Cheddar Gorge, Somerset
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A Wild Land Ready for Adventure the Mendip Hills
oS ExPlorEr maP oS ExPlorEr maP oS ExPlorEr maP oS ExPlorEr maP 141 141 154 153 GrId rEfErEnCE GrId rEfErEnCE GrId rEfErEnCE GrId rEfErEnCE A WILD LAND E Guid or T Visi St 476587 ST466539 St578609 St386557 POSTCODE POSTCODE POSTCODE POSTCODE READY FOR BS40 7au Car Park at tHE Bottom of BS27 3Qf Car Park at tHE Bottom BS40 8tf PICnIC and VISItor faCIlItIES, BS25 1DH kInGS Wood CAR Park BurrInGton ComBE of tHE GorGE nortH EaSt SIdE of lakE AdvENTURE BLACK DOWN & BURRINGTON HAM CHEDDAR GORGE CHEW VALLEY LAKE CROOK PEAK Courtesy of Cheddar Gorge & Caves This area is a very special part of Mendip.Open The internationally famous gorge boasts the highest Slow down and relax around this reservoir that sits in The distinctive peak that most of us see from the heathland covers Black Down, with Beacon Batch at inland limestone cliffs in the country. Incredible cave the sheltered Chew Valley. Internationally important M5 as we drive by. This is iconic Mendip limestone its highest point. Most of Black Down is a Scheduled systems take you back through human history and are for the birds that use the lake and locally loved by the countryside, with gorgeous grasslands in the summer ENTURE dv A Monument because of the archaeology from the late all part of the visitor experience. fishing community. and rugged outcrops of stone to play on when you get Stone Age to the Second World War. to the top. Travel on up the gorge and you’ll be faced with Over 4000 ducks of 12 different varieties stay on Y FOR FOR Y D REA Burrington Combe and Ham are to the north and adventure at every angle. -
Wrenna Climbing in the Mendip Hills
Climbing in the Mendip Hills AONB Introduction to the Mendips Climbing places within the AONB This is one of England’s most special places – the There are 22 climbing places within the AONB, with Cheddar limestone Mendip Hills with the lakes of the Chew Gorge being the best known. The others are: Ubley warren, Valley is a stunning landscape of steep slopes and Goblin Combe, Banwell, Knightcott rocks, North Quarry, undulating plateau punctuated by spectacular gorg- Crooks Peak, Compton Hill Cliff, Wavering Down, Sandford es and rocky outcrops. On the hilltops there are Quarry, Callow Rocks, Churchill Rocks, Doleburry Warren, hundreds of ancient monuments, whilst on steeper Burrington Combe, Deepstar Wall, The perch Quarry, Black slopes flower rich grasslands and wooded combes Rock Quarry, Pylon King’s Secret Crag, Ebbor Gorge, Split offer varied habitats for a wide variety of wildlife. Rock Quarry, and Horrington Hill Quarry For more information check out the RAD (Regional Access Database) on the BMC’s (British Mountaineering council) website. The AONB and the BMC Restrictions The BMC access rep for Cheddar Gorge can provide information and answer questions on climbing in Be aware that throughout the year there are restrictions the Gorge. on the times you can access climbing places. To make sure you are permitted to climb please check out the BMC RAD (link at bottom of the page) Conserving the AONB while you climb You always have to be careful whilst climbing. You have to be extra-careful in the AONB. Be aware of your surroundings and make sure you don’t have an impact on the wildlife, plants or animals. -
Palaeolithic and Pleistocene Sites of the Mendip, Bath and Bristol Areas
Proc. Univ. Bristol Spelacol. Soc, 19SlJ, 18(3), 367-389 PALAEOLITHIC AND PLEISTOCENE SITES OF THE MENDIP, BATH AND BRISTOL AREAS RECENT BIBLIOGRAPHY by R. W. MANSFIELD and D. T. DONOVAN Lists of references lo works on the Palaeolithic and Pleistocene of the area were published in these Proceedings in 1954 (vol. 7, no. 1) and 1964 (vol. 10, no. 2). In 1977 (vol. 14, no. 3) these were reprinted, being then out of print, by Hawkins and Tratman who added a list ai' about sixty papers which had come out between 1964 and 1977. The present contribution is an attempt to bring the earlier lists up to date. The 1954 list was intended to include all work before that date, but was very incomplete, as evidenced by the number of older works cited in the later lists, including the present one. In particular, newspaper reports had not been previously included, but are useful for sites such as the Milton Hill (near Wells) bone Fissure, as are a number of references in serials such as the annual reports of the British Association and of the Wells Natural History and Archaeological Society, which are also now noted for the first time. The largest number of new references has been generated by Gough's Cave, Cheddar, which has produced important new material as well as new studies of finds from the older excavations. The original lists covered an area from what is now the northern limit of the County of Avon lo the southern slopes of the Mendips. Hawkins and Tratman extended that area to include the Quaternary Burtle Beds which lie in the Somerset Levels to the south of the Mendips, and these are also included in the present list. -
Here Needs Conserving and Enhancing
OS EXPLORER MAP OS EXPLORER MAP OS EXPLORER MAP OS EXPLORER MAP 141 141 154 153 GRID REFERENCE GRID REFERENCE GRID REFERENCE GRID REFERENCE A WILD LAND VISITOR GUIDE VISITOR ST 476587 ST466539 ST578609 ST386557 POSTCODE POSTCODE POSTCODE POSTCODE READY FOR BS40 7AU CAR PARK AT THE BOTTOM OF BS27 3QF CAR PARK AT THE BOTTOM BS40 8TF PICNIC AND VISITOR FACILITIES, BS25 1DH KINGS WOOD CAR PARK BURRINGTON COMBE OF THE GORGE NORTH EAST SIDE OF LAKE ADVENTURE BLACK DOWN & BURRINGTON HAM CHEDDAR GORGE CHEW VALLEY LAKE CROOK PEAK Courtesy of Cheddar Gorge & Caves This area is a very special part of Mendip.Open The internationally famous gorge boasts the highest Slow down and relax around this reservoir that sits in The distinctive peak that most of us see from the heathland covers Black Down, with Beacon Batch at inland limestone cliffs in the country. Incredible cave the sheltered Chew Valley. Internationally important M5 as we drive by. This is iconic Mendip limestone its highest point. Most of Black Down is a Scheduled systems take you back through human history and are for the birds that use the lake and locally loved by the countryside, with gorgeous grasslands in the summer ADVENTURE Monument because of the archaeology from the late all part of the visitor experience. fishing community. and rugged outcrops of stone to play on when you get Stone Age to the Second World War. to the top. Travel on up the gorge and you’ll be faced with Over 4000 ducks of 12 different varieties stay on READY FOR FOR READY Burrington Combe and Ham are to the north and adventure at every angle. -
CPRS00002.Pdf
Schedule to Certificate No CPRS 00002 Issue No: 8 Hanson Quarry Products Europe Ltd Hanson House, 14 Castle Hill, Maidenhead, Berkshire SL6 4JJ Manufacturing Plants Table Plant Address Postcode Abergele Quarry Nant Du Road, St George, Abergele, Conway LL22 9BD Appledore Wharf Bidna Yard, Hubbastone Road, Appledore, Bideford, Devon EX39 1LZ Auckley Quarry Hurst Lane, Auckley, Doncaster, South Yorkshire DN9 3HQ Austerfield Quarry Highfield Lane, High Street, Austerfield, Nr Doncaster, South Yorkshire DN10 6RG Barton Quarry off Walton Lane, Barton-under- Needwood, Staffordshire DE13 8EJ Baston Quarry Baston Fen, Peterborough, Cambridgeshire PE6 9QA Batts Combe Quarry Warrens Hill, Cheddar, Somerset BS27 3LR Birch Quarry Roundbush Corner, Maldon Road, Layer Marney, Colchester, Essex CO5 9XE Bozeat Quarry Bozeat, Wellingborough, Northamptonshire NN29 7UN Brayford Quarry Brayford, Barnstaple, Devon EX32 7QD Bridgwater Wharf Dunball, Bridgwater, Somerset TA6 4EJ Smiths Concrete, Waverley Wood Farm, Weston Lane, Bubbenhall, Bubbenhall Quarry CV8 3BN Coventry, Warwickshire Builth Quarry Llanelwedd, Builth Wells, Powys LD2 3UB Bulls Lodge Quarry Generals Lane, Boreham, Chelmsford, Essex CM3 3HR Cardiff Wharf Roath Dock Road, Northside, Roath Dock, Cardiff CF10 4ED Cefn Mawr Quarry Cadpole Road, Pantybuarth, Mold, Flintshire CH7 5EA Chipping Sodbury Quarry Wickwar Road, Chipping Sodbury, Bristol. Avon BS37 6AY Coldstone Quarry Greenhow Hill, Pateley Bridge, Harrogate, North Yorkshire HG4 3HT Coln Quarry Claydon Pike, Lechlade, Gloucestershire GL7 -
Somerset Geology-A Good Rock Guide
SOMERSET GEOLOGY-A GOOD ROCK GUIDE Hugh Prudden The great unconformity figured by De la Beche WELCOME TO SOMERSET Welcome to green fields, wild flower meadows, farm cider, Cheddar cheese, picturesque villages, wild moorland, peat moors, a spectacular coastline, quiet country lanes…… To which we can add a wealth of geological features. The gorge and caves at Cheddar are well-known. Further east near Frome there are Silurian volcanics, Carboniferous Limestone outcrops, Variscan thrust tectonics, Permo-Triassic conglomerates, sediment-filled fissures, a classic unconformity, Jurassic clays and limestones, Cretaceous Greensand and Chalk topped with Tertiary remnants including sarsen stones-a veritable geological park! Elsewhere in Mendip are reminders of coal and lead mining both in the field and museums. Today the Mendips are a major source of aggregates. The Mesozoic formations curve in an arc through southwest and southeast Somerset creating vales and escarpments that define the landscape and clearly have influenced the patterns of soils, land use and settlement as at Porlock. The church building stones mark the outcrops. Wilder country can be found in the Quantocks, Brendon Hills and Exmoor which are underlain by rocks of Devonian age and within which lie sunken blocks (half-grabens) containing Permo-Triassic sediments. The coastline contains exposures of Devonian sediments and tectonics west of Minehead adjoining the classic exposures of Mesozoic sediments and structural features which extend eastward to the Parrett estuary. The predominance of wave energy from the west and the large tidal range of the Bristol Channel has resulted in rapid cliff erosion and longshore drift to the east where there is a full suite of accretionary landforms: sandy beaches, storm ridges, salt marsh, and sand dunes popular with summer visitors. -
Cheddar Club Site Discover Somerset
Cheddar Club Site Discover Somerset Places to see and things to do in the local area Make the most of your time 04 Tickenham Bristol Keynsham 11 Congresbury Bath Weston-super-Mare Farmborough Blagdon 09 01 06 07 East Brent 05 03 Wedmore Oakhill Frome 02 Minehead Dunster Kilve Shepton Mallet Puriton 08 12 10 Bridgwater Glastonbury Visit 1 Cheddar Gorge 4 Clevedon Pier and Caves The only fully intact, beautifully Limestone cliffs towering 450 restored Grade 1 listed pier in the feet above the gorge, and country. underground cathedrals of stalactites and stalagmites. 5 Karting A great karting experience with 2 Wells both an indoor and outdoor England’s smallest city with a track, and all year round racing. Cathedral and impressive Bishop’s Palace in it’s medieval centre. 6 Caveclimb For caving, climbing and abseiling Wookey Hole Cave adventures. 3 A wonderful day out, with amazing caves, gardens, Victorian penny Cheddar Caves arcade, shows and lots of family attractions. Don’t forget to check your Great Saving Guide for all the latest offers on attractions throughout the UK. Great Savings Guide camc.com/greatsavingsguide Walk Cycle To walk into Cheddar, turn left at 9 Strawberry Line the site entrance and walk to the A 10 mile traffic free cycle route railway arch. Go up the steps, turn offering views over the Somerset left at the top and this footpath levels. takes you into Cheddar. There is no pavement on the main road. 10 Quantock Hills 7 Mendips Technical descents, challenging climbs and outstanding views The Mendip Hills, designated await you in the Quantock Hills. -
Mendip Hills AONB
Mendip Hills AONB 6. How successful was Starfish? It is impossible to definitively answer the question of how successful Col Turner’s decoy programme was. His own estimate, considered conservative, was 2221.13 tonnes of bombs diverted to decoys - mostly at night. This figure amounts to c. 4% of tonnage delivered by the Luftwaffe over Britain. The Bristol decoy sites were considered to have been some of the more successful, and certainly the sites at Chew Magna, Stockwood and Downside do seem to have attracted most bombs. Perhaps the Luftwaffe knew that Black Down or Four craters about 9m in diameter on some of the other Bristol sites were decoys. p Black Down photographed during 1946. Thanks to John Penny’s extensive research, we Different orientations suggest that they are have this information and extract (below) from the result of two different bombing sorties the Lufwaffe’s diary for 2/3 December, 1940: and were probably the result of payloads being emptied after bombing raids on the decoy. The craters are still visible. Trees and shrubs have grown up in them, taking advantage of the shelter they provide. Mendip Hills AONB OS MAP What remains? Explorer 141: Cheddar Gorge & t Three control bunkers that Mendip Hills West doubled as bomb shelters can Landranger 182: still be seen. They each Weston-super-Mare contained three generators to power the site. It was to one of these bunkers that the 126 tele - CONTACT phone call from RAF Radlett to 01761 462338 light or fire the site was received. [email protected] t Improved ground conditions WAR WALK during the dry spring of 2015 A new War Walk on revealed this embedded metal Black Down is available feature at Burrington c, that to download from the emulated Bristol Temple Meads Discovering Black Down Station. -
Mendip Hills AONB Survey
Mendip Hills An Archaeological Survey of the Area of Outstanding Natural Beauty by Peter Ellis ENGLISH HERITAGE Contents List of figures Introduction and Acknowledgements ...................................................1 Project Summary...................................................................................2 Table 1: New sites located during the present survey..................3 Thematic Report Introduction ................................................................................10 Hunting and Gathering...............................................................10 Ritual and Burial ........................................................................12 Settlement...................................................................................18 Farming ......................................................................................28 Mining ........................................................................................32 Communications.........................................................................36 Political Geography....................................................................37 Table 2: Round barrow groups...................................................40 Table 3: Barrow excavations......................................................40 Table 4: Cave sites with Mesolithic and later finds ...................41 A Case Study of the Wills, Waldegrave and Tudway Quilter Estates Introduction ................................................................................42 -
Journal of the Russell Society, Vol 4 No 2
JOURNAL OF THE RUSSELL SOCIETY The journal of British Isles topographical mineralogy EDITOR: George Ryba.:k. 42 Bell Road. Sitlingbourn.:. Kent ME 10 4EB. L.K. JOURNAL MANAGER: Rex Cook. '13 Halifax Road . Nelson, Lancashire BB9 OEQ , U.K. EDITORrAL BOARD: F.B. Atkins. Oxford, U. K. R.J. King, Tewkesbury. U.K. R.E. Bevins. Cardiff, U. K. A. Livingstone, Edinburgh, U.K. R.S.W. Brai thwaite. Manchester. U.K. I.R. Plimer, Parkvill.:. Australia T.F. Bridges. Ovington. U.K. R.E. Starkey, Brom,grove, U.K S.c. Chamberlain. Syracuse. U. S.A. R.F. Symes. London, U.K. N.J. Forley. Keyworth. U.K. P.A. Williams. Kingswood. Australia R.A. Howie. Matlock. U.K. B. Young. Newcastle, U.K. Aims and Scope: The lournal publishes articles and reviews by both amateur and profe,sional mineralogists dealing with all a,pecI, of mineralogy. Contributions concerning the topographical mineralogy of the British Isles arc particularly welcome. Not~s for contributors can be found at the back of the Journal. Subscription rates: The Journal is free to members of the Russell Society. Subsc ription rates for two issues tiS. Enquiries should be made to the Journal Manager at the above address. Back copies of the Journal may also be ordered through the Journal Ma nager. Advertising: Details of advertising rates may be obtained from the Journal Manager. Published by The Russell Society. Registered charity No. 803308. Copyright The Russell Society 1993 . ISSN 0263 7839 FRONT COVER: Strontianite, Strontian mines, Highland Region, Scotland. 100 mm x 55 mm. -
Final Project Report
Final Project Report 1. Contestant profile . Contestant name: Dr David Watson . Contestant occupation: Head of Field, Culture and Environment . University / Organisation Bath Spa University . E-mail: . Phone (incl. country code): . Number of people in your team: 7 2. Project overview Title: Biodiversity restoration - can drones provide an accurate, efficient and safe survey method? Contest: UK Quarry name: Batts Combe Quarry, UK Prize category: ☐ Education and Raising Awareness (select all appropriate) ☒ Habitat and Species Research ☐ Biodiversity Management ☐ Student Project ☐ Beyond Quarry Borders 1/12 Abstract Drone technology is increasingly being used for scientific research and remote sensing as part of environmental monitoring. It has a wide range of applications, for example in agriculture, coastal erosion, animal tracking and land-use. It is increasingly being used in environmental monitoring, including ecological monitoring, alongside satellite images and aerial photography. It is a developing area with applications being trialled and refined, taking advantage of the high resolution images that can be captured. This project aimed to determine the efficiency and accuracy of ecological surveys undertaken using a drone compared to conventional survey techniques in monitoring biodiversity restoration within quarries. In many quarries, large stretches of benches are inaccessible or dangerous to access for ecological surveys, making it difficult to determine the success of biodiversity restoration or the extent of natural colonisation. Batts Combe is relatively unusual in that a number of quarry benches are accessible via an access track that cuts east-west across the quarry face. Both quadrat-based survey and drone-based survey work (through image capture, processing and analysis using ImageJ and Bio7) was undertaken on accessible study areas: quarry benches and adjacent donor and receptor meadow areas to determine the utility of drones in biodiversity (restoration) monitoring. -
GEOMORPHOLOGY and HYDROLOGY of the CENTRAL MENDIPS Steady Gradient of About I in 90 to Crook Peak (628 Ft.) and with Only Slightly Less Regularity to 400 Ft
Geomorphology and Hydrology or the Central Mendips. Proc. Univ. Brist. Spe1. Soc., 1969, 12 (I), 63-74. Jubilee Contribution University ofBristol Spel.eological Society Geomorphologyand Hydrology of the Central Mendips By D. T. DONOVAN, D.Se. Only in the last few years has the Society carried out and published work on cave geomorphology and hydrology. This article attempts to relate this work to the geomorphological problems of the Mendip Hills. These will be reviewed first. The first question which must be settled is the degree to which the relief of the Palreozoic rocks is an exhumed relief dating from Triassic times, revealed by the removal ofMesozoic rocks. Some authors, perhaps in spired by Lloyd Morgan (Morgan 1888 p. 250; Morgan & Reynolds 1909, p. 24), have thought Triassic erosion an important factor in determining details ofpresent relief. While the broad reliefofnorth Somerset certainly reflects that of the late Trias, when the Coal Measures vales between the Carboniferous Limestone uplands had already been eroded to their present level or lower, I question whether the relationship holds in any detail. Some of the marginal slopes of Mendip may be little more than old Carboniferous Limestone slopes exhumed by removal of Trias, but along the southern limit of the Mendips the characteristic steep, regular marginal slope is, in fact, largely cut in the Triassic Dolomitic Conglo merate which has an exceedingly irregular contact with the Carboniferous Limestone. Similarly, the summit plateau cuts indiscriminately across Carboniferous and Triassic. All the anticlinal cores were exposed by erosion in Triassic times, but except west of Rowberrow, where the Old Red Sandstone core ofthe Blackdown anticline was already eroded down to a low level in the Trias, I conclude, with Ford and Stanton (1969) that the Triassic landscape is unimportant in controlling present relief.