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Brandsby
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 reco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brandsby-type Ware
Brandsby-type Ware is a type of Medieval ceramic produced in Brandsby, North Yorkshire, England, in the 13th and 14th centuries AD.Jennings, S. 1992. ''Medieval Pottery in the Yorkshire Museum'', York, 18–21. Production zone Brandsby-type ware production is centred on the village of Brandsby, North Yorkshire,Mainman, A. and Jenner, A. 2013. ''Medieval Pottery from York'' (Archaeology of York 16/9), York, 1230–1245. 22 km from York but is presumed to have been made in a number of villages to the north of York. Fabric Brandsby-type ware is a lightly gritted fabric, generally oxidised to white, pink, pale brown, or reddish-yellow and sometimes with a grey core.Brooks, C.M. 1987. ''Medieval and Later Pottery from Aldwark and Other Sites'', York, 153–154. They are generally finer and sandier, and usually more hard-fired than the earlier and comparable York Glazed Ware. Form and decoration The main form produced from Brandsby-type ware is the jug (or baluster jug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brandsby-cum-Stearsby
Brandsby-cum-Stearsby is a civil parish in the Hambleton district of North Yorkshire, England, with a population of 234 (2001 census), increasing to 383 at the 2011 Census and including Dalby-cum-Skewsby and Yearsley. It includes the villages of Brandsby (which has a separate article) and Stearsby. There are five scheduled ancient monuments in the parish, all round barrow A round barrow is a type of tumulus and is one of the most common types of archaeological monuments. Although concentrated in Europe, they are found in many parts of the world, probably because of their simple construction and universal purpose. ...s: * Round barrow 300m south of Barhouse Farm at * Round barrow 450m north-east of Hagg Farm * Round barrow 300m east of Warren House * Round barrow 150m south of Warren House * Round barrow 300m west of Quarry House References Civil parishes in North Yorkshire {{Hambleton-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Foss
The River Foss is in North Yorkshire, England. It is a tributary of the River Ouse. It rises in the Foss Crooks Woods near Oulston Reservoir close to the village of Yearsley and runs south through the Vale of York to the Ouse in the centre of York. The name most likely comes from the Latin word Fossa, meaning ditch. It is mentioned in the ''Domesday Book''. The York district was settled by Norwegian and Danish people, so parts of the place names could be old Norse. Referring to the etymological dictionary "Etymologisk ordbog", dealing with the common Danish and Norwegian languages – roots of words and the original meaning. The old Norse word ''Fos'' (waterfall) meaning impetuous. The River Foss was dammed, and even though the elevation to the River Ouse is small, a waterfall was formed. This may have led to the name ''Fos'' which became Foss. The responsibility for the management of the river's drainage area is the Foss Internal drainage board (IDB). It has responsibility fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crayke
Crayke is a village and civil parish in the Hambleton District of North Yorkshire, England, about east of Easingwold. Etymology The name ''Crayke'' is of Brittonic origin, derived from the neo-Brittonic Cumbric ''crẹ:g'', meaning "a crag" or "prominent rock" (Welsh ''craig''). This derivation may refer to the topography associated with the Northumbrian monastery at Crayke. History There is evidence that there has been a settlement here since the times of the seven Anglo-Saxon kingdoms. The village is named in the ''Domesday Book'' as ''Crec'', part of the ''Yarlestre'' hundred and noted as belonging to the Bishop of Durham. The parish was formerly a detached part of County Durham (until 1844), due to its connection with St Cuthbert and the Diocese of Durham, which owned Crayke Castle. The seventh-century king Egfrid granted Crayke to the church in 685 to be used by Cuthbert on his visits to York, to which end Cuthbert founded a monastery here. Cuthbert died in 687AD. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yearsley
Yearsley is a small village and civil parish in the district of Hambleton in North Yorkshire, England. The population of the civil parish was less than 100 at the 2011 Census. Details are included in the civil parish of Brandsby-cum-Stearsby. It is situated between the market towns of Easingwold and Helmsley. The entire parish of Yearsley is within the Howardian Hills Area of Outstanding Natural Beauty. It was, and remains, a predominantly agricultural village with significant forestry on the moors to the north of the village. The name 'Yearsley' is recorded in the Domesday Book as 'Eureslage' and then, in the Pipe Rolls of 1176, as 'Euereslai'. The origins of the name, however, are probably Anglo-Saxon, from a word meaning Boars' Wood. Following the Norman invasion, the lands of Yearsley fell into the hands of a Norman knight, Roger de Mowbray, who, by 1160, passed the estates to another Norman nobleman, Thomas Colville (from Collville-Sur-Mer on the Normandy coast). The h ... [...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] |
Oswaldkirk
Oswaldkirk is a small village and civil parish south of Helmsley and north of York in the Ryedale district of North Yorkshire, England. It is named after the village church of St Oswald, King and Martyr, the Anglo-Saxon King of Northumbria who was slain by the pagan, Penda in 642. There was previously a Catholic church, dedicated to St Aidan, which closed in 2020. The population of the village as taken at the 2011 census was 230. The village is situated at the junction of the roads B1257 and B1363 and straddles the boundaries of the North York Moors National Park and the Howardian Hills Area of Outstanding Natural Beauty. Non-ecclesiastical amenities include a playground, a village hall and a pub called "The Malt Shovel". The Millennium Trail, a circular waymarked walk around Oswaldkirk, takes in the major historical sites and points of interest. The village is also on the path of the Ebor Way. Each year the village holds a Safari Lunch, a Cricket match and a Bonfi ... [...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] |
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] |
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] |
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] |
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] |
