Additional Information to Support an Environmental Impact Assessment
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Guided Walks and Events Programme Winter 2012-13
Cymdeithas Parc Bannau Brycheiniog Brecon Beacons Park Society www.breconbeaconsparksociety.org GUIDED WALKS AND EVENTS PROGRAMME WINTER 2012-13 Most of these walks go into the hills. Participants are reminded that the following gear must be taken. Walking boots, rucksack, hats, gloves, warm clothing (not jeans), spare sweater, water and a hot drink, lunch, extra food and of course waterproof jackets and trousers. A whistle and torch should be carried, particularly during the winter months. Participants must satisfy themselves that the walk is suitable for their abilities. You can take advice by ringing the walk leader whose telephone number is given. No liability will be accepted for loss or injury that occurs as a result of taking part. An adult must accompany young people (under 18). MOST OF THESE WALKS ARE FOR EXPERIENCED WALKERS Leaders may change or cancel the advertised route due to adverse weather conditions. Strenuous walks require fitness and stamina to cope with several steep climbs and/or cover a good distance at a steady pace. Energetic walks generally involve two steep climbs but they will still require determined application. Moderate walks will seldom have steep climbs but if they do the climb will be taken at a relaxed pace. Dogs (well controlled) are permitted unless stated otherwise in the programme. It should be noted that under the CROW Act, when taking dogs onto Open Access land they must be on a fixed lead, no more than two metres long, whenever livestock are near, and at ALL TIMES from 1st March to 31st July. Non-members of the Park Society will be asked to make a donation of £5.00 each per walk . -
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EGN MAG 11:EGN MAG 9.qxd 31/1/2014 9:41 Page 34 The Welsh Whisky Company’s blends of world class whisky Penderyn Distillery, the only and spirits. distillery in Wales, is situated The steep-sided alluvial chan- in Fforest Fawr Geopark with- nel was probably eroded by a ACTIVITIES in the picturesque Brecon sub-glacial stream flowing at Beacons National Park. The the base of a glacier during distillery provides employ- the last Ice Age. The channel ment and, through its sediments consist of soil and Exhibition Centre with more gravel (3m), gravel and clay PARKS than 20,000 visitors annually, with water (6m), sand gravel it contributes significantly to and silt (19m) clay and gravel tourism activities in Fforest (7m ) and limestone frag- Fawr Geopark. ments and sand with water which line the base (1m) and european GEO walls of the channel. Partnership Groundwater is pumped from sediments below the water between Fforest table at a depth of approxi- provides localised recharge to Water seepage mately 15m below surface. the ground and surface through waters. The results of the a vertical Fawr Geopark and The 19m thick sand gravel joint in the and silt layer, probably the research project show that, Carboniferous Cardiff University main component of the based on calculations from a Limestone aquifer, stores and transmits well pumping test, the benefits a local water fast enough to supply groundwater flow rate of the pumping well. 166,400m3/day, 60, 745,000 The groundwater at Penderyn m3/year through the alluvium business Distillery has two potential channel aquifer is sufficient renewable sources of to sustain the distillery’s In July 2013 the distillery recharge. -
Brycheiniog 39:44036 Brycheiniog 2005 27/4/16 15:59 Page 1
53548_Brycheiniog_39:44036_Brycheiniog_2005 27/4/16 15:59 Page 1 BRYCHEINIOG VOLUME XXXIX 2007 Edited by E. G. PARRY Published by THE BRECKNOCK SOCIETY and MUSEUM FRIENDS 53548_Brycheiniog_39:44036_Brycheiniog_2005 27/4/16 15:59 Page 2 THE BRECKNOCK SOCIETY and MUSEUM FRIENDS CYMDEITHAS BRYCHEINIOG a CHYFEILLION YR AMGUEDDFA OFFICERS President Sr Bonaventure Kelleher Chairman Mr K. Jones Honorary Secretary Miss H. Guichard Membership Secretary Mrs S. Fawcett-Gandy Honorary Treasurer Mr A. J. Bell Honorary Auditor Mr B. Jones Honorary Editor Mr E. G. Parry Honorary Assistant Editor Mr P. Jenkins Curator of Brecknock Museum and Art Gallery Back numbers of Brycheiniog can be obtained from the Assistant Editor, 9 Camden Crescent, Brecon LD3 7BY Articles and books for review should be sent to the Editor, The Lodge, Tregunter, Llanfilo, Brecon, Powys LD3 0RA © The copyright of material published in Brycheiniog is vested in the Brecknock Society & Museum Friends 53548_Brycheiniog_39:44036_Brycheiniog_2005 27/4/16 15:59 Page 3 CONTENTS Officers of the Society 2 Notes on the Contributors 4 Editorial 5 Reports: The Royal Regiment of Wales Museum, Brecon Alison Hembrow 7 Powys Archives Office Catherine Richards 13 The Roland Mathias Prize 2007 Sam Adams 19 Prehistoric Funerary and Ritual Monuments in Breconshire Nigel Jones 23 Some Problematic Place-names in Breconshire Brynach Parri 47 Captain John Lloyd and Breconshire, 1796–1818 Ken Jones 61 Sites and Performances in Brecon Theatrical Historiography Sister Bonaventure Kelleher 113 Frances Hoggan – Doctor of Medicine, Pioneer Physician, Patriot and Philanthropist Neil McIntyre 127 The Duke of Clarence’s Visit to Breconshire in 1890 Pamela Redwood 147 53548_Brycheiniog_39:44036_Brycheiniog_2005 27/4/16 15:59 Page 4 NOTES ON CONTRIBUTORS Sam Adams is a poet and critic who is a member of the Roland Mathias Prize Committee. -
Fforest Fawr Geopark Guide
Garn Goch © Crown Copyright: RCAHMW. Copyright: Crown © Goch Garn Dipper Sundew Dipper Cup Elf Scarlet P204838 British Geological Survey. © NERC 2010. NERC © Survey. Geological British P204838 Philip Veale, Nigel Forster, Nick Jenkins. Nick Forster, Nigel Veale, Philip © Laurie Campbell Laurie © Photographs © BBNPA, Nick Turner, Gareth Ellis, Ellis, Gareth Turner, Nick BBNPA, © Photographs expanded with a growing population. growing a with expanded are evidence of flourishing agricultural activity. Towns and villages and Towns activity. agricultural flourishing of evidence are E-mail: [email protected] E-mail: bounded by dry stone walls and pillow mounds for breeding rabbits breeding for mounds pillow and walls stone dry by bounded Brecon. LD3 7HP. Tel: 01874 624437 01874 Tel: 7HP. LD3 Brecon. witness to industrial activity on a large scale. Hill farms, fields farms, Hill scale. large a on activity industrial to witness Plas y Ffynnon, Cambrian Way, Cambrian Ffynnon, y Plas tramways and railways for transporting these resources, bears resources, these transporting for railways and tramways Brecon Beacons National Park Authority, Park National Beacons Brecon For more information contact the Geopark Development Officer at: Officer Development Geopark the contact information more For presence of quarries, mines and limekilns together with canals, with together limekilns and mines quarries, of presence • www.visitbreconbeacons.com • silica rock, rottenstone and limestone found in the Geopark. The Geopark. the in found limestone and rottenstone rock, silica • www.globalgeopark.org • coming of the Industrial Revolution led man to exploit the coal, the exploit to man led Revolution Industrial the of coming • www.europeangeoparks.org www.europeangeoparks.org • Iron Age hill forts and from Roman roads to Norman castles. -
Nant Tarw Stone Circles and Fan Foel Burial Cairn
Nant Tarw stone circles and Fan Foel burial cairn Walk Information: Maps: OS Explorer OL12 Distance: 4 or 8 miles / 6.5 or 13 kilometres Duration: Allow at least 4 hours for the shorter walk, or 7 hours including Fan Foel Difficulty: medium to hard. Includes rough ground without paths and stream crossings. Only to be attempted in good visibility. Map and compass essential and GPS useful. Start and finish: SN 82002714 Walk summary The walk takes advantage of forestry roads and open access land, visiting prehistoric burial cairns, and two stone circles. The ascent of Fan Foel is optional, but gives spectacular views across the Brecon Beacons. The summit plateau consists of Old Red Sandstone which gives much of the Brecon Beacons its distinctive appearance. The rocks were formed during the Devonian age 416-359 million years ago. This area lies within the Fforest Fawr Geopark: http://www.breconbeacons.org/fforestfawr The walk follows a forestry road before taking a footpath onto the open moorland. A series of often narrow and indistinct paths lead to a large burial cairn from where there is the option of continuing to the summit of Fan Foel or heading directly to the Nant Tarw stone circles across moorland with no paths. CPAT historic landscape walks © Clwyd-Powys Archaeological Trust: available at www.cpat.org.uk/walks 1 Nant Tarw stone circles and Fan Foel burial cairn Introduction The upland ridge of which Fan Brycheiniog is the highest summit at 802m is an impressive landscape and a distinctive local landmark. The steep northern edge falls dramatically to Llyn y Fan Fawr, while the southern side descends gently to the valleys of South Wales. -
EGN Week 2012 Name of Geopark
EGN Week 2012 Name of Geopark: .............Fforest Fawr Geopark.................................................................... Dates of geoparks week: .23 May – 10 June............................................................ Contact person: ...Alan [email protected]................................................................................... Motto of geoparks week:.......Festival 2012..................................................... Category Date Activity / Event dd.mm. 1. Geo & Geo - 26 May - Carreg Cennen Roundabout – a 11 km walk exploring a rocky landscape - 27 May - From Cwm to Cwm- an 8 km walk focusing on the landsacape - 27 May - 3. Geo & Education - 27 May - Brynaman Field Study Visit – a 4km walk introducing geology landscape and flora - 28 May - Limestone and Landscapes – a talk involving geology and industrial and cultural history - 29 May - White Water and Black Powder – a 3km walk focusing on landscape and industrial history - 29 May - Fault Folds and Firebricks – a 4 km walk focuses on the relationship between tectonics, geology and industrial history - 29 May - Dry stone walling and geology- a talk about dry stone walls, an important feature in the geopark - 30 May -Walk, talk and possibly lunch – a 4 km trail exploring the intangible heritage of Mynydd Illtud -30 May - Bountiful Bogs and Marvellous Mires – a 4 km walk explores the wildlife in a glacially -30 May - Geodiversity and geological sites – a talk concerning geoconservation in the geopark sculpted landscape - 31 May -
The Little Neath River Cave, South Wales
186 THE LITTLE NEATH RIVER CAVE, SOUTH WALES The Little Neath River Cave, South Wales By M. G. NORTON, RSa., D. SAVAGE, RSc. and P. A. STANDING ACKNOWLEDGEMENT The society is very grateful to Mr. Tom Lewis of Blaen Nedd Isaf Farm for his friendly co-operation with us in all our activities on his land and in the cave beneath it. Without his co-operation the exploration and surveying recorded in this paper could not have been done. INTRODUCTION This paper covers the work done by the society in the Little Neath River Cave (LNRC) up to May 1967. Most of the cave description has been written by MGN, whilst the geological detail, the survey notes and the drawing up of the survey has been the work of DS. The sections on history, underground drainage of the valley and bibliography have been contributed by PAS. All three authors, however, accept responsibility for the article as a whole. The decision having been taken in 1966 that all new work by the society should be recorded in the metric system, soon to be compulsory, all measurements in the following account are in metric terms. LOCATION The Nedd Fechan or Little Neath River lies in Brecknockshire to the east of the Tawe or Swansea valley and to the west of the Afon Mellte. A certain amount of controversy exists over the naming of the Nedd Fechan and readers interested in reviewing the evidence should consult F. J. North's excellent book "The River Scenery at the Head of the Vale of Neath". -
Cambridge County Geographies General Editor
CAMBRIDGE COUNTY GEOGRAPH IES GU I LLEMARD M A . M. D . G : . eneral Editor F H H , , B RECO NS H IRE C A MB RI DGE UNIVE RS ITY P RE S S F E T N u n h o n z TE R A E . C . il L E , F . NA R C . Y MA GE CLA , l o o P RIN E S S TRE E T QEDmb u rgb , C H E R AND l . S CO . B a m . A A F B R K H 1 8 mm} : . A . OC AU S ’ fi sh) Q u rk : G P P UTNAM S S O NS ‘ t tt MAC MI LLAN AND LT B u mb ag an b Qial u a: CO D. ' ’ Cam ér z ag e C o u n ty Geog r aph er B R E C O N S H I R E CH RISTOPH E R J E VANS l l ‘ M With aps, Diagrams and Illustrations Cam b ridge at th e U n iv e rsity Pr e ss P RE FACE HE author desires to acknowledge his indebtedness to several works on the history and antiquities ' The B ir ds o B r eco m b z r e of B reconshire , especially to f Mr by E . Cambridge Phillips . His thanks are also Mr due to John Ward, for his great assistance during the photographing of exhibits in the Welsh M ' ifi Mr . Car d . useum , ; to C H Priestley, for plans and information supplied ; to Dr W . -
Fforest Fawr Geopark James Cresswell (UK)
Fforest Fawr Geopark James Cresswell (UK) Fig. 1. A geological map of the Fforest Fawr Geopark. Copyright the British Geological Society. n 2005, Fforest Fawr Geopark and outcrop in the extreme western resolved the dispute by defining the became the first geopark to be portion of the geopark, between the Ordovician. He recognised that the Iestablished in Wales. As of October towns of Llandeilo and Llandovery fossil fauna in the disputed layers 2013, it was one of 58 geoparks in (Fig. 1). The names of these towns was different from both the Cambrian Europe. The park has been sculpted by may sound familiar to those who and the Silurian. Lapworth divided nearly 500myrs of geological history know something about stratigraphy, up his Ordovician, which is named and contains the highest mountains because they have been used to name after the Ordovices tribe who lived in in southern Britain, the deepest cave stages within the Ordovician and North Wales and mid Wales during in Britain, the finest collection of Silurian periods. In fact, Wales as a Roman times, into the following waterfalls in Britain and 7,000 years whole has played a very major role series: Tremadog, Arenig, Llanvirn, of recorded human occupation. in the naming of geological periods, Caradog and Ashgill, all named after The geopark lies wholly within the with the earliest three periods places in Wales or near the border, Brecon Beacons National Park, since multicellular life began - the where rocks of these ages occur. occupying the central and western Cambrian, the Ordovician and the The Llanvirn is subdivided into the part of the park. -
Fforest Fawr Traverse (Craig Y Nos to Llwyn-Y-Celyn)
Fforest Fawr Traverse (Craig y Nos to Llwyn-y-celyn YH) Fforest Fawr Traverse (Beacons Way Route) 1st walk check 2nd walk check 3rd walk check 1st walk check 2nd walk check 3rd walk check 06th May 2018 Current status Document last updated Wednesday, 03rd April 2019 This document and information herein are copyrighted to Saturday Walkers’ Club. If you are interested in printing or displaying any of this material, Saturday Walkers’ Club grants permission to use, copy, and distribute this document delivered from this World Wide Web server with the following conditions: • The document will not be edited or abridged, and the material will be produced exactly as it appears. Modification of the material or use of it for any other purpose is a violation of our copyright and other proprietary rights. • Reproduction of this document is for free distribution and will not be sold. • This permission is granted for a one-time distribution. • All copies, links, or pages of the documents must carry the following copyright notice and this permission notice: Saturday Walkers’ Club, Copyright © 2018-2019, used with permission. All rights reserved. www.walkingclub.org.uk This walk has been checked as noted above, however the publisher cannot accept responsibility for any problems encountered by readers. Fforest Fawr Traverse (Craig y Nos to Llwyn-y-celyn) Start: Craig y Nos Bus Stop Finish: Llwyn-y-celyn Bus Stop Craig y Nos bus stop, map reference SN 840 153, is 249 km west of Charing Cross, 209m above sea level and in the Tawe Valley (Cwm Tawe), Llwyn-y-celyn bus stop, map reference SN 972 226, is 15 km north east of Craig y Nos, 10 km south west of Brecon and 326m above sea. -
The Old Red Sandstone of Britain and Ireland – a Review
The Old Red Sandstone of Britain and Ireland – a review RS Kendall British Geological Survey - Cardiff University, Main Building, Park Place, Cardiff. CF10 3AT. [email protected] Abstract The Old Red Sandstone (ORS) is an informal term which is given to continental, predominantly siliclastic, strata of late Silurian to early Carboniferous age which were deposited across the continent of Laurussia at sub-tropic to tropical latitudes. The coincidental development of land plants had a major impact on the atmosphere and global climate by lowering atmospheric carbon dioxide levels, which profoundly affected the style of alluvial sedimentation during this interval, by stabilising flood plains and facilitating the development of soils. The ORS also provides examples of syn- to post- orogenic deposition related to the Caledonian Orogeny, which was affected by synchronous tectonism and volcanism. The influence of Variscan tectonics on basin deformation and tectonism are also evident in the ORS sequence. In October 2014, a symposium was held, organised by the South Wales Geologists’ Association, entitled The Old Red Sandstone: is it Old, is it Red and is it all Sandstone? The event consisted of talks and posters on topics associated with the Old Red Sandstone deposits, principally of Wales and the Welsh Borders and the Scottish Borders in the UK, and included a series of field trips. Seven of the speakers have contributed manuscripts which are presented in this volume. These include papers discussing fossil fish and plant assemblages, the Fforest Fawr Geopark, Old Red Sandstone building stones, and soft sediment deformation. A brief report on the event and acknowledgements is also included. -
THE FELL RUNNER September 1988 REASONS WHY PB’S ARE the BEST
THE FELL RUNNER September 1988 REASONS WHY PB’s ARE THE BEST Lonscale Fell N etherm ost Pike S h elter Crags Base Brow n S k id d aw Little M an Dollywaggon Pike Bowfell Brandreth S kiddaw Fairfield R osset Pike Grey Knotts L ittle Calva H art Crag Allen Crags D alehead G reat C alva Greatrigg Man Esk Pike H in d scarth Great Sea Fell Seat Sandal G reat End R obinson K nott Steel Fell 111 Crag A rd Crags C oom be Calf Crag Broad Crag Scar Crags Bowscale Fell Sergeant Man Scafell Pike C ausey Pike Bannerdale Crags High Raise Scafell Sail B lencathra T h u n ac ar K nott Lingm ell Crag H ill Clough Head Pavey Ark Y ew barrow W andope G reat Dodd Harrison Stickle Red Pike Whiteless Pike Watson Dodd Pike O’Stickle Steeple G rasm oor Stybarrow Dodd Loft Crag Scoat Fell Sand Hill Raise Pike O’Blisco Pillar Hobcarton Pike W hiteside Cold Pike Kirk Fell Ladyside Pike Helvellyn Low Man Red Howe Great Gable W hiteside Helvellyn Crinkle Crags Green Gable Grisedale Pike Mark McDermott on his way to breaking Jos Naylor’s 72 Lakeland Peaks Record set in 1975. Mark wore PB Trainers for the record breaking run of approximately 108 miles with 39,000ft of Ascent. We are the Specialist Running Centre Fast, efficient Mail Order Service - ring or write for Price List Access or Visa welcome PETE BLAND SPORTS 34A Kirkland, Kendal, Cumbria. Tel: (0539) 31012 Shop hours: 9.00 to 5.30, Monday to Saturday CONTENTS ^ O C I A T ^ Page Editorial 1 EDITORIAL Letters 2-4 The New Magazine Calendar Update 4 This is the first magazine printed fo r us by Airey & Stephenson Irish Champs Update 4 and we have changed printer to take advantage of a very com Obituary —Darren Jones 5 petitive offer after Airey <6 Stephenson printed the World Cup Gripping Yarns 2 5 programme.