3D Groundwater Vulnerability
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The Carboniferous Bowland Shale Gas Study: Geology and Resource Estimation
THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION The Carboniferous Bowland Shale gas study: geology and resource estimation i © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Disclaimer This report is for information only. It does not constitute legal, technical or professional advice. The Department of Energy and Climate Change does not accept any liability for any direct, indirect or consequential loss or damage of any nature, however caused, which may be sustained as a result of reliance upon the information contained in this report. All material is copyright. It may be produced in whole or in part subject to the inclusion of an acknowledgement of the source, but should not be included in any commercial usage or sale. Reproduction for purposes other than those indicated above requires the written permission of the Department of Energy and Climate Change. Suggested citation: Andrews, I.J. 2013. The Carboniferous Bowland Shale gas study: geology and resource estimation. British Geological Survey for Department of Energy and Climate Change, London, UK. Requests and enquiries should be addressed to: Toni Harvey Senior Geoscientist - UK Onshore Email: [email protected] ii © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Foreword This report has been produced under contract by the British Geological Survey (BGS). It is based on a recent analysis, together with published data and interpretations. Additional information is available at the Department of Energy and Climate Change (DECC) website. https://www.gov.uk/oil-and-gas-onshore-exploration-and-production. This includes licensing regulations, maps, monthly production figures, basic well data and where to view and purchase data. -
Der Europäischen Gemeinschaften Nr
26 . 3 . 84 Amtsblatt der Europäischen Gemeinschaften Nr . L 82 / 67 RICHTLINIE DES RATES vom 28 . Februar 1984 betreffend das Gemeinschaftsverzeichnis der benachteiligten landwirtschaftlichen Gebiete im Sinne der Richtlinie 75 /268 / EWG ( Vereinigtes Königreich ) ( 84 / 169 / EWG ) DER RAT DER EUROPAISCHEN GEMEINSCHAFTEN — Folgende Indexzahlen über schwach ertragsfähige Böden gemäß Artikel 3 Absatz 4 Buchstabe a ) der Richtlinie 75 / 268 / EWG wurden bei der Bestimmung gestützt auf den Vertrag zur Gründung der Euro jeder der betreffenden Zonen zugrunde gelegt : über päischen Wirtschaftsgemeinschaft , 70 % liegender Anteil des Grünlandes an der landwirt schaftlichen Nutzfläche , Besatzdichte unter 1 Groß vieheinheit ( GVE ) je Hektar Futterfläche und nicht über gestützt auf die Richtlinie 75 / 268 / EWG des Rates vom 65 % des nationalen Durchschnitts liegende Pachten . 28 . April 1975 über die Landwirtschaft in Berggebieten und in bestimmten benachteiligten Gebieten ( J ), zuletzt geändert durch die Richtlinie 82 / 786 / EWG ( 2 ), insbe Die deutlich hinter dem Durchschnitt zurückbleibenden sondere auf Artikel 2 Absatz 2 , Wirtschaftsergebnisse der Betriebe im Sinne von Arti kel 3 Absatz 4 Buchstabe b ) der Richtlinie 75 / 268 / EWG wurden durch die Tatsache belegt , daß das auf Vorschlag der Kommission , Arbeitseinkommen 80 % des nationalen Durchschnitts nicht übersteigt . nach Stellungnahme des Europäischen Parlaments ( 3 ), Zur Feststellung der in Artikel 3 Absatz 4 Buchstabe c ) der Richtlinie 75 / 268 / EWG genannten geringen Bevöl in Erwägung nachstehender Gründe : kerungsdichte wurde die Tatsache zugrunde gelegt, daß die Bevölkerungsdichte unter Ausschluß der Bevölke In der Richtlinie 75 / 276 / EWG ( 4 ) werden die Gebiete rung von Städten und Industriegebieten nicht über 55 Einwohner je qkm liegt ; die entsprechenden Durch des Vereinigten Königreichs bezeichnet , die in dem schnittszahlen für das Vereinigte Königreich und die Gemeinschaftsverzeichnis der benachteiligten Gebiete Gemeinschaft liegen bei 229 beziehungsweise 163 . -
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. -
Dales Trails NORTH YORKSHIRE
10/10/2017 Dales Trails |Home | Calendar | Trans-Dales Trail 1 | Trans-Dales Trail 2 | Trans-Dales Trail 3 | Go walking with Underwood | Dales Trails NORTH YORKSHIRE - Hovingham A good walk for any time of the year across the rolling wooded countryside of the Howardian Hills, following a part of the Ebor Way via Terrington. Fact File 17.5km (11½miles) - but can be Distance shortened to 13.5km (8½ miles) Time 4 hours OS Explorer 300 (Howardian Hills & Map Malton) Park at the village hall (next to the Malt Start/Parking Shovel inn) Grid Ref: SE 668757 Field paths, bridleways & minor roads. Terrain Can be muddy in places Grade *** (moderate) nearest Town Malton McConnellTHOMAS organic, local, fair traded general store, deli and web café in Hovingham; Refreshments Spa Tearoom, Hovingham; Village Shop Cafe in Terrington; Pubs in Hovingham and Terrington Toilets none Public 194/195 from Malton or Helmsley. http://www.dalestrails.co.uk/Hovingham.htm 1/4 10/10/2017 Dales Trails Transport Moorsbus in Summer months Suitable for for everyone. Stiles 5 Image produced from the Ordnance Survey Get-a-map service. Image reproduced with kind permission of Ordnance Survey and Ordnance Survey of Northern Ireland. 1. (Start) From the car park at the village hall turn left (south) and walk past the Worsley Arms Hotel. At the corner, cross the road to join the footpath heading up hill. Walk up the road for about 200m and take the track forking left (SP Terrington). This track crosses open farmland with views back to the North York Moors, before dropping down into woodland. -
The Meadows, West Lane, Worston, Clitheroe BB7 1QA Proposed
The Meadows, West Lane, Worston, Clitheroe BB7 1QA Proposed alterations to existing garage to create annexe accommodation. Planning Statement JDTPL0258 Judith Douglas BSc (Hons), Dip TP, MRTPI August 2016 JDTPL 0026 8 Southfield Drive, West Bradford, Clitheroe, Lancashire, BB7 4TU Telephone: 01200 425051 Mobile: 07729 302644 Email: [email protected] Website: www.jdouglastownplanning.co.uk Page 1 of 9 Registered Office: 8 Southfield Drive, West Bradford Road, Clitheroe, Lancashire, BB7 4TU. Incorporated in England No. 09911421 The Meadows, West Lane, Worston July 2020 STATEMENT IN SUPPORT OF A PLANNING APPLICATION FOR PROPOSED ALTERATIONS TO AN EXISTING GARAGE TO CREATE ANNEXE ACCOMMODAITON TO BE USED IN CONNECTION WITH THE DWELLING AT THE MEADOWS, WEST LANE, WORSTON BB7 1QA 1 INTRODUCTION 1.1 This planning statement has been prepared by Judith Douglas Town Planning Ltd in support of a householder application to adapt the existing domestic outbuilding to annexe for leisure use and to provide accommodation for family guests. 1.2 This statement provides a description of the site and the proposed development, its compliance with the development plan and an assessment of other material considerations. It should be read in conjunction with the accompanying information: 6073 01 Existing plans and elevations 6073 03 Proposed plans and elevations Site plan 1:500 Location plan. 1:2500 2.0 THE APPLICATION SITE AND SURROUNDING AREA 2.1 The Meadows is a large detached house set within a large garden area to the east of West Lane, Worston it was built in the 1930’s. A large detached garage outbuilding is set within the garden to the south. -
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 -
Baseline Report Series: 14
Baseline Report Series: 14. The Corallian of Oxfordshire and Wiltshire Groundwater Systems and Water Quality Commissioned Report CR/04/262N Science Group: Air, Land & Water Technical Report NC/99/74/14 The Natural Quality of Groundwater in England and Wales A joint programme of research by the British Geological Survey and the Environment Agency BRITISH GEOLOGICAL SURVEY Commissioned Report CR/04/262N ENVIRONMENT AGENCY Science Group: Air, Land & Water Technical Report NC/99/74/14 This report is the result of a study jointly funded by the British Baseline Report Series: Geological Survey’s National Groundwater Survey and the 14. The Corallian of Oxfordshire and Environment Agency Science Group. No part of this work may be Wiltshire reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright proprietors. J Cobbing, M Moreau, P Shand, A Lancaster All rights are reserved by the copyright proprietors. Contributors Disclaimer The officers, servants or agents of both the British Geological Survey and the R Hargreaves (GIS) Environment Agency accept no liability whatsoever for loss or damage arising from the interpretation or use of the information, or reliance on the views contained herein. Environment Agency Dissemination status Internal: Release to Regions External: Public Domain ISBN: 978-1-84432-639-6 Product code: SCHO0207BLYL-E-P ©Environment Agency, 2004 Statement of use This document forms one of a series of reports describing the baseline chemistry of selected reference aquifers in England and Wales. Cover illustration Shelly, oolitic Corallian limestone near Baulking, Vale of White Horse. -
Forest of Bowland AONB PO Box 9, Guild House Cross Street, Preston, PR1 8RD Tel:01772 531473 Fax: 01772 533423 [email protected]
Sense of Place Toolkit Forest of Bowland AONB PO Box 9, Guild House Cross Street, Preston, PR1 8RD Tel:01772 531473 Fax: 01772 533423 [email protected] www.forestofbowland.com The Forest of Bowland Area of Outstanding Natural Beauty (AONB) is a nationally protected landscape and internationally important for its heather moorland, blanket bog and rare birds. The AONB is managed by a partnership of landowners, farmers, voluntary organisations, wildlife groups, recreation groups, local councils and government agencies, who work to protect, conserve and enhance the natural and cultural heritage of this special area. Lancashire County Council acts as the lead authority for the Forest of Bowland AONB Joint Advisory Committee a partnership comprising: Lancashire County Council, North Yorkshire County Council, Craven District Council, Lancaster City Council, Pendle Borough Council, Preston City Council, Ribble Valley Borough Council,Wyre Borough Council, Lancashire Association of Parish and Town Councils,Yorkshire Local Councils Association, NWDA, DEFRA, Countryside Agency, United Utilities plc, Environment Agency, English Nature, Royal Society for the Protection of Birds (RSPB), Forest of Bowland Landowning and Farmers Advisory Group and the Ramblers Association. FOREST OF BOWLAND Area of Outstanding Natural Beauty Contents Welcome Welcome 02 Introduction 03 How to use this toolkit 05 A place to enjoy and keep special 07 Delicious local food and drink 13 A landscape rich in heritage 17 A living landscape 21 Wild open spaces 25 A special place for wildlife 29 Glossary 34 Welcome to the Sense of Place Toolkit. Its purpose is to help you to use the special qualities of the Forest of Bowland Area of Outstanding Natural Beauty (AONB) in order to improve the performance of your business. -
Back Matter (PDF)
Index of Subjects abstraction and East London and Thames Gateway Chalk geology Isle of Wight 166–169 419–444 and the law 152, 155–156 in Lincolnshire Limestone 97–100 see also boreholes; wells petrophysical temperature logs 374–375 acidic groundwater 110, 199–209 surveys in tufa areas 132 aggregates in Weardale Granite, Eastgate, Co. Durham 405–407 petrography of geomaterials 458, 461–463, 464–466 World War I British exploratory boreholes in Belgium suitability of dune sand from Libya 277–280 295–298, 300 airborne electromagnetic (EM) surveys 389–390 yields in Antrim Lava Group and Ulster White Limestone Aksu Basin, Turkey 124 66–69 algae, and tufa formation 124–125 yields in Isle of Wight aquifers 161–162, 165, 166 alkali-silica reaction 463–464 boudinage structures in highway rock cuttings 411–418 alluvia, properties of coarse grained 141–144 Boulder Clay 174 aluminium, in acidic groundwater treatment 199, 200, 201, Bouldnor Formation 165 205, 206–208 Bracklesham Group 166, 392 American Expeditionary Force 302 Brazilian tension tests, rock salt 448–450 Ancholme Group 94 bricks and brickwork, petrography 460, 461, 465–466 anhydrite, and mechanical properties of rock salt 445–454 Bridgewick Marls 420, 426 Anstrude limestone, petrography 462 Brighstone Anticline 160 anthropogenic heat sources 373 brine-pumping 445–446 Antrim Lava Group, groundwater flow 63–73 British Cement Association 464 aquifers British Expeditionary Force 293–294, 295, 299 aquifer boundaries, and environmental sensitivity analysis British Geological Survey 302 311, 312 -
The First Record of Freshwater Plesiosaurian from the Middle
Gao et al. Journal of Palaeogeography (2019) 8:27 https://doi.org/10.1186/s42501-019-0043-5 Journal of Palaeogeography ORIGINALARTICLE Open Access The first record of freshwater plesiosaurian from the Middle Jurassic of Gansu, NW China, with its implications to the local palaeobiogeography Ting Gao, Da-Qing Li* , Long-Feng Li and Jing-Tao Yang Abstract Plesiosaurs are one of the common groups of aquatic reptiles in the Mesozoic, which mainly lived in marine environments. Freshwater plesiosaurs are rare in the world, especially from the Jurassic. The present paper reports the first freshwater plesiosaur, represented by four isolated teeth from the Middle Jurassic fluviolacustrine strata of Qingtujing area, Jinchang City, Gansu Province, Northwest China. These teeth are considered to come from one individual. The comparative analysis of the corresponding relationship between the body and tooth sizes of the known freshwater plesiosaur shows that Jinchang teeth represent a small-sized plesiosaurian. Based on the adaptive radiation of plesiosaurs and the palaeobiogeographical context, we propose a scenario of a river leading to the Meso-Tethys in the Late Middle Jurassic in Jinchang area, which may have provided a channel for the seasonal migration of plesiosaurs. Keywords: Freshwater plesiosaur, Middle Jurassic, Jinchang, Gansu Province, Palaeobiogeography 1 Introduction Warren 1980;Satoetal.2003; Kear 2012). Up to now, Plesiosaurs are one of the most familiar groups of Mesozoic the taxonomic affinities of most freshwater plesio- marine reptiles, which mainly lived in marine environ- saurs have remained unclear; some of them are re- ments. The records of plesiosaurs in non-marine deposits ferred to Plesiosauroidea (Cruickshank and Fordyce are sparse in comparison to those from marine sediments. -
Areas Designated As 'Rural' for Right to Buy Purposes
Areas designated as 'Rural' for right to buy purposes Region District Designated areas Date designated East Rutland the parishes of Ashwell, Ayston, Barleythorpe, Barrow, 17 March Midlands Barrowden, Beaumont Chase, Belton, Bisbrooke, Braunston, 2004 Brooke, Burley, Caldecott, Clipsham, Cottesmore, Edith SI 2004/418 Weston, Egleton, Empingham, Essendine, Exton, Glaston, Great Casterton, Greetham, Gunthorpe, Hambelton, Horn, Ketton, Langham, Leighfield, Little Casterton, Lyddington, Lyndon, Manton, Market Overton, Martinsthorpe, Morcott, Normanton, North Luffenham, Pickworth, Pilton, Preston, Ridlington, Ryhall, Seaton, South Luffenham, Stoke Dry, Stretton, Teigh, Thistleton, Thorpe by Water, Tickencote, Tinwell, Tixover, Wardley, Whissendine, Whitwell, Wing. East of North Norfolk the whole district, with the exception of the parishes of 15 February England Cromer, Fakenham, Holt, North Walsham and Sheringham 1982 SI 1982/21 East of Kings Lynn and the parishes of Anmer, Bagthorpe with Barmer, Barton 17 March England West Norfolk Bendish, Barwick, Bawsey, Bircham, Boughton, Brancaster, 2004 Burnham Market, Burnham Norton, Burnham Overy, SI 2004/418 Burnham Thorpe, Castle Acre, Castle Rising, Choseley, Clenchwarton, Congham, Crimplesham, Denver, Docking, Downham West, East Rudham, East Walton, East Winch, Emneth, Feltwell, Fincham, Flitcham cum Appleton, Fordham, Fring, Gayton, Great Massingham, Grimston, Harpley, Hilgay, Hillington, Hockwold-Cum-Wilton, Holme- Next-The-Sea, Houghton, Ingoldisthorpe, Leziate, Little Massingham, Marham, Marshland