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Meppershall Manor House
Meppershall is a hilltop village in Bedfordshire near Shefford, Campton, Shillington, Stondon and surrounded by farmland. The village and the manor house are mentioned in the Domesday Book in 1086 - with the entry reading: ''Malpertesselle/Maperteshale: Gilbert FitzSolomon.'' The Manor House belonged to the De Meppershall family for nearly 300 years following 1086. The present house is early 17th century. Until 1844 Meppershall was partially in Hertfordshire. The detached portion of Hertfordshire was transferred to Bedfordshire in 1844, following the Counties (Detached Parts) Act 1844. St. Mary's churchdates back to the Normans. The Parish Records of St Mary, Meppershall, have been published on CD by the Parochial Church Council.
February 2011. Before the advent of greenhouses, Meppershall was a very poor community with large families living in two up, t ...
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Central Bedfordshire
Central Bedfordshire is a unitary authority area in the ceremonial county of Bedfordshire, England. It was created in 2009. Formation Central Bedfordshire was created on 1 April 2009 as part of a structural reform of local government in Bedfordshire. The Bedfordshire County Council and all the district councils in the county were abolished, with new unitary authorities created providing the services which had been previously delivered by both the district and county councils. Central Bedfordshire was created covering the area of the former Mid Bedfordshire and South Bedfordshire Districts.http://www.legislation.gov.uk/uksi/2008/907/note/made - The Bedfordshire (Structural Changes) Order 2008 The local authority is called Central Bedfordshire Council. Towns and villages Central Bedfordshire comprises a mix of market towns and rural villages. The largest town is Dunstable followed by Leighton Buzzard and Houghton Regis. Dunstable and Houghton Regis form part of the Luton/Dun ...
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Meppershall Manor House
Meppershall is a hilltop village in Bedfordshire near Shefford, Campton, Shillington, Stondon and surrounded by farmland. The village and the manor house are mentioned in the Domesday Book in 1086 - with the entry reading: ''Malpertesselle/Maperteshale: Gilbert FitzSolomon.'' The Manor House belonged to the De Meppershall family for nearly 300 years following 1086. The present house is early 17th century. Until 1844 Meppershall was partially in Hertfordshire. The detached portion of Hertfordshire was transferred to Bedfordshire in 1844, following the Counties (Detached Parts) Act 1844. St. Mary's churchdates back to the Normans. The Parish Records of St Mary, Meppershall, have been published on CD by the Parochial Church Council.
February 2011. Before the advent of greenhouses, Meppershall was a very poor community with large families living in two up, t ...
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Villages In Bedfordshire
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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Fertiliser
A fertilizer (American English) or fertiliser (British English; see spelling differences) is any material of natural or synthetic origin that is applied to soil or to plant tissues to supply plant nutrients. Fertilizers may be distinct from liming materials or other non-nutrient soil amendments. Many sources of fertilizer exist, both natural and industrially produced. For most modern agricultural practices, fertilization focuses on three main macro nutrients: nitrogen (N), phosphorus (P), and potassium (K) with occasional addition of supplements like rock flour for micronutrients. Farmers apply these fertilizers in a variety of ways: through dry or pelletized or liquid application processes, using large agricultural equipment or hand-tool methods. Historically fertilization came from natural or organic sources: compost, animal manure, human manure, harvested minerals, crop rotations and byproducts of human-nature industries (i.e. fish processing waste, or bloodmeal from a ...
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Superphosphate
Triple superphosphate is a component of fertilizer that primarily consists of monocalcium phosphate, Ca(H2PO4)2. Triple superphosphate is obtained by treating phosphate rock with phosphoric acid. Traditional routes for extraction of phosphate rock uses sulfuric acid gives single superphosphate, an approximate 1:1 mixture of Ca(H2PO4)2 and CaSO4 phosphogypsum). Double superphosphate refers to some average of triple- and single superphosphate, resulting from the extraction of phosphate rock with a mixture of phosphoric and sulfuric acids. Many fertilizers are derived from triple superphosphate, e.g. by blending with ammonium sulfate and potassium chloride Potassium chloride (KCl, or potassium salt) is a metal halide salt composed of potassium and chlorine. It is odorless and has a white or colorless vitreous crystal appearance. The solid dissolves readily in water, and its solutions have a salt .... Typical fertilizer-grade triple superphosphate contains 45% P2O5eq, single supe ...
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Sulphuric Acid
Sulfuric acid (American spelling and the preferred IUPAC name) or sulphuric acid ( Commonwealth spelling), known in antiquity as oil of vitriol, is a mineral acid composed of the elements sulfur, oxygen and hydrogen, with the molecular formula . It is a colorless, odorless and viscous liquid that is miscible with water. Pure sulfuric acid does not exist naturally on Earth due to its strong affinity to water vapor; it is hygroscopic and readily absorbs water vapor from the air. Concentrated sulfuric acid is highly corrosive towards other materials, from rocks to metals, since it is an oxidant with powerful dehydrating properties. Phosphorus pentoxide is a notable exception in that it is not dehydrated by sulfuric acid, but to the contrary dehydrates sulfuric acid to sulfur trioxide. Upon addition of sulfuric acid to water, a considerable amount of heat is released; thus the reverse procedure of adding water to the acid should not be performed since the heat released may boil ...
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Pre-historic
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ...
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Fossilised
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Coprolite
A coprolite (also known as a coprolith) is fossilized feces. Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology. The name is derived from the Greek words κόπρος (''kopros'', meaning "dung") and λίθος (''lithos'', meaning "stone"). They were first described by William Buckland in 1829. Before this, they were known as "fossil fir cones" and "bezoar stones". They serve a valuable purpose in paleontology because they provide direct evidence of the predation and diet of extinct organisms. Coprolites may range in size from a few millimetres to over 60 centimetres. Coprolites, distinct from ''paleofeces'', are fossilized animal dung. Like other fossils, coprolites have had much of their original composition replaced by mineral deposits such as silicates and calcium carbonates. Paleofeces, on the other hand, retain much of their original organic composition ...
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Counties (Detached Parts) Act 1844
The Counties (Detached Parts) Act 1844 (7 & 8 Vict. c. 61), which came into effect on 20 October 1844, was an Act of Parliament of the United Kingdom which eliminated many outliers or exclaves of counties in England and Wales for civil purposes. The changes were based on recommendations by a boundary commission, headed by the surveyor Thomas Drummond and summarized in a schedule attached to the Parliamentary Boundaries Act 1832. This also listed a few examples of civil parishes divided by county boundaries, most of which were dealt with by later legislation. Antecedents Inclosure Acts The areas involved had already been reorganised for some purposes. This was a process which began with the Inclosure Acts of the later 18th century. A parish on a county boundary which used the open-field system could have its field strips distributed among the two counties in a very complicated way. Enclosure could rationalise the boundary in the process of re-distributing land to the various lan ...
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Bedfordshire
Bedfordshire (; abbreviated Beds) is a ceremonial county in the East of England. The county has been administered by three unitary authorities, Borough of Bedford, Central Bedfordshire and Borough of Luton, since Bedfordshire County Council was abolished in 2009. Bedfordshire is bordered by Cambridgeshire to the east and north-east, Northamptonshire to the north, Buckinghamshire to the west and Hertfordshire to the south-east and south. It is the fourteenth most densely populated county of England, with over half the population of the county living in the two largest built-up areas: Luton (258,018) and Bedford (106,940). The highest elevation point is on Dunstable Downs in the Chilterns. History The first recorded use of the name in 1011 was "Bedanfordscir," meaning the shire or county of Bedford, which itself means "Beda's ford" (river crossing). Bedfordshire was historically divided into nine hundreds: Barford, Biggleswade, Clifton, Flitt, Manshead, Redbornestoke, S ...
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List Of Hertfordshire Boundary Changes
Boundary changes affecting the English county of Hertfordshire. The county borders Buckinghamshire to the west, Bedfordshire and Cambridgeshire to the north, Essex to the east and Greater London to the south. Until 1965 it had a southern boundary with Middlesex. Summary Apart from a number of minor exchanges of land with surrounding counties, the alterations in Hertfordshire's boundaries involved the following: *The county had four exclaves that were integrated into their surrounding counties in 1844, and a set of six small enclaves of Bedfordshire was annexed. *In the south, the boundary with Middlesex was somewhat complex, with Hertfordshire forming a long protrusion into it. In 1889 Hertfordshire gained some territory in this area and when Greater London was formed in 1965 the whole area, including Barnet and East Barnet, became part of the new county. Potters Bar in Middlesex was surrounded by Hertfordshire on three sides, and it was transferred to it in 1965, along with Sout ...
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