Prefatory notes and maps showing the situation of Romney Marsh in Kent (within which is incorporated Walland and Denge Marshes)
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Romney Marsh: southernmost part of Kent |
Romney Marsh is the
generic name for the unique, and geologically very recent, levels which form
the southernmost corner of Kent. It comprises: to the north east, Romney Marsh proper; to the south west,
Walland Marsh; to the south east, Denge Marsh and the shingle promontory of
Dungeness; and, to the west of Rye
and the river Rother, Pett Level, which
lies in the county of Sussex. Guldeford
Level is incorporated into Walland marsh, and lies on its south western
edge, east of Rye and north of Camber.
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Click on map to see the three divisions of the Marsh clearly This is a land drainage map of 1984 |
Romney Marsh was once a salt marsh, but has been reclaimed
from the sea by gradual degrees over the centuries. Exactly who reclaimed, or
‘inned’ which sections and when is not entirely clear, but it is certain that
Dutch expertise played a very significant part. The word ‘marsh’ is misleading: see term below
Inning is a term which may be taken quite literally to refer to the
infill of an area which has been banked or shored against the influx of the
sea.
Guldeford is pronounced as Guildford
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Guldeford Marsh C 1752. The Rother as estuary |
Guldeford
Level. Ordnance Survey 1813–1819. Cassini reprint. The river Tillingham, seen
on the far left no longer reaches the sea at Pier Head (which no longer
exists as a place name), but has controlled outlet through the Rother, centre.
From Rye harbour to the sea, the Rother flows through an artificial and
comparatively narrow channel, which is ‘vertically walled’. Sea water is
prevented from contaminating the marsh by a sluice at Scots Float approximately
2 miles inland. Consequently, as the tide turns, the Rother flows out
with such swiftness that its bed is scoured, and the build up of silt
prevented. This had been a major problem over the centuries. The Rother, historically sluggish, has meandered at different times in history eastward across Romney Marsh and exited to the sea – as far as can be ascertained from geological evidence – both at New Romney and at Hythe.
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St Mary, East Guldeford,
cannot be classed as a work of notable architectural beauty – as we normally
understand that description – yet it is a uniquely charming church, and one
that is strikingly situated. It is probably one of the least adorned churches
in the British Isles: it stands ‘four square’ and isolated (even from its
eponymous and tiny hamlet) on the western side of the marsh levels, some fifteen miles from the definitive, cliff–boundary of Hythe at
the easternmost edge of the levels. (Pett Levels, to the east of Rye, constitute the westernmost ‘section’ of Romney Marsh, even though the river Rother forms a definitive divide in the Marsh, with the first bridging point at Rye.)
It has stood here since
its consecration in 1505 by Richard Fitzjames, bishop of Chichester, in whose
diocese the church stood (in which diocese it still stands: there being no cathedral city in
East Sussex). And if it further seems strange that East Guldeford is in Sussex,
given that Romney Marsh is situated almost entirely in Kent, then that is
because the easternmost county boundary of East Sussex has thrown a little hook
into Romney Marsh and netted East Guldeford and Camber; and the apparent
inconsequentiality of this boundary – on an area that was beneath the sea at
time of the Book of Doomsday, 1086 – may well prove beyond explanation.
The building of a church
in this seemingly most unlikely of places would not have been possible (or
occurred) had not “the abbot of Robertsbridge granted Sir Richard Guldeford, by
royal licence, 1,500 acres of salt marsh to hold of the king [Henry VII] by
fealty at a rent of 12d [twelve pence] a year.” [ 1 Lutton]
The salt marsh was to the east of Rye and the river Rother; and during the
1490s was reclaimed, to form the Guldeford Inning. Once freed of salinity, the
rich alluvial soil produced fine quality grazing for the famous Romney or Kent sheep. On this reclaimed land, Sir Richard Guldeford was
granted faculty to build a church, which he carried out at his own expense. The
Guldeford family were pious: in particular, Richard’s father, Sir John, who
“expressed a strong interest in those Wealden parishes where he had greatest
interest. He stipulated that his ‘out berying to be made not pomposely’ and
bequeathed 4d to every poor household in Tenterden to pray for his soul. This
he extended to four neighbouring parishes . . .” [Lutton]
So it is that of the
fourteen surviving churches on Romney marsh, East Guldeford is the only one in
Sussex, and the only one to be built entirely of brick. This latter fact caused
me considerable confusion when I first visited the church in the 1980s. I of
course noticed the brick buttresses (as well as an unsightly patchwork of
rendering elsewhere) and assumed these to
be late nineteenth or early twentieth century attempts to shore and patch up
the church. Further the brickwork was so badly eroded by the prevailing
south–easterly gales from the English Channel – which meet with no resistance
from the westerly Pett Levels – that I feared for the entire structure. How, I
wondered, could or would funds be found to prevent it from becoming a ruin?
How, in the future could we evoke its memory but through such fine graphic
renderings as those of John Piper? Romney
Marsh, King Penguin, 1950.
Imagine my delight then,
on finding (this November, 2014) that St Mary had been thoroughly repaired and
renovated (principally by Carden and Godfrey in 2009). It now looks splendid,
and would seem to have an assured future (with financial assistance from The Romney Marsh Historic Churches Trust).
The Exterior
Prefatory
note
After first
posting this blog, I contacted Carden and Godfrey, asking if they could kindly give me some information about their
restoration of East Guldeford, and was sent a very full account by Richard
Andrews (the architect primarily responsible for this work). I am very grateful
for to Mr Andrews for his response – which gave me more details than I could
possibly have wished for – and which I thought at first of appending to my blog
(in abbreviated form). However, for the sake of continuity, I’ve decided to
include a short paraphrased introduction, followed by direct quotation of
Richard’s communication.
I think it fair to say that, before the involvement of Carden and Godfrey, the badly eroded fabric of East
Guldeford had received what might best be described as piecemeal repair,
resulting in a hotchpotch scarcely deserving the name of restoration. When
Carden and Godfrey became involved (in 2012), “the north
side was crumbling brickwork, the east wall was a mixture of render and
brickwork, and the west wall was similar but with less render While there was
clear evidence of render on the west and east walls, there was none on the
north wall, and as a result some internal consideration of whether it was right
to render the lot - was it always rendered? In the end pragmatism ruled, and I
decided simply to consolidate the north wall brickwork, replacing only the
worst bricks. The new bricks were made behind Hastings using local clays, and
matched the old in thinness and colour and moulding. The east wall had its
later buttresses (with bigger bricks) either side of the east
window removed in the 1970s I think, leaving patches of lined-out render
below, indicating that this wall was rendered before the buttresses were added
in the 18th C (?); that having been said the lining-out of the render is hardly
a 15thC feature, so was not considered to be original. In the end we put
stainless steel expanded metal over the lot and rendered over, keeping the side
buttresses exposed in repaired brickwork. The more protected west wall was
basically repaired as found. The south wall pebbledash started coming
off a couple of years ago so the opportunity was taken to replaster the
lot on expanded metal using the same render and the same contractor as for the
east wall -a benefit of this is that the arguably over-restored south wall
buttresses are less demanding than before.
All of this has been possible through the small band of dedicated
parishioners supported by the Romney
Marsh Historic Churches Trust – a great benefit of being among those
Kent churches!”
Note: the following was written before I had further information from Carden and Godfrey, but I do not think that it will cause any confusion if I leave the text unchanged.
The bricks are “of
varying colours and textures . . . laid in English
Bond Figure 2.3 (i.e. one course laid as ‘headers’ and the next course as ‘stretchers’
and so on alternately” to a depth of three feet.” [ 2 Steer]). The diagonal sections of brick
incorporated into the two buttresses either side of the doorway on the
windowless west wall are examples of brick tumbling [ 3 Barlow]: whether, in this instance, it also strengthens the structures I do not know. And quite what purpose is served by the (70º) diagonal
courses of buttress–brick adjacent to the south wall and aligned to the outer
buttress–edges, it is hard to say.
I quoted Steer above on
the “varying colours and textures” of the bricks. And truly those of the south
wall are a delight. The predominant colour is perhaps yellow ochre –
particularly of the bricks surrounding the doorway. Otherwise, the bricks are
red ochre, offset by whitish–grey lichen patches, the green of such plants as
have managed to gain purchase, the blackish wood of the door, and the white
space between the door and the chamfered or two–sided arch.
The outlines formed
by the hipped (four–sloped) roof, the pyramidal bellcote, and the south and
north buttresses form a very satisfying ‘origami’ pattern of brick and tile.
Almost, from this angle, the church looks like some kind of grand fortified
barn. Yet no barn ever had bellcote, as far as I am aware, and the building is unmistakably
ecclesiastical. However, Lutton writes that “it most resembles the barns that
scatter the marshland landscape and so translates local vernacular style into
self conscious pious statement.”
The number of buttresses
supporting the church has changed over the centuries. Steer writes that
“extra buttresses were added to the east and west walls in the 18th century . .
. to combat the thrust of a wide building on marshy ground.” This was probably
the only change made to the total of the buttresses since 1505. The current –
and no doubt permanent – total is four to the north and south, and two to the
east and west. The condition of the church as it was before at least 1973, and
as it is today can be clearly seen by comparing the photographs below.
Photograph from Steer (source not given). View from the south–west
The interior
As a result of one of those unaccountable oddities that occasionally assail
me, I did not try the church door to see if it was open. It just gave the look
of being firmly closed – as might appear from a glance at the photograph of the west front above. Yet
in fact it is never closed! (It contains no valuables, so why should it be?) However, photographs show the interior to be pleasingly light – the walls being painted
in pale cream. It has no structural division between the nave and the chancel.
Above and between the eastern windows is a painted frieze of angels. But these
are of inferior quality, and are thought to be late Victorian. There is no
evidence of any earlier decoration. There are box pews and a double decker
pulpit, but otherwise a gratifying absence of the dark Victorian wood which tends to cast a somewhat gloomy pall over so many church interiors. (Excessive embellishment or
ornamentation of churches – or cathedrals – although often of great beauty,
hardly reflects the teachings of Christ. Rather, they tend to be reflections of
a Christology with which Christ – as he is presented in the gospels – would
have been profoundly impatient.)
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East Guldeford from the north |
I do not know of any
other church that has such an unusual history – even though I am sure that such
abound. It can hardly be seen from the road or the Marshlink railway line. Like
some treasure in a provincial museum or art gallery you may have it all to
yourself – probably for several hours, if not an entire weekday. The Marsh
footpaths are difficult to follow, and its ravelled waterways may only too
easily block your way if you do not read your map very carefully. Further the eastward
path, towards Appledore station, looks very uninviting. So it is that few
venture that way – or across the Marsh at any point. Its atmosphere percolates
very slowly into the soul, and if there is any fauna that represent St. Mary,
East Guldeford, then it is the heron, that solitary watcher of the dykes. The only
difference being that St. Mary has stood sentinel for five hundred years.
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The (apparently) uninviting autumn path towards Appledore station |
Endnote:
There is more to say
about East Guldeford church; as indeed about Sir Richard Guldeford, who embarked
from Rye on a pilgrimage to Jerusalem in 1506. This I shall write about in my
next blog, which will probably be the first of 2015.
1 Rob Lutton (Lecturer in the Faculty
of Arts, University of Nottingham), Richard Guildford’s Pilgrimage: Piety and
Cultural Change in Late Fifteenth– and Early Sixteenth–Century England. From
The Journal of the Historical Association, Blackwell Publishing Ltd. 2013
2 Francis W. Speer, Guide to
the Church of St. Mary, East Guldeford. The East Guldeford Parochial Church Council. 1972
3 I am
grateful to my friend Adrian Barlow for
shedding light on this. In an email he makes this comment “the angled brickwork on the
buttresses is technically called 'tumbling-in work': it's more often seen on
gable ends. From your very clear photograph, this looks a particularly
interesting and complex example.” It seemed a further curiosity that
Steer gives the dimensions of the bricks as “approximately 9¼ by 2 inches.” I
found it hard to imagine that I’d ever seen a brick of so thin –
except perhaps on a Tudor building – and yet when I measured the Cambridge
Whites on our garden wall I found them to be 9 by 2¾; and those on the walls of
our 1888 terraced house 9 by 3 inches. Still, looking at the close–up
photograph of the East Guldeford buttress, the bricks do appear to be
approximately 3 inches in depth. Brick slips – used to fill
spaces where standard bricks will not fit – could be 2 inches thick, or less –
but these are not used for entire courses of brickwork. (I now understand that the west wall buttress bricks are atypical to East Guldeford, and that the bricks of the walls are indeed thinner. As referenced in the email from Richard Andrews, quoted above.)
Colour photographs copyright the author
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The Rother today as a managed river |