Holderness Coast: a Multi-Use Area Why Have Coastal Areas Developed?
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House Number Address Line 1 Address Line 2 Town/Area County
House Number Address Line 1 Address Line 2 Town/Area County Postcode 64 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 70 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 72 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 74 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 80 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 82 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 84 Abbey Grove Well Lane Willerby East Riding of Yorkshire HU10 6HE 1 Abbey Road Bridlington East Riding of Yorkshire YO16 4TU 2 Abbey Road Bridlington East Riding of Yorkshire YO16 4TU 3 Abbey Road Bridlington East Riding of Yorkshire YO16 4TU 4 Abbey Road Bridlington East Riding of Yorkshire YO16 4TU 1 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 3 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 5 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 7 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 9 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 11 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 13 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 15 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 17 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 19 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 21 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 23 Abbotts Way Bridlington East Riding of Yorkshire YO16 7NA 25 Abbotts Way Bridlington East Riding of Yorkshire YO16 -
Geography: Example Erosion
The Physical and Human Causes of Erosion The Holderness Coast By The British Geographer Situation The Holderness coast is located on the east coast of England and is part of the East Riding of Yorkshire; a lowland agricultural region of England that lies between the chalk hills of the Wolds and the North Sea. Figure 1 The Holderness Coast is one of Europe's fastest eroding coastlines. The average annual rate of erosion is around 2 metres per year but in some sections of the coast, rates of loss are as high as 10 metres per year. The reason for such high rates of coastal erosion can be attributed to both physical and human causes. Physical Causes The main reason for coastal erosion at Holderness is geological. The bedrock is made up of till. This material was deposited by glaciers around 12,000 years ago and is unconsolidated. It is made up of mixture of bulldozed clays and erratics, which are loose rocks of varying type. This boulder clay sits on layer of seaward sloping chalk. The geology and topography of the coastal plain and chalk hills can be seen in figure 2. Figure 2 The boulder clay with erratics can be seen in figure 3. As we can see in figures 2 and 3, the Holderness Coast is a lowland coastal plain deposited by glaciers. The boulder clay is experiencing more rapid rates of erosion compared to the chalk. An outcrop of chalk can be seen to the north and forms the headland, Flamborough Head. The section of coastline is a 60 kilometre stretch from Flamborough Head in the north to Spurn Point in the south. -
HOLDERNESS COAST FISHERY LOCAL ACTION GROUP DRAFT STRATEGY May 2011
Sustainable Seas - Better Businesses - Closer Communities HOLDERNESS COAST FISHERY LOCAL ACTION GROUP DRAFT STRATEGY May 2011 1 Contents 1. Introduction Page 3 2. A Coastal Area with a Distinctive Identity Page 4 3. The Holderness Coast Fishery Page 11 4. SWOT Analysis Page 18 5. Key Issues Affecting the Fishing Industry and its Communities Page 20 6. The Role of the FLAG Page 22 7. Development of the Strategy Page 23 8. Strategic Objective Page 24 9. Priority Themes and Programmes Page 24 10. Delivery of the Strategy Page 36 11. Measuring Success Page 41 Appendix 1 Consultation List Appendix 2 Summary of Key Projects Appendix 3 FLAG Board Members Appendix 4 Partnership Agreement Appendix 5 FLAG Co-ordinator Job Description Appendix 6 Expression of Interest Form Appendix 7 Project Application Form Appendix 8 Application Process Appendix 9 Project Selection Criteria 2 1 Introduction The Holderness Coast Fishery Local Action Group (FLAG) area covers all of the coastal parishes in the East Riding of Yorkshire from Bempton and Flamborough in the north to Easington in the south. The area encompasses the main fishing communities and resort towns of Bridlington, Hornsea and Withernsea, together with smaller landings at Flamborough, Tunstall and Easington (see map 1). The area has a coastline of over 40 miles, from the chalk cliffs of Flamborough Head, by way of the brown sea-washed cliffs of Bridlington Bay to the sand and shingle banks of Spurn Point. The FLAG area has a population of 63,761, the largest settlement and principal fishing town being Bridlington which has a population of 35,192 while the remainder of this relatively remote coastal area has a low density of population. -
Minutes of the Council Meeting 8 March 2017
Beswick Parish Council Meeting of the Council held at 7 pm on Wednesday, 8 March 2017 at Kilnwick Village Hall DRAFT MINUTES 1 Apologies for Absence: Apologies received from Cllr Plowman. Present: Parish Councillors Reid (Chair), Scaife, Feasby, Quinn, Julia Bugg (Clerk) and 2 members of the parish. 2 Declarations of pecuniary and non-pecuniary interests: None. 3 Minutes: Minutes of the meeting held on 11 January 2017 were approved as an accurate record. 4 Matters Arising from the Minutes: 4 Tuesday Club/Club for Retirees. Cllr Reid reported that attendance at the meetings on 31 January and 28 February were heartening (25 and 28 persons, respectively). At the next meeting (28 March), guest speakers Ron and Helen Chambers will be giving a presentation on Bees and Flowers. A trip to Lincoln Castle has been organised for 27 April. 4 Damage to Bench in Beswick. Cllr Scaife reported that the bench has been repaired and is now back in place. An invoice has been submitted and payment requested. Action: Clerk to inform ERYC that the repair has been carried out. Additionally, the Beswick South bus shelter guttering has been repaired and a request made for payment. 5 Proposed Storage Development at LKAB Minerals. Cllr Reid reported on correspondence with LKAB on possible contributions by LKAB to the Council for community projects. John Wallace has passed our request on to senior managers; awaiting decision. 9 Appointment of Internal Auditor. Cllr Quinn reported that Kate Johnson has once again agreed to act as IA. 10.1 Copy for Newsletter. Cllr Reid stated that, following the distribution of a draft version, the preparation was almost complete. -
Humber Estuary Coastal Authorities Group Flamborough Head to Gibraltar Point Shoreline Management Plan Non-Technical Summary
Humber Estuary Coastal Authorities Group Flamborough Head to Gibraltar Point Shoreline Management Plan Non-Technical Summary Final December 2010 Prepared for: Humber Estuary Coastal Authorities Group Humber Estuary Coastal Authorities Group Flamborough Head to Gibraltar Point Shoreline Management Plan Revision Schedule Flamborough Head to Gibraltar Point Shoreline Management Plan Non-Technical Summary December 2010 Rev Date Details Prepared by Reviewed by Approved by CD1 6 November Consultation Jonathan Short Dr John Pos David Dales 2009 draft Assistant Coastal Associate Director Engineer Laura Mitchell Engineer F1 20 December Final Laura Evans Dr John Pos David Dales 2010 Engineer Associate Director Jonathan Short Assistant Coastal Engineer Scott Wilson Scott House Alençon Link This document has been prepared in accordance with the scope of Scott Wilson's appointment with its client and is subject to the terms of that appointment. It is addressed Basingstoke to and for the sole and confidential use and reliance of Scott Wilson's client. Scott Wilson accepts no liability for any use of this document other than by its client and only for the Hampshire purposes for which it was prepared and provided. No person other than the client may RG21 7PP copy (in whole or in part) use or rely on the contents of this document, without the prior written permission of the Company Secretary of Scott Wilson Ltd. Any advice, opinions, or recommendations within this document should be read and relied upon only in the context of the document as a whole. The contents of this document do not provide legal Tel 01256 310200 or tax advice or opinion. -
1 the Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration
1 The Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration 2 of Soft Cliff Coastlines 3 4 Sally Brown1*, Max Barton1, Robert J Nicholls1 5 6 1. Faculty of Engineering and the Environment, University of Southampton, 7 University Road, Highfield, Southampton, UK. S017 1BJ. 8 9 * Sally Brown ([email protected], Telephone: +44(0)2380 594796). 10 11 Abstract: Building defences, such as groynes, on eroding soft cliff coastlines alters the 12 sediment budget, changing the shoreline configuration adjacent to defences. On the 13 down-drift side, the coastline is set-back. This is often believed to be caused by increased 14 erosion via the ‘terminal groyne effect’, resulting in rapid land loss. This paper examines 15 whether the terminal groyne effect always occurs down-drift post defence construction 16 (i.e. whether or not the retreat rate increases down-drift) through case study analysis. 17 18 Nine cases were analysed at Holderness and Christchurch Bay, England. Seven out of 19 nine sites experienced an increase in down-drift retreat rates. For the two remaining sites, 20 retreat rates remained constant after construction, probably as a sediment deficit already 21 existed prior to construction or as sediment movement was restricted further down-drift. 22 For these two sites, a set-back still evolved, leading to the erroneous perception that a 23 terminal groyne effect had developed. Additionally, seven of the nine sites developed a 24 set back up-drift of the initial groyne, leading to the defended sections of coast acting as 1 25 a hard headland, inhabiting long-shore drift. -
Coastal Erosion: Back to Nature
SEPTEMBER 2000 Online 388 Geofile Neil Punnett Coastal erosion – Back to Nature What has caused the personal disaster Figure 1: Report in The Observer, 1 December 1996 for Sue Earle, described in Figure 1? On a quiet summer’s day the British GREAT BRITAIN GETS SMALLER BY THE DAY coastline can seem a peaceful place. Waves gently lap at the foot of the At twilight the burning remains of Sue evict-and-demolish policy of East beach while children play on the sand. Earle’s clifftop farmhouse at Cowden Yorkshire Council as almost contempt Yet this is also a battle zone, a front were reflected in the tide lapping for the land. "We’re losing the very soil between the land and the sea where Mappleton Sands below. It had taken and it’s probably being washed up on tremendous energy is exerted by the 10 hours on Friday to demolish the the Dutch coast." He has researched waves attacking the coast, and where building, set fire to the broken timbers the fate of his bit of coast. He found considerable sums of money are spent and clear the site. A pall of smoke that since 1786 the distance between protecting the cliffs and beaches. drifted over the North Sea, obscuring Mappleton church and the cliff edge the flashes from a lighthouse on had been reduced by 3.5 km. In Coastal erosion is caused in several distant Flamborough Head. 1990–91 the rot stopped. ways (Figure 2). The rate of erosion largely depends upon the type of rock The £250,000 house was destroyed, "We campaigned strongly and forming the coast. -
Chronology of the American Revolution
INTRODUCTION One of the missions of The Friends of Valley Forge Park is the promotion of our historical heritage so that the spirit of what took place over two hundred years ago continues to inspire both current and future generations of all people. It is with great pleasure and satisfaction that we are able to offer to the public this chronology of events of The American Revolution. While a simple listing of facts, it is the hope that it will instill in some the desire to dig a little deeper into the fascinating stories underlying the events presented. The following pages were compiled over a three year period with text taken from many sources, including the internet, reference books, tapes and many other available resources. A bibliography of source material is listed at the end of the book. This publication is the result of the dedication, time and effort of Mr. Frank Resavy, a long time volunteer at Valley Forge National Historical Park and a member of The Friends of Valley Forge Park. As with most efforts of this magnitude, a little help from friends is invaluable. Frank and The Friends are enormously grateful for the generous support that he received from the staff and volunteers at Valley Forge National Park as well as the education committee of The Friends of Valley Forge Park. Don R Naimoli Chairman The Friends of Valley Forge Park ************** The Friends of Valley Forge Park, through and with its members, seeks to: Preserve…the past Conserve…for the future Enjoy…today Please join with us and help share in the stewardship of Valley Forge National Park. -
The Rural Economy of Holderness Medieval
!. ii' i ~ , ! The Rural Economy of Medieval i li i Holderness h i By D. J. SIDDLE HE student of the medieval landscape The plain of Holderness is the triangular is often confronted by apparently con- peninsula which forms the south-eastern ex- T flicting evidence. This fact is nowhere tremity of Yorkshire. The region is bounded better illustrated than in the plain of Holder- to the west and north by the dip slopes of the ness, one of England's smallest and most dis- Yorkshire Wolds, and to the south and east tinctive regions. The chronicler of the Cister- by the Humber estuary and the North Sea. cian monastery of Meaux (in the Hull valley), In the case of Holderness, the use of the word recording the partition of lands which fol- plain is deceptive. Within the limits of its lowed the Norman conquest, noted that the subdued relief, the region contains consider- new earle of Holderness inherited a land; able topographical variety. In the east are a "... which was exceedingly barren and in- series of arcuate moraines, extending from fertile at this time, so that it produced nothing north-east to south-east, representing various but oats. ''1 In his recent study of the Domes- stages in the glacial retreat. They often rise day material, Maxwell summarizes the Hol- to 25 ft, but are rarely above 5° ft. Much dis- derness returns in this way, "... in spite of its sected by post-glacial stream erosion, these marshy nature, Holderness was the most areas of boulder clay display little continuity, prosperous part of the East Riding in the especially in south Holderness. -
Holderness Coast (United Kingdom)
EUROSION Case Study HOLDERNESS COAST (UNITED KINGDOM) Contact: Paul SISTERMANS Odelinde NIEUWENHUIS DHV group 57 Laan 1914 nr.35, 3818 EX Amersfoort PO Box 219 3800 AE Amersfoort The Netherlands Tel: +31 (0)33 468 37 00 Fax: +31 (0)33 468 37 48 [email protected] e-mail: [email protected] 1 EUROSION Case Study 1. GENERAL DESCRIPTION OF THE AREA 1.1 Physical process level 1.1.1 Classification One of the youngest natural coastlines of England is the Holderness Coast, a 61 km long stretch of low glacial drift cliffs 3m to 35m in height. The Holderness coast stretches from Flamborough Head in the north to Spurn Head in the south. The Holderness coast mainly exists of soft glacial drift cliffs, which have been cut back up to 200 m in the last century. On the softer sediment, the crumbling cliffs are fronted by beach-mantled abrasion ramps that decline gradually to a smoothed sea floor. The Holderness coast is a macro-tidal coast, according to the scoping study the classification of the coast is: 2. Soft rock coasts High and low glacial sea cliffs 1.1.2 Geology About a million years ago the Yorkshire coastline was a line of chalk cliffs almost 32 km west of where it now is. During the Pleistocene Ice Age (18,000 years ago) deposits of glacial till (soft boulder clay) were built up against these cliffs to form the new coastline. The boulder clay consists of about 72% mud, 27% sand and 1% boulders and large Fig. -
Considering the Significance of the Yorkshire Wolds Landscape
The Post Hole Issue 33 Considering the significance of the Yorkshire Wolds landscape Dr Cath Neal1 1Department of Archaeology, University of York, The King’s Manor, York, YO1 7EP Email: [email protected] The chalk Wolds of East and North Yorkshire comprise a lightly settled rural landscape dominated by agricultural activity and they are the northernmost expanse of English chalk, forming an arc between the Humber Estuary and Flamborough Head (Figure 1). The Wolds rise steeply from the Vales to the north and west, and more gradually from the plain to the east, to a maximum height of 200m above ordnance datum, covering an area of 1350km². The area is characterised by deeply incised dry valleys and low rolling hills (Figure 2). There is a general absence of surface watercourses on the Yorkshire Wolds, with the Gypsey Race the single exception, and even this is seasonal in places. There are geological contrasts in this region, with the soft drift of Holderness, the chalk Wold ridge and the sandstones of the North Yorkshire Moors compressing a wide range of landscape diversity into a relatively small area (Roberts and Wrathmell 2000, 47). Figure 1. Distribution of chalk in England (after Stoertz 1997 ). The distinctive inverted ‘L- shape’ of the Yorkshire Wolds, results largely from the folding of the chalk that took place during the Tertiary period, and this resulted in the shallow syncline that forms the Lincolnshire and Yorkshire Wolds (Catt 1987, 13). Towards Holderness in the east, the chalk dips below substantial www.theposthole.org 13 The Post Hole Issue 33 Quaternary deposits and towards the west. -
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SYSTEMIC INSIGHTS INTO THE MANAGEMENT OF ECOSYSTEM SERVICES IN THE MARINE ENVIRONMENT Jonathan P. Atkins a, Daryl Burdon b, Mike Elliott b and Amanda J. Gregory c a Centre for Economic Policy, The Business School, University of Hull, Hull HU6 7RX, UK b Institute of Estuarine and Coastal Studies (IECS), University of Hull, Hull HU6 7RX, UK c Centre for Systems Studies, The Business School, University of Hull, Hull HU6 7RX, UK ABSTRACT This paper centres on the application of The Ecosystem Approach in the management of the marine environment, involving the identification of multi-stakeholder needs and uses of ecosystem services. The Ecosystem Approach provides ‘a strategy for the integrated management of land, water and living resources that promotes conservation and sustainable use in an equitable way’, while ecosystem services are ‘the conditions and processes through which natural ecosystems, and the species that make them up, sustain and fulfil human life’. Ever increasing and diverse use of the marine environment is leading to human-induced changes in marine-life, making necessary the development of a marine policy formation process that recognises and takes into consideration the full range of stakeholders and results in policy that addresses current, multiple, interacting uses (e.g. the EU’s Maritime Policy and Marine Strategy Framework Directive). Taking a systemic approach, incorporating an understanding of marine ecosystem structure and functioning, we identify the diversity of stakeholders and their uses of the marine environment within the framework of ecosystem services (production, regulation, cultural and over-arching support services). Informed by the DPSIR (Drivers – Pressures - State Change – Impact - Response) approach - a framework for assessing the causes, consequences and responses to change – we assess the outcomes of competing human uses and emerging pressures on the marine environment, the complexity of decision making in this area, and provide a process for informing choices in conflict resolution involving a diversity of stakeholders.