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Brecon Beacons Weekends
The 'diving board' on Fan y Big with Cribyn behind BRECON BEACONS WEEKENDS Weekend walking adventures for London-based hikers www.walkyourweekends.com 1 of 34 CONTENTS Introduction • Main features of interest 3 • Resources 5 • Where to stay 5 • Decision time! Weekend options summary 7 • Getting there 8 • Getting around 9 Suggested weekend itineraries • Weekend 1: Merthyr Tydfil & Abergavenny/Crickhowell 10 • Weekend 2: Merthyr Tydfil 13 • Weekend 3: Abergavenny/Crickhowell 15 The Walks 17 • A BEACONS TRAVERSE 18 • B LOW LEVEL WALK TO TALYBONT-ON-USK 21 • C PEN Y FAN CIRCULAR 23 • D TAFF TRAIL TO MERTHYR TYDFIL 26 • E CRICKHOWELL WALKS 27 • F SUGAR LOAF 30 • G FAN FAWR 31 • H SKIRRID FAWR 31 • I MERTHYR GENTLE WALK 32 Staying in Abergavenny 33 Staying in Merthyr Tydfil 34 www.walkyourweekends.com 2 of 34 INTRODUCTION MAIN FEATURES OF INTEREST The Brecon Beacons is a mountain range in south Wales and a national park. → CLICK HERE to see a n overview map of the Brecon Beacons ← Trail magazine's list of the 100 best mountains to climb in the UK (which is of course entirely subjective but is a useful place to start!) includes three peaks in the Brecon Beacons: • Pen y Fan – the highest peak in South Wales; between Brecon and Merthyr Tydfil. Pen y Fan sits in a cluster of other peaks including Corn Du, Cribyn and Fan y Big, so most of them can be climbed in a single walk. These are the main 'Beacons' in the Brecon Beacons. In this guide I'll refer to them as “Pen y Fan et al”. -
Learning Objective: to Find out About the Hills and Mountains of the UK
The United Kingdom Learning Objective: To find out about the hills and mountains of the UK. www.planbee.com NEXT What is the difference between a hill and a mountain? Think, pair, share your ideas. BACK www.planbee.com NEXT The difference between a hill and a mountain is not always clear and there is no set definition for the difference. Hills are generally smaller than mountains. Mountains are usually steeper than hills too and have a distinct summit. Mountain Hill Did you know that the elevation of hills and mountains is measured from sea level? BACK www.planbee.com NEXT There are several different ways in which mountains can be formed. The Earth’s crust is made up of different slabs called tectonic plates. Over millions of years these plates move. When two plates collide they fold over each other, like a car crash collision, and rock is pushed upwards. This type of mountain is called a ‘fold mountain’ and is the most common form of mountain. BACK www.planbee.com NEXT Another type of mountain are ‘dome mountains’. These occur when the pressure from lots of hot magma under the Earth’s crust pushes the earth upwards into a dome without the magma pushing through the surface. BACK www.planbee.com NEXT Volcanos are also mountains. Volcanos are caused when magma (hot melted rock) erupts through the centre of the volcano and the lava cools in a cone shape. Volcanos are built up when layers of cooled lava turn to rock which build on top of each other over time. -
Barber & Gallon, 2020
Bulletin of the British Myriapod & Isopod Group Volume 32 (2020) Upland centipedes in North Wales with a review of the Welsh Chilopoda Anthony D. Barber1 and Richard Gallon2 1 7 Greenfield Drive, Ivybridge, Devon, PL21 0UG. Email: [email protected] 2 23a Roumania Crescent, Llandudno, North Wales, LL30 1UP. Email: [email protected] Abstract Since Eason’s (1957) paper on centipedes from Carnarvonshire there has been an accumulation of centipede records from various parts of Wales but relatively few are from upland areas. Recent records from Snowdonia included several species, including Lithobius (Monotarsobius) curtipes, from locations up to around 1,000m. We present a review of centipedes recorded from the 13 Welsh vice-counties which includes 41 species, 4 of which are from buildings or heated greenhouses, 4 apparently obligate halophiles from coastal sites and one doubtful. Wales has a variety of types of habitat including both lowland and montane rural areas and urban/industrial/post-industrial locations which no doubt contributes to the diversity of its chilopod fauna. Introduction The centipede Lithobius curtipes is not known in Britain from large numbers of past records, indeed in his Cotteswold paper of 1953, E.H. Eason (Eason, 1953) had referred to his record from Kildanes Scrubs, Gloucestershire in 1952 as only the third British record. The finding of it by RG at around 1,000m in Snowdonia, along with Lithobius variegatus and Strigamia acuminata at similar heights, prompted us to look at the occurrence of upland centipedes in North Wales and in Wales in general and to review the species recorded from the principality. -
The Journal of the Fell & Rock Climbing Club
THE JOURNAL OF THE FELL & ROCK CLIMBING CLUB OF THE ENGLISH LAKE DISTRICT Edited by W. G. STEVENS No. 47 VOLUME XVI (No. Ill) Published bt THE FELL AND ROCK CLIMBING CLUB OF THE ENGLISH LAKE DISTRICT 1953 CONTENTS PAGE The Mount Everest Expedition of 1953 ... Peter Lloyd 215 The Days of our Youth ... ... ...Graham Wilson 217 Middle Alps for Middle Years Dorothy E. Pilley Richards 225 Birkness ... ... ... ... F. H. F. Simpson 237 Return to the Himalaya ... T. H. Tilly and /. A. ]ac\son 242 A Little More than a Walk ... ... Arthur Robinson 253 Sarmiento and So On ... ... D. H. Maling 259 Inside Information ... ... ... A. H. Griffin 269 A Pennine Farm ... ... ... ... Walter Annis 275 Bicycle Mountaineering ... ... Donald Atkinson 278 Climbs Old and New A. R. Dolphin 284 Kinlochewe, June, 1952 R. T. Wilson 293 In Memoriam ... ... ... ... ... ... 296 E. H. P. Scantlebury O. J. Slater G. S. Bower G. R. West J. C. Woodsend The Year with the Club Muriel Files 303 Annual Dinner, 1952 A. H. Griffin 307 'The President, 1952-53 ' John Hirst 310 Editor's Notes ... ... ... ... ... ... 311 Correspondence ... ... ... ... ... ... 315 London Section, 1952 316 The Library ... ... ... ... ... ... 318 Reviews ... ... ... ... ... ... ... 319 THE MOUNT EVEREST EXPEDITION OF 1953 — AN APPRECIATION Peter Lloyd Everest has been climbed and the great adventure which was started in 1921 has at last been completed. No climber can fail to have been thrilled by the event, which has now been acclaimed by the nation as a whole and honoured by the Sovereign, and to the Fell and Rock Club with its long association with Everest expeditions there is especial reason for pride and joy in the achievement. -
RR 01 07 Lake District Report.Qxp
A stratigraphical framework for the upper Ordovician and Lower Devonian volcanic and intrusive rocks in the English Lake District and adjacent areas Integrated Geoscience Surveys (North) Programme Research Report RR/01/07 NAVIGATION HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub-headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/01/07 A stratigraphical framework for the upper Ordovician and Lower Devonian volcanic and intrusive rocks in the English Lake The National Grid and other Ordnance Survey data are used with the permission of the District and adjacent areas Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2004. D Millward Keywords Lake District, Lower Palaeozoic, Ordovician, Devonian, volcanic geology, intrusive rocks Front cover View over the Scafell Caldera. BGS Photo D4011. Bibliographical reference MILLWARD, D. 2004. A stratigraphical framework for the upper Ordovician and Lower Devonian volcanic and intrusive rocks in the English Lake District and adjacent areas. British Geological Survey Research Report RR/01/07 54pp. -
Notes on the Geology of the English Lake District
449 NOTES ON THE GEOLOGY OF THE ENGLISH LAKE DISTRICT. By]. E. MARR, M.A., F.R.S. (Rlad July 6tlr, I,OO.) A.-INTRODUCTION. HE Council of your Association has done me the honour of T inviting me to act as Director of an excursion to Lakeland in the course of the summer. In these circumstances, as I have been engaged in studying the geology of the district for many years, and have arrived at certain conclusions which have not hitherto been published, I may be pardoned if I incorporate among notes which may serve to give some idea of the general structure of the district, a summary of such conclusions; especially as, in my opinion, a knowledge of them is requisite to a right understanding of the actual structure. For several seasons I have had the pleasure of working in Cumbria with my colleague, Mr. Alfred Harker. Many of the facts and conclusions recorded in this paper are the result of this joint work, and my colleague shares with me the credit for any records which may be of value. I shall endeavour in the paper to point out clearly such portions as must be regarded as the joint work of Mr. Harker and myself. I have obtained his permission to give this brief preliminary outline of the results of our work, and should any errors be found therein I ask that I alone may be considered responsible for them. It is well-known that the heart of Lakeland is composed of Lower Palseozoic rocks, and that around these is a girdle of later deposits of Carboniferous, Permian, and Triassic ages. -
Inhoudsopgave
Inhoudsopgave Voorwoord . 3 Overzichtskaart . 6 Algemene tips . 7 Symbolen . 7 TOP De mooiste wandelingen in Wales . .. 10 TOP GPS-Tracks . 12 TOP TOP Natuur en landschap van Wales. 16 TOP Informatie en adressen . 21 TOP Engels en Welsh voor wandelaars . 25 TOP TOP 1 5 .30 uur Cadair Idris . 28 TOP 2 1 .30 uur Rond de Foel Cynwch . 31 TOP 3 8 .00 uur Aran Fawddwy, 905 m . 33 TOP 4 2 .00 uur In de bossen van Coed Ganllwyd . 35 TOP 5 8 .00 uur Rhinog Fawr, 720 m . 37 TOP 6 6 .00 uur Arenig Fawr, 854 m . 40 TOP 7 6 .00 uur Cnicht, 689 m . 42 TOP 8 3 .30 uur Aberglaslyn en Cwm Bychan. .. 45 TOP 9 2 .00 uur Yr Eifl en Tre’r Ceiri . 47 TOP 10 6 .00 uur Snowdon, 1085 m, via Llanberis Path . 49 TOP 11 6 .30 uur Snowdon, 1085 m, via Y Lliwedd . 52 TOP 12 8 .30 uur Y Glyderau . 55 TOP 13 6 .30 uur Y Carneddau . 58 TOP 14 4 .00 uur Newborough Warren. 61 TOP 15 3 .00 uur Rhoscolyn . 64 TOP 16 3 .00 uur Carmel Head . 66 TOP 17 2 .00 uur Aber Falls . 68 TOP 18 3 .00 uur Great Orme . 70 TOP 19 4 .00 uur Naar de meren Llyn Geirionydd en Llyn Crafnant . 73 TOP 20 2 .30 uur Aan het meer Llyn Brenig . 76 TOP 21 5 .00 uur Clwydian Range . 78 TOP 22 8 .30 uur Llangollen . .. 81 TOP 23 3 .00 uur Aan Lake Vyrnwy . -
Geology in Borrowdale
Geology Situated on the boundary between the Ordovician Skiddaw Group and the Borrowdale Volcanic Group, Derwentwater Independent Hostel is perfectly located for studying the oldest rocks in the Lake District. We have 500 million years of geological history on our doorstep! The Skiddaw Group lies to the north of the hostel, while to the south you will see the craggier terrain of the Borrowdale Volcanic Group. You will also be able to study evidence of former glacial activity in Borrowdale, mainly in the form of depositional features. There are lots of old mines and quarries in Borrowdale and the adjoining valleys, and many Regionally Important Geological/Geomorphological Sites (RIGS). A very useful introduction to the geology of Cumbria and the surrounding area: http://www.naturalengland.org.uk/ourwork/conservation/geodiversity/englan ds/counties/area_id7.aspx The Cumberland Geological Society: http://www.cumberland-geol-soc.org.uk/ We have several useful Geology books in our library, including: Lakeland Rocks and Landscape: a Field Guide by The Cumberland Geological Society, and The Rocks and Landscape of the Keswick Area by Alan Smith. We also have books about the history of Honister Slate Mine, Borrowdale graphite, and Cumbrian coal mining. Local issues of geological relevance include underground nuclear waste disposal, treatment of water from the disused Force Crag Mine, and stability of the St Bees headland and adjacent coastline. The only published Geological Survey map of the area is sheet 54N 04W at the 1: 250 000 scale. OS map Outdoor Leisure Map 4: The English Lakes: North Western sheet will help you find features of interest. -
A Long Walk to Berwick
A long walk to Berwick The Great Outdoors magazine, November 2016 I’d been a long time getting to Berwick: you could reckon it in hours, years or decades, depending where you started from. Hours: eight. That wasn’t bad for 23 miles from Wooler. Years: ten, since I’d set out from Land’s End with a vague plan, to walk 800 miles across England, a bit at a time. Decades: six and a bit. I never before had found the excuse to walk through Berwick-upon-Tweed, though I’d shot past it on the train often enough, and it seemed a nice sort of place to go to, with its border history, estuary location and recently-ended war with Russia. The vagueness of my plan to cross England was very much the point. That unholy trinity of work, family and finance meant that opportunities to get into the great outdoors from my London home were all too limited, essentially just one short break a year, everything else just local lowland walking. I’d got frustrated with cherry-picking different bits of the nation each year – the North Devon Coast one time, the Black Mountains another, say. I was the sort of guy who needed a plan, one that involved a nice B&B at the end of the day. I didn’t do spartan. And that plan, before England, was Wales, starting 2002. I’d walked Offa’s Dyke Path a few years before, and it came to me that finding and walking a different, wilder, hillier line across that grand little nation might be fun. -
North West England & Isle of Man: Climate
North West England & Isle of Man: climate This describes the main features of the climate of Cheshire, Merseyside, Greater Manchester, Lancashire, Cumbria, part of North Yorkshire and the Isle of Man. The eastern boundary of the region lies along the watershed of the Pennines. There are several distinct geographical areas within the region. Much of the area west of the Pennines from Lancashire southwards forms part of a plain, mainly below 150 metres, with westward draining rivers such as the Mersey, Ribble and Lune. Liverpool and Manchester are the main centres of population. To the east, the Pennines are a chain of rolling gritstone moors rising to well over 600 metres and reaching their highest point at Cross Fell (893 metres). The Pennines form a natural barrier to east-west communications, but there are the Tyne gap linking Carlisle and Newcastle and the Aire gap linking Lancashire and Yorkshire. The Lake District in Cumbria includes Scafell Pike (978 metres), the highest mountain in England, and Windermere, the largest lake. To the north and NE, there is further low ground (below 60 metres) in the Vale of Eden and the Solway Plain, close to Carlisle. Most of the Isle of Man consists of a central mountain mass rising to 621 metres on Snaefell. Douglas is the main town and the centre of the island's tourist industry. The range of topography and altitude found in both NW England and the Isle of Man provide a climate of great variety, and the region includes both the coldest place in England (Cross Fell in the Pennines) and the wettest place in England (the Lakeland fells around Seathwaite in Cumbria). -
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. -
LCA 6 Dentdale Yorkshire Dales National Park - Landscape Character Assessment YORKSHIRE DALES NATIONAL PARK LANDSCAPE CHARACTER ASSESSMENT LANDSCAPE CHARACTER AREAS 2
1 Dentdale, looking east from nearGreenwood Haw nearGreenwood from east looking Dentdale, LCA 6 Dentdale Yorkshire Dales National Park - Landscape Character Assessment YORKSHIRE DALES NATIONAL PARK LANDSCAPE CHARACTER ASSESSMENT LANDSCAPE CHARACTER AREAS 2 LCA 6 Dentdale Key characteristics • West facing sinuous, deep U-shaped glacial valley with gently undulating valley sides. • Lower Dentdale has a broad and relatively flat valley floor; to the east of Dent, the valley is narrow, with a consistent Upper Dentdale, profile. looking east to • The limestone outcrop of Combe Scar, and the associated corrie below, is a prominent feature. Great Knoughtberry Hill from near Slack • River Dee has a smooth, platformed bed with steps or ledges, and extensive tree cover on riverbanks. • Frequent tributary gills giving valley side a folded, indented appearance, their winding form picked out by abundant tree cover. • Lush, green, well-treed valley, with linear lines of hedgerows appearing to tumble down the valley sides to connect with densely wooded river banks. • Picturesque, traditional stone-built village of Dent with narrow, cobbled streets. Many houses within Dent, and other farmsteads sited along the mid-slopes of the dale, have been rendered and painted white. • Medium to large sized fields with hay meadows, mainly enclosed by hedgerows and some drystone walls. • Narrow, winding roads with an enclosed character. • Two local stone viaducts on the Settle to Carlisle Railway are significant features at the head of Dentdale. Numbered photographs