DOCSLIB.ORG

Photographs of Bishop Monkton Borehole1

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Photographs of Bishop Monkton Borehole1 Ground Stability Assessment: Proposed Development - Church Farm, Bishop Monkton HG3 3RA G20280 Table of Contents Introduction ...................................................................................................... 3 Historical Subsidence Features ........................................................................... 4 The Pond ........................................................................................................... 4 Borehole Site Investigations ............................................................................... 7 Site Geology ...................................................................................................... 8 Field Pattern, Topography & Ground Stability .................................................... 9 Drift Condition & Ground Stability ..................................................................... 9 Bedrock Condition and Ground Stability ............................................................. 10 Comparative Instability Risk – Zone C Ripon ....................................................... 12 Foundation Design ............................................................................................. 13 Other Mitigation ................................................................................................ 13 Ground Stability Declaration .............................................................................. 13 TM Units 3a and 4 Terry Dicken Industrial Estate Ellerbeck Way Stokesley North Yorkshire TS9 7AE Tel. 01642 713779 Fax 01642713923 Email [email protected] www.geoinvestigate.co.uk 2 April 2021 Ground Stability Assessment: Proposed Development - Church Farm, Bishop Monkton HG3 3RA G20280 Introduction Phase Site Investigations provided Kebbell Homes with a geophysical survey report (Project ref GEO/2722/1023) for the site in November 2019. The Phase report is available from Kebbell Homes. It is not included in this report as it is assumed it will form part of the planning application for the Church Farm site by Kebbell Homes. The Phase report identifies two possible broadly liea iogait aoalies A ad B at the site. Anomaly A located in the north is larger and stronger, while B along the southeast site boundary is weaker and perhaps smaller. The geophysical report is uncertain whether the anomalies are gypsum related dissolution features speculating that they might instead arise from variations in geology, soil compaction or possibly even anthropogenic activity i.e., human activity concluding that the only way the uncertainty could be resolved was by intrusive investigation. Encouragingly the Phase SI report mentions that EM geophysical survey indicated that that there are no infilled troughs or peat deposits at the Church Farm site which are known to be associated with much older sinkhole activity in the Ripon area. The anomalies are indicated as BLUE areas in the subsequent desk study ground stability report carried out by Geoinvestigate, emailed to Mr Mike Mulligan of Kebbell Homes on 29 January 2020 and provided in Appendix A As part of the desk study the tentative rough historical subsidence hollow map provided in Appendix B was generated for the site and the surrounding area based on the OS map record dating from 1854. This base map was not included in the email of 29 January 2020 to Kebbell Homes. The map of 1891 is the first map showing a small circular water feature/spring or perhaps even a small embryonic sinkhole to the southeast of the site. Sometime after 1957 and by 1975 the feature is shown as a larger recognisable pond. The origin of the pond feature is discussed in Geoinvestigates early 2020 ground stability report and subsequently with Dr Tony Cooper in several informal email exchanges. Dr Cooper of the Natural Environment Research Council and the British Geological Survey, Emeritus is the UKs recognised leading authority on the egieeig geolog of ‘ipos gypsum dissolution problem. Subsequently, Dr Cooper was engaged late 2020 as a specialist consultant by Geoinvestigate to provide advice on the engineering geology of the gypsum beneath the Church Farm site and specifically to provide a report on two 45m and 50m deep rotary cored boreholes sunk at geophysical anomalies A & B in September 2020. Initially Geoinvestigate suggested that owing to the COVID pandemic and Dr Cooper shielding during this period that the core boxes were delivered to his home address to be logged by him. However, rather than receive core boxes it was felt safer for Dr Cooper to evaluate photographs of the core both in its original condition and split open (to remove surface smearing) and these were sent to him in April 2021. Subsequently Dr Cooper called for the core samples themselves to be delivered to his home for further preparation and detailed logging by him which was done in March 2021. www.geoinvestigate.co.uk 3 April 2021 Ground Stability Assessment: Proposed Development - Church Farm, Bishop Monkton HG3 3RA G20280 Dr Coopers detailed report on the borehole cores issued March is presented in Appendix C together his high- resolution core photographs. Dr Cooper is an accomplished amateur photographer. Folloig D Coopes loggig, the cores were picked-up and returned to Geoinvestigates Stokesley Head Office in April 2021 for longer term storage. Subsequently Geoinvestigate compiled logs of the cores incorporating Dr Coopers logging information. Geoiestigates logs ‘C ad ‘C at geophsial aoalies B ad A espetiel ae peseted i Appendix D Historical Subsidence Features The draft base map provided in Appendix B shows subsidence hollows, ponds, sinkhole collapse events, speculative ground water movement direction and other features of interest with respect to understanding the ground stability and gypsum dissolution situation local to the Village of Bishop Monkton and the Church Farm site. Following discussions with Dr Cooper two features, a pond which appeared sometime between 1851 – 1910, and a ground collapse c. 1830 occurring well to the west and east of the site respectively were added to the map. The appearances of the features or the first recording of them date mostly to the mid to late 1800s and early 1900s. Four ground water pumps (shown yellow circles) believed to be perhaps two wind and two hand pumps located in farmland and at a farmstead to the east of the site are shown on the map. It was speculated in Geoinvestigates desk study report that the formation of some of the subsidence hollows and ponds might be connected to ground water pumping in the late 1800s and early 1900s. As far as Geoinvestigate has been able to ascertain, few significant recent (within the last 80 years and probably longer) subsidence events/features have been reported/documented within and around the Village of Bishop Monkton and its immediate surrounding area. The Pond The ospiuous lage pepetual pond to the southeast of the site lies at a rim height of 34m AOD while the development area is at 37m to 38m rising locally to 39m AOD. Ground level rises gradually from the pond to the site. The pond occupies a wider depression/bowl crossed to the northwest by an ancient/old hawthorn hedge and the caravan park access track which may be slightly embanked. According to the site owner the pond outflows to the southwest onto lower lying ground where a second pond is formed intermittently. Recent 2020 images of the pond are shown in Appendix E On 26 April 2021 Ross Nicolson spoke to Emma Oates the landowner and the caravan site manager. According to her recollections the land was acquired some 23 years ago (1998) by her family/partners family. She grazes her horses in the pond field but had no recollection of the pond enlarging during this period or any excavation or infilling of it or raising of its banks. Her family had moved to Bishop Monkton in the 1950s and she was not aware of any ground instability event within the site or the pond or the village during this period. www.geoinvestigate.co.uk 4 April 2021 Ground Stability Assessment: Proposed Development - Church Farm, Bishop Monkton HG3 3RA G20280 With respect to the pond depth, she didt ko ut guessed it might be 2m or so placing its bottom at perhaps 32m AOD. Her horses didt ade ito the middle of it. Selected historical maps used to illustrate this section of the report are presented in Appendix F together with a recent Google satellite image of the pond. A full set of larger and smaller scale historical maps dating from 1852 are provided as part of the Phase 1 Desk Study reference materials in Appendix 1. The pond is first recorded as a small circular feature (perhaps a spring) on the OS map of 1891 and remains a small map feature up to 1957. By 1974/1975 it is shown as a larger feature of some 24m width x 29m length and 0.049ha area remaining the same size on the later map of 1989 – 1994 when it is shown some 62m from the southern site boundary. By 2003 the pond is much larger 35m x 55m, 0.197ha, and 4 times its previous surface area and now some 42m to 45m from the site boundary. The most recent Google satellite image suggests that the pond has not increased noticeably in surface area since 2003 though the northeast margin adjacent to Knaresborough Road and the east field line have perhaps been infilled in recent years. An image of possible infill material on its roadside rim is shown in the Appendix G. Much of the change in size of the pond and the subsidence arising from dissolution of the underlying gypsiferous bedrock may date from around 1960s perhaps slowing in recent
Load more

Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • IAEG2006 Field Trip Guide Ripon 1 GYPSUM DISSOLUTION
    CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive IAEG2006 Field Trip Guide Ripon GYPSUM DISSOLUTION GEOHAZARDS AT RIPON, NORTH YORKSHIRE, UK Anthony H.Cooper1 1British Geological Survey, Keyworth, Nottingham, NG12 5GG, e-mail:[email protected] Abstract: This guide is for a one-day field excursion to examine gypsum dissolution geohazards at Ripon in North Yorkshire. Gypsum is a highly soluble rock and under suitable groundwater flow conditions it can dissolve forming caves and karstic features including collapse and suffosion dolines. These have the capability of causing subsidence damage of the type that affects much of the Ripon area. The guide details the processes involved, the localities visited and some of the remedial measures undertaken. Résumé: Ce guide concerne l'excursion d'une journée ayant pour but d'étudier les géo-aléas liés à la dissolution du gypse à Ripon dans la région du North Yorkshire. Le gypse est une roche hautement soluble et, dans des conditions adéquates d'écoulement de l'eau souterraine, pouvant se dissoudre et engendrer des grottes et formes karstiques telles qu'effondrements et dolines de suffosion. Celles-ci peuvent causer des dégâts de subsidence du type de ceux qui touchent la plupart des alentours de Ripon. Ce guide fournit des explications sur les phénomènes mis en jeu, les localités visitées et quelques-unes des mesures prises pour remédier à ces problèmes. Keywords: subsidence, evaporites, aquifers, cavities, collapse, urban geosciences. INTRODUCTION Gypsum, hydrated Calcium Sulphate (CaSO4.2H2O), is attractive as satin spar, beautiful as carved alabaster, practical as plasterboard (wallboard), but the cause of a geological hazard capable of swallowing houses and collapsing dams.
    [Show full text]
  • Department of History YORKSHIRE POLITICS, 1658
    The University of Sheffield Department of History YORKSHIRE POLITICS, 1658 - 1688 being a ThesIs subitted for the Degree of Doctor of Philosophy by CffERYL AROLRRT Ui^ August, 1990 - 393 - APPENDIX - 394 - YORKSHIRE MEKBEPS OF THE COJ(ONS, 1679-1681 BOROUGH HP. 1, 2. .3. County + Henry Lord Fairfax * 4 * + Charles Lord Clifford 4 * * Aldborough x Henry Art]aington 4- Sir Godfrey Copley [1] * 4 4 Sir Bryan Stapleton 4 Sir John Reresby Cl] 1 Beverley + Sir John Hotham 4 4 4 + !icbael Varton • * * Boroughbridge x Sir Thonas Mauleverer * 4 * - Sir Henry Goodricke * Sir John Brookes Hedon x Sir Hugh Bethell * 4 d. -HenryGuy * 4 William Boynton [21 * * Hull x Leniuel Klngdon . * x Villia Raden Sir Michael Warton * * William Gee * 4 Knaresborough x Sir Thonas Slingsby 1 4 * + Villiain Stockdale * 4 * Kalton x Villiam Palines * 4 * x Sir Watklnson Payler # 4 * Northallerton + Sir Gilbert Gerard * 4 * x Sir Henry Calverley 4 4 4 Pontefract + Sir John Dawney * * * 4- Sir Patience Yard 1 * * Richmond x Thonas Cradock * 4 x Humphrey Wharton * * * John Darcy * Ripon - Sir Edind JennIngs 4 x Richard Sterne 4 * 4 Christopher Wandesford 4 * Scarborough x Villia Thompson * 4 + Francis Thompson * * * Thirsk + Sir VillIam Frankland 4 4 * x Hon. Nicholas Saunderson * 4 Sir William Ayscough * York + Sir John Hewley * 4 * x Sir Henry Thompson * * 4 - 395 - Key to Table of Yorkshire Xembers of the Coinons. 1679-1681 + voted in favour of the Exclusion bill division, 21 May 1679 - voted against the Exclusion bill division x absent on the Exclusion bill division (Source - Browning & Xilne, B,I,H,R,, xxiii (1950), 205-25.) Roman Type : new to parliament Bold Type Cavalier parliament X,P,, sane borough Underlined Cavalier parliament 1!.P., different borough Italics former I(.P.
    [Show full text]
  • Subsidence Hazards Caused by the Dissolution of Permian Gypsum in England: Geology, Investigation and Remediation
    SUBSIDENCE HAZARDS CAUSED BY THE DISSOLUTION OF PERMIAN GYPSUM IN ENGLAND: GEOLOGY, INVESTIGATION AND REMEDIATION A H Cooper, British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG. This is a recompiled version of the final draft of the published paper, it is presented with coloured versions of the figures and may differ slighly from the published edited version. Please respect copyright of BGS/NERC and refer to the final published version if you wish to quote the work. Published as: Cooper, AH. 1998. Subsidence hazards caused by the dissolution of Permian gypsum in England: geology, investigation and remediation. 265–275 in: Geohazards in engineering geology, Maund, JG, Eddleston, M (eds.). Geological Society of London. Special Publications in Engineering Geology, 15. ABSTRACT About every three years natural catastrophic subsidence, caused by gypsum dissolution, occurs in the vicinity of Ripon, North Yorkshire, England. Holes up to 35 m across and 20 m deep have appeared without warning. In the past 150 years, 30 major collapses have occurred, and in the last ten years the resulting damage to property is estimated at about £1,000,000. Subsidence, associated with the collapse of caves resulting from gypsum dissolution in the Permian rocks of eastern England, occurs in a belt about 3 km wide and over 100 km long. Gypsum (CaSO4.2H2O) dissolves rapidly in flowing water and the cave systems responsible for the subsidence are constantly enlarging, causing a continuing subsidence problem. Difficult ground conditions are associated with caves, subsidence breccia pipes (collapsed areas of brecciated and foundered material), crown holes and post-subsidence fill deposits.
    [Show full text]
  • Kirkby Malzeard Marriages 1653-1905
    KIRKBY MALZEARD MARRIAGES Page No -192- 1705/04/09 m A????? Thos & Mary Grainge 202 Abbot Dorothy otp & John Thompson ba Masham (B) wit David Greenhow Henry 1815/01/02 m 269 Lofthouse 1733/03/14 m Abbot John & Mary Wilson botp 212 1733/06/02 m Abbot Eleanor Kp & Wm Raper Grewelthorp 212 1779/12/13 m Abbot John ba & Mgt Greenhow sp botp (L) wit John Fell David Greenhow 239 Abbot Mary sp otp & Wm Wintersgill husbn Thornton le Street (B) wit Geo 1790/04/19 m 246 Burniston Mary Greenhow Thos Wilson Abbot Luke [Richd BT] Ripon & Mary Longbotham otp (B) wit R Longbotham 1823/09/23 m 275 Thos Bradbradberry 1752/05/05 m Abbott Wm Kerby & Mgt Duffield (B) Galwhey otp 220 1737/06/19 m Acres Mary Hartwith & Jas Wilson (B) 214 Acres Catherine sp & Chas Harrison shoemaker botp (B) wit Joseph Acres Mary 1760/02/25 m 225 Lacey 1770/07/17 m Acres John widr & Eliz Jackson sp botp (B) wit Thos & Esther Jackson 232 1710/09/16 m Adamson Chr Mickley & Mary Wilson 204 Addyman E_iz wid & Nicholas Darling husbn bth Hartwith otp (B) wit Thos Jullay 1790/12/05 m 247 John Wood 1767/12/30 m Addyman Wm weaver & Jane Edmundson sp botp (B) wit Geo Thirkill Wm Wood 230 1771/03/05 m Addyman John ba & Eliz Driver sp botp (B) wit Benjamin Grange Jas Addyman 233 1825/12/20 m Addyman John & Eliz Palliser bth Hartwith otp (B) wit John ?Gaddie? John 277 1742/11/03 m Air John Grantley par Ripon & Ellen Newis (B) otp 216 Airton Wm woolcomber Gargrave & Ann Close sp otp (B) wit Sarah Raynard Mary 1786/01/13 m 242 Reynard John Wood 1702/11/12 m Akers Ann Hartwith otp & Peter Parker
    [Show full text]