Archaeological Investigations on the Motorway Service Area, Junction 8, M20 at Eyhorne Street, Hollingbourne
ARCHAEOLOGICAL INVESTIGATIONS ON THE
MOTORWAY SERVICE AREA, JUNCTION 8, M20
AT EYHORNE STREET, HOLLINGBOURNE
IAN R. SCOTT
with contributions by
Alistair Barclay, Paul Booth, Angela Boyle and Philippa Bradley
SUMMARY
The Oxford Archaeological Unit carried out a field evaluation and excavation
at the proposed site of a motorway service area adjacent to Junction 8 of
the M20 at Hollingboume, on behalf of Esso Petroleum Ltd. following
consultation with the County Archaeologist. The site (centred at N.G.R. TQ
824 552) is bounded on the south side by the M20 and on the north by the
London-Folkestone railway. The underlying geology is predominantly Gault
Clay with Folkestone Sands along the south edge of the site. The evaluation
consisted of 37 trenches and the excavation of seven large areas which
revealed evidence of prehistoric activity, predominantly of later Bronze Age
date, and some limited Romano-British and medieval activity.
There is a general scatter of worked flint over most of the site, some of
Mesolithic or Neolithic date but most is probably of later Bronze Age date.
The main evidence for later prehistoric activity consists of a concentration
(N.G.R. TQ 8244 5514) of later Bronze Age pottery associated with small
pits, at least two of which are of late Bronze Age date.
There are only small amounts of Romano-British and medieval pottery
from the site. The only dated Romano-British features were a single small
ditch or gully containing Romano-British pottery, and a large ill-defined
clay-filled feature, possibly a pond, which contained a large part of a single
cooking-pot. It would appear that the centre of Romano-British activity was
to the south of the present site close to and on the line of the M20. The
medieval pottery comes mainly from a single pit which contained sherds
from a twelfth- or early-thirteenth century cooking-pot and from a linear
feature. This was one of a number of ditches laid out in a rectilinear pattern
which were identified during the excavation. It is probable that these ditches
are of medieval date.
105
IANR. SCOTT
INTRODUCTION
In March 1995 the Oxford Archaeological Unit (hereafter OAU)
carried out an archaeological desk study as part of the Environmental
Statement at Eyhorne Street, Hollingbourne in respect of a proposed
motorway service area (MSA) on behalf ofEsso Petroleum pie. After
the grant of planning permission with an archaeological condition, a
programme of fieldwork was undertaken which comprised a field
evaluation in June 1995 followed by an excavation in OctoberNovember
I 995. The development site lies on the north side of the
M20 adjacent to Junction 8 at Hollingbourne, and is approximately
11 hectares in area. A strip up to 75 m. wide, which lies parallel and
immediately adjacent to the motorway, and which forms part of the
proposed route of the Channel Tunnel Rail Link (CTRL), was
evaluated on behalf of Union Railways Ltd as a separate exercise
(URL 1996). Further details of the excavations may be found in the
site archive. The archive and finds will be deposited with Maidstone
Museum and Art Gallery.
ACKNOWLEDGEMENTS
The author wishes to thank the developers, Esso Retail Ltd for their
financial support of the fieldwork and costs of publication. Thanks
are due to Peter Jeans of the Esso Petroleum Company, Jeffrey
S tepbenson of EPCAD Consultants, Keith Mason of Woods Warren
Consulting Engineers and Stephen Gregory of Turnkey Design
Partnership. Dr John Williams and Wendy Rogers of Kent County
Council set the Brief and approved the Written Scheme oflnvestigation
(WSI) for the fieldwork. At the time of the evaluation the site formed
parts of two separate farms and thanks are due to the owners, Mr and
Mrs. Parrett of Eyhorne Farm and Messrs. R.A. and N.J. Leggatt of
Woodcut Farm, for allowing access for fieldwork. When the excavation
took place the site had been purchased by Esso Retail Ltd. For OAU
George Lam brick was responsible for providing consultancy services
to Esso Petroleum for the Environmental Statement and the development
and monitoring of the proposals for the fieldwork reported here.
George Lambrick also commented on the text. Figures 1-11 were
drawn by Lesley Collett and Figure 12 by Paul Hughes of the OAU
graphics office. The processing of the environmental samples was
supervised by Greg Campbell of the OAU, and the assessment undertaken
by Dr Mark Robinson of the Environmental Archaeology Unit,
Oxford University Museum.
106
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
scale 1 :50,000
81 83 8S
Fig. 1. Site location
107
IANR. SCOTT
LOCATION, TOPOGRAPHY, GEOLOGY (Figs. I and 2)
The site lies at the scarp foot of the North Downs, between the villages
ofHollingbourne, Eyhorne Street and Bearsted (N.G.R. TQ 824 552).
In plan the development site is an elongated triangle; its north side is
bounded by the London-Ashford railway line and its south side by the
M20. On the south side of the M20 the landscape opens out into a
wide valley. The site lay across two fields and straddled an ancient
trackway (a continuation of 'Musket Lane'), which is now a public
footpath. The field to the west of the footpath had been previously
under arable cultivation, while that to the east was under permanent
pasture.
The elevation of the site is between 58 m. and 68 m. O.D. Generally
the site slopes to the south and west with the highest point at the east
end towards the north-east corner. The eastern field slopes down to
the south and west towards the footpath where it levels out to form a
small flat spur (centred on trenches 19-20 and 25-7). From here the
ground falls away to the west, south , and south-east. Towards the
west end of the site there is a shallow dry valley, which slopes west
towards the motorway; trench 3 8 was located at the top end of this
valley. The ground rises again west of the valley. There is a second
dry valley to the south-east of the spur, but this lies mainly within the
CTRL corridor and was not explored during the MSA fieldwork.
The site straddles the boundary between two geological deposits.
The underlying geology is mainly Gault Clay, with Folkestone Sand
beds which surface approximately along the line of the CTRL corridor
to the south-west (Geological Survey of Great Britain (England and
Wales), Solid and Drift, Sheet 288, 1976). The Gault Clay overlies
the Folkestone Sand Beds and at the interface is a thin mixed deposit
marked by the occurrence of a large sandstone gravel. Many trenches
revealed mixed deposits with varying proportions of clay, sand and
silt. In the dry valleys silty colluvial deposits were found to have
accumulated.
ARCHAEOLOGICAL BACKGROUND AND PREVIOUS WORK
Both the National Archaeological Record and the Kent Sites and
Monuments Record identify a number of sites in the general area of
the development site. These are predominantl:y found on the sandy
geology to the south of the motorway. Of particular note are a scatter
of Mesolithic flint to the south-west (N.A.R. No. TQ 85 SW 6), and
nearby the site of two late Bronze Age barrows, with early Saxon
108
0
so
553
552
551
550
Evaluation 1renches
r·--1 excavation areas
L .. -.
0 100
823 824 825
Snarkhurst Wood
c-:rrench 39
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14 Trenit' 40
Fig. 2. Location of Evaluation Trenches {l-37) and Excavation Areas (38-44).
827
553
11 l1a
r·-·-1 j iTrench 43
231L. _ J 24
r·-·-,
/-Ts ! Trench 42
IAN R. SCOTT
cremations (N.A.R. No. TQ 85 SW 5). A Romano-British burial
group was found at Crismill Farm (N.A.R. No. TQ 85 NW 6) to the
west of the site, and to the south a large Roman coin hoard (N.A.R.
No. TQ 85 SW 13) was found. A possible Saxon inhumation cemetery
has been identified further south (N.G.R. TQ 827 538).
More specifically, in the 1950s the construction of the Maidstone
Bypass (now the M20), immediately adjacent to and south of the
CTRL corridor (area centred around N.G.R. TQ 8227 5500), uncovered
the probable site of an Iron Age and/or Roman settlement and pottery
dated to the first and second centuries A.O. (N.A.R. No TQ 85 NW
11 ). A ditch containing late Iron Age pottery and a series oflron Age
burial urns were uncovered to the north of the road and to the south of
the bypass excavations revealed the foundations of a small ragstone
building, accompanied by first and early second centuries Roman
pottery, as well as a late Iron Age kiln.
The present site was the subject of a field walking survey as part of
the background work for the Environmental Assessment of the route
of the Channel Tunnel Rail Link. The results of that survey are not
published here but the overall patterns of finds recovered are briefly
outlined and related to the discoveries made during fieldwork on the
MSA.
The surface collection survey by OAU on behalf of Union Railways
Ltd. covered the CTRL corridor and part of the Motorway Service
Area site to the north (BRB 1991; URL 1994; 1995 ); it did not extend
into the area east of Musket Lane. Prehistoric worked flint included a
flint knife, from within the area of the proposed MSA development.
A flint scatter including a polished axe fragment was recovered in the
field located at the intersection of the motorway and existing railway.
Two small late prehistoric pottery scatters were found. One was
found adjacent to the east corner of the M20 balancing pond, the other
on the flat spur in the middle of the site. The latter can clearly be
related to the concentration of late Bronze Age material found during
the MSA evaluation.
Within the CTRL corridor the survey also produced a scatter of first
century B.C. to first century A.O. late Iron Age to early Roman
pottery; this concentrated in the strip adjacent to the M20 south-east
from the balancing pond. The subsequent evaluation of the CTRL
corridor revealed a section of substantial ditch with late Iron Age
pottery, which can be related to the discoveries made in the 1950s.
No comparable features or material were recovered from the MSA
site.
There are no major medieval sites in the immediate area, although
the surface collection for the CTRL produced a moderate scatter of
110
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
pottery, but not considered sufficiently marked to be recognised as a
significant concentration. In both Eyhorne Street and Hollingbourne
there are medieval buildings. All Saints, Hollingbourne is
fourteenth-century in date and Hollingboume Manor contains
thirteenth-century elements. Eyhome Street has two, possibly three,
hall houses of fifteenth-century date. Approximately 1.5 km. to the
north of the development area, close to Howe Court Farm, lie the
remains of a medieval moated site, possibly a Manor House, at Ripple
Manor.
SITE DESCRIPTION
Fieldwork Methodology (Fig. 2)
The fieldwork was undertaken in two stages. An evaluation comprising
37 trenches 30 x 1.90 m. (Fig. 2: nos 1-37) located a concentration of
later Bronze Age material centred on trenches 25-27, 29 and 36 (OAU
1995a). OAU standard evaluation recording was used for these
trenches, thus 1/11 denotes feature 11 within trench I. Following
consultation with the County Archaeologist and his staff, the decision
was taken to investigate further those areas which would be most
affected by landscaping during development. This did not include the
area containing the main concentration of later Bronze Age material;
this was located partly on the line of the bund which will separate the
MSA from the Channel Tunnel Rail Link and partly under an access
road, which with some engineering modification allowed these deposits
to be preserved.
The excavation comprised seven large trenches (Fig. 2: nos 38-44).
Single context recording was undertaken for these trenches but the
trench prefix has been retained on the section drawings. Trench 38
measured approximately 40 x 40 m. (= 1600 sq. m.), trenches 39 and
40 each 20 x 15 m. (= 300 sq. m. per trench), and trenches 41-44
each approximately 45 x 45 m. (=2025 sq. m. per trench). A total of
approximately 10300 sq. m. was stripped during the excavation. The
topsoil was stripped from both the evaluation and excavation
trenches under archaeological guidance using 360° tracked excavators.
The evaluation trenches were backfilled on completion of recording,
but the excavation trenches were left open and the spoil was moved to
a single dump using 25 ton 6 x 6 dumpers. The spoil was stockpiled
over the area which contained the concentration of later Bronze Age
material to afford it protection.
111
IANR. SCOTT
Soil conditions
The modern plough-soil was a light friable loam varying in composition
from a clay loam to a sandy loam and was between 200 and 360 mm.
thick. In a number of trenches the modem plough-soil sealed a further
loam layer which was interpreted as the remnant of an earlier
plough-soil. This layer was generally 90-120 mm. thick, although
occasionally as much as 200-250 mm. thick. The natural geology was
sealed beneath this older plough-soil, except in those areas where
colluvial deposits had accumulated. The natural subsoil was extremely
variable in the area examined and much post-depositional damage was
done to the pottery by the very tenacious nature of some of the soils (see
below). The acid nature of the soil also meant that animal bone did not
survive.
Report Structure
The results of the fieldwork were limited, but the presence of
quantities of late Bronze Age pottery, and the absence of significant
Iron Age or Romano-British material so close to a known site, justifies
the publication of a brief report on the fieldwork. The stratigraphic
description is limited to a summary of the major features, but the late
Bronze Age pottery, the small quantity of Romano-British pottery the
cremated human bone and the worked flint are also reported. These
materials fonn the bulk of the finds recovered from the site.
Context references
Evaluation features and deposits are referred to by trench number and
context number thus: trench 11 contexts 1, 2 etc. are labelled 11/1,
11/2 etc., trench 12 context 1, 2 etc. are labelled 12/1, 12/2, etc. In the
subsequent excavation, contexts were recorded using a single sequence
of numbers. In the published report these context numbers are prefixed
with the trench number for consistency and clarity (38/001, 39/101,
etc.)
Environmental data
The number of contexts suitable for environmental sampling was
small, and therefore only a limited number of soil samples was taken
for analysis - twelve samples during the evaluation and 16 during
the excavation - most of these from deposits containing charcoal.
Assessment of a selection of the samples ( 18 from 28) indicated that
mollusca were absent and that the predominant charred material was
112
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
oak (Quercus) charcoal. Details of the soil samples and records of the
sample processing can be found in the archive. Reference is made to
the environmental assessment of samples from the Late Bronze Age
pits (29/3 and 38/101), the possible cremations (14/5, 26/6, 31/6
and 42/405) and the Romano-British 'pond' (context 44/618) at the
appropriate places in the following site report.
RESULTS
Struck flint
The earliest evidence from the site was a scatter of worked flint found
on the surface of the natural geology, and occasionally, in the older
plough-soil. The scatter of flint was very thin, and no concentrations
were observed, although in the evaluation slightly more material was
recovered from the eastern part of the site. The material was largely
undiagnostic and consists of mainly unretoucbed flakes, pieces of
irregular waste, cores and some relatively undiagnostic retouched
forms. The dating of the material is difficult: much of it is probably
of late Bronze Age date, some individual pieces may be of Neolithic
or even Mesolithic date (see Bradley below).
Possible cremations
Four possible cremations were identified. The complete fills of the
pits were removed as samples for the recovery of bone and other finds
and for environmental assessment. Pits 14/6, 26/5 and 31/4 produced
very small quantities of human bone about which little further can be
said. Pit 42/405 produced a slightly greater quantity, and probably
represented a single individual, possibly male. All these pits were
small, only 26/5 (Fig. 6) was more than 0.20 m. deep, and only pit 26/5
produced any datable finds. These consisted of seven Late Bronze
Age (hereafter LBA) sherds, but these are probably redeposited, since
the feature is cut into a colluvial deposit (26/3) which also produced
LBA pottery. The dating of the features is uncertain. Soil samples
from pits 14/6 (fill 14/5), 26/5 (fill 26/6) and 42/405 (fill 42/404)
produced charcoal. In the case of 14/5 this was oak (Quercus)
charcoal, and in the case of 42/405, predominantly oak charcoal. Pit
26/5 produced large quantities of charcoal amongst which oak
(Quercus) was dominant, but which also included sloe or cherry
(Prunus). Pit 31/4 produced no charred material.
113
IANR SCOTT
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Colluvial deposits (Figs. 3 and 4)
The site contained two small dry valleys or hollows partly filled by
colluvial deposits. One valley lay to the east of the central spur, the
other to the west. The eastern valley lay largely within the CTRL strip
and was explored during the evaluation undertaken for Union
Railways (URL 1996): it is not discussed here. The colluvial deposits
in the western dry valley were initially explored in evaluation trench 3.
The depth of the colluvium (0.90 m.) was determined by means of
three test pits which were cut from trench 3. Two of these were
machine-cut and one was hand-excavated and produced 10 sherds of
LBA pottery from the main colluvial deposit (3/4). The colluvium was
further investigated in trench 38 (Fig. 4). Its extent was established in
plan (Fig. 3), although the edges of the deposits were not readily
distinguishable. Sections were machine-cut across the colluvium and
much of the exposed northern half of the deposit was machine-stripped
114
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59.S0m OD
59.S0m OD
IAN R. SCOTT
under archaeological supervision. The purpose of this operation was
to establish whether or not there were features, possibly ofLBA date,
sealed beneath the colluvium. One feature (38/36), a length of ditch
or trench, had been identified apparently disappearing under the
colluvium. When the colluvium was stripped no further evidence for
the feature was found, and therefore its relationship with the colluvium
remains unclear, but it is more likely to be later in date than the
colluvium.
The date of the colluvial material is uncertain. Pockets of colluvial
material were also found in hollows in trenches 25 (25/2) and 26
(26/3). In trench 26 the colluvium was sealed by the older ploughsoil.
In trenches 25 and 26, the survival of Late Bronze Age pottery
suggests that the colluvium had not been heavily ploughed subsequent
to deposition. Nonetheless, the presence of the LBA pottery can at
best provide a terminus post quern for the deposition of the colluvium.
Although the absence of later material is perhaps surprising given the
presence of nearby late Iron Age and Roman and medieval occupation
(see below), it is also the case that unstratified LBA material was
more generally spread than material from these other periods. The
absence of later material from the colluvium is not significantly
different from its comparable sparseness in more recent plough-soils.
While the activity which led to the deposition of the colluvium occurred
during or shortly after the late Bronze Age, it could equally have
occurred at almost any later period when pottery was finding its way
onto the site.
Late Bronze Age evidence (Figs. 5 and 6)
The evaluation revealed evidence, consisting for the most part of a
concentration of pottery, for late Bronze Age occupation mainly in
the vicinity of evaluation trenches 19, 25, 26 and 29 (Fig. 5). A single
Bronze Age feature (29/3, fill 29/4) was located (Fig 5). All that
remained of this pit was a shallow circular cut 0.35 m. in diameter and
0.08 m. deep, but this was packed with 186 sherds ofLBA pottery. A
small soil sample from this pit was found to contain oak (Quercus)
charcoal. Some evidence for LBA occupation was also recovered
from trench 20 to the north, trenches 27 and 41 to the east and 36 to
the south. This area was not excavated during the second phase of
fieldwork.
In trenches 25 and 26 thin colluvial deposits (25/2 and 25/3, and
26/3) were found. These appear to have survived in slight hollows in
the natural, and in all cases these deposits contained small quantities
of Late Bronze Age pottery. In trench 26 this deposit was sealed by
the older plough-soil.
116
25/4
Trench 25
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Trench 20
Trench 19
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26/ 13,B,5, 10 .• Trench 26
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-
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IANR. SCOTT
In trench 26 (Fig. 6) a small number of small pits or possible
postholes (26/13, /8 and /10), a possible cremation (26/5) and a linear
feature (26/4) were found all containing LBA pottery. The linear
feature was not excavated but appeared to be a continuation of the
pair of parallel ditches (36/13 and /15) found in trench 36 (Fig. 5).
The features in trench 26 were cut through the colluvial material and
it is probable that the pottery which they contain is redeposited and
that they date from after the Late Bronze Age. It is possible that the
linear features were medieval in date (see below). There is no other
material to date the features. In trench 27 the older plough-soil (27/2)
contained small quantities of LBA pottery. This area was explored
further by the stripping of trench 41, but little further evidence for
late Bronze Age occupation was found.
To the west of the main LBA concentration, and down slope from
the flat top of the spur, a second late Bronze Age pit 39/101 (fills
1 02-4, finds groups 119-123) was found during the excavation in
trench 39 (Fig. 7). This pit was lined with pottery and at least three
layers of sherds had been laid on the floor with their concave faces
down. The sides of the pit were also carefully lined with pot. The pottery
was remarkably only in its lack of diagnostic features. Unfortunately,
the pit had been cut through by field drains twice, with the result that
parts of the edge of the pit had been destroyed and most of the fill
disturbed. For this reason, sampling the fill for environmental data
was not thought worthwhile. Most of the fill was removed for finds
recovery. Pottery was recovered but no charred material was found in
sieving.
Small quantities of LBA pottery were found in other trenches,
particularly on the down slope to the west of the spur. This material
was almost certainly derived from the deposits and features on the spur
and spread as a result of subsequent ploughing. Small amounts of
LBA pottery and struck flint were found throughout the colluvial
deposits in the dry valley, where they were explored in trench 38
(Fig. 3).
Iron Age/Romano-British (Figs. 8 and 9)
In trench 34, at the extreme east end of the development site, evidence
for late Iron Age or early Roman occupation was recovered. A
clay-filled feature (34/7) was sectioned. It was cut into Gault clay and
backfilled with similar material. It was extremely difficult to define,
but was found to contain a large part of a small Romano-British jar
( context 34/6). This feature was further explored during the excavation
(trench 44)(Figs. 8 and 9). It appeared irregular in plan and there was
120
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
Trench 44
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Fig. 8. Plan of Trench 44
a suggestion of more than one phase of activity. Two sections were
cut by machine through the feature, and one of these confirmed that
the feature was indeed of more than one phase, but it proved impossible
to clearly define its limits (Fig. 9, section 1 ). Only a little additional
Romano-British pottery was recovered. A sample taken from layer
618 produced large quantities of charcoal, with oak (Quercus)
dominate, but alder (Ulnus) or hazel (Cory/us) also noted. Trench 37,
which lay to the south-west near the central spur contained a linear
feature (37/3 = 37/5) which was possibly of Romano-British date
(Fig. 10); it produced a single Romano-British sherd. Given the
proximity to a known settlement site under the slip road to the M20 to
the south (centred at N.G.R. TQ 8227 5500) it is perhaps a little
121
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section 1
44/612
'" 44/813
IAN R. SCOTT
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Fig. 9. Trench 44 sections (see Fig. 8 for locations).
surprising that so little Iron Age or Romano-British material was
found. 1
Linear features and medieval occupation (Fig. 10)
The small number of cut features recovered during fieldwork comprised
for the most part slight gullies or ditches. The overall pattern of these
features suggested that they represented field boundaries laid out in a
rectilinear plan. The best evidence for the field boundaries comes
from evaluation trench 36 where a series of six ditches was revealed
1 The evaluation undertaken on the CTRL corridor also in general produced only
limited Iron Age/Romano-British material, although in this case, a substantial ditch
with well-preserved pottery was located.
122
Trench 11 z - I
11/4 --·-·-·-·-·]1.-·-·-·-·-·-·-·-·-· 11/8 ·-:--,-
·
--- ·--·--·--· ·.
11/
6 ·--·--·--·--·--·--·--·--·
11
/---
11/15
59.50m OD j 11/ 1 i
·
! 11,2 1111• 1 [=-,--·--
11/3 11/3
11/4
Trench 37
j 11/1 j
11/2
- 60. 2SmOO
-;,,;- ....,.
11111---
11110
11/8
eo.oomo o
·-·-·-·-·-·-·-·-·-·-·-·-•-·-·-·-·-·-·-·-·-, , t'-&L--·-·-·---·-·-·-·-·-·-·-·--·--·J
{._.
37/1 7
630D V
37/3
37/4
37/5
63.00m OD
,,.- ..,...
-
6
37/8
o 5 10 m
--===--===--======::::!
scale for plans
0 2m
-=-=-=====
scale for sections
Fig. 10. Trenches 11 and 37 plans and sections.
IANR. SCOTT
(Figs. 5 and 6). This picture was confirmed by the results of the
evaluation on the proposed line of the Channel Tunnel Rail Link to
the south (URL 1996), where more boundaries were found laid out in
the same pattern.
A linear feature (11/4, fills 11/5 and /14) at the north end of trench
11 (Fig. 10) in the western dry valley, on a similar alignment to the
linear features found elsewhere on the MSA site, produced evidence
for a medieval date. The upper fill (11/14) of 11/4 produced a large
medieval sherd and pieces of ragstone. Other evidence for medieval
occupation was found in the trench: the fill (11/9) of pit 11/8 produced
seven medieval sherds of twelfth- to thirteenth-century date. There
were also two undated pits. A medieval sherd was also recovered
from one of the linear features (36/4; fill 36/5) in the trench 36.
Details of the medieval pottery can be found in the site archive. It is
probable that the rectilinear pattern of linear features which was
uncovered both in work on the MSA and during the Rail Link
evaluation is a field system of medieval date.
Later features
Much of the evidence recovered from fieldwork consisted of recent
field boundaries and drains (see for example features 007 and 031 in
trench 38).
FINDS
LATE BRONZE AGE POTTERY
Alistair Barclay
Introduction
The evaluation and excavation produced a total of 987 sherds (4093
g) of predominantly flint-tempered, hand-made prehistoric pottery of
mostly Late Bronze Age date. This report discusses a selection of the
assemblage recovered from the evaluation and excavation. The pottery
under discussion has a probable date range within the Late Bronze
Age ( 1150-700 cal B.C.). It includes a small number of featured
sherds. There is a small number of sherds which could be of middle
Bronze Age or Iron Age date, although neither the quantity nor the
contexts are of significance.
On the whole the condition of the material was poor and many
sherds had lost their original surfaces. The surface damage was
124
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
post-depositional caused by the sticky/tenacious character of the
archaeological fills from which the pottery was recovered.
Methodology
Tables 1 and 2 give a quantification of the assemblage, by weight and
sherd number, recovered from the excavation and the evaluation
(excluding refitting fresh breaks and sherds less than 10 mm. in
width/diameter). The pottery is characterised by fabric, form, decoration
and colour. The sherds were analysed using a binocular microscope
(x 20) and were divided into fabric groups by principal
inclusion type. OAU standard codes are used to denote inclusion
types. A = sand ( quartz and other mineral matter), B= black sand, F=
flint, G= grog, Q= quartzite, S= shell, L= voids ( either leached shell,
burnt organic or miscellaneous). Size range for inclusions: 1 = <1
mm. fine; 2 = 1-3 mm. fine-medium and 3 = <3mm. medium-coarse.
Frequency range for inclusions: rare = <3 per cent, sparse = <7 per
cent, moderate = 10 per cent, common = 15 per cent, and abundant =
>20 per cent.
Fabrics
Twelve fabrics have been identified and these have been placed into
six fabric groups:
Sand and flint-tempered
AF l Sparse colourless quartz sand and sparse fine calcined flint.
AF2 Sparse colourless quartz sand and sparse medium calcined flint.
AFQ2 Sparse colourless quartz sand, sparse medium calcined flint
and rare medium quartzite.
Black sand and quartz sand
BA l Common coarse black sand and sparse coarse colourless quartz
sand.
Black sand and flint-tempered
BF 1 Common coarse black opaque sand and sparse fine calcined
flint.
BF2 Common coarse black opaque sand and sparse medium calcined
flint.
Flint-tempered
FI Common fine calcined flint.
F2 Common medium calcined flint.
F3 Sparse coarse calcined flint.
125
TABLE I: QUANTIFICATION OF PREHISTORIC POTTERY FROM EXCAVATION CONTEXTS (SHERD NUMBER; WEIGHT (g))
Trench/ Sand and flint Black sand Black sand and Flint Leached Grog Total
Context and sand flint shell
AFl AFl AFO2 BAI BFl BF2 Fl F2 F3 SCl.)2 GA2 GB2
38/03 1, 4g 34, 97g 12,89g 2,20g 1,3g 50, 213g
38/19 I, 7g I, 7g
38/23 I, 4g 3, 19g 6,29g I, 2g 11, 54g
39/102-3 63, 54g 63, 54g
39/104 36, 74g 36, 74g
39/107 2,2g 7,5g 9, 7g
39/108 I, lg 1,2g _ 2,3g
39/110 2, 3g 1, 2g 13, 17g 16, 22g
-
39/111 2, 3g 2,lg 4,4g
39/117 I, 5g I, 5g
39/118 I, 3g I, 8g 2, llg
39/119 28, 102g 28, 102g
39/120 18, 100g 18, 100g
39/121 343,1415g 343,1415g
39/122 57, 682g 57, 682g
i'tl
00
§
39/123 39, 170g 39, 170g
40/203 4, 19g l, Jg 1,2g 6,22g
411302 I, 3g 9,48g 4,29g 14, 80g
41/402 I, 5g
I 5g
Total I, 4g 12, L5g I, lg 1, 2g 69,193g 2, lg 609,2760g 2,20g 1,2g I, 3g 1,2g 701,3030g
372
ARCHAEOLOGICAL INVESTIGATIONS AT EYHORNE ST., HOLLINGBOURNE
Shell-tempered
S(L)2 Common medium shell platelets sometimes leached.
Grog-tempered
GA2 Sparse medium rounded grog or clay pellets and rare coarse
colourless quartz sand.
GB2 Sparse medium rounded grog or clay pellets and sparse black
opaque sand.
Tables 1 and 2 give the breakdown of fabrics by context. Two fabrics
dominate the assemblages, the black sand and flint-tempered fabric
BF2 and the flint-tempered fabric F2. Fabric BF2 accounts for 24 per
cent by sherd number and 20 per cent by sherd weight of the total
assemblage and fabric F2 accounts for 70 per cent by sherd number
and 7 5 per cent by sherd weight. The remaining 10 fabrics ( 60 sherds)
account for 6 per cent of the total assemblage by sherd number.
A local source can be suggested for most of not all the inclusions
(quartz sand, black (glauconitic) sand, flint and shell) found in the
fabrics. The mineral composition of the black sand is most probably
glauconitic and these inclusions no doubt derive from the local
Cretaceous geology, possibly from beds within the Lower Greensand
(Gallois 1992, 29-38). Flint inclusions were nearly always calcined,
angular and deliberately added as filler or opening material to the
fabrics.
Assemblage Composition
The total assemblage from the fieldwork contained 20 featured
sherds, which are discussed below; a selection is illustrated in Fig.
11. The remainder of the assemblage is summarised in Tables 1 and
2 and in the discussion section below. The majority of the featured
sherds (16) were recovered during the evaluation, and only four in
the excavation.
Two pits (29/3 and 39/101) which contained LBA pottery were
excavated. No featured sherds were found in pit 39/101, but eight
featured sherds were recovered from 29/3 (fill 29/4) in evaluation
trench 29 (Fig. 11.3-8). These sherds consist of two rim sherds (Fig.
11.3-4), a decorated body sherd (Fig. 11.5), three sherds from a neck
cordon ( of which two are illustrated Fig. 11.6) and sherds from two
bases (Fig. 11.7-8). The other featured sherds were recovered from
colluvial deposits: 3/4 (two rims), 26/3 (base sherd and decorated
body sherd), 26/7 (?spindle-whorl fragment), 27/4 (rim) and 38/3
(two rim sherds); from later pits: 26/1 l (rim) and 30/6 (rim); and from
topsoil: 38/23 (two rims). The sherds selected for illustration are
127
.....
N
00
TABLE 2: QUANTIFICATION OF PREHISTORIC POTTERY FROM EVALUATION CONTEXTS (SHERD NUMBER, WEIGHT (g))
Trench/ Sand and flint Black sand Black sand and flint Flint Flint and Total
Context and sand grog
AFl AF2 BAI BFl BF2 Fl F2 F3 FG2
3D. 1, 2g 1, lg 2,3g 3/4 5, 15g 6,2 7g 11, 42g
512 1, 5g
1, 5g
6/us 1,24g
1,24g
13/5 5, Ilg 1,5g 6, 16g
17/2 1,4g 1,4g
19/3
1, 13g 1, 13g
20/7 2,5g 2, 5g
25/2 3, 15g 3,4g l,4g 7,23g
25/6 l, 4g 1,4g
26/3 7,20g 9,20g 3,14g 19, 54g
26/4 4, 7g 4, 7 g
26/6 3,8g 6,5g 2, 7g 11, 20g
26/7 l,l 7g 2,6g 3,23g
26/9 I, Sg I, 3g 2, 82
Trench/ Sand and flint Black sand Black sand and flint Flint Flint and Total
Context and sand grog
AFl AF2 BAI BPI BF2 Fl F2 F3 FG2
26/11 2, 5g I, lg 3, 6g
27/2 l, 23 g I, 8g 2, 31g
27/4 I, 3g 8,22g
9,25g
28/1 I, 5g I, 5g
29/4 149,541g 37,148g 186,689g
29/6 1,3g I, 3g 30/6 I,