The English Riviera Global Geopark
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2020 Paignton
GUIDE 1 Welcome to the 2020 NOPS Kit Kat Tour Torbay is a large bay on Devon’s south coast. Overlooking its clear blue waters from their vantage points along the bay are three towns: Paignton, Torquay and Brixham. The bays ancient flood plain ends where it meets the steep hills of the South Hams. These hills act as suntrap, allowing the bay to luxuriate in its own warm microclimate. It is the bays golden sands and rare propensity for fine weather that has led to the bay and its seaside towns being named the English Riviera. Dartmoor National Park is a wild place with open moorlands and deep river valleys, a rich history and rare wildlife, making is a unique place and a great contrast to Torbay in terms of photographic subjects. The locations listed in the guide have been selected as popular areas to photograph. I have tried to be accurate with the postcodes but as many locations are rural, they are an approximation. They are not intended as an itinerary but as a starting point for a trigger-happy weekend. All the locations are within an hour or so drive from the hotel. Some locations are run by the National Trust or English Heritage. It would be worth being members or going with a member so that the weekend can be enjoyed to the full. Prices listed are correct at time of publication, concession prices are in brackets. Please take care and be respectful of the landscape around you. If you intend climbing or doing any other dangerous activities, please go in pairs (at least). -
Thrust Tectonics of S Devon
J. geol. Soc. London, Vol. 140, 1983, pp. 215-228, 11 figs, 1 table. Printed in Northern Ireland. Thrust tectonics of S Devon M. P. Coward & K. R. McClay SUMMARY: The tectonics of the area from Start Point to Chudleigh, SW England, are shown to be dominated by northward-verging thrust nappes. Two major thrusts are postulated. The 'Dartmouth antiform' is consideredto be a major thrust structure, nota fold structureas previously interpreted. The Torquay limestones are allochthonous and part of a klippe of a major thrust nappe with a minimum displacement of13 km northwards. A progressive and diachronous sequence of deformation has been established with deformation starting in the S and moving N. Many of the folds and cleavages are probably related to the strains developed locally in thrust tips and may have no regionalcorrelation. More intense and complex deformation is found in the S compared to the N. The diachroneity is also reflected in the K-Ar mineralages. In the S, at Start Point, southward-verging backfolding is the last significant Hercynian deformation phase folding the thrust nappes. In SW England, Hercynian orogenesis has affected the Devon we found thatthe structuralinterpretations Lower to Upper Palaeozoic rocks of Devon and Corn- indicated in previous publications and maps (e.g. wall. Much of this deformation post-dated the deposi- Lloyd 1933) were oversimplified. Further research has tion of Mid-Carboniferous Culm sediments but pre- revealed the presence of largerecumbent folds and dated the intrusion of the SW England granite bath- thrusts; it is the aim of this paperto describe the olith, which has yielded K-Ar mineral ages ranging evidence for these and discuss their significance in from 254 to 277 Ma (Dodson & Rex 1971). -
W.J. B , B.E. L and C.N. Waters
DRAFT – FOR BGS APPROVAL THE GLOBAL DEVONIAN, CARBONIFEROUS AND PERMIAN CORRELATION PROJECT: A REVIEW OF THE CONTRIBUTION FROM GREAT BRITAIN 1 2 2 3 G. WARRINGTON , W.J. BARCLAY , B.E. LEVERIDGE AND C.N. WATERS Warrington, G., Barclay, W.J., Leveridge, B.E. and Waters, C.N. 201x. The Global Devonian, Carboniferous and Permian Correlation Project: a review of the contribution from Great Britain. Geoscience in South-West England, 13, xx-xx. A contribution on the lithostratigraphy and palaeoenvironments of Devonian, Carboniferous and Permian successions onshore in Great Britain, prepared for an international project, is summarised with particular reference to south-west England. Devonian and Carboniferous successions present in that region occur in the Rhenohercynian Tectonic Zone, to the south of the Variscan Front (VF), and their complexity reflects formation in six composite basins. They differ substantially from contemporaneous successions north of the VF. Whereas Devonian successions south of the VF are largely marine, those to the north are continental. Carboniferous successions south of the VF are predominantly marine, but shallow-water and deltaic facies occur in the highest formations. North of the VF, marine conditions were superseded by paralic and continental sedimentation. Erosion, following Variscan tectonism, resulted in the Permian successions generally resting unconformably upon older Palaeozoic rocks. In south-west England a continental succession may extend, with depositional hiatuses, from the latest Carboniferous to the Late Permian and is the most complete Permian succession in Great Britain. However, the position of the Permian–Triassic boundary in the south- west, and elsewhere in the country, is not yet resolved. -
On the Geology of South Devon, with Special Reference to the Long
442 C. LAPWORTH ON THE ROOKS OF ERIBOLL DISTRIOT. Archrean, sedimentary, or intrusive materials respectively is in all probability an insoluble question. (4) Its gneisses may be either Archrean 01' (some) possibly formed by intrusion (injection of plutonic rocks) in later ages. (5) Its schists may be composed either of crushed A,·ch<.eans, crushed intrusives, or of a mixture of these with sedimentaries. (6) Its (so-called) slates may be (according to the locality, either normal slates or) crushed rocks not yet re-crystallized (and) of either Archrean, sedimentary, intrusive, or of mixed origin. ON THE GEOLOGY OF SOUTH DEVON, WITH SPECIAL REFERENOE TO THE LONG EXOURSION. By W. A. E. USSHER, F.G.S. DEVONIAN ROOKS. PLYMOUTH TYPE. TORQUAY AND TOTNES TYPE. A. Picklecombe and Staddon Grits 7. Cockington Beds-purple and grey grits and slates. 6. Berry Park Beds-bluish and dark olive slaty shales. 5. Ramsleigh Limestone. 11. Green Slates of Rame Head .., Dartmouth Slates-greenish slates. C. Lilac and grey Slates, with calc spar and ash bands local... 4. Ashprington Series (Schalstein) dia, basic rocks, and tuffs, inter. stratified with slates. D. Calcareous Shales, Plymouth Limestone ... ... ... ... 3. Stringocephalus Limestone - The Great Devon Limestone. E. Indian red and greenish Slates 2. Lower Slates-purplish and green ish slate. F. Looe Grits and Schists ... Ic, Warberry and Lincombe Hill-red grits. 1. Meadfoot grey and brownish grits and schists, To understand the Devonian Rocks of South Devon in a general way, you have to shut your eyes, as it were, to the great complexity of their relations, to ignore the many folds and flexures into which they have been thrown, and to pass over the particular difficulties which the position of this patch of limestone or that mass of shale present, unless you are prepared by slow and laborious investigation to take each complex bit of ground and un- W. -
Pembrokeshire Coast National Park Authority
Report No. 18/13 National Park Authority REPORT OF BUSINESS & PERFORMANCE MANAGER SUBJECT: INVESTIGATION INTO POTENTIAL APPLICATION FOR GEOPARK STATUS Purpose of Report To ask Members to confirm that no further action should be taken at present. Introduction/Background In 2012 the Authority approved the commissioning of an investigation into the potential economic and environmental benefits of Geopark status for some or all of the National Park. Consultants Ove Arup from Cardiff were appointed to review the benefits and problems identified by Geoparks in the UK and Europe. Summary Findings In order to obtain Geopark status, the area must not only include significant geological features, but must also promote geology through education, interpretation, events and also appoint a qualified geologist. The full report is included as an appendix, and the findings can be summarised as follows:- The quality of the geological features in Pembrokeshire would justify geopark status Although anecdotally it appears that Geopark status does have a positive impact on the local economy, this has not been proven in the few studies which have been carried out Geopark status is likely to attract only a limited number of additional visitors to the area in the short term although there is potential for additional educational visits Currently the National Park ‘brand’ is more widely recognised than geopark There is a cost to establishing, promoting and maintaining the Geopark status which depends on the amount of partnership contributions and volunteer involvement. It is likely that Geoparks will achieve UNESCO endorsement, however there is little justification in pursuing Geopark status at present, but geology should be featured more prominently in the education, interpretation and events organised by the Authority in order to prepare for a possible application in the future. -
Devon School English, Paignton, at the Heart of the English Riviera Geopark
Devon School English, Paignton, at the heart of the English Riviera Geopark. International Geoparks Pre-Conference course. Geological visits and excursions as part of the programme – notes by Nigel Heritage. Our Geopark specialist guides: Nigel Smallbones. Dip Hert Int. Retired Ranger and Manager of Berry Head NNR and SSSI for 27 years. Studied the Geology of Berry Head and Torbay. Interpreted the Geology through guided walks, displays and educational field trips. John Risdon John’s great love is the study of Devon’s heritage, namely its geology, geography and history and how all three become as one in what we call The English Riviera Geopark. John states how the greatest reward and joy he has had has been in working with people from many different walks of life and learning through them. Walking and exploration has always been a fundamental way of life in both enjoyment and learning about our wonderfully diverse world and he looks forward to being able to share his knowledge and enthusiasm for the world’s only urban geopark with you, during your stay in Torbay. Afternoon excursions week one, beginning Monday 12 September : Saltern Cove, Goodrington Sands and Waterside:- Showing Upper Devonian (Goniatite beds), Lower Devonian staddon facies of the Meadfoot Group, richly fossiliferous. Also uncomfortable contact between Lower Devonian and overlying Permian Beds. Berry Head National Nature Reserve:- A large headland of Devonian Limestone reaching a height of 60metres above sea level. Sea level changes can be observed as well as wave cut platforms on the cliffs but also with the large quarry the structure of the limestone with examples of red sandstone fissure dykes cut into the Devonian limestone and mark the first stages of the deposits in the Permo-Triassic period. -
Explore the English Riviera Global Geopark Global Riviera English the Explore
Tel: 0844 474 2233 (low cost call) cost (low 2233 474 0844 Tel: 9AP TQ5 Postcode: 882619 01803 Tel: 2JF TQ1 Postcode: 215136 01803 Tel: Tel: 01803 520022 01803 Tel: Web: www.englishriviera.co.uk/maritime Web: www.berryhead.org.uk Web: www.kents-cavern.co.uk Web: Web: www.countryside-trust.org.uk www.countryside-trust.org.uk Web: on a canoe adventure. canoe a on at the heart of Cockington Valley. Cockington of heart the at Explore the spectacular coastline coastline spectacular the Explore overnight stay in Warren Barn, Barn, Warren in stay overnight Canoe the Coves Coves the Canoe The trips can be booked with an an with booked be can trips The Rock climbing and abseiling opportunities are available. available. are opportunities abseiling and climbing Rock Shakespeare plays and ghost tours in summer. summer. in tours ghost and plays Shakespeare and group holidays. group and more inspiration. more House) and it provides a home for many rare species of wildlife. wildlife. of species rare many for home a provides it and House) attraction and host numerous events including bushcraft survival, survival, bushcraft including events numerous host and attraction to explore the Geopark coast. Geopark the explore to packages, ideal for team building trips trips building team for ideal packages, maritime website for for website maritime remains (the café and Geopark Visitor Centre are in the old Guard Guard old the in are Centre Visitor Geopark and café (the remains million years ago, the caves are a popular international visitor visitor international popular a are caves the ago, years million rush then there’s is no better way way better no is there’s then rush Trust offer some fantastic group group fantastic some offer Trust give us a call or visit our our visit or call a us give on the English Riviera. -
Field Trip Guide with Thanks to Our Sponsors: Contents
Field Trip Guide With thanks to our sponsors: Contents General Information 03 Our Geo Time Spiral 04 Introduction to the Geology of the English Riviera UNESCO Global Geopark 05 Geology Map of the English Riviera UNESCO Global Geopark 07 Field Trip Site Map 08 Field Trip Site Information 09 • Babbacombe Cliff Railway 09 • Oddicombe Beach 09 • Kents Cavern 10 • Hope’s Nose 10 • Triangle Point and Meadfoot Beach 11 • Torquay Museum 11 • Chapel Woods 12 • Torre Abbey 12 • Cockington Court and Country Park 13 • Paignton Geoplay Park 13 • Goodrington and Saltern Cove 14 • Berry Head National Nature Reserve 14 • Geopark Boat Cruises 15 Page 2 7th International Conference on UNESCO Global Geoparks | Field Trip Guide General Information Meeting point and Weather in September TOUR NUMBERS tour departure times The weather in the English Riviera in late Geopark Rocks: – T1, T2, T3, T4 All tours will depart from the Riviera September can be changeable and range from International Conference Centre. brilliant sunshine to rain, wind or low mist. Geopark Stories: – T5, T6, T7 However please note that departure Depending on where you have travelled from Overground, Underground and Cruise times for the tours differ. we are sure that some delegates will find it warm whilst others will find our temperature (Torquay Cruise): – T8, T9, T10, T11 Please check your tour departure time really quite cold. in the table below and ensure that you Overground, Underground and Cruise arrive at the conference centre at least Averages for Torbay in September: (Brixham Cruise): – T12, T13, T14, T15 20 minutes before your departure time. -
Tullypothyridina, New Late Givetian Rhynchonellid (Brachiopod) Genus
BULLETIN DE L'INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 73: 29-51, 2003 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 73: 29-51, 2003 Tullypothyridina, new late Givetian rhynchonellid (brachiopod) genus by Paul SARTENAER Sartenaer, P., 2003 - Tullypothyridina, new late Givetian rhyncho¬ name, given to a fossil by Mr. Phillips, which, from the figure nellid (brachiopod) genus. Bulletin de l'Institut royal des Sciences and description conjoined, shows with that of the Tully naturelles de Belgique, Sciences delà Terre, 73: 29-51, 1 pl., 2 textfîgs., identity 1 limestone" was table; Bruxelles-Brussel, March 31, 2003. - ISSN 0374-6291. (p. 164). Vanuxem impressed by the similarity of the specimen he figured (1842, ftg. 41 .No.l = antero-ventral, latéral and posterior views) with the one figured by Phillips (1841, pl. 34, fig. 150 = anterior view). It was an excellent Abstract observation, because Phillips's figured specimen is a good représentative of one of the various forms from South Devon A new genus, Tullypothyridina, type species T. venustula (Hall, grouped under the name "cuboides". The specimen described 1867), is described from the late Givetian of central New York, by Sowerby (1840, Pennsylvania, eastern Kentucky, and probably eastern Iowa. The type explanation of pl. 56, ftg. 24 = anterior and dorsal species of the related genus Hypothyridina Buckman, 1906, H. cu- views) shows but a faint resemblance to the one figured boides (Sowerby, 1840), the name of which was originally and sub- by Vanuxem. This is important, because Sowerby is the foun- sequently given to the American species, is discussed. -
Tor Bay Harbour Authority Port Masterplan
Tor Bay Harbour Authority Port Masterplan Fit for a Sustainable Future for the Bay and the three enclosed Harbours of Brixham, Paignton and Torquay July 2013 Tor Bay Harbour Authority Port Masterplan Client Project Manager Consultant Funder Tor Bay Harbour Authority Torbay Development Agency Royal HaskoningDHV This Port Masterplan is part- Torquay Harbour Office 3rd Floor Tor Hill House Rightwell House financed by the European Regional Beacon Quay Union Street Bretton Development Fund under the Torquay Torquay Peterborough Interreg IVA France (Channel) – TQ1 2BG TQ2 5QW PE3 8DW England 2007-2013 programme www.tor-bay-harbour.co.uk www.torbaydevelopmentagency.co.uk www.royalhaskoningdhv.com www.interreg4a-channel.eu © Copyright by Royal HaskoningDHV and TDA, July 2013 Contents Foreword 4 Consultation & Community Engagement 28 Socio-economic considerations 54 Gordon Oliver, Mayor of Torbay Tor Bay Harbour 32 Implementation and delivery 56 Executive summary 6 Significance of the harbour Fishing and commercial activities Appendices 60 Introduction 14 Transport and connectivity References Setting the scene Spatial SWOT analysis Policy background – Planning Purpose & approach of the port masterplan Planning - policy background Policy background – Transport Transport - policy background Environmental Designations Context of Tor Bay Harbour 18 Green environment Tor Bay Recreation, leisure and tourism Brixham Harbour Paignton Harbour Proposals for Tor Bay Harbour 45 Torquay Harbour Tor Bay Harbour Brixham Harbour Strategy for Tor Bay Harbour Authority 26 Paignton Harbour Torquay Harbour Tor Bay Harbour Authority Port Masterplan Tor Bay Harbour Authority 4 Port Masterplan foreword Gordon Oliver, Mayor of torbay Foreword Mayor Oliver 5 Gordon “Torbay’s coastal location has been the most influential More recently an investment of some £20m has seen a new Foreword by factor in our history and it is also an essential part of our fish landing quay, office complex, fish processing units, fish Oliver, Mayor of Torbay future. -
Tullypothyridina, New Late Givetian Rhynchonellid (Brachiopod) Genus
BULLETIN DE L’INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 73: 29-51, 2003 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 73: 29-51, 2003 Tullypothyridina, new late Givetian rhynchonellid (brachiopod) genus by Paul SARTENAER Sartenaer, P., 2003 - Tullypothyridina, new late Givetian rhyncho name, given to a fossil by Mr. Phillips, which, from the figure nellid (brachiopod) genus. Bulletin de l ’Institut royal des Sciences and description conjoined, shows identity with that of the Tully naturelles de Belgique, Sciences de la Terre. 73:29-51, 1 pl., 2 textfigs., 1 table; Bruxelles-Brussel, March 31, 2003. - ISSN 0374-6291. limestone” (p. 164). V a n u x e m was impressed by the similarity of the specimen he figured ( 1842, fig. 41 .No. 1 = antero-ventral, lateral and posterior views) with the one figured by P h i l l i p s (1841, pi. 34, fig. 150 = anterior view). It was an excellent Abstract observation, because Phillips’s figured specimen is a good representative of one of the various forms from South Devon A new genus, Tullypothyridina, type species T. venustula ( H a l l , grouped under the name “ cuboides” , The specimen described 1867), is described from the late Givetian of central New York, by S o w e r b y (1840, explanation of pi. 56, fig. 24 = anterior and Pennsylvania, eastern Kentucky, and probably eastern Iowa. The type species of the related genus Hypothyridina B u c k m a n , 1906, H. cu dorsal views) shows but a faint resemblance to the one figured boides ( S o w e r b y , 1840), the name of which was originally and sub by V a n u x e m . -
Phase I Desk Study Inglewood, Paignton, Devon
Phase I Desk Study Inglewood, Paignton, Devon WB03590 R1 Deeley Freed Estates MULTIDISCIPLINARY ENGINEERING CONSULTANTS Phase 1 Desk Study Report No. Date. WB03590 R1 2nd October 2017 Project Inglewood, Paignton, Devon Client Name Deeley Freed Estates Limited Issue Date/ Number Status Description of Amendments 12/10/16 Final - May 17 Final - 02/10/17 Final Development proposals updated Report Prepared by: Nick Edwards BSc (Hons) MSc FGS Graduate Geotechnical/Geoenvironmental Engineer Approved for Issue by: André Gilleard SiLC CSci CEnv BEng(Hons) Associate Director GeoEnvironmental Issuing Office The Cocoa House, 129 Cumberland Road, Bristol, BS1 6UY x Tel: +44 (0)117 929 2244 GF Suite, Bickleigh House, Park Five Business Centre, Exeter, EX2 7HU Tel: +44 (0)1392 369098 Unit 17.1, The Leathermarket, 11 -13 Weston Street, London, SE1 3ER Tel: +44(0)20 7939 0959 This report is provided for the benefit of the Client. We do not accept responsibility in the event that the report contents are used in whole or in part by a third party and we exercise no duty of care to any such third party. © Clarkebond (UK) Limited MULTIDISCIPLINARY ENGINEERING CONSULTANTS Phase 1 Desk Study CONTENTS EXECUTIVE SUMMARY ......................................................................................................... i 1.0 INTRODUCTION ............................................................................................................ 1 1.1 Instruction and Brief.....................................................................................................................................