church was damaged by a fire in February 1933, and was rebuilt in 1934–35 by Austin and Paley at a cost of about £9,000. Architecture The church is constructed in limestone rubble with sandstone dressings, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thornton In Lonsdale
Thornton in Lonsdale is a village and civil parish in the Craven District and ceremonial county of North Yorkshire in England. It is very close to the border with Cumbria and Lancashire and is north of Ingleton and south-east of Kirkby Lonsdale, and has a population of 308, falling to 288 at the 2011 Census. Its main claims to fame are the Marton Arms pub and St Oswald's Church, Sir Arthur Conan Doyle married his first wife at this church in 1885 and held his reception at The Marton Arms before setting off to Ireland on honeymoon. Doyle's mother resided at nearby Masongill from 1882 to 1917. History In 1086 the ''Domesday Book'' listed on folio 301v under Craven ''Torntun & in Borch, Orm vi curactes ad geld.'' – that is in ''Thornton in Lonsdale with Burrow-with-Burrow Orm has circa 720 acres of plough-land to be taxed''. This manor belonged to Orm, one of the family of Norse Noblemen who held the most land in Northern England. All estates would also include g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lancaster, Lancashire
Lancaster (, ) is a city and the county town of Lancashire, England, standing on the River Lune. Its population of 52,234 compares with one of 138,375 in the wider City of Lancaster local government district. The House of Lancaster was a branch of the English royal family. The Duchy of Lancaster still holds large estates on behalf of Charles III, who is also Duke of Lancaster. Its long history is marked by Lancaster Castle, Lancaster Priory Church, Lancaster Cathedral and the Ashton Memorial. It is the seat of Lancaster University and has a campus of the University of Cumbria. The Port of Lancaster played a big role in the city's growth, but for many years the outport of Glasson Dock has become the main shipping facility. History The name of the city first appeared in the Domesday Book of 1086, as ''Loncastre'', where "Lon" refers to the River Lune and "castre" (from the Old English ''cæster'' and Latin ''castrum'' for "fort") to the Roman fort that stood on the site. Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aisle
An aisle is, in general, a space for walking with rows of non-walking spaces on both sides. Aisles with seating on both sides can be seen in airplanes, certain types of buildings, such as churches, cathedrals, synagogues, meeting halls, parliaments and legislatures, courtrooms, theatres, and in certain types of passenger vehicles. Their floors may be flat or, as in theatres, stepped upwards from a stage. Aisles can also be seen in shops, warehouses, and factories, where rather than seats, they have shelving to either side. In warehouses and factories, aisles may be defined by storage pallets, and in factories, aisles may separate work areas. In health club A health club (also known as a fitness club, fitness center, health spa, and commonly referred to as a gym) is a place that houses exercise equipment for the purpose of physical exercise. In recent years, the number of fitness and health se ...s, exercise equipment is normally arranged in aisles. Aisles are disti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nave
The nave () is the central part of a church, stretching from the (normally western) main entrance or rear wall, to the transepts, or in a church without transepts, to the chancel. When a church contains side aisles, as in a basilica-type building, the strict definition of the term "nave" is restricted to the central aisle. In a broader, more colloquial sense, the nave includes all areas available for the lay worshippers, including the side-aisles and transepts.Cram, Ralph Adams Nave The Catholic Encyclopedia. Vol. 10. New York: Robert Appleton Company, 1911. Accessed 13 July 2018 Either way, the nave is distinct from the area reserved for the choir and clergy. Description The nave extends from the entry—which may have a separate vestibule (the narthex)—to the chancel and may be flanked by lower side-aisles separated from the nave by an arcade. If the aisles are high and of a width comparable to the central nave, the structure is sometimes said to have three naves. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay (architecture)
In architecture, a bay is the space between architectural elements, or a recess or compartment. The term ''bay'' comes from Old French ''baie'', meaning an opening or hole."Bay" ''Online Etymology Dictionary''. http://www.etymonline.com/index.php?allowed_in_frame=0&search=bay&searchmode=none accessed 3/10/2014 __NOTOC__ Examples # The spaces between posts, columns, or buttresses in the length of a building, the division in the widths being called aisles. This meaning also applies to overhead vaults (between ribs), in a building using a vaulted structural system. For example, the Gothic architecture period's Chartres Cathedral has a nave (main interior space) that is '' "seven bays long." '' Similarly in timber framing a bay is the space between posts in the transverse direction of the building and aisles run longitudinally."Bay", n.3. def. 1-6 and "Bay", n.5 def 2. ''Oxford English Dictionary'' Second Edition on CD-ROM (v. 4.0) © Oxford University Press 2009 # Where there a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westmorland
Westmorland (, formerly also spelt ''Westmoreland'';R. Wilkinson The British Isles, Sheet The British IslesVision of Britain/ref> is a historic county in North West England spanning the southern Lake District and the northern Dales. It had an administrative function from the 12th century until 1974. Between 1974 and 2023 Westmorland lay within the administrative county of Cumbria. In April 2023, Cumbria County Council will be abolished and replaced with two unitary authorities, one of which, Westmorland and Furness, will cover all of Westmorland (as well as other areas), thereby restoring the Westmorland name to a top-tier administrative entity. The people of Westmorland are known as Westmerians. Early history Background At the beginning of the 10th century a large part of modern day Cumbria was part of the Kingdom of Strathclyde, and was known as '' "Scottish Cumberland" ''. The Rere Cross was ordered by Edmund I (r.939-946) to serve as a boundary marker between England an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rubble
Rubble is broken stone, of irregular size, shape and texture; undressed especially as a filling-in. Rubble naturally found in the soil is known also as 'brash' (compare cornbrash)."Rubble" def. 2., "Brash n. 2. def. 1. ''Oxford English Dictionary'' Second Edition on CD-ROM (v. 4.0) © Oxford University Press 2009 Where present, it becomes more noticeable when the land is ploughed or worked. Building "Rubble-work" is a name applied to several types of masonry. One kind, where the stones are loosely thrown together in a wall between boards and grouted with mortar almost like concrete, is called in Italian "muraglia di getto" and in French "bocage". In Pakistan, walls made of rubble and concrete, cast in a formwork, are called 'situ', which probably derives from Sanskrit (similar to the Latin 'in situ' meaning 'made on the spot'). Work executed with more or less large stones put together without any attempt at courses is called rubble walling. Where similar work is laid in cour ... [...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] |
Austin And Paley
Sharpe, Paley and Austin are the surnames of architects who practised in Lancaster, Lancashire, England, between 1835 and 1946, working either alone or in partnership. The full names of the principals in their practice, which went under various names during its life, are Edmund Sharpe (1809–77); Edward Graham Paley (1823–95), who practised as E. G. Paley; Hubert James Austin (1841–1915); Henry Anderson Paley (1859–1946), son of Edward, usually known as Harry Paley; and, for a very brief period, Geoffrey Langshaw Austin (1884–1971), son of Hubert. The firm's commissions were mainly for buildings in Lancashire and what is now Cumbria, but also in Yorkshire, Cheshire, the West Midlands, North Wales, and Hertfordshire. The practice specialised in work on churches; the design of new churches, restoring older churches, and making additions or alterations. They also designed country houses, and made alterations to existing houses. Almost all their churches w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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