LCA5J Lower River Anton Valley Floor
General
Description
The Lower River Anton Valley Floor is a relatively narrow valley
that joins the River Test at Fullerton through which the River Anton
meanders and braids through woodland copses and well hedged fields,
before joining the River Test. It has an intimate and pastoral character
throughout, with some detracters causing local impact.
Earthworks from the dismantled railway and old canal create a
series of linear features along the southern edge.
Location
The Lower River Anton Valley Floor follows the River Anton from
its confluence with Pillhill Brook on the southern edge of Andover
to where it joins the River Test at Cottonworth.
Local Physical Influences
Geology and soils: Alluvium with
Valley Gravels to the immediate south of Andover.
Landform: Flat valley bottom with
adjacent broad slopes of the chalk downlands.
Drainage: Braided stream with numerous small
streams and ditches. The valley contains the confluence of the River
Anton with Pillhill Brook and a number of ponds and lakes within
former gravel pits.
Local Biodiversity and Vegetation Pattern
The dominant pattern in this area is permanent pasture with few
patches of woodland. Overall the area is a continuation of the downs
with quite dry pastureland reaching the river. The meadows in general
have been improved for agriculture in some way and there are only
a few that are typical traditional grazed hay meadows. Although
they still support fine-leaved grasses such as Red Fescue, Crested
Dogs-tail and Velvet Bent, coarser grasses such as Yorkshire Fog
are more frequent and the variety of flowering plants is reduced.
Other notable habitats include areas of wet carr woodland, which
with hedgerows, link to patches of ancient and semi-natural woodland
and provide an important resource. The native White-clawed crayfish
is also found in this section (a nationally important BAP species).
Local Historical Influences
A series of bedwork water meadows (Type 4) extend through the
valley of the River Anton and, combined with miscellaneous valley
floor enclosures, form the major historic landscape of the valley
floor. A single catchwork water meadow (Type 1) is present to the
south of Upper Clatford. Extensive areas of 19th century parliamentary
field systems flank the valley floor.
Settlement Pattern
The settlements of Goodworth Clatford and Upper Clatford cross
the valley floor of the river Anton and their historic cores are
both focused upon the bridging points across the Anton. There is
little later development during the later post-medieval period in
the valley floor close to these small settlements.
Very few farms occupy the valley floor of this character area
and are generally located upon the first river terrace.
Goodworth Clatford originally straddled the river Anton with historic
elements to be found on both banks. Later post-medieval settlement
has developed along the three approach roads, creating a more linear
form dispersing up the valley sides.
Upper Clatford also straddles the river Anton and has developed
in a westward direction along Philhill Brook, creating a linear
settlement, linking to the A343.
The road network is predominantly confined to the southern valley
side, starting at Goodworth Clatford. There are only two crossing
points, these are located on the two settlements.
Local Settlements and Features of Built Form
Goodworth Clatford (Eastern portion): Chalk River Valley Settlement
Type
Upper Clatford (Eastern portion); Chalk River Valley Settlement
Type
Older properties are commonly half-timbered and thatched
but the most widespread materials are brick and flint. Clay tiles
and chalk cob are also common features.
Community Perceptions
No specific comments were made for this area.
Remoteness and Tranquillity
Away from the A303 and settlement the area is secluded and quiet.
The northern end of the area is significantly affected by modern
development but is vulnerable to further visual intrusion.
Key Characteristics
River gravels and alluvium over chalk
Braided river, with the main tributary meandering across the valley
floor
Open valley floor dominated by pasture creating a strong rural
character
Land use predominantly pasture or meadow grassland
Watercress cultivation
Poplar, willow and alder lined watercourses
Settlements centred on crossing points as at Goodworth Clatford
Detractors include the sewage works, the overhead pylons and the
A303(T). The visual impact is however partly mitigated by screen
planting
Local change in character due to new housing development at Upper
Clatford
Survival of valley floor enclosures and water meadows
Presence of historic village cores straddling the River Anton.
Local Natural and Cultural Landscape Issues
Valley floor housing developments associated with Andover and
attached to Goodworth Clatford and Upper Clatford
Risk of damage to surviving earthwork evidence for water meadow
activity along the upper reaches of the River Anton
Pollution of the river and its tributaries through fertiliser
and road run off and aqua culture ventures (fish farms, water cress
beds)
Visual and acoustic impact of the A303.
Designations
Nature Conservation
SINC
3 SINCs, including agriculturally unimproved grassland and reedbed
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