Engineering Geological Aspects of Embankment Dams on Mercia Mudstone
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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. -
Aust Cliff and Manor Farm
This excursion guide is a draft chapter, subject to revision, to be published in a field guide book whose reference is: Lavis, S. (Ed.) 2021. Geology of the Bristol District, Geologists’ Association Guide No. 75. It is not to be circulated or duplicated beyond the instructor and their class. Please send any corrections to Michael Benton at [email protected] Aust Cliff and Manor Farm Michael J. Benton Maps OS Landranger 172 1:50 000 Bristol & Bath Explorer 167 1:25 000 Thornbury, Dursley & Yate BGS Sheet 250 1:50 000 Chepstow Main references Swift & Martill (1999); Allard et al. (2015); Cross et al. (2018). Objectives The purpose of the excursion is to examine a classic section that documents the major environmental shift from terrestrial to marine rocks caused by the Rhaetian transgression, as well as the Triassic-Jurassic boundary, and to sample the rich fossil faunas, and espe- cially the Rhaetian bone beds. Risk analysis Low tides are essential for the excursion to Aust Cliff. Tides rise very rapidly along this section of coast (with a tidal range of about 12 m) and strong currents sweep past the bridge abutment. Visitors should begin the excursion on a falling tide. If caught on the east side of the bridge abutment when the tide rises, visitors should continue east along the coast to the end of the cliff where a path leads back to the motorway service area. In addition, the entire section is a high cliff, and rock falls are frequent, so hard hats must be worn. The Manor Farm section lies inland and is lower, so hard hats are less necessary. -
A Mysterious Giant Ichthyosaur from the Lowermost Jurassic of Wales
A mysterious giant ichthyosaur from the lowermost Jurassic of Wales JEREMY E. MARTIN, PEGGY VINCENT, GUILLAUME SUAN, TOM SHARPE, PETER HODGES, MATT WILLIAMS, CINDY HOWELLS, and VALENTIN FISCHER Ichthyosaurs rapidly diversified and colonised a wide range vians may challenge our understanding of their evolutionary of ecological niches during the Early and Middle Triassic history. period, but experienced a major decline in diversity near the Here we describe a radius of exceptional size, collected at end of the Triassic. Timing and causes of this demise and the Penarth on the coast of south Wales near Cardiff, UK. This subsequent rapid radiation of the diverse, but less disparate, specimen is comparable in morphology and size to the radius parvipelvian ichthyosaurs are still unknown, notably be- of shastasaurids, and it is likely that it comes from a strati- cause of inadequate sampling in strata of latest Triassic age. graphic horizon considerably younger than the last definite Here, we describe an exceptionally large radius from Lower occurrence of this family, the middle Norian (Motani 2005), Jurassic deposits at Penarth near Cardiff, south Wales (UK) although remains attributable to shastasaurid-like forms from the morphology of which places it within the giant Triassic the Rhaetian of France were mentioned by Bardet et al. (1999) shastasaurids. A tentative total body size estimate, based on and very recently by Fischer et al. (2014). a regression analysis of various complete ichthyosaur skele- Institutional abbreviations.—BRLSI, Bath Royal Literary tons, yields a value of 12–15 m. The specimen is substantially and Scientific Institution, Bath, UK; NHM, Natural History younger than any previously reported last known occur- Museum, London, UK; NMW, National Museum of Wales, rences of shastasaurids and implies a Lazarus range in the Cardiff, UK; SMNS, Staatliches Museum für Naturkunde, lowermost Jurassic for this ichthyosaur morphotype. -
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. -
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. -
University of Birmingham Uppermost Triassic to Lower Jurassic
University of Birmingham Uppermost Triassic to Lower Jurassic sediments of the island of Ireland and its surrounding basins Raine, Robert; Copestake, Philip; Simms, Michael; Boomer, Ian DOI: 10.1016/j.pgeola.2020.04.001 License: Creative Commons: Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) Document Version Peer reviewed version Citation for published version (Harvard): Raine, R, Copestake, P, Simms, M & Boomer, I 2020, 'Uppermost Triassic to Lower Jurassic sediments of the island of Ireland and its surrounding basins', Proceedings of the Geologists' Association. https://doi.org/10.1016/j.pgeola.2020.04.001 Link to publication on Research at Birmingham portal 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. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. When citing, please reference the published version. -
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. -
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. -
Western Link
Western Link Ground Investigation Report 20 October 2017 Warrington Borough Council Mott MacDonald Spring Bank House 33 Stamford Street Altrincham WA14 1ES United Kingdom T +44 (0)161 926 4000 F +44 (0)161 929 8915 mottmac.com Warrington Borough Council Warrington 26-30 Horsemarket Street Western Link WA1 1XL 382900-WL-MMD-07-ZZ-RP-N-0002 https://mottmac.sharepoint.com/teams/pj-b1092/Shared Documents/12 - Geotechnics/Reports/Documents/382900-WL-MMD-07-ZZ-RP-N-0002 GIR.docx Mott MacDonald Ground Investigation Report 20 October 2017 Mott MacDonald Limited. Registered in England and Wales no. 1243967. Registered office: Mott MacDonald House, 8-10 Sydenham Road, Croydon CR0 2EE, Warrington Borough Council United Kingdom Mott MacDonald | Western Link Ground Investigation Report Contents Executive summary 1 1 Introduction 3 1.1 Scope and Objective of the Report 3 1.2 Description of Project 3 1.3 Geotechnical Category of Project 4 2 Existing Information 5 2.1 Topographic Maps (Old and Recent) 5 2.2 Geological Maps and Memoirs 5 2.3 Hydrology 6 2.4 Hydrogeology 6 2.5 Records of Mines and Mineral Deposits 6 2.6 Land Use and Soil Survey Information 7 2.7 Archaeological and Historical Investigations 7 2.8 Existing Ground Investigations 8 2.9 Consultation with Statutory Bodies and Agencies 8 2.10 Flood Records 8 2.11 Contaminated Land 8 3 Field and Laboratory Studies 9 3.1 Walkover Survey 9 3.2 Ground Investigation 9 3.3 Other Field Work 10 3.4 Laboratory Investigation 10 4 Ground Summary 12 4.1 Overview 12 5 Ground Conditions and Material Properties -
6 Merseyside
6 Merseyside 6.1 Administrative set-up Merseyside takes its name from the River Mersey and is a metropolitan county in North West England. Merseyside came into existence as a metropolitan county in 1974, after the passage of the Local Government Act 1972, and the county consists of five metropolitan boroughs adjoining the Mersey Estuary, including the City of Liverpool. Merseyside encompasses about 645 km2 (249 sq miles) and has a population of around 1,350,100 (Office of National Statistics). Number of Males Females Total Area Merseyside people per (thousands) (thousands) (thousands) (hectares) hectare Knowsley 71.7 79.1 150.8 8629.3 17.48 Liverpool 212.7 222.8 435.5 11159.08 39.03 Sefton 131.3 144.9 276.2 15455.66 17.87 St Helens 86.5 91 177.5 13589.08 13.06 Wirral 147.7 162.4 310.1 15704.9 19.75 Total 649.9 700.2 1350.1 64538.02 107.19 Table 3 Demographics of Merseyside (sourced various from ONS www.statistics.gov.uk) Merseyside County Council was abolished in 1986, and so its districts (the metropolitan boroughs) are now essentially unitary authorities. However, the metropolitan county continues to exist in law and as a geographic frame of reference. Merseyside is divided into two parts by the Mersey Estuary: the Metropolitan Borough of Wirral is located to the west of the estuary on the Wirral Peninsula; the rest of the county is located on the eastern side of the estuary. The eastern boroughs of Merseyside border Lancashire to the north and Greater Manchester to the east, and both parts of Merseyside, west and east of the estuary, border Cheshire to the south. -
Using Core and Outcrop Analogues to Predict Flow Pathways in the Subsurface: Examples from the Triassic Sandstones of North Ches
Adv. Geosci., 49, 121–127, 2019 https://doi.org/10.5194/adgeo-49-121-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Using core and outcrop analogues to predict flow pathways in the subsurface: examples from the Triassic sandstones of north Cheshire, UK Joanna Thompson, Daniel Parkes, Edward Hough, and Oliver Wakefield British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK Correspondence: Joanna Thompson ([email protected]) Received: 30 May 2019 – Accepted: 2 August 2019 – Published: 19 September 2019 Abstract. Borehole core provides detailed vertical data resources such as pore space and heat extraction. Subsurface which is used to interpret subsurface sand body architec- fluid flow is relevant to the development of new, low-carbon tures, but assumptions are made on the relationship between energy technologies (e.g., geothermal systems located in sed- the lateral and vertical thickness, and the interconnectivity imentary aquifers, underground gas storage and Carbon Cap- of units. The sedimentological complexity of the Sherwood ture and Storage; CCS). In the UK, there is the potential for Sandstone Group succession in this area, passing between the development of these geological settings where there are aeolian and fluvial packages creates local- to regional-scale porous and permeable rocks that may serve as production or heterogeneities which will impact flow pathways within the storage horizons located in proximity to sources of energy rockmass. Measured thickness in boreholes might represent such as shale gas reservoirs, coal seams or renewables; op- an architectural element’s true maximum thickness or more erational viability is increased where these geologies are lo- likely, a partial thickness as a result of incision by over- cated near areas of industrial activity or areas of dense popu- lying facies types or as a result of the borehole sitting to- lation.