The Northern Fells
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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. -
The Lakewalker Guide to Lake District Pubs
web.archive.org https://web.archive.org/web/20050209102131/http://www.miketuer.plus.com/yearly/1998.htm The Lakewalker Guide to Lake District Pubs PUBS 1998 Drink Food Atmo Staf Tot (30) (30) (30) (10) 100 3 Jun 98 Cautley Spout and The Calf Kings Head, Ravenstonedale 22 24 18 8 72 8 Jul 98 Seldom Seen via Heron Pike and Sheffield Pike to Dockray Royal Hotel, Dockray 19 24 18 8 69 8 Apr 98 Harter Fell Haweswater Hotel 19 22 20 7 68 26 Aug 98 Clough Head, then either White Pike, or Calfhow Pike, Great Dodd, Watson's Dodd, Stybarrow Dodd to Sticks Pass. Kings Head, Thirlspot 22 18 20 7 67 12 Aug 98 Braefell, Little Sca Fell, Great Sca Fell, Knott, High Pike Oddfellows Arms, Caldbeck 19 20 20 7 66 9 Sep 98 Blencathra - up Halls Fell and down Gategill Fell Salutation, Threlkeld 16 19 21 8 66 4 Nov 98 Kentmere Horseshoe - Yoke, Ill Bell, Froswick, Thornthwaite Beacon, High Street, Mardale Ill Bell, Harter Fell, Kentmere Pike, Shipman Knotts Watermill, Ings 19 19 21 6 65 24 Jun 98 Grey Knotts, Brandreth, then Base Brown and Green Gable, or Green Gable and Great Gable Dog and Gun, Keswick 16 23 18 6 63 6 May 98 Grasmoor, Whiteless Pike to Buttermere Bridge Inn, Buttermere 21 19 18 4 62 13 May 98 Ullock Pike, Long Side, (Carl Side), Skiddaw Sun Inn, Bassenthwaite 15 17 22 8 62 22 Apr 98 Causey Pike Swinside Inn 18 18 20 5 61 29 Apr 98 Sharp Edge, Blencathra, Blease Fell Salutation, Threlkeld 20 19 16 6 61 15 Apr 98 Burnbank Fell, Blake Fell and Carling Knott Lumplugh Tip 17 19 16 8 60 5 Aug 98 Fleetwith Pike & Haystacks Fish Hotel, Buttermere -
I Love to Challenge Myself
Kim Collison: I love to challenge myself I am passionate about running and off-road in particular. Fell, trail, ultra - all of them. I guess my main passion is mountains. Being out in nature and exploring comes into it too. I am quite competitive. The race element comes right to the fore for me. I love to challenge myself. Kim Collison attempts to summarise his passion for being out in the mountains. I talked to him just after he had set a new winter Bob Graham Round record this December. He went on to explain his background and how he got into his sport, whilst also giving details of that impressive winter effort. Kim Collison is not a native of Cumbria, although he has lived there for a while now. He grew up in Tring, in Hertfordshire, and ended up at Tring Running Club. His father was interested in sports and in running in particular. Kim enjoyed running from a very early age. As a young kid he was always outside playing. At Secondary School, Hemel Hempstead School, he did a bit of cross country, but says he wasn't so good at team games. ‘One year I remember not getting in the school cross country team’, he recalls, ‘and then going on and winning all the PE lesson cross countries the next year. I was that driven and competitive. I didn't stand out at County level or anything mind.’ He was in the Scouts and did a lot of hiking in the mountains. Through this he was learning navigation, being taken to the Lakes and Snowdonia. -
Langdale to Keswick 15 Miles / 24 Km - 6.5 to 7.5 Hours Walking Striding out Along Mickleden Valley
STAGE Langdale to Keswick 15 miles / 24 km - 6.5 to 7.5 hours walking Striding out along Mickleden Valley Latrigg er Greta Riv Braithwaite Castlerigg Portinscale *Stone Circle Keswick Stair Derwent Water Cat Bells Barrow Falls Littletown * This stage gives you a real Look out for ... Lodore* High Seat Falls taste of Lakeland’s rugged Grange Watendlath The distinctively craggy volcanic rock R i and scenic splendour, and of central Lakeland. v e r the walking is consequently Borrowdale harder for a time. Secluded The Stake Pass watershed. Water D Watendlath flows south into Morecambe Bay e Grange Mickleden and Langstrath r Tarn w Fell and north into the Solway Firth. e valleys sandwich this stage’s n t Blea highest point at the top of Fellow explorers on the excellent Rosthwaite Tarn Stake Pass (about 480 Coast to Coast Walk (St Bees to metres). Under the bluff of Robin Hoods Bay) which also goes Gallery Eagle Crag the rough, by Stonethwaite Beck. Force The jetty sometimes wet paths by The more elevated Allerdale Ramble at Hawes End Seatoller * Langstrath and or Cat Bells paths west of Derwent k c Stonethwaite Becks Water. e B converge. The trail follows h t Brandlehow Park on the lakeshore - a r the crystal-clear waters of t the first Lake District property s g the River Derwent as it n acquired by the National Trust in a Britain’s smallest bird L meanders through lovely 1902. of prey, the Merlin flies Borrowdale and finally the low and fast over wooded western shore of remote moorland Derwent Water towards Tips searching for small High birds, lizards Keswick at its northern end. -
Bassenthwaite Lake (English Lake District)
FRESHWATER FORUM VOLUME 25, 2006 Edited by Karen Rouen SPECIAL TOPIC THE ECOLOGY OF BASSENTHWAITE LAKE (ENGLISH LAKE DISTRICT) by Stephen Thackeray, Stephen Maberly and Ian Winfield Published by the Freshwater Biological Association The Ferry House, Far Sawrey, Ambleside, Cumbria LA22 0LP, UK © Freshwater Biological Association 2006 ISSN 0961-4664 CONTENTS Abstract ............................................................................................. 3 Introduction ....................................................................................... 5 Catchment characteristics .................................................................. 7 Physical characteristics of Bassenthwaite Lake ................................ 9 Water chemistry ................................................................................ 16 Phytoplankton .................................................................................... 32 Macrophytes ...................................................................................... 39 Zooplankton ...................................................................................... 48 Benthic invertebrates ......................................................................... 52 Fish populations ................................................................................ 52 Birds .................................................................................................. 60 Mammals ........................................................................................... 61 -
APPLICATIONS of QUANTITATIVE METHODS and CHAOS THEORY in ICHNOLOGY for ANALYSIS of INVERTEBRATE BEHAVIOR and EVOLUTION by James
APPLICATIONS OF QUANTITATIVE METHODS AND CHAOS THEORY IN ICHNOLOGY FOR ANALYSIS OF INVERTEBRATE BEHAVIOR AND EVOLUTION by James Richard Woodson Lehane A dissertation submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Department of Geology and Geophysics The University of Utah August 2014 Copyright © James Richard Woodson Lehane 2014 All Rights Reserved The University of Utah Graduate School STATEMENT OF DISSERTATION APPROVAL The dissertation of James Richard Woodson Lehane has been approved by the following supervisory committee members: Allan A. Ekdale , Chair May 5th, 2014 Date Approved Randall B. Irmis , Member June 6th, 2014 Date Approved Marjorie A. Chan , Member May 5th, 2014 Date Approved Elena A. Cherkaev , Member June 12th, 2014 Date Approved Leif Tapanila , Member June 6th, 2014 Date Approved and by John M. Bartley , Chair/Dean of the Department/College/School of Geology and Geophysics and by David B. Kieda, Dean of The Graduate School. ABSTRACT Trace fossils are the result of animal behaviors, such as burrowing and feeding, recorded in the rock record. Previous research has been mainly on the systematic description of trace fossils and their paleoenvironmental implications, not how animal behaviors have evolved. This study analyzes behavioral evolution using the quantification of a group of trace fossils, termed graphoglyptids. Graphoglyptids are deep marine trace fossils, typically found preserved as casts on the bottom of turbidite beds. The analytical techniques performed on the graphoglyptids include calculating fractal dimension, branching angles, and tortuosity, among other analyses, for each individual trace fossil and were performed on over 400 trace fossils, ranging from the Cambrian to the modem. -
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 -
Landform Studies in Mosedale, Northeastern Lake District: Opportunities for Field Investigations
Field Studies, 10, (2002) 177 - 206 LANDFORM STUDIES IN MOSEDALE, NORTHEASTERN LAKE DISTRICT: OPPORTUNITIES FOR FIELD INVESTIGATIONS RICHARD CLARK Parcey House, Hartsop, Penrith, Cumbria CA11 0NZ AND PETER WILSON School of Environmental Studies, University of Ulster at Coleraine, Cromore Road, Coleraine, Co. Londonderry BT52 1SA, Northern Ireland (e-mail: [email protected]) ABSTRACT Mosedale is part of the valley of the River Caldew in the Skiddaw upland of the northeastern Lake District. It possesses a diverse, interesting and problematic assemblage of landforms and is convenient to Blencathra Field Centre. The landforms result from glacial, periglacial, fluvial and hillslopes processes and, although some of them have been described previously, others have not. Landforms of one time and environment occur adjacent to those of another. The area is a valuable locality for the field teaching and evaluation of upland geomorphology. In this paper, something of the variety of landforms, materials and processes is outlined for each district in turn. That is followed by suggestions for further enquiry about landform development in time and place. Some questions are posed. These should not be thought of as being the only relevant ones that might be asked about the area: they are intended to help set enquiry off. Mosedale offers a challenge to students at all levels and its landforms demonstrate a complexity that is rarely presented in the textbooks. INTRODUCTION Upland areas attract research and teaching in both earth and life sciences. In part, that is for the pleasure in being there and, substantially, for relative freedom of access to such features as landforms, outcrops and habitats, especially in comparison with intensively occupied lowland areas. -
PANORAMA from Gowbarrow Fell (GR407218) 481M
PANORAMA from Gowbarrow Fell (GR407218) 481m PAN ORAMA 1 2 3 Little Mell Fell 4 5 7 8 9 12 6 The 10 11 Hause Ullswater Lowthwaite Great Hagg Meldrum Wood 1 Greystoke Forest 2 CARLISLE 3 Cold Fell 4 Melmerby Fell 5 PENRITH 6 Little Meldrum N 7 Cross Fell 8 Little Dun Fell 9 Great Dun Fell 10 POOLEY BRIDGE 11 Heughscar Hill 12 Mickle Fell E Loadpot Hill Arthur’s Pike Wether Hill 8 9 10 12 Bonscale 11 13 3 Pike Ullswater 4 6 14 5 7 Green Gowbarrow Hallin Fell 15 16 Hill 1 2 Bay Ullswater 1 Swinburn’s Park 2 Ullswater Outward Bound School 3 Swarthbeck Gill 4 Steel Knotts 5 SANDWICK 6 Martindale 7 Winter Crag 8 High Raise 9 Rampsgill Head 10 High Street 11 Thornthwaite Crag E 12 Gray Crag 13 Caudale Moor 14 Beda Head 15 The Nab 16 Rest Dodd S 17 9 10 11 12 13 14 15 16 18 1 3 4 5 6 8 2 7 Place 25 Fell 23 24 Swineside Common 20 21 Knott Fell 19 Dowthwaitehead Grisedale Glenridding Dodd 22 1 Red Screes (summit not in view) 2 Little Hart Crag 3 Dove Crag 4 Hart Crag 5 St Sunday Crag 6 Fairfield 7 Seat Sandal 8 Dollywaggon Pike 9 High Spying How 10 Helvellyn 11 Helvellyn Lower Man 12 White Side 13 Raise 14 Stybarrow Dodd 15 Hart Side 16 Birkett Fell 17 Great Dodd 18 Randerside 19 Arnison Crag 20 Hartsop Above How 21 Birks 22 Birkhouse Moor S 23 Heron Pike 24 Catstycam 25 Sheffield Pike W 8 9 10 11 12 1 6 7 2 3 4 Great Mell Souther Fell 13 Fell Wolf 5 Crags Matterdale Forest 1 Clough Head 2 Lord’s Seat 3 Barf 4 Dodd 5 Lonscale Fell 6 Skiddaw Little Man 7 Skiddaw 8 Blencathra 9 Sharp Edge 10 Bannerdale Crags 11 Bowscale Fell W 12 Carrock Fell 13 MUNGRISDALE N This graphic is an extract from The Near Eastern Fells, volume two in the Lakeland Fellranger series published in April 2008 by Cicerone Press (c) Mark Richards 2008. -
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. -
LOW BECKSIDE FARM Mungrisdale, Cumbria
LOW BECKSIDE FARM mungrisdale, cumbria LOW BECKSIDE FARM MUNGRISDALE, CUMBRIA, CA11 0XR highly regarded upland farm within the lake district national park Traditional farmhouse with four bedrooms Bungalow with three bedrooms Traditional stone barns Extensive modern livestock buildings Lot 1 – Low Beckside Farm set in approx. 195 acres of pasture, plus grazing rights on the common Lot 2 – 209 acres of off lying rough grazing, pasture and woodland IN ALL ABOUT 404 ACRES (163 HECTARES) For sale as a whole or in two lots A66 Trunk Road – 1.6 miles u Keswick – 9 miles u Penrith – 12 miles (All distances are approximate) Savills York Savills Carlisle River House, 17 Museum Street, York, YO1 7DJ 64 Warwick Road, [email protected] Carlisle, CA1 1DR 01904 617831 savills.co.uk Introduction Low Beckside Farm lies to the north of the A66 plantations adds to the amenity aspect of the holding. Across Mungrisdale fell and Bowscale fell. The farm has been in approximately 12 miles west of Penrith and just south of the road is a further 123 acres of permanent pasture plus valuable ELS and HLS Environmental Stewardship Schemes the hamlet of Mungrisdale. The farm has benefited from some rough grazing and woodland. one of which is rolling over on an annual basis. considerable investment in the state of the art livestock building completed in 2017 which was specifically designed Lot 2 comprises approximately 209 acres of pasture and Low Beckside Farm is likely to appeal to commercial farmers for sheep husbandry. The farm in all extends to approximately rough grazing including 29 acres of established woodland as well as lifestyle buyers seeking a manageable sized 404 acres offered for sale in two lots. -
2014 Introduction the Website
KESWICK Mountain Rescue Team A Registered Charity Number 509860 Annual Report 2014 Introduction The website Gategill Fell Venus Griffiths Welcome to the 2014 Annual Report of For more information about the Team, Keswick Mountain Rescue Team. see www.keswickmrt.org.uk This is a record of the Team’s activities in 2013. Please support the Team through the links from the website to The Team operates in the area shown on the map on page 2. The Charities Aid Foundation, JustGiving, JustTextGiving Occasionally the Team is called elsewhere. and (See also pages 30 and 31) Thanks Photographs The painting has been donated by Venus Griffiths. All photographs used in this report The framed original is for sale to the highest bidder. have been contributed by It may be viewed at Derwent Frames, High Hill, Keswick. Keswick Mountain Rescue Team members. All proceeds to Keswick Mountain Rescue Team. Keswick Mountain Rescue Team 2014 President: Mike Nixon MBE Deputy Team Leaders: Paul Barnes, Chris Gillyon, Chairman: Malcolm Miller Chris Harling, Simon Hodgson Secretary: Paul Cheshire Medical Officer: Dr Tim Hooper Treasurer: lan Wallace Training Officers: Gordon Barker, Steve Hepburn Spooney Green House, Radio Officer: Alan Prescott Spooney Green Lane, Vehicles Officers: Matt Eaves, Mick Guy Keswick, Cumbria CA12 4PJ Equipment Officers: Martin Bell, Tom McNally Team Leader: Chris Higgins Base Officer: Simon Noble Committee: Fiona Boyle, Paul Horder Social Secretary: Elly Whiteford Report Editor: Peter Little Secretary (Meetings & Minutes) Steve Allen Handyman