Park Hill, Lincolnshire
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Park Hill, Lincolnshire
Juicetrump Hill is a hill around half a mile north of Belchford and 4.5 miles north-east of Horncastle in Lincolnshire, UK within the Lincolnshire Wolds. The summit elevation is 124 m (407 ft) and it forms part of the slightly higher Park Hill with its summit of 140m just to the north-east. The Database of British and Irish Hills records Park Hill as having a height of , and a topographic prominence (drop) of , and being a TuMP ("Thirty and upwards Metre Prominence"). It is a limestone outcrop known as a Roachstone with the underlying Tealby Clays having been eroded at a faster rate. The Viking Way long-distance footpath runs along the western flank of the hill, though there is no public access to the summit itself. On the summit is a possible Neolithic long barrow, though this is disputed.{{Cite web , title=Heritage Gateway - Results , url=https://www.heritagegateway.org.uk/Gateway/Results_Single.aspx?resourceID=1006&uid=MLI42356 , access-date=2023-09-26 , web ...
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Lincolnshire Wolds
The Lincolnshire Wolds are a range of low hills in the county of Lincolnshire, England which run roughly parallel with the North Sea coast, from the Humber Estuary in the north-west to the edge of the Lincolnshire Fens in the south-east. They are a designated Area of Outstanding Natural Beauty (AONB), and the highest area of land in eastern England between Yorkshire and Kent.Ordnance Survey maps: Geology The Wolds are formed largely from a series of pure marine limestones formed during the Cretaceous period, known collectively as the Chalk Group. The chalk overlies a series of other sedimentary strata of late Jurassic/early Cretaceous age. The strata dip gently to the east and form a scarp which runs southeast from Barton upon Humber via Caistor before it loses its identity north of Spilsby. To the north of the Humber Gap, the same formations continue as the Yorkshire Wolds. The rock succession in stratigraphic order i.e. youngest/uppermost first, is this: *White Chalk Subgro ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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Belchford
Belchford is a village and civil parish in the East Lindsey district of Lincolnshire, England. The village is situated approximately north of Horncastle and just to the east of the A153. At the 2011 Census, the population of the parish was 255. History The village's history dates back to the Romans and the Vikings. In 1536, during the Reformation, the vicar of Belchford was hanged, drawn and quartered for treason, after leading a rebellion against the crown. Geography Steep hills and deep valleys surround the village. Belchford lies in the Lincolnshire Wolds, a designated Area of Outstanding Natural Beauty running from Louth in the north, to Horncastle in the south. The village attracts ramblers, and hang-gliders who use the ridges from the Bluestone Heath Road to launch into the valley. The Viking Way, a national long distance footpath, passes through Belchford by the Blue Bell Inn, on its way from the Humber in the north to Rutland in the south. Culture and communi ...
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Horncastle
Horncastle is a town and civil parish in the East Lindsey district in Lincolnshire, east of Lincoln. Its population was 6,815 at the 2011 census and estimated at 7,123 in 2019. A section of the ancient Roman walls remains. History Romans Although fortified, Horncastle was not on any important Roman roads, which suggests that the River Bain was the principal route of access to it. Roman Horncastle has become known recently as ''Banovallum'' (i. e. Wall on the River Bain). Although this Roman name has been adopted by some local businesses and the town's secondary modern school, it is not firmly known to be original. ''Banovallum'' was merely suggested in the 19th century through an interpretation of the '' Ravenna Cosmography'', a 7th-century list of Roman towns and road-stations, and may equally have meant Caistor. The Roman walls remain in places. One section is on display in the town's library, which was built over the top of the wall. The Saxons called the town ''Hyrne ...
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Lincolnshire
Lincolnshire (abbreviated Lincs.) is a county in the East Midlands of England, with a long coastline on the North Sea to the east. It borders Norfolk to the south-east, Cambridgeshire to the south, Rutland to the south-west, Leicestershire and Nottinghamshire to the west, South Yorkshire to the north-west, and the East Riding of Yorkshire to the north. It also borders Northamptonshire in the south for just , England's shortest county boundary. The county town is Lincoln, where the county council is also based. The ceremonial county of Lincolnshire consists of the non-metropolitan county of Lincolnshire and the area covered by the unitary authorities of North Lincolnshire and North East Lincolnshire. Part of the ceremonial county is in the Yorkshire and the Humber region of England, and most is in the East Midlands region. The county is the second-largest of the English ceremonial counties and one that is predominantly agricultural in land use. The county is fourth-larg ...
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Database Of British And Irish Hills
The mountains and hills of the British Isles are categorised into various lists based on different combinations of elevation, prominence, and other criteria such as isolation. These lists are used for peak bagging, whereby hillwalkers attempt to reach all the summits on a given list, the oldest being the 282 Munros in Scotland, created in 1891. A height above 2,000 ft, or more latterly 610 m, is considered necessary to be classified as a mountain – as opposed to a hill – in the British Isles. With the exception of Munros, all the lists require a prominence above . A prominence of between (e.g. some Nuttalls and Vandeleur-Lynams), does not meet the International Climbing and Mountaineering Federation (UIAA) definition of an "independent peak", which is a threshold over . Most lists consider a prominence between as a "top" (e.g. many Hewitts and Simms). Marilyns, meanwhile, have a prominence above , with no additional height threshold. They range from small hills to ...
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Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ...
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TuMP
The mountains and hills of the British Isles are categorised into various lists based on different combinations of elevation, prominence, and other criteria such as isolation. These lists are used for peak bagging, whereby hillwalkers attempt to reach all the summits on a given list, the oldest being the 282 Munros in Scotland, created in 1891. A height above 2,000 ft, or more latterly 610 m, is considered necessary to be classified as a mountain – as opposed to a hill – in the British Isles. With the exception of Munros, all the lists require a prominence above . A prominence of between (e.g. some Nuttalls and Vandeleur-Lynams), does not meet the International Climbing and Mountaineering Federation (UIAA) definition of an "independent peak", which is a threshold over . Most lists consider a prominence between as a "top" (e.g. many Hewitts and Simms). Marilyns, meanwhile, have a prominence above , with no additional height threshold. They range from small hills to ...
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Viking Way
The Viking Way is a long distance trail in England running between the Humber Bridge in North Lincolnshire and Oakham in Rutland. History The route was officially opened on Sunday 5 September 1976 at Tealby, by the Deputy Chairman of Lincolnshire County Council; it was to be opened by the chairman, John Hedley-Lewis, but he was ill, and died the following December. Hedley-Lewis was President of the local Ramblers' Associations, and a memorial stile was made for him on the route at Stenwith, a half-mile north of the ''Rutland Arms'' in Woolsthorpe-by-Belvoir. The Countryside Commission recognised the significance of the Viking Way as a high quality long distance walk linking other major routes in Eastern England, these being the Yorkshire Wolds Way at the northern end, the Hereward Way and Macmillan Way from Oakham and indirectly via the Hereward Way, the Jurassic Way from Stamford and the southern end of the Peddars Way from Thetford. Most of the route is designated as par ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ...
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Long Barrow
Long barrows are a style of monument constructed across Western Europe in the fifth and fourth millennia BCE, during the Early Neolithic period. Typically constructed from earth and either timber or stone, those using the latter material represent the oldest widespread tradition of stone construction in the world. Around 40,000 long barrows survive today. The structures have a long earthen tumulus, or "barrow", that is flanked on two sides with linear ditches. These typically stretch for between 20 and 70 metres in length, although some exceptional examples are either longer or shorter than this. Some examples have a timber or stone chamber in one end of the tumulus. These monuments often contained human remains interred within their chambers, and as a result, are often interpreted as tombs, although there are some examples where this appears not to be the case. The choice of timber or stone may have arisen from the availability of local materials rather than cultural difference ...
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