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28 2.1.2 Enclosed West Chalk UplandsKey characteristic features • Broad, rolling upland relief incised by branching, rounded dry valley
systems. Landform and contextThe south facing dip-slope of the west chalk uplands displays the broad, rounded ridges and gently curving slope profiles typical of chalk upland relief. The landform becomes more steeply undulating, and in places deeply folded, particularly towards the north, where the sloping chalk plateau is most elevated. The enclosed west chalk uplands landscape extends westwards from the Arun valley to the Hampshire border. Further east, the southern part of the chalk dip-slope between the Arun and the Findon valleys is also included within this landscape character area. The chalk dip slope in these areas is made up of Upper and Middle Chalk. Clay-with-Flints occurs only very locally; on the ridgetop of Bow Hill and in the Stansted Forest area to the west. The uplands have been carved into sweeping forms by dry valleys, which in places form steep, rounded coombes. Many of these branching dry valley systems are included within the enclosed west chalk uplands landscape character area. The historic combination of land use and landscape pattern has made this landscape a finely detailed mosaic in which such subtle contrasts of landform are a less important influence on visual character than in the more exposed chalk uplands to the east. However, the branching valleys of the Ems and the Lavant do provide a significant contrast in relief. These relatively broad valleys have eroded the upland plateau to leave undulating ridges which extend southwards and westwards from the escarpment to subdivide the uplands on a larger scale than is typical of the open chalk uplands of East Sussex. These ridges, which include the summits of Bow Hill, Charlton Down and Rewell Hill, broadly structure the topography of the west chalk uplands. Some are remnants of the secondary escarpment along the southern edge of the dip slope. This more elevated land is indicated on the landscape character map as large-scale enclosed west chalk uplands, broadly separating it from areas of the dip-slope which have lower relief and which generally have a more subdivided landscape pattern with a smaller scale. Land use and landscape patternThis landscape is made up of a diverse mosaic of different land uses and landscape patterns. Woodlands, copses and areas of extensive commercial forestry subdivide farmland in which arable land predominates, but which also includes substantial areas of pasture and smaller fragments of chalk grassland and scrub. The picture is further complicated by the strong influence of several large estates and designed parkland landscapes with their distinctive sweeping landforms and carefully grouped clumps of trees. Such estates own substantial areas of the dip-slope. Each typically encompasses a wide variety of different landscapes and their presence over the years has helped to maintain the typically diverse landscape pattern. This landscape is particularly rich in local, distinctive features such as individual rounded summits, follies, banks, and avenues which form characterful landmarks and give the area a strong, expressive identity. The landscape mosaic tends to have a larger, bolder scale and a less regular form on the more elevated land. Here woodland and commercial forestry plantations are more extensive and fields are generally larger with irregular shapes. They are often partially enclosed by woodland. The steep slopes of the many deep coombes in these areas are usually a combination of pasture, rough grazing and patches of woodland. Forest edges are often bold and straight, forming strong woodland blocks which sometimes create hard, rather geometric edges. This is particularly evident along the northern margins of the chalk dip slope where the woodlands abut the open rounded summits of the wooded chalk escarpment. The division between the large-scale landscape mosaic on the more elevated parts of the dip slope and the finer-grain of the smaller scale landscape on the lower slopes is not clear-cut. There is a very gradual transition which in places is masked by local variation. On the lower slopes of the chalk plateau the fields become considerably smaller and form a more coherent patchwork. Most have irregular shapes but straight edges. The visual effect of such geometric outlines tends to be softened by the presence of numerous small woodlands, especially where these have irregular, organic shapes. Hedgerows enclose most fields and the small blocks of woodland are important elements in the landscape, linking with the hedgerows and hedgerow trees to give a relatively enclosed character. Arable farmland predominates, but is interspersed with areas of pasture, much of which is intensively managed. The combination of farmland, woodland and hedgerows on the undulating chalkland relief creates a complex, diverse patchwork in which trees and fields form distinctive local patterns. Historic parkland landscapes often interrupt the farmland patchwork and designed features such as avenues, follies and vistas contribute to the lively, unpredictable character of this landscape. This landscape pattern continues to the east of the Arun valley, although here large estates have less influence. This, together with the narrowing of the AONB, has resulted in a simplified landscape mosaic with less land use diversity. SettlementNumerous small villages and hamlets, typically with a nuclear form, are grouped in sheltered sites throughout the small-scale landscape of the lower slopes. The more elevated areas are less populated but there are many individual farms, isolated farm cottages and, occasionally, tiny hamlets on the upper slopes of the ridges and within woodland clearings. The villages tend to be strongly hierarchical in form, with large houses surrounded by cottages and farms. The larger properties are often carefully sited on sloping land at a slight distance from the village and are prominent features in local views. Chalk flint is the most important building material; often attractively edged in red brick. Villages on the south margins of the dip-slope tend to have a more diverse mix of buildings, with rendered and brick houses interspersed with those of the traditional flint. The influence of the estates is made evident in most villages, and the countryside immediately surrounding them, by the presence of well-built flint stone walls which give enclosure and character to the settlements. Subjective responseThe combination of farmland, woodlands and dense hedgerows provide a rich variety of landscape patterns, all with a strong sense of enclosure and a bold, distinctive identity. The landscape of the enclosed west chalk uplands seems all the more diverse and secluded because it contrasts so dramatically with the bleaker, exposed open chalk uplands to the east. The bold patchwork of farmland and woodland, combined with undulating relief, forms a particularly diverse landscape with many contrasts of texture and form. The overall impression is one of well-balanced, harmonious rural scenery, where views are unpredictable and constantly changing; panoramas from high points such as Bow Hill and The Trundle are particularly important in understanding the overall setting and form of the area in relation to its surroundings. Such viewpoints describe the coastal plain to the south and the chalk escarpment to the north. The many villages, distinctive local features and historic parklands give the landscape an idyllic, welcoming character. Much of the area seems deeply rural, but without feeling remote or inaccessible. The clustered villages, stone walls and parkland features have a timeless quality and evoke a strong sense of history. Hundreds of years of management have left many traces, from ancient earthworks to yew forests and stately homes. It all adds to the intrigue, mystery and rich variety of local interest which characterise this landscape. Sensitivity to changeThe relatively wooded character of this landscape gives it some capacity to absorb change without reducing its overall visual integrity. However, the broad, rolling form of the chalkland relief ensures that most of the landscape is highly visible, since any one area might be viewed from a number of different aspects. This complexity and diversity, and an associated sense of unpredictability, combine to make a significant contribution to local character. Detailed visual analysis, which takes account of the full range of possible viewpoints, is therefore an essential prerequisite to any form of built development and should also be considered in relation to changing patterns of land use related to forestry and agricultural practice. In general terms, very small-scale changes can be accommodated in this area if they are carefully sited and designed so that they are closely integrated with the pattern and scale of the local landscape. The most vulnerable areas are likely to be parts of the small-scale enclosed west chalk uplands where there is an irregular, finely-grained pattern of fields and hedgerows. Such areas are often closely related to settlement and are therefore under particular pressure for change. Examples are the expansion of horse paddocks and planting for game crops, shelterbelts and small plantations which are unrelated to landform and existing hedgerow patterns and the proliferation of modern farm buildings. In addition, the creeping commercialisation of the larger estates may represent a threat to the overall unity of the landscape, and in particular the setting of the historic parklands. Road improvements, signage, car parks and the use of exotic species in planting schemes are likely to be particular concerns and require careful control to ensure that they do not have a negative visual impact. Key issues for landscape managementFarmland mosaic • Retain and strengthen the existing diversity of the landscape mosaic,
and in particular the broad variations between the large-scale landscape
pattern on the more elevated slopes and the smaller-scale patchwork of
fields and woodlands on the lower chalk dip-slope. Wherever possible,
plan ongoing changes in land uses to reflect these variations in scale
so as to give more visual emphasis to landform. Hedgerows• The visual structure of this landscape is determined by the scale of its patchwork of fields and hedgerows. Future management should ensure that the existing hedgerow network is maintained and reinforced along its existing alignments. Where hedgerow trees are characteristic, they should be planted to provide visual links with small woodlands and copses and to enhance the setting of farms and villages within the wider landscape. • There is some evidence to suggest that hedgerows have been removed to increase agricultural productivity. Wherever possible, replanting should be considered to strengthen the hedgerow network, defining the lane and field boundaries in areas where it has been depleted. Sympathetic hedgerow management should be encouraged and mechanical over-flailing avoided. • Conserve hedgerows, banks and broad verges associated with existing tracks and byways to retain their importance as visual features within the wider landscape. Trees and woodland • New planting should be designed to reflect and emphasise the existing
scale and structure of the landscape. Within the large-scale landscape,
areas of woodland should be extensive, with woodland edges partially enclosing
groups of fields at a time. In contrast, the small-scale landscape should
contain smaller woodlands which closely relate to the existing hedgerow
structure. Parkland• Encourage conversion of arable land to permanent pasture in areas of
parkland trees. Priorities for action • Management of small woodlands. Modify and design the structure and
edges of larger woodlands and commercial plantations. |