Ancient Monuments

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Multivallate hillfort at Berth Hill

A Scheduled Monument in Maer, Staffordshire

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Latitude: 52.9485 / 52°56'54"N

Longitude: -2.3174 / 2°19'2"W

OS Eastings: 378772.304959

OS Northings: 339054.303541

OS Grid: SJ787390

Mapcode National: GBR 03L.2YC

Mapcode Global: WH9C0.C4QZ

Entry Name: Multivallate hillfort at Berth Hill

Scheduled Date: 30 November 1925

Last Amended: 3 February 1995

Source: Historic England

Source ID: 1009771

English Heritage Legacy ID: 21569

County: Staffordshire

Civil Parish: Maer

Traditional County: Staffordshire

Lieutenancy Area (Ceremonial County): Staffordshire

Church of England Parish: Maer St Peter

Church of England Diocese: Lichfield


The monument occupies a prominent sandstone outcrop on the south east
periphery of Maer Hills, approximately 600m north west of Maer Hall, and
includes the earthwork and buried remains of a multivallate Iron Age hillfort
and the earthwork remains of a 19th century ornamental landscape garden.
The hillfort has an irregular plan governed largely by the outline of the hill
upon which it is located. The defensive earthworks enclose a central area of
approximately 3.75ha and include an inner rampart and ditch, beyond which, in
some sections, is a second rampart. The two ramparts have both been formed by
a re-definition of the natural hillslope; the inner by a combination of
cutting back into and building out over the hillside and the outer purely by a
process of dumping. The flat-topped, inner rampart which measures up to 15m
wide and rises to a height of 0.8m internally, is constructed of earth and
stone. The rampart is a complex structure which retains evidence of a complex
history of development. To the north, where the natural hillslope is less
steep, there is an outer rampart, 10m wide and 1m high. A ditch, up to 10m
wide, has been formed beyond the inner rampart. This earthwork is, in effect,
a terracing and steepening of the natural hillslope. A low, discontinuous bank
is visible, in parts, running along the outer lip of this terrace.
Access into the interior of the hillfort is by means of causeways in the
central part of the south west side and at the north end of the east defences.
The former is a 2m-3m wide inturned or funnel entrance which was originally
approached from the north west along a steep embanked causeway built along a
gully. The second entrance is marked by a break in the inner rampart, although
this area has been damaged by quarrying. A break in the north defences of the
site is thought to be modern in date and is approached by a track which cuts
through the outer defences at the north east corner of the site and climbs
diagonally up the face of the hill. The west side of this entrance is revetted
by a dry-stone wall which is thought to belong to the 19th century phase of
the site's history when it was incorporated in a landscaped garden. No
internal earthworks associated with the hillfort's occupation are visible, but
the buried remains of structures will survive beneath the ground surface. A
spring exists within the east part of the interior from which, during the 19th
century, water was piped to Maer Hall and the village of Maer by a member of
the Wedgewood family. An aqueduct which transported the water from the spring
remains visible terraced into the east side of the hill and has damaged a
section of the inner rampart in this area. This 19th century feature provides
evidence for later alterations to the hillfort's east defences and is included
in the scheduling.
During the 19th century the hillfort's defences, particularly in the north and
east parts of the site, were partly modified to create a series of garden
walkways set within an ornamental landscape centred on the remains of the
hillfort. In the north part of the site, a zig-zag pathway is visible leading
to a small platform within the hillfort's defences. This platform is thought
to have been created during the 19th century as a viewing area. A small
grotto, carved with the date 1824, has been cut into the rock face in the
north west part of the site and is thought to be associated with this phase in
the site's history. These ornamental features are interesting evidence for the
19th century reuse of the site and are included in the scheduling.
All fence posts are excluded from the scheduling, but the ground beneath these
features is included.

The site of the monument is shown on the attached map extract.

Source: Historic England

Reasons for Scheduling

Large multivallate hillforts are defined as fortified enclosures of between
5ha and 85ha in area, located on hills and defined by two or more lines of
concentric earthworks set at intervals of up to 15m. They date to the Iron
Age period, most having been constructed and used between the sixth century BC
and the mid-first century AD. They are generally regarded as centres of
permanent occupation, defended in response to increasing warfare, a reflection
of the power struggle between competing elites.
Earthworks usually consist of a rampart and ditch, although some only have
ramparts. Access to the interior is generally provided by two entrances
although examples with one and more than two have been noted. These may
comprise a single gap in the rampart, inturned or offset ramparts,
oblique approaches, guardrooms or outworks. Internal features generally
include evidence for intensive occupation, often in the form of oval or
circular houses. These display variations in size and are often clustered,
for example, along streets. Four- and six-post structures, interpreted as
raised granaries, also occur widely while a few sites appear to contain
evidence for temples. Other features associated with settlement include
platforms, paved areas, pits, gullies, fencelines, hearths and ovens.
Additional evidence, in the form of artefacts, suggests that industrial
activity such as bronze- and iron-working as well as pottery manufacture
occurred on many sites.
Large multivallate hillforts are rare with around 50 examples recorded
nationally. These occur mostly in two concentrations, in Wessex and the Welsh
Marches, although scattered examples occur elsewhere.
In view of the rarity of large multivallate hillforts and their importance in
understanding the nature of social organisation within the Iron Age period,
all examples with surviving archaeological potential are believed to be of
national importance.

The hillfort at Berth Hill survives well and represents a good example of this
class of monument. Despite partial excavation, buried features and artefactual
evidence associated with the occupation and development of the hillfort will
survive within the defensive ramparts and the site's interior. These internal
structures and the defensive ditch will retain environmental evidence relating
to the economy of the site's inhabitants and the landscape in which they
The earthwork and other remains of a 19th century ornamental landscape garden
centred on the hillfort provide unusual information reflecting the
contemporary preoccupation with archaeological sites and antiquity.

Source: Historic England


Books and journals
'Keele Archaeology Group Newsletter' in Hillfort at Berth Hill, , Vol. 6, (1966), 1
Challis, A J, Harding, D, 'BAR 20, Part 2' in Later Prehistory from the Trent to the Tyne, , Vol. 20, (1975), 45
Simms, B B, 'Transactions of the North Staffordshire Field Club' in Investigations of the Hillfort and Camp at Berth Hill, , Vol. 66, (1932), 91-100
RCHME, SJ73NE7 : Berth Hill IA hillfort, (1974)

Source: Historic England

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