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Church Of St Peter And St Paul, Trottiscliffe
The Church of St Peter and St Paul is an active Church of England, Anglican parish church in Church Lane, Trottiscliffe, in the Borough of Tonbridge and Malling, Kent, England. It is situated below the North Downs on the lowest levels of the Chalk Group, Lower Chalk, above a spring (hydrology), spring on the Gault, Gault clay top at approximately 280 feet above ordnance datum. The church dates from the late 11th century and is dedication, dedicated to saints Saint Peter, Peter and Paul the Apostle, Paul. It is a Pilgrim Church as it is located near to the Pilgrims' Way, the historical route purportedly taken by pilgrims from Winchester, Hampshire, Winchester in Hampshire, to the shrine of Thomas Becket at Canterbury in Kent. The church has been recorded in the National Heritage List for England as a designated Listed building#England and Wales, Grade I listed building since 1959 and is also notable for its large pulpit, which stood in Westminster Abbey until 1820. History ...
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Trottiscliffe
Trottiscliffe ( ) is a village in Kent, England about north west of West Malling. It is often incorrectly spelled ''Trosley'' after Trosley Country Park at the top of the North Downs, which was once part of the Trosley Towers Estate. The spelling ''Trottesclyve'' appears with nearby '' Hallyng'' in 1396. Labelled as Trotterscliffe on the Ordnance Survey map published in 1870. Historic buildings Its most notable features are the neolithic Coldrum Long Barrow and the medieval Church of St. Peter and St. Paul. Notable residents Trottiscliffe was the English home of artist Graham Sutherland Graham Vivian Sutherland (24 August 1903 – 17 February 1980) was a prolific English artist. Notable for his paintings of abstract landscapes and for his portraits of public figures, Sutherland also worked in other media, including printmaking ... from 1937 until his death in 1980. He was buried by Trottiscliffe parish church. References External links Trottiscliffe History Projec ...
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Addington, Kent
Addington is a village in the English county of Kent. It is close to the M20 motorway, and between the villages of Wrotham Heath and West Malling. In the Domesday Book of 1086 it is called Eddintune. The meaning of the village's name is "Æddi's (or Eadda's) estate". The village is notable for the long barrows, Neolithic chamber tombs. Its parish covers a little under , containing 291 houses. Addington Brook runs through the parish. History Addington has been continuously inhabited for over 5,000 years. Many Neolithic artifacts have been extracted from the village, but much archaeological evidence has been lost to mechanical digging. Some sites were excavated during the building of the motorway. It had two mills at the time of the Domesday survey. There was a watermill powered by the Addington Brook (TQ 656 587 ), demolished in the nineteenth century; the site now lies within West Malling Golf Course. The remains of an old structure named the Addington Place were visible until th ...
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Dedication
Dedication is the act of consecrating an altar, temple, church, or other sacred building. Feast of Dedication The Feast of Dedication, today Hanukkah, once also called "Feast of the Maccabees," is a Jewish festival observed for eight days from the 25th of Kislev (usually in December, but occasionally late November, due to the lunisolar calendar). It was instituted in the year 165 B.C. by Judas Maccabeus, his brothers, and the elders of the congregation of Israel in commemoration of the reconsecration of the Jewish Temple in Jerusalem, and especially of the altar of burnt offerings, after they had been desecrated during the persecution under Antiochus Epiphanes (168 BC). The significant happenings of the festival were the illumination of houses and synagogues, a custom probably taken over from the Feast of Tabernacles, and the recitation of . According to the Second Book of Chronicles, the dedication of Solomon's Temple took place in the week before the Feast of Tabernac ...
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Ordnance Datum
In the British Isles, an ordnance datum or OD is a vertical datum used by an ordnance survey as the basis for deriving altitudes on maps. A spot height may be expressed as AOD for "above ordnance datum". Usually mean sea level (MSL) is used for the datum. In particular: * In Great Britain, OD for the Ordnance Survey is ODN (Ordnance Datum Newlyn), defined as the MSL as recorded by the tidal gauge at Newlyn in Cornwall between 1915 and 1921. **Prior to 1921, OD was defined as MSL as recorded in the Victoria Dock, Liverpool, during a short period in 1844 (ODL). * In Northern Ireland, OD for the Ordnance Survey of Northern Ireland is Belfast Ordnance Datum, the MSL at Clarendon Dock, Belfast, between 1951 and 1956. * In the Republic of Ireland, OD for the Ordnance Survey of Ireland is Malin Ordnance Datum: the MSL at Portmoor Pier, Malin Head, County Donegal, between 1960 and 1969.
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Gault
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 London Basin ...
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Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust ( pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ...
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Chalk Group
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud ("micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium carbonate pla ...
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North Downs
The North Downs are a ridge of chalk hills in south east England that stretch from Farnham in Surrey to the White Cliffs of Dover in Kent. Much of the North Downs comprises two Areas of Outstanding Natural Beauty (AONBs): the Surrey Hills and the Kent Downs. The North Downs Way National Trail runs along the North Downs from Farnham to Dover. The highest point in the North Downs is Botley Hill, Surrey ( above sea level). The ''County Top'' of Kent is Betsom's Hill ( above sea level), which is less than 1 km from Westerham Heights, Bromley, the highest point in Greater London at an elevation of . Etymology 'Downs' is from Old English ''dun'', meaning, amongst other things, "hill". The word acquired the sense of "elevated rolling grassland" around the 14th century. The name contains "North" to distinguish them from a similar range of hills – the South Downs – which runs roughly parallel to them but some to the south. Geography The narrow spine of the Hog's Back b ...
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Borough Of Tonbridge And Malling
Tonbridge and Malling is a local government district with borough status in Kent, England. Tonbridge is the largest settlement but the authority is based in the modern development of Kings Hill. Geography Tonbridge and Malling Borough covers an area from the North Downs at Burham and Snodland in the north to the town of Tonbridge in the south. The River Medway meanders north-east through the borough towards the Medway Gap, having in the west of the area received the River Eden. The castle-passing Eden Valley Walk is also mostly in this borough. Administrative history The district was created on 1 April 1974 by the merger of the urban district of Tonbridge, together with Malling Rural District and the civil parishes of Hadlow and Hildenborough from Tonbridge Rural District. The district received borough status on 16 December 1983 and the council was renamed Tonbridge and Malling Borough Council. The ceremonial head of the council, the chairman, was known as mayor after tha ...
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Parish Church
A parish church (or parochial church) in Christianity is the church which acts as the religious centre of a parish. In many parts of the world, especially in rural areas, the parish church may play a significant role in community activities, often allowing its premises to be used for non-religious community events. The church building reflects this status, and there is considerable variety in the size and style of parish churches. Many villages in Europe have churches that date back to the Middle Ages, but all periods of architecture are represented. Roman Catholic Church Each diocese (administrative unit, headed by a Bishop) is divided into parishes. Normally, a parish comprises all Catholics living within its geographically defined area. Within a diocese, there can also be overlapping parishes for Catholics belonging to a particular rite, language, nationality, or community. Each parish has its own central church called the parish church, where religious services take plac ...
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Interregnum
An interregnum (plural interregna or interregnums) is a period of discontinuity or "gap" in a government, organization, or social order. Archetypally, it was the period of time between the reign of one monarch and the next (coming from Latin ''inter-'', "between" and ''rēgnum'', "reign" rom ''rex, rēgis'', "king", and the concepts of interregnum and regency therefore overlap. Historically, longer and heavier interregna have been typically accompanied by widespread unrest, civil and succession wars between warlords, and power vacuums filled by foreign invasions or the emergence of a new power. A failed state is usually in interregnum. The term also refers to the periods between the election of a new parliament and the establishment of a new government from that parliament in parliamentary democracies, usually ones that employ some form of proportional representation that allows small parties to elect significant numbers, requiring time for negotiations to form a governmen ...
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Province Of Canterbury
The Province of Canterbury, or less formally the Southern Province, is one of two ecclesiastical provinces which constitute the Church of England. The other is the Province of York (which consists of 12 dioceses). Overview The Province consists of 30 dioceses, covering roughly two-thirds of England, parts of 1915–1916 Church of England border polls, Wales, all of the Channel Islands and continental Europe, Morocco, Turkey, Mongolia and the territory of the former Soviet Union (under the jurisdiction of the Diocese of Gibraltar in Europe). The Province previously also covered all of Wales but lost most of its jurisdiction in 1920, when the then four dioceses of the Church in Wales were Welsh Church Act 1914, disestablished and separated from Canterbury to form a distinct ecclesiastical province of the Anglican Communion. The Province of Canterbury retained jurisdiction over eighteen areas of Wales that were defined as part of "border parishes", parishes whose ecclesiastical bo ...
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