Area 8 Farrington Gurney Farmlands
Summary of Landscape Character
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Gently undulating landscape
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Red soils
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Numerous minor brooks and
tributaries
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Distinctive angular field pattern of late
medieval enclosure
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Historical wet meadowlands along the Cam
and Wellow Brook valleys
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Historical core to settlements of
Hallatrow and Farrington Gurney
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Distinctive ‘treed’ setting of Farrington
Gurney and Hallatrow
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Lias Limestone and Pennant Sandstone
buildings with some painted and rendered houses
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Open landscape
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Views to surrounding ridges and distant
churches
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Disused Farrington, Old Mills and
Springfield Collieries now used for a variety of uses
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Disused North Somerset Railway passes
through the area
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Distinctive local Pennant Sandstone
stiles
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Many detractors such as modern barns and
pylons and development at Old Mills
Context
Introduction
7.8.1 Farrington Gurney Farmlands character
area is a little over 5sq km located towards the centre of the
southern boundary of the area. It is a gently undulating landscape
linking the upper reaches of the Cam Brook to the north, and Wellow
Brook to the south. It is bounded by the Hollow Marsh, Hinton
Blewett and Newton St Loe Plateau Lands, the Cam and Wellow Brook
Valleys and the Paulton and Peasedown St John Ridge character
areas.
Geology, Soils and Drainage
7.8.2 Mercia Mudstones are the main geological
outcrop found throughout the area except for the north central
section south of Hallatrow. The Mercia Mudstones consist of red
siltstone and mudstone of the Triassic desert basins resulting in
the underlying characteristic of the gently rolling valley
landscape. The central northern section south of Hallatrow consists
of Supra-Pennant Measures which includes the upper coal measures
and outcrops of sandstone.
7.8.3 The soils are generally reddish and are
loamy and more rarely clayey in nature. The reddish soils are
mainly found in association with the Mercia Mudstones.
Major Planning Designations
7.8.4 It is outside any Green Belt or AONB
designation.
Description
Landform and Drainage Pattern
7.8.5 The area is crossed by tributaries of
the Cam Brook, which flows through the northern part of the site
and tributaries of the Wellow Brook towards the southern part of
the area. This drainage pattern has given rise to its distinctive
gently undulating character.
Land-uses
7.8.6 The land is used both for pasture and
arable.
Fields, Boundaries and Trees
7.8.7 There is a roughly equal mix of small
and medium sized fields, typically angular and irregular in form.
They are generally enclosed by clipped hedges generally with few
trees. There are very few trees or woods within the area. Most
trees are located along the watercourses and at the edges of the
settlements. Enclosure took place during the late medieval period
as evidenced by the remaining pattern of relatively small regular
and often rectilinear fields. The enclosed areas of rich, wet
grassland along the Cam and Wellow Brook Valleys are also of
particular note. Historically these areas of meadowland provided
early seasonal growth of grass.
Settlement and Communications
7.8.8 Farrington Gurney and Hallatrow are the
main settlements in the area. The older cores of the settlements
were linear in form but each has been extended around the edges
during the 20th century. Paulton abuts the area to the east.
Elsewhere there are occasional isolated farms. The traditional
buildings are of Lias Limestone with clay tile roofs. Cream
coloured rendering and Pennant Sandstone is also evident.
Farrington Gurney church, an important landmark, is constructed of
both Pennant Sandstone and Lias Limestone. The main settlements of
Farrington Gurney and Hallatrow are both set within a ‘well-treed’
setting.
7.8.9 Three major routes radiate from
Farrington Gurney including the A39 Glastonbury to Bath Road, the
A37 Shepton Mallet to Bristol Road and the A362 running eastwards
to Midsomer Norton and Radstock. There is also a secondary road to
Paulton.
Landscape Characteristics
7.8.10 The landscape has an open character
giving some long distance views for example to the churches at Ston
Easton and Chilcompton and Downside Abbey. Otherwise views are
typically contained by surrounding ridges that are often clothed
with hedges with occasional trees and broken lines of trees.
7.8.11 The relicts of the industrial past are
very evident within the area. Of particular note is the widely
visible and distinct conical shape of the Old Mills batch with its
generally unvegetated surface. There are at least three disused
collieries in the area, which have subsequently been developed for
light industry, a depot and a superstore. The buildings and
associated features are widely visible as a result of the scale of
the developments. The line of the North Somerset Railway that once
crossed the area is now evident from scrub along its course and its
gently curved alignment that now forms field boundaries. Pennant
Sandstone was locally available and was used to make the curved
stones of the distinctive local stiles.
7.8.12 There are several detracting elements
within the landscape such as pylons, modern barns and commercial
development at the edge of the settlements which dominate some
views into and within the area.
Landscape Change and Condition
7.8.13 In places the landscape has a distinct
and cohesive character with a wealth of features such as
characteristically curved Pennant Sandstone stiles and local
landmarks such as Farrington Gurney church. There has however been
significant loss of hedges since the 1st edition OS map through
amalgamation of smaller fields. There has also been a parallel loss
of larger trees both within hedges and within fields. Part of the
loss can be attributed to Dutch elm disease which has affected elm
trees since the late nineteen sixties. The combination of various
changes and the presence of detracting elements have in places
resulted in erosion of the cohesive and distinct character of the
landscape.
7.8.14 The disused collieries within the area
are now typically used for depots and light industry which are
often visible over a wide area. The North Somerset Railway, which
was important for coal mining in the area, is now
disused.