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Yorkshire's Hidden Vale Area
YORKSHIRE’S HIDDEN VALE The roles of the River Derwent and the River Hertford in Landscape Action for the Eastern Vale of Pickering A report by Bowles Green Ltd and The Yorkshire Wildlife Trust With generous support from LEADER Coast, Wolds, Wetlands and Waterways (CWWW) through the East Riding and North Yorkshire Waterways Partnership; The Rural Development Programme for England/LEADER East Riding of Yorkshire 1 Acknowledgements This report would not have been possible without the generous grant from LEADER Coast, Wolds, Wetlands and Waterways (CWWW) via the East Riding and North Yorkshire Waterways Partnership. The authors would also like to thank Harriet Linfoot for her hard work in the local communities, gathering the essential information which shaped this report. Over 200 people provided responses to face to face questions or the on-line survey. Their honest engagement made this report possible and worthwhile. A large number of people commented on the draft of this report and others unselfishly allowed their works and writings to be used or quoted. To all these people, our grateful thanks. Cover photograph Flixton Brow view from the top of the escarpment across the Valley ©Tim Burkinshaw Senior Authors Yorkshire Wildlife Trust Kevin Bayes Harriet Linfoot Bowles Green Steven Green Judith Bowles 2 Contents page 1.0 Summary 5 2.0 Introduction to the document 7 3.0 Introduction to Yorkshire’s Hidden Vale 8 4.0 Background documents on Landscape and Significance 9 5.0 Programme Area 10 6.0 The Cultural and Natural Heritage of the Programme -
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. -
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. -
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. -
EYMS) Has Notified the Council of a Large Number of Changes to Local Bus Services in the East Riding Which Will Come Into Effect from Sunday 6Th May 2018
East Yorkshire Motor Services – May 2018 Changes Introduction East Yorkshire Motor Services (EYMS) has notified the Council of a large number of changes to local bus services in the East Riding which will come into effect from Sunday 6th May 2018. These include changes to a large number of commercial services, which are outside the direct control of the Council. The changes also include a number of local bus and home to school services which were funded by the Council. In this note you will find details of the replacement operators on the home to school services relinquished by EYMS and details of the replacement services and bus operators for the contracted local bus services previously provided by EYMS. The Council has also taken action to replace two commercial services the 220 and 504 cancelled by EYMS. If your local bus service is not operated by EYMS, or if it is operated by EYMS but not in the list below, then there are no planned changes. Changes to Commercial Services These changes are being introduced by East Yorkshire Motor Services from Sunday 6th May 2018 and are changes to services which are not funded by the Council. Details of the revised services can be found at www.eyms.co.uk 2 Bridlington Town Service to Avocet Way 3 Bridlington Town Service to West Hill & Hospital 4 Bridlington Town Service to New Pasture Lane 5 Bridlington Town Service to Bempton Lane 6 Bridlington Town Service to The Crayke 12/13 Bridlington to Scarborough 14 Bridlington to Flamborough 45/46 Bridlington to York** 60/60A Hull to Cottingham 61/62 Hull -
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. -
2008 Serapis Report
2008 Diver Investigations of the Suspected Serapis Site Ambodifototra, Isle Ste Marie, Madagascar Authored by: Michael C. Tuttle With Contributions by: Norine Carroll, Kelly Bumpass, Michael Krivor, and Jason Burns Presented by: April 2010 VISIT US AT WWW.SERAPISPROJECT.ORG ACKNOWLEDGEMENTS A project of this scope could not have taken place without the cooperation and hard work of numerous dedicated individuals and institutions. First and foremost are Dr. David Switzer of the Institute of New Hampshire Studies, Plymouth State University and Mrs. Amy Swete Pruett (daughter of Mr. Dick Swete). These two individuals have kept the project on a steady keel. Dr. Chantal Radimilahy of the Institute of Civilizations/Museum of Art and Archaeology of the University of Antananarivo and Prof. Jean-Aime Rakotoarisoa who have been involved with the project since 1999 are also thanked for their support. Malagasy government officials who aided the project include His Excellency Zina Andrianarivelo, Ambassador and Permanent Representative of Madagascar to the United Nations who facilitated our travel to Madagascar; Mr. Jerome Sambalis, Directeur General of the Agence Portuaire Maritime et Fluviale took time to meet and hear our concerns for Madagascar’s submerged cultural heritage. On Isle Ste Marie, Mr. le President de la Délégation Spéciale Dieu Donné Alphonse and Mme. le Chef District Marie Annick Bevazaha supported the project, as did Mr. Jacquit Vanghou and Mme. Nicol Courrissaka of the Queen Betty Cultural Center on Ilot Madame, Isle Ste Marie. The project team was made up of archaeologists who took time off to contribute their time and expertise. They were Mr. -
East Riding of Yorkshire Council and Kingston Upon Hull City Council Joint Minerals Development Plan Document Habitats Regulatio
East Riding of Yorkshire Council and Kingston upon Hull City Council Joint Minerals Development Plan Document Habitats Regulations Assessment: Stage 1 - Screening Report January 2011 East Riding of Yorkshire Council and Kingston upon Hull City Council Joint Minerals Development Plan Document Habitats Regulations Assessment: Stage 1 - Screening Report January 2011 Notice This report was produced by Atkins Limited (Atkins) for East Riding of Yorkshire Council and Kingston upon Hull City Council in response to their particular instructions. This report may not be used by any person other than East Riding of Yorkshire Council and Kingston upon Hull City Council without express permission. In any event, Atkins accepts no liability for any costs, liabilities or losses arising as a result of the use of or reliance upon the contents of this report by any person other than East Riding of Yorkshire Council and Kingston upon Hull City Council. No information provided in this report can be considered to be legal advice. 5049925.014 Contents Section Page 1. Introduction and Background 1 1.1 Background to this Assessment Report 1 1.2 Background to Habitats Regulations Assessment 1 1.3 Outline of this Review Report 2 2. Plan Details 3 2.1 Proposed Plan 3 2.2 Provisions within the Plan that Protect International Sites 3 3. Methodology 4 3.1 Determination of the International Sites included in the HRA 4 3.2 Obtaining Information on International Sites with the Potential to be Affected 4 3.3 Obtaining Information on Other Projects and Plans 6 3.4 Assessing the Impacts of the Plan 7 4. -
Flamborough Head and Bempton Cliffs SPA Seabird Monitoring Programme
Flamborough Head and Bempton Cliffs SPA Seabird Monitoring Programme 2014 Report © Chrys Mellor 2014 David Aitken, Michael Babcock, Keith Clarkson, Ruth Jeavons RSPB Bempton Cliffs, 9-11 Cliff Lane, Bempton, East Riding of Yorkshire, YO15 1JD Flamborough Head and Bempton Cliffs SPA Seabird Monitoring Programme 2014 Contents Page number 1. Summary 4 2. Introduction 7 3. Methods 10 4. Results 19 5. Discussion and conclusion 29 6. References 31 7. Acknowledgements 31 Figures Page number 1. Site designations on Flamborough Headland 7 2. Fulmar productivity plot locations 10 3. Gannet productivity plot locations 11 4. Razorbill productivity plot locations 11 5. Guillemot productivity plot locations 12 6. Kittiwake productivity plot locations 12 7. Herring Gull productivity plot locations 13 8. Razorbill study-plot locations 13 9. Guillemot study-plot locations 14 10. Kittiwake study-plot locations 14 11. Guillemot diet and provisioning plot locations 15 12. Flamborough and Bempton SPA and seabird colony boundary 16 13. Shag communal roost monitoring site at Flamborough 17 14. Flamborough Head Kittiwake tagging site 2014 18 15. Trend in Fulmar productivity 2009-2014 19 16. Trend in Gannet productivity 1986-2014 20 17. Trend in Razorbill productivity 2005-2014 20 18. Trend in Guillemot productivity 1991-2014 21 19. Trend in Kittiwake productivity 1986-2014 22 20. Trend in Herring Gull productivity 2009-2014 22 21. Guillemot diet composition results 2014 24 22. Herring Gull population trend at Flamborough and Bempton 24 23. Shag population trend at Flamborough and Bempton 25 24. Shag roost and Trektellen seawatch data for Flamborough 25 25. GPS tracking data from Kittiwakes at Flamborough and Filey 27 26. -
Download the Revolution on the High Seas (PDF)
© Warlord Games © Warlord GAMING THE AWI WITH BLACK SEAS THEME THE REVOLUTION ON THE HIGH SEAS From the outset of the American Revolution, the newly formed Congress recognised the requirement for the newly independ- ent states to have a navy. The foe they faced was the most powerful naval force on the earth at the time: the Royal Navy. By David Davies n a time of poor roads and no rail PLAYING THE REVOLUTION AT SEA transportation, river and coastal While the Americans were limited in The British likewise do not yet have transportation were key to trade. the size of their fleet, the British faced the experience they would earn in While the British did have some similar issues. They simply couldn’t the decades to come. Thus, they also supply lines from the loyalist areas be everywhere at once, and nor were do not have the ‘Drilled’ special rule Ithey controlled, they were primarily their larger ships suitable for naviga- from page 78 of the rulebook. They reliant on supplies and materials from tion up the larger rivers or for opera- should have the ‘Admiralty’ special across the Atlantic, which made them tions close in to the shore. Interdiction, rule, however. Likewise, their ships vulnerable to privateers. Colonial ef- patrol, and convoy duties were left to should be limited to sloops, brigs, forts were at first haphazard, but grow- the more manoeuvrable frigates and and frigates, as most of the time the ing experience (and help from abroad) smaller unrated vessels. Americans would outrun the larger allowed the Americans to 'redirect' ships of the line (USS Randolf vs HMS much-needed supplies to their hands. -
John Paul Jones and the Curse of Home. Philological Quarterly, 99(1), Pp
Mckeever, G. (2020) John Paul Jones and the curse of home. Philological Quarterly, 99(1), pp. 95-117. This is the author’s final accepted version. There may be differences between this version and the published version. You are advised to consult the publisher’s version if you wish to cite from it. http://eprints.gla.ac.uk/184557/ Deposited on: 03 October 2020 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk John Paul Jones and the Curse of Home There were at least two versions of a chapbook titled History of Paul Jones, the Pirate circulating in nineteenth-century Britain, part of a body of literature on this sea captain, an international sensation and source of domestic mythology even before his death in Paris in 1792.1 John Paul, or Paul Jones as he became known, was as these chapbooks tell it, “of a wild and ardent disposition,” well-suited to “a sea-faring life.” “Prompted partly by a spirit of revenge, and partly by the prospect of plunder,” Jones would eventually “desert his national standard” and, using “his complete knowledge of the northern coasts of Great Britain,” mount a series of “marauding schemes” on behalf of the Revolutionary United States. Returning to his “native place” in April 1778, not only did Jones attack the town of Whitehaven on the English side of the Solway, where he had trained as a young mariner, but he also made a “warlike” appearance at St. Mary’s Isle in Kirkcudbrightshire, looking to take the Earl of Selkirk hostage.