Sussex: Rye Bay to Chichester Harbour
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126. South Coast Plain Area Profile: Supporting Documents
National Character 126. South Coast Plain Area profile: Supporting documents www.naturalengland.org.uk 1 National Character 126. South Coast Plain Area profile: Supporting documents Introduction National Character Areas map As part of Natural England’s responsibilities as set out in the Natural Environment White Paper,1 Biodiversity 20202 and the European Landscape Convention,3 we are revising profiles for England’s 159 National Character Areas North (NCAs). These are areas that share similar landscape characteristics, and which East follow natural lines in the landscape rather than administrative boundaries, making them a good decision-making framework for the natural environment. Yorkshire & The North Humber NCA profiles are guidance documents which can help communities to inform West their decision-making about the places that they live in and care for. The information they contain will support the planning of conservation initiatives at a East landscape scale, inform the delivery of Nature Improvement Areas and encourage Midlands broader partnership working through Local Nature Partnerships. The profiles will West also help to inform choices about how land is managed and can change. Midlands East of Each profile includes a description of the natural and cultural features England that shape our landscapes, how the landscape has changed over time, the current key drivers for ongoing change, and a broad analysis of each London area’s characteristics and ecosystem services. Statements of Environmental South East Opportunity (SEOs) are suggested, which draw on this integrated information. South West The SEOs offer guidance on the critical issues, which could help to achieve sustainable growth and a more secure environmental future. -
Population Change in an East Sussex Town Lewes 1660-1800
SUSSEX INDUSTRIAL HISTORY Winter 1971/72 & Section of the River. -i _1 7o* re, eo ,ae? /tie Enjoy the fuller flavour of Carling Black Label SUSSEX INDUSTRIAL HISTORY Journal of the Sussex Industrial Archaeology Study Group THREE WINTER 1971/72 page POPULATION CHANGE IN AN EAST SUSSEX TOWN : 2 LEWES 1660-1800 James P. Huzel KINGSTON MALTHOUSE, 1844-1971 20 Adrian Barritt NOTES AND NEWS 29 BOOK REVIEW 32 Edited by John Farrant, Arts Building, University of Sussex, Falmer, Brighton, BN 1 9QN . Sussex Industrial History has as a principal objective the publication of the results of recording, surveying and preservation of industrial monuments and processes done under the aegis of the Sussex Industrial Archaeology Study Group . But its field is not narrowly defined, for it aims to integrate the findings of industrial archaeology into general historical thinking and writing, by studying the impact of industrial change, principally during the past two centuries, on a rural county. The Editor is very interested to hear from prospective contrib- utors of articles of any length, and to receive items for the `Notes and News' section on work in progress, requests for information and assistance, recent publications, forthcoming conferences and meetings. Published twice yearly ; annual subscription 75p (15s.). Subscriptions and all business or advertising correspondence should be addressed to the publisher, Phillimore & Co . Ltd., Shopwyke Hall, Chichester, Sussex . Contributions and correspondence about editorial content should be addressed to the Editor. Members of S.I.A.S.G. receive Sussex Industrial History free; enquiries about membership should be addressed to the General Secretary, E.J. -
Agenda Item 7 Report PC15/17 Report to Planning Committee Date
Agenda Item 7 Report PC15/17 Report to Planning Committee Date 9 March 2017 By Director of Planning Title of Report Revised Policies for the Pre-Submission South Downs Local Plan Purpose of Report To comment on the revised policies of the Pre-Submission South Downs Local Plan Recommendation: The Committee is recommended to 1) Endorse the direction of the policies as detailed in Appendices 1 to 7 of this report for inclusion in the Pre-Submission Local Plan document, subject to any comments made by the Planning Committee being addressed. 2) Note that the Pre-Submission Local Plan will be reported to Planning Committee for consideration prior to publication for public consultation, and 3) Note that the Pre-Submission Local Plan document will be subject to final approval by the National Park Authority. 1. Summary 1.1 This report introduces the following revised draft Local Plan policies, which are set out as appendices to this report: Appendix 1: Sites & Settlements Appendix 2: Strategic Sites Appendix 3: Affordable Housing Appendix 4: Green Infrastructure Appendix 5: Water Appendix 6: Climate Change Appendix 7: Design 1.2 The first recommendation is that they are endorsed for inclusion in the emerging Local Plan, subject to any comments made by the Planning Committee being addressed. This endorsement would also acknowledge that the policies may need further amendments prior to being incorporated into the whole document, in order to fit within other draft policies. Recommendations (2) and (3) also note that the complete draft Pre-Submission Local Plan will be reported to Planning Committee for consideration prior to final approval by the South Downs National Park Authority (SDNPA) for consultation. -
Shoreline R2: Brighton to Rottingdean R1
R2 Landscape Character Areas R1 : Seaford to Beachy Head Shoreline R2: Brighton to Rottingdean R1 R: Shoreline R2 Historic Landscape Character Fieldscapes Woodland Unenclosed Valley Floor Designed Landscapes Water R1 0101- Fieldscapes Assarts 0201- Pre 1800 Woodland 04- Unenclosed 06- Valley Floor 09- Designed Landscapes 12- Water 0102- Early Enclosures 0202- Post 1800 Woodland Settlement Coastal Military Recreation 0103- Recent Enclosures Horticulture 0501- Pre 1800 Settlement 07- Coastal 10- Military 13- Recreation 0104- Modern Fields 03- Horticulture 0502- Post 1800 Expansion Industry Communications Settlement 08- Industry 11- Communications R: Shoreline LANDSCAPE TYPE R: SHORELINE R.1 The Shoreline landscape type comprises the narrow band of inter-tidal beach that occurs at the base of the steep chalk cliffs, and is defined between the high or the cliff top, and low water marks. DESCRIPTION Integrated Key Characteristics: • Inter-tidal shoreline occurring at the base of the steep chalk cliffs where the South Downs meet the sea. • Characterised by flint shingle beaches, formed from erosion of chalk to reveal flint nodules that are eroded into pebbles. • Chalk rubble, resulting from cliff falls, forms spits of land that extend into the sea. • A dynamic and continually changing landscape featuring constant erosion and re- stocking of the beaches. • An exposed, wild landscape which is open to the elements and whose character is governed by the weather. • Engineered solutions to coastal erosion, sometimes extensive, such as wooden or concrete groynes and concrete retaining structures. • Coastal features such as lighthouses, associated with coastal navigation, and anti- invasion defences. • Extensive views out across the sea to the horizon. -
Barcoding Chrysomelidae: a Resource for Taxonomy and Biodiversity Conservation in the Mediterranean Region
A peer-reviewed open-access journal ZooKeys 597:Barcoding 27–38 (2016) Chrysomelidae: a resource for taxonomy and biodiversity conservation... 27 doi: 10.3897/zookeys.597.7241 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research Barcoding Chrysomelidae: a resource for taxonomy and biodiversity conservation in the Mediterranean Region Giulia Magoga1,*, Davide Sassi2, Mauro Daccordi3, Carlo Leonardi4, Mostafa Mirzaei5, Renato Regalin6, Giuseppe Lozzia7, Matteo Montagna7,* 1 Via Ronche di Sopra 21, 31046 Oderzo, Italy 2 Centro di Entomologia Alpina–Università degli Studi di Milano, Via Celoria 2, 20133 Milano, Italy 3 Museo Civico di Storia Naturale di Verona, lungadige Porta Vittoria 9, 37129 Verona, Italy 4 Museo di Storia Naturale di Milano, Corso Venezia 55, 20121 Milano, Italy 5 Department of Plant Protection, College of Agriculture and Natural Resources–University of Tehran, Karaj, Iran 6 Dipartimento di Scienze per gli Alimenti, la Nutrizione e l’Ambiente–Università degli Studi di Milano, Via Celoria 2, 20133 Milano, Italy 7 Dipartimento di Scienze Agrarie e Ambientali–Università degli Studi di Milano, Via Celoria 2, 20133 Milano, Italy Corresponding authors: Matteo Montagna ([email protected]) Academic editor: J. Santiago-Blay | Received 20 November 2015 | Accepted 30 January 2016 | Published 9 June 2016 http://zoobank.org/4D7CCA18-26C4-47B0-9239-42C5F75E5F42 Citation: Magoga G, Sassi D, Daccordi M, Leonardi C, Mirzaei M, Regalin R, Lozzia G, Montagna M (2016) Barcoding Chrysomelidae: a resource for taxonomy and biodiversity conservation in the Mediterranean Region. In: Jolivet P, Santiago-Blay J, Schmitt M (Eds) Research on Chrysomelidae 6. ZooKeys 597: 27–38. doi: 10.3897/ zookeys.597.7241 Abstract The Mediterranean Region is one of the world’s biodiversity hot-spots, which is also characterized by high level of endemism. -
Streams, Ditches and Wetlands in the Chichester District. by Dr
Streams, Ditches and Wetlands in the Chichester District. By Dr. Carolyn Cobbold, BSc Mech Eng., FRSA Richard C J Pratt, BA(Hons), PGCE, MSc (Arch), FRGS Despite the ‘duty of cooperation’ set out in the National Planning Policy Framework1, there is mounting evidence that aspects of the failure to deliver actual cooperation have been overlooked in the recent White Paper2. Within the subregion surrounding the Solent, it is increasingly apparent that the development pressures are such that we risk losing sight of the natural features that underscore not only the attractiveness of the area but also the area’s natural health itself. This paper seeks to focus on the aquatic connections which maintain the sub-region’s biological health, connections which are currently threatened by overdevelopment. The waters of this sub-region sustain not only the viability of natural habitat but also the human economy of employment, tourism, recreation, leisure, and livelihoods. All are at risk. The paper is a plea for greater cooperation across the administrative boundaries of specifically the eastern Solent area. The paper is divided in the following way. 1. Highlands and Lowlands in our estimation of worth 2. The Flow of Water from Downs to Sea 3. Wetlands and Their Global Significance 4. Farmland and Fishing 5. 2011-2013: Medmerry Realignment Scheme 6. The Protection and Enhancement of Natural Capital in The Land ‘In Between’ 7. The Challenge to Species in The District’s Wildlife Corridors 8. Water Quality 9. Habitat Protection and Enhancement at the Sub-Regional Level 10. The policy restraints on the destruction of natural capital 11. -
CERTAIN INSECT VECTORS of APLANOBACTER STEWARTI ' by F
CERTAIN INSECT VECTORS OF APLANOBACTER STEWARTI ' By F. W. Poos, senior entomologist, Division of Cereal and Forage Insects, Bureau of Entomology and Plant Quarantine; and CHARLOTTE ELLIOTT, associate pa- thologist, Division of Cereal Crops and Diseases, Bureau of Plant Industry, United States Department of Agriculture ^ INTRODUCTION Bacterial wilt of corn (Zea mays L.) caused by Aplanobacter stewarti (E. F. Sm.) McC. was exceedingly destructive and more widely dis- tributed during 1932 and 1933 than during any previous time in the history of the disease. Since 1897, when it was first described by Stewart, it has been studied by a number of investigators whose work has pointed more and more toward insects as a means of dis- semination of the causal organism. Kand and Cash (7) ^ during 1920-23 found that bacterial wilt could be transmitted from diseased to healthy com plants by two species of flea beetles, Chaetocnema pulicaria Melsh. and C, denticulata (111.), and by the spotted cucum- ber beetle, Diabrotica duodecimpunctata (Fab.). IvanoíF (ö) reported transmission from diseased to healthy plants by the larval stage of the corn rootworm, Diabrotica longicornis (Say), as it attacked the roots of young seedling com plants. He also reported that the bac- teria of A. stewarti entered the corn plants through wounds made by white grubs, the larvae of Phyllophaga sp., feeding upon the roots in infested soil. A summary of this work, together with a brief review of the other literature on this disease, has recently appeared else- where (1), The results of experiments by previous investigators on soil trans- mission of the causal organism indicate that transmission through the soil to uninjured roots of com plants is exceedingly rare, if it ever occurs. -
Landslides at Beachy Head, Sussex
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Landslides at Beachy Head, Sussex Beachy Head (Figures 1 and 2) is a famous natural and historic site and tourist attraction on the south coast. The cliff top area is part of the Downland Country Park managed by Eastbourne District Council. The section of cliff surveyed at Beachy Head is situated to the east of the modern lighthouse. The survey spans a 400 m south-facing stretch of beach with a cliff height of between 120 and 160 m. Figure 1 Cliffs and lighthouse at Beachy Head Figure 2 Field sketch at Beachy Head As part of a programme of work monitoring coastal erosion and landsliding at several sites around the coast of Great Britain, BGS has surveyed the cliffs at Beachy Head in Sussex using terrestrial LiDAR — see Terrestrial LiDAR Survey Techniques Geology The geology of the cliffs at Beachy Head consist of Cretaceous chalk comprising the Seaford Chalk and Lewes Nodular Chalk formations (formerly called the Upper Chalk Formation) overlying the New Pit Chalk Formation (formerly part of the Middle Chalk). The New Pit Chalk Formation (Turonian) in the lower part of the cliff is largely obscured by chalk debris. This is principally blocky, white firm to moderately hard chalk with numerous marls. Flint occurs sporadically or in seams in different part of the formation. Overlying the New Pit Chalk Formation is the Lewes Nodular Chalk Formation, which is Turonian to Coniacian in age. This consists of hard nodular chalk and chalkstone, which is locally porcellaneous. -
View Characterisation and Analysis
South Downs National Park: View Characterisation and Analysis Final Report Prepared by LUC on behalf of the South Downs National Park Authority November 2015 Project Title: 6298 SDNP View Characterisation and Analysis Client: South Downs National Park Authority Version Date Version Details Prepared by Checked by Approved by Director V1 12/8/15 Draft report R Knight, R R Knight K Ahern Swann V2 9/9/15 Final report R Knight, R R Knight K Ahern Swann V3 4/11/15 Minor changes to final R Knight, R R Knight K Ahern report Swann South Downs National Park: View Characterisation and Analysis Final Report Prepared by LUC on behalf of the South Downs National Park Authority November 2015 Planning & EIA LUC LONDON Offices also in: Land Use Consultants Ltd Registered in England Design 43 Chalton Street London Registered number: 2549296 Landscape Planning London Bristol Registered Office: Landscape Management NW1 1JD Glasgow 43 Chalton Street Ecology T +44 (0)20 7383 5784 Edinburgh London NW1 1JD Mapping & Visualisation [email protected] FS 566056 EMS 566057 LUC uses 100% recycled paper LUC BRISTOL 12th Floor Colston Tower Colston Street Bristol BS1 4XE T +44 (0)117 929 1997 [email protected] LUC GLASGOW 37 Otago Street Glasgow G12 8JJ T +44 (0)141 334 9595 [email protected] LUC EDINBURGH 28 Stafford Street Edinburgh EH3 7BD T +44 (0)131 202 1616 [email protected] Contents 1 Introduction 1 Background to the study 1 Aims and purpose 1 Outputs and uses 1 2 View patterns, representative views and visual sensitivity 4 Introduction 4 View -
Coarse Fishing Close Season on English Rivers
Coarse fishing close season on English rivers Appendix 1 – Current coarse fish close season arrangements The close season on different waters In England, there is a coarse fish close season on all rivers, some canals and some stillwaters. This has not always been the case. In the 1990s, only around 60% of the canal network had a close season and in some regions, the close season had been dispensed with on all stillwaters. Stillwaters In 1995, following consultation, government confirmed a national byelaw which retained the coarse fish close season on rivers, streams, drains and canals, but dispensed with it on most stillwaters. The rationale was twofold: • Most stillwaters are discrete waterbodies in single ownership. Fishery owners can apply bespoke angling restrictions to protect their stocks, including non-statutory close times. • The close season had been dispensed with on many stillwaters prior to 1995 without apparent detriment to those fisheries. This presented strong evidence in favour of removing it. The close season is retained on some Sites of Special Scientific Interest (SSSIs) and the Norfolk and Suffolk Broads, as a precaution against possible damage to sensitive wildlife - see Appendix 1. This consultation is not seeking views on whether the close season should be retained on these stillwaters While most stillwater fishery managers have not re-imposed their own close season rules, some have, either adopting the same dates as apply to rivers or tailoring them to their waters' specific needs. Canals The Environment Agency commissioned a research project in 1997 to examine the evidence around the close season on canals to identify whether or not angling during the close season was detrimental to canal fisheries. -
English Nature Research Report
Maritime Natural Area: MIO. Whitstable to Geological Significance: Notable North Foreland (provisional) General geologicaVgeomorpholugicaIcharactcr: The Whitstable to North Foreland Maritime Natural Area has a varied coastline with relatively low-lying coast in thc cast rising to boulder clay and chalk cliffs towards the Isle of Thanet. Geological Htrtory: This coastline is characterised by the Cretaceous chalk of the Isle oTThanet bounded to the west by clays, silts and sands of the Lower ‘I’ertiary. Upper Cretaceous Santonian chalk (87-83 Ma) is exposed dipping gently to the west from Margatc to the eastern side of Herne Bay. Unconformably overlying the chalk is a sequence of Lower Tertiary scdiments which are exposed in I Ierne Bay; the Palaeocenc Thanet, Woolwicli and Oldhaven Formations overlain by the Eocene London Clay Formation. The Chalk was deposited by a shallow sea which covered much of Northwestern Europe towards the end of the Cretaceous. Sea lcvel fall was followed by the unconformabie deposition of Tertiary Palaeocene and Ikcene sedirnents. Dominantly marine in origin, these scdiments were deposited by a rising, but fluctuating sea, which covered much of Southeast England. Marine conditions were well established by the Eocene leading to the deposition ofthe i,ondon Clay Formation. Thc fossil fauna and flora from the Tertiary rocks indicates a gradually warming climate with sub-tropical conditions established by the Eocene. Subsequent uplilt (associated with the Alpine Orogeny) and resultant erosion removed much of the remaining Tertiary sediments, the next deposition occurring during the Pleistocene. Though not covercd by ice, the area was affectcd by periglacial erosion in a tundra-like environment during the last glaciation (Devensian). -
Bosham Life — 1 — April 2021
Bosham Life — 1 — April 2021 Bosham Life — 2 — April 2021 The Churches of Bosham HOLY TRINITY with ST NICHOLAS Holy Trinity Church, High Street, Bosham, Chichester PO18 8LS Vicar: Canon Martin Lane The Vicarage, Bosham Lane, Bosham, Chichester PO18 8HX 01243 573228 [email protected] Parish Administrator and Secretary of the PCC: Kate Cameron 01243 210242 [email protected] OfLice hours: Monday, Tuesday and Thursday, 9:30am-12:30pm For baptisms, weddings and funerals, please contact the Parish Administrator Sunday Services As we go to8:00am: press, a Holy socially Communion distanced service is being9:30am: held every Sung Sunday, Eucharist at 9:00am. The church is Commoncurrently Worshipclosed for Order private Two prayer. HoweCommonver—this Worshipmay all change!Order One Please check the church website, either to book oneWeekday or more Servicesseats for the Sunday service, or for an update on the currentHoly situation.Communion is celebrated in the Parish Church at the following times: Holy Trinity Church OfLice Holy Trinity Website ℅ The Vicarage, Bosham Lane, Webmaster: Adrian Mosley 945404 Bosham, Chichester PO18 8HX website: boshamchurch.org.uk Churchwarden email: [email protected] Laura Ritchie 574959 ‘‘‘Bosham‘Bosham LifeLife’’ magazine 2 Manor Villas, Taylors Lane, Editors: Priscilla Pendle and Mike Whittle Bosham, Chichester PO18 8QQ c/o 2 Marcuse Fields 572195 [email protected] Bosham, Chichester PO18 8NA Churchwarden website: boshamlife.co.uk Dan Lambert 576317 email: [email protected] 29