Area 15 Norton Radstock Southern Farmlands
Summary of Landscape Character
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Limestone plateau surrounded on three
sides by river valleys
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Relatively steep river valleys
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Small irregular shaped fields in valley
and rectilinear shaped fields on the plateau
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Fields enclosed by clipped hedges on
plateau with unclipped hedges in the valleys
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Industrial past evident from remains of
railway and colliery spoil heaps
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Core of coal mining village of Haydon
built in Lias Limestone with small scale modern in-fill
development,
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Some individual farmsteads
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Prominent 20th century
industrial and residential development
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Few individual hedgerow trees but large
areas of hawthorn scrub, scrub woodland and new plantation
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Open landscape on higher plateau with wide
views
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Older buildings built from Lias Limestones
with slate roofs. New buildings are brick and concrete
tile.
Context
Introduction
7.15.1 This small character area of just over
3sq km lies between the southern boundary of the area and the
built-up areas of Midsomer Norton and Radstock. The character of
this area results from its relationship to the built-up area and
the associated coal mining heritage. It is divided into three
separate areas and includes several tributary valleys of the Wellow
Brook including the River Somer, Snail’s Bottom and Kilmersdon
Brook. The position of the boundaries is mainly dictated by the
urban edge and the administrative boundary of the area.
Geology, Soils and Drainage
7.15.2 The floors of Somer Valley and Snail’s
Bottom are Mercia Mudstones. The base of the Kilmersdon Valley,
however, is of alluvium deposits. Above this on both sides of all
of the valleys is a band of shales and clays from the Penarth
Group. These rocks are from the Triassic period. The majority of
the remaining upland is Lias Limestone (white and blue) while the
very highest part above 130m, south of Haydon, is a small outcrop
of Inferior Oolitic Limestone. This part of the plateau is
virtually a small western outlier of the Cotswolds that has been
separated by erosion of the intervening area. All these limestones
are from the Jurassic period. The steepest slopes of both the
Kilmersdon and Snail’s Bottom Valleys have frequently slipped.
Below all of the area is the coal bearing Carboniferous strata.
7.15.3 The soils of the valleys and valley
slopes are generally derived from the Mercia Mudstones and are
slowly permeable, reddish and clayey. The remaining higher land has
shallow, well-drained calcareous soil derived from the
limestones.
Principal Planning Designations
7.15.4 The area is outside any Green Belt or
AONB designation.
Description
Landform and Drainage Pattern
7.15.5 The two smallest parts of the character
area lie to the west of the A367 and comprise principally the upper
steep slopes of the River Somer Valley. The lower slopes and part
of the valley floor are developed mainly for housing. The largest
part of the character area lies to the east of the A367. The
dominating landform characteristic here derives from the high
Oolitic Limestone central plateau area around Haydon which is
bounded by two steep-sided tributaries of the Wellow Brook; Snail’s
Bottom to the west and Kilmersdon Brook to the east. The
tributaries curve around the plateau to the north and merge at the
Radstock Railway Lands. To the south west of Snail’s Bottom is a
small part of a lower, more undulating Lias Limestone plateau and
in this area the Snail’s Bottom Valley is more asymmetrical. The
western valley side is very shallow and the eastern valley side is
steep where it abuts the Oolitic Limestone plateau. The lowest
point of the area at the Radstock railway lands is about 75m. The
highest point is 136m above Haydon.
7.15.6 T he tributaries of the Wellow Brook
through the area have several minor tributaries such as those
flowing from Redhouse Farm to the stream along Snail’s Bottom and
from Foxhills to the stream from Kilmersdon. They are fed from
numerous springs that issue from the point where the Lias
Limestones meet the Penarth Group shales and clays. The frequency
of springs particularly east of Haydon gives a marshy character to
this part of the valley.
Land-uses
7.15.7 The land on the plateau is mainly used
for arable with some short-term pasture. In the valleys by contrast
the land is mainly used for permanent and short term pasture with
some scrub and woodland on the steeper slopes.
Fields, Boundaries and Trees
7.15.8 The field pattern is angular but
irregular and the fields are medium and small in size. The steeper
slopes tend to have the smaller more irregular fields. The hedges
of both the higher and the lower plateau areas tend to be low and
well clipped but with very few trees within, giving a very open
character. In the valleys the hedges are commonly unclipped but are
also sometimes clipped and they tend to be quite ‘gappy’. In places
scrub merges with the hedges and as a result the boundaries of
fields are often quite indistinct.
7.15.9 Grove Wood to the west of Haydon is one
of the most distinct areas of woodland in the area and is
registered as ancient semi-natural woodland. There is considerable
scrub along the stream sides and upper slopes of the valleys and
some scrubby woodland on the spoil heap by the colliery tramway at
Haydon. Newly planted areas are found adjacent to Grove Wood and
along the upper slopes of the Kilmersdon Valley. The scrub consists
mainly of hawthorn and bramble with course grasses. A more open
scrub is found on the disused workings west of Haydon where the
spoil cannot support larger species.
Settlement and Communications
7.15.10 Haydon is the main settlement in the
area. It is a compact village of mining terraces in Lias Limestone
with concrete and slate roofs. There is also some more modern
in-fill development. Other buildings are stone farmhouses with a
mixture of outbuildings and barns in both traditional and modern
materials. The former colliery site is now an industrial estate to
the east of Haydon.
7.15.11 The principal roads through the area
are aligned north to south connecting settlements to the south with
Midsomer Norton and Radstock. The most important is the A367, which
is the Roman road the Fosse Way. A smaller road connects Haydon to
Kilmersdon across the high point of the area. The line of the
disused railway follows the floor of the valley north of
Kilmersdon.
Landscape Characteristics
7.15.12 The valleys give an enclosed feel to
the landscape in contrast to the plateaux with their open views.
The tower of Downside Abbey is visible across the plateau to the
south. The strongest elements of this landscape are the remains of
the coal mining industry and the close proximity of the built-up
area both residential and industrial which influence almost all
views and brings with it pressures for recreational use. The large
new warehouses at the Westfield Industrial Estate are an unsightly
and dominating influence in the Snail’s Bottom area. Snail’s
Bottom, the old Haydon tip and Kilmersdon Valleys are particularly
well used for casual recreation.
7.15.13 Haydon itself is an outlier of
Radstock and was built to house the miners for the local pit. The
disused railway line and inclined railway at Haydon form important
elements within the Kilmersdon valley east of Haydon.
7.15.14 There is a tumulus to the north of
Haydon and the land around it is of archaeological significance.
There is a quarry nearby which would have provided Lias Limestone
for local buildings and is now designated a SSSI.
Landscape Change and Condition
7.15.17 The landscape has changed in the last
150 years from a rural scene to an industrial one dominated by the
coal industry and back to a rural scene. The modern landscape has a
less maintained and ‘rougher’ character and texture than
neighbouring agricultural areas. This is caused in the main by the
remnants of the coal industry and its infrastructure and changes in
agricultural management. The disturbance caused by coal mining and
the railways and the subsequent ending of mining and disuse of the
railways has created valuable habitats of nature conservation
interest. The plateau is well maintained as a traditional rural
landscape. As such it has changed relatively little compared to the
Haydon Valleys.
7.15.18 Since the 1st edition OS map
considerably more woodland and scrub has been allowed to develop
along the valley sides and by the streams. Further planting has
increased the rate of this change. However hedgerow trees are fewer
in number as indeed are the hedgerows themselves. This is
consistent throughout the area but most noticeable on the plateau
areas. There used to be a few scattered small orchards across the
plateau and its slopes, few of these exist today.