English Riviera Geopark Management Plan Executive Summary
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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). -
South West River Basin District Flood Risk Management Plan 2015 to 2021 Habitats Regulation Assessment
South West river basin district Flood Risk Management Plan 2015 to 2021 Habitats Regulation Assessment March 2016 Executive summary The Flood Risk Management Plan (FRMP) for the South West River Basin District (RBD) provides an overview of the range of flood risks from different sources across the 9 catchments of the RBD. The RBD catchments are defined in the River Basin Management Plan (RBMP) and based on the natural configuration of bodies of water (rivers, estuaries, lakes etc.). The FRMP provides a range of objectives and programmes of measures identified to address risks from all flood sources. These are drawn from the many risk management authority plans already in place but also include a range of further strategic developments for the FRMP ‘cycle’ period of 2015 to 2021. The total numbers of measures for the South West RBD FRMP are reported under the following types of flood management action: Types of flood management measures % of RBD measures Prevention – e.g. land use policy, relocating people at risk etc. 21 % Protection – e.g. various forms of asset or property-based protection 54% Preparedness – e.g. awareness raising, forecasting and warnings 21% Recovery and review – e.g. the ‘after care’ from flood events 1% Other – any actions not able to be categorised yet 3% The purpose of the HRA is to report on the likely effects of the FRMP on the network of sites that are internationally designated for nature conservation (European sites), and the HRA has been carried out at the level of detail of the plan. Many measures do not have any expected physical effects on the ground, and have been screened out of consideration including most of the measures under the categories of Prevention, Preparedness, Recovery and Review. -
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. -
Torbay's Urban Forest
Torbay’s Urban Forest Assessing Urban Forest Effects and Values A report on the fi ndings from the UK i-Tree Eco pilot project Torbay’s Urban Forest Assessing Urban Forest Effects and Values A report on the fi ndings from the UK i-Tree Eco pilot project Published by Treeconomics First published in 2011 by Treeconomics Exeter © Treeconomics 2011 British Library Cataloguing in Publication Data A catalogue record of this book is available from the British Library ISBN 978-0-9571371-0-3 The author and publisher have made every effort to trace original copyright holders of material used in this book in order to obtain their permission. We would like to take this opportunity of making acknowledgement to any copyright holder that we may have failed to contact. Printed on FSC accredited paper Printed by Exe Valley Design and Print Ltd, Exeter ForewordForeward Few doubt the importance of trees or that they are services. By placing a value on the beneRts to intrinsically linked to our health and well-being. society of the urban forest the importance of this Nowhere is this more apparent than in our cities. resource can be made tangible to policy makers, Over half the worlds population now live in urban communities and businesses. areas and because of this the urban forest plays a crucial role in the ecology of human habitats. With better information (including economic Trees and green spaces make our towns and understanding) we can make better long term cities better places to live. decisions to maintain and improve the urban environment for the beneRt of current and future Trees Rlter pollutants from the air, provide habitat populations of Torbay. -
Neighbourhood Plan Chelston Cockington and Livermead
Neighbourhood Plan Chelston Cockington and Livermead General Our Ward is a diverse mix of largely fully developed areas in Chelston and Livermead while open countryside/parkland and rural environment in Cockington. Chelston represents a contrast between the original Victorian developments of major houses/villas/ terraces interspaced with small park areas, and other more modern housing built in the 20th century. We have two conservation areas: in Chelston it encompasses the major Victorian area; while in Cockington an original family estate of manor house (Cockington Court), five farmsteads and ancient village is now a significant visitor attraction. We also have a large part of Occombe Farm within our Ward which is an organic demonstration farm, nature trail and visitor attraction. Our Ward also includes a stretch of coastline including Hollicombe, Livermead and Corbyn Head beaches. Livermead beach includes the remnants of the original harbour for Torre Abbey that could be considered for historic protection. Development Opportunities and Planning controls There is plenty to preserve and enhance in our Ward; while little scope to offer much in significant development opportunities other than the brown-field Hollicombe gas works site opposite Hollicombe Park. It had been suggested that The ‘Old Piggeries’ green-field site adjacent to Cockington Country Park was suitable for housing we believe it is unsuitable for this use due to its impact on the adjacent important rural landscape and should be used for an expansion of community allotments as an extension to the TCC Trust’s ethos or as an asset for Cockington Country Park Ring fence Cockington Country Park and Occombe Farm from green-field housing development or encroachment by visually obtrusive new developments on its borders. -
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. -
Cockington, Chelston and Livermead Community Partnership
COCKINGTON, CHELSTON AND LIVERMEAD COMMUNITY PARTNERSHIP Description of the area The area is made up of distinct parts. Cockington and Stantor Barton retain their ancient manor house, estate village, farms and woodland. Much of Chelston is made up of Victorian villas, houses and terraces. More modern mid-20th century housing predominates in Livermead; while upper Chelston has a significant area of social or former social housing. Most of Victorian Chelston and Cockington Village are Conservation Areas. Local facilities are located in the local centres at Old Mill Road and Walnut Road, Chelston and the smaller neighbourhood centres at Queensway and Sherwell Valley Road, Chelston and Roundhill Road, Livermead. Two secondary and four primary schools also lie within the area, along with a significant number and variety of open spaces, several visitor attractions (t Cockington Country Park and Occombe Country Park), and accessible beaches at Hollicombe, Livermead and Corbyn Head. POLICIES, OPPORTUNITIES AND ACTIONS Community Support Create and develop sustainable Community Hubs in Lower Chelston/Old Mill Road area and Queensway to provide a range of community support services and activities prioritising but not limited to the vulnerable, young and older residents. Maintain effective communications and organisations to ensure the Community are kept informed and given the opportunity to influence decision making on matters affecting them. Support the development and maintenance of a range of children’s play equipment in accessible green spaces across the area. Planning and Development Maintain a diverse mix of housing with a focus on family homes by promoting small scale infill and brownfield development. Protect the Country Parks at Occombe and Cockington (including the Village) and the Stantor Barton Countryside area from new housing or other commercial developments. -
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. -
The Panorama of Torquay, a Descriptive and Historical Sketch Of
(f •••*. ( ; I o _- I ° & j^ ®; Sfc *-% (£>> '4 jk, '^i 0F>> wnt. onStont fy m)^Tm,^m$i toiEJssra's ©j^nsm^i PuilTSted^y E . C ocfcr em , Torofu.a-y. THE PANORAMA OF TORQUAY, DESCRIPTIVE AND HISTORICAL SKETCH OF THE DISTRICT COMPRISED BETWEEN THE DART AND TEIGN, BY OCTAVIAN BLEWITT. ^ecmrtr ©fctttfliu EMBELLISHED WITH A MAP, AND NUMEROUS LITHOGRAPHIC AND WOOD ENGRAVINGS. 3Utllf0tt SIMPKIN AND MARSHALL, AND COCKREM, TORQUAY. MDCCCXXXII. ; — Hie terrarura mihi prseter omnes Angulus ridet, ubi non Hymetto Mella decedunt, viridi que certat Bacca Venafro ; Ver ubi longum, tepidas que praebet Jupiter brumas. Hor. Car : Lis. 11. 6, These forms of beauty have not been to me As is a landscape in a blind man's eye But oft in lonely rooms, and mid the din Of crowds and cities, I have owed to them. In hours of weariness, sensations sweet, Felt in the blood, and felt along the heart, And passing even unto my purer mind With tranquil restoration. Wordsworth. v. entorrtr at gztztitititx!? %att. n ^ TO HENRY WOOLLCOMBE, Esq. Clje \Bvesitismt, AND TO THE OTHER MEMBERS OP THE PLYMOUTH ATHENAEUM, THIS ATTEMPT TO ILLUSTRATE ONE OP THE MOST BEAUTIFUL DISTRICTS OF £0uti) Btban, IS RESPECTFULLY INSCRIBED, WITH THE AUTHOR'S BEST WISHES FOR THE INCREASING PROSPERITY OF €f)Z Iitftttuttfftu PREFACE. In presenting to the public a new edition of this Sketch, a few words may, perhaps, be expected from me ; and I offer them the more willingly since it is my duty to acknowledge here the sources of my information. The following pages have been wholly re-written, and now contain more than ten times as much matter as the first Edition,—although that impression has been twice pirated. -
62 Bus Time Schedule & Line Route
62 bus time schedule & line map 62 Cockington View In Website Mode The 62 bus line (Cockington) has 3 routes. For regular weekdays, their operation hours are: (1) Cockington: 10:05 AM - 3:55 PM (2) Torquay: 12:00 PM (3) Torquay Harbour: 9:30 AM - 4:10 PM Use the Moovit App to ƒnd the closest 62 bus station near you and ƒnd out when is the next 62 bus arriving. Direction: Cockington 62 bus Time Schedule 11 stops Cockington Route Timetable: VIEW LINE SCHEDULE Sunday Not Operational Monday 10:05 AM - 3:55 PM Strand Harbourside, Torquay Harbour Tuesday 10:05 AM - 3:55 PM Pavilion, Torquay Torbay Road, Torquay Wednesday 10:05 AM - 3:55 PM English Riviera Centre, Torquay Thursday 10:05 AM - 3:55 PM Friday 10:05 AM - 3:55 PM Derwent Hotel Belgrave Road, Torquay Belgrave Road, Torquay Saturday Not Operational Abbey Court Hotel, Torquay Falkland Road, Torquay Torre Valley Playing Fields, Torquay 62 bus Info Direction: Cockington Walnut Road Shops, Chelston Stops: 11 Walnut Road, Paignton Trip Duration: 18 min Line Summary: Strand Harbourside, Torquay Chelston Road, Chelston Harbour, Pavilion, Torquay, English Riviera Centre, Chelston Road, Paignton Torquay, Derwent Hotel Belgrave Road, Torquay, Abbey Court Hotel, Torquay, Torre Valley Playing Hennapyn Road, Torquay Fields, Torquay, Walnut Road Shops, Chelston, Hennapyn Road, Paignton Chelston Road, Chelston, Hennapyn Road, Torquay, Cockington Village, Cockington, Cockington Court, Cockington Village, Cockington Cockington Cockington Court, Cockington Direction: Torquay 62 bus Time Schedule 24 stops Torquay Route Timetable: VIEW LINE SCHEDULE Sunday Not Operational Monday 12:00 PM Cockington Village, Cockington Tuesday 12:00 PM Cockington Court, Cockington Wednesday 12:00 PM Nut Bush Lane 73, Chelston Thursday 12:00 PM Nut Bush Lane 43, Chelston Friday 12:00 PM Nut Bush Lane, Chelston Saturday Not Operational Hamilton House, Chelston Herbert Road, Paignton St Matthew's Road, Chelston 62 bus Info Direction: Torquay St Matthew's Field, Chelston Stops: 24 Trip Duration: 26 min St.