1990 – 1 JAN the Team Travelled to Kendal Stopping Overnight With
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Open Access Newsletter
[Type text] OpenAccess Access Newsletter Newsletter October 2015 Access Fund The first year report on the National Park’s Access Fund is now available at www.peakdistrict.gov.uk/accessfund. This is a ring-fenced fund for access improvements. The report is an annual one. The report shows the contributions received and what they have been spent on in this first year. Interim progress reports on projects which are still ongoing and for new work will be reported to the Local Access Forum. The report also includes quotes from those who have made donations. Their words and deeds best convey the importance of access and how we can care for this special place for the enjoyment and inspiration of all. Peak Paths Appeal The National Park Authority works with landowners to install and maintain access points and paths on access land and takes a leading role in negotiating and maintaining concessionary routes and increasing access rights to create links and improve the network. One of the paths which we help to look after is the one leading to Grindslow Knoll and the Edale skyline. This is a path on access land but an important one and is now quite eroded and has widened. We have already carried out some works to improve the drainage and would like to carry out further works to the surface of the path and the areas adjacent. This will make it easier to walk on and will encourage revegetation. The work will be carried out sensitively in a manner suitable for this location and its use. -
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. -
Yorkshire Painted and Described
Yorkshire Painted And Described Gordon Home Project Gutenberg's Yorkshire Painted And Described, by Gordon Home This eBook is for the use of anyone anywhere at no cost and with almost no restrictions whatsoever. You may copy it, give it away or re-use it under the terms of the Project Gutenberg License included with this eBook or online at www.gutenberg.net Title: Yorkshire Painted And Described Author: Gordon Home Release Date: August 13, 2004 [EBook #9973] Language: English Character set encoding: ASCII *** START OF THIS PROJECT GUTENBERG EBOOK YORKSHIRE PAINTED AND DESCRIBED *** Produced by Ted Garvin, Michael Lockey and PG Distributed Proofreaders. Illustrated HTML file produced by David Widger YORKSHIRE PAINTED AND DESCRIBED BY GORDON HOME Contents CHAPTER I ACROSS THE MOORS FROM PICKERING TO WHITBY CHAPTER II ALONG THE ESK VALLEY CHAPTER III THE COAST FROM WHITBY TO REDCAR CHAPTER IV THE COAST FROM WHITBY TO SCARBOROUGH CHAPTER V Livros Grátis http://www.livrosgratis.com.br Milhares de livros grátis para download. SCARBOROUGH CHAPTER VI WHITBY CHAPTER VII THE CLEVELAND HILLS CHAPTER VIII GUISBOROUGH AND THE SKELTON VALLEY CHAPTER IX FROM PICKERING TO RIEVAULX ABBEY CHAPTER X DESCRIBES THE DALE COUNTRY AS A WHOLE CHAPTER XI RICHMOND CHAPTER XII SWALEDALE CHAPTER XIII WENSLEYDALE CHAPTER XIV RIPON AND FOUNTAINS ABBEY CHAPTER XV KNARESBOROUGH AND HARROGATE CHAPTER XVI WHARFEDALE CHAPTER XVII SKIPTON, MALHAM AND GORDALE CHAPTER XVIII SETTLE AND THE INGLETON FELLS CHAPTER XIX CONCERNING THE WOLDS CHAPTER XX FROM FILEY TO SPURN HEAD CHAPTER XXI BEVERLEY CHAPTER XXII ALONG THE HUMBER CHAPTER XXIII THE DERWENT AND THE HOWARDIAN HILLS CHAPTER XXIV A BRIEF DESCRIPTION OF THE CITY OF YORK CHAPTER XXV THE MANUFACTURING DISTRICT INDEX List of Illustrations 1. -
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 -
Carneddau (Mountains of the Cairns)
Carneddau (Mountains of the Cairns) Reprint of a section of the 1993 guidebook to Ogwen and Carneddau by Iwan Arfon Jones (with Simon Cardy, Geoff Milburn, Andy Newton, Chris Parkin, & Mike Raine) 1993 guide ISBN: 0-901601-52-7 Edited by Ian Smith and Geoff Milburn and typeset by Ian Smith This reprint prepared for web publishing by John Willson Published by The Climbers’ Club The 1993 guide is no longer available. A completely new guide to Ogwen is in advanced stages of preparation, and publication is scheduled for 2009. Work is now also under way on a new Carneddau guide (which will include Crafnant and Dyffryn Conwy). The original route descriptions text for Carneddau is here being made available to bridge the gap. Please note that this is not a supplement or update – the content is completely unmodified. If you have any comments on the route descriptions or any new-route information, please forward it immediately: go to the Climbers’ Club website, click on the ‘Guidebooks in preparation’ tab, and follow the instructions. Good action photos (any format) are also sought. Please submit any you would like to offer for considerationbyfollowingthesameprocedure. www.climbers-club.co.uk 2 3 Contents Introduction Introduction 3 Whosoever ventures into the Carneddau shall certainly realise that they have enteredanarenawhereclimbingsometimes takes second place to enjoyment Cwm Llafar 5 and a feeling for mountains. They shall also find that high crag routes can also Ysgolion Duon 5 be found in North Wales away from Clogwyn Du’r Arddu. Many of the routes are brilliant mountain climbs of high quality and historical value. -
List of Illustrations from Chapter 4, Natural History of Upper Weardale, Geomorphology and Glacial Legacy
List of Illustrations from Chapter 4, Natural History of Upper Weardale, Geomorphology and glacial legacy. by David J A Evans This document provides a larger version of the illustrations for Chapter 4 of the Natural History of Upper Weardale, Geomorphology and Glacial Legacy. By providing this in a PDF format it should be possible to enlarge to some extent and gain a clearer insight. Figure 1: Northern England contour colour coded digital elevation model (DEM) derived from NEXTMap imagery (courtesy of NERC via the Earth Observation Data Centre). The main physiographic areas are highlighted and include the streamlined (drumlin filled) corridors created by fast ice stream flow during glaciations. The fluvial drainage pattern and largely V-shaped valley cross profiles of the North Pennines (Alston Block) are also prominent. (a) (b) Figure 2: Previous reconstructions of the glaciation of the North Pennines: a) the valley-confined style of glaciation of the north Pennines produced by Dwerryhouse (1902). The Stainmore Gap and Tyne Gap ice streams drain the regional, Scottish-nourished ice eastwards and the North Pennines are characterized by the Teesdale, South Tyne and Weardale glaciers. Note the prominent ice-dammed lakes that are depicted along the south edge of Tyne Gap ice but also smaller examples along the margins of the Teesdale and Weardale glaciers; b) a similar depiction of the regional ice by Raistrick and Blackburn (1931), showing what they regarded as a later stage of ice sheet recession. Figure 3: Examples of the lithological -
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. -
Summits Lakeland
OUR PLANET OUR PLANET LAKELAND THE MARKS SUMMITS OF A GLACIER PHOTO Glacially scoured scenery on ridge between Grey Knotts and Brandreth. The mountain scenery Many hillwalkers and mountaineers are familiar The glacial scenery is a product of all these aries between the different lava flows, as well as the ridge east of Blea Rigg. However, if you PHOTO LEFT Solidi!ed lava "ows visible of Britain was carved with key features of glacial erosion such as deep phases occurring repeatedly and affecting the as the natural weaknesses within each lava flow, do have a copy of the BGS geology map, close across the ridge on High Rigg. out by glaciation in the U-shaped valleys, corries and the sharp arêtes that whole area, including the summits and high ridges. to create the hummocky landscape. Seen from the attention to what it reveals about the change from PHOTO RIGHT Peri glacial boulder!eld on often separate adjacent corries (and which provide Glacial ‘scouring’ by ice sheets and large glaciers summit of Great Rigg it is possible to discern the one rock formation to another as you trek along the summit plateau of Scafell Pike. not very distant past. some of the best scrambles in the Lakeland fells, are responsible for a typical Lakeland landscape pattern of lava flows running across the ridgeline. the ridge can help explain some of the larger Paul Gannon looks such as Striding Edge and Sharp Edge). of bumpy summit plateaus and blunt ridges. This Similar landscapes can be found throughout the features and height changes. -
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. -
Mountain Accidents 2015
ISSN 2046-6277 LAKE DISTRICT SEARCH & MOUNTAIN RESCUE ASSOCIATION MOUNTAIN ACCIDENTS 2015 Cambridge Crag and Bowfell from ‘Wainwright’s Southern Fells’ and reproduced by courtesy of the Westmorland Gazette The Lake District Search and Mountain Rescue Association would like to acknowledge the contributions given to this association by all members of the public, public bodies and trusts. In particular, this association gratefully acknowledges the assistance given by Cumbria Constabulary. Contents Introduction ................................................................... 2 Chairman’s Report ........................................................ 3 Incident Details 2015 January ................................................................. 5 February ................................................................ 7 March .................................................................... 12 April ....................................................................... 16 May ....................................................................... 21 June ...................................................................... 26 July ........................................................................ 31 August ................................................................... 35 September ............................................................. 43 October ................................................................. 48 November .............................................................. 54 December ............................................................. -
The Western Fells (646M, 2119Ft) the WESTERN FELLS
Seatoller FR OM Blakeley Raise THE BASE BROWN NORTH Heckbarley FR Honister GREY KNOTTS OM GREEN GABLE GRIKE GREAT GABLE Pass THE LANK RIGG BRANDRETH FLEETWITH PIKE SOUTH CRAG FELL FR OM BUCKBARROW HAYSTACKS THE KIRK FELL EAS IRON CRAG Black Sail Pass Whin Fell MIDDLE FELL FR T Stockdale Scarth Gap Mosser OM HIGH CRAG Hatteringill Head Buttermer THE Moor FELLBARROW W SEATALLAN (801m, 2628ft) (801m, asdale WES YEWBARROW HIGH STILE Smithy Fell CAW FELL e Head PILLAR 12 Green Gable Green 12 T Sourfoot Fell BUCKBARROW LOW FELL RED PIKE (W) Darling Dodd GREA SCOAT FELL F Loweswater G ell ABLE GREEN GABLE HAYCOCK STEEPLE Styhead Crummock T RED PIKE (W) Pass SEATALLAN SCOAT FELL MELLBREAK Oswen Fell MIDDLE FELL Black Crag Wa HAYCOCK BRANDRETH te BR BASE (899m, 2949ft) (899m, r STARLING DODD Burnbank Fell OW PILLAR SCOAT FELL W N LOW FELL Lamplugh ast RED PIKE (W) 11 Great Gable Great 11 Sharp Knott Wa Black Crag CAW FELL GREY KNOTTS te FELLBARR BLAKE FELL r HEN COMB PILLAR KNOCK MURTON Honister GREAT BORNE Fothergill Head Pass HIGH CRAG YEWBARROW OW FLEETWITH PIKE GAVEL FELL Carling Knott MELLBREAK HIGH STILE Looking Stead RED PIKE (B) BLAKE FELL (616m, 2021ft) (616m, Burnbank Fell Floutern Cop STARLING DODD Floutern Pass W asdale KIRK FELL Oswen Fell 10 Great Borne Great 10 GREAT BORNE GREAT BORNE Buttermer Head Ennerdale Gale Fell KNOCK MURTON STARLING DODD Floutern Cop e Beck Head Wa RED PIKE (B) te HEN COMB r HIGH STILE GAVEL FELL GREAT GABLE CRAG FELL HIGH CRAG MELLBREAK Scarth Gap GRIKE Crummock THE (526m, 1726ft) (526m, HAYSTACKS Styhead