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Sutton Waldron
Sutton Waldron is a village and civil parish in north Dorset, England, situated on the A350 road between Iwerne Minster and Fontmell Magna, in the Blackmore Vale under the scarp of Cranborne Chase, north of Blandford Forum and south of Shaftesbury. In the 2011 census the parish had 93 dwellings, 87 households and a population of 200. The parish covers about in a strip of land that, from west to east, is composed of Kimmeridge clay, Lower Greensand, Gault Clay, Upper Greensand and chalk. In 1086 in the Domesday Book, Sutton Waldron was recorded as ''Sudtone''; it had 24 households, one mill, six ploughlands, of meadow and of woodland. It was in the hundred of Gillingham and the lord and tenant-in-chief was Waleran the hunter. The parish church dates from 1847 and is constructed in the Decorated Gothic 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 cathe ...
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Dorset (unitary Authority)
Dorset is a unitary authority area in the ceremonial county of Dorset, England, which came into existence on 1 April 2019. It covers all of the ceremonial county except for Bournemouth, Christchurch and Poole. The council of the district is Dorset Council (UK), Dorset Council, which was in effect Dorset County Council re-constituted so as to be vested with the powers and duties of five district councils which were also abolished, and shedding its partial responsibility for and powers in Christchurch. History and statutory process Statutory instruments for re-organisation of Dorset (as to local government) were made in May 2018. These implemented the Future Dorset plan to see all councils then existing within the county abolished and replaced by two new unitary authorities on 1 April 2019. *The unitary authorities of Bournemouth Borough Council, Bournemouth and Poole Borough Council, Poole merged with the non-metropolitan district of Christchurch, Dorset, Christchurch to create a ...
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Kimmeridge Clay
The Kimmeridge Clay is a sedimentary deposit of fossiliferous marine clay which is of Late Jurassic to lowermost Cretaceous age and occurs in southern and eastern England and in the North Sea. This rock formation is the major source rock for North Sea oil. The fossil fauna of the Kimmeridge Clay includes turtles, crocodiles, sauropods, plesiosaurs, pliosaurs and ichthyosaurs, as well as a number of invertebrate species. Description Kimmeridge Clay is named after the village of Kimmeridge on the Dorset coast of England, where it is well exposed and forms part of the Jurassic Coast World Heritage Site. Onshore, it is of Late Jurassic (Kimmeridgian) age and outcrops across England, in a band stretching from Dorset in the south-west, north-east to North Yorkshire. Offshore, it extends into the Lower Cretaceous (Berriasian Stage) and it is found throughout the Southern, Central and Northern North Sea. The foundations of the Humber Bridge on the southern (Barton) side of the bridg ...
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Gothic Revival Architecture
Gothic Revival (also referred to as Victorian Gothic, neo-Gothic, or Gothick) is an architectural movement that began in the late 1740s in England. The movement gained momentum and expanded in the first half of the 19th century, as increasingly serious and learned admirers of the neo-Gothic styles sought to revive medieval Gothic architecture, intending to complement or even supersede the neoclassical styles prevalent at the time. Gothic Revival draws upon features of medieval examples, including decorative patterns, finials, lancet windows, and hood moulds. By the middle of the 19th century, Gothic had become the preeminent architectural style in the Western world, only to fall out of fashion in the 1880s and early 1890s. The Gothic Revival movement's roots are intertwined with philosophical movements associated with Catholicism and a re-awakening of high church or Anglo-Catholic belief concerned by the growth of religious nonconformism. Ultimately, the "Anglo-Catholicism" t ...
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Waleran The Hunter
Waleran the Hunter (floruit 1086) (Latin: ''Waleran Venator'') was an Anglo-Norman magnate who held 51 manors as recorded in the Domesday Book of 1086, including Whaddon in Wiltshire and several in Hampshire, including West Dean, within the New Forest. His Latin name (perhaps an epithet) as recorded in the Domesday Book, ''Venator'' ("the Hunter"), suggests that he was a hunt-official of that royal forest A royal forest, occasionally known as a kingswood (), is an area of land with different definitions in England, Wales, Scotland and Ireland. The term ''forest'' in the ordinary modern understanding refers to an area of wooded land; however, the ....Hoare, Modern Wiltshire, 'Hundred of Cawden,' iii. 24 Little else is known about him. Descendants His descendants assumed the surname ''Waleran'', and Waldron one of the descendants in a junior line of which was Robert Walerand (died 1273), Justiciar to King Henry III. The senior line of the family retained the manor of West ...
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Tenant-in-chief
In medieval and early modern Europe, the term ''tenant-in-chief'' (or ''vassal-in-chief'') denoted a person who held his lands under various forms of feudal land tenure directly from the king or territorial prince to whom he did homage, as opposed to holding them from another nobleman or senior member of the clergy.Bloch ''Feudal Society Volume 2'' p. 333Coredon ''Dictionary of Medieval Terms & Phrases'' p. 272 The tenure was one which denoted great honour, but also carried heavy responsibilities. The tenants-in-chief were originally responsible for providing knights and soldiers for the king's feudal army.Bracton, who indiscriminately called tenants-in-chief "barons" stated: "sunt et alii potentes sub rege qui barones dicuntur, hoc est robur belli" ("there are other magnates under the king, who are called barons, that is the hardwood of war"), quoted in Sanders, I.J., ''Feudal Military Service in England'', Oxford, 1956, p.3; "Bracton's definition of the ''baro''" (plur ''baro ...
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Gillingham, Dorset
Gillingham ( ) is a town and civil parish in the Blackmore Vale area of Dorset, England. It lies on the B3095 and B3081 roads, approximately south of the A303 road, A303 trunk road and northwest of Shaftesbury. It is the most northerly town in the county. In the 2011 United Kingdom census, 2011 census the civil parish had a population of 11,756. The neighbouring hamlets of Peacemarsh, Bay and Wyke have become part of Gillingham as it has expanded. Gillingham is pronounced with a hard initial "g" (), unlike Gillingham, Kent, which is pronounced with a soft "g" (). History There is a Stone Age tumulus, barrow in the town, and evidence of Roman Britain, Roman settlement in the 2nd and 3rd centuries; however the town was established by the Saxons. The St Mary the Virgin's Church, Gillingham, Dorset, church of St Mary the Virgin has a Anglo-Saxons, Saxon Christian cross, cross shaft dating from the 9th century. The name Gillingham was used for the town in its 10th century Saxon c ...
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Hundred (county Division)
A hundred is an administrative division that is geographically part of a larger region. It was formerly used in England, Wales, some parts of the United States, Denmark, Southern Schleswig, Sweden, Finland, Norway, the Bishopric of Ösel–Wiek, Curonia, the Ukrainian state of the Cossack Hetmanate and in Cumberland County in the British Colony of New South Wales. It is still used in other places, including in Australia (in South Australia and the Northern Territory). Other terms for the hundred in English and other languages include ''wapentake'', ''herred'' (Danish and Bokmål Norwegian), ''herad'' ( Nynorsk Norwegian), ''hérað'' (Icelandic), ''härad'' or ''hundare'' (Swedish), ''Harde'' (German), ''hiird'' ( North Frisian), ''satakunta'' or ''kihlakunta'' (Finnish), ''kihelkond'' (Estonian), ''kiligunda'' (Livonian), '' cantref'' (Welsh) and ''sotnia'' (Slavic). In Ireland, a similar subdivision of counties is referred to as a barony, and a hundred is a subdivision of a pa ...
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Ploughland
The carucate or carrucate ( lat-med, carrūcāta or ) was a medieval unit of land area approximating the land a plough team of eight oxen could till in a single annual season. It was known by different regional names and fell under different forms of tax assessment. England The carucate was named for the carruca heavy plough that began to appear in England in the late 9th century, it may have been introduced during the Viking invasions of England.White Jr., Lynn, The Life of the Silent Majority, pg. 88 of Life and Thought in the Early Middle Ages, ed. Robert S. Hoyt, University of Minnesota Press, Minneapolis. 1967 It was also known as a ploughland or plough ( ang, plōgesland, "plough's land") in the Danelaw and usually, but not always, excluded the land's suitability for winter vegetables and desirability to remain fallow in crop rotation. The tax levied on each carucate came to be known as " carucage". Though a carucate might nominally be regarded as an area of 120 acres (49 hec ...
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Domesday Book
Domesday Book () – the Middle English spelling of "Doomsday Book" – is a manuscript record of the "Great Survey" of much of England and parts of Wales completed in 1086 by order of King William I, known as William the Conqueror. The manuscript was originally known by the Latin name ''Liber de Wintonia'', meaning "Book of Winchester", where it was originally kept in the royal treasury. The '' Anglo-Saxon Chronicle'' states that in 1085 the king sent his agents to survey every shire in England, to list his holdings and dues owed to him. Written in Medieval Latin, it was highly abbreviated and included some vernacular native terms without Latin equivalents. The survey's main purpose was to record the annual value of every piece of landed property to its lord, and the resources in land, manpower, and livestock from which the value derived. The name "Domesday Book" came into use in the 12th century. Richard FitzNeal wrote in the ''Dialogus de Scaccario'' ( 1179) that the book ...
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Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ...
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Gault Clay
The Gault Formation is a geological formation of stiff blue clay deposited in a calm, fairly deep-water marine environment during the Lower Cretaceous Period (Upper and Middle Albian). It is well exposed in the coastal cliffs at Copt Point in Folkestone, Kent, England, where it overlays the Lower Greensand formation, and underlies the Upper Greensand Formation. These represent different facies, with the sandier parts probably being deposited close to the shore and the clay in quieter water further from the source of sediment; both are believed to be shallow-water deposits. The etymology of the name is uncertain and probably of local origin. Distribution It is found in exposure on the south side of the North Downs and the north side of the South Downs. It is also to be found beneath the scarp of the Berkshire Downs, in the Vale of White Horse, in Oxfordshire, England, and on the Isle of Wight where it is known as Blue Slipper. Gault underlies the chalk beneath the Londo ...
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Greensand
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil-rich, such as in the late-Cretaceous deposits of New Jersey. Occurrence Important exposures are known from both northern and western Europe, North America, southeastern Brazil and north Africa. Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware. Although greensand h ...
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