Area 5 - The Dundry Plateau
Summary of Landscape Character
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Dundry Hill of Oolitic Limestone and lower
shelf / plateau of Lias Limestone
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Open windswept landscape
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Indented valleys at edges of area
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Landslips at junction of limestone and
clay
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Norton Court parkland with parkland
trees
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Small woods and tree belts in valleys and
around settlement
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Prominent modern farm buildings on higher
ground (pig and poultry units),
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Buildings either in small groups or
isolated cottages or farmsteads – typically of Lias Limestone often
rendered or painted
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High species diversity in hedges
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Iron age hill fort at Maes Knoll and strip
lynchets indicating late medieval enclosure of steep-sided
slopes
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Wansdyke linear earthwork
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Disused North Somerset Railway marked by
trees, scrub and field boundaries
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Landmarks include Maes Knoll hillfort and
Norton Malreward church tower.
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Urban fringe problem of tipping along
Whitchurch Lane
Context
Introduction
The Dundry Plateau character area covers an area of 18sq km. of
higher ground. It extends from the south-western edge of Keynsham
westwards to the district boundary near Chew Hill north of Chew
Magna. It rises to a number of significant hills including Maes
Knoll at 197m. and Dundry Hill, beyond the district boundary, at
202m. The boundary generally follows the top of the distinct scarp
slopes. This typically marks the junction between the Lias
Limestone of the plateau and the Mercia Mudstones typical of the
lower lying Chew Valley to the south. The character area of
Stockwood Vale and Charlton Bottom abuts to the north at the
eastern end.
Geology, Soils and Drainage
The most significant geological formation is the Inferior Oolite
of the Jurassic period found on the higher ground including Maes
Knoll. This overlays the Lower Lias Clay found on the adjoining
slopes. The clays make a poor foundation and landslips are
characteristic on the slopes. This area was once connected to the
Cotswolds. The intervening land has subsequently been eroded
leaving this outlier with many of the characteristics of the
Cotswold Plateau.
Equally characteristic is a lower shelf or plateau formed of
white and blue Lias Limestone of the Lower Lias period. This is
typically edged with clay and shale of the Penarth Group.
The soils within this area are often clayey. On the hills and
plateaux the soils are over limestone and are generally well
drained. The soils of the upper slopes by contrast are more silty
and are prone to seasonal waterlogging.
Major planning designations
The whole of the undeveloped area is within the Bristol/Bath
Green Belt and the whole area is within the Forest of Avon
Community Forest area.
Description
Landform and Drainage Pattern
The most characteristic feature of the landscape is Dundry Hill
which forms the highest ground surrounded by a steep scarp leading
to a lower shelf or plateau. The land is generally flat or gently
sloping except for the more dramatic steeply sloping scarp slopes
at the edge of the Oolitic Limestone Dundry Hill and the edge of
the Lias Limestone lower plateau. The landscape is sculpted by a
series of watercourses which arise from this area including those
occupying Charlton Bottom, the valley at Queen Charlton and
numerous tributaries of the River Chew such as those through Norton
Hawkfield and Norton Malreward. These provide the
characteristically indented edge to the character area. The
evocative names of Publow Hill, Hursley Hill, Settle Hill, Guy’s
Hill, Chew Hill and Limeburn Hill reflect the significance of the
landform where routes have been created through this landscape
often becoming eroded over time resulting in dramatic sunken
lanes.
Land-uses
The land is used both for pasture and cereal production. Arable
predominates in areas such as to the west of Maes Knoll while
pasture predominates further east in the area north of Gibbet
Lane.
There are remnants of a significant park at Norton Court
including a number of giant redwood trees. Many of the parkland
trees shown on the 1st Edition OS map have been lost,
however, the park appears to be fairly well preserved around the
buildings of Norton Malreward Court.
Fields, Boundaries and Trees
Fields are mainly enclosed by well-trimmed hedges with high
species diversity; some appear quite wide and are trimmed to an
A-shape. Less frequently hedges are unclipped such as to the south
of Whitchurch. Fields are predominantly medium in size, with small
and large fields also, the large ones concentrated in the western
part of the area. The fields feature few trees. The landscape is
open in appearance with only occasional but very significant trees
within the hedges. There are also occasional scattered small woods
and tree belts. The most significant are located within the valleys
such as around Norton Hawkfield, Norton Malreward and North Wick.
Other wooded parts include Queen Charlton and Queen Charlton Lane,
beside the old railway near New Barn Farm and the steeper slopes
north of Maes Knoll.
Settlement and Communications
A network of minor roads follow the indented valleys such as the
roads through Norton Malreward, Norton Hawkfield and North Wick or
follow higher ground avoiding the steepest slopes. Settlement
generally takes the form of isolated farms or cottages or ribbon
development such as along Gibbet Lane and at Lypiatt. It generally
avoids the highest ground though East Dundry just outside the
district exceptionally is located on higher ground on Dundry Hill.
Villages are typically located around the boundaries of the area on
or at the foot of the surrounding scarp slopes.
Local buildings are traditionally constructed of Lias Limestone,
some with a painted or rendered finish, with slate or clay tiled
roofs. More recent post-war ribbon development such as in Lypiatt
and Gibbet Lane has an assortment of materials including brick,
reconstituted stone and rendering.
Landscape Characteristics
The landscape is open and windswept. The elevated character of
the area gives extensive views taking in the settlements of
Bristol, Keynsham, Saltford and Bath as well as the Chew valley and
Mendip Hills. Conversely the hills of the Dundry plateau are
visible over a wide area forming a backdrop to many views.
The outline of isolated trees, and more rarely small woods or
tree belts, on the skyline are typical of the area. Two of the most
significant historical features within the area are the Iron Age
hill fort at Maes Knoll and the Wansdyke which is a later linear
earthwork which starts at the hill fort and runs to Horsecombe Vale
to the south-west of Bath. The fort is triangular in shape taking
advantage of the natural topography of the hill. The existing scarp
slopes were steepened and a large rampart and ditch were built on
the north-west side. There are also remnants of medieval strip
lynchets on the slopes around Maes Knoll. There is no clear
evidence on the origin or purpose of the Wansdyke however it forms
a significant feature consisting of a substantial bank and ditch on
its northern side. This section from Maes Knoll to Cottles within
the Chew Valley character area is well preserved.
The now disused North Somerset Railway passed through this area
south of Whitchurch. Its course is evident through remaining
earthworks and surviving hedge boundaries. Other landmarks include
the church tower at Norton Malreward.
In the northern part of the character area, along Whitchurch
Lane, typical urban fringe problems of damage to gates and fences,
tipping and car burning are evident in gateways, lay-bys and
passing places – the appearance markedly contrasting with the
otherwise well cared for appearance of the character
area.
Landscape Change and Condition
The landscape appears to be in good condition. There has
generally been little change to the landscape structure since the
1st edition OS map of 1884. Rarely larger fields have
been created by hedge removal such as to the east of Norton
Malreward. Generally only a few hedges have been removed largely to
rationalise smaller fields which were created based on the medieval
strip field system layout.
Changes in agriculture have locally brought significant change.
Of particular significance is the erosion in the extent of the
parkland at Norton Court. Other more subtle changes include
increasing pressure on remaining trees through agricultural
activity with little evidence of replacement planting. The
construction of large agricultural buildings and adding to existing
farm buildings is also having a significant impact on views within
the area.