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Race Instructions
Race Instructions Cowes-Torquay and Torquay-Cowes Offshore Powerboat Races 25 AND 26 AUGUST 2018 UKOPRA National Marathon Championship Races – Rounds 3 & 4 Harmsworth Trophy - Rounds 3 & 4 Organised by: British Powerboat Racing Club Ltd 83 High Street, Cowes, Isle of Wight PO31 7AJ Tel: +44 (0) 1983 290558 Email: [email protected] Contents Page No. Risk statement 3 1. Event approval 4 2. Race and licence status 4 3. Competitors’ responsibility 4 4. Organising committee, race officials and management team 4 5. Timetable and tide times 5 6. Rules and regulations 5-6 7. Race administration and registration 6 8. Pit areas, parking and special conditions 6-7 9. Pre-race scrutineering 7 10. Launching 7 11. Official practice and testing 7 12. Drivers’ briefing 7 13. Noise and speed restrictions 8 14. Departure and transit to the muster areas 8 15. Start procedure 8-9 16. Event safety cover 9 17. Trackers and electronic chart plotters 9 18. Retirement 9 19. Finishing 9-10 20. Outside assistance 10 21. Flag signals 10 22. Post-race declaration 10 23. Post-race scrutineering 10 24. Penalties 10 25. Protests 10 26. Podium presentations and prize giving 10 27. Social, Pit Passes 11 28. Trophies 11 Safety information 12 Appendix 1 : Chart showing extent of Cowes Harbour 6knot speed limit 13 Appendix 2 : Chart showing new breakwater in Cowes Harbour 14 Appendix 3 : Cowes race boat parade details 15 Appendix 4 : Cowes to Torquay race details 16-20 Appendix 5 : Torquay race boat parade details 21 Appendix 6 : Torquay to Cowes race details 22-26 Appendix 7 : Rough weather courses 27-32 2 RISK STATEMENT Powerboat Racing is by its nature a dangerous sport and therefore inherently involves an element of risk. -
Portsmouth Harbour
Information Sheet on Ramsar Wetlands (RIS) Categories approved by Recommendation 4.7 (1990), as amended by Resolution VIII.13 of the 8th Conference of the Contracting Parties (2002) and Resolutions IX.1 Annex B, IX.6, IX.21 and IX. 22 of the 9th Conference of the Contracting Parties (2005). Notes for compilers: 1. The RIS should be completed in accordance with the attached Explanatory Notes and Guidelines for completing the Information Sheet on Ramsar Wetlands. Compilers are strongly advised to read this guidance before filling in the RIS. 2. Further information and guidance in support of Ramsar site designations are provided in the Strategic Framework for the future development of the List of Wetlands of International Importance (Ramsar Wise Use Handbook 7, 2nd edition, as amended by COP9 Resolution IX.1 Annex B). A 3rd edition of the Handbook, incorporating these amendments, is in preparation and will be available in 2006. 3. Once completed, the RIS (and accompanying map(s)) should be submitted to the Ramsar Secretariat. Compilers should provide an electronic (MS Word) copy of the RIS and, where possible, digital copies of all maps. 1. Name and address of the compiler of this form: FOR OFFICE USE ONLY. DD MM YY Joint Nature Conservation Committee Monkstone House City Road Designation date Site Reference Number Peterborough Cambridgeshire PE1 1JY UK Telephone/Fax: +44 (0)1733 – 562 626 / +44 (0)1733 – 555 948 Email: [email protected] 2. Date this sheet was completed/updated: Designated: 28 February 1995 3. Country: UK (England) 4. Name of the Ramsar site: Portsmouth Harbour 5. -
A Valuation of the Chichester Harbour Provisioning Ecosystem Services Provided by Shellfish
Rpep A valuation of the Chichester Harbour Provisioning Ecosystem Services provided by shellfish Report for Sussex IFCA and the Environment Agency Title: A valuation of the Chichester Harbour Provisioning Ecosystem Services provided by shellfish Date: January 25th 2018 Authors: Chris Williams, William Davies and Jake Kuyer Client: Sussex Inshore Fisheries and Conservation Authority (SxIFCA) NEF Consulting is the consultancy arm of the leading UK think tank, New Economics Foundation. We help to put new economic ideas into practice. TheNew content Economicss of this report Foundation can be shared isfreely the within UK’s the only organisation people named-powered above as think the client tank.. However, please contact us if you would like to publish the report, or extracts from the report, on a websiteThe Foundation or in any other way.works Unless to explicitlybuild a agreed new otherwise,economy all where publishing people rights remainreally with take NEFcontrol. Consulting. NEF Consulting Limited New Economics Foundation 10 Salamanca Place London SE1 7HB www.nefconsulting.com Tel: 020 7820 6361 [icon] Contents 1. Background and context …………………………………………………………………….…4 Chichester harbour ...................................................................................................................... 5 Conservation significance and status ........................................................................................ 5 Shellfishery context ..................................................................................................................... -
Download Our 2021-22 Media Pack
formerly Scuttlebutt Europe 2021-22 1 Contents Pages 3 – 9 Seahorse Magazine 3 Why Seahorse 4 Display (Rates and Copy Dates) 5 Technical Briefing 6 Directory 7 Brokerage 8 Race Calendar 9 New Boats Enhanced Entry Page 10 “Planet Sail” On Course show Page 11 Sailing Anarchy Page 12 EuroSail News Page 13 Yacht Racing Life Page 14 Seahorse Website Graeme Beeson – Advertising Manager Tel: +44 (0)1590 671899 Email: [email protected] Skype: graemebeeson 2 Why Seahorse? Massive Authority and Influence 17,000 circulation 27% SUBS 4% APP Seahorse is written by the finest minds 14% ROW & RETAIL DIGITAL PRINT and biggest names of the performance 5,000 22% UK 28% IRC sailing world. 4,000 EUROPE 12% USA 3,000 International Exclusive Importance Political Our writers are industry pro's ahead of and Reach Recognition 2,000 journalists - ensuring Seahorse is the EUROPE A UK S UK 1,000 EUROPE U 14% RORC last word in authority and influence. ROW A A S ROW UK S ROW U 0 U ROW EUROPE IRC ORC RORC SUBS & APP 52% EUROPE (Ex UK) 27% ORC Seahorse is written assuming a high RETAIL SUBS level of sailing knowledge from it's The only sailing magazine, written Recognised by the RORC, IRC & from no national perspective, entirely ORC all of whom subscribe all readership - targetting owners and dedicated to sailboat racing. An their members and certificate afterguard on performance sailing boats. approach reflected by a completely holders to Seahorse as a benefit international reach adopt and adapt this important information into their design work. -
Solent News the Newsletter of the Solent Forum Issue 43: Winter 2017/18
Solent News The newsletter of the Solent Forum Issue 43: Winter 2017/18 Inside this issue... • Latest news from the Solent Forum • Great British Beach Clean • Microbead plastic ban • 2017 Bathing Water results • New fishing byelaws • New good practice guidance for marine aggregates • Managing marine recreational activities in Marine Protected Areas • Saltmarsh recharge at Lymington Harbour • Waders and brent goose strategy update Beneficial Use of Dredge Sediment in the Solent (BUDS) • Green Halo project launch During the course of 2017, the Solent Forum progressed Phase 1 of the ‘Beneficial Use of Environmentally friendly • Dredge Sediment in the Solent’ (BUDS) project. This showed that around one million cubic moorings workshop metres of fine sediment is typically excavated each year in the area; however, no more • The Blue Belt Programme than 0.02 percent of this (at best) is used beneficially to protect and restore its deteriorating • Solent Oyster marshes and coastline. Regeneration project update Phase 1 of the project is being undertaken by ABPmer (who have also contributed to the initiative from their own research budget) and is being overseen by a specialist technical • Southern Water tackles misconnections group. The project team have undertaken the following tasks: • The Year of the Pier • A brief introductory literature review to provide a context for the investigation and review the • Haslar Barracks challenges, identify other contemporary initiatives and describe proven case examples. development • A specific investigation into the costs and benefits of using sediment to restore habitats • Ferry travel art inspiration in order to inform discussions about the objectives of, and funding streams for, future projects. -
The International Flying Dutchman Class Book
THE INTERNATIONAL FLYING DUTCHMAN CLASS BOOK www.sailfd.org 1 2 Preface and acknowledgements for the “FLYING DUTCHMAN CLASS BOOK” by Alberto Barenghi, IFDCO President The Class Book is a basic and elegant instrument to show and testify the FD history, the Class life and all the people who have contributed to the development and the promotion of the “ultimate sailing dinghy”. Its contents show the development, charm and beauty of FD sailing; with a review of events, trophies, results and the role past champions . Included are the IFDCO Foundation Rules and its byelaws which describe how the structure of the Class operate . Moreover, 2002 was the 50th Anniversary of the FD birth: 50 years of technical deve- lopment, success and fame all over the world and of Class life is a particular event. This new edition of the Class Book is a good chance to celebrate the jubilee, to represent the FD evolution and the future prospects in the third millennium. The Class Book intends to charm and induce us to know and to be involved in the Class life. Please, let me assent to remember and to express my admiration for Conrad Gulcher: if we sail, love FD and enjoyed for more than 50 years, it is because Conrad conceived such a wonderful dinghy and realized his dream, launching FD in 1952. Conrad, looked to the future with an excellent far-sightedness, conceived a “high-perfor- mance dinghy”, which still represents a model of technologic development, fashionable 3 water-line, low minimum hull weight and performance . Conrad ‘s approach to a continuing development of FD, with regard to materials, fitting and rigging evolution, was basic for the FD success. -
The Sedimentology and Palaeoecology of the Westleton Member of the Norwich Crag Formation (Early Pleistocene) at Thorington, Suffolk, England
Geol. Mag. 136 (4), 1999, pp. 453–464. Printed in the United Kingdom © 1999 Cambridge University Press 453 The sedimentology and palaeoecology of the Westleton Member of the Norwich Crag Formation (Early Pleistocene) at Thorington, Suffolk, England A.E. RICHARDS*, P.L. GIBBARD & M. E. PETTIT *School of Geography, Kingston University, Penrhyn Road, Kingston-upon-Thames, Surrey, KT1 2EE, UK Godwin Institute of Quaternary Research, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK (Received 28 September 1998; accepted 29 March 1999) Abstract – Extensive sections in the Thorington gravel quarry complex in eastern Suffolk include the most complete record to date of sedimentary environments of the Westleton Beds Member of the Norwich Crag Formation. New palaeoecological and palaeomagnetic evidence is presented, which confirms that the Member was deposited at or near a gravelly shoreline of the Crag Sea as sea level fluctuated during a climatic ameloriation within or at the end of the Baventian/ pre-Pastonian ‘a’ Stage (Tiglian C4c Substage). 1. Introduction 2. Late Pliocene to Early Pleistocene deposits in Suffolk The gravel quarry complex at Thorington (TM 423 728) is situated 8 km west of Southwold in northern A stratigraphical table, comparing British nomencla- Suffolk (Fig. 1). This paper will present details of ture with that of the Netherlands, is given in Table 1. observations in the quarry during the period from The earliest Pleistocene deposits that occur in June 1994 to September 1997, which provide signifi- northern Suffolk are the East Anglian Crags, which cant biostratigraphical and sedimentological evidence were deposited at the margins of the southern North for depositional environments associated with the Sea Basin. -
Submerged Gravel and Peat in Southampton Water
PAPERS AND . PROCEEDINGS 263 SUBMERGED GRAVEL AND PEAT IN SOUTHAMPTON WATER. B y C . E . EVERARD, M.SC. Summary. OCK excavations and numerous bore-holes have shown that gravel and peat-beds, buried by alluvial mud, occur at D many points in Southampton Water and its tributary estuaries. A study of a large number of hitherto unpublished borings has shown that the gravel occurs as terraces, similar to those found above sea-level. There is evidence that the terraces mark stages, three in number, in the excavation of the estuaries during the Pleistocene Period, and that the peat and mud have been deposited mainly during the post-glacial rise in sea-level. Introduction. The Hampshire coast, between Hurst Castle and Hayling Island, illustrates admirably the characteristic estuarine features of a coast of submergence. It is probable that, following the post- glacial rise in sea-level, much of the Channel coast presented a similar appearance, but only in limited areas have the estuaries survived subsequent coastal erosion. The Isle of Wight has, for example, preserved from destruction the Solent and Southampton Water, and their tributary estuaries. The fluviatile origin of these estuaries has been accepted for many years, following the work of Reid (1, 2) and Shore (3, 4), among others, but, as much of the evidence is below low water- level, detailed knowledge of their stratigraphy and history is limited. The deposits of gravel, peat and mud which largely fill the estuaries are known chiefly from dock constructions, borings and dredging. The shores of Southampton Water have been the scene of much activity of this nature during the past century, and a large quantity of information has accumulated concerning the submerged deposits, but surprisingly little has been published. -
Solent Pilotage Directions
Solent Pilotage Introduction Welcome to Solent Pilotage. The Solent is one of the busiest waterways in Europe with a mix of commercial, recreational and military traffic. It is also a complex tapestry of maritime jurisdictions and responsibilities that are a result of history. The high density of mixed traffic in the Solent has implications for safety that have long been recognized by the harbour authorities in the area with the result that a number of safety management groups have been established. One recommendation from these groups has been this guide to the pilotage responsibilities and maritime jurisdictions of each Pilotage authority. It is designed to be a one-stop shop for busy mariners requiring pilotage in the Solent and to provide other mariners with an appreciation of the regulations and responsibilities of each authority. The Solent includes five main ports, four of which (ABP Southampton, Portsmouth International Port, Langstone Harbour and Cowes) are Competent Harbour Authorities (CHA) with their own pilotage directions. The fifth is the Dockyard Port of Portsmouth, controlled by the has statutory responsibilities for both the waters inside Portsmouth Harbour and for 50 square miles of the Solent1. QHM's statutory powers are extensive, including powers to close areas to non-military traffic and impose exclusion zones around vessels. Many of QHM's regulations have been issued as General Directions which A diagram showing approximate boundaries for CHAs and the Dockyard Port of Portsmouth can be found below. Summary of Pilotage Requirements In broad terms, agreement between the harbour authorities means that vessels requiring pilotage to transit between the outer reaches of the Solent and a particular port are to follow the pilotage direction for that port. -
Solent Recreation Mitigation Strategy
© Pete Durnell Solent Recreation Mitigation Strategy December 2017 Foreword by Cllr Seán Woodward - Chairman, PUSH The value of good partnerships cannot be overstated. Clear thinking, practical application and professional commitment really can change the world. The Partnership for Urban South Hampshire (PUSH) has been proud of its involvement with the Solent Recreation Mitigation Partnership (SRMP) from its very inception. True concern about protecting the coastline of the wider Solent region, backed up by valid research and a pragmatic approach to dealing with developers and the public alike has led to some ground-breaking progress, with the work of the SRMP being regarded nationally as best practice. The existence of the SRMP means that our coastline can remain evolving and vibrant, benefitting from considered and relevant development whilst also ensuring ecological needs are duly met. With a public-facing brand - Bird Aware – the SRMP has achieved unprecedented success in engaging with the wider public and is developing into a major and positive force for behaviour change. I am proud to present to you the Solent Recreation Mitigation Strategy – a document that embodies a progressive way of thinking and an opportunity to ensure our landscape is developed to meet the needs of society and our unique ecological assets. I look forward to seeing the many benefits that will arise as a result of this strategy and I invite you all to take steps to become more bird aware when visiting our beautiful coastline. 2 Contents Summary .................................................................................................................................... -
Ice-Rafted Erratics with Early Middle Pleistocene Shallow Marine
Published in Proceedings of the Geologists’ Association (2011) Possible ice-rafted erratics in late Early to early Middle Pleistocene shallow marine and coastal deposits in northeast Norfolk, UK. Nigel R. Larkina*, Jonathan R. Leeb & E. Rodger Connellc a The Natural History Department, Norfolk Museums and Archaeology Service, Shirehall, Market Avenue, Norwich, Norfolk NR1 3JQ, UK [email protected] b British Geological Survey, Keyworth, Nottingham NG12 5GG, UK [email protected] c Geography and Environment, School of Geosciences, University of Aberdeen, St Mary’s, Elphinstone Road, Aberdeen, AB24 3UF UK [email protected] *Corresponding author: email [email protected] telephone 07973 869613 Abstract Erratic clasts with a mass of up to 15 kg are described from preglacial shallow marine deposits (Wroxham Crag Formation) in northeast Norfolk. Detailed examination of their petrology has enabled them to be provenanced to northern Britain and southern Norway. Their clustered occurrence in coastal sediments in Norfolk is believed to be the product of ice-rafting from glacier incursions into the North Sea from eastern Scotland and southern Norway, and their subsequent grounding and melting within coastal areas of what is now north Norfolk. The precise timing of these restricted glaciations is difficult to determine. However, the relationship of the erratics to the biostratigraphic record and the first major expansion of ice into the North Sea suggest these events occurred during at least one glaciation between the late Early Pleistocene and early Middle Pleistocene (c. 1.1−0.6 Ma). In contrast to the late Middle (Anglian) and Late Pleistocene (Last Glacial Maximum) glaciations, where the North Sea was largely devoid of extensive marine conditions, the presence of far-travelled ice-rafted materials implies that earlier cold stage sea-levels were considerably higher. -
Caistor St Edmund Quarry Are Echinoids, Molluscs, Sponges and Other Fosssils Associated with the Chalk
CAISTOR ST. EDMUND QUARRY, NORFOLK INTRODUCTION TO CAISTOR ST. EDMUND QUARRY Thank you for enrolling on our fossil hunting event. THE GEOLOGY The large quarry at Caistor St. Edmund allows This site displays the best exposure of the Upper Cretaceous you to explore the rocks and fossils from both the (Late Campanian) Beeston Chalk, a unit not exposed in Cretaceous and later Pleistocene epochs. coastal sections, and representing some of the youngest of situchalk in Britain. The site is famous for its large flints, This quarry is mostly popular for its superb known as ‘potstones’ and ‘paramoudras’, with their echinoids, which can be found well-preserved in remarkable contained burrow systems. The Chalk here very flint from the Pleistocene gravels. Sponges and fossiliferous; of note are the specimens of the molluscs Belemnitella and Inoceramus and sea urchin Echinocorys corals can also be found in these flints, which are which it commonly yields. usually piled up and easy to pick through. At the top of the quarry are several meters of Pleistocene The Cretaceous Chalk itself yields many different gravels of the Norwich Crag Formation of Baventian age fossils from 83.6 to 72.1 million years ago, found (which ended 1.8 Mya). These contain flints, stones and by searching the chalk embankments around the sands, deposited at the front of the ice sheets further north. edge of the quarry or in the loose scree. Most Sitting directly on top of the chalk, is the Norwich Crag fossils are found by breaking the chalk boulders Basement Bed; full of flints, stones gravels and shelly apart using a geological hammer or pick.