122.2.8 On the hills above the London Clay, the capping of the fine sands of the Bagshot Beds by thepebbly clay drifts have led to acidic soils with low natural fertility that are easily cultivated.2.2.9 In the northwest of the Study Area, the geology changes to glacial tills composed of sandsand gravels overlain by the most extensive soils in the area, pelosols. These are heavy acidicsoils often prone to waterlogging in winter months and to shrinking and cracking in summerresulting in a predominance of pasture fields on the low hills and ridges.2.2.10 In the northwest of Uttlesford, the altitude reaches just over 130m AOD to the west ofSaffron Walden. In this area the chalk is exposed at the surface and has given the area itscharacteristic rolling topography and free draining poor alkaline soils that support widespreadcereal farming.2.2.11 The Study Area has a large intricate network of rivers and streams. These are an importantcomponent of the area’s topography, character and identity and are frequently of landscape,nature conservation and heritage value. To the north the valleys become steeper and moredeeply cut.2.2.12 Most of the rivers flow towards either the Thames or the North Sea (see Figure 2.2). Onlythe Cam flows northward. Principal rivers within the Study Area are the Stour, Colne,Blackwater, Chelmer and Crouch. The Colne, Blackwater, Chelmer and tributaries rise in theplateau to the north and flow south where their estuaries are extensive and contribute to thedeeply indented coastline. The Crouch flows east across the undulating lowland to the southof the plateau and when joined by the Roach forms an estuary complex that includes theislands of Wallasea, Potton and Foulness.2.2.13 The coastline is mainly marshland and is characterised by a maze of winding shallow creeks,drowned estuaries, mudflats and broad tracts of tidal salt-marsh with sand and shinglebeaches along the coast edge. The relatively permanent, branching, meandering creeks,dissect the salt marshes.Landcover and Ecological <strong>Character</strong>2.2.14 The rural landscape of the Study Area is predominantly used for arable or improved pasture,particularly on the flat or gently undulating land. The rich soils are intensively cultivated andlarge cereal fields are a major feature of the landscape. The cereal field margins occasionallysupport uncommon plants such as cornflower, broad-leaved cudweed, corn cleavers andshepherd’s needle.2.2.15 There are significant areas of remaining semi-natural habitat that make an importantcontribution to the area’s distinctive character. The presence and distribution of thesehabitats is strongly influenced by geology and landform, and include woodland, grassland,heath, estuary, saltmarsh and mudflat and freshwater and open water habitats. Many siteswhere these habitats occur are designated as Ramsar Sites, candidate Special Areas ofConservation (cSAC), Sites of Special Scientific Interest (SSSI), Sites of Importance forNature Conservation (SINCs) 1 , Special Protection Areas (SPA), National Nature Reserves(NNR) and/or Local Nature Reserves (LNR). The distribution of these areas designated fortheir nature conservation value are shown on Figure 2.3 and described below in relation tokey habitat types.1 SINCs are also referred to as County Wildlife Sties, which will become known as Local Wildlife Sites in duecourse.Section 2.0 – Overview of the Study Area11100101R Final LCAs_09-06
13Woodland2.2.16 There are areas of lowland beech and yew woodland scattered in the west of the Study Areaon the pelosols overlying glacial tills. This type of woodland includes a variety of vegetationtypes reflecting soil and topographical differences. The canopy can include mixtures ofbeech, ash, sycamore, yew and whitebeam. Some of these woods are former pasturewoodland, where grazing as well as wood production was practised.2.2.17 Ancient Woodland, practically all of which have been coppiced since medieval times orearlier, are found throughout the Study Area on the various soil types. Examples of theancient woodland include Bovingdon Hall Woods SSSI (north of Braintree), West Wood,Little Sampford SSSI (northeast of Thaxted), Nunn Wood SSSI (west of Ashdon). Many ofthe areas of ancient woodland are ancient Pedunculate Oak-Hornbeam coppice-withstandardswoodland. They provide valuable habitats for invertebrates, dormouse andbreeding birds.Grassland2.2.18 There are a number of broad types of grassland determined by the plant species which arelargely influenced by the soil type and underlying geology. However within the Study Area alot of the grassland has been drained and agriculturally improved for pasture, but somegrasslands of conservation importance remain. For example there are two small areas ofcalcareous grassland on the chalk hills at Debden Water SSSI near Newport in the northwestof the Study Area and a further small area of calcareous grassland as well as unimprovedneutral grassland at Ashdon Meadows SSSI near Saffron Walden.2.2.19 Wet grasslands are also common in the Study Area. Of particular importance are thefloodplain marshes of the Thames and Cam, where areas of permanent grassland aredeliberately flooded to prevent rivers over-topping.Heath2.2.20 The largest remaining fragments of heath within the Study Area are located around Danburyeast of <strong>Chelmsford</strong> on the brown calcareous earths. Danbury Common SSSI is one of thelargest areas of heathland remaining in Essex and shows various stages in the successionfrom open heath, through bracken and gorse scrub, to birch and oak woodland. The upperparts of the site are located on the glacial gravels capping Danbury Ridge. Lower down,spring lines and flushes at the junction between the gravels and the underlying clay give riseto boggy areas of heath and moist woodlands. Unimproved meadows adjacent to theCommon support a rich grassland flora including a number of uncommon species. There arealso other smaller fragments found in the south and in the northeast corner.Estuary, Saltmarsh and Mudflat2.2.21 The Essex Coast is among the top five coastal wetlands in the UK. Grazing marshesdominate the southeast corner of the Study Area along the coast of the Greater ThamesEstuary such as at Sandbeach Meadows SSSI located on the intertidal alluvial muds. Theestuaries, floodplain and coastal marshes are important for the invertebrate fauna of both thewet grasslands and their associated ditches, and support internationally important populationsof wintering waterfowl. These areas along the coast of the Study Area are of internationalsignificance and designated as candidate Special Areas of Conservation (cSACs), SpecialProtection Areas (SPAs), or Ramsar sites as well as Sites of Special Scientific Interest(SSSIs) and National Nature Reserves (NNRs).11100101R Final LCAs_09-06Section 2.0 – Overview of the Study Area
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187 Potential major road improvemen
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3428.2.3 Planners, developers, arch
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344Drafting Core Policies and Suppo
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348 change in the degree of key fac
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APPENDIX ASTAKEHOLDER CONSULTATION
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with the County assessment, but sho
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Fit with adjacent classificationsCB
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Appendix A - Stakeholder Consultati
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CBA gave a brief overview of the st
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9. Summary and Recommendations/Appl
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GLOSSARYCommunity StrategyAll local
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APPENDIX CSOURCES OF FURTHER INFORM
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English Heritage, 2003, Register of
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HISTORIC LANDSCAPE CHARACTER AREAS
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APPENDIX ECURRENT LOCAL PLANNING SI
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APPENDIX FDRAFT CORE STRATEGY LANDS
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