THE SCENIC HIGHLIGHTS of the PENNINE WAY Discover the True Spirit of the North on England’S Original National Trail

Total Page:16

File Type:pdf, Size:1020Kb

THE SCENIC HIGHLIGHTS of the PENNINE WAY Discover the True Spirit of the North on England’S Original National Trail ENGLAND’S GREAT WALKING TRAILS | THE PENNINE WAY LIMESTONE AND LEGEND: THE SCENIC HIGHLIGHTS OF THE PENNINE WAY Discover the true spirit of the North on England’s original National Trail Steeped in history and traversing spectacular upland landscapes in some of England’s most popular National ParKs, the Pennine Way is the most iconic of England’s Great WalKing Trails. Stretching for 268 miles (435Km) across England’s wild northern uplands, with a combined ascent that eXceeds the height of Mount Everest, it’s also arguably the toughest. OVERVIEW • Distance: 74 miles/120km • Start/Finish: Skipton/Appleby-in-Westmorland • Number of Days: 8 • Grade: Challenging • Theme: History / Geology • Landscape: Type High Hills & Moorland Opened in 1965, the Pennine Way blazed a trail for public access to some of England’s wildest landscapes – hitherto the sole preserve of a wealthy elite. Conceived by founder member of The Ramblers Tom Stephenson and popularised by the legendary Alfred Wainwright, the full route follows the rocky spine of England – stretching from the hills of the Derbyshire Peak District, through the Yorkshire Dales and onwards through Durham and Northumberland to the Scottish Border. Roughly following the line of the watershed from which great rivers like the Tyne and the Tees, the Lune and the Eden, flow east and west respectively, the bulk of this legendary trail lies at more than 1,000ft/305m above sea level. Our shortened 8-day itinerary explores the striking limestone landscapes of Malham in the Yorkshire Dales before climbing up onto the lonely massif of Cross Fell, where the Lakeland Fells are clearly visible across the Eden Valley. The spectacular finale follows the headwaters of the River Tees to the head of the breath-taking High Cup Nick before descending along the lip of this steep-sided glacial canyon and finishing in the historic market town of Appleby. THE ROUTE This itinerary breaks down the 8-day itinerary into daily sections of between 7 and 27km/4.5 and 17 miles. The shorter days allow for transfers in and out on the first and last days. Owing to the nature of the terrain and limited accommodation en route, only minimal options for flexing the itinerary exist – although back-packers will benefit from a little more flexibility. DAY 1 SKIPTON TO MALHAM START: Catch the 210 bus from Skipton to Malham and enjoy a short ‘leg-stretcher’ to familiarise yourself with the terrain. This 4.5-mile circular walk explores the jaw-dropping natural amphitheatre of Malham Cove, the ‘clints’ and ‘grykes’ of the limestone pavement above and the waterfalls below before returning to the bustling little hamlet of Malham, where the lively pubs will be packed with fellow hikers. Stay at pub or B&B in Malham. 7km/4.5 miles DAY 2 MALHAM TO HORTON-IN-RIBBLESDALE Your first day on the Pennine Way proper leads north, past tranquil Malham Tarn and over Fountains Fell into Three Peaks Country – named after the trio of 2000ft/610m mountains that dominate this landscape: Ingleborough, Whernside and Pen-y-gent (Mountain of the Winds). Scale the rugged southern face of Pen-y-gent before descending into the pretty Yorkshire Dales village of Horton-in-Ribblesdale. Stay at pub or B&B in Horton. 24km/15 miles. DAY 3 HORTON-IN-RIBBLESDALE TO HAWES Follow the River Ribble upstream to the stunning viaduct at Ribblehead before following old packhorse routes around the summit of 2191ft/668m Dodd Fell and descending into Wensleydale – famous for the eponymous cheese so beloved of Wallace and Gromit – to reach your overnight destination of Hawes. This close-knit upland village is the centre of a farming community that ekes out a living on these remote fells. Village pubs like The Board Inn offer superb local ales and hearty food and the local creamery – home of Wensleydale Cheese – is not to be missed! 22.5km / 14miles DAY 4 HAWES TO THE TAN HILL INN Leaving Hawes, stop off at the powerful cascade of Hardraw Force before continuing north on the sustained climb to the summit of Great Shunner Fell. A stunning panorama stretching for 40 miles in each direction rewards your efforts before descending into the gentler, flower-filled pastures of Swaledale and the achingly pretty villages of Thwaite and Keld. Admire the geometric patterns inscribed on the landscape by the dry stone walls before climbing again to reach the sanctuary of Britain’s highest pub: the Tan Hill Inn – for the definitive Pennine Way pub experience. 25.7km/16 miles. DAY 5 TAN HILL INN TO MIDDLETON-IN-TEESDALE The longest day on the trail crosses the boundary into County Durham and traverses lonely moorland and secret valleys, where the wildflowers are at their best in late spring. This is the most remote section of the trail and you’ll only have the upland birds and grazing cattle for company while distant echoes of Roman Legions and Bronze Age burials are carried away on the breeze into the rustling cotton grass. The descent into Middleton is one of the scenic highlights of the walk. You’ll be ready for a pint at one of this handsome town’s many inns. 27km/17 miles DAY 6 MIDDLETON-IN-TEESDALE TO LANGDON BECK Follow the river beneath brooding crags upstream to the thundering waterfalls that punctuate the Upper Tees Valley. Revel in the wildflowers that carpet your route in this largely undiscovered Area of Outstanding Natural Beauty and marvel at the mighty torrents of Low Force and High Force, where the Tees tumbles over the Whin Sill – the fault line where iron-hard volcanic dolerite meets softer sedimentary rocks to spectacular effect. Detour for coffee and cake to the informative Bowless Visitor Centre and stay at the Langdon Beck Hotel – another quirky country inn. 12.8Km/8 miles DAY 7 LANGDON BECK TO DUFTON Fuel up with a full English breakfast for a big day ahead that most aficionados agree is the best day on the entire Pennine Way. Scramble over the rock formations beside the River Tees to another stunning waterfall at Cauldron Snout, before striking out west across the exposed vastness of the Cross Fell Plateau to the stark eastern escarpment of the Eden Valley. Admire the huge views across to the Lakeland fells before encountering the deep glacial gorge of High Cup Nick. Stride out along its northern lip then descend into the hamlet of Dufton. 19km/12 miles DAY 8 DUFTON TO APPLEBY-IN-WESTMORLAND Enjoy a lie-in before gently ambling down the Eden Valley to Appleby-in-Westmorland, another vibrant market town with a good choice of pubs and restaurants to celebrate journey’s end. The train journey back to Skipton on the scenic Settle-Carlisle railway is one of the most spectacular journeys in Europe - the perfect book-end to your Pennine Way adventure. 6.4km/4 miles ACCOMMODATION Accommodation on this section of the Pennine Way can vary from welcoming village Inns like the Lister Arms at Malham to remote yet lively upland pubs such as the iconic Tan Hill Inn – the highest pub in Britain (1732ft/528m above sea level). If the snow starts to fall, your stay may be longer than anticipated…! TRAVEL AIR/RAIL Flights into Leeds Airport followed by train to Skipton then 210 bus to Malham to join the trail. Return train to Leeds on the scenic Settle Carlisle railway then transfer to airport. From Manchester and Newcastle airports, the train journey is circa three hours. Train from London to Skipton: three hours. FERRIES Car Ferry to Hull from Rotterdam then two-hour (130km) drive to Skipton. Return direct to Skipton via rail on Settle Carlisle Railway. Collect car and return to Hull for ferry. NEED TO KNOW While there is a good choice of accommodation at each end of this itinerary in Skipton and Appleby, accommodation en route is limited and it’s wise to book ahead well in advance. The limestone sections are usually well-drained, but the sections further north could be water-logged in winter and early spring so walking boots and a full set of waterproofs are recommended. The route remains open all year, but snow and ice can make some sections quite challenging during the winter months (November – March) – particularly the Malham, Pen-y-gent and High Cup Nick sections. The longest days (24km and 26km) may present a challenge to complete in daylight during these months. FOOD & DRINK They take beer very seriously in these parts and walkers will find a bewildering range of local to slake their thirst – ranging from light refreshing pale or golden ales like Hadrian and Border Brewery’s Pennine Ambler to dark and complex brews like Wensleydale Brewery’s Black Dub that are often strong in alcohol. The best food options can be found in the pubs and inns, where hearty pies, warming stews and local lamb feature heavily on the menu. CREATE YOUR OWN TRIP Want to go solo and design your own itinerary? There’s a huge range of resources at the National Trails website: www.nationaltrail.co.uk. Plan your own bespoke itinerary and find recommended accommodation en route. GUIDEBOOKS AND FURTHER READING Pennine Way Official National Trail Guide by Damian Hall. Pub Aurum Press 2012 The Pennine Way by Paddy Dillon. Pub Cicerone Press 2017. A Pennine Way Companion by Alfred Wainwright (Revised Edition Chris jesty. Pub Frances Lincoln 2012* .
Recommended publications
  • Malhamdale and Southern/South Western Dales Fringes
    Malhamdale and Southern/South Western Dales Fringes + Physical Influences Malhamdale The landscape of Malhamdale is dominated by the influence of limestone, and includes some of the most spectacular examples of this type of scenery within the Yorkshire Dales National Park and within the United Kingdom as a whole. Great Scar limestone dominates the scenery around Malham, attaining a thickness of over 200m. It was formed in the Carboniferous period, some 330 million years ago, by the slow deposition of shell debris and chemical precipitates on the floor of a shallow tropical sea. The presence of faultlines creates dramatic variations in the scenery. South of Malham Tarn is the North Craven Fault, and Malham Cove and Gordale Scar, two miles to the south, were formed by the Mid Craven Fault. Easy erosion of the softer shale rocks to the south of the latter fault has created a sharp southern edge to the limestone plateau north of the fault. This step in the landscape was further developed by erosion during the various ice ages when glaciers flowing from the north deepened the basin where the tarn now stands and scoured the rock surface between the tarn and the village, leading later to the formation of limestone pavements. Glacial meltwater carved out the Watlowes dry valley above the cove. There are a number of theories as to the formation of the vertical wall of limestone that forms Malham Cove, whose origins appear to be in a combination of erosion by ice, water and underground water. It is thought that water pouring down the Watlowes valley would have cascaded over the cove and cut the waterfall back about 600 metres from the faultline, although this does not explain why the cove is wider than the valley above.
    [Show full text]
  • Lichen Flora of the Malham Tarn Area
    Field Studies, 10, (2001) 57 - 92 LICHEN FLORA OF THE MALHAM TARN AREA M. R. D. SEAWARD Department of Environmental Science, University of Bradford, Bradford BD7 1DP AND A. PENTECOST Division of Life Sciences, King's College London, Franklin-Wilkins Building, 150 Stamford Street, London SE1 8WA ABSTRACT A checklist of lichens, lichenicolous fungi and associated fungi recorded from an area within 5 km of the Malham Tarn Field Centre, Yorkshire is accompanied by background information on the ecology and the history of recording there. In all, 346 taxa (including Lecidea obluridata Nyl., new to Britain) have been recorded from the area; 48 are based on old records, most of which are presumed extinct, but some are questionable in the absence of supporting herbarium material. COLLECTORS The earliest lichen records from Malham are attributable to Richard Richardson (1663- 1741) of North Bierley, the first Yorkshireman to collect lichens; his localised material, used by Johann Jacob Dillenius (1684-1747) for his revision of Ray's Synopsis (1724) and his own Historia Muscorum (1742), is to be found in the Dillenian and Sherardian Herbaria at Oxford University (OXF). Other botanists contributing to our knowledge of Malham lichens in the 18th and 19th centuries include John G. Baker (1834-1920), William Borrer (1781-1862), Benjamin Carrington (1827-1893), Samuel Hailstone (1768-1851), Thomas Hebden (1849-1931), William Hudson (1734-1793), Frederic A. Lees (1847-1921), John Nowell (1802-1867), Abraham Shackleton (1830-1916), Abraham Stansfield (1802-1880), William West (1848- 1914) and John Windsor (1787-1868). Hailstone's Malham records appear in Whitaker (1805), but many are unlocalised, being expressed as occurring in 'the Craven area'.
    [Show full text]
  • Grade 2 Listed Former Farmhouse, Stone Barns
    GRADE 2 LISTED FORMER FARMHOUSE, STONE BARNS AND PADDOCK WITHIN THE YORKSHIRE DALES NATIONAL PARK swale farmhouse, ellerton abbey, richmond, north yorkshire, dl11 6an GRADE 2 LISTED FORMER FARMHOUSE, STONE BARNS AND PADDOCK WITHIN THE YORKSHIRE DALES NATIONAL PARK swale farmhouse, ellerton abbey, richmond, north yorkshire, dl11 6an Rare development opportunity in a soughtafter location. Situation Swale Farmhouse is well situated, lying within a soughtafter and accessible location occupying an elevated position within Swaledale. The property is approached from a private driveway to the south side of the B6260 Richmond to Reeth Road approximately 8 miles from Richmond, 3 miles from Reeth and 2 miles from Grinton. Description Swale Farmhouse is a Grade 2 listed traditional stone built farmhouse under a stone slate roof believed to date from the 18th Century with later 19th Century alterations. Formerly divided into two properties with outbuildings at both ends the property now offers considerable potential for conversion and renovation to provide a beautifully situated family home or possibly multiple dwellings (subject to obtaining the necessary planning consents). The house itself while needing full modernisation benefits from well-proportioned rooms. The house extends to just over 3,000 sq ft as shown on the floorplan with a total footprint of over 7,000 sq ft including the adjoining buildings. The property has the benefit of an adjoining grass paddock ideal for use as a pony paddock or for general enjoyment. There are lovely views from the property up and down Swaledale and opportunities such as this are extremely rare. General Information Rights of Way, Easements & Wayleaves The property is sold subject to, and with the benefit of all existing wayleaves, easements and rights of way, public and private whether specifically mentioned or not.
    [Show full text]
  • Durham Dales Map
    Durham Dales Map Boundary of North Pennines A68 Area of Outstanding Natural Barleyhill Derwent Reservoir Newcastle Airport Beauty Shotley northumberland To Hexham Pennine Way Pow Hill BridgeConsett Country Park Weardale Way Blanchland Edmundbyers A692 Teesdale Way Castleside A691 Templetown C2C (Sea to Sea) Cycle Route Lanchester Muggleswick W2W (Walney to Wear) Cycle Killhope, C2C Cycle Route B6278 Route The North of Vale of Weardale Railway England Lead Allenheads Rookhope Waskerley Reservoir A68 Mining Museum Roads A689 HedleyhopeDurham Fell weardale Rivers To M6 Penrith The Durham North Nature Reserve Dales Centre Pennines Durham City Places of Interest Cowshill Weardale Way Tunstall AONB To A690 Durham City Place Names Wearhead Ireshopeburn Stanhope Reservoir Burnhope Reservoir Tow Law A690 Visitor Information Points Westgate Wolsingham Durham Weardale Museum Eastgate A689 Train S St. John’s Frosterley & High House Chapel Chapel Crook B6277 north pennines area of outstanding natural beauty Durham Dales Willington Fir Tree Langdon Beck Ettersgill Redford Cow Green Reservoir teesdale Hamsterley Forest in Teesdale Forest High Force A68 B6278 Hamsterley Cauldron Snout Gibson’s Cave BishopAuckland Teesdale Way NewbigginBowlees Visitor Centre Witton-le-Wear AucklandCastle Low Force Pennine Moor House Woodland ButterknowleWest Auckland Way National Nature Lynesack B6282 Reserve Eggleston Hall Evenwood Middleton-in-Teesdale Gardens Cockfield Fell Mickleton A688 W2W Cycle Route Grassholme Reservoir Raby Castle A68 Romaldkirk B6279 Grassholme Selset Reservoir Staindrop Ingleton tees Hannah’s The B6276 Hury Hury Reservoir Bowes Meadow Streatlam Headlam valley Cotherstone Museum cumbria North Balderhead Stainton RiverGainford Tees Lartington Stainmore Reservoir Blackton A67 Reservoir Barnard Castle Darlington A67 Egglestone Abbey Thorpe Farm Centre Bowes Castle A66 Greta Bridge To A1 Scotch Corner A688 Rokeby To Brough Contains Ordnance Survey Data © Crown copyright and database right 2015.
    [Show full text]
  • 7-Night Southern Yorkshire Dales Festive Self-Guided Walking Holiday
    7-Night Southern Yorkshire Dales Festive Self-Guided Walking Holiday Tour Style: Self-Guided Walking Destinations: Yorkshire Dales & England Trip code: MDPXA-7 1, 2, 3 & 4 HOLIDAY OVERVIEW Enjoy a festive break in the Yorkshire Dales with the walking experts; we have all the ingredients for your perfect self-guided escape. Newfield Hall, in beautiful Malhamdale, is geared to the needs of walkers and outdoor enthusiasts. Enjoy hearty local food, detailed route notes, and an inspirational location from which to explore this beautiful national park. WHAT'S INCLUDED • High quality en-suite accommodation in our country house • Full board from dinner upon arrival to breakfast on departure day • The use of our Discovery Point to plan your walks – maps and route notes available www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 HOLIDAYS HIGHLIGHTS • Use our Discovery Point, stocked with maps and walks directions, for exploring the local area • Head out on any of our walks to discover the varied landscape of the Southern Yorkshire Dales on foot • Enjoy magnificent views from impressive summits • Admire green valleys and waterfalls on riverside strolls • Marvel at the wild landscape of unbroken heather moorland and limestone pavement • Explore quaint villages and experience the warm Yorkshire hospitality at its best • Choose a relaxed pace of discovery and get some fresh air in one of England's most beautiful walking areas • Explore the Yorkshire Dales by bike • Ride on the Settle to Carlisle railway • Visit the spa town of Harrogate TRIP SUITABILITY Explore at your own pace and choose the best walk for your pace and ability.
    [Show full text]
  • Water in Turner's Yorkshire
    Thornton Force Thornton Water in Turner’s Yorkshire Let the rivers & waterfalls guide you... This is a Turner Trails downloadable guide. You can discover more about Turner’s Yorkshire at www.yorkshire.com/turner. Water in Turner’s Yorkshire Turner was usually found walking or riding along the banks of rivers and streams while searching for viewpoints to sketch from. Whether drawing castles, churches or historic houses, his vantage points are often looking along a nearby river towards his subject. Sometimes the water itself was his focus and rivers and waterfalls literally flow through many of Turner’s Yorkshire sketches and paintings. He included them to link the different elements of the landscape together and take the viewer’s eye from foreground to his subject in the background. He approached one of his very first sketches in Yorkshire in exactly this way Interesting Fact... when he drew Rotherham Minster and Bridge from the River Don. Here water Water, Water Everywhere was periphery to the main subject yet essential to make the composition work 1816 was one of the wettest by holding the different elements of summers on record. Turner the picture together in an aesthetic and made one of his longer pleasing way. If you’d like to find out Yorkshire tours during more about how Turner included water this year of rains so his in his sketches and paintings of castles, encounters with water were please see Castles in Turner’s Yorkshire. Plumpton Rocks more than he bargained for. He had to fight downpours to sketch but this meant Yorkshire’s swollen rivers and surging waterfalls were at their most spectacular.
    [Show full text]
  • Find out More About the Three Peaks Project At
    The Yorkshire Three Peaks walk Distance: 39km (24 miles) Parking: Horton car park ( BD24 0HF, SD 807 724) Other transport: Horton train station on the Settle to Carlisle line is close to the start Toilets: Horton car park Refreshments: pubs and café in Horton, Station Inn at Ribblehead and the Old Hill Inn in Chapel-le-dale This is a major challenge walk which is long and involves over 1600m (5000 feet) of climbing over the Three Peaks of Pen-y-ghent, Whernside and Ingleborough. There is one section on road, but the paths are good. You do need to be able to navigate and cope with conditions in the high fells. Route description 1. Walk south out of the village passing the Golden Lion pub and church and cross a small stream. Then turn left up a minor tarmac road. Follow this up towards Brackenbottom and just before reaching some buildings take a footpath on your left signed to Pen-y-ghent. 2. Climb steadily up through fields with Pen-y-ghent ahead of you. The final section of the route to the summit is steeper for a while before reaching the trig point and shelter. 3. Cross the wall at the summit and follow the clear path heading roughly north. This zig zags down, passing the gash of Hunt Pot, to reach the head of a walled lane. 4. Carry straight on to follow the new path over Whitber Hill to reach a clear track. Turn right and follow this for 1.5km (1 mile) and then take the path on the left towards Birkwith cave.
    [Show full text]
  • Dent to Aye Gill Pike This Rewarding Walk Has Spectacular Views of the Howgill Fells (Below), the Three Peaks of Yorkshire, and Dentdale
    Dent to Aye Gill Pike This rewarding walk has spectacular views of the Howgill Fells (below), the Three Peaks of Yorkshire, and Dentdale. Start: Dent car park (GPS: SD 703 871) Distance: 10.5km (6.5 miles) Highest point: 556m (Aye Gill Pike summit) Time: Allow 3 to 4 hours Grade: Difficult Notes: This route has sections with no obvious path, so a map and navigational skills are required. There are short sections on quiet roads where care should be taken, and the route can be boggy in places. There are toilets, a village shop, café and pubs in Dent. Other options: For a more challenging experience, follow this route in the opposite direction, beginning with the very steep climb up to Aye Gill Pike. 1. (GPS: SD 704 870) Turn left out of the car park and walk through the cobbled village centre. Leave the village on this road and pick up the riverside path for the Dales Way on your left, just before the river Dee. Follow this path until you reach the tarmac road. 2. (GPS: SD 700 873) Turn right along the road and pick up the Dales Way again on your right, continuing along the river to the road at Barth Bridge. 3. (GPS: SD 694 878) At the road turn right. Walk along here for a short distance (approx 150m) and turn up the small tarmac lane on your right. Continue along this quiet lane for approximately 1km, until reaching Lunds Farm. 4. (GPS: SD 694 887) At the entrance to Lunds Farm turn left and continue through the cobbled yard.
    [Show full text]
  • Waterfalls: Forms, Distribution, Processes and Rates of Recession
    QUAESTIONES GEOGRAPHICAE 39(1) • 2020 WATERFALLS: FORMS, DISTRIBUTION, PROCESSES AND RATES OF RECESSION ANDREW S. GOUDIE School of Geography, Centre for the Environment, University of Oxford, Oxford, United Kingdom Manuscript received: December 15, 2019 Revised version: February 2, 2020 GOUDIE A. S., 2020. Waterfalls: forms, distribution, processes and rates of recession. Quaestiones Geographicae 39(1), Bo- gucki Wydawnictwo Naukowe, Poznań, pp. 59–77. 8 figs, 3 tables. ABSTRACT: A waterfall is a very steep (commonly nearly vertical) fall of some magnitude in a river course. Waterfalls are widespread fluvial landforms that have been described from many parts of the world. Thirty-eight World Heritage Properties include waterfalls in their designation. In addition, some waterfalls are actual or potential geomorphosites. Waterfalls occur in almost all climatic environments, though they are particularly common in formerly glaciated areas. They occur on a huge diversity of rock types, although in general, they do not form persistent or large falls on soft or unconsolidated rocks. Waterfalls also occur in a wide range of geomorphological settings: glaciated areas, areas of ac- tive tectonism, areas of sea-cliff retreat and sea-level change, great escarpments on passive margins, basins with river capture, rifted and faulted areas and areas that have been subjected to megaflooding. Multiple processes account for waterfall retreat and varying rates of recession. Although the greatest interest has been in rates of waterfall recession, there are examples of waterfalls that prograde as a result of tufa deposition. KEY WORDS: waterfalls, caprock, knickpoints, plunge pools, tufa Corresponding author: Andrew Goudie, [email protected] Introduction distribution and rates of retreat.
    [Show full text]
  • Trail and Fell Running
    Trail and Fell Running in the Yorkshire Dales Trail and Fell Running in the About the Author Pete Ellwood is an experienced fell runner, running and racing in the hills for over thirty years. He has lived Yorkshire Dales in the north all his life and, since his teenage years, has attempted to spend every possible waking hour on the hills and mountains. Pete holds a long service award for volunteering as a member of a mountain rescue team, 40 runs and he completed the Munros in 2003. He regularly com- petes in fell races and mountain marathons in the North in the National Park, of England and Scotland, winning a class of the Saunders Lakeland Mountain Marathon in 2013. including the Three Peaks Pete lives on the edge of the Yorkshire Dales with his wife, two boys and a daily view of Ingleborough to keep by Pete Ellwood him company. Juniper House, Murley Moss, Oxenholme Road, Kendal, Cumbria LA9 7RL www.cicerone.co.uk © Pete Ellwood 2019 Register your book: To sign up to receive free updates, special offers First edition 2019 and GPX files where available, register Contents ISBN: 978 1 85284 922 1 your book at www.cicerone.co.uk. Map key ................................................................7 Printed by KHL Printing, Singapore Acknowledgements Overview map ..........................................................8 A catalogue record for this book is Route summary table ....................................................9 This book would not have been possible available from the British Library. without the help and support of a large ULTRA ................................................................15 © Crown copyright 2019 number of people. I would like to take OS PU100012932 this opportunity to thank all the Settle Harriers who checked routes and posed The Yorkshire Dales .......................................................
    [Show full text]
  • Ω W ¢ Y Aysgarth Falls National ” Park Centre 01969 662910
    YOUR VISIT STARTS HERE…AYSGARTH FALLS Housed in converted railway cottages and with Top tip? Explore on foot - there’s always What’s on the popular Coppice Café on site, Aysgarth Falls something new to discover. The light is always • Dales Festival of Food and Drink in Leyburn National Park Centre is located right by the changing, the river rises and falls so every view is (4, 5 and 6 May) - a feast for all food lovers. spectacular three-stepped waterfalls, with lovely fresh. I love the diversity of the landscape within • Wensleydale Triathlon (11 August) - the ‘Full Freeholders’ Wood on its doorstep. the National Park. Cheese’ event is an incredible 2,000 metre Drop by for a wealth of information about the Best view of all? From Raydaleside to Hawes, swim in Semerwater, 42 mile bike ride and local area. Displays in the centre relate the story looking west with all of Wensleydale opening 20km run. of the woodland as a natural larder, the rocks up before you. • West Burton village fete (August) beneath our feet and how the falls were created. Favourite walk? The bridleway above Carperby Our knowledgeable Information Advisors can tell “with its long views and the interest of mining you all about the wildlife you’ll see and how the remains, stone circles and then down to the woodland is managed - including the right of nature reserve at Ballowfield. the ‘freeholders’ of Carperby to collect coppiced wood. Marnie, Information Advisor Aysgarth Falls National Park Centre Why not enjoy the circular woods and falls walk, then treat yourself to lunch in the café garden, spotting the local wildlife at the bird feeders.
    [Show full text]
  • Download Chapter In
    Freshwater life Martyn G Kelly, Trevor D Cris, Ben Lamb and Brian Whitton Introduction Without the River Tees there would be no Teesdale and so, whilst much of the attention in this book is focussed on the plant and animal life in the fields and fells, we should not ignore either the river or the numerous tributary streams that feed it. Cow Green Reservoir, too, plays an important part in the story of Upper Teesdale, not just because of the ways in which it has altered the landscape and habitats in the upper valley, but also because the decision to impound the river precipitated many significant ecological studies and, ironically, raised the profile of the Teesdale rarities beyond a small band of botanical cognoscenti. The River Tees was the first British River to receive a detailed biological survey (by Butcher and colleagues in the mid-1930s). This was followed in the 1970s and 1980s by studies of the upper reaches of the main river and its tributaries by Durham University and the Freshwater Biological Association (later Institute of Freshwater Ecology and now Centre for Ecology and Hydrology). Since the previous edition of this book, further studies have investigated a wide range of factors including gravel, heavy metals, availability of salmonid spawning habitat and water colour. The upper tributaries of the Tees range from torrential streams, fed at times of peak flow mainly by surface run-off, to calcareous streams with some or much of their water from limestone springs. Those with the most water from springs are the ones which vary least in flow and have the highest calcium concentrations.
    [Show full text]