Archdeacon Newton
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Archdeacon Newton
Archdeacon Newton is a hamlet and rural parish of several farms in the borough of Darlington and the ceremonial county of County Durham, in England. The population taken at the 2011 Census was less than 100. Details are maintained in the parish of Walworth. It is associated with an abandoned village site under pasture and farm buildings, and situated a short distance to the north-west of Darlington. The lost settlement was in existence by the early 15th century, and remained inhabited at least until the 1890s. There was a moated manor house at the southern end, part of which remains as the Old Hall, now a barn. At the north end of the site was the chapel, and in the middle were tofts and enclosures, with a ridge and furrow field and a trackway leading to the south-east. The site of the abandoned village is now a scheduled monument and the Old Hall is a listed building. Geographical and political The underlying composition here is of glacial clay with pockets of gravel, sa ...
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Darlington (borough)
The Borough of Darlington is a unitary authority and borough in County Durham, Northern England. The borough is named after the town of Darlington, and in 2011 had a population of 106,000. It is in the Tees Valley mayoralty. The borough borders three local authority areas; County Durham is to the north and west, Stockton-on-Tees to the east and North Yorkshire to the south, the River Tees forming the border for the latter. History The current borough boundaries were formed on 1 April 1974, by the creation of a new non-metropolitan district of Darlington by the Local Government Act 1972, covering the previous county borough of Darlington along with nearly all of Darlington Rural District (the Newton Aycliffe parts of which went to Sedgefield). It remained part of County Durham for administrative purposes until reconstituted as a unitary authority on 1 April 1997. For ceremonial purposes it remains part of County Durham, with whom it continues to share certain local services, s ...
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Glacial Period
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ...
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Archdeacon Of Durham
The Archdeacon of Durham is a senior ecclesiastical officer of the diocese of Durham (Church of England). They have, within the geographical area the ''archdeaconry of Durham'', pastoral oversight of clergy and care of church buildings (among other responsibilities). History The first archdeacons in the diocese occur after the Norman Conquest – around the same time the post of archdeacon first started to occur elsewhere in England. There is no evidence of more than one archdeacon in the diocese until the mid-12th century, when two lines of office holders start to appear in sources. The titles "Archdeacon of Durham" and "Archdeacon of Northumberland" are not recorded until later in the century, although it is possible to discern which of the two lines became which post. Here are listed the sole archdeacons of Durham diocese, then those of the senior of two unnamed lines, then all those called Archdeacon of Durham. The archdeaconry has been split twice: once on 23 May 1882, to crea ...
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Cockerton
Cockerton is an area, or township, of north-west Darlington in the borough of Darlington, County Durham, England. The Cocker Beck flows through the area and empties into the River Skerne via The Denes, an area and string of valleyed parks donated for the town in the early 20th century. It is also near Mowden, Branksome, West Park and Faverdale. Etymology The -''ton'' of ''Cockerton'' is from Old English ''tūn'' 'estate'; the ''cocker-'' element is less certain but seems to have been a Cumbric river-name, still represented as the name of Cocker Beck. Allen Mawer, ''The place names of Northumberland and Durham'' (Cambridge: Cambridge University Press, 1920), s.v.; Bethany Fox, 'The P-Celtic Place-Names of North-East England and South-East Scotland', The Heroic Age, 10 (2007), http://www.heroicage.org/issues/10/fox.html (appendix at http://www.heroicage.org/issues/10/fox-appendix.html). Cockerton Village The original village layout, known still as "Cockerton Village", rema ...
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A1 Road (Great Britain)
The A1 is the longest numbered road in the UK, at . It connects Greater London, London, the capital of England, with Edinburgh, the capital of Scotland. It passes through or near North London, Hatfield, Hertfordshire, Hatfield, Welwyn Garden City, Stevenage, Baldock, Letchworth, Letchworth Garden City, Biggleswade, St Neots, Huntingdon, Peterborough, Stamford, Lincolnshire, Stamford, Grantham, Newark-on-Trent, Retford, Doncaster, York, Pontefract, Wetherby, Ripon, Darlington, Durham, England, Durham, Sunderland, Tyne and Wear, Sunderland, Gateshead, Newcastle upon Tyne, Morpeth, Northumberland, Morpeth, Alnwick and Berwick-upon-Tweed. It was designated by the Department for Transport, Ministry of Transport in 1921, and for much of its route it followed various branches of the historic Great North Road (Great Britain), Great North Road, the main deviation being between Boroughbridge and Darlington. The course of the A1 has changed where towns or villages have been bypass (road), ...
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Branksome, County Durham
Branksome is a suburb of Darlington in County Durham, in England. It is situated to the north-west of the town, close to Mowden, Cockerton, West Park and Faverdale. It is largely made up from council owned properties and service buildings started in the late 1940s through to the 1970s. Although some of the council built houses and flats have been sold to tenants since the 1980s under the government 'right to buy' scheme, many are still retained as rented properties by the Housing Department of Darlington Borough Council (unitary authority). This management situation was consulted on in 2003-04 and the Housing Dept. retained management after consultations with tenants throughout the borough who expressed a desire to remain under local authority management rather than the alternatives. It lies in the Cockerton West Ward of the Darlington Borough and elects two councillors every four years. Adjacent to Branksome on the Northern side lies the old Darlington to Barnard Castl ...
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Councillor
A councillor is an elected representative for a local government council in some countries. Canada Due to the control that the provinces have over their municipal governments, terms that councillors serve vary from province to province. Unlike most provincial elections, municipal elections are usually held on a fixed date of 4 years. Finland ''This is about honorary rank, not elected officials.'' In Finland councillor (''neuvos'') is the highest possible title of honour which can be granted by the President of Finland. There are several ranks of councillors and they have existed since the Russian Rule. Some examples of different councillors in Finland are as follows: * Councillor of State: the highest class of the titles of honour; granted to successful statesmen * Mining Councillor/Trade Councillor/Industry Councillor/Economy Councillor: granted to leading industry figures in different fields of the economy *Councillor of Parliament: granted to successful statesmen *Off ...
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Wards Of The United Kingdom
The wards and electoral divisions in the United Kingdom are electoral districts at sub-national level, represented by one or more councillors. The ward is the primary unit of English electoral geography for civil parishes and borough and district councils, the electoral ward is the unit used by Welsh principal councils, while the electoral division is the unit used by English county councils and some unitary authorities. Each ward/division has an average electorate of about 5,500 people, but ward population counts can vary substantially. As of 2021 there are 8,694 electoral wards/divisions in the UK. England The London boroughs, metropolitan boroughs and non-metropolitan districts (including most unitary authorities) are divided into wards for local elections. However, county council elections (as well as those for several unitary councils which were formerly county councils, such as the Isle of Wight and Shropshire Councils) instead use the term ''electoral division''. In s ...
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Carboniferous Limestone
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup. Depositional basins Within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east–west aligned belt of land stretching through central Wales and the English Midlands to East Anglia and on into Belgium. The limestones deposited to its south form a distinct South Wales-Mendip province which extends from Pembrokeshire in the west through ...
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ...
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Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ...
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Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ...
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