Regional Geology
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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. -
Wales Regional Geology RWM | Wales Regional Geology
Wales regional geology RWM | Wales Regional Geology Contents 1 Introduction Subregions Wales: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks Older sedimentary rocks 3 Basement rocks Rock structure 4 Groundwater 5 Resources 6 Natural processes Further information 7 - 21 Figures 22 - 24 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Wales Regional Geology Introduction This region comprises Wales and includes the adjacent inshore area which extends to 20km from the coast. Subregions To present the conclusions of our work in a concise and accessible way, we have divided Wales into 6 subregions (see Figure 1 below). We have selected subregions with broadly similar geological attributes relevant to the safety of a GDF, although there is still considerable variability in each subregion. The boundaries between subregions may locally coincide with the extent of a particular Rock Type of Interest, or may correspond to discrete features such as faults. -
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. -
STRATEGIC STONE STUDY a Building Stone Atlas of NORTH-EAST YORKSHIRE
STRATEGIC STONE STUDY A Building Stone Atlas of NORTH-EAST YORKSHIRE Published May 2012 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © NE Yorkshire Bedrock Geology NERC. All rights reserved Click on this link to visit NE Yorkshire’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window http://maps.bgs.ac.uk/buildingstone?County=North-EastYorkshire ) NE Yorkshire Strategic Stone Study 1 Stratigraphical column of the Permian (in part),Triassic, Jurassic and Cretaceous rocks and Quaternary deposits in North-east Yorkshire showing the common buildings stones (bold) and alternative stone names. The oldest rocks are at the bottom of the table. Gp., Group; Fm., Formation; Mbr., Member. North East Yorkshire: Permian, Triassic, Jurassic, Cretaceous & Quaternary Building Stones PERIOD GROUP FORMATION MEMBER Common/alternative Stone Name Calcareous Tufa; Aquarium Stone Till (Boulder Clay) and Fluvio-glacial sand Quaternary and gravel; boulders Tertiary Cleveland Dyke Whinstone Flamborough Chalk Fm. Flamborough Chalk; White Chalk Burnham Chalk Fm. Burnham Chalk; White chalk Chalk Group Welton ChalkFm. Cretaceous Ferriby Chalk Fm. Grey chalk ungrouped Hunstanton Fm. Speeton Clay Kimmeridge Clay ungrouped Ampthill Clay North Grimston Upper Calcareous Grit Upper Calcareous Grit Cementstone North Grimston Cementstone Formation Coral Rag Member Coral Rag Malton Oolite Member Malton Oolite; Hildenley Limestone; Corallian Hildenley Stone Group Middle Calcareous Grit Middle Calcareous Grit Coralline Oolite Formation Member Birdsall Calcareous Grit Birdsall Calcareous Grit Member Hambleton Oolite Hambleton Oolite Member Yedmandale Member Passage Beds; Wallstone Lower Calcareous Grit Fm. Lower Calcareous Grit Oxford Clay Fm. -
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. -
TMS-01 04 Butler (To D) 14/10/05 10:42 Am Page 43
TMS-01 04 Butler (to_d) 14/10/05 10:42 am Page 43 The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway N. BUTLER1, M. A. CHARNOCK2, K. O. HAGER2,3 & C. A. WATKINS1 1Robertson Research International Ltd., Llanrhos, Llandudno LL30 1SA, UK (e-mail [email protected]) 2Norsk Hydro AS, Research Centre, N-5020, Bergen, Norway 3Norsk Hydro AS, N-0246, Oslo, Norway Abstract: A palynostratigraphical study of the Middle Jurassic Ravenscar Group, Cleveland Basin, northern England involving the integration of miospore and microplank- ton data with sedimentary facies data has resulted in improvements in the stratigraphical resolution of offshore hydrocarbon-bearing strata in the North Viking Graben and Mid- Norway. The Dogger Formation is of ‘earliest’ Aalenian age and is correlative with the uppermost Dunlin Group, Drake Formation and Båt Group, Ror Formation. The overly- ing Aalenian Saltwick and Eller Beck formations correlate with the Brent Group, Broom–Rannoch–Etive–Ness and the Fangst Group, Ile–Not–‘lower’ Garn genetic packages. The Cloughton Formation is either unrepresented or condensed in the Brent Province and Mid-Norway due to a regional unconformity, which truncates lower Bajocian sediments. The Scarborough Formation is of ‘latest’ early to ‘earliest’ late Bajocian age and correlative with the older part of the Tarbert–Heather and the ‘upper’ Garn–Melke genetic packages. These interpretations contrast markedly with the majority of those published. Despite their maturity of exploration and Methodology and techniques development, Middle Jurassic sandstones of the North Sea and offshore Mid-Norway still repre- The analyses were concentrated on three key sent some of the most prolific hydrocarbon sections near Whitby, Ravenscar and Scar- reservoirs in northwest Europe. -
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. -
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. -
Stratigraphical Framework for the Middle Jurassic Strata of Great
Stratigraphical framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf Geology and Landscape Programme Research Report RR/11/06 BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/11/06 The National Grid and other Stratigraphical framework for the Ordnance Survey data © Crown copyright and database rights 2012. Ordnance Survey Licence Middle Jurassic strata of Great No. 100021290 Britain and the adjoining Key words Geology, stratigraphy, lithostratigraphy, Inferior Oolite continental shelf Group, Great Oolite Group, Ravenscar Group, Great Estuarine Group, Sutherland Group, Ancholme Group, Jurassic. A J M Barron, G K Lott, J B Riding Front cover Hilltop Quarry, Leckhampton Hill, Cheltenham, Glos.: the Birdlip Limestone Formation overlain by the Aston Limestone Formation. (P775213, A J M Barron) Bibliographical reference BARRON, A J M, LOTT, G K, AND RIDING, J B. 2012. Stratigraphical framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf. British Geological Survey Research Report, RR/11/06. 187pp. ISBN 978 0 85272 695 2 Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided -
Landscape-Strategy-Dark-Peak.Pdf
www.peakdistrict.gov.uk 3: Dark Peak Peak District National Park Authority Dark Peak Dark Peak open moorland © Peak District National Park Authority Introduction The Dark Peak is a sparsely settled area of gritstone uplands lying at the southern end of the Pennine Hills. The area comprises an extensive upland plateau with steep gritstone slopes, sometimes with rocky edges, that drop away to lower lying slopes, wooded cloughs and deep valleys, some of which have been flooded to create large reservoirs. It contrasts sharply with the adjoining limestone uplands of the White Peak and is named on account of the dark hues created in the landscape by the peat moors and exposed gritstone. Whilst this landscape character area contrasts with the White Peak, the transition to other landscape character areas such as the Dark Peak Eastern and Western Fringe landscapes is much more gradual; these are landscapes of similar character but tend to be lower lying, more settled and more intensively managed than the Dark Peak with enclosed farmland rather than open moorland predominating. The Eastern Moors to the south-east of the Dark Peak are similar to it in character but lower lying with less deep peat creating a landscape that has been more obviously modified by people than the Dark Peak generally has. In the north, the moorland plateau of the Dark Peak continues into the Southern Pennines. 2 Landscape Strategy and Action Plan Peak District National Park Authority 3: Dark Peak such as the golden plover and the dunlin. On the lower moorland Physical influences slopes heather dominates, with varying amounts of bilberry, The Dark Peak is an extensive area of high moorland and adjacent cowberry and crowberry.