John Norton (architect)
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John Norton (architect)
John Norton (28 September 1823 – 10 November 1904) was an English architect who designed country houses, churches and a number of commercial buildings. Early life Norton was born and educated in Bristol. He became the pupil of architect Benjamin Ferrey (1810–80) in 1846. Ferrey was an early member of the Royal Institute of British Architects and a close friend of the designer Augustus Pugin (1812–52), who took his inspiration from the Gothic medieval styles of the pre-Reformation era. Ferrey's association with Pugin had a profound effect upon Norton, who adopted Pugin's principles and Christian moral dimensions in his own subsequent designs for church architecture. The vital tenets of Pugin's and thus Norton's creed were centred on the revival of the pointed structure of the Gothic arch. It was argued that only this construction truly symbolised Christian striving towards heaven and Christ's resurrection, Classical architecture having been based on pagan temples. Further ...
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Country House
An English country house is a large house or mansion in the English countryside. Such houses were often owned by individuals who also owned a town house. This allowed them to spend time in the country and in the city—hence, for these people, the term distinguished between town and country. However, the term also encompasses houses that were, and often still are, the full-time residence for the landed gentry who ruled rural Britain until the Reform Act 1832. Frequently, the formal business of the counties was transacted in these country houses, having functional antecedents in manor houses. With large numbers of indoor and outdoor staff, country houses were important as places of employment for many rural communities. In turn, until the agricultural depressions of the 1870s, the estates, of which country houses were the hub, provided their owners with incomes. However, the late 19th and early 20th centuries were the swansong of the traditional English country house lifest ...
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Bath Stone
Bath Stone is an oolitic limestone comprising granular fragments of calcium carbonate. Originally obtained from the Combe Down and Bathampton Down Mines under Combe Down, Somerset, England. Its honey colouring gives the World Heritage City of Bath, England its distinctive appearance. An important feature of Bath Stone is that it is a ' freestone', so-called because it can be sawn or 'squared up' in any direction, unlike other rocks such as slate, which form distinct layers. Bath Stone has been used extensively as a building material throughout southern England, for churches, houses, and public buildings such as railway stations. Some quarries are still in use, but the majority have been converted to other purposes or are being filled in. Geological formation Bath Stone is an oolitic limestone comprising granular fragments of calcium carbonate laid down during the Jurassic Period (195 to 135 million years ago) when the region that is now Bath was under a shallow sea. Layer ...
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The Crystal Palace
The Crystal Palace was a cast iron and plate glass structure, originally built in Hyde Park, London, Hyde Park, London, to house the Great Exhibition of 1851. The exhibition took place from 1 May to 15 October 1851, and more than 14,000 exhibitors from around the world gathered in its exhibition space to display examples of technology developed in the Industrial Revolution. Designed by Joseph Paxton, the Great Exhibition building was long, with an interior height of , and was three times the size of St Paul's Cathedral. The introduction of the sheet glass method into Britain by Chance Brothers in 1832 made possible the production of large sheets of cheap but strong glass, and its use in the Crystal Palace created a structure with the greatest area of glass ever seen in a building. It astonished visitors with its clear walls and ceilings that did not require interior lights. It has been suggested that the name of the building resulted from a piece penned by the playwright Doug ...
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Sydenham, London
Sydenham () is a district of south-east London, England, which is shared between the London boroughs of London Borough of Lewisham, Lewisham, London Borough of Bromley, Bromley and London Borough of Southwark, Southwark. Prior to the creation of the County of London in 1889, Sydenham was located in Kent, bordering Surrey. Historically, the area was very affluent, with the Crystal Palace being relocated to Sydenham Hill in 1854. Today, Sydenham is a diverse area, with a population of 28,378 (2011 census) and borders Forest Hill, London, Forest Hill, Dulwich, Crystal Palace, London, Crystal Palace, Penge, Beckenham, Catford and Bellingham, London, Bellingham. History Originally known as Shippenham, Sydenham began as a small settlement, a few cottages among the woods, whose inhabitants grazed their animals and collected wood. In the 1640s, springs of water in what is now Sydenham Wells Park, Wells Park were discovered to have medicinal properties, attracting crowds of people to the ...
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Crystal Palace Road
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification. The word ''crystal'' derives from the Ancient Greek word (), meaning both "ice" and "rock crystal", from (), "icy cold, frost". Examples of large crystals include snowflakes, diamonds, and table salt. Most inorganic solids are not crystals but polycrystals, i.e. many microscopic crystals fused together into a single solid. Polycrystals include most metals, rocks, ceramics, and ice. A third category of sol ...
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Somerton, Somerset
Somerton ( ) is a town and civil parish in the English county of Somerset. It gave its name to the county and was briefly, around the start of the 14th century, the county town, and around 900 was possibly the capital of Wessex. It has held a weekly market since the Middle Ages, and the main square with its market cross is today popular with visitors. Situated on the River Cary, approximately north-west of Yeovil, Somerton has its own town council serving a population of 4,697 as of 2011. Residents are often referred to locally as Somertonians. The civil parish includes the hamlets of Etsome, Hurcot, Catsgore, and Catcombe. Archaeological remains at Somerton are evidence of a Celtic settlement. The discovery of a high status cemetery in 2019, suggests that these local people adopted a more Roman lifestyle. During the Anglo-Saxon era, Somerton was an important political and commercial centre. After the Norman conquest of England the importance of the town declined, despite bei ...
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Jurassic Limestone
The Jurassic ( ) is a geologic period The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronol ... 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 ...
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Blue Lias
The Blue Lias is a geological formation in southern, eastern and western England and parts of South Wales, part of the Lias Group. The Blue Lias consists of a sequence of limestone and shale layers, laid down in latest Triassic and early Jurassic times, between 195 and 200 million years ago. The Blue Lias is famous for its fossils, especially ammonites. Its age corresponds to the Rhaetian to lower Sinemurian stages of the geological timescale, thus fully including the Hettangian stage. It is the lowest of the three divisions of the Lower Jurassic period and, as such, is also given the name ''Lower Lias''. Stratigraphically it can be subdivided into three members: the Wilmcote Limestone, Saltford Shale and Rugby Limestone. Lithology and facies The Blue Lias comprises decimetre scale alternations of argillaceous limestone and mudstone. These alternations are caused by short-term climatic variations during the Early Jurassic attributed to orbital forcing (Milankovitch cycles). Th ...
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Walton, Somerset
Walton is a village and civil parish, on the Polden Hills, west of Street in the Mendip district of Somerset, England. The parish includes the hamlet of Asney. History Saxon pressure seems to have driven the Britons from the immediate area around 650 A.D. About 700 A.D. the former Celtic monastery at Glastonbury was revived under royal Saxon patronage. By about 740 A.D. the general lines of parish boundaries in this area seem to have been fixed. This early development may well have been due to the organising urges of the monastic authorities. The parish of Walton was part of the Whitley Hundred, which took its name from Whitley Wood in the parish. The name Walton comes from settlement/farmstead of Wealas — native Celts which is what the new Anglo Saxon speaking peoples called the native inhabitants of England. There is strong evidence that in many areas of England taken over by Germanic speaking settlers, the native British (Wealas) remained undisturbed, farming the same ...
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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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Bath, Somerset
Bath () is a city in the Bath and North East Somerset unitary area in the county of Somerset, England, known for and named after its Roman-built baths. At the 2021 Census, the population was 101,557. Bath is in the valley of the River Avon, west of London and southeast of Bristol. The city became a World Heritage Site in 1987, and was later added to the transnational World Heritage Site known as the "Great Spa Towns of Europe" in 2021. Bath is also the largest city and settlement in Somerset. The city became a spa with the Latin name ' ("the waters of Sulis") 60 AD when the Romans built baths and a temple in the valley of the River Avon, although hot springs were known even before then. Bath Abbey was founded in the 7th century and became a religious centre; the building was rebuilt in the 12th and 16th centuries. In the 17th century, claims were made for the curative properties of water from the springs, and Bath became popular as a spa town in the Georgian era. ...
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