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My 214 Story Name: Christopher Taylor Membership Number: 3812 First Fell Climbed
My 214 Story Name: Christopher Taylor Membership number: 3812 First fell climbed: Coniston Old Man, 6 April 2003 Last fell climbed: Great End, 14 October 2019 I was a bit of a late-comer to the Lakes. My first visit was with my family when I was 15. We rented a cottage in Grange for a week at Easter. Despite my parents’ ambitious attempts to cajole my sister Cath and me up Scafell Pike and Helvellyn, the weather turned us back each time. I remember reaching Sty Head and the wind being so strong my Mum was blown over. My sister, 18 at the time, eventually just sat down in the middle of marshy ground somewhere below the Langdale Pikes and refused to walk any further. I didn’t return then until I was 28. It was my Dad’s 60th and we took a cottage in Coniston in April 2003. The Old Man of Coniston became my first summit, and I also managed to get up Helvellyn via Striding Edge with Cath and my brother-in-law Dave. Clambering along the edge and up on to the still snow-capped summit was thrilling. A love of the Lakes, and in particular reaching and walking on high ground, was finally born. Visits to the Lakes became more regular after that, but often only for a week a year as work and other commitments limited opportunities. A number of favourites established themselves: the Langdale Pikes; Lingmoor Fell; Catbells and Wansfell among them. I gradually became more ambitious in the peaks I was willing to take on. -
Welsh 3000S – 24Hrs Y DAITH FYNYDDIG GLASUROL CYMREIG
SNOWDONIA: THE CLASSIC WELSH MOUNTAIN JOURNEY Welsh 3000s – 24hrs Y DAITH FYNYDDIG GLASUROL CYMREIG OVERVIEW Are you ready For the 15 highest peaks iN NortherN Welsh 3000s – 24hrs Snowdonia - all over 3000ft - in 1 loNg day? This may prove to be one of the most challenging 03:40 Meet your MouNtaiN Leader in LlaNberis or NaNt Peris for liFt to Pen y Pass start point routes you can Follow in the UK mountains; over 04:00 Start the Welsh 3000s rocky and rough terrain in places. With over 4200m 05:25 Crib Goch summit of ascent over 3 magniFicent mountain ranges, you’ll 06:30 Carnedd Ugain summit be Forgiven For wanting to be picked up by Flying 06:50 SnowdoN summit angels towards your last summit! 08:15 Arrive iNto NaNt Peris - valley stop (hot driNks/breakFast rolls) For the 24hr continuous effort, with prior training, 08:45 Depart NaNt Peris preparation and commitment oN the day – it is 10:15 Elidir Fawr summit achievable in approximately 18-20 hours For Fit aNd experienced walkers. Do Not uNderestimate the 11:30 Y Garn summit preparation and stamina required For this endurance 12:40 Glyder Fawr summit (aFter luNch) walk; it will require much traiNiNg oN similar, 13:15 Glyder Fach summit mouNtaiNous grouNd. 14:30 TryFaN summit 15:45 Arrive iNto OgweN - valley stop (savoury snacks/soup) Our costs iNclude all staFFiNg required, traNsport to 16:00 Depart OgweN valley and From eveNt start/finish. For the 24hr event, costs 17:30 PeN yr ole WeN summit include repleNishmeNt oF water aNd sNacks at two 17:50 Carnedd DaFydd summit locatioNs. -
Seascale Magazine
G E O THE L S JULY A F MAGAZINE C O 2015 LINKING S R SUMMER 3 PARISHES A T EDITION E DRIGG H S & CARLETON OWLS STAY AT MUNCASTER joined by hawks a a and falcons r r e e h Y h S A R M E N D I N t A W t S O E H N S I L T U R A A P E e e L Y A B D G K N S I E T t t T N I A A P D E C Y I A L L Y P R S I C D A s r MONDAY 8:30am – 5:30pm u o TUESDAY 8:30am – 5:30pm h WEDNESDAY 8:30am – 5:30pm g n THURSDAY 8:30am – 5:30pm i n FRIDAY 8:30am – 5:30pm e p later appointments at request o G E O L S A F ARISH C O P S R A T E DRIGG H & CARLETON EWS S N Editor: Eileen Eastwood 019467 28653 THE [email protected] MAGAZINE Production: Trevor Preece 019467 28449 LINKING [email protected] 3 PARISHES SEASCALE On 1 June I ceased being a District Councillor and the Mayor of Copeland. It has been a privilege to serve the community over the last 12 years and to finish my time as a Copeland Councillor as the last Mayor of Copeland. My thanks to everyone in the community who has baked, given prizes, run a bingo session, having a coffee morning, opening a garden to the public – you were all stars. -
New Additions to CASCAT from Carlisle Archives
Cumbria Archive Service CATALOGUE: new additions August 2021 Carlisle Archive Centre The list below comprises additions to CASCAT from Carlisle Archives from 1 January - 31 July 2021. Ref_No Title Description Date BRA British Records Association Nicholas Whitfield of Alston Moor, yeoman to Ranald Whitfield the son and heir of John Conveyance of messuage and Whitfield of Standerholm, Alston BRA/1/2/1 tenement at Clargill, Alston 7 Feb 1579 Moor, gent. Consideration £21 for Moor a messuage and tenement at Clargill currently in the holding of Thomas Archer Thomas Archer of Alston Moor, yeoman to Nicholas Whitfield of Clargill, Alston Moor, consideration £36 13s 4d for a 20 June BRA/1/2/2 Conveyance of a lease messuage and tenement at 1580 Clargill, rent 10s, which Thomas Archer lately had of the grant of Cuthbert Baynbrigg by a deed dated 22 May 1556 Ranold Whitfield son and heir of John Whitfield of Ranaldholme, Cumberland to William Moore of Heshewell, Northumberland, yeoman. Recites obligation Conveyance of messuage and between John Whitfield and one 16 June BRA/1/2/3 tenement at Clargill, customary William Whitfield of the City of 1587 rent 10s Durham, draper unto the said William Moore dated 13 Feb 1579 for his messuage and tenement, yearly rent 10s at Clargill late in the occupation of Nicholas Whitfield Thomas Moore of Clargill, Alston Moor, yeoman to Thomas Stevenson and John Stevenson of Corby Gates, yeoman. Recites Feb 1578 Nicholas Whitfield of Alston Conveyance of messuage and BRA/1/2/4 Moor, yeoman bargained and sold 1 Jun 1616 tenement at Clargill to Raynold Whitfield son of John Whitfield of Randelholme, gent. -
Back Matter (PDF)
PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 309 INDEX TO VOLUME 55 General index unusual crinoid-coral association 301^ Lake District Boreholes Craven inliers, Yorkshire 241-61 Caradoc volcanoes 73-105 Chronostratigraphy Cretoxyrhinidae 111, 117 stratigraphical revision, Windermere Lithostratigraphy crinoid stems, N Devon 161-73 Supergroup 263-85 Localities crinoid-coral association 301-4 Lake District Batholith 16,73,99 Minerals crinoids, Derbiocrinus diversus Wright 205-7 Lake District Boundary Fault 16,100 New Taxa Cristatisporitis matthewsii 140-42 Lancashire Crummock Fault 15 faunal bands in Lower Coal Measures 26, Curvirimula spp. 28-9 GENERAL 27 Dale Barn Syncline 250 unusual crinoid-coral association 3Q1-A Acanthotriletes sp. 140 Dent Fault 257,263,268,279 Legburthwaite graben 91-2 acritarchs 243,305-6 Derbiocrinus diversus Wright 205-7 Leiosphaeridia spp. 157 algae Derbyshire, limestones 62 limestones late Triassic, near York 305-6 Diplichnites 102 foraminifera, algae and corals 287-300 in limestones 43-65,287-300 Diplopodichnus 102 micropalaeontology 43-65 origins of non-haptotypic palynomorphs Dumfries Basin 1,4,15,17 unusual crinoid-coral association 301-4 145,149,155-7 Dumfries Fault 16,17 Lingula 22,24 Alston Block 43-65 Dunbar-Oldhamstock Basin 131,133,139, magmatism, Lake District 73-105 Amphoracrinus gilbertsoni (Phillips 1836) 145,149 Manchester Museum, supplement to 301^1 dykes, Lake District 99 catalogue of fossils in Geology Dept. Anacoracidae 111-12 East Irish Sea Basin 1,4-7,8,10,12,13,14,15, 173-82 apatite -
Complete 230 Fellranger Tick List A
THE LAKE DISTRICT FELLS – PAGE 1 A-F CICERONE Fell name Height Volume Date completed Fell name Height Volume Date completed Allen Crags 784m/2572ft Borrowdale Brock Crags 561m/1841ft Mardale and the Far East Angletarn Pikes 567m/1860ft Mardale and the Far East Broom Fell 511m/1676ft Keswick and the North Ard Crags 581m/1906ft Buttermere Buckbarrow (Corney Fell) 549m/1801ft Coniston Armboth Fell 479m/1572ft Borrowdale Buckbarrow (Wast Water) 430m/1411ft Wasdale Arnison Crag 434m/1424ft Patterdale Calf Crag 537m/1762ft Langdale Arthur’s Pike 533m/1749ft Mardale and the Far East Carl Side 746m/2448ft Keswick and the North Bakestall 673m/2208ft Keswick and the North Carrock Fell 662m/2172ft Keswick and the North Bannerdale Crags 683m/2241ft Keswick and the North Castle Crag 290m/951ft Borrowdale Barf 468m/1535ft Keswick and the North Catbells 451m/1480ft Borrowdale Barrow 456m/1496ft Buttermere Catstycam 890m/2920ft Patterdale Base Brown 646m/2119ft Borrowdale Caudale Moor 764m/2507ft Mardale and the Far East Beda Fell 509m/1670ft Mardale and the Far East Causey Pike 637m/2090ft Buttermere Bell Crags 558m/1831ft Borrowdale Caw 529m/1736ft Coniston Binsey 447m/1467ft Keswick and the North Caw Fell 697m/2287ft Wasdale Birkhouse Moor 718m/2356ft Patterdale Clough Head 726m/2386ft Patterdale Birks 622m/2241ft Patterdale Cold Pike 701m/2300ft Langdale Black Combe 600m/1969ft Coniston Coniston Old Man 803m/2635ft Coniston Black Fell 323m/1060ft Coniston Crag Fell 523m/1716ft Wasdale Blake Fell 573m/1880ft Buttermere Crag Hill 839m/2753ft Buttermere -
Supplementary Information
Heritage Team 4th Floor 100 Parliament Street London SW1A 2BQ T: 020 7211 2018 [email protected] www.gov.uk/dcms 11 November 2016 Dear Ms Bourdin, Thank you for your letter of 17 October requesting further information regarding the nomination of the English Lake District for World Heritage inscription. You have asked for further details concerning proposals for development in the English Lake District and we feel that it would be helpful to preface our response with some explanation of the planning functions and powers of the Lake District National Park Authority, which is the planning authority for the whole of the candidate English Lake District World Heritage site. The English Lake District is an outstanding cultural landscape that has evolved over a long period of time and needs to continue evolving to sustain its future. We have a vibrant community of some 42,000 residents and an economy that is sustained by the key activities of upland hill farming and tourism. These activities inevitably need to develop in order to sustain the local economy and along with other requirements of the Lake District community, they generate planning applications which are determined by the Lake District National Park Authority. UK National Parks have the highest level of planning protection in the UK and the framework for our decision-making is outlined below. BACKGROUND TO THE PLANNING FUNCTION OF UK NATIONAL PARKS UK National Parks were established under the National Parks and Access to the Countryside Act 1949, and amended by the Environment Act 1995, to: conserve and enhance the natural beauty, wildlife and cultural heritage (of the National Parks); and promote opportunities for the understanding and enjoyment of the special qualities (of the National Parks) by the public. -
Physiological Demands of Mountain Running Races
Rodríguez-Marroyo1, J.A. et al.: PHYSIOLOGICAL DEMANDS OF MOUNTAIN... Kinesiology 50(2018) Suppl.1:60-66 PHYSIOLOGICAL DEMANDS OF MOUNTAIN RUNNING RACES Jose A. Rodríguez-Marroyo1, Javier González-Lázaro2,3, Higinio F. Arribas-Cubero3,4, and José G. Villa1 1Department of Physical Education and Sports, Institute of Biomedicine (IBIOMED), University of León, León, Spain 2European University Miguel de Cervantes, Valladolid, Spain 3Castilla y León Mountain Sports, Climbing and Hiking Federation, Valladolid, Spain 4Faculty of Education and Social Work, University of Valladolid, Valladolid, Spain Original scientific paper UDC: 796.61.093.55:612.766.1 Abstract: The aim of this study was to analyze the exercise intensity and competition load (PL) based on heart rate (HR) during different mountain running races. Seven mountain runners participated in this study. They competed in vertical (VR), 10-25 km, 25-45 km and >45 km races. The HR response was measured during the races to calculate the exercise intensity and PL according to the HR at which both the ventilatory (VT) and respiratory compensation threshold (RCT) occurred. The exercise intensity below VT and between VT and RCT increased with mountain running race distance. Likewise, the percentage of racing time spent above RCT decreased when race duration increased. However, the time spent above RCT was similar between races (~50 min). The PL was significantly higher (p<.05) during the longest races (145.0±18.4, 288.8±72.5, 467.3±109.9 and 820.8±147.0 AU in VR, 10-25 km, 25-45 km and >45 km, respectively). The ratio of PL to accumulative altitude gain was similar in all races (~0.16 AU·m-1). -
A Tectonic History of Northwest England
A tectonic history of northwest England FRANK MOSELEY CONTENTS Introduction 56x Caledonian earth movements 562 (A) Skiddaw Slate structures . 562 (B) Borrowdale Volcanic structures . 570 (C) Deformation of the Coniston Limestone and Silurian rocks 574 (D) Comment on Ingleton-Austwick inlier 580 Variscan earth movements. 580 (A) General . 580 (B) Folds 584 (C) Fractures. 587 4 Post Triassic (Alpine) earth movements 589 5 References 59 ° SUMMARY Northwest England has been affected by the generally northerly and could be posthumous Caledonian, Variscan and Alpine orogenies upon a pre,Cambrian basement. The end- no one of which is entirely unrelated to the Silurian structures include early N--S and later others. Each successive phase is partially NE to ~NE folding. dependent on earlier ones, whilst structures The Variscan structures are in part deter- in older rocks became modified by succeeding mined by locations of the older massifs and in events. There is thus an evolutionary structural part they are likely to be posthumous upon sequence, probably originating in a pre- older structures with important N-S and N~. Cambrian basement and extending to the elements. Caledonian wrench faults were present. reactivated, largely with dip slip movement. The Caledonian episodes are subdivided into The more gentle Alpine structures also pre-Borrowdale Volcanic, pre-Caradoc and follow the older trends with a N-s axis of warp end-Silurian phases. The recent suggestions of or tilt and substantial block faulting. The latter a severe pre-Borrowdale volcanic orogeny are was a reactivation of older fault lines and rejected but there is a recognizable angular resulted in uplift of the old north Pennine unconformity at the base of the volcanic rocks. -
Early Christian' Archaeology of Cumbria
Durham E-Theses A reassessment of the early Christian' archaeology of Cumbria O'Sullivan, Deirdre M. How to cite: O'Sullivan, Deirdre M. (1980) A reassessment of the early Christian' archaeology of Cumbria, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/7869/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk Deirdre M. O'Sullivan A reassessment of the Early Christian.' Archaeology of Cumbria ABSTRACT This thesis consists of a survey of events and materia culture in Cumbria for the period-between the withdrawal of Roman troops from Britain circa AD ^10, and the Viking settlement in Cumbria in the tenth century. An attempt has been made to view the archaeological data within the broad framework provided by environmental, historical and onomastic studies. Chapters 1-3 assess the current state of knowledge in these fields in Cumbria, and provide an introduction to the archaeological evidence, presented and discussed in Chapters ^--8, and set out in Appendices 5-10. -
NLCA06 Snowdonia - Page 1 of 12
National Landscape Character 31/03/2014 NLCA06 Snowdonia Eryri – Disgrifiad cryno Dyma fro eang, wledig, uchel, sy’n cyd-ffinio’n fras â Pharc Cenedlaethol Eryri. Ei nodwedd bennaf yw ei mynyddoedd, o ba rai yr Wyddfa yw mynydd uchaf Cymru a Lloegr, yn 3560’ (1085m) o uchder. Mae’r mynyddoedd eraill yn cynnwys y Carneddau a’r Glyderau yn y gogledd, a’r Rhinogydd a Chadair Idris yn y de. Yma ceir llawer o fryndir mwyaf trawiadol y wlad, gan gynnwys pob un o gopaon Cymru sy’n uwch na 3,000 o droedfeddi. Mae llawer o nodweddion rhewlifol, gan gynnwys cribau llymion, cymoedd, clogwyni, llynnoedd (gan gynnwys Llyn Tegid, llyn mwyaf Cymru), corsydd, afonydd a rhaeadrau. Mae natur serth y tir yn gwneud teithio’n anodd, a chyfyngir mwyafrif y prif ffyrdd i waelodion dyffrynnoedd a thros fylchau uchel. Yn ddaearegol, mae’n ardal amrywiol, a fu â rhan bwysig yn natblygiad cynnar gwyddor daeareg. Denodd sylw rhai o sylfaenwyr yr wyddor, gan gynnwys Charles Darwin, a archwiliodd yr ardal ym 1831. Y mae ymhell, fodd bynnag, o fod yn ddim ond anialdir uchel. Am ganrifoedd, bu’r ardal yn arwydd ysbryd a rhyddid y wlad a’i phobl. Sefydlwyd bwrdeistrefi Dolgellau a’r Bala yng nghyfnod annibyniaeth Cymru cyn y goresgyniad Eingl-normanaidd. Felly, hefyd, llawer o aneddiadau llai ond hynafol fel Dinas Mawddwy. O’i ganolfan yn y Bala, dechreuodd y diwygiad Methodistaidd ar waith trawsffurfio Cymru a’r ffordd Gymreig o fyw yn y 18fed ganrif a’r 19eg. Y Gymraeg yw iaith mwyafrif y trigolion heddiw. -
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.