Baseline Report Series:20. the Permo-Triassic Sandstone
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A Building Stone Atlas of Warwickshire
Strategic Stone Study A Building Stone Atlas of Warwickshire First published by English Heritage May 2011 Rebranded by Historic England December 2017 Introduction The landscape in the county is clearly dictated by the Cob was suitable for small houses but when more space was underlying geology which has also had a major influence on needed it became necessary to build a wooden frame and use the choice of building stones available for use in the past. The wattle fencing daubed with mud as the infilling or ‘nogging’ to geological map shows that much of this generally low-lying make the walls. In nearly all surviving examples the wooden county is underlain by the red mudstones of the Triassic Mercia frame was built on a low plinth wall of whatever stone was Mudstone Group. This surface cover is however, broken in the available locally. In many cases this is the only indication we Nuneaton-Coventry-Warwick area by a narrow strip of ancient have of the early use of local stones. Adding the stone wall rocks forming the Nuneaton inlier (Precambrian to early served to protect the wooden structure from rising damp. The Devonian) and the wider exposure of the unconformably infilling material has often been replaced later with more overlying beds of the Warwickshire Coalfield (Upper durable brickwork or stone. Sometimes, as fashion or necessity Carboniferous to early Permian). In the south and east of the dictated, the original timber framed walls were encased in county a series of low-lying ridges are developed marking the stone or brick cladding, especially at the front of the building outcrops of the Lower and Middle Jurassic limestone/ where it was presumably a feature to be admired. -
Davenport Green to Ardwick
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 | MA07 MA07: Davenport Green to Ardwick High Speed Two (HS2) Limited Two Snowhill, Snow Hill Queensway, Birmingham B4 6GA Freephone: 08081 434 434 Minicom: 08081 456 472 Email: [email protected] H10 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 MA07: Davenport Green to Ardwick H10 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. -
Electoral Changes) Order 2000
508409100105-06-00 23:14:45 Pag Table: STATIN PPSysB Unit: PAG1 STATUTORY INSTRUMENTS 2000 No. 1418 LOCAL GOVERNMENT, ENGLAND The Borough of Oswestry (Electoral Changes) Order 2000 Made - - - - 24th May 2000 Coming into force in accordance with article 1(2) Whereas the Local Government Commission for England, acting pursuant to section 15(4) of the Local Government Act 1992(a), has submitted to the Secretary of State a report dated August 1999 on its review of the borough(b) of Oswestry together with its recommendations: And whereas the Secretary of State has decided to give effect to those recommendations: Now, therefore, the Secretary of State, in exercise of the powers conferred on him by sections 17(c) and 26 of the Local Government Act 1992, and of all other powers enabling him in that behalf, hereby makes the following Order: Citation, commencement and interpretation 1.—(1) This Order may be cited as the Borough of Oswestry (Electoral Changes) Order 2000. (2) This Order shall come into force— (a) for the purposes of article 4, on the day after that on which it is made; (b) for the purpose of proceedings preliminary or relating to any election to be held on 1st May 2003, on 10th October 2002; (c) for all other purposes, on 1st May 2003. (3) In this Order— “borough” means the borough of Oswestry; “existing”, in relation to a ward, means the ward as it exists on the date this Order is made; and any reference to the map is a reference to the map prepared by the Department of the Environment, Transport and the Regions marked “Map of the Borough of Oswestry (Electoral Changes) Order 2000”, and deposited in accordance with regulation 27 of the Local Government Changes for England Regulations 1994(d). -
Environment Agency Midlands Region Wetland Sites Of
LA - M icllanAs <? X En v ir o n m e n t A g e n c y ENVIRONMENT AGENCY MIDLANDS REGION WETLAND SITES OF SPECIAL SCIENTIFIC INTEREST REGIONAL MONITORING STRATEGY John Davys Groundwater Resources Olton Court July 1999 E n v i r o n m e n t A g e n c y NATIONAL LIBRARY & INFORMATION SERVICE ANGLIAN REGION Kingfisher House. Goldhay Way. Orton Goldhay, Peterborough PE2 5ZR 1 INTRODUCTION................................................................................................................................... 3 1.) The Agency's Role in Wetland Conservation and Management....................................................3 1.2 Wetland SSSIs in the Midlands Region............................................................................................ 4 1.3 The Threat to Wetlands....................................................................................................................... 4 1.4 Monitoring & Management of Wetlands...........................................................................................4 1.5 Scope of the Report..............................................................................................................................4 1.6 Structure of the Report.......................................................................................................................5 2 SELECTION OF SITES....................................................................................................................... 7 2.1 Definition of a Wetland Site................................................................................................................7 -
The Early Evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin
University of Birmingham The early evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin DOI: 10.3389/fevo.2015.00142 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Butler, R, Montefeltro, F & Ezcurra, M 2016, 'The early evolution of Rhynchosaurs', Frontiers in Ecology and Evolution. https://doi.org/10.3389/fevo.2015.00142 Link to publication on Research at Birmingham portal Publisher Rights Statement: Frontiers is fully compliant with open access mandates, by publishing its articles under the Creative Commons Attribution licence (CC-BY). Funder mandates such as those by the Wellcome Trust (UK), National Institutes of Health (USA) and the Australian Research Council (Australia) are fully compatible with publishing in Frontiers. Authors retain copyright of their work and can deposit their publication in any repository. The work can be freely shared and adapted provided that appropriate credit is given and any changes specified. General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. -
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. -
Geological Assessment
Lydia Clare Ellis Hill Farm Swinscoe Ashbourne Derbyshire DE6 2HH Geological Assessment: This report contains a geological description of the specified site or area. It is based on currently available 1:10 000 scale geological maps, unless otherwise stated, together with other relevant local information such as borehole records. The report includes extracts from digitised 1:50 000 scale geological maps (DigMapGB-50). The report contains the following modules: Geological Assessment (area) Geological Map Extracts Geoscience Data List Natural Ground Stability Report Id: GR_218809/1 Client reference: Search location This report describes a site located at National Grid Reference 413096, 345351. Note that for sites of irregular shape, this point may lie outside the site boundary. Where the client has submitted a site plan the assessment will be based on the area given. Search location indicated in red This product includes mapping data licensed from Ordnance Survey. © Crown Copyright and/or database right 2018. Licence number 100021290 EUL Scale: 1:5 000 (1cm = 50 m) Contains Ordnance Survey data © Crown Copyright and database right 2018 OS Street View: Scale: 1:5 000 (1cm = 50 m) Date: 24 July 2018 Page: 2 of 28 © NERC, 2018. All rights reserved. BGS Report No: GR_218809/1 Geological Map Extracts This part of the report contains extracts of geological maps taken from the 1:50 000 scale BGS Digital Geological Map of Great Britain (DiGMapGB-50). The geological information in DiGMapGB is separated into four themes: artificial ground, landslide deposits, superficial deposits and bedrock, shown here in separate maps. The fifth ‘combined geology’ map superimposes all four of these themes, to show the geological formations that occur at the surface, just beneath the soil. -
A Beaked Herbivorous Archosaur with Dinosaur Affinities from the Early Late Triassic of Poland
Journal of Vertebrate Paleontology 23(3):556±574, September 2003 q 2003 by the Society of Vertebrate Paleontology A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND JERZY DZIK Instytut Paleobiologii PAN, Twarda 51/55, 00-818 Warszawa, Poland, [email protected] ABSTRACTÐAn accumulation of skeletons of the pre-dinosaur Silesaurus opolensis, gen. et sp. nov. is described from the Keuper (Late Triassic) claystone of KrasiejoÂw in southern Poland. The strata are correlated with the late Carnian Lehrberg Beds and contain a diverse assemblage of tetrapods, including the phytosaur Paleorhinus, which in other regions of the world co-occurs with the oldest dinosaurs. A narrow pelvis with long pubes and the extensive development of laminae in the cervical vertebrae place S. opolensis close to the origin of the clade Dinosauria above Pseudolagosuchus, which agrees with its geological age. Among the advanced characters is the beak on the dentaries, and the relatively low tooth count. The teeth have low crowns and wear facets, which are suggestive of herbivory. The elongate, but weak, front limbs are probably a derived feature. INTRODUCTION oped nutrient foramina in its maxilla. It is closely related to Azendohsaurus from the Argana Formation of Morocco (Gauf- As is usual in paleontology, with an increase in knowledge fre, 1993). The Argana Formation also has Paleorhinus, along of the fossil record of early archosaurian reptiles, more and with other phytosaurs more advanced than those from Krasie- more lineages emerge or extend their ranges back in time. It is joÂw (see Dutuit, 1977), and it is likely to be somewhat younger. -
8. Hydrogeology and Land Contamination
Greenpark Energy Ltd April 2010 8. Hydrogeology and Land Contamination 8.1 Summary This chapter assessed the hydrogeological context of the proposed development together with possible impacts resulting from the development and considered the following key issues: The impact of the development on aquifers and groundwater located beneath the site; The impact of the development on nearby groundwater abstractions; Mitigation measures to be undertaken during site preparation, drilling and production and restoration of the site to prevent potential adverse impacts. This chapter also considered the current contamination status of the site and the potential for land contamination resulting from the proposed development and considers the following key issues: Potential contamination of land resulting from the proposed development; Mitigation measures to be undertaken during site preparation, drilling and production and restoration of the site to prevent potential adverse impacts. The site has variable shallow drift geology including glacial sand and gravel and glacial till to depths of between 0.9 and 2.6m below ground level. The solid geology below the site comprises strata of the Mercia Mudstone Group. The Mercia Mudstones overlie strata of the Triassic Sherwood Sandstone Group which comprises thick sandstones and is classified as a Major Aquifer by the Environment Agency; these strata extend up to approximately 300m in thickness in the area and are locally abstracted by Severn Trent Water for public potable supply. The Sherwood Sandstones lie unconformably above Upper Carboniferous Strata which include the Coal Measures Strata which are the target strata for the CBM gas development. The Coal Measures Strata are separated from the overlying Sherwood Sandstone by the Carboniferous Barren Measures Strata which are classified as a Minor Aquifer. -
Core Strategy
Shropshire Local Development Framework : Adopted Core Strategy March 2011 “A Flourishing Shropshire” Shropshire Sustainable Community Strategy 2010-2020 Contents Page 1 Introduction 1 2 Spatial Portrait 7 Shropshire in 2010 7 Communities 9 Economy 10 Environment 13 Spatial Zones in Shropshire 14 3 The Challenges We Face 27 Spatial Vision 28 Strategic Objectives 30 4 Creating Sustainable Places 34 Policy CS1: Strategic Approach 35 Policy CS2: Shrewsbury Development Strategy 42 Policy CS3: The Market Towns and Other Key Centres 48 Policy CS4: Community Hubs and Community Clusters 61 Policy CS5: Countryside and Green Belt 65 Policy CS6: Sustainable Design and Development Principles 69 Policy CS7: Communications and Transport 73 Policy CS8: Facilities, Services and Infrastructure Provision 77 Policy CS9: Infrastructure Contributions 79 5 Meeting Housing Needs 82 Policy CS10: Managed Release of Housing Land 82 Policy CS11: Type and Affordability of Housing 85 Policy CS12: Gypsies and Traveller Provision 89 6 A Prosperous Economy 92 Policy CS13: Economic Development, Enterprise and Employment 93 Policy CS14: Managed Release of Employment Land 96 Policy CS15: Town and Rural Centres 100 Policy CS16: Tourism, Culture and Leisure 104 7 Environment 108 Policy CS17: Environmental Networks 108 Policy CS18: Sustainable Water Management 111 Policy CS19: Waste Management Infrastructure 115 Policy CS20: Strategic Planning for Minerals 120 Contents Page 8 Appendix 1: Saved Local and Structure Plan Policies replaced by the Core Strategy 126 9 Glossary 138 -
Lct 5: Undulating Enclosed Farmland
LCT 5: UNDULATING ENCLOSED FARMLAND General Description This character type is defined by undulating topography and the associated small to medium scale enclosure into which it is divided. Key characteristics are the generally cohesive and un-fragmented historic landscape in the south of the borough, small woodlands, ponds and streams, nucleated rural villages and scattered farmsteads. Land use is mainly pasture. Away from main roads, railways and settlement the landscape is generally quiet and rural. Views within this type very much depend upon location and the nature of the immediate topography. There is a range of monuments from Bronze Age barrows to post medieval canal locks. The character type is found across a large part of the Cheshire West and Chester borough; to the east between Northwich and the Sandstone Ridge and in the south of the borough. Visual Character The location of this landscape type is reflected in the prevailing views which extend to adjacent character areas, either out over the low-lying plain or up towards the often dominant Sandstone Ridge. Roads typically follow the rolling topography, offering extensive views from high vantage points out over the immediate field pattern and extending to the high ground in the far distance such as the Pennines in the east. Long distance views are sometimes affected by large scale industrial works in adjacent areas. LCT 5: Undulating Enclosed Farmland 138 From low ground the landscape appears smaller in scale due to the increase in enclosure and the contained views where skylines are typically formed by hedgerow trees, woodland and farmsteads, with occasional electricity pylons and church spires. -
Engineering Geological Aspects of Embankment Dams on Mercia Mudstone
Engineering Geological Aspects of Embankment Dams on Mercia Mudstone Tim Blower, CEng, MICE, CGeol, FGS Outline of Presentation • Introduction • Lincoln case study • Initial studies into Mercia Mudstone • Site investigations • Research on historical dams • Observations • Lincoln case study - reprise Embankment Dams on Mercia Mudstone Introduction • Lincoln WTW Project • Promoters are ANGLIAN WATER • Forecast supply deficit of 20 Ml/d by 2035 in Lincoln area • Business Case solution is a new 20 Ml/d treatment works in the Lincoln area • To satisfy future demand growth in this area, but also to improve resilience (increasing demand further south) Embankment Dams on Mercia Mudstone Newton Cliff SAM RWR Raw water pipeline Treated water pipeline New Pumping Station Existing WTW New river intake New WTW RWR Lincoln WTW Project – Storage Reservoir • Earth fill embankment dam • Roughly oval shape • 10 days storage including outage time • Capacity 285,000m 3 • Earthworks volumes - cut & fill: 220,000m 3 Embankment Dams on Mercia Mudstone Desk Study • Project Constraints • Risk Areas • Planning the GI • Initial studies on the Mercia Mudstone • Walkover survey Embankment Dams on Mercia Mudstone General References on Mercia Mudstone • Chandler, R.J. & Forster, A (2001). Engineering in Mercia mudstone. CIRIA Report C570. • Hobbs, P.R.N. et. al. (2001). Engineering Geology of British Rocks and Soils - Mudstones of the Mercia Mudstone Group; BGS Research Report RR/01/02. • Howard, A.S. et.al. (2008). A Formational Framework for the Mercia Mudstone Group (Triassic) of England and Wales; BGS Research Report RR/08/04. Embankment Dams on Mercia Mudstone Outcrop of Mercia Mudstone 10 MM age from Mid Triassic (Anisian) to latest Triassic 9 (Rhaetian) 8 6 (241 – 205 mybp).