The Journal of the Fell & Rock Climbing Club
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Road Biking Guide
SUGGESTED ITINERARIES QUICK TIP: Ride your bike before 10 a.m. and after 5 p.m. to avoid traffic congestion. ARK JASPER NATIONAL P SHORT RIDES HALF DAY PYRAMID LAKE (MAP A) - Take the beautiful ride THE FALLS LOOP (MAP A) - Head south on the ROAD BIKING to Pyramid Lake with stunning views of Pyramid famous Icefields Parkway. Take a right onto the Mountain at the top. Distance: 14 km return. 93A and head for Athabasca Falls. Loop back north GUIDE Elevation gain: 100 m. onto Highway 93 and enjoy the views back home. Distance: 63 km return. Elevation gain: 210 m. WHISTLERS ROAD (MAP A) - Work up a sweat with a short but swift 8 km climb up to the base MARMOT ROAD (MAP A) - Head south on the of the Jasper Skytram. Go for a ride up the tram famous Icefields Parkway, take a right onto 93A and or just turn back and go for a quick rip down to head uphill until you reach the Marmot Road. Take a town. Distance: 16.5 km return. right up this road to the base of the ski hill then turn Elevation gain: 210 m. back and enjoy the cruise home. Distance: 38 km. Elevation gain: 603 m. FULL DAY MALIGNE ROAD (MAP A) - From town, head east on Highway 16 for the Moberly Bridge, then follow the signs for Maligne Lake Road. Gear down and get ready to roll 32 km to spectacular Maligne Lake. Once at the top, take in the view and prepare to turn back and rip home. -
Eiger Bike Challenge 22 Km Holzmatten – Bort – Unterer Lauchbühl Grosse Scheidegg – First Waldspitz – Aellfluh Einfache Dorfrunde Grindelwald Rules of Conduct
Verhaltensregeln IG Bergvelo Eiger Bike Challenge 55 km Eiger Bike Challenge 22 km Holzmatten – Bort – Unterer Lauchbühl Grosse Scheidegg – First Waldspitz – Aellfluh Einfache Dorfrunde Grindelwald Rules of Conduct Grosse First Holzmatten Bort Holzmatten Grosse Scheidegg First Waldspitz Befahre nur bestehende Wege und respektiere vorhandene Sperrungen. 1690 Unterer Bort Scheidegg 2184 1565 Wetterhorn Terrassenweg Oberhaus Wetterhorn 1690 1964 2184 Oberhaus 1904 Terrassenweg Stählisboden 1964 Holenwang Oberhalb Bort Lauchbühl 1565 Nodhalten Nodhalten Grindelwald Bussalp 1226 Grindelwald Grindelwald 1140 1355 1226 Grindelwald 1548 1644 1355 1675 1675 Grindelwald Anggistalden 1140 1182 Kirche Gletscher- Grindelwald Meide die Trails nach Regenfällen und möglichst das Blockieren der Räder Grindelwald 1455 Grindelwald 2200 1036 1791 Oberhaus 1036 1036 1036 Wetterhorn Grindelwald Grindelwald Grindelwald Holenwang Aellfluh Grindelwald 1036 1038 schlucht 1036 Holenwang 1355 1036 1226 1036 2200 1036 1036 1036 1548 1430 1036 2000 beim Bremsen – dies begünstigt die Erosion. Bergwege sind keine Renn- 1548 Gletscher- 2000 1800 Wetterhorn schlucht 1800 1800 1800 strecken, darum fahre auf Sicht und rechne mit Hindernissen und anderen 1600 1226 Gletscher- schlucht 1600 1600 1600 1400 1400 1400 1400 1400 Nutzern auf den Wegen. Hinterlasse keine Abfälle. 1200 1200 1200 1200 1200 1200 1000 1000 1000 Only ride on existing trails and respect closures. Avoid using the trails after 1000 1000 1000 0202 5 10 152530 35 40 45 50 55 km 0 2 4 6 81810 12 1416 20 22 km 0122 4 6 81810 1416 20 22 24 km 0122 4 6 81810 1416 20 22 26 km 061 2 3 495 7128 1011 1314 15 16 17 19 km 061 2 3 495 7128 1011 13 14.5 km rainfall and wheel blockage when braking (to stop erosion). -
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. -
2010 Club Experience - Cheap Weekend Walking Breaks Enjoy the High Pennines, Hadrian’S Wall & Durham on Our Annual Short Summer Break
“Outdoor activities for all” 2010 Club Experience - Cheap Weekend Walking Breaks Enjoy the High Pennines, Hadrian’s Wall & Durham on our annual Short Summer Break Thursday 1st to Monday 5th July 2010 John Hillaby’s Journey through Britain: “No botanical name-dropping, can give an adequate impression of the botanical jewels sprinkled on the ground above High Force. In this valley, a tundra has been marvellously preserved; the glint of colour, the reds, deep purples, and blues have the quality of Chartres glass.” High Force Booking Information & Form High England – Hadrian’s Wall and The North Pennines, a designated Area of Outstanding Natural Beauty, for much of its history a wild and dangerous frontier zone until the union of the crowns in 1603 largely ended centuries of war with Scotland. Today, it is sadly an area often overlooked by walkers as we head further north to the mountains of Scotland or to the Lake District. On our Club Experience summer short breaks we seek remoteness, the lure of hills, trails and paths to suit all abilities, places of culture and history and a destination that can enable us to escape for a short while from the stress of work and enjoy the social fun and community we all crave. Blackton Grange www.blacktongrangefarmhouse.com I promise will surprise - surrounded by rolling uplands, quiet lanes, dry stone walls and scenic reservoirs it is the perfect destination to escape the hustle and bustle and enjoy a relaxing break, with the comforts of home in a spectacular setting. This great venue can sleep up to 45 persons, but for our club experience long weekend the maximum number accommodated will be 28 persons, giving us a minimum of 6 double/twin rooms available and no more than four persons will share the other spacious bedrooms (these shared rooms will be allocated on a single sex basis unless booked by couples or friends who may wish to share). -
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. -
A Hydrographic Approach to the Alps
• • 330 A HYDROGRAPHIC APPROACH TO THE ALPS A HYDROGRAPHIC APPROACH TO THE ALPS • • • PART III BY E. CODDINGTON SUB-SYSTEMS OF (ADRIATIC .W. NORTH SEA] BASIC SYSTEM ' • HIS is the only Basic System whose watershed does not penetrate beyond the Alps, so it is immaterial whether it be traced·from W. to E. as [Adriatic .w. North Sea], or from E. toW. as [North Sea . w. Adriatic]. The Basic Watershed, which also answers to the title [Po ~ w. Rhine], is short arid for purposes of practical convenience scarcely requires subdivision, but the distinction between the Aar basin (actually Reuss, and Limmat) and that of the Rhine itself, is of too great significance to be overlooked, to say nothing of the magnitude and importance of the Major Branch System involved. This gives two Basic Sections of very unequal dimensions, but the ., Alps being of natural origin cannot be expected to fall into more or less equal com partments. Two rather less unbalanced sections could be obtained by differentiating Ticino.- and Adda-drainage on the Po-side, but this would exhibit both hydrographic and Alpine inferiority. (1) BASIC SECTION SYSTEM (Po .W. AAR]. This System happens to be synonymous with (Po .w. Reuss] and with [Ticino .w. Reuss]. · The Watershed From .Wyttenwasserstock (E) the Basic Watershed runs generally E.N.E. to the Hiihnerstock, Passo Cavanna, Pizzo Luceridro, St. Gotthard Pass, and Pizzo Centrale; thence S.E. to the Giubing and Unteralp Pass, and finally E.N.E., to end in the otherwise not very notable Piz Alv .1 Offshoot in the Po ( Ticino) basin A spur runs W.S.W. -
Stevie Haston Aleš Česen Malcolm Bass Tom Ballard Steve Skelton F.Lli Franchini Korra Pesce
# 33 Stile Alpino Luoghi & Montagne MONTE BIANCO BHAGIRATHI III CIVETTA KISHTWAR SHIVLING GASHERBRUM IV HIMALAYA MALTA TAULLIRAJU Protagonisti STEVIE HASTON ALEš ČESEN MALCOLM BASS TOM BALLARD STEVE SKELTON F.LLI FRANCHINI KORRA PESCE Speciale PILASTRO ROSSO DEL BROUILLARD In collaborazione con: ALPINE STUDIO EDITORE Trimestrale anno VIII n° 33 settembre 2016 (n. 3/2016) € 4,90 La giacca più leggera e impermeabile del momento LIGHTWEIGHT WITHOUT COMPROMISE MINIMUS 777 JACKET Con un peso di soli 139g, la Minimus 777 è una giacca per Alpinismo e da Trail di una leggerezza estrema, con 3 strati impermeabili, una traspirabilità elevata e una comprimibilità senza precedenti. Pertex® Shield + exclusive technology: 7 denier face, 7 micron membrane, 7 denier tricot backer montane.eu La giacca più leggera e EDITORIAL # 33 impermeabile del momento • Firstly I would like to openly admit that I do not really like to write about or com- ment on other peoples mountaineering endeavors, because it is impossible to comple- tely understand an experience in the mountains unless you have lived it yourself. Ten years after my predecessor I will have the difficult task to replace Fabio Palma in writing the editorials of Stile Alpino. Certainly he is better skilled than me in writing and has been one of the creators of this magazine founded by the Ragni di Lecco group. Nonetheless, I will try to be up to the job helping to select the last ascents around the world and to suggest new places but always taking care to include ascents in the Alps and close to home. The objective of Stile Alpino is to improve and steadily grow in order to publish ar- ticles, that might not have been published before, on ascents in unknown or known areas. -
19. South Cumbria Low Fells Area Profile: Supporting Documents
National Character 19. South Cumbria Low Fells Area profile: Supporting documents www.gov.uk/natural-england 1 National Character 19. South Cumbria Low Fells Area profile: Supporting documents Introduction National Character Areas map As part of Natural England’s responsibilities as set out in the Natural Environment White Paper 1, Biodiversity 20202 and the European Landscape Convention3, we are revising profiles for England’s 159 National Character Areas (NCAs). These are North areas that share similar landscape characteristics, and which follow natural lines East in the landscape rather than administrative boundaries, making them a good decision-making framework for the natural environment. Yorkshire & The North Humber NCA profiles are guidance documents which can help communities to inform West their decision-making about the places that they live in and care for. The information they contain will support the planning of conservation initiatives at a East landscape scale, inform the delivery of Nature Improvement Areas and encourage Midlands broader partnership working through Local Nature Partnerships. The profiles will West also help to inform choices about how land is managed and can change. Midlands East of Each profile includes a description of the natural and cultural features that shape England our landscapes, how the landscape has changed over time, the current key drivers for ongoing change, and a broad analysis of each area’s characteristics London and ecosystem services. Statements of Environmental Opportunity (SEOs) are South East suggested, which draw on this integrated information. The SEOs offer guidance South West on the critical issues, which could help to achieve sustainable growth and a more secure environmental future. -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
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. -
Appleby & Dufton
Vol: 31 Issue 5 7th May 2017 APPLEBY & DUFTON Coach leaves Appleby at 5.00pm and Dufton at 5.30pm. The first drop-off stop will be Black Bull PROGRAMME OF EVENTS May 2017 11 May Thursday Car – Yarrow Valley 10.30am start - Sat Nav: PR7 3QL Map Ref: GR570153 B: Allan Benson Meet at Birkacre Visitor Centre 17 May Stroller – Longton 10.30am start - Sat Nav: PR4 5HA S: Joan & Allan Meet at the Rams Head car park, then Rams Head Pub 21 May Sunday Car B: Tockholes 10.30am start - Sat Nav: BB3 0PA Dorothy Dobson Meet at Tockholes Information Centre car park C: Edgworth Reservoirs 10.30am start - Sat Nav: BL7 0AP Map Ref: GR 742166 Margaret & Bob Meet c.park behind "The Barlow" Building next door to cricket club June 2017 4 June Coach – Great Langdale 8.00am start – Return 5.30pm – first drop-off Black Bull A: Crinkle Crags & Bowfell Leader : Dave Colbert B+: Stickle Tarn Leader: Val Walmsley B: Lingmoor Fell Leader: Colin Manning C: Elterwater Circular Leader: Joyce Bradbury Thursday Car – Yarrow Valley – 11 May 8 miles (12.9km) with no significant climbing Leader: Allan Benson Meet at Birkacre Visitor Centre (Sat Nav: PR7 3QL Map Ref: GR570153), ready for the usual start time of 10.30am. We start our walk from the country park and follow the River Yarrow through Saunders Bank and Big Wood to Duxbury Park. We then follow the Leeds Liverpool Canal for approximat ely 2 miles before making our way back to Yarrow Park via Sandy Lane, footpaths and some quiet roads. -
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.