Ig UIDE to GROUNDWATER VULNERABILITY MAPPING in ENGLAND and WALES National Rivers Authority
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A CRITICAL EVALUATION of the LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD of the CHALK UPLANDS of NORTHWEST EUROPE Lesley
A CRITICAL EVALUATION OF THE LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD OF THE CHALK UPLANDS OF NORTHWEST EUROPE The Chilterns, Pegsdon, Bedfordshire (photograph L. Blundell) Lesley Blundell UCL Thesis submitted for the degree of PhD September 2019 2 I, Lesley Blundell, confirm that the work presented in this thesis is my own. Where information has been derived from other sources, I confirm that this has been indicated in the thesis. Signed: 3 4 Abstract Our understanding of early human behaviour has always been and continues to be predicated on an archaeological record unevenly distributed in space and time. More than 80% of British Lower-Middle Palaeolithic findspots were discovered during the late 19th/early 20th centuries, the majority from lowland fluvial contexts. Within the British planning process and some academic research, the resultant findspot distributions are taken at face value, with insufficient consideration of possible bias resulting from variables operating on their creation. This leads to areas of landscape outside the river valleys being considered to have only limited archaeological potential. This thesis was conceived as an attempt to analyse the findspot data of the Lower-Middle Palaeolithic record of the Chalk uplands of southeast Britain and northern France within a framework complex enough to allow bias in the formation of findspot distribution patterns and artefact preservation/discovery opportunities to be identified and scrutinised more closely. Taking a dynamic, landscape = record approach, this research explores the potential influence of geomorphology, 19th/early 20th century industrialisation and antiquarian collecting on the creation of the Lower- Middle Palaeolithic record through the opportunities created for artefact preservation and release. -
Strategic Stone Study a Building Stone Atlas of Cambridgeshire (Including Peterborough)
Strategic Stone Study A Building Stone Atlas of Cambridgeshire (including Peterborough) Published January 2019 Contents The impressive south face of King’s College Chapel, Cambridge (built 1446 to 1515) mainly from Magnesian Limestone from Tadcaster (Yorkshire) and Kings Cliffe Stone (from Northamptonshire) with smaller amounts of Clipsham Stone and Weldon Stone Introduction ...................................................................................................................................................... 1 Cambridgeshire Bedrock Geology Map ........................................................................................................... 2 Cambridgeshire Superficial Geology Map....................................................................................................... 3 Stratigraphic Table ........................................................................................................................................... 4 The use of stone in Cambridgeshire’s buildings ........................................................................................ 5-19 Background and historical context ........................................................................................................................................................................... 5 The Fens ......................................................................................................................................................................................................................... 7 South -
Chapter 2 Physical Characteristics of the Study Area
CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area. -
Using the Solid Density to Assess Data Quality
Materials and Structures DOI 10.1617/s11527-015-0767-3 ORIGINAL ARTICLE Porosities of building limestones: using the solid density to assess data quality Christopher Hall . Andrea Hamilton Received: 15 June 2015 / Accepted: 16 December 2015 Ó The Author(s) 2016. This article is published with open access at Springerlink.com Abstract A good knowledge of the volume-fraction the solid density should always be calculated for this porosity is essential in any technical work on porous purpose when the Archimedes method is used. This materials. In construction materials the porosity is check can be useful also when porosities are measured commonly measured by the Archimedes buoyancy by helium pycnometry or by mercury intrusion method, from which the bulk density of the test porosimetry. specimen is also obtained. The porosity and the bulk density together fix the solid density of the specimen, Keywords Porosity Á Density Á Archimedes method Á as only two of the three quantities are independent. Limestone Á Calcite The solid density, although rarely discussed, is determined by the mineralogy of the specimen, and therefore can provide a valuable check on the accuracy 1 Introduction of porosity and bulk density measurements. Our analysis of published data on calcitic limestones Most inorganic construction materials, including the shows that the solid density is generally close to the main building stones, are porous. In research on ideal crystallographic density of calcite. Small devi- mechanics, transport, and durability in these materials, ations can often be traced to variations in mineral the porosity is often used as an explanatory (indepen- composition. However some published porosity–den- dent) variable, and so it is measured and reported as a sity data are inconsistent with the known mineralogy. -
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. -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
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. -
Mineral Resources Report for Wiltshire
Mineral Resource Information in Support of National, Regional and Local Planning Wiltshire (comprising Wiltshire and the Borough of Swindon) Commissioned Report CR/04/049N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/04/049N Mineral Resource Information in Support of National, Regional and Local Planning Wiltshire (comprising Wiltshire and the Borough of Swindon) G E Norton, D G Cameron, A J Bloodworth, D J Evans, G K Lott, I J Wilkinson, H F Burke, N A Spencer, and D E Highley This report accompanies the 1;100 000 scale map: Wiltshire (comprising Wiltshire and the Borough of Swindon) Mineral Resources Key words Mineral resource planning, Wiltshire, Swindon. Front cover Westbury Cement Works, Lafarge Cement UK (Blue Circle Cements), and Westbury White Horse. Bibliographical reference G E NORTON, D G CAMERON, A J BLOODWORTH, D J EVANS, G K LOTT, I J WILKINSON, H F BURKE, N A SPENCER, and D E HIGHLEY. 2004. Mineral Resource Information in Support of National, Regional and Local Planning. Wiltshire (comprising Wiltshire and the Borough of Swindon) British Geological Survey Commissioned Report, CR/04/049N. 12pp. Keyworth, Nottingham British Geological Survey 2004 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the British Geological Survey offices BGS Sales Desks at Nottingham, Edinburgh and London; see contact details below or shop online at Keyworth, Nottingham NG12 5GG www.geologyshop.com 0115B936 3100......................... Fax 0115B936 3200 e-mail: sales @bgs.ac.uk The London Information Office also maintains a reference www.bgs.ac.uk collection of BGS publications including maps for Online shop: www.geologyshop.com consultation. -
BGS Report, Single Column Layout
INDUSTRIAL CARBON DIOXIDE EMISSIONS AND CARBON DIOXIDE STORAGE POTENTIAL IN THE UK Report No. COAL R308 DTI/Pub URN 06/2027 October 2006 Contractor British Geological Survey Keyworth Nottingham NG12 5GG United Kingdom Tel: +44 (0)115 936 3100 By S. Holloway C.J. Vincent K.L. Kirk The work described in this report was carried out under contract as part of the DTI Carbon Abatement Technologies Programme. The DTI programme is managed by Future Energy Solutions. The views and judgements expressed in this report are those of the contractor and do not necessarily reflect those of the DTI or Future Energy Solutions First published 2006 © DTI 2006 Foreword This report is the product of a study by the British Geological Survey (BGS) undertaken for AEA Technology plc as part of agreement C/07/00384/00/00. It considers the UK emissions of carbon dioxide from large industrial point sources such as power stations and the potential geological storage capacity to safely and securely store these emissions. Acknowledgements The authors would like to thank the UK DTI for funding the work, and Dr Erik Lindeberg of Sintef Petroleum Research for provision of a programme to calculate the density of CO2. Contents Foreword.........................................................................................................................................i Acknowledgements.........................................................................................................................i Contents...........................................................................................................................................i -
Mid-Cretaceous Orbitolinids, from the Decoy Basin, Newton Abbot (Devon)
C. Nicholas and M.B. Hart MID-CRETACEOUS ORBITOLINIDS, FROM THE DECOY BASIN, NEWTON ABBOT (DEVON) C. NICHOLAS1 AND M.B. HART2 Nicholas, C. and Hart, M.B. 2004. Mid-Cretaceous orbitolinids from the Decoy Basin, Newton Abbot (Devon). Geoscience in south-west England, 11, xxx-yyy. Within the Upper Greensand (mid-Cretaceous) succession of the Decoy Basin cherts are regularly found to contain the benthic foraminiferid Orbitolina. This genus is a large agglutinated taxon that almost certainly lived in warm, shallow waters (by analogy to modern species). South-western England marks the most northerly limit of this genus, which has been recorded elsewhere in Devon and in the glauconitic sands of Cenomanian age found around the Haig Fras granite west of the Scilly Isles. The species identification is difficult as the preservation of the fauna, within chert, means that many of the detailed internal structures (on which the determination must be based) are missing. Previous work has indicated that the species is probably Orbitolina sp. cf. O. concava. This species characterises the lower Cenomanian in France and other regions of Europe and the Middle East. Recent work on Middle Eastern faunas has shown that the external shape of the specimens is controlled by the environment and can be used to place assemblages within a sequence stratigraphical context. The fauna from Zig Zag Quarry appear to indicate deposition in a transgressive sedimentary succession. 1David Roche Geo Consulting, 19 Richmond Road, Exeter, EX4 4JA, U.K. (E-mail: ) 2School of Earth, Ocean & Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, U.K. -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
An Investigation of the Petrockstowe and Bovey Basins, South West United Kingdom
CENOZOIC TERRESTRIAL PALAEOENVIRONEMTAL CHANGE: AN INVESTIGATION OF THE PETROCKSTOWE AND BOVEY BASINS, SOUTH WEST UNITED KINGDOM by MOHAMMED SULEIMAN CHAANDA A thesis submitted to Plymouth University for the partial fulfilment for the degree of DOCTOR OF PHILOSOPHY School of Geography, Earth and Environmental Sciences Faculty of Science and Technology May 2016 Copyright Statement This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rest with its author and that no quotation from the thesis and no information derived from it may be published without the author’s prior consent. Signed: Date: 25-05-2016 CENOZOIC TERRESTRIAL PALAEOENVIRONMENTAL CHANGE: AN INVESTIGATION OF THE BOVEY AND PETROCKSTOWE BASINS, SOUTH WEST UNITED KINGDOM, Mohammed S. Chaanda The Petrockstowe and Bovey basins are two similar pull apart (strike slip) basins located on the Sticklepath – Lustleigh Fault Zone (SLFZ) in Devon, SW England. The SLFZ is one of the several faults on the Cornubian Peninsula and may be linked to Variscan structures rejuvenated in Palaeogene times. The bulk of the basins’ fill consists of clays, silts, lignites and sands of Palaeogene age, comparable to the Lough Neagh Basin (Northern Ireland), which is also thought to be part of the SLFZ. In this study a multiproxy approach involving sedimentary facies analysis, palynological analysis, stable carbon isotope (δ13C) analysis and organic carbon palaeothermometer analyses were applied in an attempt to understand the depositional environment in both basins. A negative carbon isotope excursion (CIE) with a magnitude of 2‰ was recorded at ~ 580 m in the siltstone, silty clay to clay lithofacies in the 13 lower part of Petrockstowe Basin, with minimum δ CTOC values of -28.6‰.