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Latitude: 51.2351 / 51°14'6"N
Longitude: -1.6967 / 1°41'48"W
OS Eastings: 421271.219871
OS Northings: 148477.166049
OS Grid: SU212484
Mapcode National: GBR 4ZF.HVZ
Mapcode Global: VHC2N.J7W0
Entry Name: Boundary earthwork across Dunch Hill Golf Course
Scheduled Date: 6 March 1990
Last Amended: 3 January 1997
Source: Historic England
Source ID: 1015480
English Heritage Legacy ID: 10203
County: Wiltshire
Civil Parish: Tidworth
Built-Up Area: Tidworth
Traditional County: Hampshire
Lieutenancy Area (Ceremonial County): Wiltshire
Church of England Parish: TidworthHoly Trinity
Church of England Diocese: Salisbury
The monument includes a boundary earthwork of Late Bronze Age ranch type. It
is of bank/ditch/bank construction, with an overall width of c.12m. It can be
traced across the golf course but has been destroyed near the `Seven Barrows',
barrow group. It relates to the `Devil's Ditch' linear earthwork system.
MAP EXTRACT
The site of the monument is shown on the attached map extract.
Source: Historic England
The most complete and extensive survival of chalk downland archaeological
remains in central southern England occurs on Salisbury Plain, particularly in
those areas lying within the Salisbury Plain Training Area. These remains
represent one of the few extant archaeological "landscapes" in Britain and are
considered to be of special significance because they differ in character from
those in other areas with comparable levels of preservation. Individual sites
on Salisbury Plain are seen as being additionally important because the
evidence of their direct association with each other survives so well.
Boundary earthworks which include linear earthworks, so called ranch
boundaries, dykes and cross ridge dykes are particularly well preserved in the
Salisbury Plain Training Area. They provide important evidence of prehistoric
landholdings, land reorganisation and changing agricultural practices through
time.
Source: Historic England
Other
Trust for Wessex Archaeology, (1987)
Wiltshire Library & Museum Service, (1987)
Source: Historic England
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