BLEA RIGG – View from the Summit
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Mountain Ringlet Survey Squares 2010
MOUNTAIN RINGLET SURVEY SQUARES 2014 – NOTES FOR SURVEYORS ----------------------------------------------------------------------------- Please note: The following relates only to dedicated Mountain Ringlet searches. For casual records please use our website “Sightings” page where possible. Click on sightings report on: www.cumbria-butterflies.org.uk/sightings/ ----------------------------------------------------------------------------- We’d welcome surveys in any of the squares listed below, but are particularly interested in those marked * and +, ie where there have been recent positive sightings well away from known colonies or discovery of possible new colonies. The areas to be surveyed fall into 3 groups, in colour below, but also suffixed (1), (2) or (3) for those with black & white printers etc. 1. Grid squares that have previous positive sightings (shown in red) (1) 2. Grid squares adjacent to the above (shown in blue) (2) 3. Grid squares that are previously unrecorded but may have potential to hold Mountain Ringlet populations (shown in green) (3) The objective of these surveys is to try to determine the geographical spread of some known colonies, but also to survey areas that have suitable geology and which may hold previously unrecorded Mountain Ringlet populations. All the 1-km grid squares listed below lie in the 100-km square: NY AREA 1 - LANGDALE 2608 Martcrag Moor / Stake Pass (2) 2607 (north-east corner only) Part of Martcrag Moor (2) 2806 (northern edge) Raven Crag (1) 2807 Harrison Stickle (1) 2710 (eastern half only) -
Jennings Ale 2Alt
jennings 4 day ambleside ale trail Day 3 - langdale hotel, elterwater - wordsworth hotel, grasmere This is the peak bagging day of the trip. After leaving the Langdale Hotel the route heads out along the old tracks down Langdale to the hotel at the foot of Stickle Gill. From here a fairly stiff climb gives access to the dramatic crag ringed corrie occupied by Stickle Tarn. Unlikely as it might seem standing amongst all the towering crags there is a sneaky route to the surrounding summits from the tarn. It leads in zig-zags to the dip between Harrison Stickle and Pavey Ark from where both peaks can easily be gained. The obvious diagonal line that cuts across the crags of Pavey Ark is Jack’s Rake which is a popular scramble. The rest of the crag provides top quality rock climbs. Having summited these two a big loop takes in Thunacar Knott and Sergeant Man, and then heads down, via Blea Rigg and Easedale Tarn, to the pastoral beauty of Grasmere and the welcome sight of the Wordsworth Hotel where a lovely, refreshing pint of Cumberland Ale awaits you! Before setting off please make sure you plot the suggested route on OS maps and pack a compass. They are essential for a safe, enjoyable day in the hills! Grade: Time/effort 3, Navigation 3, Technicality 3 stunning unrestricted views to the south out over Langdale and Start: Langdale Hotel, Elterwater GR NY326051 towards the giants of the Coniston Fells. The next of the ‘Pikes’ Finish: Wordsworth Hotel, Grasmere GR NY337074 is Thunacar Knott. -
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. -
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. -
The Esker - Pre 2011 Blogs
The Esker - Pre 2011 Blogs The Esker - Festive Races & Other Stuff The First Word A big welcome to all the new members, membership numbers have really boomed in the opening races of the Winter Series good to see your names on the finish sheets. Competitor numbers are up in the races too, not even the truly autumnal weather has put you off. Racing and training safely Please be safe on the hills, so don‟t forget your kit, Rule 9 FRA Handbook states competitors should arrive prepared to carry Windproof whole body cover (or other whole body cover appropriate for the weather conditions), map and compass suitable to navigate the course, whistle and emergency food in the longer races. The winter and summer series races are usually partially marked, but please be prepared to navigate your way to the finish. Dave would always love to hear from anyone who can help out with course marking and clearing, and/or sweeping on the race day, its good training or for easing back steadily from injury. Training and Social Training nights are taking off, 30th November meet 7.00pm lay-by ¼ mile south of Great Broughton, headtorch and winter gear a must, click the link to the Alpkit Gamma headtorch - an effective good value headtorch, though there are many more on the market. Alpkit Gamma headtorch December - 7th and 14th from the High Green Car Park, Great Ayton meet at 7.00pm. The run on the 14th will be followed by our Club Christmas dinner at the Panda Chinese Restaurant in Stokesley at 8.30pm, contact Phil „the chair‟ Conner to book your place. -
Trip Notes ------Believe Achieve Inspire ------Lake District Peaks Challenge Uk
TRIP NOTES ------------------------- BELIEVE ACHIEVE INSPIRE ------------------------- LAKE DISTRICT PEAKS CHALLENGE UK Sat 05 Sep - Sat 05 Sep 2020 OVERVIEW LAKE DISTRICT PEAKS CHALLENGE - UK 2 In aid of your choice of charity 05 Sep - 05 Sep 2020 1 DAYS | UK | CHALLENGING Challenge yourself to take on three, five or · Choose between 3, 5 or 8 peaks in one challenging day! · Summit Scafell Pike, England’s highest mountain EIGHT peaks of the Lake District – and in just · Trek in Greater Langdale, one of the Lake Districts most one day! This is one of the toughest challenges stunning areas · Celebrate with a buffet dinner in a beautiful Lake District that the UK has to offer, putting you through the pub ultimate test of strength, endurance and determination. You will tackle some of England’s most rugged and demanding mountains over a matter of hours. Scafell Pike and Great End will be among the peaks you ascend on this journey through the majestic Lake District. The terrain is extremely varied and involves some very steep ascents and descents so trekkers must be fit and confident. This is a tough challenge which is not for the faint-hearted, but the sense of achievement is immense. +44 (0)20 8346 0500 facebook.com/charitychallenge [email protected] twitter.com/charitychall www.charitychallenge.com ITINERARY LAKE DISTRICT PEAKS CHALLENGE - UK 3 YOUR CHALLENGE DAY BY DAY DAY 1 Sat 05 Sep - The challenge! Pit yourself against one of the toughest challenges that the UK has to offer, as you take on up to eight of the Lake District’s most famous peaks. -
Q9495 the Lake District National Park Suthority Fix the Fells Orders 2013
Order Decision Hearing opened on 12 May 2015 by Heidi Cruickshank BSc (Hons), MSc, MIPROW an Inspector appointed by the Secretary of State for Environment, Food and Rural Affairs Decision date: 7 October 2015 Order Ref: FPS/Q9495/4/46 referred to as ‘Order A’ This Order is made under Section 119 of the Highways Act 1980 and Section 53A(2) of the Wildlife and Countryside Act 1981. It is known as The Lake District National Park Authority (Fix the Fells path 243030/407026, Scale Beck to Red Pike, Parishes of Loweswater and Ennerdale & Kinniside.) Public Path Diversion and Definitive Map and Statement Modification Order 2013. The Order is dated 7 May 2013 and proposes to divert a footpath from the western side of Scale Beck to the east and the continuation towards Red Pike onto a more north- easterly alignment in the vicinity of Lingcomb Edge, as shown in the Order plan and described in the Order Schedule. There was one objection outstanding when the Lake District National Park Authority submitted the Order to the Secretary of State for Environment, Food and Rural Affairs for confirmation. Summary of Decision: The Order is confirmed subject to modifications set out in the Formal Decision. Order Ref: FPS/Q9495/4/47 referred to as ‘Order B’ This Order is made under Section 119 of the Highways Act 1980 and Section 53A(2) of the Wildlife and Countryside Act 1981. It is known as The Lake District National Park Authority (Fix the Fells paths, Burtness to Red Pike summit, parishes of Buttermere & Brackenthwaite and Loweswater) Public Path Diversion and Definitive Map and Statement Modification Order 2013. -
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. -
Axe Working Sites on Path Renewal Schemes, Central Lake District
AXE WORKING SITES ON PATH RENEWAL SCHEMES, CENTRAL LAKE DISTRICT CUMBRIA Archaeological Survey Report Oxford Archaeology North June 2009 The National Trust and Lake District National Park Authority Issue No 2008-2009/903 OAN Job No:L10032 NGR: NY 21390 07921 NY 21891 08551 NY 27514 02410 NY 23676 08230 NY 36361 11654 (all centred) Axe Working Sites on Path Renewal Schemes, Cumbria: Archaeological Survey Report 1 CONTENTS SUMMARY................................................................................................................ 2 ACKNOWLEDGEMENTS ............................................................................................ 3 1. INTRODUCTION ................................................................................................... 4 1.1 Circumstances of the Project......................................................................... 4 1.2 Objectives..................................................................................................... 4 2. METHODOLOGY.................................................................................................. 6 2.1 Project Design .............................................................................................. 6 2.2 The Survey ................................................................................................... 6 2.4 Archive......................................................................................................... 7 3. TOPOGRAPHIC AND HISTORICAL BACKGROUND ................................................ 8 -
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. -
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.