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North York Moors and Cleveland Hills Area Profile: Supporting Documents
National Character 25. North York Moors and Cleveland Hills Area profile: Supporting documents www.gov.uk/natural-england 1 National Character 25. North York Moors and Cleveland Hills Area profile: Supporting documents Introduction National Character Areas map As part of Natural England’s responsibilities as set out in the Natural Environment 1 2 3 White Paper , Biodiversity 2020 and the European Landscape Convention , we are North revising profiles for England’s 159 National Character Areas (NCAs). These are areas East that share similar landscape characteristics, and which follow natural lines in the landscape rather than administrative boundaries, making them a good decision- Yorkshire making framework for the natural environment. & The North Humber NCA profiles are guidance documents which can help communities to inform their West decision-making about the places that they live in and care for. The information they contain will support the planning of conservation initiatives at a landscape East scale, inform the delivery of Nature Improvement Areas and encourage broader Midlands partnership working through Local Nature Partnerships. The profiles will also help West Midlands to inform choices about how land is managed and can change. East of England Each profile includes a description of the natural and cultural features that shape our landscapes, how the landscape has changed over time, the current key London drivers for ongoing change, and a broad analysis of each area’s characteristics and ecosystem services. Statements of Environmental Opportunity (SEOs) are South East suggested, which draw on this integrated information. The SEOs offer guidance South West on the critical issues, which could help to achieve sustainable growth and a more secure environmental future. -
Being a Thesis Submitted for the Degree Of
The tJni'ers1ty of Sheffield Depaz'tient of Uistory YORKSRIRB POLITICS, 1658 - 1688 being a ThesIs submitted for the Degree of Doctor of Philosophy by CIthJUL IARGARRT KKI August, 1990 For my parents N One of my greater refreshments is to reflect our friendship. "* * Sir Henry Goodricke to Sir Sohn Reresby, n.d., Kxbr. 1/99. COff TENTS Ackn owl edgements I Summary ii Abbreviations iii p Introduction 1 Chapter One : Richard Cromwell, Breakdown and the 21 Restoration of Monarchy: September 1658 - May 1660 Chapter Two : Towards Settlement: 1660 - 1667 63 Chapter Three Loyalty and Opposition: 1668 - 1678 119 Chapter Four : Crisis and Re-adjustment: 1679 - 1685 191 Chapter Five : James II and Breakdown: 1685 - 1688 301 Conclusion 382 Appendix: Yorkshire )fembers of the Coir,ons 393 1679-1681 lotes 396 Bibliography 469 -i- ACKNOWLEDGEMENTS Research for this thesis was supported by a grant from the Department of Education and Science. I am grateful to the University of Sheffield, particularly the History Department, for the use of their facilities during my time as a post-graduate student there. Professor Anthony Fletcher has been constantly encouraging and supportive, as well as a great friend, since I began the research under his supervision. I am indebted to him for continuing to supervise my work even after he left Sheffield to take a Chair at Durham University. Following Anthony's departure from Sheffield, Professor Patrick Collinson and Dr Mark Greengrass kindly became my surrogate supervisors. Members of Sheffield History Department's Early Modern Seminar Group were a source of encouragement in the early days of my research. -
FEN BOG from the Website North Yorkshire for the Book Discover Butterflies in Britain © D E Newland 2009
FEN BOG from www.discoverbutterflies.com the website North Yorkshire for the book Discover Butterflies in Britain © D E Newland 2009 The North Yorkshire Moors Railway passes along the western edge of Fen Bog Fen Bog is 20 ha (50 acres) of This well-known site in TARGET SPECIES boggy marshland at the head Yorkshire is noted for its Large Heath (June and early of Newtondale, near Pickering many different species of July), Small Pearl-bordered in North Yorkshire. It is 3 butterflies, moths and and Dark Green Fritillaries; miles south of Goathland and dragonflies. There is a deep commoner species. lies on the route of the North bed of peat where many Yorkshire Moors Railway different bog plants flourish. It from Pickering to Grosmont. lies within a wide valley with heather, hard fern, mat grass and purple moor grass all growing stongly. The reserve is cared for by the Yorkshire Wildlife Trust. The North York Moors became one of our first National Parks in 1952. Its moors are one of the largest areas of heather moorland in Britain and cover an area of 550 square miles. It is hard to imagine that they were once permanently covered in ice and snow. When global warming took effect at the end of the Ice Age, the snowfields began to melt and melt water flowed south. It gouged out the deep valley of Newtondale where the Pickering Beck now flows. Newtondale runs roughly north-south parallel to the A169 Whitby to Pickering road and is a designated SSSI of 940 ha (2,300 acres). -
Quakers in Thirsk Monthly Meeting 1650-75," Quaker Studies: Vol
Quaker Studies Volume 9 | Issue 2 Article 6 2005 Quakers in Thirsk onM thly Meeting 1650-75 John Woods [email protected] Follow this and additional works at: http://digitalcommons.georgefox.edu/quakerstudies Part of the Christian Denominations and Sects Commons, and the History of Christianity Commons Recommended Citation Woods, John (2005) "Quakers in Thirsk Monthly Meeting 1650-75," Quaker Studies: Vol. 9: Iss. 2, Article 6. Available at: http://digitalcommons.georgefox.edu/quakerstudies/vol9/iss2/6 This Article is brought to you for free and open access by Digital Commons @ George Fox University. It has been accepted for inclusion in Quaker Studies by an authorized administrator of Digital Commons @ George Fox University. For more information, please contact [email protected]. QUAKER STUDIES 912 (2005) [220-233] WOODS QUAKERS INTHIRSK MONTHLY MEETING 1650-75 221 ISSN 1363-013X part of the mainly factual records of sufferings, subject to the errors and mistakes that occur in recording. Further work of compilation, analysis, comparison and contrast with other areas is needed to supplement this narra tive and to interpret the material in a wider context. This interim cameo can serve as a contribution to the larger picture. QUAKERS IN THIRSK MONTHLY MEETING 1650-75 The present study investigates the area around Thirsk in Yorkshire and finds evidence that gives a slightly different emphasis from that of Davies. Membership of the local community is apparent, but, because the evidence comes from the account of the sufferings of Friends following their persecution John Woods for holding meetings for worship in their own homes, when forbidden to meet in towns, it shows that the sustained attempt in this area during the decade to prevent worship outside the Established Church did not prevent the Malton,North Yorkshire,England 1660-70 holding of Quaker Meetings for worship in the area. -
Stakeholder Contribution and Conflict in Pickering, North Yorkshire: Trying to Reconcile Science with Project Delivery in a Pilot Flood Risk Management Scheme
Stakeholder contribution and conflict in Pickering, North Yorkshire: trying to reconcile science with project delivery in a pilot flood risk management scheme Nick Odoni School of Geographical Sciences, Bristol University ([email protected]) Stakeholder engagement - (rough) outline of today‟s talk Part 1: Preliminaries - Some ideas about stakeholders and stakeholdership - Use of models … why might we trust in a model? Part 2: residents and scientists working as individuals co-producing knowledge - the RELU Knowledge Controversies (“KC”) project, competency group working in Pickering (and Uckfield); - how we worked, bunding the Beck, development of “OVERFLOW” Stakeholder engagement - (rough) outline of today‟s talk Part 1: Preliminaries - Some ideas about stakeholders and stakeholdership - Use of models … why might we trust in a model? Part 2: residents and scientists working as individuals co-producing knowledge - the RELU Knowledge Controversies (“KC”) project, competency group working in Pickering (and Uckfield); - how we worked, bunding the Beck, development of “OVERFLOW” Part 3: „representative agent‟ working in a project delivery setting - the Slowing the Flow at Pickering and Sinnington (“STF”) project; - Forest Research (“FR”), OVERFLOW, and some progress; - bunding again, and project collapse(?) Part 4: comments, thoughts and lessons - what worked in Pickering (and Uckfield) and the STF project; - how the bund scheme collapsed, and (maybe) why; - stakeholdership … why do you want to use it and what do you want from it? -
Brotherton and Fairburn Ings Western CEF Walk No. 4 Brotherton and Fairburn Ings
Brotherton and Fairburn Ings Parish 9 Parking Toilets Parish MILES HOURS Hall 4 Available Available Hall Ledsham Church Brotherton and Fairburn Ings Western CEF Walk no. 4 A very pleasant, easy walk following the River Aire to Fairburn Ings where you can linger awhile to observe the varied bird life and take refreshments at the Visitor Centre. From the Visitor Centre the 9 mile walk follows Newfield Lane northwards past a wooded plantation to the beautiful village of Ledsham and its historic All Saints Church which is well worth a visit. From Ledsham we return along a scenic route via Wormstall Wood, Lambkin Hill and Caudle Hill Plantation with panoramic views across Fairburn Ings to arrive in the interesting village of Fairburn with its historic local jail which is built into a rock wall. We then continue via Cut Road down to the River Aire to retrace the first outward leg of the riverside walk back to Brotherton passing the historic Church of St. Edward the Confessor en route. There are gentle gradients and some stiles on this walk but all of the walking is generally easy underfoot although some grassy and unsurfaced sections may be slippery in wet weather. There may be livestock in some of the grass meadows on the return leg from Ledsham. The walk is unsuitable for wheelchairs and pushchairs. Brotherton and Fairburn Ings Overview North Road (A162) at Brotherton grid ref. Distance - 9 miles (can shorten to 7.0 SE48621 25642. miles – see route directions) OS Map - Explorer 290 York, Selby and Time - 4 hours (9 miles) Tadcaster. -
Directory of Establishments 2020/21- Index
CHILDREN AND YOUNG PEOPLE’S SERVICE DIRECTORY OF ESTABLISHMENTS 2020/21- INDEX Page No Primary Schools 2-35 Nursery School 36 Secondary Schools 37-41 Special Schools 42 Pupil Referral Service 43 Outdoor Education Centres 43 Adult Learning Service 44 Produced by: Children and Young People’s Service, County Hall, Northallerton, North Yorkshire, DL7 8AE Contact for Amendments or additional copies: – Marion Sadler tel: 01609 532234 e-mail: [email protected] For up to date information please visit the Gov.UK Get information about Schools page at https://get-information-schools.service.gov.uk/ 1 PRIMARY SCHOOLS Status Telephone County Council Ward School name and address Headteacher DfE No NC= nursery Email District Council area class Admiral Long Church of England Primary Mrs Elizabeth T: 01423 770185 3228 VC Lower Nidderdale & School, Burnt Yates, Harrogate, North Bedford E:admin@bishopthorntoncofe. Bishop Monkton Yorkshire, HG3 3EJ n-yorks.sch.uk Previously Bishop Thornton C of E Primary Harrogate Collaboration with Birstwith CE Primary School Ainderby Steeple Church of England Primary Mrs Fiona Sharp T: 01609 773519 3000 Academy Swale School, Station Lane, Morton On Swale, E: [email protected] Northallerton, North Yorkshire, Hambleton DL7 9QR Airy Hill Primary School, Waterstead Lane, Mrs Catherine T: 01947 602688 2190 Academy Whitby/Streonshalh Whitby, North Yorkshire, YO21 1PZ Mattewman E: [email protected] Scarborough NC Aiskew, Leeming Bar Church of England Mrs Bethany T: 01677 422403 3001 VC Swale Primary School, 2 Leeming Lane, Leeming Bar, Stanley E: admin@aiskewleemingbar. Northallerton, North Yorkshire, DL7 9AU n-yorks.sch.uk Hambleton Alanbrooke Community Primary School, Mrs Pippa Todd T: 01845 577474 2150 CS Sowerby Alanbrooke Barracks, Topcliffe, Thirsk, North E: admin@alanbrooke. -
The Medieval Manuscripts in Leeds University Library
The Medieval Manuscripts in Leeds University Library Oliver Pickering and Katja Airaksinen The online publication in September 2008 of some 685 images of illuminated pages in Leeds manuscripts, opening the collection to the world, has prompted this wider survey of the University Library’s medieval holdings. Twenty-seven manuscripts qualified for the digitisation project in containing illumination. There are as many manuscripts again in terms of codices, along with a considerable number of documents and fragments.1 The most important items came to the Library in 1936 as part of the Brotherton Collection, the private library amassed in the 1920s by the Yorkshire industrialist Sir Edward Allen Brotherton, who was ennobled shortly before his death in 1930 as Baron Brotherton of Wakefield. But this event will be treated here as the main highlight in a broader account of benefaction to and acquisition by Leeds University Library. Lord Brotherton’s collection, when it arrived, gave the Library’s medieval holdings both coherence and substance, but he had earlier joined with other local benefactors in 1925 in presenting a single medieval manuscript, a copy of the Anglo-Norman didactic verse treatise, Le Manuel des péchés, counted amongst the general run of the Library’s manuscripts (MS 1).2 This is a relatively modest production of the early fourteenth century, having a two- column layout typical of vernacular verse manuscripts of that date, with the initial letters of each line slightly offset and picked out in red. There are significant omissions from the text, which the scribe is said to have treated ‘fort librement’.3 However, the Library first acquired a medieval manuscript, a copy of Juvenal’s Satires (MS 4), in October 1921, a purchase (for five guineas) from a bookseller’s catalogue. -
! National Rivers Authority ! Information Centre '9Ad Office Jass N O
NATIONAL RIVERS AUTHORITY YORKSHIRE REGION RIVER FLOW & RAINFALL STATISTICS UPDATED TO 31ST DECEMBER 1992 National Rivers Authority Northumbria & Yorkshire Region Olympia House Gelderd Lane Gelderd Road Leeds LS12 6DD August 1993 ! National Rivers Authority ! Information Centre '9ad Office Jass N o ................. | accession No NATIONAL RIVERS AUTHORITY YORKSHIRE REGION RIVER FLOW AND RAINFALL STATISTICS UPDATED TO 31ST DECEMBER 1992 This publication combines the 1992 annual reports on River Flow Statistics and on Rainfall. It is in two sections:- (i) River Flow Statistics updated to 31st December 1992. (ii) Annual Rainfall Report 1992. IMPORTANT NOTICE The published d^ta are the best available in August 1993. Please consult the Resource Planning and Hydrometry Section about the accuracy of the data, and the possibility of revision, before using these records for detailed investigations. The Section would also be pleased to be notified of any errors which may be discovered. Telephone: Leeds 440191 NRA Northumbria & Yorkshire Region August 1993 RIVER FLOW STATISTICS UPDATED TO 31ST DECEMBER 1992 Introduction This publication contains summary data for 1992 and analyses of long period river flow records. The data should be used with some caution. All the published river flows are "net" or "as measured". No adjustments have been made in respect of abstractions.from, or discharges to, the river upstream of the flow measuring station, or for changes in storage of reservoirs etc. Records allowing for such adjustments are usually available from the appropriate Division of Yorkshire Water pic or from NRA Northumbria and Yorkshire Region Resource Planning and Hydrometry Section. Records have been included for some stations which were designed primarily to measure low flows. -
Agenda Meeting: Planning and Regulatory Functions Committee Venue
Agenda Meeting: Planning and Regulatory Functions Committee Venue: The Grand Meeting Room, County Hall, Northallerton Date: Tuesday, 23 July 2019 at 10.00 a.m. Recording is allowed at County Council, committee and sub-committee meetings which are open to the public, please give due regard to the Council’s protocol on audio/visual recording and photography at public meetings, a copy of which is available to download below. Anyone wishing to record is asked to contact, prior to the start of the meeting, the Officer whose details are at the foot of the first page of the Agenda. We ask that any recording is clearly visible to anyone at the meeting and that it is non-disruptive. http://democracy.northyorks.gov.uk Business 1. Minutes of the Meeting held on 2 April 2019. (Pages 5 to 9) 2. Declarations of Interest. 3. Public Questions or Statements. Members of the public may ask questions or make statements at this meeting if they have given notice of their question/statement to Steve Loach of Democratic Services (contact details below) by midday on Thursday 18 July 2019. Each speaker should limit themselves to 3 minutes on any item. Members of the public who have given notice will be invited to speak:- Continued overleaf/… Enquiries relating to this agenda please contact Steve Loach Tel: 01609 532216 or e-mail [email protected] Website: www.northyorks.gov.uk at this point in the meeting if their questions/statements relate to matters which are not otherwise on the Agenda (subject to an overall time limit of 30 minutes); or when the relevant Agenda item is being considered if they wish to speak on a matter which is on the Agenda for this meeting If you are exercising your right to speak at this meeting, but do not wish to be recorded, please inform the Chairman, who will instruct anyone who may be taking a recording to cease while you speak. -
Permian Gypsum in the Ripon and Bedale Areas, North Yorkshire
Geological Society, London, Special Publications Subsidence and foundering of strata caused by the dissolution of Permian gypsum in the Ripon and Bedale areas, North Yorkshire A. H. Cooper Geological Society, London, Special Publications 1986; v. 22; p. 127-139 doi:10.1144/GSL.SP.1986.022.01.11 Email alerting click here to receive free email alerts when new articles cite this service article 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, Special Publications or the Lyell Collection Notes Downloaded by Anthony Hamilton Cooper on 11 January 2008 © 1986 Geological Society of London Subsidence and foundering of strata caused by the dissolution of Permian gypsum in the Ripon and Bedale areas, North Yorkshire A.H. Cooper SUMMARY: Underground dissolution of thick gypsum beds in the Edlington Formation and Roxby Formation of the Zechstein sequence in North Yorkshire, England, has resulted in a 3 km-wide and 100 km-long belt of ground susceptible to foundering. Within this belt a large subsidence depression at Snape Mires, near Bedale, was largely filled with lacustrine deposits in the later part of the Late Devensian and during the Flandrian. South of Snape Mires the Nosterfield-Ripon-BishopMonkton area has suffered about 40 episodes of subsidence in the past 150 years, and the presence of several hundred other subsidence hollows indicates considerable activity from the later part of the Devensian onwards. The linear and grid-like arrangement of these subsidence hollows indicates collapse at intersections in a joint- controlled cave system. -
Regional Geology
CHAPTER III REGIONAL GEOLOGY The area known as the West Riding was an administrative EARLY PALAEOZOIC division of the ancient county of Yorkshire and includes (ORDOVICIAN TO DEVONIAN SYSTEMS) parts of the modern administrative areas of West Ordovician rocks outcrop as small inliers east of Howgill Yorkshire, North Yorkshire, Cumbria and Lancashire. Fells and more extensively in the extreme northwest Geographically the area extends from the high ground around Sedburgh. Historically they were exploited on a (>600m) of the Pennines in the north and west into the local basis for building stone, flagstones and roofing slates. lowland areas marginal to the Vale of York in the east. The Silurian rocks were exploited for flagstones in the These major topographic subdivisions reflect changes Ingleton and Horton-in-Ribblesdale areas and were used in the underlying geological formations (Fig. 6). The locally for grave stones, boundary and milestone markers. high mountainous spine of the Pennine area that crosses The best known of these stones were the Horton Flags the West Riding from north to south, is underlain by which were quarried around Helwith Bridge (from the hard, durable rocks ranging from Precambrian to seventeenth to nineteenth centuries: Mitchell, W. 1985). Namurian (Carboniferous) in age. The lower ground to The massive sandstones of the Austick Grits were also the south-east is underlain by the thick Coal Measure used locally for building. Stones from this succession have successions exposed in the deeply incised valleys of the not so far been identified in the Anglo-Saxon carved Yorkshire Coalfield, extending southwards from Leeds to Sheffield.