Monument records in the NRHE AMIE database were created or amended whereappropriate. The project recorded 655 previously unknown archaeological features <strong>and</strong>amended details for 265 records.The monument record consisted of a textual description of the site linked to indexedlocation, period, type <strong>and</strong> form of evidence. The record also included digital crossreferences to other monuments <strong>and</strong> datasets (usually the HER or scheduling information)as well as a list of the main aerial photographs <strong>and</strong> other sources for the site. An Eventrecord in the NRHE AMIE database was created to provide data on project scope <strong>and</strong>procedures. Archive records were created for each quarter sheet. The Event <strong>and</strong> archiverecords are linked to each monument record.All data <strong>and</strong> documentation relating to the project was archived at the <strong>English</strong> <strong>Heritage</strong>Archive (formerly the National Monuments Record). Full monument records are availablevia Pastscape (www.pastscape.org.uk). <strong>Mapping</strong> <strong>and</strong> monument records are available onrequest from the <strong>English</strong> <strong>Heritage</strong> Archive Services. All data was supplied to the EastSussex HER.DitchLevelled Ridge & FurrowBankExtant Ridge & FurrowStructure (e.g Buildings)Large Area FeatureLarge cut feature e.g. quarrySlopeFigure 3 <strong>Mapping</strong> conventions.© ENGLISH HERITAGE 5 22 - 2013
NEOLITHIC LONG BARROWSIn the absence of either causewayed enclosures or flint mines from the project area, theearliest monuments encountered are a series of probable or possible Neolithic longbarrows: Money Burgh (AMIE: 406246), Camel’s Humps (406570), Windover Hill(408708), Hunter’s Burgh (408732), Litlington (408791), <strong>and</strong> Exceat (470226). A possiblenew discovery was seen as cropmarks at Rathfinny Farm (1568872). Further long barrowslie just outside the project area, for example: Long Burgh (408646); Alfriston (408685);<strong>and</strong> Firle Beacon (405738).Although the Sussex long barrows featured prominently in explanatory models for thedevelopment of the Neolithic across the South Downs (For example Drewett 1978,2003; Russell 2001, 2002), there has been surprisingly little fieldwork undertaken on them.Sussex’s causewayed enclosures <strong>and</strong> flint mines, many of which were discovered duringthe inter-war years, have seen many episodes of investigation during the 20 th century.However, the only East Sussex long barrow to be excavated was the mound at Alfriston(Drewett 1975), located just outside the project area.The first publication dealing specifically with Sussex long barrows was by Herbert Toms,curator of Brighton Museum <strong>and</strong>, in the 1890s, assistant to Pitt Rivers during some of hiskey excavations on his Cranborne Chase estate. Toms’ 1922 paper on the Sussexmounds featured measured surveys of all 5 long barrows known at the time, 3 of them –Money Burgh, Camel’s Humps, <strong>and</strong> Windover Hill (which he discovered shortly aftersurveying the other 4) – located within the project area. Another, Hunter’s Burgh, wasnoted soon after on aerial photographs. The number has risen gradually since then, ofcourse, but one principal feature of long barrow distribution on the Sussex Downs hasremained relatively constant – most lie in the area of downl<strong>and</strong> between Brighton <strong>and</strong>Eastbourne.Perhaps the key development of recent decades was Drewett’s (1975, 1978, 1986 etc)efforts to distinguish a class of ‘oval barrow’ in the wake of his excavations at Alfriston.These, he argued, were shorter than long barrows generally, their mounds – as the namesuggests – more oval than long (or trapezoidal), <strong>and</strong> – on the basis of his excavations atthe Alfriston example <strong>and</strong>, subsequently, North Marden in West Sussex – later in datethan the larger long barrows. Consequently they could be seen as an intermediate stagebetween the long mounds of the earlier Neolithic <strong>and</strong> the round mounds of the BronzeAge. The idea of a distinct class of oval barrows within Sussex has come in for severecriticism (For example Kinnes 1992; Russell 2001, 2002; Field 2006 etc) – barrows ofsimilar dimensions <strong>and</strong> morphology are quite widespread across southern Britain (Forexample the so-called ‘Cranborne Chase Type’), <strong>and</strong> there is no evidence for them beingmarkedly later, either individually or as a class, than any other kind of long barrow.The recent project focusing primarily on the dating of causewayed enclosures, usingBayesian analysis (Whittle et al 2011), noted of long <strong>and</strong> oval barrows in Sussex that© ENGLISH HERITAGE 6 22 - 2013
- Page 1 and 2: RESEARCH REPORT SERIES no. 22-2013S
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Figure 33 Trenches aligned approxim
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The aerial photographs taken by the
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However, for his painting Coastal D
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war aerial photographs show a group
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Figure 40 Camouflage netting over t
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Description of the current Long Man
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which would certainly fit with sugg
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separate from it. The toes of the t
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other parts of the body, and indeed
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lip of a large chalk quarry, was, a
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something for which the likes of Pe
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Hill and the Lavant Caves, both nea
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to the present day…’ (Butler &
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least was unsupported by evidence f
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CONCLUSION AND RECOMMENDATIONS FOR
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documentary sources or fieldwork. N
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Barber M, Wickstead, H in press Dam
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Drewett, P 1978 Neolithic Sussex, i
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Lowry, B (eds) 2001 20 th Century D
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ENGLISH HERITAGE RESEARCH AND THE H