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St Patrick's Church, Preston Patrick
St Patrick's Church is the parish church of Preston Patrick, Cumbria, England. It is an active Anglican church, one of eight parish churches served by the Kirkby Lonsdale Team Ministry. It is in the archdeaconry of Westmorland and Furness, and the diocese of Carlisle. The church is recorded in the National Heritage List for England as a designated Grade II listed building. History Until the 19th century, this locality was within the large rural parish of Heversham. However, there was a chapel on the site. In 1850 the Lancaster architects Edmund Sharpe and E. G. Paley reported that the chapel appeared, from its architectural design, to have been built during the reign of Henry VII (1457–1509). The architects designed a new church. Building started in 1852 and the new church opened on 28 November of that year. It cost about £1,400 (), and had seating for 1,386 people. In 1892 the chancel was rebuilt by Paley, Austin and Paley, the successors of Sharpe and ...
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Preston Patrick
Preston Patrick is a village and civil parish in South Lakeland, Cumbria, England. It has junction 36 of the M6 motorway in its south west corner and extends north east on both sides of the motorway until just beyond the B2564 road. In the 2001 census the parish had a population of 438, decreasing at the 2011 census to 426. It is set in the drumlin landscape south of Kendal. The neighbouring parishes are Old Hutton and Holmescales to the north, Lupton to the east, Beetham to the south and Preston Richard to the west. Buildings There are 27 buildings or structures in the parish which are listed. The building with the highest listing is Preston Patrick Hall which is Grade II* listed. It dates probably from the late 14th century, comprising the remains of a medieval tower house altered in the 17th century. It is now a private house. The other listed buildings, which include several milestones, are Grade II. The former primary school, built in 1775, closed in 1949 and is no ...
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Edmund Sharpe
Edmund Sharpe (31 October 1809 – 8 May 1877) was an English architect, architectural historian, railway engineer, and sanitary reformer. Born in Knutsford, Cheshire, he was educated first by his parents and then at schools locally and in Runcorn, Greenwich and Sedbergh. Following his graduation from Cambridge University he was awarded a travelling scholarship, enabling him to study architecture in Germany and southern France. In 1835 he established an architectural practice in Lancaster, initially working on his own. In 1845 he entered into partnership with Edward Paley, one of his pupils. Sharpe's main focus was on churches, and he was a pioneer in the use of terracotta as a structural material in church building, designing what were known as "pot" churches, the first of which was St Stephen and All Martyrs' Church, Lever Bridge. He also designed secular buildings, including residential buildings and schools, and worked on the development of railways in north-west ...
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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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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 ...
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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 ...
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English Gothic Architecture
English Gothic is an architectural style that flourished from the late 12th until the mid-17th century. The style was most prominently used in the construction of cathedrals and churches. Gothic architecture's defining features are pointed arches, rib vaults, buttresses, and extensive use of stained glass. Combined, these features allowed the creation of buildings of unprecedented height and grandeur, filled with light from large stained glass windows. Important examples include Westminster Abbey, Canterbury Cathedral and Salisbury Cathedral. The Gothic style endured in England much longer than in Continental Europe. The Gothic style was introduced from France, where the various elements had first been used together within a single building at the choir of the Abbey of Saint-Denis north of Paris, completed in 1144. The earliest large-scale applications of Gothic architecture in England were Canterbury Cathedral and Westminster Abbey. Many features of Gothic architecture ...
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Niche (architecture)
A niche (CanE, or ) in Classical architecture is an exedra or an apse that has been reduced in size, retaining the half-dome heading usual for an apse. Nero's Domus Aurea (AD 64–69) was the first semi-private dwelling that possessed rooms that were given richly varied floor plans, shaped with niches and exedrae; sheathed in dazzling polished white marble, such curved surfaces concentrated or dispersed the daylight. A is a very shallow niche, usually too shallow to contain statues, and may resemble a blind window (a window without openings) or sealed door. (Compare: blind arcade) The word derives from the Latin (), via the French . The Italian '' nicchio'' () may also be involved,OED, "Niche" as the traditional decoration for the top of a niche is a scallop shell, as in the illustration, hence also the alternative term of "conch" for a semi-dome, usually reserved for larger exedra. In Gothic architecture, a niche may be set within a tabernacle framing, like a richly de ...
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Coping (architecture)
Coping (from ''cope'', Latin ''capa'') is the capping or covering of a wall. A splayed or wedge coping is one that slopes in a single direction; a saddle coping slopes to either side of a central high point. A coping may be made of stone (capstone), brick, clay or terracotta, concrete or cast stone, tile, slate, wood, thatch, or various metals, including aluminum, copper, stainless steel, steel, and zinc. In all cases it should be weathered (have a slanted or curved top surface) to throw off the water. In Romanesque work, copings appeared plain and flat, and projected over the wall with a throating to form a drip. In later work a steep slope was given to the weathering (mainly on the outer side), and began at the top with an astragal; in the Decorated Gothic style there were two or three sets off; and in the later Perpendicular Gothic these assumed a wavy section, and the coping mouldings continued round the sides, as well as at top and bottom, mitring at the angles, as ...
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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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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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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. ...
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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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