Area 13 Paulton and Peasedown St.John Ridge
Summary of Landscape Character
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A fairly flat limestone plateau / ridge
with gentle undulations
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Shallow well-drained clay soils on higher
ground
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Most farmland is arable with more
grassland in the western part
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Open landscape with wide views to
surrounding areas
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Fields usually enclosed by low clipped
hedges
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Unclipped hedges though less common are
found more towards the west of the area
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Large fields that are regular in
shape
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Infrequent small woodlands that are often
regularlyshaped
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Woodland on batches often containing a
proportion of coniferous trees
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Small roads that run along the ridge or
straight across it
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Fosse Way runs diagonally across the
ridge
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Large prominent villages of Peasedown St.
John and Paulton with coal mining history
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20th century expansion of
Peasedown St. John and Paulton widely visible
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19th century farms often with
prominent modern buildings
Context
Location of Area
7.13.1 The Paulton and Peasedown St John Ridge
character area is nearly 17 sq km in area. It includes Paulton at
the western end, Peasedown St John near the middle and Upper and
Middle Twinhoe at the eastern end. It is about 2 km across at its
widest point near Peasedown St John. It is a limestone ridge that
separates the Cam and Wellow Brook Valleys character area and also
abuts the Farrington Gurney Farmlands character area at the western
end. The boundary is typically defined as the top of the adjoining
valley sides.
Geology, Soils and Drainage
7.13.2 Geologically the area can be divided
into two. To the east of Peasedown St John greater Oolitic
Limestone forms the capping layer giving way to bands of limestone
and Fuller’s Earth on the lower slopes. Below the Fuller’s Earth
there is a band of inferior Oolitic Limestone which comes to the
surface on the edge of the ridge. To the west of Peasedown St John
the capping geology consists of inferior Oolitic Limestone which is
above upper Lias Clay followed by Lias Limestones and clays and
shales of the Penarth Group.
7.13.3 The soils are generally shallow,
well-drained, calcareous brashy clays. Where the Fuller’s Earth and
Lias Clays are found they are more slowly draining and thicker
though still calcareous in nature with patches of brashy material.
On both soil types cereal crops and permanent or short-term pasture
is common.
Principal Planning Designations
7.13.4 The extreme eastern section is
within the Cotswold AONB eastwards from Bath Hill between Wellow
and Combe Hay. The Bristol/Bath Green Belt includes the eastern
part of the area eastwards from Peasedown St John.
Description
Landform and Drainage Pattern
7.13.5 This is a simple landscape that
consists of a relatively flat plateau with shallow undulations. It
ranges in height from about 100 m to high points of 164 m at
Camerton Farm and 168 m at White Ox Mead Knoll. The area is above
the spring line of the ridge and so open water is absent. However
there are springs along the edges of the area and most farms have a
well.
Land-uses
7.13.6 The land is mainly used for arable
crops but in the western part up to half the area is grassland.
Fields, Boundaries and Trees
7.13.7 Hedges are the most common boundary
though in places fences have replaced them. The hedges are usually
low and well clipped. In the western half there are also
characteristically unclipped and taller hedges. Where stock is
farmed the hedges are generally supplemented with post and wire
fences. Trees in the hedgerows are common but not abundant and are
mostly oak or ash. The fields are medium to large and regular in
shape reflecting the field pattern of late medieval times. There
are infrequent woodlands that are usually less than one hectare in
size. These are also regular in shape and fit easily with the grain
and texture of this landscape. The woodlands are mostly broadleaf
consisting of mainly oak and ash, with a proportion of sycamore.
Many woods have a small conifer element but this is not universal.
The batches at Camerton, Braysdown and Tyning have a higher
proportion of conifers in common with many of the other batches in
the area.
Settlement and Communications
7.13.8 Peasedown St John, the largest
settlement, is located in a prominent position near the centre of
the area. It is quite visible from much of the surrounding areas.
Likewise Paulton occupies a prominent location at the western end.
Clandown at the edge of Radstock adjoining the area is sited at the
head of a small valley. All three are former mining settlements
established in the 19th century. The expansion of these settlements
in the 20th century has made them stand out prominently in the
landscape. The regular size, form, ‘newness’ in colour and the lack
of mature tree cover mean that the housing development on the south
side of Peasedown St John stands out from the rest of the village
and its surrounding countryside. Although Paulton has a mining
history, printing has been the predominant industry since the
beginning of the 20th century. The works are on the north side of
the village and the large buildings dominate the surrounding urban
and rural areas.
7.13.9 There are scattered individual
farmsteads located across the area. These tend to be of typical
19th century design using mostly local materials and so harmonise
well with the landscape. However many of them have large modern out
buildings and barns that have a high impact due to their size,
material and functional design.
7.13.10 The roads are few and narrow. They
generally run either along the line of the ridge or straight across
it. In either case they are often sunken into the ground or
enclosed by hedges on either side giving a ‘closed in’ feeling to
them. The exception to this is the A367 Radstock to Bath road,
which cuts diagonally across the plateau. Part follows the Roman
Fosse Way which has been a major route way leading south from Bath
for hundreds of years.
Landscape Characteristics
7.13.11 This is an open landscape often with a
windswept character. Long views over the valleys on either side to
the surrounding hills are typical. There is rarely a sense of
enclosure as woodlands are not common and the hedges are mostly low
and well clipped. The sky is an important feature of the views and
the few tall elements such as pylons, telecommunication towers and
floodlights are consequently highly visible.
7.13.12 The A367 is a major feature adding
movement and noise to this landscape. Away from this busy road it
is tranquil, typified by the spring and summer sounds of skylarks.
Other detractors include a covered reservoir north of Clandown, a
landfill site beside Bath Old Road north of Tyning and large modern
barns and associated unnatural earthworks. There are dark night
skies in those areas away from the larger settlements.
7.13.13 There is considerable archaeological
evidence to show that this plateau has been settled for thousands
of years. There are Neolithic flint finds that date from the 5th
century BC. There are Bronze-age burial mounds near Camerton, the
site of a Roman settlement near Clandown and the site of a Roman
villa near White Ox Mead Knoll.
Landscape Change and Condition
7.13.14 Agriculturally there have been
significant postwar changes resulting in the amalgamation of fields
particularly within the areas favourable to arable use. There has
also been a reduction in the number of trees within hedgerows with
a resultant opening up of the character of the higher areas.
Historically the blight and hectic activity associated with coal
mining in this area in the 19th and early 20th centuries has now
largely been greened over. In the latter half of the 20th century
the most evident changes to this landscape have increasingly come
from development pressure. Development is evident by the
encroachment into the landscape of features such as pylons and
other overhead wires as well as telecommunication towers. In
addition flood lighting is seen around Clandown. In this flat
landscape where tall vertical objects are proportionately more
noticeable this has had a significant effect upon the character of
the area. The recent by-pass and housing at Peasedown St John have
significantly affected the landscape around the village by
extending the built-up area and changing the character of the
interface between the built-up area and the countryside. The
realigned A367 road and the associated noise attenuation bund has
resulted in a strong barrier between the settlement and the
surrounding landscape. Land to the south-east is designated as
employment land. This will result in significant changes along the
southern boundary of the village.