Upper Piddle Valley
In contrast to the Cerne & Sydling Valley, the Upper Piddle Valley, with the associated River Piddle, Devils Brook and Cheselbourne, has a more enclosed character defined by a ‘V’ shaped profile and dry, rounded coombes.
In contrast to the Cerne & Sydling Valley, the Upper Piddle Valley, with the associated River Piddle, Devils Brook and Cheselbourne, has a more enclosed character defined by a ‘V’ shaped profile and dry, rounded coombes.
In contrast to the Cerne & Sydling Valley, the Upper Piddle Valley, with the associated River Piddle, Devils Brook and Cheselbourne, has a more enclosed character defined by a ‘V’ shaped profile and dry, rounded coombes. There is a branching pattern of narrow, steep-sided dry coombes, off the main central valley with small pockets of broad-leaved woodland and relic hazel coppice with rough chalk pastures and patches of scrub. Towards the upper slopes, open and expansive uplands of large arable fields are crossed with straight roads leading down the valley sides. Towards the northern escarpment the landscape becomes smaller scale with steep valley sides. Linear settlements follow historical transport routes that connect villages along the valley floor. Settlements are enclosed by small-scale pastoral fields with dense hedgerows and hedgerow trees with old water meadows along the floodplain and remnant areas of parkland, making such areas intimate and enclosed places with strong historical associations.
Land shape and structure
The Upper Piddle Chalk Valley and its tributaries of the Devils Brook and Chesselbourne drain into the River Piddle to the south. The narrow valley bottom retains a sense of enclosure from the surrounding hollows and coombes rising towards the open uplands. The valley bottoms are particularly enclosed towards the north by the twisting escarpment.
Soils and vegetation
The chalk provides free draining soils which on the steeper slopes support small relic areas of unimproved chalk grassland and patches of scrub. Small broadleaved woodlands and relic hazel coppice are found dotted along the valley sides leading down towards damper pastures along the valley bottom. An extensive area of chalk downland is found at Lyscombe Bottom.
Settlement and land cover
Linear settlements within the valley follow the linear road system. The southern part of the valley has more of an urbanised character than other chalk valleys, with business and industrial land uses encroaching into the open countryside. As with other valleys, landcover is typically pastoral along the valley floors with extensive arable fields on the surrounding uplands.
Historic character
In the western half of the valley, strip fields predominate. Elsewhere, the character is planned enclosures with a concentration of parliamentary enclosures in the south west. Broadleaved woodlands are found on the valley sides with more recent small coniferous woodlands to the west of the area. The network of field boundaries and footpaths often reflect the tracks, droves and hollow ways that took the livestock to and from the downs in prehistoric times. Cross dykes and earthworks survive at Lyscombe Bottom with large expanses of prehistoric fields found throughout the area.
Visual character and perceptions
The narrow valley floor defines the intimate and enclosed visual character of the Upper Piddle valley. Landscapes surrounding settlements often have a strong cultural association, with small pastures leading up towards the larger scale arable farmland. Although the area retains a strong sense of rural tradition, there is pressure to increase the scale and intensity of farming enterprises. Accommodating such expansion within elevated and visually exposed locations is particularly challenging and there is a risk that the cumulative effects of such growth may erode the undeveloped rural character of the area.
Strength of character
The landscape is judged to have a moderate character. Although the distinctive valley landform evokes a consistent sense of place and visual unity, the distinct and recognisable pattern of features such as grazed valley floor pasture, historic water meadows, parklands, vernacular linear villages are less apparent than other chalk valleys. There are some detracting features that weaken the character, such unsympathetic Leylandii planting and signage that occur along the lanes, and urban fringe land use. Some arable use along the valley floor has weakened the pattern of characteristic damp chalk pastures.
Condition
Only small and isolated areas of semi-natural habitat remain in the Piddle Valley. Patches of remnant chalk grassland have become fragmented by woodland planting and extensive arable use on the valley sides. Along the valley floor, wet woodlands and meadows are now mostly confined to a narrow line of Willow and Alder along the river. Traditional water meadow management is no longer practiced. Settlements edges often intrude into the open countryside with many boundaries often being in relatively poor condition. Traffic along the road network impacts on the surrounding rural tranquillity. Extensive areas of chalk upland have been subject to agricultural intensification with a loss of boundaries and natural habitat. Overall landscape condition is moderate and stable.
The overall management aim should be to conserve the strong pattern of existing features, whilst restoring woodlands and meadows, chalk grasslands and boundary features. To maintain undeveloped rural character, careful consideration should be given to the design of developments such as settlement extensions and large agricultural barns. Sensitive siting and tailored landscaping measure should be pursued. Indirect effects arising from farm diversification and intensification should be considered, particularly where widespread changes to landscape management may arise.
Planning guidelines
Management guidelines