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ON the ROCKS Newsletter of the Yorkshire Branch of the Open University Geological Society March 2018
ON THE ROCKS Newsletter of the Yorkshire Branch of the Open University Geological Society March 2018 A view of Great Gable (899m – the 9th highest mountain in England), Cumbria, looking northeast from the end of Wast Water, where the River Irt starts its short journey to the Irish Sea. Wast Water is the deepest lake in England (76m). The mountains are all from the Borrowdale Volcanic Group. (Peter Roberts 27.3.17 Grid Ref: NY 14535 03878) Welcome to the Spring edition of your newsletter Contents I hope you enjoy reading it and feel inspired to contribute to future issues. I must 1. Editor’s piece start with an apology. Unfortunately, the minutes of the AGM are not yet available 2. Rick’s musings but will be appearing in the next issue along with a copy of the accounts. 3. - 6. Blencathra report 7. Guide to minerals Our main article this time is the first of a number of reports by Peter Vallely on last 7. Obituary autumn’s Blencathra trip, and, if the photos are anything to go by, the hardy 8. Climate change article participants enjoyed a lovely sunny, if rather chilly, day out. 9. YOUGS 2018 field trips Peter Roberts has kindly provided the above photo, and we have another “simple 10. Snippets guide to minerals”, David Cousins’ personal view on surviving climate change, an 11. 2018 Blencathra obituary to Bill Graham who was a long-time Branch member, and a full listing of this year’s field trips, including separate details of this year’s Blencathra trip. -
Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from Gravity Survey and Structural Inversion
ESSOAr | https:/doi.org/10.1002/essoar.10501104.1 | CC_BY_NC_ND_4.0 | First posted online: Mon, 11 Nov 2019 01:27:37 | This content has not been peer reviewed. Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from gravity survey and structural inversion Rob Westaway 1,*, Sean M. Watson 1, Aaron Williams 1, Tom L. Harley 2, and Richard Middlemiss 3 1 James Watt School of Engineering, University of Glasgow, James Watt (South) Building, Glasgow G12 8QQ, UK. 2 WSP, 70 Chancery Lane, London WC2A 1AF, UK. 3 School of Physics, University of Glasgow, Kelvin Building, Glasgow G12 8QQ, UK. * Correspondence: [email protected]; Abstract: The Butterknowle Fault is a major normal fault of Dinantian age in northern England, bounding the Stainmore Basin and the Alston Block. This fault zone has been proposed as a source of deep geothermal energy; to facilitate the design of a geothermal project in the town of Bishop Auckland further investigation of its geometry was necessary and led to the present study. We show using three-dimensional modelling of a dense local gravity survey, combined with structural inversion, that this fault has a ramp-flat-ramp geometry, ~250 m of latest Carboniferous / Early Permian downthrow having occurred on a fault surface that is not a planar updip continuation of that which had accommodated the many kilometres of Dinantian extension. The gravity survey also reveals relatively low-density sediments in the hanging-wall of the Dinantian fault, interpreted as porous alluvial fan deposits, indicating that a favourable geothermal target indeed exists in the area. -
Short Walks Group
SHORT WALKS GROUP We’ve been blessed with good weather this spring so have been able to walk each month though the March walk had to be altered as the ground was so boggy and muddy. 11th March The walk was changed to a shortish road walk from the Derby Arms at Witherslack with refreshments at the pub afterwards. A good group of walkers joined the walk including my husband Chris on his scooter. After a spell of bad weather everyone was delighted to have a pleasant day and get out and enjoy a walk. We walked the old road to Millside and then up the quiet lane to Beckhead where the stream appears from under the rocks – a wonderfully tranquil spot. We carried on a short distance to where the lane ends and stopped for coffee. We then retraced our steps past some wonderful houses at Beckhead to Millside where we deviated down a short path to see the old millwheel- now part of someone’s garden. Back to the road we wound our way along the quiet lanes back to the Derby Arms for a welcome drink. 8th April It was a cold but bright day, and nineteen intrepid walkers gathered in Gummer’s Howe Car Park. A very pleasant 5 miler on good paths across pasture and fell side with magnificent views all the way lay ahead. We were all surprised how busy the car park was, but then realised that it was half term for Cumbria. Several family groups were headed for Gummer’s Howe, but not us. -
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. -
Northern England Regional Geology RWM | Northern England Regional Geology
Northern England regional geology RWM | Northern England Regional Geology Contents 1 Introduction Subregions Northern England: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks 3 Older sedimentary rocks Basement rocks 4 Rock structure 5 Groundwater 6 Resources 7 Natural processes Further information 8 - 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 | Northern England Regional Geology Introduction This region comprises Cumbria, Northumberland, Durham and Tyne and Wear and parts of Lancashire and Yorkshire. The region includes the adjacent inshore areas which extend to 20km from the coast in the east and west and the Scottish border defines the northern boundary. Subregions To present the conclusions of our work in a concise and accessible way, we have divided the region into 5 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. -
Eden Valley Fringe
1 Valley of Dalebanks Beck, to the west of Crosby Ravensworth of Crosby the west Beck, to of Dalebanks Valley LCA 1 Eden Valley Fringe Yorkshire Dales National Park - Landscape Character Assessment YORKSHIRE DALES NATIONAL PARK LANDSCAPE CHARACTER ASSESSMENT LANDSCAPE CHARACTER AREAS 2 LCA 1 Eden Valley Fringe Key characteristics • Sheltered and enclosed farmland landscape on gently undulating slopes of the small tributary valleys of the River Eden which run north-east from the Orton Fells limestone plateau • The steep becks on the edge of the limestone plateau flow sporadically, but there is a dense network of small, winding streams within the valleys and throughout the lowland valley fringe landscape • Well settled landscape with spring-line villages on the edge of the fells to the south and nucleated stream-side villages within the valleys • Small-scale, historic field pattern on fringes of villages, with strong patterns of long tofts defined by walls, and isolated farmsteads • Fields are enclosed by limestone walls on the fringes of the limestone plateau and by a mixture of stone walls and hedgerows within the valleys. • Narrow tree lined gills and becks are perceptible in the more open upper valley landscapes as wooded features; small blocks of woodland, tree belts and hedgerow trees create a fairly enclosed landscape character overall • Small historic villages, built with local limestone and ‘pink’ sandstone, often centred on long greens • Villages are connected by a network of winding, narrow lanes, which are often enclosed by tall hedgerows. • Occasional long views from the upper valley slopes across the Eden Valley Fringe LCA to the upland ridges of the North Pennines and Cumbrian Fells to the north and west. -
The Historic County of Westmorland
The Historic County of Westmorland A Case Study on the range, availability and usefulness of publications relating to the Historic County of Westmorland, and on the current provision of support for Local Historical Studies, with specific reference to the county town of Kendal Contents Introduction 3 Purpose and Scope of the Report 3 The Historic County of Westmorland 4 A Survey and Critical Evaluation of the Scholarly Resources Relevant to the History of the County of Westmorland, and to the County Town of Kendal, from the Early Modern Period to the Present Day Antiquarians and Archive Makers of the 16th and 17th Centuries 6 The First County History in Print 12 In Search of the Picturesque/Losing sight of the Goal 13 Late 19th Century Foundation of Modern Historical Scholarship 15 The Historical Society and the Victoria County History 16 Local History Groups 17 Contemporary Narratives for Kendal 18 An Assessment of Current Provision for Local History Studies in Westmorland and the County Town of Kendal Libraries and Archives 19 Online/Digital Resources 20 Conclusion 21 Bibliography 22 Appendices 26 Appendix I Annotated Lists of Published Resources Appendix Ia Selected 16th & 17th Century Scholarship Appendix Ib Selected 18th Century Scholarship Appendix Ic Selected 19th Century Scholarship Appendix Id Selected Modern Scholarship Appendix Ie Selected Cartographic Evidence Appendix If Selected Resources for Kendal Appendix II Libraries, Archives and Record Offices Appendix III Historical Societies and Local History Groups Appendix IV Online/Digital Resources Illustrations Cover: Detail from William Hole’s county map of ‘Cumberlande, Westmorlande’ of 1622, created to illustrate Michael Drayton’s 15,000-line poem the Poly-Olbion P4: ‘The Countie Westmorland and Kendale the Cheif Towne Described with the Arms of Such Nobles as have been Earles of Either of Them’. -
NYM-Landscape-Character-Assessment-Reduced.Pdf
WHITE YOUNG GREEN ENVIRONMENTAL NORTH YORK MOORS NATIONAL PARK LANDSCAPE CHARACTER ASSESSMENT CONTENTS Page No 1.0 INTRODUCTION 1 1.1 Background to the Report 1 1.2 The North York Moors National Park 1 1.3 Context and Scope of the Study 1 1.4 The Study Area 2 1.5 Relationship to Previous Studies 2 1.6 Relationship to Studies Undertaken within Areas Bounding the National Park 5 1.7 Methodology 6 1.8 Structure of the Report 7 1.9 The Next Steps 7 2.0 THE NORTH YORK MOORS NATIONAL PARK 8 2.1 Key Characteristics 8 2.2 Landscape Character 8 2.3 Physical Influences 9 2.4 Historical and Cultural Influences 10 2.5 Buildings and Settlement 11 2.6 Land Cover 11 3.0 CHANGE IN THE LANDSCAPE 13 3.1 Introduction 13 3.2 Agriculture 13 3.3 Upland Management 15 3.4 Biodiversity Aims 15 3.5 Trees, Woodland and Commercial Forestry 16 3.6 Recreation and Tourism 17 3.7 Settlement Change and Expansion 18 3.8 Communications, Power Generation and Distribution, Military Infrastructure 18 3.9 Roads and Traffic 19 3.10 Mining and Quarries 20 3.11 External Influences 20 3.12 Air Pollution and Climate Change 20 3.13 Geological and Archaeological Resource 20 4.0 LANDSCAPE CHARACTER TYPES AND AREAS 22 Moorland 23 (1a) Western Moors 26 (1b) Central & Eastern Moors 27 (1c) Northern Moors 29 Narrow Moorland Dale 34 (2a) Ryedale 37 (2b) Bilsdale 38 (2c) Bransdale 39 (2d) Farndale 40 (2e) Rosedale 41 (2f) Hartoft 42 (2g) Baysdale 42 (2h) Westerdale 43 (2i) Danby Dale 43 North York Moors National Park Authority North York Moors National Park Landscape Character Assessment -
Eden-Swim-ST.Pdf
Swimming the Eden L-r: Mike Field, Robbie Hudson, Jack Hudson, Calum Hudson and Mark Thurstan at Stanwix bridge. Mike and Mark were part of the Outdoor Swimming Society’s adventure swim The Eden Project series and won a ballot to join the Hudson brothers for the last two days, hence Brothers Calum, Jack and Robbie Hudson returned to the red caps their Cumbrian roots to become the first people to swim the 90-mile length of the River Eden. Cath Harris reports Swimming the Eden Swim route ‘The brothers endured hours of hree brothers have swum, slid and could do,’ he says. ‘It was a bit like Swallows River Eden: 90 miles in nine days cold and suffered bruises, cuts and, scrambled the entire length of and Amazons.’ Day 1 Saturday August 15 – Hell Gill to Kirkby one of England’s longest rivers, The 90-mile adventure was conceived by Stephen 11.5 miles in Calum’s case, the torment of a raising funds for swim teaching at Calum, 26, who wanted to ‘create something a Notable challenges: Hell Gill waterfall, scramble to the same time. Calum, Jack and little bit different and unique’. He sensed his the source will require overnight camping. Access: severe three-day ear ache’ Robbie Hudson completed their own stagnation in a London office job and will have to hike to the source, no kayaks required. mammoth challenge in the chilly mass-participation swims and triathlons were Pick-up: Bridge with river access. waters of the Solway Firth nine days after no longer sufficiently satisfying. -
Geology Around Kirkby Stephen Mid-Week Geology Group. Monday
Geology around Kirkby Stephen Mid-Week Geology Group. Monday 8th May 2017 Kirkby Stephen Nateby Kirkby Stephen Station Wharton Hall Looking north toward Kirkby Stephen showing route for the day. Full distance (station - station) is 6km on a mixture of paths and tracks. Brockram St Bees Sandstone Bill Fraser. April 2017 Geology around Kirkby Stephen Kirkby Stephen is situated in the southern (upper) end of the Vale of Eden surrounded by the Pennines to the north and east, the Howgill and Lakeland hills to the west and is underlain by rocks of Carboniferous and Permo-Triassic ages. NFF SF Alston Block PFS BF Vale of Eden LF Stainmore Trough DL Lake Kirkby District Stephen Askrigg DF Block Based on Fig 2 British Regional Geology: Northern England with the permission of the British Geological Survey Faults DF Dent Fault DL Dent Line PFS Pennine Fault System SF Stublick Fault NFF Ninety Fathom Fault LF Lunedale Fault BF Butterknowle Fault Outline geology of northern England Geological History Late in the Devonian and continuing until the end of the Visean in the Carboniferous, north-south extensional tectonics created a series of fault controlled subsiding basins between elevated blocks. The fault zones developed along pre-existing lines of weakness in the underlying Lower Palaeozoic rocks that had been formed during the closing of Iapetus. Movements on these faults, as well as changes in sea level, strongly affected deposition throughout Carboniferous times. Following this the fault zones were reactivated a number of times: (i) at the end of the Carboniferous during the main Variscan (Hercynian) Orogeny when E - W crustal extension resulted in the formation of a half-graben that influenced deposition during Permo-Triassic times. -
The Palaeoglaciology of the Central Sector of the British and Irish Ice Sheet: Reconciling Glacial Geomorphology and Preliminary Ice Sheet Modelling
This is a repository copy of The palaeoglaciology of the central sector of the British and Irish Ice Sheet: reconciling glacial geomorphology and preliminary ice sheet modelling. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/83244/ Article: Evans, D.J.A., Livingstone, S.J., Vieli, A. et al. (1 more author) (2009) The palaeoglaciology of the central sector of the British and Irish Ice Sheet: reconciling glacial geomorphology and preliminary ice sheet modelling. Quaternary Science Reviews, 28 (7-8). 739 - 757. ISSN 0277-3791 https://doi.org/10.1016/j.quascirev.2008.05.011 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 The palaeoglaciology of the central sector of the British and Irish Ice Sheet: reconciling glacial geomorphology and preliminary ice sheet modelling. -
Mid-Week Geology Group Newsletter November 2018
Mid-Week Geology Group Newsletter November 2018 John Williams Sheila Wilson Margaret Crawford Barry Tymon Programme planner Communications Treasurer Webmaster This is John’s last Newsletter before he stands down as Programme Planner. It takes our Programme to the end of May 2019. So far no individual has offered to replace John in this crucial role longer term. Meanwhile, to ensure continuity, I am pleased to report that three members have agreed to become part of a small sub group to arrange one or two events each next year. If anyone else wishes to become involved, please contact Sheila before the AGM. This newsletter provides further information on the 2019 Programme that was outlined in the June 18 Newsletter, with details of meeting points and what each event will cover. Our numbers have increased to 55 this year but actual attendance numbers at some events has reduced. Maybe some meetings are too far for some members? Or is it that most local locations have already been visited in recent years? We would like to discuss this issue further at the AGM. Our theme for the past two years as highlighted at the Skipton meeting is “How Geology Has Generated Industry in Yorkshire”. Many of our walks in 2017, 2018 and 2019 demonstrate this theme. The topic for our December AGM, however, seems to break away from this theme. Now that we know so much about the geology of our own planet, - as demonstrated by the many talks on faraway places that we have covered on recent Members Days – we will find out what the other rocky planets and moons of the Solar System may offer for the future.