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Bow Hill, West Sussex
Bow Hill is an elongated hill ridge, high, and running roughly from north to south in the South Downs, in the county of West Sussex, England.Ordnance Survey 1:25,000 ''Explorer'' map series, No. 120 It has a prominence of 74 metres. Location Bow Hill is the highest point of Stoughton Down which lies to the east of the village of Stoughton in West Sussex. The summit itself is 2 kilometres due east of Stoughton and about 7 kilometres northwest of the nearest large town, Chichester. To the south are Stoke Down and the village of West Stoke; to the east and southeast are the villages of West Dean and Mid Lavant in the valley of the River Lavant, to the north are East Marden and Chilgrove. Description Bow Hill is the highest point on a north-to-south running and steep-sided ridge and there is a trig point at the top. Its crest and upper slopes are densely wooded, but the lower slopes are open downland. Various tracks and bridleways run pass close to the summit and there is a ...
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Tump (hill)
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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East Marden
East Marden is a village on the spur of the South Downs in the Chichester district of West Sussex, England. It is within the civil parish of Marden, West Sussex. It is first mentioned in the Domesday Book as Meredone and was given in 1086 to Roger, Earl of Montgomery. The church, St Peters (UK Ordnance Survey grid reference SU807145), dates from the 12th century and is still used for worship every other Sunday. Its oldest house today dates back to 1728 ( Salzman, 1953). The village, some 100 metres above sea level, is in an area of unusually high rainfall. Its most famous landmark is the thatched well on the village green. The population has remained static for over a century.1861 Census/63 residents; 1991/60(Genuki) It is in the civil parish of Compton Compton may refer to: Places Canada * Compton (electoral district), a former Quebec federal electoral district * Compton (provincial electoral district), a former Quebec provincial electoral district now part of Mégantic-Comp ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Devil's Humps
The Devil's Humps (also known as the Kings' Graves) are four Bronze Age barrows situated on Bow Hill on the South Downs near Stoughton, West Sussex. They are situated on a downland ridgeway crossed by an ancient trackway, above Kingley Vale.Dyer 2001, p.171. The Devil's Humps are counted among the most impressive round barrows surviving on the South Downs. The Devil's Humps are within the Kingley Vale National Nature Reserve. The two bell barrows together with two pond barrows and a cross dyke are listed as Scheduled Ancient Monument 1008371,Historic England: The National Heritage List for England: List entry Number 1008371. while the two bowl barrows are listed as Scheduled Ancient Monument 1008372.Historic England: The National Heritage List for England: List entry Number 1008372. The barrows The four mounds form a small cemetery group running in a line southwest to northeast. The two southwestern mounds are located close together; they are bell barrows with a banked depressio ...
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Hillfort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. Many ...
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Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ...
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Goosehill Camp
Goosehill Camp is a prehistoric earthwork that dates back to the Iron Age. It consists of two concentric banks and ditches. The inner enclosure has one entrance and surround two levelled hut sites. Goosehill Camp is within the Kingley Vale National Nature Reserve, on the South Downs. Excavations Goosehill Camp's first recorded excavation was carried out by J. R. Boyden. This excavation was carried out between 1953 and 1955. An excavation took place between 2008-2009 and was carried out by the University College London's Institute of Archaeology, under Mark Roberts. These excavations were complemented by a topographical survey and a magnetometry survey. More recently, between 2014 and 2016 a field survey has been conducted, around Kingley Vale, by programme of volunteer based fieldwork, led under the guidance and support of professional archaeologists.Goosehill Camp was included in the survey. See also *Devil's Humps, Stoughton The Devil's Humps (also known as the Kings' G ...
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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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Tumuli
A tumulus (plural tumuli) is a mound of earth and stones raised over a grave or graves. Tumuli are also known as barrows, burial mounds or ''kurgans'', and may be found throughout much of the world. A cairn, which is a mound of stones built for various purposes, may also originally have been a tumulus. Tumuli are often categorised according to their external apparent shape. In this respect, a long barrow is a long tumulus, usually constructed on top of several burials, such as passage graves. A round barrow is a round tumulus, also commonly constructed on top of burials. The internal structure and architecture of both long and round barrows has a broad range; the categorization only refers to the external apparent shape. The method of may involve a dolmen, a cist, a mortuary enclosure, a mortuary house, or a chamber tomb. Examples of barrows include Duggleby Howe and Maeshowe. Etymology The word ''tumulus'' is Latin for 'mound' or 'small hill', which is derived from the ...
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Cross Dyke
A cross dyke or cross-dyke (also referred to as a cross-ridge dyke, covered way, linear ditch, linear earthwork or spur dyke) is a linear earthwork believed to be a prehistoric land boundary that usually measures between in length. A typical cross dyke consists of one or more ditches running in parallel with one or more raised banks. Univallate cross dykes typically have a flat-bottomed ditch while the ditches of multivallate cross dykes possess a V-shaped cross-section. A defining characteristic of a cross dyke is that it cuts across the width of an upland ridge or the neck of an upland spur.English Heritage 1990a. Cross dykes generally occur at altitudes over above mean sea level.English Heritage 1990c. Function Cross dykes were built over the course of approximately one thousand years from the Middle Bronze Age (c. 1500–1000 BC) onwards. Interpretations of the reason for their construction vary and include their use as defensive earthworks, cattle droveways, trackways, t ...
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Chilgrove
West Dean is a village, Anglican parish and civil parish in the District of Chichester in West Sussex, England north of Chichester on the A286 road just west of Singleton. The parishes include the hamlets of Binderton and Chilgrove. The civil parish has a land area of . The 2001 Census recorded 425 people living in 177 households, of whom 248 were economically active. The village is on the Monarch's Way long-distance footpath. West Dean is in the Lavant Valley in the South Downs and has a Church of England parish church and one public house, ''The Selsey Arms''. The church and most of the houses are built of flint, in most cases with brick quoins and window dressings. History West Dean The Manor of West Dean was in the ancient hundred of Singleton, but was not mentioned by name in the Domesday Book of 1086. West Dean is a large Anglican parish and in 1861 extended to of arable, pasture, and woodland with a population of 681. The parish included Chilgrove. Binderton The D ...
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River Lavant, West Sussex
The River Lavant is a winterbourne that rises at East Dean and flows west to Singleton, then south past West Dean and Lavant to Chichester. From east of Chichester its natural course was south to the sea at Pagham, but the Romans diverted it to flow around the southern walls of Chichester and then west into Chichester Harbour. History The Lavant may once have had its source north of Midhurst, with the increased drainage area possibly leading to size more akin to the River Rother; however, erosion and weathering over centuries have led to its current source and size. The Lavant's course has changed on multiple occasions, one significant instance being in Roman times when the river was believed to have been diverted through Chichester to provide drinking water for the town. The Lavant is believed to have made its way to the sea via Pagham Rife and Pagham Harbour. Newbury notes historians have conjectured this diversion may have taken place in either Roman or medieval times, ...
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