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Thoughts on the archaeology of the Upper Basin,
Faversham Creek
Dr Patricia Reid
Honorary Archaeologist for the Faversham Society
Nov 2008
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View across Stonebridge Pond looking south east
across Flood Lane, in 2007
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Thoughts on the
archaeology of the Upper Basin, Faversham Creek
Introduction
This part of Faversham is bounded
to the south by the north side of West Street (numbers
64 to 78), to the west by the Westbrook and Stonebridge
Pond, in the north by Faversham Creek into which the
Brook and Pond feed and to the east ultimately by North
Lane (Fig 1). It is nowadays a quiet and attractive
area, with the Flood Lane Recreation Area particularly
idyllic. Yet this has not always been the case, as this
paper will show.
A number of recently available
sources have been drawn upon to build up the narrative
of this zone. These include:
-
Four test pits, a
geo-resistivity survey and a surveyed profile
carried out as part of a Community Archaeology
project Hunt the Saxons in 2005/61
-
An archaeological evaluation
carried out in 1991 after the demolition of the Gas
Works and before the building of a Coop superstore
on the site2
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An archaeological evaluation
carried out at nearby Ordnance Wharf in 20053
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A hydrographic study of
Faversham Creek navigation, carried out in 20054
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A recently published
documentary study of Faversham as a port in the 16th-18th
centuries5
Fig 1 shows the locations of the
various archaeological investigations.
The paper also draws upon the large
archive of maps and photographs at the Fleur de Lis
Heritage Centre in Faversham, on such stalwarts as
Swaine’s 1969 survey of historic buildings in Faversham6, the knowledge of experts in Faversham history and
local residents with long memories. Philp’s published
account of the archaeology revealed in the sewage shaft
sunk near TS Hazard in 19657 is also very relevant.
Although this short paper will
raise as many questions as it answers, it should form a
useful contribution to any decision making about the
future of this odd little area, which is already under
pressure from a new set of development issues in the 21st
century (see last part Things to Come )
Unless otherwise indicated, all photographs have been
taken by Jim Reid of FSARG. Any use of these or other
material from this paper should be credited to the
Faversham Society.
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Fig 1:
Excavations in the study area
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Key
Hunt
the Saxons Test Pits: 1: TP24 2: TP22 3:
TP23B 4: TP23A 11: TP9
Gas Works evaluation: 5: South Section
6: line of main trench along which 8
sections were recorded
Sewage Shaft: 7
Ordnance Wharf evaluation trenches: 8
Davington Priory: 9
Davington Barn evaluation: 10
Roman burial site (found in 1770) shown on map.
Geo resistivity survey area
1)
Main
research issues
The
main topics are as follows
a) Where was the head
of the tide in the past and how and why has this changed
over time?
Flood Lane lies at the
present head of the tide in Faversham creek, with the
waters of the Westbrook and Stonebridge Pond held back
by sluices (Fig 1). No systematic research has been done
on the tidal situation in pre-sluice times. Due to post
glacial subsidence in SE England, sea level is higher
than, say, 2000 years ago8 and one would
expect tides to penetrate further inland nowadays than
in the past. Downstream, however, considerable silting
has taken place, along with land reclamation9 10.
Anything which can throw light on this complex process
will be useful.
b)
How was this area settled in early (pre-16th
century) times?
This corner of Faversham
is often assumed to have been continuously settled since
at least the Roman period11. The use of this
part of the river for shipping e.g. from the nearby
Roman settlement of Durolevum12 seems likely,
as does the use of the stream for milling: both uses
are mentioned in documents from the mid-medieval period
onwards13. No archaeological evidence has
been found for these activities in the early period, and
testing of these assumptions is needed.
c) Industrial
development
The rapid development of
relatively large scale industry from the 16th
century onwards in this zone and its complete
disappearance by the late 20th century needs
careful charting, not least because of regeneration
proposals for the area under consideration.
d)
The people
Changes in the
lifestyles of the local people in relation to the
changes noted in (c) are of key interest in
thiscommunity archaeology project.
It is
hoped that this paper will make some small contribution
towards answering these questions and be able to
identify possible ways forward.
2)
The question of
tides
Of
the above mentioned sources, only the Gas Works
Evaluation (GWE) and the Ordnance Wharf Evaluation (OWE)
can contribute directly to the question of river/marine
deposits. The four Hunt the Saxons (HSX05) test
pits went to a maximum depth of 1.2 metres (c 3.5m OD)
and did not reach any silt layers. Three of these test
pits (23A, 23B and 22) were in gardens at the southern
end of the area, comparable only to GWE profile 8 and
the South Section. Profile 8 reached the natural (head
brickearth) at c OD 3.2. Other GWE profiles have the
natural at greater depths, or not encountered at all.
Fig 2 shows the range of heights covered by the various
excavations and their relationship to modern sea level.
Fig 2
also shows information coming from one of the few deep
excavations to have taken place close to Faversham
Creek. This was the boring of a new shaft for a sewage
pumping station in 1965 just down stream from the main
sluice on the town (east) side14. Starting at
an OD of c 3.5m and penetrating an initial make-up
layer, the shaft went down through, in total, around 6m
of ‘grey-black mud silts’15. At around 0 OD,
150 large sherds of 13th century pottery were
recovered, along with portions of leather shoes.
Ranging from around 0 OD to + 1.5 OD were upright wooden
rectangular posts, running east-west, with more posts
slightly further down. These posts are tentatively
interpreted as remains of a medieval wharf or staging
from which the 13th century rubbish went into
the mud.
This
would give the bank-foot 13th century creek
bed at present day 0 OD, with the wharf (presumably at
bank-top level) at around 1/1.5 OD. The two metres of
silts above the pottery deposit were seen by Philp as
having accumulated subsequent to the deposition, and
then sealed by wharf building in the late18th
- 19th century. At a depth of -2.5m, a thin
peat layer was revealed which Philp sees as an ancient
land surface of unknown date.
Table
1 shows the top OD level of silts as identified in the
Gas Works and Ordnance Wharf excavations and the 1965
sewage shaft. There is close agreement between the top
levels of river/marine deposits at the three locations
i.e. 2.5 m OD, even though there are uncertainties about
the contribution of dumps from dredging (see later, Part
4). All of the silts exposed in excavations are overlain
by later make-up of rubble and surfaces (see Fig 2). In
practice, this suggests that the medieval bank lies
below the top silt levels in the reclaimed areas with
the bank-foot medieval creek bed 2.5 m below this.
In 2005 a study of Faversham Creek basin
was carried out by HR Wallingford, Hydraulics
Consultants16, to inform decisions about
regeneration of the Creek basin. Although they were
only interested in changes in silt levels since 1993,
their data is useful for the purposes of this paper, and
is partly summarised in Table 2. Fig 3 shows the
locations of the cross sections used in the Navigation
Study.
Table 1: taken from
published reports
Ordnance Datum (OD) refers to mean sea level at
Newlyn, Cornwall, measured for the period
1915-1921. Due to isostatic subsidence, the
equivalent mean sea level figure for 1300AD was
lower down in absolute terms. A peat layer found at
-2.5.OD in the pumping station shaft is almost
certainly a much earlier land surface of uncertain
date: in the post-glacial prehistoric period, local
sea level was much lower than now.
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Intervention |
Stratigraphic location
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OD in metres |
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OWE trench B2 |
Top of ‘pure’ silts |
2.4 |
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OWE trench C |
Top of ‘pure’ silts |
2.0 |
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OWE trench D |
Top of ‘pure’ silts |
3.0 |
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OWE trench E |
Top of ‘pure’ silts |
Not reached at 2 (structural
intervention) |
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GWE profile 1 |
Top of alluvium |
2.6 |
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GWE profile 2 |
Top of alluvium |
2.6 |
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GWE profile 3 |
Top of alluvium |
2.6 |
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GWE profile 4 |
Top of river deposits |
2 with reeds and straw at
1.75 |
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GWE profile 5 |
Top of river deposits |
2.0 |
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GWE profile 6 |
Top of river deposits |
2.0, with waterlogged wooden
upright |
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Pumping station |
Top of silts |
c 2.5 |
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Pumping station |
Top of wooden posts |
c 1.5 |
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Pumping station |
Pottery layer |
0.0 |
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Pumping station |
Peat layer (under silts) |
-2.5 |
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HSX05 TP24 |
Base of pit |
3.5 No silt revealed |
Table 2: Taken from the HR Wallingford report
NB: Heights were given based on Chart Datum (CD) and
have been converted into OD using a constant of 2.8
supplied by Medway Ports Authority17.
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Profile
numbers
and dates |
Max. height OD of
bed level 1m from
north (west) bank |
Min. height OD of
bed level
in profile |
Max. height OD of
bed level 1m from
south (east) bank |
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A1 |
1983 |
2.5 |
-0.3 |
1.0 |
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1994 |
2.9 |
0.1 |
0.9 |
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2005 |
2.9 |
0.3 |
1.0 |
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A3 |
1983 |
2.7 |
-1.0 |
0.6 |
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1994 |
2.9 |
0.3 |
1.6 |
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2005 |
2.9 |
0.2 |
1.5 |
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A5 |
1983 |
1.7 |
0.0 |
0.7 |
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1994 |
2.9 |
0.1 |
0.5 |
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2005 |
2.9 |
0.2 |
0.5 |
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A8 |
1983 |
2.9 |
-0.2 |
0.0 |
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1994 |
2.9 |
-0.5 |
0.0 |
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2005 |
2.9 |
0.2 |
0.4 |
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Fig 2: range of depths of excavations in the
Upper Basin and surrounding areas
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Fig 3: Cross
sections of Faversham Creek used in the
Wallingford report From sluice: A1, A3, A5, A8
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As can be seen from Table
2, the bed level on the town (south/east) side of the
creek is much less than the 2m OD top of the silt
identified in the excavations, and at or close to the
OD level of the 13th century deposits in the
Sewage Shaft (Table 1). What has happened to Philp’s 2m
of post-1300 silt?
The
history of this part of the creek is one of
disturbances, with at least four major interventions:
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1559: building of the first main sluice to be used
to flush the creek. The location was just to the
west of the current main sluice.18
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By 1710: the channel had been rerouted slightly to
the east and a new sluice built.19
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Late 18th century: the channel rerouted
westwards close to its former position and a new
sluice built, with the creek widened and
straightened.20
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Mid 19th century: major dredging and
brick reinforcement of wharves in the upper basin.
This was mainly to accommodate greatly increased
coal imports for the gas works.21
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Fig 4: The
TS Hazard area in c 175022
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Fig 4
also shows clearly an embayment for small craft next to
the 15th century Town Warehouse (nowadays
known as TS Hazard). As far as I can tell, this
embayment is the location for the sinking of the sewage
shaft that found the 0.0 OD 13th century
pottery, and confirms the long-term usage of this part
of the Creek frontage as a wharf (Town Quay).23
The late 18th century shift of the channel
westwards must have filled in this embayment and sealed
it from the modern creek. The later extensive dredging
of the late 19th century
must have removed huge
quantities of mud and silt and although they were
supposed to dump it ‘not less than 60 feet from the
creek in fields’24 one wonders just how far
from the bank this material actually went. Is this some
of the made ground on the Gas Works site? Perhaps
because of this dredging, the modern course of the
Westbrook at low tide runs close to the east bank. It
seems that only on the west side of the Creek Upper
Basin, where there were no wharves and little settlement
that silt has been allowed to accumulate to great
depths.
Allen et al see GWE
Profile 8 and the South Section as showing an early bank
side location. They suggest that in that area the Creek
bank was formerly about 60m inland from its current
position, with reclamation taking place by revetment and
infill around the late 17th century to give a
channel much the same as at present. Presumably the
wooden upright (Profile 6) at c2m OD and reeds/straw
deposits (Profile 5) at c 1.75 OD date to before this
reclamation took place. The pottery amount was small,
but sherds ranging in date from AD1175 to the 17th
century recovered from the South Section in silty clays
suggest that this area was adjacent to occupation i.e.
that these sherds were debris thrown from the sloping
bank (back gardens of West St houses) into the shallow,
muddy stream/creek.25
Some kind of control of
the Westbrook itself does, however, seem to date back at
least until the early 16th century... A
pictorial map of 1520 shows what seems to be a muddy
millrace coming along the present Westbrook course to
meet a main stream coming down on the western side of
the Mill?26 The main difficulty here relates
to the adjacent Stonebridge Pond. The curious layout is
a consequence of the important gunpowder industry which
developed here ‘in the time of Queen Elizabeth if not
earlier’.27 These modifications of the
stream/creek were in place by 1750 but the start date of
the Stonebridge pond complex is uncertain at present.28
Even the course of the pre-gunpowder stream/creek is not
known. Although the contours of the basin suggest a
route to the west, it is quite possible that water
impoundment for other uses of water power predates the
gunpowder industry in this area (see later, Part 4). The
complete lack of environmental archaeological evidence
means that the penetration of the tide in pre-gunpowder
times remains a mystery.
Finally, the location of
the medieval and earlier banks of the Upper Basin a)
along the stretch between the sluice and the Coop
superstore site on the east, and b) between the sluice
and Ordnance Wharf on the west, remain largely
uninvestigated both archaeologically and historically:
this will be addressed along with other issues in the
last part of this paper.
3) Early settlement (up to
medieval)
The Ordnance Wharf and most of the Gas Works
excavations did not find anything earlier than 19th
century: indeed, few finds other than various
rubbles are reported from either site, though this
could be to do with the conditions at the time of
excavation and the methodological approaches. This
part will use the four Test Pits (where all material
was meticulously sieved)29 and the South
Section and profile 8 from the Gas Works
excavations. Of these, all except TP24 are on what
Allen et al identified as the former bank/ bank edge
of the early river/creek.
Although artefactual evidence for Roman settlement
had been found very close to this area30
and is abundant in the Faversham area31,
only one small, much-abraded sherd of Roman pottery
was identified from this area (TP23A) The absence of
Saxon occupational evidence is perhaps less
remarkable, being generally far less abundant.
Pottery from around AD1150 to 1500 was, however,
found in all of the Test Pits and in the GWE South
Section.
Table 3: Medieval pottery
The numbers show weight in grams and, in brackets,
the percentage of medieval pottery in the
appropriate Spit. Weightings have been applied in
cases where Spit 4 was not fully excavated.
| |
Spit 1
(0-30cm) |
Spit 2
(31-60cm) |
Spit 3
(61-90cm) |
Spit 4
(91-120cm) |
|
TP24 |
12
(8%) |
0 |
8
(10%) |
0
|
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TP22 |
10
(1%) |
16
(0.8%) |
55
(2%) |
75
(13%)* |
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TP23A |
12
(1%) |
23
(7%) |
8 (3%) |
276
(54%) |
|
TP23B |
0 |
0 |
0 |
22
(100%) |
CWE
South Section |
Fill (11)
: one sherd AD 1175-1250, depth 1.3m
Fill (3) : several
sherds, storage jar, AD 1375-1500, depth
1.2m |
* includes 2 sherds
Saxo-Norman AD 1150-1200
The South Section
sherds came from grey-green silty clay contexts,
seen as fluvial, i.e. the broken pottery had been
dumped in shallow muddy frequently flooded ground at
the foot of gardens. The Test Pit medieval pottery
was, however, from clay matrices. As is typical of
garden deposits, a complicated sequence of
mini-events (digging rubbish pits, turning over
soil, dumping grate ash, importing top soil,
improving soils, terracing using demolition
materials, surfacing paths) has resulted in churned
deposits. These deposits are, however, often
sandwiched between undisturbed strata which are
outcomes of specific events (e.g. demolition layers
or occupational surfaces). Even with churned
deposits, the frequency of older pottery does
usually increase with depth except in the non-bank
side Test Pit 24.
TP 23B bottomed out initially with the base of a
demolished wall running north-south (left in situ)
and then, 10cm further down to the west, a cobbled
surface. The only pottery found in the slot formed
by the wall base and cobbles was medieval. TP23A,
higher up on a terrace closer to the house, bottomed
out around 1.1.m with what appeared to be a
horizontal lath and plaster wall, which was
interpreted as a remnant of the house which had
occupied the site previous to the present house
built around 1640. Yet the 54% of the pottery in
the deposits immediately above the plaster was
medieval, the rest being 16th-17th
century with no 18th- 20th
century pottery content. Possibly this horizontal
wall was a remnant of an even earlier property, or
perhaps the covering layer was imported from a
nearby garden or farmland.
TP 22 was not layered in the same way and was
excavated to the full depth permitted (1.2m). Spit
4 was dominated by 16th-17th
century pottery with other finds such as a Nuremburg
Jetton (SF46) and five 17th clay pipes in
a soft brown loam-clay matrix. The amount of 18th-20th
century pottery was negligible. Here the medieval
content is residual, working its way ‘upwards’
through garden-working processes. The house
associated with this Test Pit is one of the oldest
surviving buildings in town (15th
century), and the rear ground floor is now partially
‘basementised’, due to the build up of the garden
deposits.
The GWE profile 8 showed natural brickearth reached
at a depth of c2m from a start point of 5.1 OD.
None of the Test Pits penetrated as deeply (see fig
2) and our feeling was that we were down to a
dominantly 16th-17th century
level at the bottom of Test Pits 22 and 23A. Test
Pit 23B possibly exposed earlier deposits, and
dating of the cobbled surface (rounded beach pebbles
about 8 cm diameter) would have been useful.
Nine 15th century houses still stand in
Lower West Street32 and the Test Pits and
GWE South Section have provided evidence for
continuous occupation back to AD1150 on the Creek
side. The fact that no evidence was found for
earlier activity may simply be a reflection of the
depth of the garden deposits in this area.
4) The rise
and fall of industry.
This part relies
mainly on evidence from maps and documents,
although much industrial debris and make-up was
found in all of the excavations.
A mill for
Faversham is recorded in the Domesday Book, and
documents relating to the Maison Dieu at
Ospringe refer to mills owned on the Westbrook.33
The precise location of most of these early
mills is not known and the industrial process
carried out is not recorded but was probably
corn milling. The earliest definite information
comes from the 1520 pictorial map mentioned in
part 1 above and shows an undershot mill built
up over the stream supported by a stone wall.
The 1520 mill does look like a tidal mill. Tidal
mills were common by the 16th century
but the widespread assumption that the Saxon
(Domesday) mill was also tidal is less
justifiable, although not impossible – the
earliest known tidal mill in Kent is one on
Dover harbour, mentioned in about AD 1070 as an
obstruction to shipping.34
There is much
debate over the location of the mills, with the
1520 mill often seen as being located on what is
now Ordnance Wharf. An evaluation carried out
in 2005 at Ordnance Wharf, however, did seem to
show that this inter-stream tongue of land is an
improbable location, and prior to the 19th
century was probably just a mud bank.35
Wilkinson interprets the palisade shown behind
the mill in the 1520 map as being possibly
related to early gunpowder works. The date for
the beginnings of the gunpowder industry, as
already stated, is uncertain but could be as
early as this time and it has been suggested
that there could be some link with Faversham
Abbey though, as Arthur Percival points out,
documentary evidence is not available.
Certainly by the
17th century the gunpowder industry
was well established in the Westbrook valley36
and the Jacob map of 175037 shows
clearly the modification to the drainage to
produce Stonebridge Ponds and the location of
two gunpowder water mills just behind Ordnance
Wharf. Either of these two mill sites is a more
probable location for the 1520 mill, in my view,
given the continuity that often exists for this
kind of establishment. In 1750, however, the
rest of the study zone for this paper is empty
of development except for the line of properties
along West St itself. No wharves are shown at
this end of the creek, although a Wardmote book
of 1555 refers to ‘Lady Amcotts Wharf’ upstream
from Town Quay.38
By 1840, as shown
on the tithe map,39 considerable
change has taken place. The zone has begun to
fill up with a scatter of cottages, particularly
along Flood Lane, and a number of industrial
buildings. This includes a Malt House owned by
Samuel Shepherd at the Creek end of Flood Lane
and next to this is the infant Faversham
Gas-Light and Coke Company (founded in 1830)
with one tiny gasholder. Other shed-like
buildings lie to the east. What we now call
Ordnance Wharf is labelled here as Island Wharf.
To the west of the Flood Lane/ West St
junction, on the Westbrook by Stonebridge (built
1776) a 4 storey warehouse has been built, and
functions as a wool storehouse and fellmongers.40
By 1865, the zone
was packed with development. The Malt House had
gone and the Gas Works had expanded and now had
two gasholders. Most of the new development,
however, was housing. Flood Lane was lined with
properties and the lower gardens of the West
Street houses had been exploited to create new
housing areas, notably Ordnance Place (for
gunpowder workers) just south of the Gas Works,
and Well Lane running down from West Street to
the Creek in the eastern part of the zone. The
long trench used in the GWE ran across this area
of 19th century housing.
By 1907, the Gas
Works had expanded even more, to the east and
the south. There were now three gasholders and
Ordnance Place and most of Well Lane had
disappeared under them. A new block of offices
had been built on West St itself. By this time,
the Gas Company had taken over Ordnance Wharf
and built the Purifier building, using the Wharf
itself for the Guiseley Purifiers.41 Large
amounts of coal were being brought in by sea at
this stage, so considerable wharfage was needed
and dredging carried out to enable ships of up
to 200 tons to
berth. (See section 2) The Flood Lane houses
have, however, survived the ravages of the Gas
Works, and an abattoir has been established
behind number 70 West St. The Gas Works reached
its spatial apogee in 1916, with a last great
expansion, this time southwards to West St
itself.42 This meant the demolition
of numbers 79 to 88 in West St. although not, of
course, the Gas Works West St Office. A giant
new gasholder now loomed over West St, and was
not demolished until 1991.
Post war maps show
an overwhelming dominance of this zone by the
Gas Works. At this stage coal was being brought
in by rail,43 the beginning of the
decline in creek usage. A large warehouse and
depot occupies the space to the east and apart
from West St itself, only Flood Lane retained
its housing. Nearly all of this was, however,
demolished during the late fifties and early
sixties, including the pair of cottages shown on
the 1840 map next to the Malt House. The
gunpowder industry had migrated to Scotland in
the 1930s, and the Stonebridge Pond area was
being used for allotments (as it still is).
Since the 1990s,
the entire Gas Works site has been occupied by a
stylish Coop superstore and carefully landscaped
car park. At the time of writing (2008) the
Purifier building still stands, but is boarded
up with no plans for usage at the moment. The
office building on West St, empty for years,
became the Gasworks Gallery but is now disused
again. Flood Lane is now a charming
recreational open space and the West St
properties are once more well-cared for and
sought after.
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Fig 5:
Flood Lane (east side) houses on the
verge of demolition in the 1960s and the
same view in 2007. Early photograph by
courtesy of Arthur Percival
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Fig 6:
Flood Lane houses (west side) in around
1895 and the same view in 2007. The
stream has disappeared. The early
picture is taken from the Croseur slide
collection at the Fleur de Lis Heritage
Centre, Faversham
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Fig
7: Lower West Street in 1968 and in
2007, showing the re-gentrification of
the area. Early photograph from Swaine
1969
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5)
Changing lifestyles
Insufficient
evidence exists to make judgments about the
prosperity of this area during the medieval
period, but the surviving substantial 15th
century properties do imply a degree of
comfort at least by the later medieval
period. At this time, Faversham’s Guildhall
and market are thought to have been in this
corner of town, only moving up to the
present location in 1547 ( see Hunting
the Saxons, in prep) . It is clear,
though, that this part of town did well in
the 17th-18th century.
The pottery assemblages of this period from
TPs 22 and 23A show a variety of quality and
imported types, such as early English Delft,
Raeren, Rhenish Stoneware, Bellarmine ware
and some small sherds of early 19th
century porcelain. (Fig 6) Fifteen of the
larger brick-built properties in the area
were built at this time, probably replacing
earlier timber framed properties, and some
timber framed properties were fronted with
brick and generally modernised in
fashionable ways.
The infilling
properties built from the mid 19th
century onwards were, however, a very
different type of housing. They were small
cheaply built properties, sometimes brick
but often weather boarded. Fig 5 shows
Flood Lane cottages on the brink of
demolition in the early 1960s. Phyllis, a
local who has lived in the area for 80
years, tells us that the other Flood Lane
cottages shown in Fig 6 had no proper
sanitation but used the stream at the back,
and that most of the houses were not really
fit for human habitation. The stream visible
in the 1895 slide has since been filled in,
using rubble from the demolished houses.
No known pictures exist for
the short-lived mid-19th century
Ordnance Place and Well St cottages, but it
can be assumed from the layout that these
were housing for the workers, probably
weatherboard. At this time, the West St
houses have for the most part lost their
extensive gardens and are increasingly
hemmed in by low cost housing and smelly,
fast-growing industries. By the mid 20th
century, these have mostly gone, or are
about to go but lower West St is in a dismal
state, as is shown by a 1969 photograph of
neglected houses damaged by lorries and the
gasholder filling the skyline.44 (Fig
7) It is only in the last 15 or so years
that this corner of town has recovered some
of its former grace.
Conclusions: Things
to come
At the
time of the building of the new Coop
superstore in the mid-90s, Faversham
Creek was seen by many local people as a
bit of an embarrassment, little more
than an open sewer and bordered mainly
by industries, some of which were active
but others declining or dead. Only the
sailing barge enthusiasts downstream at
Standard Quay and Iron Wharf kept the
sea links going. Over the last ten
years, however, the nationwide fashion
for waterside residential developments
has lead to the Creekside becoming a
desirable location (much to the
astonishment of locals). Four
developments have already taken place
along the banks below the sluice gates,
and over the last three years at least
five more proposals have been put
forward. If all had been agreed,
Faversham Creek would by now be lined
with private residential development.
Most relevant to the Upper Basin were
proposals for Ordnance Wharf which
included a maritime museum as well as
fashionable flats and for Weston’s car
park area for residential development.
All this
interest has lead to much discussion
about the future of the neglected and
rapidly silting Creek. In 2005, a
multi-representational group was formed
to review the situation.45
The HR Wallingford report was
commissioned to examine the situation
more closely, and has been invaluable.
A fundamental agreed priority for the
Creek has been the retention of its
identity as a navigable waterway (as it
has been for 2000 years) and to retain
traditional Creekside activities. At
the time of writing, the immediate needs
of restoration to action of sluice and
swing bridge and major dredging of the
creek have been agreed. The Coop site,
including the empty Purifier building
takes on a new light with all this
interest, and rumours abound. What ten
years ago was seen as a welcome use for
a toxic and unpleasant site seems far
less obvious now. Even the future of
the charming allotment site at
Stonebridge Ponds cannot be taken for
granted, although it is owned by Swale
Council.
This paper
has tried to show that this is an
important archaeological area which has
only recently been looked at in a
serious way. Although the broad
outlines have emerged, many questions
are outstanding. The early stages of
the gunpowder industry (16th
century?) are shrouded in mystery46,
as indeed are the medieval and Roman
waterfronts. Prehistory has scarcely
been considered.
Development is hard to resist (although
Faversham people have a pretty good try)
but the work currently being done by the
Creek Consortium means that it should at
least be controlled in a way that does
not damage the town. What is essential
is that all changes are accompanied by
thoughtful and thorough archaeology,
paying as much attention to the
industrial as to the early history.
Possible priorities could be:
-
Auguring & environmental
investigations in the Stonebridge
Pond basin
-
Excavation of early mill sites
-
Investigation of the west (north)
bank of the Creek
-
Investigation of early sluice sites
-
Watching brief on dredging if levels
at 0 OD or below are reached.
Any
development of a creek museum/ heritage
centre would be able to make good use of
such investigations of a much-neglected
historic asset.
P M
Reid
November 2008
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