Area 18 Bathford and Limpley Stoke Valley
Summary of Landscape Character
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Broad open valley of the River Avon in
places dramatic and gorge-like
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Narrower Frome River and Midford and By
Brooks valleys
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Steep generally wooded valley
sides
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Meandering course of Rivers Avon, Frome
and the Midford and By Brooks edged with groups of alder and
willow
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Important transport corridors
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Settlements on valley sides
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Extensive views across and along the
valleys
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Views contained by ridges and woodland
each side of the valleys
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Generally hedged field boundaries, some
clipped and some unclipped
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Several fields enclosed by walls
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Impressive houses and attractive
farmhouses usually of characteristic golden Oolitic Limestone on
valley sides in wooded or parkland setting
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Distinctive canal architecture including
Dundas Aqueduct and bridges
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Mill buildings and associated features
such as mill races
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Second World War pill boxes
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Brown’s Folly
Context
Location of Area
7.18.1 The character area covers nearly 15sq
km. It consists of the valley floor and the steep and often
wellwooded slopes of the Rivers Frome and Avon and the Midford and
By Brooks. It is generally bounded by hills and plateaux and, in
the context of this assessment, also by development and the area
boundary. It follows the Avon Valley east of Bath from the edge of
Batheaston to the north around to the Midford Brook Valley near
Monkton Combe to the south. It includes a branch westwards along
the Midford Brook and Horsecombe Brook Valleys and eastwards along
the By Brook Valley at Bathford. The River Avon continues
southwards beyond the area boundary into West Wiltshire. The
character area also has an isolated section to the south
incorporating part of the River Frome Valley.
Geology, Soils and Drainage
7.18.2 The sides of the rivers and brooks
contain drift geology of alluvium, gravel and occasionally head
such as below Warleigh Lodge Farm. Typically the valley sides
consist of Fuller’s Earth and Lias Clays which are overlain with
Oolitic Limestone on the high ground. Landslips are a feature
throughout the valleys resulting from limestone above unstable
clays.
7.18.3 The main soils are calcareous clayey
soils typically used for grazing and occasionally for arable use.
Fine well-drained calcareous loamy soils occur over the limestone
towards the boundaries of the area and typically support a more
diverse range of agricultural uses. Welldrained soils are also
found towards the north of the area in the vicinity of the
Bathampton Meadows.
Principal Planning Designations
7.18.4 All the area falls within the Cotswold
AONB except at the two extremes; the Bathampton meadows at the
northern end and the Farleigh Plain and Iford plantation at the
southern end are outside the AONB. All the undeveloped part also
falls within the Bristol/Bath Green Belt.
Description
Landform and Drainage Pattern
7.18.5 The River Avon occupies a comparatively
broad but steep sided valley. The steepness of the valley sides in
relation to the breadth of the valley gives a dramatic almost
gorge-like feel to the landform in places. The River Frome and
Midford and By Brooks by contrast occupy narrow valleys also with
steep sides. The floor of each valley is generally flat or gently
sloping, gradually increasing in steepness higher up the valley
sides. The present form of the Avon Valley with its markedly
undulating side slopes has to a large extent resulted from the
instability of the Oolitic Limestone over clay leading to landslips
along the section east of Bath.
Land-uses
7.18.6 The land is principally used for
grazing. Only part is in arable use such as to the south of
Bathford. There are sports pitches north of Bathampton and along
the By Brook and Midford Brook Valleys. There are also areas of
parkland with mature specimen trees at Claverton Manor, now the
American Museum, and at Warleigh Manor, now converted to smaller
housing units.
Fields, Boundaries and Trees
7.18.7 Much of the field pattern throughout
the valleys reflect relatively modern adjustment of earlier
enclosures. There are however areas of medieval enclosure of rich
wet grassland such as alongside the River Frome and By Brook and
alongside the River Avon between Claverton and Bathford. There is
evidence of late medieval enclosure of steep sided cultivation in
some areas such as below Warleigh Wood. The medium sized fields are
generally enclosed by hedgerows; some are well trimmed and others
are tall and unclipped. The hedges often contain mature oaks and
other trees. Walls are also present but are less common.
7.18.8 The valley sides are typically
well-wooded. Most of the larger areas of woodland are registered as
ancient semi-natural woodland. As well as native woodland there are
also characteristic parkland trees including copper beech and
redwood trees as for example at Claverton Manor and Warleigh Manor.
There is often also a transition to patchy scrub on the more gentle
lower slopes.
Settlement and Communications
7.18.9 Throughout history the area has been
important as a communication corridor. The Avon Valley contains not
only the river, but also the Kennet and Avon Canal, the railway,
the A4 Batheaston Bypass and the A36 Warminster Road, and a number
of public footpaths all of which make use of the comparative
convenience of the valley floor. The Kennet and Avon Canal was
important for moving stone but is now important for recreation. The
Somersetshire Coal Canal joined it at Dundas and a short remaining
section can still be seen near the aqueduct. The Camerton branch of
the railway once followed the Midford Brook Valley. This was made
famous in the film ‘The Titfield Thunderbolt’. The A36 was
originally built in 1830 as a turnpike road by Macadam. The A363
Bradford Road climbs the eastern valley side. The Rivers Frome and
Avon and the Midford and By Brooks were commercially important
giving rise to a number of mills which constitute important
features in the landscape. The area also contains a network of
minor routes following the valley and rising up the valley sides.
These are often narrow and enclosed by hedges.
7.18.10 The main settlements include Bathford,
Claverton, Monkton Combe, Limpley Stoke and Freshford. They each
occupy sloping ground on the sides of the valleys. There are also
several farms and large properties, many of Georgian origin, which
characteristically occupy strategic positions on the upper slopes
overlooking the valleys. Examples include Warleigh and Claverton
Manors.
Landscape Characteristics
7.18.11 The landscape is open providing
extensive views both along and across the valley. Views are
contained or framed by the ridges and dense woodland on each side
and wider views beyond the valley are rare. In places the valley
sides are so steep and well-wooded that they give a dramatic and
gorge-like feeling to the valley whilst the overall scale of the
landscape maintains a sense of openness. The course of the rivers
and brooks is marked by groups of willow and alder trees. Although
the lower slopes and valley floor of the River Avon are occupied by
busy main roads and the railway, much of the area has a remarkably
tranquil quality. Similarly the River Frome and Midford and By
Brook Valleys are all to a greater or lesser extent transport
corridors, but taking less traffic they have a more tranquil
character similar to the quieter parts of the Avon Valley.
7.18.12 Impressive houses and smaller farm
houses located on the valley sides, often nestled into woodland or
within parkland on the upper slopes, are distinctive features
within the landscape. The traditional building material is Oolitic
Limestone with clay tile and sometimes slate roofs. Reconstituted
stone is now widely used often with dark coloured concrete tile
roofs.
7.18.13 There are distinctive structures
associated with the canal, river and railway. The A36 viaduct and
Dundas Aqueduct near Monkton Combe are particularly distinctive, as
are the smaller bridge structures such as the one over the canal
near Claverton. There are numerous other features such as Claverton
Pumping Station built in 1813 to pump water from the river to the
canal; mills or evidence of mills at Freshford, Bathford and
Tucking Mill; Brown’s Folly above Bathford and remnants of the
Second World War defences known as the Outer Bristol Defences which
pass through the area in the vicinity of Freshford Mill. The most
evident features of these defences are a series of pill boxes such
as the one at Woodside near Freshford.
7.18.14 Significant detractors within the
landscape include traffic on the A4 and A36, pylons, communication
masts and some new development by virtue of its scale, location
and/or design.
Landscape Change and Condition
7.18.15 The area is generally in good
condition and maintains its distinct harmonious character. There
are however signs of creeping changes which could have implications
on the long term cohesiveness and health of the landscape. Since
the 1st Edition OS map was surveyed hedges have often been taken
out to enlarge fields as for example to the west of Bathford Hill.
Remaining hedges have often become ‘gappy’ and there has been a
reduction in the number of trees in the hedges and within the
fields. The extent of woodland appears to be relatively constant
though factors such as clear-felling and replanting and storm
damage have influenced its appearance. Reduction in the areas that
are grazed has resulted in some newer areas of woodland. More
recently Phytophthora disease has resulted in dead and dying alders
beside the river affecting many views.
7.18.16 Development in the form of new housing
for example at Bathford and to a lesser extent at Monkton Combe;
larger shed type buildings and associated car parking and lighting
located on the valley floor such as at Manor Farm, Bathampton and
Freshford Mill; and development on or close to the skyline, for
example at the University of Bath have all had varying degrees of
impact on the character and cohesion of the landscape.
7.18.17 In general the landscape appears to be in good health
and relatively robust in maintaining its distinct character. The
effect of a combination of the above changes has however resulted
in degrading the character and cohesion of the landscape in places.
The valley with its river, canal and public rights of way network
is an important area for recreation. This can influence landscape
character through for example the demand for playing fields. Other
pressures on the landscape include demands for utility structures
such as masts and pylons.