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Latitude: 51.2083 / 51°12'29"N
Longitude: -0.7414 / 0°44'29"W
OS Eastings: 488015.121313
OS Northings: 146205.121323
OS Grid: SU880462
Mapcode National: GBR DBC.5CZ
Mapcode Global: VHDY3.3WDL
Entry Name: Soldier's Ring hillfort
Scheduled Date: 30 November 1925
Last Amended: 12 January 1994
Source: Historic England
Source ID: 1007885
English Heritage Legacy ID: 20178
County: Surrey
Civil Parish: Seale and Sands
Built-Up Area: The Sands
Traditional County: Surrey
Lieutenancy Area (Ceremonial County): Surrey
Church of England Parish: Seale, Puttenham and Wanborough
Church of England Diocese: Guildford
The monument includes an oval enclosure, identified as a slight univallate
hillfort, situated on a steep-sided natural knoll of Greensand on the north
side of Crooksbury Hill. It is one of a pair of similar enclosures within 500m
of each other.
The enclosure is defined by a bank and outer ditch, with additional defences
on the south and north sides, and includes an area c.48m across. The bank
survives to a height of 0.5m and is 5m wide. The ditch has become partially
infilled over the years but is visible as an earthwork feature 4m wide and up
to 1m deep. Beyond the ditch on the north side of the monument the steep slope
has been scarped to form an additional defence, while to the south an
embankment has been constructed providing a strong rampart 16m wide and 2.4m
high. Without such a rampart, this area would have been particularly
vulnerable to attack.
MAP EXTRACT
The site of the monument is shown on the attached map extract.
It includes a 2 metre boundary around the archaeological features,
considered to be essential for the monument's support and preservation.
Source: Historic England
Slight univallate hillforts are defined as enclosures of various shapes,
generally between 1ha and 10ha in size, situated on or close to hilltops and
defined by a single line of earthworks, the scale of which is relatively
small. They date to between the Late Bronze Age and Early Iron Age (eighth -
fifth centuries BC), the majority being used for between 150 and 200 years
prior to their abandonment or reconstruction. Slight univallate hillforts have
generally been interpreted as stock enclosures, redistribution centres, places
of refuge and permanent settlements. The earthworks generally include a
rampart, narrow level berm, external ditch and counterscarp bank, while access
to the interior is usually provided by two entrances comprising either simple
gaps in the earthwork or an inturned rampart. Postholes revealed by excavation
indicate the occasional presence of portal gateways while more elaborate
features like overlapping ramparts and outworks are limited to only a few
examples. Internal features include square or rectangular buildings supported
by four to six postholes and interpreted as raised granaries, timber or stone
round houses, large storage pits and hearths as well as scattered postholes,
stakeholes and gullies. Slight univallate hillforts are rare with around 150
examples recorded nationally. Although on a national scale the number is low,
in Devon they comprise one of the major classes of hillfort. In other areas
where the distribution is relatively dense, for example, Wessex, Sussex, the
Cotswolds and the Chilterns, hillforts belonging to a number of different
classes occur within the same region. Examples are also recorded in eastern
England, the Welsh Marches, central and southern England. In view of the
rarity of slight univallate hillforts and their importance in understanding
the transition between Bronze Age and Iron Age communities, all examples which
survive comparatively well and have potential for the recovery of further
archaeological remains are believed to be of national importance.
Soldier's Ring hillfort survives well and contains both archaeological remains
and environmental evidence relating to the monument and the landscape in which
it was constructed. Together with the broadly contemporary site of Botany
Hill, 500m to the west, the site will enhance our understanding of settlement
and social organisation during the Iron Age period in this area.
Source: Historic England
Other
1728,
Ordnance Survey, SU 88/46,
OW819 SU92,
Source: Historic England
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