Bedrock Geology UK

Total Page:16

File Type:pdf, Size:1020Kb

Bedrock Geology UK Long 8° 30’ 7° 30’ 6° 30’ 5° 30’ 4° 30’ 3° 30’ Long Long 30’ Long 13° 30’ W 45 4° 30’ W 75 90 2° 00’ W 1° 00’ W 75 2 000m 2 000m 3 000m 4 000m 04 0 5 0 6 0 7 0 8 0 9 10 1 1 12 13 14 15 16 17 18 19 2 0 2 1 2 2 2 3 24 2 5 2 6 2 7 2 8 2 9 3 0 3 1 3 2 3 3 34 3 5 3 6 3 7 2 5 2 6 2 7 4 0 4 1 4 2 4 3 4 4 4 5 4 6 4 7 9 000m 90 D2 990 000m 1030 000m 1030 000m D3 1220 000m 1220 000m CP D2 A1 NORTHERN G SD ROCKALL X8 CP SULE SKERRY SHETLAND EO 9 8 9 8 10 2 10 2 S1 A1 X5-6 12 EO 12 Lat 1 1 Lat STACK SKERRY 1:625 000 Scale Lat 59° 00’ N Lat 57° 30’ N D3 58° 30’ N E1-2 59° 00’ N F X5 F CP 131 Lat X1 130 EO 9 7 9 7 1010 000m 1010 000m 57° 30’ N F MOINE THRUST (MT) OS 45 2 5 2 6 2 7 75 X X4 S1 BEDROCK GEOLOGY UK NORTH E3 12 12 A2 X1 SD 2 000m 2 000m 0 0 LEWIS & HARRIS D2 X X1-3 X F D2 Long 113 OS SD CP Long D2 SD EO 13° 30’ W (North) 1:100 000 Z X1 Y1 116 4° 30’ W X D1 D1 SD A3 A1 Z X D1 F OS D1 X1-3 EO (North of National Grid Line 460 km N) 9 6 OS 9 6 Z E3 A1 129 S1 CP SD X A1 X X4 Long E1-2 X1 115 Lat Long 119 119 114 SD SD 00 8° 30’ W A1 58° 30’ N 60 6° 00’ W 90 X1 OS OS X5-6 0 000m OS 1 000m 1 000m 5th EDITION Z LINE OF SECTION OS SD X1-3 0 0 0 SD X1-3 D2 1 1 1 2 3 D1-3 7 8 SD SD X 9 5 X 9 5 1040 000m 1040 000m A1 A1 Z X OS X4 Geological interpretation and map compilation by J D Floyd, R Addison and D Reay. The copyright of materials derived from the British Geological X1 A1 X1-3 SD A1 Z A1 A2 F E1-2 118 SD 118 Geological cross-section compiled by A G Leslie. Survey’s work is vested in the Natural Environment Research Z X CP Lat SD X1-3 X X1-3 A2 SD Lat Data preparation by A H Myers and P Turner. Council (NERC). No part of these materials may be reproduced 107 X SD A1 60° 30’ N A2 60° 30’ N X X1-3 X1-3 X1-3 A2 A2 SD D1 RONA A1 SD A1 SD Digital cartography by J W Arbon and I L Cooke. or transmitted in any form (analogue or digital) or by any means, Z SD A1 A3 X1 SULA SGEIR A Smith, Project Manager, Digital Geological Map of Great Britain. or stored in a retrieval system of any nature, without the prior 9 4 9 4 10 3 10 3 X6 A3 OS D1 SD SD X4 OS X4 M Smith, Chief Geologist, Scotland. G Earls, Director, Geological Survey of Northern Ireland. permission of the BGS Intellectual Property Rights Manager Z A1 D1 X6 PT Z Z A1 SD 117 SD 117 A2 A2 Z ASSYNT X1 A1 E1-2 M K Lee, Director of Geology and Resources. (British Geological Survey, Kingsley Dunham Centre, Keyworth, Z Z X CP Published 2007. John N Ludden, PhD. Executive Director, British Geological Survey. Nottingham, NG12 5GG. Telephone 0115 936 3381). www.bgs.ac.uk A1 A2 E3 109 X X5-6 X5-6 A1 SD Lat A1 SD OS 108 59° 00’ N SD X6-7 F SD OS SD X5-6 Coastline © HarperCollins Publishers Ltd 2005. www.collinsmaps.com BGS © NERC 2009. All rights reserved. F Y3 X OS 110 E1-2 9 3 Z A1 F SD X1-3 9 3 1020 000m 1020 000m SD X X1 SD Z X1-3 SD X4 SD Z X 60 90 X6-7 Z OS X 17 18 SD X5-6 Z A2 SD Lat 11 SD X6-7 OS 11 1 000m 1 000m 6 SD 6 A1 59° 00’ N Z2 X1-3 OS X6 E1-2 A1 F Z X X1-3 X1-3 Long OS A2 Z SD SD OS X 6° 00’ W SD 58° Z A1 D1 SD SD OS SD D1 X6-7 9 Z SD 9 2 F X1 OS SD 2 D2 X4 INDEX AND EXPLANATION X D1 CENTRAL E1-2 SD X 2° 30’ 115 SD X6-7 115 LEWIS & HARRIS SD A1 D1 X8 SHETLAND Z Y3 A1 X1-3 OS (South) 1:100 000 Z Z SEDIMENTARY and METAMORPHIC ROCKS X A1 SD SD X6-7 Z F X1 Z X X D2 A1 A2 E1-2 X X1-3 3 8 3 9 4 0 4 1 4 2 F OS F Z X 9 1 A2 X 9 1 Z A1 E3 E1-2 A1 SD WESTERN ERA PERIOD EPOCH/AGE REGIONAL VARIATIONS X SD D2 Z2 D2 D2 F A1 114 D2 SHETLAND 114 G Z A1 101 102 SD X1 Million Z J4-6 103 Z SD Years Y3 X1 SD SD SD X6-7 NEOGENE Miocene N Buchan Gravels Formation A1 D1 58° 23 N G A1 J1 9 A3 A2 Z X J1 J2-4 9 X6-7 0 G X PT 0 Eocene - A1 CENOZOIC PALAEOGENE G Lough Neagh Clays Group X1 X8 Oligocene G E3 X1 113 113 65 G NORTHERN IRELAND Cretaceous to F SD SD SD KG Z1 A3 Z A2 X1 X Palaeogene rocks A2 91 X Ulster White Limestone and Hibernian Z X X K6 White Chalk Subgroup chalk with flints K6 A1 X X SD X8 Greensands formations, undivided J1 X1 D3 60° Chalk Group Z 60° X K5 Grey Chalk Subgroup clayey chalk 8 9 8 9 D2 Z A1 Z X CRETACEOUS Z Z X1 GREAT GLEN FAULT (GGF) X6-7 Z1 X1 112 112 K K4 Hunstanton Formation red chalk A2 A3 Z PT E1-2 SD A2 A3 X1 X Z F K2-3 Speeton Clay Formation mudstone MT X SD Z Y3 X SD 146 A1 G D2 X6-7 D2 SOUTHERN 8 A1 Z 90 Z A1 92 8 8 G 8 J6 Kimmeridge Clay and Ampthill Clay formations X SHETLAND Late Z PT Z D3 D2 11 1 111 X3 X6-7 Jurassic Corallian Group Upper Jurassic rocks, undifferentiated (J4-6) Z Z J4-6 G Z J5 Z X1 D1 X1 95 limestone, sandstone, siltstone and mudstone Z1 J4-6 93 94 D3 MESOZOIC Oxford Clay, Kellaways and Osgodby Clay fms Z J2-4 X1 96 JURASSIC J4 F A1 X Mid mudstone, locally sandy 8 A2 A2 8 J 7 A1 G 7 Jurassic Dogger Fm, Ravenscar Gp and Cornbrash Fm Middle Jurassic rocks, undifferentiated (J2-4) Z1 X1 J2-4 X1-3 J1 X6 X J2-3 J4-6 PT X7 11 11 sandstone, limestone and ironstone A1 A1 X D1 0 0 30’ A3 G D1 Z G J2-4 G SD D1 X5 Early J1 Lias Group mudstone and limestone G G X2 PT D3 OS Jurassic A1 A2 X2 D1 200 X2 X3 J4-6 D2 OS 97 Z G X1-3 Mercia Mudstone and Penarth groups A2 J2-4 Z E1-2 T2 8 F A1 X2 OS D1 8 mudstone with siltstone and evaporite 6 J2-4 X OS 6 G D1 X OS TRIASSIC Z D3 10 10 A1 Z Z X7 9 9 T T1 Sherwood Sandstone Group A2 J2-4 J2-4 G G G X D2 D2 X7 251 D3 X6 X6 D1 X7 X7 SD G F X7 SD Cumbrian Coast and Zechstein groups New Red Sandstone Supergroup A1 A1 SD P3 G PT A2 OS X5 X D2 OS mudstone (excluding Zechstein and Belfast groups) A3 G D2 X5 CP Z OS N X7 Zechstein and Belfast groups 8 5 A2 G 8 5 PERMIAN 80 X1 X2 X5 OS P2 limestone, dolostone, evaporite and mudstone G G X1 A1 X1-3 X X6 P J2-4 G SD X2 OS 87 10 8 108 Appleby, Stewartry, Enler and Rotliegende gps Stainmore Fm 81E 83 OS X8 OS OS P1 C4 G J1 82 A1 85 SD D2 CP 30’ sandstone, conglomerate and mudstone mainly sandstone Yoredale Group F PT SD X CP 299 NORTHERN ENGLAND X1 X1 84 OS OS mudstone, siltstone, G G OS SD C3 Alston Formation A3 SD E3 A2 X OS sandstone and Warwickshire Group A2 G X1 X2 X2 86 OS C8 X X6 OS N X7 CP limestone sandstone, siltstone and mudstone 8 G J1 N 8 D2 C2 Tyne Limestone Fm 4 81W F X2 SD SD SD SD 4 UIST & BARRA G CP CP OS C7 G X2 N 10 000m Upper X1 SD A1 OS X1-3 OS 70 1070000m Pennine Coal Measures G G SD X X5 Westphalian Coal Measures Group (North) 1:100 000 PT X1 X8 C5-8 Group A1 Z X2 SD GGF SD Lat Lat X1 4 C5-7 coal-bearing mudstone, C6 A2 A2 F SD X3 SD X7 OS Middle X2 90 75 SD X 59° 30’ N 4 0 4 1 4 2 4 3 4 4 4 5 4 6 4 7 59° 30’ N NORTHERN IRELAND coal bearing mudstone, SD SD X1-3 X1-3 OS X CP X siltstone and sandstone 3 000m X1-3 X8 000m A1 X2 OS OS siltstone and sandstone X1 A2 X1 CP C5 Slievebane Group C5 Lower 8 3 G J4-6 OS 8 3 Z A2 G CP OS Long Long CARBONIFEROUS UIST & BARRA G X6 Clackmannan Group C4 Kilskeery Group Millstone Grit Group G J1 G CP 2° 00’ W 30’ 1° 00’ W C Namurian C4 G X2 OS OS OS C3-4 sandstone, siltstone, mudstone, mudstone, sandstone and siltstone (South) 1:100 000 G G D1 X1-3 OS X6 X X C4 Leitrim and Ballycastle groups G PT SD A3 A1 X1-3 limestone and coal Craven and Bowland High groups F X1 X1 X2 X3 X6 CP G G X1 X2 X3 C3 Armagh Group C3 mudstone and siltstone with limestone A3 J2-4 J1 G G A3 SD Long Strathclyde Group G G G X1 72 X8 X8 3° Long Visean G SD X2 X2 SD OS D1 OS OS C2 C2 Great Scar Limestone and Border gps SD 05 90 G G SD G X8 3° 30’ W 2° 30’ W sandstone, siltstone and oil-shale C2 Tyrone and Carlingford limestone groups C2 8 2 G G SD X SD SD D1 8 2 limestone, sandstone and mudstone G G X1-3 SD 3 000m 3 000m A3 SD SD SD SD 70 G E3 PT G X1 X1-3 G G X1 X6 Inverclyde Group Omagh Sandstone, Roe Valley, Holywood Inverclyde and Ravenstonedale gps J4-6 SD X7 X7 3 1 3 2 3 3 34 3 5 3 6 3 7 3 8 Tournaisian C1 C1 C1 A1 A2 X1 X X3 SD 75 D1-3 359 sandstone, cementstone and limestone and Owenkillew Sandstone groups sandstone, limestone and mudstone E1-2 G SD SD OS OS 1060 000m 1060 000m F X1 E3 X1 MT SD OS 76 Late G SD X2 74 OS 77 D3 Upper Old Red Sandstone (Stratheden Group) Upper Devonian sandstones 71 X7 X7 Devonian D3 G X1 SD 73 X5 SD D1 (including Mell Fell Conglomerate) J2-4 G X1 SD SD X1-3 OS X5 X7 SD Mid 57° 8 G G G X1 X6 SD 8 1 D2 Middle Old Red Sandstone (Fintona Group) 1 A3 X2 X5 D1-3 Devonian NORTHERN MIDLAND VALLEY Old Red Sandstone A2 X2 SD ORKNEY D2 ISLE OF MAN X2 X2 X SD OS OS DEVONIAN Supergroup X OS G G A1 X1 SD D1-3 SD 1:100 000 D D1 Strathmore Group sandstone, siltstone, D2 D1-3 Lower Devonian sandstones G Y2 SD SD 10 10 Early D1 G SD SD SD 5 5 mudstone and PT X1 X1 SD X6 SD X7 Devonian D1 Arbuthnott - Garvock Gp (Peel Group) G SD D1 Lower Old Red Sandstone (Fintona and conglomerate X2 X SD PALAEOZOIC G G G SD X SD 416 Cross Slieve groups) G G X2 X SD X1-3 SD D2 D1 Dunnottar - Crawton Gp LAKE DISTRICT G X1 X2 X OS 8 0 X1 A1 X SD 8 0 A1 X1 X1-3 SD Pridoli Kirkby Moor Formation G F F X S3-4 Stonehaven Group G G SD SD CP S3-4 sandstone and siltstone 60 X2 X1 X1-3 SD D1-3 SD SD OS A2 G G SD SD X7 SD X1 OS 10 D3 D2 10 Ludlow Coniston Group G A1 X5 SD OS 4 4 S3 CP X2 SD X6 OS wacke Windermere G X SD SD X D3 SILURIAN G G J1 G X1 CP X5 X7 OS Wenlock S2 Riccarton Group Supergroup F OS SD X SD S wacke and siltstone; G J2-4 61 X1 G SD 63 64 (including 7 9 A1 SD 7 9 57° CP S1-3 mudstone and wacke X1 X1 X2 X2 SD SD S1 Hawick Group S1-2 in Midland Valley SHETLAND Dalby Group, OS CP 62 D1-3 X6 OS SD S1-2 SD X HIGHLAND BOUNDARY FAULT (HBF) D2 Llandovery and Northern Ireland Isle of Man) SD O1-2 S1 Gala Group G X3 X5 X5 SD 444 S1 Unst Phyllite Group G X1 SD CP OS X7 10 3 CP D2 D2 10 3 SD X6 OS S3-4 Shinnel and Dent Group CP X8 67 D3 Ashgill O5 O5 A1 G G X2 SD SD D1 SD Glenlee formations Scaur Leadhills Supergroup mudstone and sandstone G SD X3 SD SD
Recommended publications
  • 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.
    [Show full text]
  • 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‰.
    [Show full text]
  • Brief Overview of the Quarried Formations Around the UK
    Brief overview of the quarried formations around the UK David Entwisle, Don Cameron, Keith Ambrose and Andrew Bloodworth © NERC All rights reserved Quarrying in the UK ~1750 active quarries © NERC All rights reserved Materials quarried Rock aggregate Rail ballast, road stone, sub base, concrete, fill, drainage medium ‘Stone’ Armourstone, building stone, roofing, walling, kerbs, flagstone, flooring, monumental, decorative, rockery Clay/Mudstone Bricks, refractories, tiles, pipes, ceramics, fillers, cement, landfill liner, construction clay/fill, puddling, sea defences, paper Coal Energy Limestones Aggregate, cement, chemical industry, lime, pigment Minerals Barytes (drilling fluid), Fluorspar (flux, chemical industry), Gypsum (plaster, cement, chemical industry) Peat Horticulture, energy Sand Glass, Glass fibre, sport, horticulture, construction © NERC All rights reserved Quarries - one product for many uses Product used for • armourstone, • crushed rock aggregate • road stone • rail ballast Granodiorite, Mountsorrel complex, Ordovician, Mountsorrel Quarry, Loughborough, Leicestershire. Material extracted by blasting. © NERC All rights reserved Quarry working several mineral types for one product Oxford Clay, Kellaways, Cornbrash, Blisworth Limestone and Blisworth Clay formations, Jurassic, Ketton Quarry, Rutland. The of mudstone and limestone with different engineering characteristics – all used to manufacture cement © NERC All rights reserved Working of aggregates below the water table River Terrace Deposits – Sand and gravel © NERC
    [Show full text]
  • 1 GEOLOGICAL CONTROLS on RADON POTENTIAL in ENGLAND Scheib, C1, Appleton J. D.1, Miles J. C. H. 2*, .Hodgkinson, E 1British Geol
    GEOLOGICAL CONTROLS ON RADON POTENTIAL IN ENGLAND Scheib, C1, Appleton J. D.1, Miles J. C. H. 2*, .Hodgkinson, E1† 1British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. 2Health Protection Agency-Radiation Protection Division, Chilton, Didcot, Oxon OX11 0RQ, UK. *Present Address: 49 Nobles Close, Grove, Oxfordshire OX12 0NR, UK †Present Address: 87 Orchard Road, Birstall, Leicester LE4 4GD Corresponding author: Cathy Scheib British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. Email: [email protected] Tel: +44(0)115 936 3038 Fax: +44(0)115 936 3200 1 Abstract Radon exposure is a chronic and serious geohazard but with the correct knowledge of its distribution provided by an accurate radon potential map, this risk to human health can be reduced through well directed radon testing programmes and building control regulations. The radon potential map presented here, produced by mapping radon concentrations in homes, grouped by underlying geology, provides the most detailed and accurate assessment of radon in England. Bedrock and superficial geology associated with the most radon prone areas are investigated using the joint HPA-BGS radon potential dataset, geological information and, where available, soil geochemistry, airborne radiometric or laboratory analysis. Some of the geological units associated with high radon potential are well known, such as the granite intrusions in south west England, the Carboniferous limestones of Derbyshire and the Jurassic ironstones in Northamptonshire. This study provides a more comprehensive description of the main bedrock geological units associated with intermediate to high radon potential in England including: granites and associated uranium mineralisation in south west England; Devonian, Carboniferous, Permian and Jurassic limestones and dolomites; Devonian, Carboniferous, Jurassic and Cretaceous sandstones; Silurian, Devonian, Lower Carboniferous and Jurassic mudstones; Jurassic ironstones; and some Triassic breccias and conglomerates.
    [Show full text]
  • Mineral Resource Information in Support of National, Regional And
    Mineral Resource Information in Support of National, Regional and Local Planning: Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park) Commissioned Report CR/05/096N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/05/096N Mineral Resource Information in Support of National, Regional and Local Planning Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park) A J Bloodworth, G E Norton, C J Mitchell, R C Scrivener, D G Cameron, S F Hobbs, D J Evans, G K Lott and D E Highley This report accompanies the 1:100 000 scale maps: Devon, Key words North and South (comprising Devon, Plymouth, Torbay, Mineral resources, mineral Dartmoor National Park and part of Exmoor National planning, Devon. Park) Front cover Ball Clay extraction in the Bovey Basin, Devon. Photo by David Highley © BGS NERC 2006 Bibliographical reference BLOODWORTH, A J, NORTON, G E, MITCHELL, C J, SCRIVENER, R C, CAMERON, D G, HOBBS, S F, EVANS, D J, LOTT, G K AND HIGHLEY, D E. 2006. Mineral Resource Information in Support of National, Regional and Local Planning – Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park). British Geological Survey Commissioned Report, CR/05/096N. 16 pp. © Crown Copyright 2006 Keyworth, Nottingham British Geological Survey 2006 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation.
    [Show full text]
  • Leeds Thesis Template
    Middle to Late Miocene terrestrial biota and climate by Matthew James Pound M.Sci., Geology (University of Bristol) Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Earth and Environment September 2012 - 2 - Declaration of Authorship The candidate confirms that the work submitted is his/her own, except where work which has formed part of jointly-authored publications has been included. The contribution of the candidate and the other authors to this work has been explicitly indicated below. The candidate confirms that appropriate credit has been given within the thesis where reference has been made to the work of others. Chapter 2 has been published as: Pound, M.J., Riding, J.B., Donders, T.H., Daskova, J. 2012 The palynostratigraphy of the Brassington Formation (Upper Miocene) of the southern Pennines, central England. Palynology 36, 26-37. Chapter 3 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B. 2012. Global vegetation dynamics and latitudinal temperature gradients during the mid to Late Miocene (15.97 - 5.33 Ma). Earth Science Reviews 112, 1-22. Chapter 4 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B., Lunt, D.J. and Hunter, S.J. 2011. A Tortonian (Late Miocene 11.61-7.25Ma) global vegetation reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology 300, 29-45. This copy has been supplied on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. © 2012, The University of Leeds, British Geological Survey and Matthew J.
    [Show full text]
  • New Evidence from the Southern Petrockstow Basin, Devon
    Read at the Annual Conference of the Usher Society, January 1992 PALAEOGENE BASIN DEVELOPMENT: NEW EVIDENCE FROM THE SOUTHERN PETROCKSTOW BASIN, DEVON C. M. BRISTOW, Q. G. PALMER AND D. PIRRIE Bristow, C. M., Palmer, Q. G. and D. Pirrie. 1992. Palaeogene basin development: new evidence from the Southern Petrockstow Basin, Devon. Proceedings of the Ussher Society, 8, 19-22. The Petrockstow Basin is bounded by faults belonging to the Sticklepath-Lustleigh fault zone (SLFZ). New exposures in the Woolladon and Stockleigh ball clay pits at the southern end of the basin show the faulted contacts on both the east and west sides of the basin. On both sides the Palaeogene basinal sediments are overlain by the Upper Carboniferous Bude Formation. The faulted contacts dip away from the basin margin at angles between sub-horizontal and 25°. Field evidence suggests active vertical fault movement coeval with sedimentation. Basin development was clearly related to reactivation of major Variscan strike-slip faults, although the sense of fault motion is uncertain. C. M. Bristow and D. Pirrie, Camborne School of Mines, Redruth TR15 3SE Q. G. Palmer, ECC Ball Clays, Wareham BH2O 4AW INTRODUCTION In south west England there are a large number of north-west-southeast This is consistent with an interpreted palaeoflow direction from south- orientated strike-slip faults, on which the main dextral movement predates east to northwest. The shelf areas to the north-east and south-west the intrusion of the Variscan granites. The Sticklepath-Lustleigh fault zone are clay-dominated, although sands also occur in the Woolladon shelf (SLFZ) appears to belong to this group of faults, although this fault zone has sequence to the south-west.
    [Show full text]
  • Pre-Quaternary Geomorphological History and Geoheritage of Britain
    Pi o t r Mi g o ń & An d r e w go u d i e QUAESTIONES GEOGRAPHICAE 31(1) • 2012 PRE-QUATERNARY GEOMORPHOLOGICAL HISTORY AND GEOHERITAGE OF BRITAIN Pi o t r Mi g o ń Department of Geography and Regional Development, University of Wrocław, Wrocław, Poland ANDREW GOUDIE China Centre, University of Oxford, Oxford, U.K. Manuscript received: January 18, 2012 Revised version: March 12, 2012 Mi g o ń , P. & go u d i e A., Pre-Quaternary geomorphological history and geoheritage of Britain. Quaestiones Geogra- phicae 31(1), Bogucki Wydawnictwo Naukowe, Poznań 2012, pp. 67–79. 9 Figs. DOI 10.2478/v10117-012-0004-x, ISSN 0137-477X. ABSTR A CT . Substantial parts of the British Isles preserve landscapes that are the legacy of pre-Quaternary times. Some of these may be the result of burial and exhumation of pre-Cenozoic features. However, most landscapes post-date the Cretaceous transgression during which a Chalk mantle was laid down. Much of the British Isles became land during the Palaeogene and the Chalk cover was rapidly removed over large areas. Sea floor spre- ading, thermal uplift, and intrusion and extrusion of igneous material occurred. Landscapes also evolved in response to warm climatic conditions and this may have led to etchplanation. In the Neogene various surface formed and were affected by ongoing tectonic activity. Various estimates have been made of Cenozoic denu- dation rates and amounts, but they appear to have varied spatially and temporally. Landscapes which provide tangible evidence of pre-Quaternary times include those of north-east Scotland and southern England.
    [Show full text]
  • UK Coal Resource for New Exploitation Technologies Final Report
    UK Coal Resource for New Exploitation Technologies Final Report Sustainable Energy & Geophysical Surveys Programme Commissioned Report CR/04/015N BRITISH GEOLOGICAL SURVEY Commissioned Report CR/04/015N UK Coal Resource for New Exploitation Technologies Final Report *Jones N S, *Holloway S, +Creedy D P, +Garner K, *Smith N J P, *Browne, M.A.E. & #Durucan S. 2004. *British Geological Survey +Wardell Armstrong # Imperial College, London The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Coal resources, UK, maps, undergound mining, opencast mining, coal mine methane, abandoned mine methane, coalbed methane, underground coal gasification, carbon dioxide sequestration. Front cover Cleat in coal Bibliographical reference Jones N S, Holloway S, Creedy D P, Garner K, Smith N J P, Browne, M.A.E. & Durucan S. 2004. UK Coal Resource for New Exploitation Technologies. Final Report. British Geological Survey Commissioned Report CR/04/015N. © NERC 2004 Keyworth, Nottingham British Geological Survey 2004 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks.
    [Show full text]
  • Ig UIDE to GROUNDWATER VULNERABILITY MAPPING in ENGLAND and WALES National Rivers Authority
    NRA Water Resources 28 Ig UIDE TO GROUNDWATER VULNERABILITY MAPPING IN ENGLAND AND WALES National Rivers Authority GUIDE TO GROUNDWATER VULNERABILITY MAPPING IN ENGLAND AND WALES R C Palmer, I P Holman (Soil Survey and Land Research Centre, Cranfield University) N S Robins, M A Lewis (British Geological Survey) The Information Centre National Rivers Authority Waterside Drive © National Rivers Authority, 1995. Applications for reproduction should be to HMSO Copyright Unit, St Crispins, Norwich NR3 1PD First edition 1995 ISBN 0 11 310103 1 ISSN 1358-328X This Guide was produced for the NRA by the Soil Survey and Land Research Centre (SSLRC) and The British Geological Survey (BGS) under a contract constituting part of the NRA’s Research and Development programme. Designed by HMSO Graphic Design Cover and text printed on recycled materials (HMSO Recycled Register — Score 60.0) FOREWORD In 1992 the National Rivers Authority published its Policy and Practice for the Protection of Groundwater. The implementation of the policy depends upon the definition of groundwater source protection zones and on the preparation of vulnerability maps. This guide is one of two volumes which provide the background to the production and use of these two policy tools and complement the original policy document. The companion volume to this Guide is the Guide to Groundwater Protection Zones in England and Wales. GUIDE TO GROUNDWATER VULNERABILITY MAPPING IH ENGLAND AND WALES CONTENTS 1 INTRODUCTION 1 1.1 Aims of the guide 1 1.2 Background 1 1.3 Groundwater vulnerability
    [Show full text]
  • Zig Zag Quarry Environmental Permit Application Environmental Setting
    Zig Zag Quarry Environmental Permit Application Environmental Setting and Site Design Report May 2020 Prepared By Project Quality Control Sheet ORIGINAL Author Checked by Approved by Signature Date 22/05/2020 26/05/2020 27/05/2020 Company Aardvark EM Ltd Aardvark EM Ltd Aardvark EM Ltd Location: Harleyford Aggregates Ltd, Zig Zag Quarry, Aller Brake Road, Newton Abbot, TQ12 5FN Grid Reference: SX 88017 69020 Project Manager: Jon Pettitt MSc PIEMA Report Author: Matthew Wiese BSc Hons Report Number: 1922 – R005 Report Status: FINAL Copyright: All copyright in this document is reserved. Liability: This document contains information and may contain conclusions and recommendations. Every effort has been made to ensure that the information is accurate and that the opinions expressed are sound. However, Aardvark EM Limited cannot be made liable for any errors or omissions or for any losses or consequential losses resulting from decisions based on the information. Report Written and Produced By Aardvark EM Limited, Higher Ford, Wiveliscombe, Taunton, Somerset, TA4 2RL Telephone: 01984 624989, Facsimile: 01984 623912 Email: [email protected], Web: www.aardvarkem.co.uk Contents 1 Introduction .................................................................................................................. 1 2 Site details .................................................................................................................... 2 2.1 Site location ..........................................................................................................
    [Show full text]
  • Proceedings Ussher Society
    PROCEEDINGS OF THE USSHER SOCIETY VOLUME TWO PART TWO _______________ Edited by E. B. SELWOOD _______________ REDRUTH, NOVEMBER 1969 THE USSHER SOCIETY Chairman Dr. W. R. Dearman Vice-Chairman Mr. G. Bisson Secretary Dr. C. T. Scrutton Treasurer Dr. P. A. Floyd Editor Dr. E. B. Selwood Committee members : Mr. C. M. Bristow Mr. N. S. Butcher Dr. R. Goldring Prof. S. Simpson Mr. A. H. B. Stride Membership of the Ussher Society is open to all on written application to the Secretary and payment of the annual subscription Copies of this part and Parts 1 to 6 of Volume 1 are available, post free, from the Secretary who can also supply copies of the Bristol Abstracts (1960), post free. Correspondence and requests for membership and publications should be addressed to: Dr. C. T. Scrutton, Department of Geology, The University, Newcastle upon Tyne, NE1 7RU. PROCEEDINGS OF THE USSHER SOCIETY VOLUME TWO PART TWO _______________ Edited by E. B. SELWOOD _______________ REDRUTH, NOVEMBER 1969 CONTENTS page CHAIRMAN'S REPORT. … … … 59 INVITATION ADDRESS. Transgression of the Cretaceous sea in South-West England. By J. M. Hancock. … 61 The Cretaceous structure of Great Haldon (Abstract). By E. M. Durrance and R. J. O. Hamblin. … … 84 The structure of the southern margin of the Bovey Basin (Abstract). By C. M. Bristow and D. E. Hughes. … 84 Preliminary results of the mapping of the Bovey Basin (Abstract). By R. A. Edwards. … … 85 A new interpretation of the Pleistocene succession in the Bristol Channel area (Abstract). By D. Q. Bowen. … 86 Post glacial sea level changes in the Bristol Channel (Abstract).
    [Show full text]