Figures 12.1 to 12.3

Total Page:16

File Type:pdf, Size:1020Kb

Figures 12.1 to 12.3 LEGEND ¯ SOLID GEOLOGY Appleby Group Cumbrian Coast Group Mercia Mudstone Group Millstone Grit Group [see also MIGR] Pennine Coal Measures Group Sherwood Sandstone Group Warwickshire Group TORKINGTON HAZEL GROVE Coal seam, observed Fault Lines A6 Fossil Lines WYTHENSHAWE Norbury Moor Hazel Grove Railway Line WOODHOUSE PARK Proposed A6 bus bridge B5166 A5143 Old Mill SCHEME CHEADLE HULME Lane Norbury Brook A6 HEALD GREEN Potential Working Areas MOSS NOOK A523 B5358 A34 STANLEY GREEN BRAMHALL B5094 A555 MANCHESTER CHEADLE HANDFORTH HAZEL STOCKPORT GROVE CHEADLE HULME A5102 BRAMHALL POYNTON Manchester A555 Airport POYNTON A34 CHESHIRE EAST 0250 500 1000 1500 m A5102 A5149 Scale @ A3 Date 1:35,000 07-10-13 This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Controller of Her Majesty’s Stationery Office © Crown copyright. Unauthorised reproduction infringes Crown copyright and may lead to prosecution or civil proceedings. (LA100019571) (2009). This drawing may be used only for the purpose intended and only written dimensions shall be used Client Stockport M.B.C Project SEMMMS A6 to Manchester Airport Relief Road Title SOLID GEOLOGY Figure No. FIGURE 12.1 © Mouchel LEGEND DRIFT GEOLOGY ¯ Alluvial Fan Deposits Alluvium Glaciofluvial Deposits, Devensian Glaciofluvial Sheet Deposits, Devensian Glaciolacustrine Deposits, Devensian Lacustrine Deposits Peat River Terrace Deposits (undifferentiated) TORKINGTON Shirdley Hill Sand Formation Till, Devensian HAZEL GROVE Coal seam, observed WYTHENSHAWE Fault Lines Norbury Moor Fossil Lines WOODHOUSE PARK HIGH LANE SCHEME CHEADLE HULME HEALD GREEN Potential Working Areas MOSS NOOK STANLEY GREEN BRAMHALL MANCHESTER CHEADLE HAZEL WILMSLOW STOCKPORT GROVE CHEADLE HULME BRAMHALL Manchester Airport POYNTON POYNTON CHESHIRE EAST 0250 500 1000 1500 m Scale @ A3 Date 1:35,000 02-10-13 This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Controller of Her Majesty’s Stationery Office © Crown copyright. Unauthorised reproduction infringes Crown copyright and may lead to prosecution or civil proceedings. (LA100019571) (2009). This drawing may be used only for the purpose intended and only written dimensions shall be used Client Stockport M.B.C Project SEMMMS A6 to Manchester Airport Relief Road Title DRIFT GEOLOGY Figure No. FIGURE 12.2 © Mouchel LEGEND POTENTIAL CONTAMINATED SITES Potential Contaminated Site ¯ within 500m study area Potential Contaminated Site - Likely to be disturbed during construction PCS1 Mill Bank Farm PCS2 Hill Green Farm PCS3 Upper Swineseye Farm PCS4 Bramhall Oil Terminal PCS5 Ashmere Farm PCS6 Land off Dairy House Lane Handforth-A PCS7 Land off Dairy House Lane Handforth-B PCS8 Former Star Grove Petrol Station PCS9 Styal Road Service Station TORKINGTON PCS10 Airport Woodhouse Park HAZEL GROVE WYTHENSHAWE Norbury Moor WOODHOUSE PARK SCHEME CHEADLE HULME Potential Working Areas HEALD GREEN PCS9 PCS1 PCS10 MOSS NOOK STANLEY GREEN BRAMHALL PCS2 PCS8 PCS4 MANCHESTER CHEADLE HAZEL HANDFORTH STOCKPORT GROVE CHEADLE HULME BRAMHALL PCS6 PCS5 Manchester POYNTON Airport POYNTON CHESHIRE EAST PCS7 0 500 1000 2000 m PCS3 Scale @ A3 Date 1:40,000 02-10-13 This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Controller of Her Majesty’s Stationery Office © Crown copyright. Unauthorised reproduction infringes Crown copyright and may lead to prosecution or civil proceedings. (LA100019571) (2009). This drawing may be used only for the purpose intended and only written dimensions shall be used Client Stockport M.B.C Project SEMMMS A6 to Manchester Airport Relief Road Title POTENTIAL CONTAMINATED SITES Figure No. FIGURE 12.3 © Mouchel.
Recommended publications
  • Wales Regional Geology RWM | Wales Regional Geology
    Wales regional geology RWM | Wales Regional Geology Contents 1 Introduction Subregions Wales: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks Older sedimentary rocks 3 Basement rocks Rock structure 4 Groundwater 5 Resources 6 Natural processes Further information 7 - 21 Figures 22 - 24 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Wales Regional Geology Introduction This region comprises Wales and includes the adjacent inshore area which extends to 20km from the coast. Subregions To present the conclusions of our work in a concise and accessible way, we have divided Wales into 6 subregions (see Figure 1 below). We have selected subregions with broadly similar geological attributes relevant to the safety of a GDF, although there is still considerable variability in each subregion. The boundaries between subregions may locally coincide with the extent of a particular Rock Type of Interest, or may correspond to discrete features such as faults.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • Regional Geology
    CHAPTER III REGIONAL GEOLOGY The area known as the West Riding was an administrative EARLY PALAEOZOIC division of the ancient county of Yorkshire and includes (ORDOVICIAN TO DEVONIAN SYSTEMS) parts of the modern administrative areas of West Ordovician rocks outcrop as small inliers east of Howgill Yorkshire, North Yorkshire, Cumbria and Lancashire. Fells and more extensively in the extreme northwest Geographically the area extends from the high ground around Sedburgh. Historically they were exploited on a (>600m) of the Pennines in the north and west into the local basis for building stone, flagstones and roofing slates. lowland areas marginal to the Vale of York in the east. The Silurian rocks were exploited for flagstones in the These major topographic subdivisions reflect changes Ingleton and Horton-in-Ribblesdale areas and were used in the underlying geological formations (Fig. 6). The locally for grave stones, boundary and milestone markers. high mountainous spine of the Pennine area that crosses The best known of these stones were the Horton Flags the West Riding from north to south, is underlain by which were quarried around Helwith Bridge (from the hard, durable rocks ranging from Precambrian to seventeenth to nineteenth centuries: Mitchell, W. 1985). Namurian (Carboniferous) in age. The lower ground to The massive sandstones of the Austick Grits were also the south-east is underlain by the thick Coal Measure used locally for building. Stones from this succession have successions exposed in the deeply incised valleys of the not so far been identified in the Anglo-Saxon carved Yorkshire Coalfield, extending southwards from Leeds to Sheffield.
    [Show full text]
  • Chapter 14 Midland Valley of Scotland 15/03/2012
    Chapter 14 Midland Valley of Scotland 15/03/2012 Chapter 14 Midland Valley of Scotland C. N. WATERS, M. A. E. BROWNE, N. S. JONES & I.D. SOMERVILLE Carboniferous rocks occupy much of the Midland Valley of Scotland, but are commonly obscured at surface by Quaternary deposits. The succession occupies an ENE-trending graben bounded by the complexes of the Highland Boundary Fault to the northwest and the Southern Upland Fault to the southeast. Onshore, the graben is about 90 km wide and extends some 150 km from the Ayrshire coast and Glasgow in the west to the east Fife and East Lothian coasts in the east (Fig. 14.1). The basins within the graben are associated with Carboniferous rocks more than 6 km thick. The Highland Boundary and Southern Upland faults were active and helped control sedimentation, initially during the Tournaisian as sinistral strike/oblique slip faults and subsequently in the Visean to Westphalian a regime of dextral strike/oblique-slip deformation (Browne & Monro 1989; Ritchie et al. 2003; Underhill et al. 2008). Isolated exposures also occur on the Island of Arran and at Machrihanish in Kintyre. The Midland Valley of Scotland was separated from basins to the south (Tweed and Solway Firth basins and the Northumberland Trough- see Chapter 13) by the Lower Palaeozoic rocks of the Southern Uplands block, which formed a positive, mainly emergent area throughout the Carboniferous. However, this was breached during the Carboniferous by narrow NW–SE trending basins, for example Stranraer and Sanquhar to Thornhill. The Scottish Highlands to the north, of Lower Palaeozoic and Precambrian rocks, were similarly a positive, mainly emergent area with outcrops of Carboniferous (Johnstone 1966) limited to the west coast around Inninmore (Sound of Mull), Bridge of Awe (Pass of Brander) and Glas Eilean (Sound of Islay).
    [Show full text]
  • Compartmentalisation and Groundwater
    Durham Research Online Deposited in DRO: 14 July 2020 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Wilson, Miles. P. and Worrall, Fred. and Clancy, Sarah. A. and Ottley, Christopher. J. and Hart, Alwyn. and Davies, Richard. J. (2020) 'Compartmentalisation and groundwatersurface water interactions in a prospective shale gas basin : assessment using variance analysis and multivariate statistics on water quality data.', Hydrological processes., 34 (15). pp. 3271-3294. Further information on publisher's website: https://doi.org/10.1002/hyp.13795 Publisher's copyright statement: c 2020 The Authors. Hydrological Processes published by John Wiley Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Received: 23 January 2020 Accepted: 25 April 2020 DOI: 10.1002/hyp.13795 RESEARCH ARTICLE Compartmentalisation and groundwater–surface water interactions in a prospective shale gas basin: Assessment using variance analysis and multivariate statistics on water quality data Miles P.
    [Show full text]
  • Origin of Carboniferous Sandstones Fringing the Northern Margin of the Wales-Brabant Massif: Insights from Detrital Zircon Ages
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by NERC Open Research Archive Origin of Carboniferous sandstones fringing the northern margin of the Wales-Brabant Massif: insights from detrital zircon ages ANDREW MORTON1,2*, COLIN WATERS3, MARK FANNING4, IAN CHISHOLM5 and MATT BRETTLE6 1 HM Research Associates, 2 Clive Road, Balsall Common, CV7 7DW, UK 2 CASP, University of Cambridge, 181a Huntingdon Road, Cambridge CB3 0DH, UK 3 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 4 Research School of Earth Sciences, The Australian National University, Canberra ACT0200, Australia 5 4 Park Street, Loughborough, Leicestershire, LE11 2EG, UK 6 Premier Oil UK Limited, 53 Blenheim Place, Aberdeen AB25 2DZ, UK *Correspondence to: Andrew Morton, HM Research Associates, 2 Clive Road, Balsall Common, CV7 7DW, UK. Email: [email protected] ABSTRACT A study of detrital zircon age populations in Namurian-Westphalian (Carboniferous) sandstones in the southern Central Pennine Basin of the UK has revealed considerable complexity in their provenance history. The Pendleian-Marsdenian Morridge Formation, which is known to have been derived from the Wales-Brabant Massif to the south on the basis of palaeocurrent and petrographic information, is dominated by zircons ultimately derived from the Caledonian belt to the north. These zircons were recycled from sandstones of northern origin that had been previously deposited over the massif during Middle to Late Devonian times. The Morridge Formation also includes Late Neoproterozoic zircons of local Wales-Brabant Massif origin. The south lobe of the Yeadonian Rough Rock has been previously interpreted as having a complex provenance including sediment of northern origin interbedded with sediment ascribed to a Wales- Brabant Massif source.
    [Show full text]
  • How to Navigate This Document How to Navigate This Document
    BRITISH GEOLOGICAL SURVEY RESEARCH REPORT NUMBER RR/99/07 A lithostratigraphical framework for the Carboniferous rocks of the Midland Valley of Scotland Version 2 M A E Browne, M T Dean, I H S Hall, A D McAdam, S K Monro and J I Chisholm Geographical index Midland Valley of Scotland Subject index Geology, Carboniferous Bibliographical Reference M A E Browne, M T Dean, I H S Hall, A D McAdam, S K Monro and J I Chisholm. 1999. A lithostratigraphical framework for the Carboniferous rocks of the Midland Valley of Scotland British Geological Survey Research Report, RR/99/07 © NERC Copyright 1999 British Geological Survey Keyworth Nottingham NG12 5GG UK HOW TO NAVIGATE THIS DOCUMENT HOW TO NAVIGATE THIS DOCUMENT ❑ The general pagination is designed for hard copy use and does not correspond to PDF thumbnail pagination. ❑ 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 and tables irrespective of which part of the document the user is viewing. ❑ In addition, the report contains links: ✤ from the principal section and sub-section headings back to the contents page, ✤ from each reference to a figure or table directly to the corresponding figure or table, ✤ from each figure or table caption to the first place that figure or table is mentioned in the text and ✤ from each page number back to the contents page. Return to contents page Contents 1 Summary 7.4 Passage Formation 2 Preface 8 Coal Measures 3 Introduction 8.1 Lower Coal Measures 8.2 Middle
    [Show full text]
  • REGIONAL GEOLOGY by Graham K. Lott
    CHAPTER II REGIONAL GEOLOGY by Graham K. Lott The ‘quarrying’ and use of local stone in Notting- the Triassic comprises a thick succession of non- hamshire, for both building and decorative purposes, marine, green-grey to reddish brown sandstones, dates back to Roman times. However, the lithological siltstones and mudstones, the latter including thinly units that characterise the geological succession interbedded, grey-green, dolomitic, very fine grained within the county contain only a few beds of stone sandstones (known locally as skerry). In contrast, the suitable for these purposes. This lack of indigenous early Jurassic marine succession is only sporadically stone useful for decorative carving is reflected in the exposed along the northern edge of the low-lying composition of the suite of carved stone fragments Vale of Belvoir and comprises a succession of grey that have been studied as part of this Corpus project. limestones and mudstones (Lias Group). The eastern By far the majority of the stones examined consist part of the county is locally blanketed by extensive of lithologies (primarily sandstones and limestones) tracts of glacial and alluvial sediments (unconsolidated sourced from outside the county border. sands, gravels, clays and muds) of Quaternary age. carboniferous THE GEOLOGY OF NOTTINGHAMSHIRE Pennine Coal Measures Group Nottinghamshire has a relatively simple geological The Carboniferous rocks that crop out in the west of succession comprising a sequence of eastwards- the county form part of the Pennine Coal Measures dipping sedimentary rock units whose outcrops Group. This succession is best known economically extend from north to south across the county (see for its coal reserves but also contains a number of Fig.
    [Show full text]
  • 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.
    [Show full text]