Spring 12 Newsletter
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Jennings Ale Alt
jennings 4 day helvellyn ale trail Grade: Time/effort 5, Navigation 3, Technicality 3 Start: Inn on the Lake, Glenridding GR NY386170 Finish: Inn on the Lake, Glenridding GR NY386170 Distance: 31.2 miles (50.2km) Time: 4 days Height gain: 3016m Maps: OS Landranger 90 (1:50 000), OS Explorer OL 4 ,5,6 & 7 (1:25 000), Harveys' Superwalker (1:25 000) Lakeland Central and Lakeland North, British Mountain Maps Lake District (1:40 000) Over four days this mini expedition will take you from the sublime pastoral delights of some of the Lake District’s most beautiful villages and hamlets and to the top of its best loved summits. On the way round you will be rewarded with stunning views of lakes, tarns, crags and ridges that can only be witnessed by those prepared to put the effort in and tread the fell top paths. The journey begins with a stay at the Inn on the Lake, on the pristine shores of Ullswater and heads for Grasmere and the Travellers Rest via an ancient packhorse route. Then it’s onto the Scafell Hotel in Borrowdale via one of the best viewpoint summits in the Lake District. After that comes an intimate tour of Watendlath and the Armboth Fells. Finally, as a fitting finish, the route tops out with a visit to the lofty summit of Helvellyn and heads back to the Inn on the Lake for a well earned pint of Jennings Cocker Hoop or Cumberland Ale. Greenside building, Helvellyn. jennings 4 day helvellyn ale trail Day 1 - inn on the lake, glenridding - the travellers’rest, grasmere After a night at the Inn on the Lake on the shores of Ullswater the day starts with a brief climb past the beautifully situated Lanty’s Tarn, which was created by the Marshall Family of Patterdale Hall in pre-refrigerator days to supply ice for an underground ‘Cold House’ ready for use in the summer months! It then settles into its rhythm by following the ancient packhorse route around the southern edge of the Helvellyn Range via the high pass at Grisedale Hause. -
Glenridding Common
COMMONMEMBERS’ NEWSGROUND A JOHN MUIR TRUST PUBLICATION SUMMER 2019 Welcome to Glenridding Common In late autumn 2017, following consultation with local and I was taken on as Property Manager following a 23-year role as national stakeholders, we were delighted when the Lake District area ranger with the National Park Authority, while the National Park Authority confirmed that the John Muir Trust employment of Isaac Johnston from Bowness, funded by Ala would take over the management of Glenridding Common, Green, has enabled a young person to gain a full-time position at initially on a three-year lease. the very start of his conservation and land management career. For those unfamiliar with our work, the John Muir Trust is a As you will read in the pages that follow, we have been UK-wide conservation charity dedicated to the experience, extremely busy over the past 18 months. Our work has included protection and repair of wild places. We manage wild land, vital footpath maintenance and repair – again utilising the skills of inspire people of all ages and backgrounds to discover wildness two local footpath workers – the enhancement of England’s most through our John Muir Award initiative, valuable collection of Arctic-alpine and campaign to conserve our plants (generously aided by the Lake wildest places. District Foundation), litter collection To be entrusted with managing and tree planting. Glenridding Common – the first time We have also carried out extensive that the Trust has been directly survey work to establish base-line involved in managing land outside information for a variety of species on this Scotland – is a responsibility that we nationally important upland site. -
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. -
Dove Crags ‘Cirqueform’ and Gasgale Gill Asymmetric Valley, English Lake District, Attributed to Large-Scale RSF of Pre-LGM Origins
Proceedings of theYorkshire Geological Society 2015 Anomalous terrain at Dove Crags ‘cirqueform’ and Gasgale Gill asymmetric valley, English Lake District, attributed to large-scale RSF of pre-LGM origins David Jarman and Peter Wilson slides are grouped thematically, Supporting Information ppt not by order of appearance in the text SI-02 - 04 Lake District RSF distribution, site locations; Northwestern Fells locus; Dove Crags RSF causes* SI-05 - 09 Gasgale Gill valley SI-10 - 21 Dove Crags cirque and slipmass; moraines SI-22 - 24 Hause Crag scar and slipmass SI-25 - 30 Liza Beck cutbank sections, springs, dry channels SI-31 - 35 reconstruction – pre-RSF Gasgale valley, Grasmoor plateau, Whiteside ridge SI-36 - 39 the vicinity – Coledale Hause; Hope Gill; cirque pattern and seeding* SI-40 - 45 comparator sites (Lake District) : Clough Head / Cotley / Robinson / Revelin Crag / Fairfield / Kirk Fell / Whelter Crags SI-46 (Snowdonia) : Pen yr Helgi-du SI-47 - 50 (Highlands / Sweden) : Cobbler / Streap, Karkevagge / Sgurr an Fhuarail / Tullich Hill SI-51 - 52 alternative interpretations – cirque floor rebound* (B an Fhidhleir); parafluvial RSF* (B Buidhe Arnisdale) SI-53 - 54 general diagrams - RSF typology; Lakes RSF:geology; non-exploitation of RSF cavities by glaciers SI-55 - 58 - measures of RSF depth; cataclinal slopes; zone of crush : Beinn Fhada; Norway drill logs SI-59 - 60 Gasgale Gill diagrams - volume calculations – long sections SI-61 - 62 - sequence of events : spatial / temporal SI-63 comparator reconstruction - Clough Head * -
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. -
Blencathra, the Easy Way!
Blencathra, the easy way! If you are capable of walking a few miles uphill and prefer a grass slope to a rocky ridge, then this walk is for you! It involves an ascent of Blease Fell, the wide curve of the fell as seen from above the stone circle at Castlerigg. Climbing Blencathra via Blease Fell is possibly the simplest route to the top. This smooth grassy hill is the western extension of Blencathra and has no knife edge ridges or sheer drops, just a straightforward path to the top. There is a small carpark at the Blencathra Centre. Parking here cuts off the climb from Threlkeld village, making the walk less than 500 metres to the top of Blease Fell. There is a finger post sign at the foot of the climb to set you on your way. Once you have reached the top of Blease Fell, there is a short undulating ridge to the summit, which takes the walk to a total of 2.5 miles. The true top of Blencathra is called Hallsfell Top, the highest point being 868m. There is a glorious view of the surrounding fells - the vale of Keswick an the Helvellyn range. When you reach the top, you have two options. You can retrace your steps and walks back the way you came, making it a round trip of 5 miles. Alternatively (and more importantly, involving a pub) you can walk down to Scales. This down hill stretch is around 2 miles, reaching the White Horse Inn for a pint and maybe a bite to eat. -
Patterdale Hut Meet - Lakes (George Starkey Hut)
HINCKLEY MOUNTAINEERING CLUB Patterdale Hut Meet - Lakes (George Starkey Hut) (+Thurs) Fri-Sun Walking: The hut is a perfect place to begin a huge variety of walks requir- (10th) 11-13 Sep ‘20 ing different levels of experience and strength. Choose from the beauty of GR NY 396160 the falls at Aira Force or the challenges of Striding Edge and Helvellyn. SATNAV CA11 ONL Climbing: Not especially kind to the roadside warrior, but put in the ef- 180 mls from Hinckley (3hrs 30 fort however, and there’s hidden gems (Gowbarrow Crag; Thrangs Crag) mins). M6. Take J. 36 and take the A590/A591 Westbound to Windermere. and for those operating in the upper grades, venues such as Raven Crag, At the mini roundabout, turn right onto the A592, signposted Penrith and Ulls- Dove Crag and Eagle Crag offer a selection of routes from S up to E7. water. This road takes you over Kirk- stone Pass past Brotherswater and Hartsop, to Patterdale. Pass the White MTB: Ullswater Loop from the door? Helvellyn range or High Street via Lion, and school –the hut is on the right The Knott & The Cockpit - both offer a great day out. Upload your photos to our Facebook page Cycling: Kirkstone Pass is just up the road, but from the hut there’s a good route taking in Ullswater, Eamont, Penrith and Greystoke on reason- ably quiet and very scenic roads. BEDS: 20 Mixed in 2 dorms - and we reserve the smaller room for the ladies. Don’t forget your sleeping bag. Additional night is booked for Thurs. -
Ullswater-Canoe-Trail-Leaflet.Pdf
Safety Bridge Pooley The Middle Reaches Glenridding • Always wear adequate buoyancy when canoeing, a personal Pooley Bridge - meaning the hill by The Middle Reaches - Glenridding - meaning the buoyancy aid or life jacket. Canoes/kayaks should be fitted with enough buoyancy to allow them to float in the event of capsizing. the pool or stream, the hill being Dunmallard Howtown on the south shore of the glen overgrown with bracken, Spray decks are recommended for kayaks. on top of which are the remains of an Iron lake is the mid-point of the steamers’ the village at the southern end of Ullswater • Hypothermia kills. Wear adequate clothing for your journey and the time of year. Ullswater is deep and cold for most of the year. Age hill fort. This small village at the northern journey between Glenridding and Ullswater. It owes its existence to Fatalities have occurred when ill equipped. end of Ullswater has a bridge dating back Pooley Bridge. The pier stands on a the presence of the lead mine at Canoe • Be flexible, the wind is the main controlling factor on the lake and to the 16th century where previously there small headland formed by debris Greenside. The mine was worked can make some trips impossible and/or dangerous. Therefore you Trail may need to change your plans. Check the weather forecast before had been a fish trap. A fish market was washed down by Fusedale Beck. A almost continually during its life your trip. It is generally easier to go downwind but you might find it too difficult to paddle back. -
Helvellyn from Thirlmere ROUTE
Helvellyn from Thirlmere At first glance the western side of the Helvellyn range may seem a little dull. They display slopes of a fairly uniform nature which when compared with the likes of Striding Edge and Swirral Edge on the other, eastern side, certainly lack that immediate, 'in your face' drama. Helvellyn though is a big mountain and the two sides of it are an integral part of why it is such a popular mountain. If you are into a total scrambling experience then there is nothing wrong with doing the edges. If on the other hand you want to savour the fantastic view down on to the edges from the summit, and if you just want to walk to get it rather than scramble then there is no finer way of doing it than approaching up the well-graded paths from the Thirlmere side. The three highest peaks of the main ridge can quite comfortably be done by climbing the zig- zags of the Helvellyn Gill Path to Helvellyn's summit. Then descending to Grisedale Tarn taking in Nethermost Pike and Dollywaggon Pike along the way. The best way back is down by Raise Beck, which is a little confined but soon leads down to Dunmail Raise from where you can make use of the permissive path to get back to the start. Grade: Intermediate Start/Finish: Thirlmere (NY316169) Distance: 9.3 miles (15km) Time: 5 hours Height gain: 819m Terrain: Steep stony fellside, summit ridge, scree, tarn, steep narrow gill and forest. Maps: British Mountain Maps, Lake District (1:40 000; OS Explorer OL5, Harveys' Superwalker (1:25 000) Lakeland East. -
Jennings Ale 2Alt
jennings 4 day ambleside ale trail Day 4 - wordsworth hotel, grasmere - inn on the lake, glenridding The final day involves crossing the backbone of the Helvellyn range back to the start at the Inn on the Lake. To do this the route exploits the line taken by an ancient packhorse trail that crosses the ridge at the dip between Dollywaggon Pike and Fairfield. Between these two giants lies a broad depression occupied by the wild waters of Grisedale Tarn; 33m at its deepest point it is reported to hold some of the largest trout found in the Lake District’s high tarns. Either side of the tarn on the western side are a couple of cols. The route over from Grasmere crosses the southern of the two called Grisedale Hause. The approach to Grisedale Hause is short but steep, whilst the descent down the other side along Grisedale is long but at a more moderate angle. The last leg is over the minor subsidiary ridge of Keldas which at the high point of Lanty’s Tarn gives an absolutely stunning view down to Ullswater. 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 2, Technicality 2 a second footbridge over Grisedale Beck. Cross this and Start: Wordsworth Hotel, Grasmere GR NY337074 continue all the way down Grisedale until you reach the road Finish: Inn on the Lake, Glenridding, GR NY386170 head just by Thornhow. Distance: 8.25 miles (13.25km) 4 Turn left at the road head and cross Grisedale Beck by the Time: 5-6 hours bridge. -
Lakeland Haute Route
Lakeland Haute Route One step is what made all the difference. Somewhere between lifting my right foot, swinging it forward and placing it back down in front of me the world changed. The erratic sounds and smells of the towns were replaced by a calming breeze, the rich green views of pastures and the refreshing aroma of the countryside. That one step was on the Walna Scar Road, a man-made bridleway linking the Coniston valley to the Dunnerdale valley in the Lake District. It was the moment we stepped out from day walking into long distance paths; the moment we started to sense the magic of Trail’s Lakeland Haute Route. A month earlier I had been in a pub with Trail’s Jeremy Ashcroft and Matt Swaine, reminiscing about great days on the hills while trying to work out how to celebrate the magazine’s 20th birthday. “When Trail started back in 1990 we definitely did more multi- day backpacking routes,” I said. “Drawing the maps, the challenge was trying to fit on the page because they were so long!” said Jeremy. “Europe’s haute routes are some of the finest,” I said. “Why don’t we create one for the Lake District?” Haute route means ’high route’, and in the Alps they take in the high mountain passes between valleys and give walkers stupendous views of the major peaks. Our Lakeland Haute Route would need to do the same thing, taking advantage of Youth Hostels rather than mountain huts, offering ascents of the big-name Lakeland peaks for those who wanted to tailor their route, and making sure that every night would bring us back to great food and public transport links. -
The Last Glacier in Dovedale, Lake District
ISSN 1476-1580 North West Geography Volume 11, Number 1, 2011 North West Geography, Volume 11, 2011 14 The last glacier in Dovedale, Lake District Peter Wilson Environmental Sciences Research Institute, School of Environmental Sciences, University of Ulster, Coleraine, Northern Ireland Email: [email protected] Abstract Field mapping of moraine ridges and mounds in Dovedale, Lake District, has enabled the reconstruction of a small valley glacier. At its maximum extent the glacier covered an area of 3.39 km2 and had an equilibrium line altitude of ~522 m. The presence of moraines in both the lower and upper parts of the valley suggests that the glacier underwent active retreat. Some of the ‘moraine ridges’ may have resulted from or been enhanced by fluvial erosion of thick drift sheets. Although the age of the moraines has not been determined it is inferred that the glacier developed during the Loch Lomond Stadial (12.9-11.7 ka BP). If this inference is correct the Dovedale glacier was the largest glacier to have developed in the eastern Lake District during this interval, and it probably connected across parts of the drainage divide with glaciers in neighbouring valleys. Key words Moraines, Glacier reconstruction, Loch Lomond Stadial, Lake District. Introduction 2002; Wilson 2002, 2004a), thus extending the total area of Moraine ridges and mounds associated with the last glaciers glacier ice in the LLS. that occupied the cirques and upper reaches of valleys in In some Lake District valleys there are moraines the Lake District of northwest England have been mapped that Sissons (1980) thought were related to stillstands or and their significance discussed on many occasions since readvances of an ice cover that pre-dated the LLS.