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7-Night Southern Lake District Tread Lightly Guided Walking Holiday for Solos
7-Night Southern Lake District Tread Lightly Guided Walking Holiday for Solos Tour Style: Tread Lightly Destinations: Lake District & England Trip code: CNSOS-7 2, 3 & 5 HOLIDAY OVERVIEW We are all well-versed in ‘leaving no trace’ but now we invite you to join us in taking it to the next level with our new Tread Lightly walks. We have pulled together a series of spectacular walks which do not use transport, reducing our carbon footprint while still exploring the best landscapes that the Southern Lake District have to offer. You will still enjoy the choice of three top-quality walks of different grades as well as the warm welcome of a HF country house, all with the added peace of mind that you are doing your part in protecting our incredible British countryside. Relax and admire magnificent mountain views from our Country House on the shores of Conistonwater. Walk in the footsteps of Wordsworth, Ruskin and Beatrix Potter, as you discover the places that stirred their imaginations. Enjoy the stunning mountain scenes with lakeside strolls or enjoy getting nose-to-nose with the high peaks as you explore their heights. Whatever your passion, you’ll be struck with awe as you explore this much-loved area of the Lake District. www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 HOLIDAYS HIGHLIGHTS • Head out on guided walks to discover the varied beauty of the South Lakes on foot • Choose a valley bottom stroll or reach for the summits on fell walks and horseshoe hikes • Let our experienced leaders bring classic routes and hidden gems to life • Visit charming Lakeland villages • A relaxed pace of discovery in a sociable group keen to get some fresh air in one of England’s most beautiful walking areas • Evenings in our country house where you can share a drink and re-live the day’s adventures TRIP SUITABILITY This trip is graded Activity Level 2, 3 and 5. -
Folk Song in Cumbria: a Distinctive Regional
FOLK SONG IN CUMBRIA: A DISTINCTIVE REGIONAL REPERTOIRE? A dissertation submitted in partial fulfilment of the degree of Doctor of Philosophy by Susan Margaret Allan, MA (Lancaster), BEd (London) University of Lancaster, November 2016 ABSTRACT One of the lacunae of traditional music scholarship in England has been the lack of systematic study of folk song and its performance in discrete geographical areas. This thesis endeavours to address this gap in knowledge for one region through a study of Cumbrian folk song and its performance over the past two hundred years. Although primarily a social history of popular culture, with some elements of ethnography and a little musicology, it is also a participant-observer study from the personal perspective of one who has performed and collected Cumbrian folk songs for some forty years. The principal task has been to research and present the folk songs known to have been published or performed in Cumbria since circa 1900, designated as the Cumbrian Folk Song Corpus: a body of 515 songs from 1010 different sources, including manuscripts, print, recordings and broadcasts. The thesis begins with the history of the best-known Cumbrian folk song, ‘D’Ye Ken John Peel’ from its date of composition around 1830 through to the late twentieth century. From this narrative the main themes of the thesis are drawn out: the problem of defining ‘folk song’, given its eclectic nature; the role of the various collectors, mediators and performers of folk songs over the years, including myself; the range of different contexts in which the songs have been performed, and by whom; the vexed questions of ‘authenticity’ and ‘invented tradition’, and the extent to which this repertoire is a distinctive regional one. -
3.5 How Natural Resources Were Exploited
R2R 04 26/10/09 08:30 Page 56 3.5 How Natural Resources Were Exploited When thy father went a-hunting, A spear on his shoulder, a club in his hand, He would call the nimble hounds … When thy father went to the mountain He would bring back a roe-buck, a wild boar, a stag, A speckled grouse from the mountain, A fish from Derwent waterfall … Wild boar and lynx and fox …’ Translated seventh century Cumbric/Welsh lullaby from ‘The Book of Aneurin’ All the survey teams uncovered a wealth of evidence We cannot travel far within the two parishes with- regarding the manner in which past generations have out observing the evidence of quarrying (Map 8). utilised the natural resources available in the land- Many are large-scale slate quarries such as Common- scape. The rock that forms the mountains, the water wood, Walna Scar and Stainton Ground. Slate that carves the valleys, woodland and wild animals quarrying in the valley developed in the seventeenth have all at one time or another been managed and century. Although the larger quarries had already utilised by resourceful and self-sufficient inhabitants. been well-documented, the groups nevertheless Map 8 Abandoned quarries and mines recorded by R2R in the Duddon Valley. Most of the quarrying was for slate, while the mines mainly extracted copper and lead ores. It will be noted that while some quarries and mines were located close to present-day roads, tracks and bridleways, in other cases there are no obvious routes by which the minerals were transported other than on tracks that have become modern day footpaths. -
New Additions to CASCAT from Carlisle Archives
Cumbria Archive Service CATALOGUE: new additions August 2021 Carlisle Archive Centre The list below comprises additions to CASCAT from Carlisle Archives from 1 January - 31 July 2021. Ref_No Title Description Date BRA British Records Association Nicholas Whitfield of Alston Moor, yeoman to Ranald Whitfield the son and heir of John Conveyance of messuage and Whitfield of Standerholm, Alston BRA/1/2/1 tenement at Clargill, Alston 7 Feb 1579 Moor, gent. Consideration £21 for Moor a messuage and tenement at Clargill currently in the holding of Thomas Archer Thomas Archer of Alston Moor, yeoman to Nicholas Whitfield of Clargill, Alston Moor, consideration £36 13s 4d for a 20 June BRA/1/2/2 Conveyance of a lease messuage and tenement at 1580 Clargill, rent 10s, which Thomas Archer lately had of the grant of Cuthbert Baynbrigg by a deed dated 22 May 1556 Ranold Whitfield son and heir of John Whitfield of Ranaldholme, Cumberland to William Moore of Heshewell, Northumberland, yeoman. Recites obligation Conveyance of messuage and between John Whitfield and one 16 June BRA/1/2/3 tenement at Clargill, customary William Whitfield of the City of 1587 rent 10s Durham, draper unto the said William Moore dated 13 Feb 1579 for his messuage and tenement, yearly rent 10s at Clargill late in the occupation of Nicholas Whitfield Thomas Moore of Clargill, Alston Moor, yeoman to Thomas Stevenson and John Stevenson of Corby Gates, yeoman. Recites Feb 1578 Nicholas Whitfield of Alston Conveyance of messuage and BRA/1/2/4 Moor, yeoman bargained and sold 1 Jun 1616 tenement at Clargill to Raynold Whitfield son of John Whitfield of Randelholme, gent. -
Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C. -
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 -
Supplementary Information
Heritage Team 4th Floor 100 Parliament Street London SW1A 2BQ T: 020 7211 2018 [email protected] www.gov.uk/dcms 11 November 2016 Dear Ms Bourdin, Thank you for your letter of 17 October requesting further information regarding the nomination of the English Lake District for World Heritage inscription. You have asked for further details concerning proposals for development in the English Lake District and we feel that it would be helpful to preface our response with some explanation of the planning functions and powers of the Lake District National Park Authority, which is the planning authority for the whole of the candidate English Lake District World Heritage site. The English Lake District is an outstanding cultural landscape that has evolved over a long period of time and needs to continue evolving to sustain its future. We have a vibrant community of some 42,000 residents and an economy that is sustained by the key activities of upland hill farming and tourism. These activities inevitably need to develop in order to sustain the local economy and along with other requirements of the Lake District community, they generate planning applications which are determined by the Lake District National Park Authority. UK National Parks have the highest level of planning protection in the UK and the framework for our decision-making is outlined below. BACKGROUND TO THE PLANNING FUNCTION OF UK NATIONAL PARKS UK National Parks were established under the National Parks and Access to the Countryside Act 1949, and amended by the Environment Act 1995, to: conserve and enhance the natural beauty, wildlife and cultural heritage (of the National Parks); and promote opportunities for the understanding and enjoyment of the special qualities (of the National Parks) by the public. -
Trusmadoor and Other Cumbrian `Pass' Words
Trusmadoor and Other Cumbrian `Pass' Words Diana Whaley University of Newcastle Nobody ever sang the praises of Trusmadoor, and it's time someone did. This lonely passage between the hills, an obvious and easy way for man and beast and beloved by wheeling buzzards and hawks, has a strange nostalgic charm. Its neat and regular proportions are remarkable—a natural `railway cutting'. What a place for an ambush and a massacre!1 No ambushes or massacres are promised in the following pages, but it will be argued that the neglected name of Trusmadoor holds excitements of a quieter kind. I will consider its etymology and wider onomastic and historical context and significance, and point to one or possibly two further instances of its rare first element. In the course of the discussion I will suggest alternative interpretations of two lost names in Cumbria. Trusmadoor lies among the Uldale Fells in Cumbria, some five miles east of the northern end of Bassenthwaite Lake (National Grid Reference NY2733). An ascending defile, it runs south-east, with Great Cockup to its west and Meal Fell to the north-east. The top of the pass forms a V-shaped frame for splendid views north over the Solway Firth some twenty miles away. Trusmadoor is a significant enough landscape feature to appear on the Ordnance Survey (OS) One Inch and 1:50,000 maps of the area, yet it is unrecorded, so far as I know, until its appearance on the First Edition Six Inch OS map of 1867. In the absence of early spellings one would normally be inclined to leave the name well alone, a practice followed, intentionally or not, by the editors of the English Place-Name Society survey of Cumberland.2 However, to speakers or readers of Welsh the name is fairly transparent. -
References Geological Society, London, Memoirs
Geological Society, London, Memoirs References Geological Society, London, Memoirs 2002; v. 25; p. 297-319 doi:10.1144/GSL.MEM.2002.025.01.23 Email alerting click here to receive free email alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Geological Society, London, Memoirs or the Lyell Collection Notes Downloaded by on 3 November 2010 © 2002 Geological Society of London References ABBATE, E., BORTOLOTTI, V. & PASSERINI, P. 1970. Olistostromes and olis- ARCHER, J. B, 1980. Patrick Ganly: geologist. Irish Naturalists' Journal, 20, toliths. Sedimentary Geology, 4, 521-557. 142-148. ADAMS, J. 1995. Mines of the Lake District Fells. Dalesman, Skipton (lst ARTER. G. & FAGIN, S. W. 1993. The Fieetwood Dyke and the Tynwald edn, 1988). fault zone, Block 113/27, East Irish Sea Basin. In: PARKER, J. R. (ed.), AGASSIZ, L. 1840. Etudes sur les Glaciers. Jent & Gassmann, Neuch~tel. Petroleum Geology of Northwest Europe: Proceedings of the 4th Con- AGASSIZ, L. 1840-1841. On glaciers, and the evidence of their once having ference held at the Barbican Centre, London 29 March-1 April 1992. existed in Scotland, Ireland and England. Proceedings of the Geo- Geological Society, London, 2, 835--843. logical Society, 3(2), 327-332. ARTHURTON, R. S. & WADGE A. J. 1981. Geology of the Country Around AKHURST, M. C., BARNES, R. P., CHADWICK, R. A., MILLWARD, D., Penrith: Memoir for 1:50 000 Geological Sheet 24. Institute of Geo- NORTON, M. G., MADDOCK, R. -
(Chondrichthyes, Elasmobranchii) from the Middle Jurassic of SW Germany and NW Poland
Neoselachian remains (Chondrichthyes, Elasmobranchii) from the Middle Jurassic of SW Germany and NW Poland JÜRGEN KRIWET Kriwet, J. 2003. Neoselachian remains (Chondrichthyes, Elasmobranchii) from the Middle Jurassic of SW Germany and NW Poland. Acta Palaeontologica Polonica 48 (4): 583–594. New neoselachian remains from the Middle Jurassic of SW Germany and NW Poland are described. The locality of Weilen unter den Rinnen in SW Germany yielded only few orectolobiform teeth from the Aalenian representing at least one new genus and species, Folipistrix digitulus, which is assigned to the orectolobiforms and two additional orectolobi− form teeth of uncertain affinities. The tooth morphology of Folipistrix gen. nov. indicates a cutting dentition and suggests specialised feeding habits. Neoselachians from Bathonian and Callovian drill core samples from NW Poland produced numerous selachian remains. Most teeth are damaged and only the crown is preserved. Few identifiable teeth come from uppermost lower to lower middle Callovian samples. They include a new species, Synechodus prorogatus, and rare teeth attributed to Palaeobrachaelurus sp., Pseudospinax? sp., Protospinax cf. annectans Woodward, 1919, two additional but unidentifiable Protospinax spp. and Squalogaleus sp. Scyliorhinids are represented only by few isolated tooth crowns. No batoid remains have been recovered. The two assemblages contribute to the knowledge about early neoselachian distribution and diversity. Key words: Chondrichthyes, Neoselachii, Jurassic, Germany, Poland, taxonomy, diversity. Jürgen Kriwet [[email protected]], Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, United Kingdom. Introduction Woodward 1889; Frass 1896; Thies 1992, 1993), Northern France (Duffin and Ward 1993), Luxembourg (Delsate Neoselachii is a well−defined monophyletic clade and repre− 1995), Belgium (Delsate and Thies 1995; Delsate and Gode− sents one of the most successful groups of selachians. -
Inn Way to the Lake District
Walking Holidays in Britain’s most Beautiful Landscapes Inn Way to the Lake District The Lakes Inn Way is a 90 mile circular walk starting and finishing in the popular tourist town of Ambleside. This trail takes in some of the more remote corners of the Lake District, and takes you through the Lake District’s stunning deep sided valleys, along lake shores and over remote mountain passes – as well as past over 40 traditional Lakeland inns. The full route takes you through the popular tourist towns of Ambleside, Coniston, and Grasmere (site of Dove Cottage, former home of the Romantic Poet Wordsworth), as well as through a few of the Lake District’s most impressive valleys – Borrowdale, Ennerdale, and Great Langdale, linked together with paths over high mountain passes, with great views of the surrounding fells. A highlight is a visit to remote Wasdale Head, in the shadow of Scafell Pike, the highest mountain in England. Why is the route known as the Inn Way to the Lake District? Because it is devised so that at each day the route passes a pub at lunchtime and there will always be one nearby – or you will be staying in one – at each overnight stop. There are many traditional Lakeland Inns to choose from, – so you can plan your trip looking forward to log fires, local ales and good food, often made with local produce. Mickledore - Walking Holidays to Remember 1166 1 Walking Holidays in Britain’s most Beautiful Landscapes Summary you will need to read a map and use the route path and pass between Barrow and Outerside Why do this walk? description. -
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.