English Riviera 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). -
South Devon , but There Is a General Idea That It May Be Said to Be Within a Line from Teignmouth to Modbury, Spreading Inward in an Irregular Sort of Way
SO UT H D EVO N PAI NTED BY E H ANNAF O RD C . D ESC R IBED BY C H AS R R WE M . I . O , J . WI TH 2 4 F U LL- PAG E I LLU STRATI O NS I N C O LO U R L O N D O N ADAM AND CH ARLES BLACK 1 907 C ONTENTS I NTRO DU C TO RY TO R"UAY AND TO R B AY DARTMO U T H TEIGNMO U 'I‘ H N EWTO N A B B O T ToTNEs K INGSB RI D GE I ND E" LIST O F ILLU STRATIONS 1 S . Fore treet, Totnes F ACING 2 C . A Devonshire ottage 3 . Torquay 4 B abbacombe . , Torquay An i 5 . st s Cove , Torquay 6 C C . ompton astle 7 . Paignton 8 . Brixham Butterwalk 9 . The , Dartmouth 1 ’ 0. C Bayard s ove , Dartmouth 1 1 S . Fosse treet, Dartmouth 1 2 . Dittisham , on the Dart 1 3 . rt Kingswear, Da mouth 1 4 Shaldon , Teign mouth from 1 5 . Teignmouth and The Ness 1 6 . Dawlish 1 St ’ 7 . Leonard s Tower, Newton Abbot LI ST OF ILLUSTRATIONS Bradley Woods, Newton Abbot Berry Pomeroy Castle Salcombe Kingsbridge Salcombe Castle S Bolt Head, alcombe Brent S O U T H D E V O N INTRODU C TORY PER HAPS there is no rigorously defined region in cluded under the title of South Devon , but there is a general idea that it may be said to be within a line from Teignmouth to Modbury, spreading inward in an irregular sort of way . -
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. -
Record of Decision Lease of Land and Building Quaywest Waterpark
Record of Decision Lease of Land and Building Quaywest Waterpark, Goodrington, Paignton Decision Taker Elected Mayor on 23 January 2019 Decision That the Assistant Director of Business Services, in consultation with the Chief Executive, be authorised to grant a lease renewal of 25 years with a further option of 15 years of the land and building known as Quaywest Waterpark, Goodrington, Paignton to Lemur Waterparks Limited (Company Number 06883534) as shown in plan no. 16 145 003. Reason for the Decision It is considered the lease renewal of the land and buildings known as Quaywest Waterpark, Goodrington, Paignton to Lemur Waterparks Limited to be in the best interests of the Council and will secure the long term future of the facility. Implementation This decision will come into force and may be implemented on 31 January 2019 unless the call- in procedure is triggered (as set out in Standing Orders in relation to Overview and Scrutiny). Information Due to the ending of the non-renewable lease for the Waterpark, Goodrington in November 2016, a tender process was undertaken for the granting of a new long lease for the area of the existing Waterpark, go-kart area and Peter Pan area at Goodrington Sands, Tanners Road, Paignton. As part of the tender the bidder set out a series of investment proposals in the facility which would enhance the site and be beneficial to residents, visitors and the Council. A Record of Decision was signed and published on 19 September 2016 based on these terms. The existing operator has continued to operate the facility since this time whilst detailed discussions have been on-going to finalise and agree the exact terms of occupation. -
Devon Rigs Group Sites Table
DEVON RIGS GROUP SITES EAST DEVON DISTRICT and EAST DEVON AONB Site Name Parish Grid Ref Description File Code North Hill Broadhembury ST096063 Hillside track along Upper Greensand scarp ST00NE2 Tolcis Quarry Axminster ST280009 Quarry with section in Lower Lias mudstones and limestones ST20SE1 Hutchins Pit Widworthy ST212003 Chalk resting on Wilmington Sands ST20SW1 Sections in anomalously thick river gravels containing eolian ogical Railway Pit, Hawkchurch Hawkchurch ST326020 ST30SW1 artefacts Estuary cliffs of Exe Breccia. Best displayed section of Permian Breccia Estuary Cliffs, Lympstone Lympstone SX988837 SX98SE2 lithology in East Devon. A good exposure of the mudstone facies of the Exmouth Sandstone and Estuary Cliffs, Sowden Lympstone SX991834 SX98SE3 Mudstone which is seldom seen inland Lake Bridge Brampford Speke SX927978 Type area for Brampford Speke Sandstone SX99NW1 Quarry with Dawlish sandstone and an excellent display of sand dune Sandpit Clyst St.Mary Sowton SX975909 SX99SE1 cross bedding Anchoring Hill Road Cutting Otterton SY088860 Sunken-lane roadside cutting of Otter sandstone. SY08NE1 Exposed deflation surface marking the junction of Budleigh Salterton Uphams Plantation Bicton SY041866 SY0W1 Pebble Beds and Otter Sandstone, with ventifacts A good exposure of Otter Sandstone showing typical sedimentary Dark Lane Budleigh Salterton SY056823 SY08SE1 features as well as eolian sandstone at the base The Maer Exmouth SY008801 Exmouth Mudstone and Sandstone Formation SY08SW1 A good example of the junction between Budleigh -
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. -
Private Individuals Paignton PI1-4
Torbay Local Plan- A landscape for success: The Plan for Torbay 2012-32 and beyond Schedule of representations –Name/Organisation Order (A-Z) Consultee ID File Person / Organisation No. 417506 PI1 Adrian Gee Gee 829682 PI2 Leaf Lovejoy Lovejoy 468988 PI3 John Pouney Pouney 358268 PI4 Mr Michael Webster Webster 1 Pickhaver, David From: Adrian Gee Sent: 06 April 201 To: Planning, Strategic Subject: Draft Plan comments on Part 5 I Paignton West I Collaton St Mary Attachments: I am writing to comment upon the Draft Local Plan.doc I would like to comment upon the draft local plan. Firstly I would like to agree with the Forum's suggested changes to the plan and especially agree with their view that the number of houses likely to be needed should be predominately calculated by correlation with realistic employment forecasts for Torbay. I would agree that It would seem that the plan has over estimated the number or houses that will be needed in the plan period. I would like to point out that the draft plan shows that Torbay is still keeping firmly to it's historical strategy of calculating numbers for supplying housing for incomers to the area in preference to supplying realistic numbers of homes in Torbay solely for local and locally employed people. I would like to draw attention to 5.2.2 Paignton and Western Area and 5.2.2.1 through to 5.2.2.11 in particular paragraphs which contain references to development at Collaton St. Mary. In Paragraph 5.2.2.4 it states that 'development would be achievable towards the end of the plan period'. -
On the Geology of Tor and Babbacombe Bays, Devon
Downloaded from http://trn.lyellcollection.org/ at University of Auckland on March 22, 2015 V.—On the Geology of Tor and Babbacombe Bays, Devon. BY HENRY THOMAS DE LA BECHE, ESQ. F.G.S. P.R.S. F.L.S., &c. [Read November 16th, 1827.] THE district to be noticed in this communication enables us to trace the dis turbance of the Exeter red conglomerate, carboniferous limestone, and old red sandstone of the coasts of Tor and Babbacombe Bays, to the intrusion of trap rocks, subsequent to the formation of the Exeter red conglomerate. The following is a general sketch of the coast. There is no beach to the cliffs from near the Ness-point, at the mouth of the Teign, to Hope's Nose, the northern point of Tor Bay, with the exception of the bottom of a few coves, and the Babbacombe-sands, and their continuation the Oddicombe- sands, both misnomers, for they are shingle beaches. The cliffs plunge di rectly into the sea, and are well seen only from a boat. The coast is equally bold from Hope's Nose to Torquay, with the exception of Meadfoot-sands, which are, however, backed by a high broken hill. After passing the hill between Torquay and Tor Abbey, the coast assumes a milder character: the cliffs, where they occur, are of no great elevation; and there are extensive sands both at Paington and Goodrington, separated by Roundham Head. Further south, low cliffs intervene between Goodrington-sands and the Broad-sands. Beyond the low rocky land of Galmpton Point, the cliffs are bolder, and con tinue so to the Berry Head, being, in a few places, broken into coves, the most considerable of which is occupied by the harbour of Brixham. -
Head of Tor Bay Harbour Authority and Tor Bay Harbour Master
Head of Tor Bay Harbour Authority and Tor Bay Harbour Master Salary between £57,341 and £61,004 pa Plus a Competitive Salary Pension Scheme An exciting opportunity has arisen for someone with the right level of vision, drive and leadership to join Torbay Council and oversee the delivery of a successful and well-established municipal harbour. Tor Bay Harbour is situated on the stunning south coast of Devon and sits within the jewel that is the English Riviera. Not only is Torbay a major holiday destination as one of the UK’s premier coastal resorts, but we also have a UNESCO Global Geopark. The Tor Bay Harbour area occupies 16 square miles of open sea and has 22 miles of extraordinary coastline. It includes three enclosed harbours and provides a sheltered anchorage for shipping which has been widely used during the pandemic drawing visitors just to see the cruise ships at anchor. The Bay is also a venue for a wide range of maritime events, including various national and international championships. The right candidate will be responsible for the overall management, direction and leadership of the Harbour Authority and will need to use their expansive maritime and leadership knowledge to influence and shape the services provided. As a senior officer within the local authority, you will manage and lead the statutory harbour function of Tor Bay Harbour, as required by Torbay Council. The Harbour Authority manages the enclosed harbours of Brixham, Torquay and Paignton, who within their own right host fishing, leisure and small commercial vessels, including seasonal passenger craft. -
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. -
Update on the Effects of Covid-19 on the Delivery of Nautical Publications
I [12/21] ADMIRALTY Charts affected by the Publication List ADMIRALTY Charts ADMIRALTY Charts ADMIRALTY Publications 26 3497 NP 131 208 4654 NP 136(1) 343 4657 e-NP 136(1) 431 AUS 24 NP 136(2) 432 AUS 27 e-NP 136(2) 1175 AUS 28 1188 AUS 152 Erratum 1270 Q 6110 1274 SC 5600 e-NP 63 1275 1368 International Charts 1378 1479 INT 654 1490 INT 657 1557 INT 1466 2214 INT 1553 2230 INT 1554 2232 INT 1565 2236 INT 1724 2237 INT 1848 2238 INT 5363 2283 INT 12991 2452 3496 UPDATE ON THE EFFECTS OF COVID-19 ON THE DELIVERY OF NAUTICAL PUBLICATIONS As a result of ongoing effects of COVID-19 on distribution infrastructure around the world, for safety reasons, we took the decision a few months ago to delay the publication of any non-essential ADMIRALTY Nautical Publications until further notice. We started to ease the restrictions on the dispatch of some of our paper publications for July 2020. We are continuing this effort and following some positive feedback on successful receipts of publications, we are now in a position to confirm the publications schedule for the rest of the year. As previously, we will continue to closely monitor our distribution network capacities. We reserve ourselves the right to amend this publications schedule accordingly should significant dispatch issues start arising again. denotes chart available in the ADMIRALTY Raster Chart Service series. 1.6 I ADMIRALTY CHARTS AND PUBLICATIONS NOW PUBLISHED AND AVAILABLE NEW EDITIONS OF ADMIRALTY CHARTS AND PUBLICATIONS New Editions of ADMIRALTY Charts published 25 March 2021 Chart Title, limits and other remarks Scale Folio 2021 Catalogue page 26 International Chart Series, England - South Coast, Harbours on the South 1 22 INT 1724 Coast of Devon.