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Rawden Brandesby
Brandsby is a village in North Yorkshire, England. The village is the main constituent of the Brandsby-cum-Stearsby Civil Parish in the District of Hambleton. The village is mentioned in the ''Domesday book''. It lies between Easingwold and Hovingham, some north of York. History The village toponymy is of Scandinavian origin named after a Norseman called Brand and the suffix of ''by'' meaning settlement or habitation. At the time of the Norman conquest, it was held by Cnut, son of Karli and afterwards by Hugh, son of Baldric. Later the village and the surrounding lands were given to Baron Roger de Mowbray. It was part of the Bulford Hundred. The Baron left the lordship of the manor to Nicholas de Riparia (or de le Ryver), whose family held it until the reign of Queen Elizabeth I. After this the lordship passed via marriage to the Cholmeley family, descended from the Cholmondeley family of Cheshire. They provided a long lineage of Brandsby squires but, unfortunately, few recor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hambleton District
Hambleton is a local government district in North Yorkshire, England. The administrative centre is Northallerton, and the district includes the outlying towns and villages of Bedale, Thirsk, Great Ayton, Stokesley, and Easingwold. The district was formed by the Local Government Act 1972 on 1 April 1974, as a merger of Northallerton Urban District, Bedale Rural District, Easingwold Rural District, Northallerton Rural District, and parts of Thirsk Rural District, Stokesley Rural District and Croft Rural District, all in the North Riding of Yorkshire. Geography Hambleton covers an area of 1,311.17 km² most of which, 1,254.90 km², is green space. The district is named after the Hambleton Hills, part of the North York Moors National Park, on the eastern edge of the district. This area is the subject of a national habitat protection scheme as articulated in the United Kingdom's Biodiversity Action Plan. About 75% of the district lies in the Vales of Mowbray and of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stillington, North Yorkshire
Stillington is a village and civil parish in the Hambleton district of North Yorkshire, England. It lies on the York to Helmsley road about north of York. Stillington Mill was the endpoint of the Foss Navigation Act of 1793. History The village is mentioned in the ''Domesday Book'' as ''Stivelincton'' in the ''Bulford hundred''. The lordship of the manor was in the possession of the ''Archbishop of York St Peter'' at the time of the Norman invasion and remained so afterwards. The church continued to hold the land until 1616, when it was leased to a ''William Ramsden''. The lease was then granted to ''Christopher Croft'' in 1625. During the first year of the Commonwealth, many church lands were put up for sale and Croft purchased the manor outright. Following the Restoration, Christopher Croft, son of the former, sought a grant from the church for the manor when many church lands were being reclaimed. He was Lord Mayor of York at the time and was knighted soon after. The Cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fred Rowntree
Frederick (Fred) Rowntree (19 April 1860 Scarborough – 7 January 1927 Hammersmith) was an Arts and Crafts architect. Life and career Rowntree was the son of John Rowntree, a master grocer and Ann Webster. His brother, John Rowntree, traded in tea and coffee. The Rowntree family were Quakers and related to Rowntree's, the well-known confectioners. Fred was a scholar at Bootham School in York, and was articled to Charles Augustus Bury of Scarborough from 1876 to 1880. He became an assistant to Edward Burgess in London and was appointed a clerk of works in Leicestershire, ending in 1885 when joined Charles Edeson of Scarborough, the company name changing to ''Edeson & Rowntree''. On 6 October 1886 Rowntree married Mary Anna Gray (10 June 1862 - 19 July 1933), a daughter of William Gray of the biscuit manufacturers Gray, Dunn & Company, who were also Quakers. They raised a family of 5 children. He located to London in 1890, and also entered into partnership with Malcolm Star ... [...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] |
Temple Lushington Moore
Temple Lushington Moore (7 June 1856 – 30 June 1920) was an English architect who practised in London. He is famed for a series of fine Gothic Revival churches built between about 1890 and 1917 and also restored many churches and designed church fittings. He did some work on domestic properties, and also designed memorial crosses. Life and career Temple Moore was born in Tullamore, County Offaly, Ireland, and was the son of an army officer. He was educated at Glasgow High School, then from 1872 privately by the Revd Richard Wilton in Londesborough in the East Riding of Yorkshire. In 1875, he moved to London and was articled to architect George Gilbert Scott, Jr. Although Moore set up his own practice in 1878, he continued to work closely with Scott, helping to complete his works when Scott's health deteriorated. From the early 1880s he travelled widely studying buildings on the continent, chiefly in Germany, France and Belgium. He was particularly impressed by the grea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thomas Atkinson (architect)
Thomas Atkinson (1729–1798) was an English architect, best remembered for remodelling Bishopthorpe Palace in the Gothic Revival style. Life Atkinson was born at York, the son of Thomas and Jane Marshall Atkinson. His father was a mason. He worked with his father and later developed an architectural practice based in York. The house that he built there for himself in about 1780 still stands at 20 St Andrewgate in the city centre. He was the leading Yorkshire-based architect of the second half of the 18th century. Atkinson converted to Roman Catholicism; he received a number of commissions from the Yorkshire Catholic gentry. He was commissioned to design a new chapel for Bar Convent. The dome was concealed beneath a slate roof, so that it was hidden from view. Atkinson also built eight different escape routes into the Chapel, to ensure that if the building was stormed, the worshippers would be able to escape. In 1776, he produced designs for a planned development of the city o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
All Saints Church, Brandsby - Geograph
All or ALL may refer to: Language * All, an indefinite pronoun in English * All, one of the English determiners * Allar language (ISO 639-3 code) * Allative case (abbreviated ALL) Music * All (band), an American punk rock band * ''All'' (All album), 1999 * ''All'' (Descendents album) or the title song, 1987 * ''All'' (Horace Silver album) or the title song, 1972 * ''All'' (Yann Tiersen album), 2019 * "All" (song), by Patricia Bredin, representing the UK at Eurovision 1957 * "All (I Ever Want)", a song by Alexander Klaws, 2005 * "All", a song by Collective Soul from ''Hints Allegations and Things Left Unsaid'', 1994 Science and mathematics * ALL (complexity), the class of all decision problems in computability and complexity theory * Acute lymphoblastic leukemia * Anterolateral ligament Sports * American Lacrosse League * Arena Lacrosse League, Canada * Australian Lacrosse League Other uses * All, Missouri, a community in the United States * All, a brand of Sun Products * A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northallerton
Northallerton ( ) is a market town and civil parish in the Hambleton District of North Yorkshire, England. It lies in the Vale of Mowbray and at the northern end of the Vale of York. It had a population of 16,832 in the 2011 census, an increase from 15,741 in 2001. It has served as the county town of the North Riding of Yorkshire and, since 1974, of North Yorkshire. Northallerton is made up of four wards: North, Broomfield, Romanby and Central. There has been a settlement at Northallerton since Roman times; however its growth in importance began in the 11th century when King William II gifted land to the Bishop of Durham. Under the Bishop's authority Northallerton became an important religious centre. Later, it was a focus for much conflict between the English and the Scots, most notably the Battle of the Standard, fought nearby in 1138, which saw losses of as many as 12,000 men. In later years trade and transport became more important. The surrounding area was discovere ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oolite
Oolite or oölite (''egg stone'') is a sedimentary rock formed from ooids, spherical grains composed of concentric layers. The name derives from the Ancient Greek word for egg (ᾠόν). Strictly, oolites consist of ooids of diameter 0.25–2 millimetres; rocks composed of ooids larger than 2 mm are called pisolites. The term ''oolith'' can refer to oolite or individual ooids. Composition Ooids are most commonly composed of calcium carbonate ( calcite or aragonite), but can be composed of phosphate, clays, chert, dolomite or iron minerals, including hematite. Dolomitic and chert ooids are most likely the result of the replacement of the original texture in limestone. Oolitic hematite occurs at Red Mountain near Birmingham, Alabama, along with oolitic limestone. They are usually formed in warm, supersaturated, shallow, highly agitated marine water intertidal environments, though some are formed in inland lakes. The mechanism of formation starts with a small fragment of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lias Group
The Lias Group or Lias is a lithostratigraphic unit (a sequence of rock strata) found in a large area of western Europe, including the British Isles, the North Sea, the Low Countries and the north of Germany. It consists of marine limestones, shales, marls and clays. ''Lias'' is a Middle English term for hard limestone, used in this specific sense by geologists since 1833. In the past, geologists used ''Lias'' not only for the sequence of rock layers, but also for the timespan during which they were formed. It was thus an alternative name for the Early Jurassic epoch of the geologic timescale. It is now more specifically known that the Lias is Rhaetian to Toarcian in age (over a period of 20 million years between ) and thus also includes a part of the Triassic. The use of the name "Lias" for a unit of time is therefore slowly disappearing. Subdivisions In southern England, the Lias Group is often divided into Lower, Middle and Upper subgroups. In Southern England the Lias is d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
