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Northill Church
Northill is a village and civil parish in the Central Bedfordshire district of the county of Bedfordshire, England about southeast of the county town of Bedford. The 2011 census showed the population for Northill village as 338 and for the civil parish, 2,270. The parish includes the village of Upper Caldecote and the hamlets of Budna, Lower Caldecote, Hatch, Ickwell and Thorncote Green. Northill has a small village green with duck pond, owned by the parish council. Geography Northill is west southwest of Sandy, west northwest of Biggleswade, southwest of Cambridge and north of Central London. Area The civil parish covers an area of . Its eastern boundary is the River Ivel. Landscape Topographically, Northill stands on a slightly elevated ridge that runs north to south. The village lies on the border of the Bedfordshire and Cambridgeshire Claylands and the Bedfordshire Greensand Ridge; National Character Areas designated by Natural England. Central Bedfordshire Coun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural England
Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, freshwater and marine environments, geology and soils, are protected and improved. It also has a responsibility to help people enjoy, understand and access the natural environment. Natural England focuses its activities and resources on four strategic outcomes: * a healthy natural environment * enjoyment of the natural environment * sustainable use of the natural environment * a secure environmental future Roles and responsibilities As a non-departmental public body (NDPB), Natural England is independent of government. However, the Secretary of State for Environment, Food & Rural Affairs has the legal power to issue guidance to Natural England on various matters, a constraint that was not placed on its predecessor NDPBs. Its powers inc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greensand Ridge Walk
The Greensand Ridge Walk is a long-distance walk of that traverses the county of Bedfordshire in England, with brief sections in the neighbouring counties of Cambridgeshire and Buckinghamshire. Its southern endpoint is at Leighton Buzzard and the route runs north-east to finish at Gamlingay. As can be inferred from the name, the walk follows the Bedfordshire Greensand Ridge (not to be confused with the Greensand Way, the greensand ridge that can be found in Surrey, Sussex and Kent). The waymarker for the route employs a silhouette of the muntjac Muntjacs ( ), also known as the barking deer or rib-faced deer, (URL is Google Books) are small deer of the genus ''Muntiacus'' native to South Asia and Southeast Asia. Muntjacs are thought to have begun appearing 15–35 million years ago, ..., a common sight in the vicinity of the village of Woburn, through which the walk passes. References External links * * Footpaths in Bedfordshire Long-distance footpaths in Engla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gambrel
A gambrel or gambrel roof is a usually symmetrical two-sided roof with two slopes on each side. (The usual architectural term in eighteenth-century England and North America was "Dutch roof".) The upper slope is positioned at a shallow angle, while the lower slope is steep. This design provides the advantages of a sloped roof while maximizing headroom inside the building's upper level and shortening what would otherwise be a tall roof. The name comes from the Medieval Latin word ''gamba'', meaning horse's hock or leg. The term ''gambrel'' is of American origin, the older, European name being a curb (kerb, kirb) roof. Europeans historically did not distinguish between a gambrel roof and a mansard roof but called both types a mansard. In the United States, various shapes of gambrel roofs are sometimes called Dutch gambrel or Dutch Colonial gambrel with bell-cast eaves, Swedish, German, English, French, or New England gambrel. The cross-section of a gambrel roof is similar to that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campaign To Protect Rural England
CPRE, The Countryside Charity, formerly known by names such as the ''Council for the Preservation of Rural England'' and the ''Council for the Protection of Rural England'', is a charity in England with over 40,000 members and supporters. Formed in 1926 by Patrick Abercrombie to limit urban sprawl and ribbon development, the CPRE claims to be one of the longest running environmental groups in the UK. CPRE campaigns for a "sustainable future" for the English countryside. They state it is "a vital but undervalued environmental, economic and social asset to the nation." They aim to "highlight threats and promote positive solutions." They campaign using their own research to lobby the public and all levels of government. History CPRE was formed following the publication of “The Preservation of Rural England” by Sir Patrick Abercrombie in 1926. Abercrombie became its Honorary Secretary. The inaugural meeting was held in December 1926 at the London offices of the Royal Institute ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Light Pollution
Light pollution is the presence of unwanted, inappropriate, or excessive use of artificial Visible spectrum, lighting. In a descriptive sense, the term ''light pollution'' refers to the effects of any poorly implemented lighting, during the day or night. Light pollution can be understood not only as a phenomenon resulting from a specific source or kind of pollution, but also as a contributor to the wider, collective impact of various sources of pollution. Although this type of pollution can exist throughout the day, its effects are magnified during the night with the contrast of darkness. It has been estimated that 83 percent of the world's people live under light-polluted skies and that 23 percent of the world's land area is affected by skyglow. The area affected by artificial illumination continues to increase. A major side-effect of urbanization, light pollution is blamed for compromising health, disrupting ecosystems, and spoiling aesthetic environments. Globally, it has incr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively. These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam. In the , textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and |
Ampthill Clay
The Ampthill Clay is a Mesozoic geologic formation in southern England. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. Vertebrate paleofauna * '' Cryptosaurus eumerus'' "Femur.""Table 17.1," in Weishampel, et al. (2004). Page 367. See also * List of dinosaur-bearing rock formations ** List of stratigraphic units with few dinosaur genera This list of stratigraphic units with few non-avian dinosaur genera includes Mesozoic stratigraphic units of formation rank or higher that have produced dinosaur body fossils which have been referred to at most five genera. Since taxonomy frequent ... Footnotes References * Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. . Oxfordian Stage {{UK-geologic-formation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Gravel
River gravel is a name given to gravel composed of small pieces of rounded stone of various colors, usually no larger than a large coin. It is named for the effect of many years of rounding of the edges of the stones due to a flow of water over it, as often takes place in a river. River gravel is often used in outdoor settings, such as a park walkway.{{cite web, url=http://www.anlscape.com.au/page/decorative_gravels.html , title=Australian Native Landscapes , accessdate=2009-04-14 , url-status=dead , archiveurl=https://web.archive.org/web/20090204070123/http://www.anlscape.com.au/page/decorative_gravels.html , archivedate=February 4, 2009 When a hard surface is also desired, river gravel is often set in a concrete aggregate mix. Owing to much higher cost than either asphalt or concrete pavement, the use of river gravel is generally limited to places where the appearance and/or its lack of sharp edges (when used alone) is of primary importance. The American National Park Servi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Superficial Deposits
Superficial deposits (or surficial deposits) refer to geological deposits typically of Quaternary age (less than 2.6 million years old). These geologically recent unconsolidated sediments may include stream channel and floodplain deposits, beach sands, talus gravels and glacial drift and moraine. All pre-Quaternary deposits are referred to as bedrock. Types and history There are several types of superficial deposit, including raised beaches and brickearth. These were formed in periods of climate change during the ice ages. The raised beaches were generally formed during periods of higher sea level, when ice sheets were at a minimum, and the sand and shingle deposits can be seen in many low cliffs. The brickearth is originally a wind-blown dust deposited under extremely cold, dry conditions but much has been re-deposited by flood water and mixed with flints. Superficial deposits were originally recorded only onshore and around the coast where they were laid down by various natu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boulder Clay
Boulder clay is an unsorted agglomeration of clastic sediment that is unstratified and structureless and contains gravel of various sizes, shapes, and compositions distributed at random in a fine-grained matrix. The fine-grained matrix consists of stiff, hard, pulverized clay or rock flour. Boulder clay is also know as either known as drift clay; till; unstratified drift, geschiebelehm (German); argile á blocaux (French); and keileem (Dutch).Charlesworth, J. K., 1957. ''Chap 18, Boulder Clay''. In ''The Quaternary Era, with Special Reference to its Glaciation''. v. 1, London, United Kingdom, Edward Arnold, p. 376-388.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''boulder clay'' is infreqently used for gravelly sedimentary deposits of nonglacial origin. These deposits include submarine slump and slide deposits along continental margins,Reineck, H.E. and Si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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