Dorset and East Devon Coast for Inclusion in the World Heritage List
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Dorset History Centre
GB 0031 D40E Dorset History Centre This catalogue was digitised by The National Archives as part of the National Register of Archives digitisation project NRA 12726 The National Archives DORSET RECORD OFFICE H. M. C. 12726 D40E Deposited by Thos. ooornbs £ Son, Solicitors^ NATIONA L REGISTER 15th May, 1967. OF ARCHIVES (See also NRA 16221 WESLEY FAMILY PAPERS, Dorset R.O. D40 G) pfr u Bundle No. Date Description of Documents No. of nocumenti DORSET"" 1. 1798 "Report on the Coast of Dorsetshire, 1793" by Wm. Morton 1 vol. Pitt, for purpose of planning defence. Largely on pos sible landing places, present armament; suggestions as to stationing guns and troops. At back: table showing guns serviceable, unserviceable and wanting. At front: map of Dorset reduced from Isaac Taylor's 1" map and published by \i, Faden in 1796. 2. 1811 Dorset 1st ed. 1" O.S. map showing coast from Charmouth 1 to Bindon Hill. - 3. 1811 Dorset 1st ed. 1" O.S. map, sheet XV, showing Wimborne 1 and Cranborne area and part of Hampshire. BUCKLAID NEWTON 4. 1840 Copy tithe map. 1 CHARMINSTER ND 5. Extract from tithe map, used in case Lord Ilchester v. 1 Henning. DCRCHESTER 6. (Post 1834) Map , undated. (Goes with survey in Dorchester 3orough 1 records which is dated 1835 or after). Shows properties of Corporation, charities, schools. 7. - 1848 Map, surveyed 1810, corrected 1848 by F.C. Withers. 4 Indicates lands belonging to Earl of Shaftesbury, Robert Williams, the Corporation; shows parish boundaries.(2 copies). Survey showing proprietors, occupiers, descri ption of premises, remarks. -
The Dorset Heath 2013 So Once Again You Have Me As Editor
NewsletterThe ofD theo Dorsetrset Flora H eGroupath 201 4 Chairman and VC9 Recorder Robin Walls; Secretary Laurence Taylor Editorial: John Newbould It would appear that the group had no complaints about the layout and content of the Dorset Heath 2013 so once again you have me as editor. The year was somewhat difficult for me as somehow, whenever I had to leave the room in Yorkshire Naturalists’ Union committee meetings in 2011, they managed to appoint me President for 2013 resulting in extra commitments in that county. During April 2013, Dorset hosted the National Forum for Biological Recording’s annual conference at the R.N.L.I. College at Poole. What a fabulous conference venue and the overnight accommodation was excellent. NFBR then joined Dorset naturalists with a joint meeting based at Studland helping to survey for the Cyril Diver project. Once again, duties took me away as I seem to be the conference administrator. The Flora Group had an interesting year, with variable numbers at field meetings. Never-the-less some important recording has been achieved including members engaging with recording bryophytes for the first time, one meeting to record fungi near Hardy’s Cottage, which thanks to the expertise of Bryan Edwards was very successful. We also had a few members try their hand at lichen recording In June 2014, I have been tasked by the Linnean Society to organise their annual field trip, which will be in June starting with a day on Portland and Chesil on the Saturday with Ballard Down and Studland on the Sunday. -
A Critique of Phanerozoic Climatic Models Involving Changes in The
Earth-Science Reviews 56Ž. 2001 1–159 www.elsevier.comrlocaterearscirev A critique of Phanerozoic climatic models involving changes in the CO2 content of the atmosphere A.J. Boucot a,), Jane Gray b,1 a Department of Zoology, Oregon State UniÕersity, CorÕallis, OR 97331, USA b Department of Biology, UniÕersity of Oregon, Eugene, OR 97403, USA Received 28 April 1998; accepted 19 April 2001 Abstract Critical consideration of varied Phanerozoic climatic models, and comparison of them against Phanerozoic global climatic gradients revealed by a compilation of Cambrian through Miocene climatically sensitive sedimentsŽ evaporites, coals, tillites, lateritic soils, bauxites, calcretes, etc.. suggests that the previously postulated climatic models do not satisfactorily account for the geological information. Nor do many climatic conclusions based on botanical data stand up very well when examined critically. Although this account does not deal directly with global biogeographic information, another powerful source of climatic information, we have tried to incorporate such data into our thinking wherever possible, particularly in the earlier Paleozoic. In view of the excellent correlation between CO2 present in Antarctic ice cores, going back some hundreds of thousands of years, and global climatic gradient, one wonders whether or not the commonly postulated Phanerozoic connection between atmospheric CO2 and global climatic gradient is more coincidence than cause and effect. Many models have been proposed that attempt to determine atmospheric composition and global temperature through geological time, particularly for the Phanerozoic or significant portions of it. Many models assume a positive correlation between atmospheric CO2 and surface temperature, thus viewing changes in atmospheric CO2 as playing the critical role in r regulating climate temperature, but none agree on the levels of atmospheric CO2 through time. -
Hydrogeological Field Guide to the Wessex Basin
Hydrogeological Field Guide to the Wessex Basin Technical Report IR/00/77 R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds This page is blank BRITISH GEOLOGICAL SURVEY Natural Environment Research Council TECHNICAL REPORT IR/00/77 Hydrogeology Series Technical Report IR/00/77 Hydrogeological Field Guide to the Wessex Basin R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds This report was prepared for an EU BASELINE fieldtrip. Bibliographic Reference Tyler-Whittle R, Shand P, Griffiths K J and Edmunds W M, 2000 Hydrogeological Field Guide to the Wessex Basin British Geological Survey Report IR/00/77 NERC copyright 2000 British Geological Survey Keyworth, Nottinghamshire BRITISH GEOLOGICAL SURVEY BRITISH GEOLOGICAL SURVEY KEYWORTH NOTTINGHAM NG12 5GG UNITED KINGDOM TEL (0115) 9363100 FAX (0115) 9363200 DOCUMENT TITLE AND AUTHOR LIST Hydrogeological Field Guide to the Wessex Basin R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds CLIENT CLIENT REPORT # BGS REPORT# IR/00/77 CLIENT CONTRACT REF BGS PROJECT CODE CLASSIFICATION Restricted SIGNATURE DATE SIGNATURE DATE PREPARED BY CO-AUTHOR (Lead Author) CO-AUTHOR CO-AUTHOR PEER REVIEWED BY CO-AUTHOR CHECKED BY CO-AUTHOR (Project Manager or deputy) CO-AUTHOR APPROVED BY CO-AUTHOR (Project Director or senior staff) CO-AUTHOR APPROVED BY OS Copyright (Hydrogeology acknowledged Group Manager) Assistant Director Layout checked by clearance (if reqd) BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from Keyworth, Nottingham NG12 5GG the BGS Sales Desk at the Survey headquarters, ☎ 0115-936 3100 Telex 378173 BGSKEY G Keyworth, Nottingham. The more popular maps and Fax 0115-936 3200 books may be purchased from BGS-approved stockists Murchison House, West Mains Road, Edinburgh, EH9 3LA and agents and over the counter at the Bookshop, Gallery ☎ 37, Natural History Museum, Cromwell Road, (Earth 0131-667 1000 Telex 727343 SEISED G Fax 0131-668 2683 Galleries), London. -
S I D M O U T H
S I D M O U T H Newsletter September 2017 Issue 48 From the Chairman I closed my piece in the last newsletter by wishing you a great summer unfortunately that has now passed and, according to the met office, we are now officially in Autumn! One of the "hot topics" for the last newsletter was the proposed takeover of the lease of St Francis Church Hall by the Sidmouth Town Band, this has been delayed with no further developments likely until December this year. I'm confident that many organisations, apart from the U3A, hope that the layout of the hall does not change regardless of who operates the lease. It is with some sadness that I've learnt of the passing of Joy Pollock, a founder member of Sidmouth U3A. Joy along with Madge White and June Newbould were the three ladies who met at the Sidmouth Sports Centre and decided to create a steering committee to set-up a U3A branch in Sidmouth. That small seed planted in October 1993 with 15 members has blossomed into our present branch with approaching 350 members. The original membership fee was £5 per head but interestingly the attendance charge for a monthly meeting was 50p the same as it is today! The U3A which Joy helped to start was very different to the organisation we have today, however, when Joy attended the anniversary lunch in 2014 she seemed to approve of the way the branch had developed. There will be those who remember Joy and mourn the passing of one our founder members. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
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South West Coast Path : Weymouth to Lulworth Cove Walk
Saturday Walkers Club www.walkingclub.org.uk South West Coast Path : Weymouth to Lulworth Cove walk Weymouth Bay, then a dramatic cliff walk past small beaches, then higher cliffs past Durdle Door (stack) to Lulworth Cove Length 11.1 miles / 17.8 km Toughness 8 out of 10 - 2,400 feet / 730m of ascent (lots of small climbs) Features This spectacular coast walk follows the waymarked South West Coastal Path (SWCP) / England Coast Path (ECP) from Weymouth (seaside town with picturesque harbour) along its seafront promenade, then over spectacular cliffs and past secluded coves and beaches towards Durdle Door (stack) and Lulworth Cove. All, with views over Weymouth Bay and the Isle of Portland. The start is gentle - along the seafront then seawall. Then over a small hill (pub, cafe, both with sea views) to Bowleaze Cove with its spectacular art deco hotel. Then past some small beaches to the Smugglers Inn in Osmington for lunch. After lunch the cliff top path continues on past Ringstead and above Burning Cliff beach (the fire went out in in 19th C). It passes St Catherine-by- the-Sea church (nice picnic spot), and then becomes an undulating cliff edge walk (a more level inland option is available) to Durdle Door (a stack, great beach) before descending to Lulworth Cove. Return to Wool Station by bus (summer only) or taxi This walk can also be done in reverse, indeed transport considerations may may that a better option. In this case, take a bus from Wool to Lulworth Cove. At the end, continue along the coast to Weymouth's Historic Harbour area which is much nicer than the tacky seafront next to the train station https://www.walkingclub.org.uk/walk/weymouth-to-lulworth-cove/ 1/6 You hardly need a map for this walk as the SWCP is very well waymarked, and you are just following the coast, but it is useful to check your progress. -
The C-SCOPE Marine Plan (Draft)
The C-SCOPE Marine Plan (Draft) C-SCOPE Marine Spatial Plan Page 1 Contents List of Figures & Tables 3 Chapter 5: The Draft C-SCOPE Marine Plan Acknowledgements 4 5.1 Vision 67 Foreword 5 5.2 Objectives 67 The Consultation Process 6 5.3 Policy framework 68 Chapter 1: Introduction 8 • Objective 1: Healthy Marine Environment (HME) 68 Chapter 2: The international and national context for • Objective 2: Thriving Coastal Communities marine planning (TCC) 81 2.1 What is marine planning? 9 • Objective 3: Successful and Sustainable 2.2 The international policy context 9 Marine Economy (SME) 86 2.3 The national policy context 9 • Objective 4: Responsible, Equitable and 2.4 Marine planning in England 10 Safe Access (REA) 107 • Objective 5: Coastal and Climate Change Chapter 3: Development of the C-SCOPE Marine Plan Adaptation and Mitigation (CAM) 121 3.1 Purpose and status of the Marine Plan 11 • Objective 6: Strategic Significance of the 3.2 Starting points for the C-SCOPE Marine Plan 11 Marine Environment (SS) 128 3.3 Process for producing the C-SCOPE • Objective 7: Valuing, Enjoying and Marine Plan 16 Understanding (VEU) 133 • Objective 8: Using Sound Science and Chapter 4: Overview of the C-SCOPE Marine Plan Area Data (SD) 144 4.1 Site description 23 4.2 Geology 25 Chapter 6: Indicators, monitoring 4.3 Oceanography 27 and review 147 4.4 Hydrology and drainage 30 4.5 Coastal and marine ecology 32 Glossary 148 4.6 Landscape and sea scape 35 List of Appendices 151 4.7 Cultural heritage 39 Abbreviations & Acronyms 152 4.8 Current activities 45 C-SCOPE -
Autumn 2009 Free Issue No
Autumn 2009 Free Issue no. 7 no. Issue A mini version of Tower Bridge and a brontosaurus Photo-montage by Tim Heap straddling the water were two of the more tongue-in- be rustic, constructed of timber, appreciably wider with cheek suggestions put to the design team visiting passing places, extended so as to avoid the mud, and to Charmouth on September 10th. Representatives from have an arched elevation similar to the current design. Dorset Engineering Consultancy, the Coastal Ranger team, and the artists, Sans facon, met with District and Parish According to Sans facon, the artists, they do not start from Councillors, adjacent businesses and over 40 locals eager to a preconceived aesthetic: their approach consists of share their thoughts and concerns regarding the understanding a context, from its physical and social replacement footbridge over the Char river. location to the uses and functions of the place. Rather than parachute in ideas or recipes from somewhere else, they People spoke of the natural beauty of the landscape, the aim to utilise and integrate their response ideas within the importance of the geology of the area and the need for a specific quality of the location. The Velator viewing platform new structure that will sit comfortably within its rural they created in Devon (www.sansfacon.co.uk/vel/vel.html) surroundings. The general consensus was that the bridge illustrates this by drawing inspiration from and responding directly to the site and its essence. They will be working in close collaboration with the engineers and the rest of the ‘Palaeontology in Charmouth’ team to develop a joint design. -
The Ammonite Faunas of the Osmington Oolite Formation (Jurassic, Middle Oxfordian) of the Dorset Coast
G Model PGEOLA-140; No. of Pages 8 Proceedings of the Geologists’ Association xxx (2011) xxx–xxx Contents lists available at ScienceDirect Proceedings of the Geologists’ Association journal homepage: www.elsevier.com/locate/pgeola The ammonite faunas of the Osmington Oolite Formation (Jurassic, Middle Oxfordian) of the Dorset coast John K. Wright * Department of Earth Sciences, Royal Holloway, Egham Hill, Egham, Surrey TW20 0EX, United Kingdom ARTICLE INFO ABSTRACT Article history: A detailed study of the lithologies of each of the beds present in the Osmington Oolite Formation of south Received 30 June 2010 Dorset is used to allocate numerous loose-collected ammonites to their correct stratigraphic horizons. Received in revised form 16 February 2011 Much new material has been collected by the author in addition to the limited amount of material Accepted 17 February 2011 available in museum collections. The age of the faunas of the three constituent members of the Available online xxx Osmington Oolite Formation is each assessed and placed into the context of Middle Oxfordian ammonite sequences elsewhere in England and in Europe. Keywords: ß 2011 The Geologists’ Association. Published by Elsevier Ltd. All rights reserved. Stratigraphy Oxfordian stage Dorset Osmington Oolite Formation Oxfordian ammonites 1. Introduction seems incongruous. However, some of the facies present, i.e., cross- bedded oolites, are generally unsuitable for ammonite preserva- The Osmington Oolite Formation, one of the principal members tion. Other more suitable facies, -
Chesil Beach and Adjacent Area: Outline of Existing Data And
INTERNAL DOCUMENT 94 GHESIL BEA.CH AHD ADJACENT AEEA- OUTLINE OF EXISTING DATA AND SUGGESTIONS FOR FUTURE RESEARCH Report to the Dorset County Council and ¥essex Water Authority [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. INSTITUTE OF \ OCEAN a GRAPHIC SCIENCES INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey, GU8 BUB. (042-879-4141) (Director: Dr. A. 8. Laughton) Bidston Observatory, Crossway, Birkenhead, Taunton, Merseyside, L43 7RA. Somerset, TA1 2DW. (051-652-2396) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) OUTLIETE OP EXISTING MTA AND SUGGESTIONS FOR FUTURE RESEARCH Report to the Dorset CoTxnty Council and ¥essex Water Authority P GARR Internal Document No 94 Institute of Oceanographic Sciences Crossway Taunton Somerset June 198O CONTENTS Page SUMMARY 1 1. INTRODUCTION " 2 2. EXISTING PUBLISHED DATA 2 3. OTHER SOURCES OF DATA 4 3*1 Offshore 4 3.2 Wave data; computed and observed 5 3.3 Beach Sections 6 3.4 Gravel extraction 7 3.5 Tracer experiments and littoral drift 8 3.6 Additional sources 8 4. VALIDITY OF DATA 9 5. THE BEACH AS A FINITE RESOURCE 11 5.1 Introduction 11 5.2 Mechanism of replacement 11 5.3 Conclusions 12 5.4 Further research 12 6. IMPLICATIONS OF DATA ON SEA. DEFENCES, CO&ST PROTECTION 14 WORK AM) GRAVEL EXTRACTION 7. CONCLUSIONS 16 ACKNOWLEDGMENTS 19 REFERENCES TABLES APPENDICES FIGURES TABLES 1. Nature Conservancy beach sections availability* 1965-68 2. Dorset County Council " ; 1955—59 3. " " " " .. " " ; 1974-78 4.