Galloper Wind Farm Project - National Infrastructure Planning

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2842_SLVIA Appendix 2: Regional Landscape Character Descriptions Coastal Dunes & Shingle Ridges, Coastal Levels, Estate Sandlands and Rolling Estate Sandlands
5 Coastal Dunes and Shingle Ridges EP/Edit1/02.08.10 Coastal Dunes and Shingle Ridges Location Key Characteristics • Flat or gently rolling landform of sand or shingle • Low fragile vegetation • Vast open uncluttered landscape • Historic military structures • Occasional large buildings in an empty landscape • Occasional fishing huts and boats on the beach • Only in short stretches is there the paraphernalia of intensive tourist activity, beach huts and piers This landscape is found in five narrow bands along the Suffolk coast: short stretches to the north of Lowestoft; at Kessingland; from Southwold to the north side of Dunwich; a long stretch from the south side of Dunwich Heath through to Bawdsey, including the substantial shingle spit of Orford Ness; and then a final short stretch at Felixstowe, ending at Landguard Point. There is also a small area of dunes that now form Felixstowe Ferry Golf Links. Geology and landform These shingle ridges or coastal dunes are formed by wave action and longshore drift on sand and stones. When forming beaches, the shingle creates a long high ridge backed by soft cliffs or saltmarsh. However, apart from on Orford Ness there are no areas of natural transition from beach to saltmarsh because of the presence of sea defences. At Orford Ness a succession of shingle ridges has coalesced to form a broad and very flat plain, although the long tail of the spit remains a broad ridge. This 11-mile-long spit is the largest of its type on the east coast and has been evolving since at least the Middle Ages, though the ‘nose’ or ‘ness’ that was more prominent in the past has been largely lost since 1601. Soils and vegetation Because there is essentially no soil on the shingle, it is extremely arid and salty making it very difficult for plants to colonise these habitats. However vegetation does make a contribution to this landscape. Over time, wave action will sort the stone of the beach by size creating ridges of fine material on which it is possible for some plant life to colonise. However any disturbance of this vertical sorting of the stone will cause the matrix of plant roots and fine gravel to break down, resulting in permanent loss of the vegetated shingle. Suffolk Landscape Character Assessment
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Galloper Wind Farm Project Environm
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GALLOPER WIND FARM ENVIRONMENTAL ST
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September 2011 GALLOPER WIND FARM S
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September 2011 GALLOPER WIND FARM S
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2842_LVIA 6 September 2011 GALLOPER
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2842_LVIA 8 September 2011 GALLOPER
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2842_LVIA 10 September 2011 GALLOPE
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2842_LVIA 100 September 2011 GALLOP
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2842_LVIA 154 Receptor, sensitivity
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2842_LVIA 156 Table 5: Effects Summ
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2842_LVIA 158 Receptor, sensitivity
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2842_LVIA September 2011 GALLOPER W
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Character Area 82 Suffolk Coast and
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This area also fostered the first c
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several small greens in an attempt
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1 Ancient Estate Claylands EP/Edit1
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5 Coastal Dunes and Shingle Ridges
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6 Coastal Levels EP/Edit1/02.08.10
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6 Coastal Levels EP/Edit1/02.08.10
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7 Estate Sandlands EP/Edit1/02.08.1
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7 Estate Sandlands EP/Edit1/02.08.1
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7 Guidance Note Estate Sandlands EP
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Management Guidelines 1 Ensure new
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Management Guidelines Sandlings Woo
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Management Guidelines 1 Retain the
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Management Guidelines 1 Do not grub
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How to use the Landscape Character
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Galloper Wind Farm Substation Lands
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2890_mitigation August 2011 Gallope
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2890_mitigation 2 August 2011 Gallo
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2890_mitigation 10 August 2011 Gall
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egion of 16.5m was appropriate on t
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offering to return this to the land
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X:\JOBS\2890 Greater Gabbard - LVIA
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From: Bob.Chamberlain@SuffolkCoasta
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From: Peter.Holborn@suffolk.gov.uk
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From: Rob.Gully@rwe.com To: Colin.M
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Subject: Galloper Wind Farm Landsca
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Path: X:\JOBS\2890 Greater Gabbard
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Path: X:\JOBS\2890 Greater Gabbard
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Path: X:\JO BS\2890 Greater Gabbard
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Path: X:\J O BS\2890 Greater Gabbar
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X/JOBS/2890_Greater Gabbard/6docs/2
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GALLOPER WIND FARM ENVIRONMENTAL ST
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2842_SLVIA Contents 1.0 Introductio
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2842_SLVIA Appendix Appendix 1: Sea
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2842_SLVIA 1 1.0 Introduction 1.1.1
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2842_SLVIA 3 The majority of the WT
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2842_SLVIA 5 2.0 Assessment Methodo
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2842_SLVIA 7 currently available an
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2842_SLVIA 9 Table 2: Consultation
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2842_SLVIA 11 Consultees Date of Co
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2842_SLVIA 13 3.0 Landscape and Sea
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2842_SLVIA 15 3.2. Landscape Design
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2842_SLVIA 17 Suffolk Heritage Coas
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2842_SLVIA 19 Conservation Areas 3.
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2842_SLVIA 21 � Coastal Dunes and
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2842_SLVIA 23 Coastal Levels 4.2.17
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2842_SLVIA 25 Beyond the ongoing te
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2842_SLVIA 27 4.2.37. This landscap
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2842_SLVIA 29 Sensitivity to Change
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2842_SLVIA 31 seascape and visual e
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2842_SLVIA 33 dominated by the buil
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2842_SLVIA 35 visible from within i
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2842_SLVIA 37 visible from within i
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2842_SLVIA 39 Extensive, long dista
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2842_SLVIA 41 Perceptual Qualities
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2842_SLVIA 43 5.2.4. As can be seen
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2842_SLVIA 45 River Ore and to east
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2842_SLVIA 47 5.4.7. It is assumed
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2842_SLVIA 49 5.8.3. Distances from
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2842_SLVIA 51 Distance and Directio
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2842_SLVIA 53 interest within the v
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2842_SLVIA 55 Viewpoint 5 - Orford
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2842_SLVIA 57 Existing View 5.8.21.
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2842_SLVIA 59 5.8.25. The viewpoint
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2842_SLVIA 61 Table 8: Existing Vie
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2842_SLVIA 63 main effect. There wi
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2842_SLVIA 65 Special Landscape Are
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2842_SLVIA 67 6.3.11. Similarly, fo
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2842_SLVIA 69 6.4. Operational Effe
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2842_SLVIA 71 Table 10: Operational
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2842_SLVIA 73 nature and extent wit
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2842_SLVIA 75 the proposed WTGs of
Page 396 and 397: 2842_SLVIA 77 7.3. Representative V
Page 398 and 399: 2842_SLVIA 79 Magnitude and Signifi
Page 400 and 401: 2842_SLVIA 81 east-southeast sector
Page 402 and 403: 2842_SLVIA 83 horizon line by appro
Page 404 and 405: 2842_SLVIA 85 Viewpoint Viewpoint 5
Page 406 and 407: 2842_SLVIA 87 Alderton and to Oak H
Page 408 and 409: 2842_SLVIA 89 structures/embankment
Page 410 and 411: 2842_SLVIA 91 8.0 Cumulative Effect
Page 412 and 413: 2842_SLVIA 93 8.4. Cumulative Seasc
Page 414 and 415: 2842_SLVIA 95 8.5.2. The assessment
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Page 420 and 421: 2842_SLVIA 101 effects. There could
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Page 428 and 429: 2842_SLVIA Appendix 1: Seascape, La
Page 430 and 431: 2842_SLVIA � The effects of histo
Page 432 and 433: 2842_SLVIA � A desk study of nati
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Page 436 and 437: 2842_SLVIA � High - Total or majo
Page 438 and 439: 2842_SLVIA Making positive/adverse
Page 440 and 441: 2842_SLVIA how each of the key char
Page 442 and 443: 2842_SLVIA fact that they are in a
Page 444 and 445: 2842_SLVIA The cumulative assessmen
Page 448 and 449: 5 Coastal Dunes and Shingle Ridges
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Page 452 and 453: 6 Coastal Levels EP/Edit1/02.08.10
Page 454 and 455: 6 Coastal Levels EP/Edit1/1.10.10 C
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Page 458 and 459: 7 Estate Sandlands EP/Edit1/02.08.1
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Page 462 and 463: 7 Guidance Note Estate Sandlands EP
Page 468 and 469: 16 Guidance Note Rolling Estate San
Page 470 and 471: 16 Guidance Note Rolling Estate San
Page 472 and 473: 16 Rolling Estate Sandlands EP/Edit
Page 474 and 475: 2842_SLVIA Appendix 3: Methodology
Page 476 and 477: 2842_SLVIA viewpoint is then genera
Page 478 and 479: 2842_SLVIA Appendix 4: Source Docum
Page 480 and 481: 2842_SLVIA Landscape capacity refer
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