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3-D Bedrock Geology Model of the Permo-Triassic of Yorkshire and East Midlands
3-D Bedrock geology model of the Permo-Triassic of Yorkshire and East Midlands Geology and Landscape Southern Britain Programme Internal Report CR/06/091 BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE SOUTHERN BRITAIN PROGRAMME INTERNAL REPORT CR/06/091 The National Grid and other Ordnance Survey data are used with the permission of the 3-D Bedrock geology model of Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2006. the Permo-Triassic of Yorkshire Keywords and East Midlands Report; 3-D Model; Sherwood Sandstone Group; Mercia Mudstone Group; Sneinton Formation; Permian; Roxby Formation; Brotherton Ford, J., Napier, B., Cooper, A., Pharaoh, T., Vincent, C., Carney, Formation; Edlington Formation; J., Thorpe, S., Brayson, J. Cadeby Formation; Yellow Sands Formation; Basal Permian Breccia; Aquifer;. Front cover Model output showing faulted elevation grid for the base Sherwood Sandstone Group and the thickness of the Sherwood Sandstone Group Bibliographical reference FORD, J., NAPIER, B., COOPER, A., PHARAOH, T., VINCENT, C., CARNEY, J., THORPE, S., BRAYSON, J.. 2005. 3-D Bedrock geology model of the Permo-Triassic of Yorkshire and East Midlands. British Geological Survey Internal Report, CR/06/091. 39pp. 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 a full acknowledgement is given of the source of the extract. -
Developing a Geological Framework
21/2/12 GeolFrameworkPaper_postreview_v2acceptchanges_editorcomments New insights from 3D geological models at analogue CO2 storage sites in Lincolnshire and eastern Scotland, UK. Alison Monaghan1*, Jonathan Ford2, Antoni Milodowski2, David McInroy1, Timothy Pharaoh2, Jeremy Rushton2, Mike Browne1, Anthony Cooper2, Andrew Hulbert2 and Bruce Napier2 1 British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA, UK. 2 British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham, NG12 5GG, UK. * Corresponding author (email [email protected] (Approx.15,600 words in total, 25 figures) SUMMARY: Subsurface 3D geological models of aquifer and seal rock systems from two contrasting analogue sites have been created as the first step in an investigation into methodologies for geological storage of carbon dioxide in saline aquifers. Development of the models illustrates the utility of an integrated approach using digital techniques and expert geological knowledge to further geological understanding. The models visualize a faulted, gently dipping Permo-Triassic succession in Lincolnshire and a complex faulted and folded Devono-Carboniferous succession in eastern Scotland. The Permo-Triassic is present in the Lincolnshire model to depths of -2 km OD, and includes the aquifers of the Sherwood Sandstone and Rotliegendes groups. Model-derived thickness maps test and refine Permian palaeogeography, such as the location of a carbonate reef and its associated seaward slope, and the identification of aeolian dunes. Analysis of borehole core samples established average 2D porosity values for the Rotliegendes (16%) and Sherwood Sandstone (20%) groups, and the Zechstein (5%) and Mercia Mudstone (<10%) groups, which are favourable for aquifer and seal units respectively. Core sample analysis has revealed a complex but well understood diagenetic history. -
Devonian and Carboniferous Stratigraphical Correlation and Interpretation in the East Irish
CR/16/040 Last modified: 2016/05/30 11:40 Carboniferous stratigraphical correlation and interpretation in the Irish Sea Energy and Marine Geoscience Programme Commissioned Report CR/16/040 CR/16/040 Last modified: 2016/05/30 11:40 BRITISH GEOLOGICAL SURVEY ENERGY AND MARINE GEOSCIENCE PROGRAMME COMMISSIONED REPORT CR/16/040 Carboniferous stratigraphical correlation and interpretation The National Grid and other Ordnance Survey data © Crown Copyright and database rights in the Irish Sea 2015. Ordnance Survey Licence No. 100021290 EUL. Keywords O. Wakefield, C. N. Waters and N. J. P Smith Report; Stratigraphy, Carboniferous, East Irish Sea. Front cover View of the Great Orme, Llandudno, North Wales, comprising thick carbonate platform successions typical of the Carboniferous Limestone Supergroup of the Irish Sea and adjacent areas (P007274). ©BGS NERC Bibliographical reference Wakefield, O. Waters, C.N. and Smith, N.J.P. 2016. Carboniferous stratigraphical correlation and interpretation in the Irish Sea. British Geological Survey Commissioned Report, CR/16/040. 82pp. 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 a full acknowledgement is -
Garforth and Church Fenton
High Speed Two Phase 2b ww.hs2.org.uk October 2018 Working Draft Environmental Statement High Speed Rail (Crewe to Manchester and West Midlands to Leeds) Working Draft Environmental Statement Volume 2: Community Area report | Volume 2 | LA16 LA16: Garforth and Church Fenton High Speed Two (HS2) Limited Two Snowhill, Snow Hill Queensway, Birmingham B4 6GA Freephone: 08081 434 434 Minicom: 08081 456 472 Email: [email protected] H27 hs2.org.uk October 2018 High Speed Rail (Crewe to Manchester and West Midlands to Leeds) Working Draft Environmental Statement Volume 2: Community Area report LA16: Garforth and Church Fenton H27 hs2.org.uk High Speed Two (HS2) Limited has been tasked by the Department for Transport (DfT) with managing the delivery of a new national high speed rail network. It is a non-departmental public body wholly owned by the DfT. High Speed Two (HS2) Limited, Two Snowhill Snow Hill Queensway Birmingham B4 6GA Telephone: 08081 434 434 General email enquiries: [email protected] Website: www.hs2.org.uk A report prepared for High Speed Two (HS2) Limited: High Speed Two (HS2) Limited has actively considered the needs of blind and partially sighted people in accessing this document. The text will be made available in full on the HS2 website. The text may be freely downloaded and translated by individuals or organisations for conversion into other accessible formats. If you have other needs in this regard please contact High Speed Two (HS2) Limited. © High Speed Two (HS2) Limited, 2018, except where otherwise stated. Copyright in the typographical arrangement rests with High Speed Two (HS2) Limited. -
1. Ripon, a City of Just Under 17,000 People, Is 54 Degrees N and 1.5 Degrees West and Sits Near to the Northern End of the Sout
RIPON CITY PLAN Supporting Document: Sustainable Ripon Appendix A.n: Ripon’s Geodiversity Introduction 1. Ripon, a city of just under 17,000 people, is 54 degrees N and 1.5 degrees west and sits near to the northern end of the Southern Magnesian Limestone National Character Area (NCA 30) defined by the underlying Permian Zechstein Group, formerly known as the Magnesian Limestone. It creates a very long and thin area stretching from Thornborough in North Yorkshire to the outskirts of Nottingham. The limestones, marls and enclosed gypsum horizons create a ridge, or narrow belt of elevated land, running north–south and forming a prominent landscape feature. The geology has influenced the form of the landscape, the use of limestone for local building stone and mortar, the specialised limestone grasslands, and in Ripon’s case, and the villages to the north and south, produces unstable land and a particular topography that has defined its settlement history and has geographically limited development. 2. The key to the unique landscape and development of the settlement of Ripon is its geodiversity, defined as earth materials, landforms and processes that shape the Earth. The geodiversity is manifested as the rocks, minerals, soils, topography, rivers and landscape of the area. Ripon sits at 30m above sea level on fluvio-glacial and river terraces that form the higher land between the Ure, Laver and Skell valleys. In the recent past these rivers cut deeply into the underlying Permian deposits, especially to the west of the City, when the flow greatly increased with meltwater from the glaciers of the last Ice Age only 13,000 years ago. -
A Lithostratigraphical Framework for the Carboniferous Successions of Northern Great Britain (Onshore)
A lithostratigraphical framework for the Carboniferous successions of northern Great Britain (onshore) Research Report RR/10/07 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub- headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY The National Grid and other Ordnance Survey data are used RESEARCH REPOrt RR/10/07 with the permission of the Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2011. Keywords Carboniferous, northern Britain, lithostratigraphy, chronostratigraphy, biostratigraphy. A lithostratigraphical framework Front cover for the Carboniferous successions View of Kae Heughs, Garleton Hills, East Lothian. Showing of northern Great Britain Chadian to Arundian lavas and tuffs of the Garleton Hills Volcanic Formation (Strathclyde Group) (onshore) exposed in a prominent scarp (P001032). Bibliographical reference M T Dean, M A E Browne, C N Waters and J H Powell DEAN, M T, BROWNE, M A E, WATERS, C N, and POWELL, J H. 2011. A lithostratigraphical Contributors: M C Akhurst, S D G Campbell, R A Hughes, E W Johnson, framework for the Carboniferous N S Jones, D J D Lawrence, M McCormac, A A McMillan, D Millward, successions of northern Great Britain (Onshore). -
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. -
The Stratigraphic Nomenclature of the Irish Offshore Basins
The Stratigraphic Nomenclature of the Irish Offshore Basins Published by the Department of the Environment, Climate and Communications gov.ie Front cover: Sheet-like basin floor sandstone beds in the Pennsylvanian Ross Sandstone Formation, Loop Head, Co. Clare. The dark, heterogeneous unit in the centre of the picture is a laterally-extensive slump deposit. (Photo: Pat Shannon) Published in Ireland by the Department of the Environment, Climate and Communications 29-31 Adelaide Road Dublin, D02 X285 ____________________________________________________________________ The Stratigraphic Nomenclature of the Irish Offshore Basins Patrick M. Shannon1, Kara L. English2,3 & Michael Hanrahan2, 4 1UCD School of Earth Sciences, University College Dublin, Belfield, Dublin, D04 V1W8, Ireland. 2Petroleum Affairs Division, Department of Communications, Climate Action and Environment, 29-31 Adelaide Road, Dublin, D02 X285, Ireland. 3Present address: Stellar Geoscience, Dublin, and UCD School of Earth Sciences, University College Dublin, Belfield, Dublin, D04 V1W8, Ireland. 4Present address: Geoscience Regulation Office, Department of the Environment, Climate and Communications, 29-31 Adelaide Road, Dublin D02 X285, Ireland. ________________________________________________________________________ Bibliographic reference The Stratigraphic Nomenclature of the Irish Offshore Basins Department of the Environment, Climate and Communications, PAD Special Publication 2/21. Table of Contents 1. INTRODUCTION ............................................................................................................. -
BRITISH GEOLOGICAL SURVEY Natural Environment Research Council
BRITISH GEOLOGICAL SURVEY Natural Environment Research Council -CONFIDENTIAL UNTIL END OF 2005- TECHNICAL REPORT CR/00/94 Revised geological maps of Darlington based on new borehole information: explanation and description A H COOPER & J.GORDON Geographical index UK, County Durham, Darlington Subject index Geology, stratigraphy, boreholes, Permian, gypsum, dissolution, geohazards, subsidence Bibliographic Reference Cooper, A.H & J.Gordon. 2000. Revised geological maps of Darlington based on new borehole information: explanation and description. British Geological Survey Technical Report CR/00/94 ©NERC copyright 2000, Keyworth, British Geological Survey, 2000 SUMMARY The geology of the Darlington area has been revised based on the interpretation of new borehole information and a re-examination of archival data. The Permian Zechstein Group has been mapped through the district where it forms a series of easterly-dipping formations. These strata have been folded and an easterly-plunging syncline, faulted on its southern side, is mapped through the town of Darlington. This fold structure is partially modified by the dissolution of gypsum in the sequence resulting in the partial collapse and foundering of the strata. A series of maps is presented showing the revised geology, rockhead, drift thickness and the thickness of the gypsum sequence present at two horizons; the Hartlepool Anhydrite (present in the Edlington Formation) and the Billingham Anhydrite (present in the Roxby Formation). A series of five structure contour maps are presented -
Triassic: Seasonal Rivers, Dusty Deserts and Saline Lakes
Triassic: seasonal rivers, dusty deserts and saline lakes Ruffell, A., & Hounslow, M. (2006). Triassic: seasonal rivers, dusty deserts and saline lakes. In P. F. Rawson, & P. Brenchley (Eds.), The Geology of England & Wales. (pp. 295-325). Geological Society of London. Published in: The Geology of England & Wales. Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:28. Sep. 2021 Triassic: seasonal rivers, 13 dusty deserts and saline lakes M. W. HOUNSLOW & A. H. RUFFELL The collision of Siberia and the Kazakstan microplate with European palaeoenvironmental signatures the eastern side of the Fennoscandia continent in the Permian amalgamated the last major continental fragments to produce The Permian witnessed the fragmentation of the core of the the supercontinent Pangaea, which persisted into the Jurassic Variscan Mountains into a number of separate areas, such as the Armorican, Bohemian and Iberian massifs (Fig. -
BGS Report, Single Column Layout
Doncaster Geodiversity Assessment Volume 1 – Report Geology and Landscape South Programme Commissioned Report CR/07/025N BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE SOUTH PROGRAMME COMMISSIONED REPORT CR/07/025N Doncaster Geodiversity Assessment Volume 1 – Report S Engering and H F Barron The National Grid and other Ordnance Survey data are used with the permission of the Contributors Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2007. Keywords Geodiversity; Doncaster. Editor Front cover A H Cooper Permian Bryozoan reef, North Cliff Quarry, Doncaster Bibliographical reference ENGERING, S & BARRON, H F. 2007. Doncaster Geodiversity Assessment. British Geological Survey Commissioned Report, CR/07/025N. 139pp. 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 a full acknowledgement is given of the source of the extract. Maps and diagrams in this report use topography based on Ordnance Survey mapping. © NERC 2007. All rights reserved Keyworth, Nottingham British Geological Survey 2007 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS British Geological Survey offices Sales Desks at Nottingham, Edinburgh and London; see contact details below or shop online at www.geologyshop.com Keyworth, Nottingham NG12 5GG The London Information Office also maintains a reference 0115-936 3241 Fax 0115-936 3488 collection of BGS publications including maps for consultation. -
Back Matter (PDF)
PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 355 INDEX TO VOLUME 47 prepared by A. S. HOWARD General Index Liesegang rings, origin 42 Boreholes magnetic survey, Tertiary dyke 200ff. Chronostratigraphy metalliferous deposits, mining of 1-2 Lithostratigraphy mica crystallinity, Skiddaw Group 327ff. Localities mineralisation, Northern Pennine Orefield Iff. Minerals molluscs, late Quaternary 127-129 New taxa MOSELEY, F., Sorby medallist 280-281 mylonites, Permo-Carboniferous, Shetland 339ff. Market Weighton anomaly 47ff. GENERAL INDEX Mid North Sea High, late Permian palaeogeography 313ff. Midland Valley, Lower Carboniferous stratigraphy 215ff. 150th Anniversary celebrations 96-102 Moore Medal 281-282 acritarchs, Ordovician 271-274 North Sea, late Permian palaeogeography 313ff. amygdales, Whin Sill 250-251 North Yorkshire, Craven Reef Belt 55ff. Annual Report 1988 277-279 North Yorkshire, Middle Jurassic palynostratigraphy 349ff. aplites, Whin Sill 251 North Yorkshire, Rhaetian 29ff. brachiopods, Lower Carboniferous I3ff., 55ff. North Yorkshire, Westbury Formation 29ff. brachiopods, functional morphology 18-19,59-62 North Yorkshire, field meeting 105-106 brachiopods, palaeoecology 62-63 North-east England, Upper Permian 33ff., 285ff. brachiopods, productoid 13ff., 55ff. North-east England, late Permian palaeogeography 285ff., 313ff. Borders Region, Tertiary dyke 199ff. North-west England, metamorphic history 325ff. cannon-ball concretions 35-36 North Pennine Orefield, mineralisation Iff. carbonate beds, Coal Measures 195-196 Northern Pennines, structural history 2-4 climatic change, late Quaternary 127ff. Northumberland, dolerite-pegmatites 249ff. coleoid cephalopods, late Jurassic 149ff. ostracods, late Quaternary 129-131 concretions, calcitization and compaction 35-40 palaeokarst, Dinantian 345ff. coralline concretions 37 palaeontology, Dinantian rugose corals 155ff., 233ff. corals, Dinantian 155ff. palaeontology, Dinantian trilobites 163ff. corals, Visean biostratigraphy of 233ff.