August - September 2013
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
The Stratigraphy and Archaeology of the Late-Glacial and Post
LATE-GLACIAL AND POST-GLACIAL DEPOSITS AT BREAN DOWN 67 The Stratigraphy and Archreology of the Late-Glacial and Post-Glacial Deposits at Brean Down, Somerset By A. M. ApSIMON, B.A., D. T. DONOVAN, D.Sc., AND H. TAYLOR, M.B., Ch.B. CONTENTS PAGE I. Introduction and Acknowledgements - 67-69 z. Erosion Features on the Down 69 3. Description of the Deposits - 71 Site A. The Sand Cliff - 72 Site B. The"Reindeer Rift" 88 Site C- 90 Site D- 91 Site D' - 93 Site E. The" Cemented Breccia" 93 Site F- 94 4. Interpretation of the Sections 9S S. Correlation - 99 Local Correlation 99 General Correlation 1°4 6. Pottery and Other Artefacts - 1°9 7. The Cemetery 120 8. Conclusions and ArchleOlogical Summary 122 References - 127 Appendix I: Fauna, by R.J. G. Savage 13° Appendix 11: Report on the Soil Samples, by I. W. Cornwall 132 Appendix Ill: Carbon-I4 Age Determinations of the" Solutrean Ameliora tion" I. INTRODUCTION The first writer to notice the deposits at Brean Down was the local historian, F. A. Knight, who wrote: "Against the southern side of the down ..• is a great heap of drifted sand, in which human bones are sometimes brought to light by rabbits •.. several complete skeletons have been found"; and .. in the fissures on the south side there have been found many bones and antlers of Reindeer" (Knight, 19°2, pp. 299, 308). Twenty years later Knight's daughter, Mrs. Dutton, published a pamphlet on the Down in which the deposits were again briefly mentioned, although they were referred to as . -
BRSUG Number Mineral Name Hey Index Group Hey No
BRSUG Number Mineral name Hey Index Group Hey No. Chem. Country Locality Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-37 Copper Au) 1.1 4[Cu] U.K., 17 Basset Mines, nr. Redruth, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-151 Copper Au) 1.1 4[Cu] U.K., 17 Phoenix mine, Cheese Wring, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-280 Copper Au) 1.1 4[Cu] U.K., 17 County Bridge Quarry, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and South Caradon Mine, 4 miles N of Liskeard, B-319 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-394 Copper Au) 1.1 4[Cu] U.K., 17 ? Cornwall? Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-395 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-539 Copper Au) 1.1 4[Cu] North America, U.S.A Houghton, Michigan Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-540 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-541 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, -
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. -
The Late Pleistocene Sequence at Wells, Somerset
Proc. Univ. Bristol Spelaeol. Soc, 1988, l« (2), 241-257 THE LATE PLEISTOCENE SEQUENCE AT WELLS, SOMERSET by D. T. DONOVAN ABSTRACT Late Quaternary deposits and geomorphologicai features within a radius of about 4 km of Wells, Somerset, England are reviewed. The earliest well dated occurrence is the Hippopotamus fauna from Milton Hill, assigned to the warm interglacial episode corresponding to Oxygen Isolopc Stage 5c in deep sea cores. The dissected Reward Grave! is thoughl to be older, perhaps O.I.S. 6. The Wookey Hole ravine developed during ihe early part of the lasi glaeiulion (O.I.S. 5?), the Ebbor gorge later (O.I.S. 37) The Wells and Wookey Station gravel spreads, the former with woolly rhinoceros and ?mummoth, are correlated with the maximum glacial advance of the Late Devensian. INTRODUCTION The City of Wells has in its immediate vicinity an unusually rich assortment of Late Pleistocene deposits and sites. Many of these were investigated by the late H. E. Balch, Curator of Wells Museum, and his finds are to be found in the Museum along with more casual discoveries. The present paper is an attempt to survey some of this material and its chronological significance. It is convenient to deal in some detail with the Late Pleistocene as defined by Bovven et a!. (1987, p. 299), that is, beginning at the base of Oxygen Isotope Stage 5e. Middle Pleistocene deposits of great importance are found at Westbury-sub-Mendip, only 6 km from Wells (Bishop, 1982) but at present they cannot be satisfactorily connected with the chronology of the later deposits. -
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. -
Cheddar Gorge, Somerset
Cheddar Gorge, Somerset Place To Walk Location & Access: Cheddar Gorge is located at grid reference ST 471 543 (Sat Nav – BS27 3QF) next to the village of Cheddar (population 5,700). It can be accessed via the A371 from Wells, 7 miles to the south east. There are car parks in the village, and there are two car parks within the gorge itself at ST 474 545 and ST 468 540. First Bus serves Cheddar Gorge from Weston-Super-Mare, Axbridge, Wells and Street. Key Geography: Limestone gorge, tourist honey pot, caving and other adventure sports. Description: Cheddar Gorge is the finest example of a limestone gorge in Britain, lying on the southern edge of the Mendip Hills in Somerset. It is almost three miles long, and has a maximum depth of 137 metres. There is a near-vertical cliff-face to the south, and steep, grassy slopes to the north. Contrary to popular belief, Cheddar Gorge is not a collapsed cavern – but is a gorge cut by a surface river, and since left high and dry as drainage went underground. The gorge was formed by meltwater floods during the many cold periglacial periods over the last 1.2 million years. During these Arctic episodes, the development of permafrost blocked the caves with ice and frozen mud making the limestone rock impermeable. Snowmelt floods during the brief summers were then forced to flow on the surface, carving out the gorge in the process. During the warmer interglacial periods, the water flowed underground again through the permeable limestone – leaving the gorge dry. -
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. -
Natural Natural
CLUB SITES HURN LANE & BATH CHEW VALLEY Hurn Lane’s nearest crowd-puller is a makeover for Weston’s second pier, LEFT: A view from Brean Leisure Park, which offers more than Birnbeck Pier, at Anchor Head. on top of the 30 funfair rides and other attractions, Our second site, the well-established Mendip Hills ABOVE: Bath’s including indoor and outdoor swimming Bath Chew Valley Caravan Park, joined the famous Roman pools, live shows, bars, restaurants and an Club fold recently as an Affiliated Site. baths and abbey 18-hole golf course. Further afield, Animal Hidden amid quiet lanes at the edge of Farm Adventure Park has a variety of Bishop Sutton, it is much smaller than activities for younger children. Hurn Lane. With delightful pitches – Burnham-on-Sea, a quiet Victorian increasing from 35 to 45 by the end of May resort that has seen better days, has an – set among lawns, shrubs and flower beds esplanade, the shortest leisure pier in (there’s even a pond of koi carp), it has a Britain and three lighthouses. One, real ‘garden’ feel which, along with the >> the Round Tower, reduced to half its original size and inactive since 1832, is on the esplanade, while the others, the INFORMATION TOURISM High and Low lighthouses, are at the I Bath TIC, Abbey Chambers, Abbey Church Yard, Bath BA1 NATURAL northern end of town. NATURAL 1LY. Tel 0906 711 2000 or email [email protected] The High lighthouse, 99ft tall, was Burnham-on-Sea TIC, South Esplanade, Burnham-on-Sea difficult for mariners to see at low tide, so TA8 1BU. -
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 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