Hodthorpe And Belph
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Hodthorpe And Belph
Hodthorpe and Belph is a civil parish within the Bolsover district, of the county of Derbyshire, England. The parish includes the village of Hodthorpe and the hamlet of Belph. In 2011 the parish had a population of 663. It is 132 miles north west of London, 27 miles north east of the county city of Derby, and 5 miles north east of the market town of Bolsover. The parish touches Welbeck, Whitwell, Elmton with Creswell and Holbeck, and is the easternmost in Derbyshire. There is one listed building in Hodthorpe and Belph. Toponymy Belph: It has been suggested this placename derives from ''Belge'' meaning 'roaring river', although only gentle flowing streams are in the vicinity. A further claim is one from the Old English term ''belg'' meaning 'bag', used in respect of the geography of the area. Another possible form is of Norman/Saxon origin, ''le bulgh'' meaning 'gap', possibly in reference to the gorge by the stream nearby. The nameplace itself was not reported in Domesday ho ...
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Bolsover (UK Parliament Constituency)
Bolsover (, and commonly ) is a constituency in Derbyshire, represented in the House of Commons of the UK Parliament by Mark Fletcher, a member of the Conservative Party. The constituency was created in 1950, and is centred on the town of Bolsover. Between 1970 and 2019, the constituency was represented by Labour's Dennis Skinner, who by 2019 was the oldest member of the House of Commons and the second longest-serving. At the constituency's inception it was one of the safest Labour seats in the country, but over the following half century Skinner's vote share dropped from 77% in 1970, still holding a high vote share of 65% in 2005, to only 36% in 2019, with the result that he lost the seat to the Conservatives by a margin of 11%. History Before the Reform Act 1832, relatively wealthy people (forty-shilling freeholders) of the whole county could attend elections when there was an opposition candidate. From 1868 until 1885 the area formed part of the East Derbyshire constitue ...
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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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Narrow-nosed Rhinoceros
The narrow-nosed rhinoceros (''Stephanorhinus hemitoechus'') is an extinct species of rhinoceros that lived in western Eurasia and North Africa during the Pleistocene. It first appeared in Europe some 600,000 years ago, and survived there until as recently as 40,000 years Before Present Description The narrow-nosed rhinoceros was a large animal, reaching a shoulder height of as much as . It can be distinguished from other species of ''Stephanorhinus'' by its very long and low skull. Its nasals are relatively low, and its horn base poorly developed. Teeth are forward shifting. The narrow-nosed rhinoceros probably favored temperate open areas rich in low-growing vegetation. It displayed many similarities to its better known extinct relative, the woolly rhinoceros. However, it was probably not a true grazer, but a mixed feeder, eating low-growing vegetation in open habitats. In Apulia in southern Italy, remains of narrow-nosed rhinoceros from the middle Late Pleistocene were fo ...
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Hippopotamus
The hippopotamus ( ; : hippopotamuses or hippopotami; ''Hippopotamus amphibius''), also called the hippo, common hippopotamus, or river hippopotamus, is a large semiaquatic mammal native to sub-Saharan Africa. It is one of only two extant species in the family Hippopotamidae, the other being the pygmy hippopotamus (''Choeropsis liberiensis'' or ''Hexaprotodon liberiensis''). Its name comes from the ancient Greek for "river horse" (). Aside from elephants and rhinos, the hippopotamus is the largest land mammal. It is also the largest extant land artiodactyl. Despite their physical resemblance to pigs and other terrestrial even-toed ungulates, the closest living relatives of the hippopotamids are cetaceans (whales, dolphins, porpoises, etc.), from which they diverged about 55 million years ago. Hippos are recognisable for their barrel-shaped torsos, wide-opening mouths with large canine tusks, nearly hairless bodies, pillar-like legs, and large size: adults average ...
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Ipswichian Interglacial
The Eemian (also called the last interglacial, Sangamonian Stage, Ipswichian, Mikulin, Kaydaky, penultimate,NOAA - Penultimate Interglacial Period http://www.ncdc.noaa.gov/global-warming/penultimate-interglacial-period Valdivia or Riss-Würm) was the interglacial period which began about 130,000 years ago at the end of the Penultimate Glacial Period and ended about 115,000 years ago at the beginning of the Last Glacial Period. It corresponds to Marine Isotope Stage 5e. Although sometimes referred to as the "last interglacial" (in the "most recent previous" sense of "last"), it was the second-to-latest interglacial period of the current Ice Age, the most recent being the Holocene which extends to the present day (having followed the last glacial period). The prevailing Eemian climate was, on average, around 1 to 2 degrees Celsius (1.8 to 3.6 Fahrenheit) warmer than that of the Holocene. During the Eemian, the proportion of in the atmosphere was about 280 parts per million. The ...
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Lime (material)
Lime is a calcium-containing inorganic material composed primarily of oxides and hydroxide, usually calcium oxide and/or calcium hydroxide. It is also the name for calcium oxide which occurs as a product of coal-seam fires and in altered limestone xenoliths in volcanic ejecta. The International Mineralogical Association recognizes lime as a mineral with the chemical formula of CaO. The word ''lime'' originates with its earliest use as building mortar and has the sense of ''sticking or adhering''. These materials are still used in large quantities as building and engineering materials (including limestone products, cement, concrete, and mortar), as chemical feedstocks, and for sugar refining, among other uses. Lime industries and the use of many of the resulting products date from prehistoric times in both the Old World and the New World. Lime is used extensively for wastewater treatment with ferrous sulfate. The rocks and minerals from which these materials are derived, typ ...
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New Red Sandstone
The New Red Sandstone, chiefly in British geology, is composed of beds of red sandstone and associated rocks laid down throughout the Permian (300  million years ago) to the end of the Triassic (about 200 million years ago), that underlie the Jurassic-Triassic age Penarth Group. The name distinguishes it from the Old Red Sandstone which is largely Devonian in age, and with which it was originally confused due to their similar composition. Its upper layers consist of mudstones, but most of the formation consists of reddish to yellowish sandstones, interbedded with rare evaporite minerals such as halite and gypsum. These indicate deposition within a hot and arid palaeo-environment, such as a desert or sabkha.Benton MJ and Walker AD. 1985. Palaeoecology, taphonomy and dating of Permo-Triassic reptiles from Elgin, North-East Scotland. Palaeontology 28:207–234. Geographical distribution The New Red Sandstone was originally identified in Scotland, at quarries in Elgin. ...
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Pennine Coal Measures Group
The Pennine Coal Measures Group is a lithostratigraphical term referring to the coal-bearing succession of rock strata which occur in the United Kingdom within the Westphalian Stage of the Carboniferous Period. In formal use, the term replaces the Coal Measures Group as applied to the succession of coal-bearing strata within the Pennine Basin which includes all of the coalfields of northern England and the English Midlands. It includes the largely concealed Canonbie Coalfield of southern Scotland and the coalfields of northeast Wales and the minor Anglesey coalfield. The sequence consists in the main of mudstones and siltstones together with numerous sandstones, the more significant ones of which are individually named. Some are laterally extensive, others are more restricted in their range. There are numerous coal seams, again with some being more laterally continuous than others. Those which were economically valuable were named though any individual seam may have attracted di ...
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Worksop
Worksop ( ) is a market town in the Bassetlaw District in Nottinghamshire, England. It is located east-south-east of Sheffield, close to Nottinghamshire's borders with South Yorkshire and Derbyshire, on the River Ryton and not far from the northern edge of Sherwood Forest. Other nearby towns include Chesterfield, Doncaster, Retford, Gainsborough and Mansfield. Worksop had a population of 41,820 as of the 2011 Census and it is twinned with the German town Garbsen. History Anglo-Saxon and Anglo-Norman history Worksop was part of what was called Bernetseatte (burnt lands) in Anglo-Saxon times. The name Worksop is likely of Anglo Saxon origin, deriving from a personal name 'We(o)rc' plus the Anglo-Saxon placename element 'hop' (valley). The first element is interesting because while the masculine name Weorc is unrecorded, the feminine name Werca (Verca) is found in Bede's ''Life of St Cuthbert''. A number of other recorded place names contain this same personal name element. In ...
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Renishaw, Derbyshire
Renishaw is a village in the district of North East Derbyshire in England. It is in the civil parish of Eckington, Derbyshire, Eckington. Renishaw lies on the A6135 road between the villages of Eckington, Derbyshire, Eckington and Barlborough. To the west is a section of the Trans Pennine Trail long distance footpath which runs along a former railway line. Adjacent to this is the route of the Chesterfield Canal which passes along the edge of the village. The canal is being restored in stages, with this section having some clearance work done in preparation for the section from Staveley to the south being reinstated. While Renishaw is the name for the village as a whole, in respect of the group of roads that lie south of the A6135 road, A6135, in the section of the highway that is locally named as Main Road (between Hague Lane (B6419) and Emmett Carr Lane), that part is named Emmett Carr. To the northwest of the village is Renishaw Hall, a country house belonging to the Sitwell B ...
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Barlborough
Barlborough is a village and civil parish in the Bolsover district of Derbyshire, England. According to the 2001 census it had a population of 3,018, increasing to 3,261 at the 2011 Census. The village is near junction 30 of the M1 motorway and is about north of Bolsover. Notable residents * John Osborne, goalkeeper for West Bromwich Albion, who won an FA Cup winner's medal in 1967–68, was born here in 1940.Superstars in Stripes - John Osborne
West Bromwich Albion F.C. Official Site accessed June 2007 *
Francis Rodes Sir Francis Rodes (c. 1530–1588) of Barlborough Hall in the parish of Barlborough, Derbyshire, was an English judge who took ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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