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The Lake District Mountain Trial Association
LDMT 2016 Course Planning Comments Sept 2016 The “Newfield” provided an excellent base for this years event, planning unfamiliar routes away and back to the pub was a challenge, the location of the map handout enabled the position of the 1st controls to provide good route choices, the run in was aptly described as an “adventure trail”. Early stages in the planning had the classic course returning via Hard Knott and Dunnerdale Forest/ Harter Fell but without making it too technical the route would have been rather dull, switching the route to return over Grey Friar then meant avoiding recently erected fences. Creating a loop to the north side Wrynose that gave good route choice without “dog legs” took quite a few attempts, Andy and I agreed that we didn’t want the north side of Blisco to be a favourable option but it was used, as was a route over Blisco’s summit! On the medium course I initially had control 5 in the vicinity of Hell Gill Pike, this would have given more weight to the option of a contouring route to the north of Wetherlam, limits on number of checkpoint officials and no obvious feature for a control resulted in the knoll to the south of Grey Friar being used and hence “dog legging” out of control 4 for some competitors. The short course is always problematic in that you are catering for novices and the elderly at the same time, the roughness of the terrain a particular problem for the elderly, the introduction of a “running assistant” takes away some of the worry but a separate course may have to come. -
Troutal Farm Duddon
High Tilberthwaite Farm Troutal Farm Duddon Troutal Farm Thank you for your interest… In what we think is a great opportunity for the right people to work at Troutal Farm in the coming years with us in the National Trust. Since our current tenants gave notice in September 2018, we’ve been working really hard to look at how farming in balance with nature will continue here and how we will work closely with our new tenants to make a successful partnership for everyone. This farm is in an amazing part of the Lake District that is loved by millions – the area is so special that, in 2017, the Lake District became a World Heritage Site as a Cultural Landscape – in no small part due to the way in which people have interacted with and been influenced by the landscape over hundreds of years. Farming has been one of the key elements of this and we are working to help it continue. It’s a time of real change and uncertainty at the moment as Brexit looms and the future is unclear – but we believe that it is also a time of opportunity for you and for us. We are really clear that we want a successful farming enterprise here that also helps us meet our national strategy, our ambition for the land – a shared purpose for the countryside. We know that we can achieve this by working together – through the period of change and uncertainty and beyond into what we hope will be a strong long term relationship. Thank you again for your interest in Troutal Farm. -
The Lakes Tour 2015
A survey of the status of the lakes of the English Lake District: The Lakes Tour 2015 S.C. Maberly, M.M. De Ville, S.J. Thackeray, D. Ciar, M. Clarke, J.M. Fletcher, J.B. James, P. Keenan, E.B. Mackay, M. Patel, B. Tanna, I.J. Winfield Lake Ecosystems Group and Analytical Chemistry Centre for Ecology & Hydrology, Lancaster UK & K. Bell, R. Clark, A. Jackson, J. Muir, P. Ramsden, J. Thompson, H. Titterington, P. Webb Environment Agency North-West Region, North Area History & geography of the Lakes Tour °Started by FBA in an ad hoc way: some data from 1950s, 1960s & 1970s °FBA 1984 ‘Tour’ first nearly- standardised tour (but no data on Chl a & patchy Secchi depth) °Subsequent standardised Tours by IFE/CEH/EA in 1991, 1995, 2000, 2005, 2010 and most recently 2015 Seven lakes in the fortnightly CEH long-term monitoring programme The additional thirteen lakes in the Lakes Tour What the tour involves… ° 20 lake basins ° Four visits per year (Jan, Apr, Jul and Oct) ° Standardised measurements: - Profiles of temperature and oxygen - Secchi depth - pH, alkalinity and major anions and cations - Plant nutrients (TP, SRP, nitrate, ammonium, silicate) - Phytoplankton chlorophyll a, abundance & species composition - Zooplankton abundance and species composition ° Since 2010 - heavy metals - micro-organics (pesticides & herbicides) - review of fish populations Wastwater Ennerdale Water Buttermere Brothers Water Thirlmere Haweswater Crummock Water Coniston Water North Basin of Ullswater Derwent Water Windermere Rydal Water South Basin of Windermere Bassenthwaite Lake Grasmere Loweswater Loughrigg Tarn Esthwaite Water Elterwater Blelham Tarn Variable geology- variable lakes Variable lake morphometry & chemistry Lake volume (Mm 3) Max or mean depth (m) Mean retention time (day) Alkalinity (mequiv m3) Exploiting the spatial patterns across lakes for science Photo I.J. -
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 -
A Survey of the Lakes of the English Lake District: the Lakes Tour 2010
Report Maberly, S.C.; De Ville, M.M.; Thackeray, S.J.; Feuchtmayr, H.; Fletcher, J.M.; James, J.B.; Kelly, J.L.; Vincent, C.D.; Winfield, I.J.; Newton, A.; Atkinson, D.; Croft, A.; Drew, H.; Saag, M.; Taylor, S.; Titterington, H.. 2011 A survey of the lakes of the English Lake District: The Lakes Tour 2010. NERC/Centre for Ecology & Hydrology, 137pp. (CEH Project Number: C04357) (Unpublished) Copyright © 2011, NERC/Centre for Ecology & Hydrology This version available at http://nora.nerc.ac.uk/14563 NERC has developed NORA to enable users to access research outputs wholly or partially funded by NERC. Copyright and other rights for material on this site are retained by the authors and/or other rights owners. Users should read the terms and conditions of use of this material at http://nora.nerc.ac.uk/policies.html#access This report is an official document prepared under contract between the customer and the Natural Environment Research Council. It should not be quoted without the permission of both the Centre for Ecology and Hydrology and the customer. Contact CEH NORA team at [email protected] The NERC and CEH trade marks and logos (‘the Trademarks’) are registered trademarks of NERC in the UK and other countries, and may not be used without the prior written consent of the Trademark owner. A survey of the lakes of the English Lake District: The Lakes Tour 2010 S.C. Maberly, M.M. De Ville, S.J. Thackeray, H. Feuchtmayr, J.M. Fletcher, J.B. James, J.L. Kelly, C.D. -
Duddon Valley - Eskdale Drive
Coniston - Duddon Valley - Eskdale drive A drive that includes the most challenging mountain pass roads in the Lake District along with some remote and beautiful scenery. The drive also visits a number of historic attractions and allows a glimpse of bygone industry in the area. Eskdale Railway, Dalegarth Route Map Summary of main attractions on route (click on name for detail) Distance Attraction Car Park Coordinates 0 miles Coniston Village N 54.36892, W 3.07347 0.8 miles Coniston Water N 54.36460, W 3.06779 10.5 miles Broughton in Furness N 54.27781, W 3.21128 11.8 miles Duddon Iron Furnace N 54.28424, W 3.23474 14.5 miles Duddon Valley access area N 54.31561, W 3.23108 21.7 miles Forge Bridge access area N 54.38395, W 3.31215 23.7 miles Stanley Force waterfall N 54.39141, W 3.27796 24.1 miles Eskdale Railway & Boot N 54.39505, W 3.27460 27.5 miles Hardknott Roman Fort N 54.40241, W 3.20163 28.2 miles Hardknott Pass N 54.40290, W 3.18488 31.6 miles Wrynose Pass N 54.41495, W 3.11520 39.4 miles Tilberthwaite access area N 54.39972, W 3.07000 42.0 miles Coniston Village N 54.36892, W 3.07347 The Drive Distance: 0 miles Location: Coniston Village car park Coordinates: N 54.36892, W 3.07347 The village of Coniston is in a picturesque location between Coniston Water and The Old Man of Coniston, the mountain directly behind. The village has a few tourist shops, cafes, pubs and access to some great walking country. -
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. -
The Heart of Lakeland
TOUR 21 The Heart of Lakeland Leave the soft red sandstones of Carlisle and the Eden Valley to weave through hills of volcanic rocks and lakes carved out during the last Ice Age, before heading into the Pennines, with their different, gentler beauty. ITINERARY CARLISLE Ǡ Caldbeck (13m-21km) GRASMERE Ǡ Ambleside (4m-6.5km) CALDBECK Ǡ Bassenthwaite AMBLESIDE Ǡ Coniston (7m-11km) (9m-14.5km) CONISTON Ǡ Bowness (10m-16km) BASSENTHWAITE Ǡ Buttermere BOWNESS Ǡ Patterdale (13m-21km) (20m-32km) PATTERDALE Ǡ Penrith (14m-23km) BUTTERMERE Ǡ Keswick (13m-21km) PENRITH Ǡ Haltwhistle (34m-55km) KESWICK Ǡ Grasmere (15m-24km) HALTWHISTLE Ǡ Carlisle (23m-37km) 2 DAYS ¼ 175 MILES ¼ 282KM GLASGOW Birdoswald hing Irt Hadrian's ENGLAND B6318 Wall HOUSESTEADS A6 A69 A 07 Greenhead 7 1 4 9 Haltwhistle Ede A6 n Brampton 11 A 9 6 A6 8 9 CARLISLE Jct 43 Knarsdale 5 9 9 9 Eden 5 2 A Slaggyford S A 5 6 A Tyne B 6 8 Dalston 9 South Tynedale A689 Railway B Alston 53 Welton Pe 05 t te r i B l 52 M 99 6 Caldbeck Eden Ostrich A Uldale 1 World Melmerby 59 6 1 A w 8 6 6 A B5291 2 lde Ca Langwathby Cockermouth Bassenthwaite Penrith A Bassenthwaite 10 A A6 66 6 Lake 6 6 931m Wh A A66 inla 5 Skiddaw Pas tte 91 M Brougham Castle Low s r 2 6 66 9 A 2 5 6 2 Lorton A A B5292 3 4 5 Aira B B 5 Force L 2 Keswick o 8 Derwent Ullswater w 9 t Crummock Water e h l e Water a Glenridding r Buttermere d Thirlmere w o Patterdale 3 r 950m Buttermere r o Helvellyn 9 B Honister A 5 Pass 9 Rydal Kirkstone 1 5 Mount Pass Haweswater A Grasmere 5 9 2 Ambleside Stagshaw 6 Lake District National 3 59 Park Visitor Centre A Hawkshead Windermere Coniston 85 B52 8 7 0 10 miles Bowness-on-Windermere Near Sawrey 0 16 km Coniston Windermere 114 Water _ Carlisle Visitor Centre, Old Town Leave Bassenthwaite on Crummock Water, Buttermere Hall, Green Market, Carlisle unclassified roads towards the B5291 round the northern E Keswick, Cumbria Take the B5299 south from shores of the lake, then take The capital of the northern Lake Carlisle to Caldbeck. -
Back Matter (PDF)
Index Note: Page numbers in italic type refer to illustrations; those in bold type refer to tables. Acadian Orogeny 147, 149 Cambrian-Silurian boundary. 45 occurrence of Skiddaw Slates 209 application to England 149 correspondence 43 thrusting 212 cause of 241 Green on 82 topography 78 cleavage 206,240 Hollows Farm 124 Black Combe sheet 130 deformation 207,210,225,237 Llandovery 46 black lead see graphite and granites 295 maps 40-41 Blackie, Robert 176 and lapetus closure 241,294 portrait 40 Blake Fell Mudstones 55 Westmorland Monocline 233,294 section Plate IV Blakefell Mudstone 115 accessory minerals 96 on unconformity below Coniston Limestone Series 83 Blea Crag 75 accretionary prism model 144, 148, 238 Bleaberry Fell 46 accretionary wedge, Southern Uplands 166, 237 Backside Beck 59.70. 174 Bleawath Formation 276,281 Acidispus 30 backthrusts 225,233,241. 295 Blencathra 162 Acritarchs Bad Step Tuff 218, 220 see also Saddleback Bitter Beck 118 Bailey, Edward B. 85, 196 Blengdale 276 Calder River 198 Bakewell, Robert 7,10 Blisco Formation 228 Caradoc 151 Bala Group 60, 82 Boardman, John 266, 269 Charles Downie on 137 Bala Limestone Bohemian rocks, section by Marr 60 Holehouse Gill 169, 211,221,223 Caradoc 21 Bolton Head Farm 276 Llanvirn 133 and Coniston Limestone 19.22, 23.30 Bolton. John 24, 263 Troutbeck 205 and lreleth Limestone 30 Bonney, Thomas 59 zones 119 Middle Cambrian 61 boreholes 55 Actonian 173, 179 Upper Cambrian 20 Nirex 273 Agassiz, Louis 255,257 Bala unconformity 82, 83.85 pumping tests 283, 286 Agnostus rnorei 29 Ballantrae complex 143 Wensleydale 154 Aik Beck 133 Balmae Beds 36 Borrowdale 9, 212,222 Airy, George 9 Baltica 146, 147, 240. -
Why Did the Lake District Need Another Man-Made Lake? the Short Answer Is the Industrial Revolution
Viewpoint Fancy a brew? Time: 15 mins Region: North West England Landscape: Rural Location: Eastern shore of Thirlmere, Cumbria, CA 12 4TW Grid reference: NY 32172 14921 Getting there: Approximately 2.2 miles south of the ‘St John’s in the Vale’ turn-off, stop at the lay-by on the west side of the A591 between Grasmere and Keswick near a castle-shaped building. Keep an eye out for: The castle like red brick building by the water’s edge was built to filter the lake water before it enters the aqueduct. Looking at this body of water between Keswick to the north and Grasmere to the south, you might not realise that unlike most of the other natural lakes that give the Lake District its name, Thirlmere is artificial. This lake is in fact a reservoir – a purpose built space to store water. Why did the Lake District need another man-made lake? The short answer is the Industrial Revolution. In the late nineteenth century, the city of Manchester was booming. Increasing volumes of water were needed to power its mills and factories and to supply the growing population of city workers with a clean supply of water. The existing water source (Longdendale in Derbyshire) would soon be exhausted so another supply was needed. Originally Ullswater was earmarked, but the hard rock surrounding Ullswater on all sides would have meant pumping or boring through miles of rock. So why Thirlmere? The Thirlmere valley was chosen for the new reservoir as it is long, has a relatively flat bottom and is flanked by some of the highest peaks in England including Helvellyn and Dunmill Raise. -
Thirlmere - Blencathra from Sosgill Bridge ©Andrew Locking ©Andrew Bridge Sosgill from Blencathra - Thirlmere
Thirlmere - Blencathra from Sosgill Bridge©Andrew Locking Thirlmere Although relatively small in size, the Today, it is the physical aspects of the thirsty, fast-growing urban population valley of Thirlmere, formerly known water industry that stand out in the in Manchester, and the dam was built. as Wythburn, is dominated by its large main valley. The Thirlmere reservoir Today, United Utilities owns 4,700 reservoir and its looming, steep-sided is the most obvious of these but the hectares of land in the Thirlmere Valley fells. The bulk of Hellvellyn hangs dam infrastructure itself is considered and the reservoir continues to supply impressively over its eastern edge with to be of historic value. It was the first around 11% of the water demand of the mighty Skiddaw and Blencathra ever masonry gravity dam and one of the North West of England. to the north. Dunmail Raise to the only two arch dams in England and it south of Thirlmere is considered to be supplies Manchester with water via a But despite the defeat, the battle was the boundary between the north and 96-mile long underground aqueduct. a significant moment in the history south Lake District. The famous cairn Other industries to impact Thirlmere of the conservation movement, both at the summit of Dunmail Raise is said were copper and lead mining as well as in the UK and globally. It inspired the to be the burial place of King Dunmail, slate quarrying. formation of the National Trust and it the last monarch of the medieval brought to a head the appreciation of kingdom of Cumbria, dating to around Thirlmere’s history tells the story of the vulnerability of the Lake District 945AD. -
Southern Lake District Wainwright Bagging Holiday - the Southern Fells
Southern Lake District Wainwright Bagging Holiday - the Southern Fells Tour Style: Challenge Walks Destinations: Lake District & England Trip code: CNWAT Trip Walking Grade: 6 HOLIDAY OVERVIEW “All Lakeland is exquisitely beautiful, the Southern Fells just happen to be a bit of heaven fallen upon the earth” said Wainwright. The Southern Fells area of the Lake District is centred between the Langdale Valley to the north, Wastwater to the northwest, and Coniston village and Ambleside to the northeast, and includes England’s highest mountain, Scafell Pike. Within this area the fells are the highest and grandest in Lakeland, and make for a marvellous week of mountain walking. During the week we will ascend 28 of the 30 Wainwright Southern Fells which feature in Wainwright’s "A pictorial guide to the Lakeland fells, Book 4". As well as ascending the fells, the delightful valleys leading to them offer charming approaches and contrast to the rugged heights of the fells. WHAT'S INCLUDED • Great value: all prices include Full Board en-suite accommodation, a full programme of walks with all transport to and from the walks, and evening activities • Great walking: enjoy the challenge of bagging the summits in Wainwright’s Southern Fells Pictorial Guide, www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 accompanied by an experienced leader • Accommodation: enjoy comfortable en-suite rooms at the beautiful National Trust property, Monk Coniston, overlooking Coniston Water HOLIDAYS HIGHLIGHTS • Follow in the footsteps of Alfred Wainwright exploring some of his favourite fells • Bag the summits in his Southern Fells Pictorial Guide • Enjoy challenging walking and a fantastic sense of achievement • Head out on guided walks to discover the varied beauty of the South Lakes on foot • Let our experienced leaders bring classic routes and hidden gems to life • After each walk enjoy fantastic accommodation at Monk Coniston which is beautifully located on the shores of Coniston Water; oozing history and all the home comforts needed after a day adventuring.