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Number 71 October 2013
Number 71 FellFarerthe October 2013 Editorial CLUB OFFICIALS Sometimes you get a photograph that you know just has to be the front page picture. PRESIDENT: Gordon Pitt Tel: 015395 68210 Sometimes you don’t and you struggle to find VICE PRESIDENT: Roger Atkinson Tel: 01539732490 any reasonable picture that will do. Then , perversely, they seem to come along like buses TRUSTEES Vicky Atkinson Tel: 07971 408378 - too many all at the same time. Mick Fox Tel: 01539 727531 Cheryl Smallwood Tel: 01629 650164 That’s how it was this time; I had several Mark Walsh Tel: 01606 891050 photographs that would have all made great front cover shots. So which one to choose? COMMITTEE Well, most of the contenders were of the Chairman: Roger Atkinson Tel: 01539 732490 198, Burneside Road Shinscrapers on the crags around Kendal on Kendal LA96EB Thursday evenings but there was just this one, email: [email protected] a happy accident, taken in the dark at the campsite on the shore of Ullswater. I asked Vice Chairman: Mark Walsh Tel: 01606 891050 20, Knutsford Road the Secretary to choose and she answered Antrobus without hesitation. I was pleased. She was Northwich right so I used it. Cheshire CW9 6JW Thanks you to this issue’s contributers : email: [email protected] John Peat, Paul East, Sarah, Matt and Emma Secretary: Clare Fox Tel: 01539 727531 Jennings, Helen Speed, Alec Reynolds, Joan 50, Gillinggate Abbot, David Birkett, Ruth Joyce, Peter and Kendal Nat Blamire LA94JB email: [email protected] Ed. Cover Photograph: Treasurer: Val Calder Tel: 01539727109 Jess Walsh and Kirsten Ball toasting marshmallows, 86, Vicarage Drive The Water Weekend Kendal LA95BA Side Farm Campsite. -
On the Junction of the Silurian Rocks and Carboniferous Limestone On
Downloaded from http://pygs.lyellcollection.org/ by guest on September 30, 2021 309 JUNCTION OF THE SILURIAN HOCKS WITH THE OVERLYING MOUNTAIN LIMESTONE, AT MOUGHTON FELL, IN RIBBL1S- DALE. BY THE EDITOR. (SEE PHOTOGRAPH.) THE photograph issued with this year's volume of proceedings, illustrates an important section exposed in the valley of the Bibble, nearly opposite the village of Horton. The Silurian rocks, composed of grits, slates and limestones, extend over a large area, bounded by the line of the Pennine Fault, running in a north and south direction, and that of the equally important series of Craven Faults which run eastward from Ingleton, their position being indicated by the precipitous Scars of GiggXeswick, Attermire, Malham, Yordale and Kilnsey. Bounded on the west and south by these Faults, the Silurian rocks underlie all the highest moun• tains in Yorkshire, forming a tolerably even base, with a general dip to the north-east. Sections exposing the junction of these rocks with the superincumbent Mountain Limestone may be seen beneath Whernside and Ingleborough, in the Ingleton and Dale Becks, and in Clapdale; underlying Cross Fell and Mickle Fell, they may be seen at High Cup Gill, and as shown by Mr. Dakyns, at the Pencil Mill, near Cronkley Scar. Penyghent, and the extensive Limestone Fells of Malham and Kilnsey also have a basement of Silurian Grits. Perhaps the finest section, showing the junction of the two formations, anywhere exposed, is the one chosen for the subject of this photograph. The Silurian Rocks have long been quarried, and are locally known as the Horton Flagstones; they are a bluish grey colour, rather coarse structure, and can be obtained of very large size. -
Moor House - Upper Teesdale B6278 Widdybank Farm, Langdon Beck, River Tees NNR Forest-In-Teesdale, B6277 Barnard Castle, Moor House – Cow Green Middleton- Co
To Alston For further information A686 about the Reserve contact: A689 The Senior Reserve Manager Moor House - Upper Teesdale B6278 Widdybank Farm, Langdon Beck, River Tees NNR Forest-in-Teesdale, B6277 Barnard Castle, Moor House – Cow Green Middleton- Co. Durham DL12 0HQ. Reservoir in-Teesdale To Penrith Tel 01833 622374 Upper Teesdale Appleby-in- National Nature Reserve Westmorland B6276 0 5km B6260 Brough To Barnard Castle B6259 A66 A685 c Crown copyright. All rights reserved. Kirkby Stephen Natural England 100046223 2009 How to get there Front cover photograph: Cauldron Snout The Reserve is situated in the heart of © Natural England / Anne Harbron the North Pennines Area of Outstanding Natural Beauty. It is in two parts on either Natural England is here to conserve and side of Cow Green Reservoir. enhance the natural environment, for its intrinsic value, the wellbeing and A limited bus service stops at Bowlees, enjoyment of people and the economic High Force and Cow Green on request. prosperity that it brings. There is no bus service to the Cumbria © Natural England 2009 side of the Reserve. ISBN 978-1-84754-115-1 Catalogue Code: NE146 For information on public transport www.naturalengland.org.uk phone the local Tourist Information Natural England publications are available Centres as accessible pdfs from: www.naturalengland.org.uk/publications Middleton-in-Teesdale: 01833 641001 Should an alternative format of this publication be required, please contact Alston: 01434 382244 our enquiries line for more information: 0845 600 3078 or email Appleby: 017683 51177 [email protected] Alston Road Garage [01833 640213] or Printed on Defra Silk comprising 75% Travel line [0870 6082608] can also help. -
Y6 Geography: Mountains of the UK Local Study: the Pennines
Y6 Geography: Mountains of the UK Local Study: The Pennines Mountain Ranges of the UK Can you identify these mountain areas of the UK? Mark the highest peak in each range with a triangle. Label the mountain and its height in metres. How are mountain areas shown on maps? Find out about contour lines and look at some examples on Ordnance Survey maps. • Pennines • Cumbrian Mountains • Sperrin Mountains • Grampians • Snowdonia • Dartmoor https://www.bbc.co.uk/bitesize/topics/z849q6f/articles/z4g3qp3 QUIZ Which country is the Sperrin Range in? What is the highest mountain in the whole of the UK? Which range is the furthest south? Which parts of the UK have no mountainous areas? Which ranges are easily accessible from Bolton? Which mountain in the UK has a ski slope? Which mountain has a train going to the top? Local Study: The Pennines The Pennines are a mountain range in England. Often said to be the "backbone of England", they form an unbroken range stretching from the Peak District in the Midlands, through the Yorkshire Dales, parts of Greater Manchester, the West Pennine Moors of Lancashire and Cumbrian Fells to the Cheviot Hills on the Scottish border. Their total length is about 250 mi (402 km). The name Pennines is believed to come from the Celtic pennioroches, meaning "hill", although the earliest written reference to the name dates only from the 18th century. Altitude and size The mountains are not very tall and are often called hills. The highest is Cross Fell in eastern Cumbria, at 893 m (2,930 ft). -
Barnard Castle
THA TBSSDaLU MEHUUKT—W£x>N ANU ARY 5, iy)6 The Top of Mickle The Urban Council. Fell. ROBERT ORD’S GREAT WINTER SALE THE CHAIRMAN ANO A LASTINC ANO HONOURABLE. PEACE. HIGHEST POINT IH YORKSHIRE. OF DRAPERY GOODS The monthly meeting ot the members of the Ba: aid Caatio Urba; District Council was IBY HARWOOD BRIERLEY.] heli on Thnr’day night. Mr J. Wiseman, J.P^ It is the ambition of most pedestrians and Commenced on Tuesday, 4th January, 1916. presided, and there were also present the Rev. Climbers in Upper Teasdale to reach the roof H. W. H. Birchair, Messrs F. Wi 830, J. Guy, R. of Yorkshire—vix., Mickle Fell, in tho north Woodhams, H. Waiker, C. J. Smith, W. idodgsoo, west angle of onr br- ;d acre’d shire. They J I Dawson (clerk), J. H. Vol .ch (aseiatant- are conscious of it® -operative nearness to Special Bargains in all departments derk). C. H. We-fnrd, M D. (medical officer), H. the one acceptable . .rting-point, which is E. Raire (surveyor), and F. V. Ord (oclloctor). High Force Hotel, and only bad weather will deter them from embracing this opportunity _ Seasonable Greeting*. to conquer the elusive crest, whose exact The Chairman said he would like at the whereabouts still remains to be determined. THE HORSE MARKET, BARNARD CASTLE. outse': to wish tho compliments of the season The practised mountaineer would regard it as to the members and cffioisia of tile C 'UuclL incredible that an elevation only five miles avd to express a hope that tbe dark cloud of not find it such an easy matter to skirt the war wcnld have pass'd away before mother distant to the south-west as the crow would old-time leadminers’ “brakes ” cut to a depth fly should have to be discovered, and especially BABUTARD CAETLE 'Aesdale Guardians, year oiosod, »nd that they would have a of about 20 feet in places, up and down whose ’sstlng and hoc urab’e psaoo es.abllehsd. -
Full Edition
THE UPPER WENSLEYDALE NEWSLETTER ISSUE 188 FEBRUARY 2013 Donation please: 30p suggested or more if you wish tarmac to reduce run-off, using less energy (see Published by Upper Wensleydale Editorial Rose Rambler on page 30) or even upping our The Upper Wensleydale Newsletter Newsletter ooking back and forth! Back, there was giving to the poorest in the world. It can also Burnside Coach House, the Jubilee and then the Olympics. cheer us up, ‘doing our bit’. Forth, anything to take the mind to Burtersett Road, Hawes DL8 3NT Issue 188— February 2013 L As for the other really big issues, at home or pleasant things? To date it isn’t looking good. abroad, shouldn’t we really try to read up the Features What will be the ‘main issues’ this year; what facts, so that when any opportunity comes to Tel: 667785 will really concern us? Already, triviality is rais- ‘have our say’ we know what we are talking ing its head; we write as even the Prime Minis- e-mail: [email protected] Editorial 3 about and don’t make up our minds on hearsay ter has had to answer questions about horse or prejudice? ____________________________ meat, and a local authority is talking about pun- After the usual thorough committee discussion Printed by Wensleydale Press Hawes Auction Mart 12 ishment for throwing snowballs. Do we make a on this we agreed it was a bit gloomy and ________________ ____________ fuss about the right things? Whatever next? Not heavy. Could readers suggest, we mused, any Committee: Alan S.Watkinson, Our Schools 14 that a bit of trivia and gossip is particularly Barry Cruickshanks (web), Sue E .Duffield, good, cheerful stuff for the future to cheer us ____________________________ harmful but… Sue Harpley, , Alastair Macintosh, up… and then we thought “ Oh yes, Bradford Ranger Report 17 Far from trivial, on the world stage, are new City!” Neil Piper, Janet W. -
North Pennine Ridge South Section
Route Information Distance 23 kilometres (14.5 miles) Ascent 1050 metres (3450 feet) Time needed 9 hours (approx) Start point Dufton village green, approx 3½ miles north of Appleby-in-Westmorland. Parking available in the small car park just off the village green at NY 689 249 Public Transport Dufton is served by bus routes 573 and 625 (limited service) © Crown Copyright 2011. All rights reserved. Licence no 100019596 (Southern Section) Part of this route crosses open access land on a managed grouse moor, over which DOGS ARE NOT ALLOWED. This area is coloured red on the accompanying map. Access may be further restricted during the nesting season and at other times of the year. To avoid disappointment, please visit www.countrysideaccess.gov.uk to get the latest restriction information, before you set out. Hurning Lane follows naturally on offering fine views of Dufton Pike, with further gates and stiles to approach and pass Halsteads, a traditional farmstead now used for stock- handling. This is the last hint of settlement on the walk until Hartside Café. From the gate beside the buildings the Pennine Way leads up the open track, flanked by a remnant hedge. The track curves downhill to arrive at a wall-stile and Currick near Fiend’s Fell, Hartside gate, promptly step over the clapper-bridge spanning Great Rundale Beck. Follow on In The North Pennines of Outstanding Natural Area Beauty & European Geopark Begin from the village car park at the with the wallside track, gradually rising to a eastern end of the attractive, wide, tree- kissing-gate, the upper walled lane portion lined green. -
Definition of Favourable Conservation Status for Marsh Saxifrage
Definition of Favourable Conservation Status for Marsh Saxifrage Saxifraga hirculus Defining Favourable Conservation Status Project Author: Ian Taylor www.gov.uk/natural-england Contents About the DFCS project ........................................................................................................................ 2 Introduction ........................................................................................................................................... 3 Definitions and ecosystem context ....................................................................................................... 4 Natural range and distribution ............................................................................................................... 7 Population ........................................................................................................................................... 10 Habitat for the species ........................................................................................................................ 13 Annex 1: References .......................................................................................................................... 14 Annex 2: Tenth Birds Directive Reporting ........................................................................................... 14 About the DFCS project Natural England’s Defining Favourable Conservation Status (DFCS) project is defining the minimum threshold for thriving habitats and species in England. We are doing this so we can -
Nutt No Name Nutt Ht Alt Area District Group Done Map Photo 1 Scafell
Nutt no Name Nutt ht Alt Area District Group Done Map Photo 1 Scafell Pike 3209 978 LAKE DISTRICT SOUTH SCAFELL y map Scafell Pike from Scafell 2 Scafell 3163 964 LAKE DISTRICT SOUTH SCAFELL y map Scafell 3 Symonds Knott 3146 959 LAKE DISTRICT SOUTH SCAFELL y map Symonds Knott 4 Helvellyn 3117 950 LAKE DISTRICT EAST HELVELLYN y map Helvellyn summit 5 Ill Crag 3068 935 LAKE DISTRICT SOUTH SCAFELL y map Ill Crag 6 Broad Crag 3064 934 LAKE DISTRICT SOUTH SCAFELL y map Broad Crag 7 Skiddaw 3054 931 LAKE DISTRICT NORTH SKIDDAW y map Skiddaw 8 Helvellyn Lower Man 3035 925 LAKE DISTRICT EAST HELVELLYN y map Helvellyn Lower Man from White Side 9 Great End 2986 910 LAKE DISTRICT SOUTH SCAFELL y map Great End 10 Bowfell 2959 902 LAKE DISTRICT SOUTH BOWFELL y map Bowfell from Crinkle Crags 11 Great Gable 2949 899 LAKE DISTRICT WEST GABLE y map Great Gable from the Corridor Route 12 Cross Fell 2930 893 NORTH PENNINES WEST CROSS FELL y map Cross Fell summit 13 Pillar 2926 892 LAKE DISTRICT WEST PILLAR y map Pillar from Kirk Fell 14 Nethermost Pike 2923 891 LAKE DISTRICT EAST HELVELLYN y map Nethermost Pike summit 15 Catstycam 2920 890 LAKE DISTRICT EAST HELVELLYN y map Catstycam 16 Esk Pike 2904 885 LAKE DISTRICT SOUTH BOWFELL y map Esk Pike 17 Raise 2897 883 LAKE DISTRICT EAST HELVELLYN y map Raise from White Side 18 Fairfield 2864 873 LAKE DISTRICT EAST FAIRFIELD y map Fairfield from Gavel Pike 19 Blencathra 2858 868 LAKE DISTRICT NORTH BLENCATHRA y map Blencathra 20 Bowfell North Top 2841 866 LAKE DISTRICT SOUTH BOWFELL y map Bowfell North Top from -
Trend-Surface Analysis of Central Pennine Erosion Surfaces
Trend-Surface Analysis of Central Pennine Erosion Surfaces Cuchlaine A. M. King Transactions of the Institute of British Geographers, No. 47. (Sep., 1969), pp. 47-59. Stable URL: http://links.jstor.org/sici?sici=0020-2754%28196909%291%3A0%3A47%3C47%3ATAOCPE%3E2.0.CO%3B2-3 Transactions of the Institute of British Geographers is currently published by The Royal Geographical Society (with the Institute of British Geographers). Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/about/terms.html. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/journals/rgs.html. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. The JSTOR Archive is a trusted digital repository providing for long-term preservation and access to leading academic journals and scholarly literature from around the world. The Archive is supported by libraries, scholarly societies, publishers, and foundations. It is an initiative of JSTOR, a not-for-profit organization with a mission to help the scholarly community take advantage of advances in technology. For more information regarding JSTOR, please contact [email protected]. -
Durham Rare Plant Register 2013 Covering VC66 and the Teesdale Part of VC65
Durham Rare Plant Register 2013 Covering VC66 and the Teesdale part of VC65 JOHN L. DURKIN MSc. MCIEEM BSBI Recorder for County Durham 25 May Avenue. Winlaton Mill, Blaydon, NE21 6SF [email protected] www.durhamnature.co.uk Contents Introduction to the rare plants register Notes on plant distribution and protection The individual species accounts in alphabetical order Site Index First published 2010. This is the 2013, third edition. Improvements in this edition include- An additional 10% records, most of these more recent and more precise. New colour coded maps produced from DMAP. This edition is “regionally aligned”, that is, several species which are county rare in Northumberland, but were narrowly rejected for the Durham first edition, are now included. Cover picture—Spring Gentian at Widdybank Fell. Introduction Many counties are in the process of compiling a County Rare Plant Register, to assist in the study and conservation of their rare species. The process is made easier if the county has a published Flora and a strong Biological Records Centre, and Durham is fortunate to have Gordon Graham's Flora and the Durham Wildlife Trust’s “Recorder" system. We have also had a Biodiversity project, based at Rainton Meadows, which until 2013 carried out conservation projects to protect the rare species. It is hoped that the “RPR” will act as a stimulus for local botanists to make special efforts to improve the database by recording these species. The register will be used to increase our understanding of the status and distribution of the rare species, and to aid and promote their conservation. -
Download Chapter In
Geomorphology and Quaternary glacial legacy by David J A Evans The last 2.6 million years of Earth history (the Quaternery Period) is characterised by large volumes of global ice relative to previous geological periods and is the culmination of a long-term cooling trend that began some 55 million ago. The extent of ice has varied in an oscillatory fashion so that the Quaternary Period is characterised by two dominant climate extremes called glacials and interglacials. However, the climate is never stable, oscillating instead dynamically from one extreme state to the other and necessitating the use of the terms stadial and interstadial to refer to phases of relative cold and warmth during glacial stages. Many physiographic details of the North Pennines relate specifically to the lithological and structural control of the underlying bedrock, whose denudation and incision has resulted in conspicuous stepped hillslope profiles and tableland type topographic features. Additionally, the area contains some remarkable relict channels and underfit valleys (those now hosting streams too small to have been capable of cutting them), which are developed respectively on valley sides and across lower lying, undulatory to hummocky topography; such valleys are either of a glacial meltwater origin or relate to more complex and longer timescale combined fluvial and glacial origin (Evans 2017). The longer timescale drainage features date to fluvial processes that may have operated long before the onset of the Ice Age or the Quaternary Period. Glaciation is manifest in the landscapes of Teesdale and the North Pennines in the form of erosional features cut directly by the ice or by its meltwater and more obviously in the form of glacigenic drift.