141. Mendip Hills Area Profile: Supporting Documents
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Repeated Dye Traces of Underground Streams in the Mendip Hills, Somerset
47 Proc. Univ., Bristol Spelaeol. Soc, 1981. 16 (1). 47-58 REPEATED DYE TRACES OF UNDERGROUND STREAMS IN THE MENDIP HILLS. SOMERSET by W. I. STANTON and P. L. SMART ABSTRACT Three underground streams were dye traced as many as twenty-four times, at various Hows between the extremes of Hood and drought. This systematic study, the first of its kind to our knowledge, has shown that: 1. Travel time (the time between input of dye at the swallet and its first arrival at the resurgence) is inversely proportional (1:1) to mean resurgence outpul over the same period. This is characteristic of simple phreatie streams, which should be distinguishable using graphic analysis from vadose and complex phrcatic streams. 2. Rhodamine WT dye. the most stable of the common fluorescent dyes, Ls progress ively lost, to a significant and unpredictable extent, in transit from swallci to resurgence. Successful tracing therefore requires more dye at low flows than at high flows. BACKGROUND Water tracing in the Mendip caves has a long and distinguished history (Barrington and Stanton 1977, 209-213). The early experimenters, beginning at Wookey Hole Cave (ST 532.480) in 1860, used chaff, dyes or coloured powders, hoping for results visible to the naked eye. The modern phase of water tracing began in 1965 using the spores of a moss, Lycopodium clavatum, which were flushed down the swallets and caught at the resurgences in plankton nets. For the first time the tracing agent could not be detected by the unaided senses, and some attempt at quantitative analysis of results could be made (Atkinson, Drew and High 1967; Drew, Newson and Smith 1968). -
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. -
Wales Regional Geology RWM | Wales Regional Geology
Wales regional geology RWM | Wales Regional Geology Contents 1 Introduction Subregions Wales: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks Older sedimentary rocks 3 Basement rocks Rock structure 4 Groundwater 5 Resources 6 Natural processes Further information 7 - 21 Figures 22 - 24 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Wales Regional Geology Introduction This region comprises Wales and includes the adjacent inshore area which extends to 20km from the coast. Subregions To present the conclusions of our work in a concise and accessible way, we have divided Wales into 6 subregions (see Figure 1 below). We have selected subregions with broadly similar geological attributes relevant to the safety of a GDF, although there is still considerable variability in each subregion. The boundaries between subregions may locally coincide with the extent of a particular Rock Type of Interest, or may correspond to discrete features such as faults. -
St Laurence Bronze Assessed Joining Instructions
St Laurence Bronze Assessed Expedition 18th and 19th June 2021 Joining Instructions for Parents and Participants Please read these carefully to ensure we get everyone to the right place at the right time with the right kit The weekend will be run as far as is possible to replicate a DofE Bronze assessed expedition without the camping element. Participants will still be expected to carry full expedition kit, please see kit list for advice on the following. On both days groups will walk independently of an instructor but under distance supervision, times for pick up are assumed, we are assuming groups will stick to the times they have planned, navigate without mistakes and cover ground at the assumed rate. Kit to carry and wear • Boots that must cover the ankle bone with good walking socks. • Walking ( preferably non cotton ) clothing to wear and a full change in a waterproof bag to carry inside the rucksack. No shorts ( ticks are bad in the Mendips ), no strappy tops, proper sports leggings are acceptable but walking trousers are preferable. • Sleeping bag ( In a compression sack and waterproof bag ) and roll mat • Waterproof Jacket and Trousers ( No matter what the forecast ) • A Sunhat and sun cream ( no exceptions here unless on specified medical grounds ) • Full size expedition rucksack ( group kit will have to be carried ) • A substantial packed lunch, 2 Ltrs of water ( minimum ) and the ingredients to make a hot drink on the stove. Participants should also ensure they have a very good breakfast on the day before leaving the house. • Any Covid compliant equipment as specified by the school but certainly all participants should bring an appropriate mask and a small bottle of hand sanitizer. -
Part of Claverton Down SNCI) (Part of Rush Hill & Eastover Coppice SNCI) Areas Adjacent to Kennet and Avon Canal Ash Brake
SNCI Site Name (part of Claverton Down SNCI) (part of Rush Hill & Eastover Coppice SNCI) Areas adjacent to Kennet and Avon Canal Ash Brake Ashcombe Wood Atgrove Wood and stream Avoncliff Wood Ayford Farm Babylon Brook Bannerdown, and Shockerwick and Woodleaze Woods Bath University (part) (part of Bathampton Down and Woodlands SNCI) Bathampton Down and Woodlands SNCI (part of ) Bathampton Oxbow Bathford Brook and adjacent land Bathwick Slopes (part of) (part of Bathampton Down and Woodlands SNCI) Bathwick Wood (part of Bathampton Down and Woodlands SNCI) Beach Wood Complex Beach Wood complex Beacon Hill Beechen Cliff Belle Vue Tip Bellflower Hill Bengrove Wood and adjacent fields Bitham's Wood and meadows Bitton to Bath railway track Bladdock Gutter Blagdon Lake SSSI and adjacent land Bowlditch Quarry SSSI Brake Wood Breach Hill Common Breach Wood and adjacent land Broad Mead field Broad Wood Broadhill Copse Bromley Farm mine Brown's Folly - Warleigh complex Buckley Wood, Lady Wood, and adjacent fields Burledge Common and adjacent fields Burnett Brook and woods By Brook and associated marginal habitats Cam Brook and adjacent land Cam Brook disused railway Camerton New Pit Tip Camerton Wood Carrs Wood Castle Wood Catsley Wood Charlcombe Lane field Charlcombe Valley Charlton Bottom and Queen Charlton Watercourse Charmy Down Chelscombe and Lansdown Woods SNCI Chew Valley Lake SSSI and adjacent land Chewstoke Brook Clandown Bottom Claverton Wood & Vineyard Bottoms Clay Pits Woods Cleaves Wood, adjacent woodland and fields Cleveland Walk and -
Environment Agency South West Region
ENVIRONMENT AGENCY SOUTH WEST REGION 1997 ANNUAL HYDROMETRIC REPORT Environment Agency Manley House, Kestrel Way Sowton Industrial Estate Exeter EX2 7LQ Tel 01392 444000 Fax 01392 444238 GTN 7-24-X 1000 Foreword The 1997 Hydrometric Report is the third document of its kind to be produced since the formation of the Environment Agency (South West Region) from the National Rivers Authority, Her Majesty Inspectorate of Pollution and Waste Regulation Authorities. The document is the fourth in a series of reports produced on an annua! basis when all available data for the year has been archived. The principal purpose of the report is to increase the awareness of the hydrometry within the South West Region through listing the current and historic hydrometric networks, key hydrometric staff contacts, what data is available and the reporting options available to users. If you have any comments regarding the content or format of this report then please direct these to the Regional Hydrometric Section at Exeter. A questionnaire is attached to collate your views on the annual hydrometric report. Your time in filling in the questionnaire is appreciated. ENVIRONMENT AGENCY Contents Page number 1.1 Introduction.............................. .................................................... ........-................1 1.2 Hydrometric staff contacts.................................................................................. 2 1.3 South West Region hydrometric network overview......................................3 2.1 Hydrological summary: overview -
Saints, Monks and Bishops; Cult and Authority in the Diocese of Wells (England) Before the Norman Conquest
Peregrinations: Journal of Medieval Art and Architecture Volume 3 Issue 2 63-95 2011 Saints, Monks and Bishops; cult and authority in the diocese of Wells (England) before the Norman Conquest Michael Costen University of Bristol Follow this and additional works at: https://digital.kenyon.edu/perejournal Part of the Ancient, Medieval, Renaissance and Baroque Art and Architecture Commons Recommended Citation Costen, Michael. "Saints, Monks and Bishops; cult and authority in the diocese of Wells (England) before the Norman Conquest." Peregrinations: Journal of Medieval Art and Architecture 3, 2 (2011): 63-95. https://digital.kenyon.edu/perejournal/vol3/iss2/4 This Feature Article is brought to you for free and open access by the Art History at Digital Kenyon: Research, Scholarship, and Creative Exchange. It has been accepted for inclusion in Peregrinations: Journal of Medieval Art and Architecture by an authorized editor of Digital Kenyon: Research, Scholarship, and Creative Exchange. For more information, please contact [email protected]. Costen Saints, Monks and Bishops; cult and authority in the diocese of Wells (England) before the Norman Conquest Michael Costen, University of Bristol, UK Introduction This paper is founded upon a database, assembled by the writer, of some 3300 instances of dedications to saints and of other cult objects in the Diocese of Bath and Wells. The database makes it possible to order references to an object in many ways including in terms of dedication, location, date, and possible authenticity, and it makes data available to derive some history of the object in order to assess the reliability of the information it presents. -
Mining the Mendips
Walk Mining the Mendips Discover the hidden history of a small Mendips village Black Down in winer © Andrew Gustar, Flickr (CCL) Time: 3 hours Distance: 6 miles Landscape: rural Welcome to the Mendips in Somerset. This is Location: an area of limestone escarpments and open Shipham, Somerset countryside; with rich and varied scenery, magnificent views and a fascinating history. Start: The Square, Shipham BS25 1TN Discover why the area’s curious geology made Finish: this a centre of lead and zinc mining and find Lenny’s Cafe out how the lives of villagers changed during the ‘boom and bust’ stages of Mendip’s mining Grid reference: past. ST 44416 57477 Rich resources need defending and this walk Keep an eye out for: will take you on a journey through the past Wonderful views of the Bristol Channel and its islands from an Iron Age hill fort to the remains of a fake decoy town designed to distract German bombers away from Bristol. Thank you! This walk was created by Andrew Newton, a Fellow of The Royal Geographical Society (with IBG) Every landscape has a story to tell – find out more at www.discoveringbritain.org Route and stopping points 01 Shipham Square 02 Layby on Rowberrow Lane 03 The Swan Inn, Rowberrow Lane 04 Rowberrow Church 05 Dolebury Warren Iron Age Hill Fort 06 Junction between bridleway to Burrington Combe and path to Black Down 07 Black Down 08 Starfish Control Bunker 09 Rowberrow Warren Conifer plantation 10 The Slagger’s Path 11 Gruffy Ground 12 St Leonard’s Church 13 Lenny’s Café Every landscape has a story to tell – Find out more at www.discoveringbritain.org 01 Shipham Square Welcome to the Mendips village of Shipham. -
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. -
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. -
The Weathered Carboniferous Limestone at Bullslaughter Bay, South Wales: the First Example of Ghost-Rock Recorded in the British Isles
GEOLOGICA BELGICA (2014) 17/1: 33-42 The weathered Carboniferous limestone at Bullslaughter Bay, South Wales: the first example of ghost-rock recorded in the British Isles Matt D. ROWBERRY1, Yvonne BATTIAU-QUENEY2, Peter WALSH3, Błażej Błażejowski4, Viviane BOUT-ROUMAZEILLES2, Alain TRENTESAUX2, Lenka křížová5, & Hywel GRIFFITHS6. 1 Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, V Holešovičkách 41, 18209 Prague 8, Czech Republic. E-mail: [email protected] 2 CNRS UMR 8217 Geosystems, University of Lille1, 59655 Villeneuve d’Ascq cedex, France. 3 Department of Geomorphology, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland. 4 Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland. 5 Department of Physical Geography and Geoecology, Charles University in Prague, Albertov 6, 128 43 Prague 2, Czech Republic. 6 Institute of Geography & Earth Sciences, Llandinam Building, Aberystwyth University, Ceredigion, SY23 3DB, United Kingdom. ABSTRACT: The Carboniferous Limestone at Bullslaughter Bay hosts some of the most notable examples of deep weathering in the British Isles as well as two members of an enigmatic suite of breccias known as the Gash Breccias. The weathered limestone has been investigated thoroughly in order to identify the process responsible for the weathering. In this paper it is demonstrated that the weathering is isovolumetric but the weathering profile is not characterised by a vertical gradient and its depth suggests that meteoric waters did not contribute significantly to the weathering process. The weathered limestone has lost significant amounts of calcium and parts are virtually decalcified. It is seen that the dominant primary minerals of illite and quartz have been preserved while secondary clay minerals are generally absent.