DOCSLIB.ORG

Inferred Cleveland Dyke and the Whin Sill Offers a Complex Interpretation Challenge

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Durham E-Theses Magnetic investigation of igneous intrusions in Teesdale, Northern England Mwandoe, Elijah How to cite: Mwandoe, Elijah (2005) Magnetic investigation of igneous intrusions in Teesdale, Northern England, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/2712/ 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 Durham E-Theses • 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 Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk MAGNETIC INVESTIGATION OF IGNEOUS INTRUSIONS IN TEESDALE, NORTHERN ENGLAND By: Elijah Mwandoe Presented to the Graduate School, Durham University In Partial Fulfilment of the Degree of M.Sc. (RES) in Geophysics March 2005 Supervisors: Professors: R. C. Searle and N. Goulty Department of Earth Sciences University of Durham United Kingdom Magnetic Investigation of Igneous intrusions in Teesdale Abstract A total field magnetic survey was conducted in Harwood valley in Northern Teesdale, and the neighbouring area, to investigate the igneous intrusions which could be the cause of a magnetic anomaly and metasomatism in the mineralization of the area. Niccolite and other nickel-bearing minerals had been found in magnetite-rich ore at three localities in Harwood valley by a team of the British Geological Survey. This mineral assemblage has only been sighted in a few other zones and the cause of mineralization was assumed to be metamorphism due to the emplacement of the Whin Sill and associated dykes during the late Carboniferous-early Permian age. Magnetic profiles recently acquired in the area confirm the existence of a dyke intruding the Teesdale fault along the Harwood valley. The average amplitude of the anomaly is 350nT, reversed with respect to the present field. Further investigations to the south- east and north-west of the valley relate the intrusion with the known outcrops of the Cleveland dyke (Tertiary). An outcrop of an igneous intrusion that bears similar properties with samples of the Cleveland dyke rock was recently sighted by the author at lower Langdon Beck near the confluence of the Tees and Harwood rivers. Thin sections of this rock displayed an identical match in grain size and pigment composition with the Cleveland dyke samples from other known outcrops, confirming the dyke’s presence along the Teesdale Fault. Elijah Mwandoe 2 Magnetic Investigation of Igneous intrusions in Teesdale 2.5D modelling of the magnetic profiles was carried out and the results reflect the depth to the top of the dyke at Harwood to be about 30m. Thickness of the body varies from 5 to 25m but is 12m at Harwood and about 14m in Etters Gill. Further south of the valley at Langdon Beck is another geological formation; the Burtreeford Disturbance. This is a series of faulting and folding that was a result of compressional stress (Permian age) from a WSW direction. It also produced the E- facing monoclinal folds of the Dent Fault zone and the easterly directed Pennine thrusts of the Cross Fell Inlier before, during and after the emplacement of the Whin. The study here reflects the Disturbance as a magnetic high and its confluence with the Teesdale fault, the inferred Cleveland dyke and the Whin Sill offers a complex interpretation challenge. A GIS data base for the project area was created using Arc-GIS, GRAVMAG, SURFER, DIDGER and other Microsoft Office applications. General interpretation of the anomalies is conducted but conclusions raise several questions. The cause of the mineralization in Harwood Valley is still uncertain, though it could be due to the cooling Cleveland dyke (58Ma) or the dyke could be forming a passage for the fluids of unknown age from the lower crust or mantle that cool and crystallize at shallower depths. Elijah Mwandoe 3 Magnetic Investigation of Igneous intrusions in Teesdale Acknowledgements I would first wish to acknowledge my two supervisors; Professors R. C. Searle and N. Goulty for their tireless efforts in guiding me throughout the course, especially during the trying moments when I seemed to despair. Many thanks to all the staff and post graduate students at the department of Earth Sciences for their keen interest in my project and undiminished enthusiasm whenever I sought their help. Much gratitude to Dr. B. Young of the British Geological Survey for his repeated visits to offer the much needed geological expertise in the survey area, and to all the farmers in Harwood in whose land I was kindly permitted access during data acquisition. Last, but not least, I would wish to thank my wife and children in Kenya for their support and sacrifice in seeing the project to fruition as well as the Kenyan Government for the availed scholarship. Elijah Mwandoe 4 Magnetic Investigation of Igneous intrusions in Teesdale Table of contents Page 1. INTRODUCTION ...................................................................................................................... 13 2. GEOLOGY ................................................................................................................................. 18 2.1.1 REGIONAL GEOLOGY ........................................................................................................ 18 2.1.2 STATIGRAPHY ..................................................................................................................... 20 2.1.3 INTRUSIONS ......................................................................................................................... 23 2.2 GEOLOGY OF HARWOOD ..................................................................................................... 30 2.3 GEOLOGY OF CRONKLEY AND LANGDON BECK .......................................................... 31 2.3.1 SEDIMENTS .......................................................................................................................... 32 2.3.2 BURTREEFORD DISTURBANCE ....................................................................................... 32 2.3.3 DRIFT ..................................................................................................................................... 33 3. PREVIOUS GEOPHYSICAL WORK........................................................................................ 34 3.1 WHIN SILL AND ASSOCIATED DYKES .............................................................................. 34 3.1.1 WHIN SILL ............................................................................................................................ 34 3.1.2 PERMIAN DYKES ................................................................................................................ 37 3.1.3 TERTIARY DYKES............................................................................................................... 39 3.1.4 THE BURTREEFORD DISTURBANCE .............................................................................. 41 3.1.5 THE TEESDALE INLIER...................................................................................................... 42 4. THE MAGNETIC METHOD ..................................................................................................... 43 4.1 THEORY OF THE MAGNETIC METHOD ............................................................................. 43 4.2 THE GEOMAGNETIC FIELD .................................................................................................. 44 4.3 ROCK MAGNETIZATION ....................................................................................................... 45 4.4 METHODOLOGY...................................................................................................................... 47 4.4.1 DATA ACQUISITION TECHNIQUE ................................................................................... 47 4.4.2 DATA INTEGRATION ......................................................................................................... 48 4.4.3 DATA REDUCTION ............................................................................................................. 50 5 RESULTS ................................................................................................................................... 55 5.1 QUALITATIVE DATA ANALYSIS ......................................................................................... 55 5.1.1 ROUND HILL AREA ............................................................................................................ 55 5.1.2 HARWOOD AREA ................................................................................................................ 58 5.1.3 LANGDON BECK AREA ..................................................................................................... 61 5.1.4 ETTERS GILL AREA ............................................................................................................ 65 6 QUANTITATIVE ANALYSIS .................................................................................................. 70 6.1 INTRODUCTION .....................................................................................................................
Recommended publications
  • Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from Gravity Survey and Structural Inversion

    Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from Gravity Survey and Structural Inversion

    ESSOAr | https:/doi.org/10.1002/essoar.10501104.1 | CC_BY_NC_ND_4.0 | First posted online: Mon, 11 Nov 2019 01:27:37 | This content has not been peer reviewed. Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from gravity survey and structural inversion Rob Westaway 1,*, Sean M. Watson 1, Aaron Williams 1, Tom L. Harley 2, and Richard Middlemiss 3 1 James Watt School of Engineering, University of Glasgow, James Watt (South) Building, Glasgow G12 8QQ, UK. 2 WSP, 70 Chancery Lane, London WC2A 1AF, UK. 3 School of Physics, University of Glasgow, Kelvin Building, Glasgow G12 8QQ, UK. * Correspondence: [email protected]; Abstract: The Butterknowle Fault is a major normal fault of Dinantian age in northern England, bounding the Stainmore Basin and the Alston Block. This fault zone has been proposed as a source of deep geothermal energy; to facilitate the design of a geothermal project in the town of Bishop Auckland further investigation of its geometry was necessary and led to the present study. We show using three-dimensional modelling of a dense local gravity survey, combined with structural inversion, that this fault has a ramp-flat-ramp geometry, ~250 m of latest Carboniferous / Early Permian downthrow having occurred on a fault surface that is not a planar updip continuation of that which had accommodated the many kilometres of Dinantian extension. The gravity survey also reveals relatively low-density sediments in the hanging-wall of the Dinantian fault, interpreted as porous alluvial fan deposits, indicating that a favourable geothermal target indeed exists in the area.
  • NYM-Landscape-Character-Assessment-Reduced.Pdf

    NYM-Landscape-Character-Assessment-Reduced.Pdf

    WHITE YOUNG GREEN ENVIRONMENTAL NORTH YORK MOORS NATIONAL PARK LANDSCAPE CHARACTER ASSESSMENT CONTENTS Page No 1.0 INTRODUCTION 1 1.1 Background to the Report 1 1.2 The North York Moors National Park 1 1.3 Context and Scope of the Study 1 1.4 The Study Area 2 1.5 Relationship to Previous Studies 2 1.6 Relationship to Studies Undertaken within Areas Bounding the National Park 5 1.7 Methodology 6 1.8 Structure of the Report 7 1.9 The Next Steps 7 2.0 THE NORTH YORK MOORS NATIONAL PARK 8 2.1 Key Characteristics 8 2.2 Landscape Character 8 2.3 Physical Influences 9 2.4 Historical and Cultural Influences 10 2.5 Buildings and Settlement 11 2.6 Land Cover 11 3.0 CHANGE IN THE LANDSCAPE 13 3.1 Introduction 13 3.2 Agriculture 13 3.3 Upland Management 15 3.4 Biodiversity Aims 15 3.5 Trees, Woodland and Commercial Forestry 16 3.6 Recreation and Tourism 17 3.7 Settlement Change and Expansion 18 3.8 Communications, Power Generation and Distribution, Military Infrastructure 18 3.9 Roads and Traffic 19 3.10 Mining and Quarries 20 3.11 External Influences 20 3.12 Air Pollution and Climate Change 20 3.13 Geological and Archaeological Resource 20 4.0 LANDSCAPE CHARACTER TYPES AND AREAS 22 Moorland 23 (1a) Western Moors 26 (1b) Central & Eastern Moors 27 (1c) Northern Moors 29 Narrow Moorland Dale 34 (2a) Ryedale 37 (2b) Bilsdale 38 (2c) Bransdale 39 (2d) Farndale 40 (2e) Rosedale 41 (2f) Hartoft 42 (2g) Baysdale 42 (2h) Westerdale 43 (2i) Danby Dale 43 North York Moors National Park Authority North York Moors National Park Landscape Character Assessment
  • Mid-Week Geology Group Newsletter November 2018

    Mid-Week Geology Group Newsletter November 2018

    Mid-Week Geology Group Newsletter November 2018 John Williams Sheila Wilson Margaret Crawford Barry Tymon Programme planner Communications Treasurer Webmaster This is John’s last Newsletter before he stands down as Programme Planner. It takes our Programme to the end of May 2019. So far no individual has offered to replace John in this crucial role longer term. Meanwhile, to ensure continuity, I am pleased to report that three members have agreed to become part of a small sub group to arrange one or two events each next year. If anyone else wishes to become involved, please contact Sheila before the AGM. This newsletter provides further information on the 2019 Programme that was outlined in the June 18 Newsletter, with details of meeting points and what each event will cover. Our numbers have increased to 55 this year but actual attendance numbers at some events has reduced. Maybe some meetings are too far for some members? Or is it that most local locations have already been visited in recent years? We would like to discuss this issue further at the AGM. Our theme for the past two years as highlighted at the Skipton meeting is “How Geology Has Generated Industry in Yorkshire”. Many of our walks in 2017, 2018 and 2019 demonstrate this theme. The topic for our December AGM, however, seems to break away from this theme. Now that we know so much about the geology of our own planet, - as demonstrated by the many talks on faraway places that we have covered on recent Members Days – we will find out what the other rocky planets and moons of the Solar System may offer for the future.
  • Near-Surface Palaeocene Fluid Flow, Mineralisation and Faulting At

    Near-Surface Palaeocene Fluid Flow, Mineralisation and Faulting At

    Near-surface Palaeocene fluid flow, mineralisation and faulting at Flamborough Head, UK: new field observations and U-Pb calcite dating constraints Nick M W Roberts1, Jack K Lee1, 2, Robert E Holdsworth2, Christopher Jeans3, Andrew R. Farrant4, 5 Richard Haslam4 1Geochronology & Tracers Facility, British Geological Survey, Environmental Science Centre, Nottingham, NG12 5GG, UK 2Department of Earth Sciences, Durham University, Science Labs, Durham, UK 3Department of Earth Sciences, University of Cambridge, Downing Place, Cambridge, UK 4British Geological Survey, Environmental Science Centre, Nottingham, UK 10 Correspondence to: Nick M W Roberts ([email protected]) Abstract. We present new field observations from Selwicks Bay, NE England, an exposure of the Flamborough Head Fault Zone (FHFZ). We combine these with U-Pb geochronology of syn- to post-tectonic calcite mineralisation to provide absolute constraints on the timing of deformation. The extensional Frontal Fault zone, located within the FHFZ, was active at ca. 63 Ma, with protracted fluid activity occurring as late as ca. 55 Ma. Other dated tensile fractures overlap this timeframe, and also 15 cross-cut earlier formed fold structures, providing a lower bracket for the timing of folding and compressional deformation. The Frontal Fault zone acted as a conduit for voluminous fluid flow, linking deeper sedimentary units to the shallow sub- surface, potentially hosting open voids at depth for a significant period of time, and exhibiting a protracted history of fracturing and fluid-flow over several million years. Such fault-hosted fluid pathways are important considerations in understanding chalk reservoirs and utilisation of the sub-surface for exploration, extraction and storage of raw and waste materials.
  • An Overview of the Geology of Britain

    An Overview of the Geology of Britain

    An Overview of the Geology of Britain An Overview of the Geology of Britain The very creation of Britain as an island is a represented, with Proterozoic rocks of fascinating story in itself resulting from hun- between 1,500 and 3,000 million years of age dreds of millions of years of tectonic activity sharing the island with much younger sedi- wherein land masses collided and split apart ments from the Palaeogene less than 60 mil- again as they moved across the surface of the lion years of age. This diversity is readily globe in their tectonic ballet. Even since apparent as one journeys around Britain, as Precambrian times, which ended 542 million has been discovered during the preparation of years ago, the various land masses have been this book. This section provides a brief over- pirouetting across the globe with areas which view, with the following sections providing a are now oceans variously covered by land and greater level of detail for specific areas of vice versa. The history of the Earth of course interest. reaches much further back to 4,600 million If we start in East Anglia and work our way years ago, but if we documented the various clockwise around Britain we shall discover tectonic events just since the Precambrian much of this interesting geological variation. period, we should have an interesting list. If On the eastern coasts of Norfolk, Suffolk and just one of these events had been different, if a Essex, the geology is quite young with the moving land mass had altered its course by just sedimentary layers being deposited primarily a few degrees, if a continental split had occurred within the Palaeogene period, less than 65 at a slightly different position, if the timings million years ago.
  • National Geological Screening: Eastern England Region

    National Geological Screening: Eastern England Region

    National Geological Screening: Eastern England region Minerals and Waste Programme Commissioned Report CR/17/092 BRITISH GEOLOGICAL SURVEY MINERALS AND WASTE PROGRAMME COMMISSIONED REPORT CR/17/092 National Geological Screening: Eastern England region J Powell1, D Schofield1, R Haslam2, T Pharaoh2, E Crane3, J P Bloomfield3, J R Lee4, B Baptie4, R P Shaw5, T Bide5 and F M McEvoy 1Rock type, 2Rock structure, 3Groundwater, 4Natural processes, 5Resources Contributors/editors LP Field, R Terrington, P Williamson, I Mosca, N J P Smith, D E Evans, M Lewis, C Gent, M Barron, A Howard, G Baker, R M Lark, A Lacinska S Thorpe, H Holbrook, I Longhurst, L Hannaford and J R Ford The National Grid and other Ordnance Survey data © Crown Copyright and database rights 7. Ordnance Survey Licence No. 100021290 EUL. Keywords National geological screening, GDF, Eastern England, rock type, structure, groundwater, natural processes, resources Bibliographical reference POWELL, J, SCHOFIELD, D, HASLAM, R, PHARAOH, T, CRANE, E, BLOOMFIELD, J P B, LEE, J R, BAPTIE, B, SHAW, R P, BIDE, T AND F M MCEVOY. 2018. National geological screening: Eastern England region. British Geological Survey Commissioned Report, CR/17/092. 80pp BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at Nottingham, Edinburgh, London and Cardiff (Welsh British Geological Survey offices publications only). See contact details below or shop online at www.geologyshop.com Environmental Science Centre, Keyworth, Nottingham The London Information Office also maintains a reference NG12 5GG collection of BGS publications, including maps, for Tel 0115 936 3100 consultation. We publish an annual catalogue of our maps and other BGS Central Enquiries Desk publications; this catalogue is available online or from any of Tel 0115 936 3143 the BGS shops.
  • 2018 Thursday – Whitby Shore and Cleveland Dyke with Paul Hildreth

    2018 Thursday – Whitby Shore and Cleveland Dyke with Paul Hildreth

    th SEPTEMBER 13 2018 Thursday – Whitby Shore and Cleveland Dyke with Paul Hildreth Purpose of the visit To study the Lower and Middle Jurassic rocks of North Yorkshire exposed on the shore at Whitby. We will compare the litho- and biostratigraphies of the two major groups present (Whitby Mudstones and Saltwick Formation) and discuss their environments of deposition. Towards Saltwick Nab we will be able to study in detail the nature of the boundary between them. If time permits we can also consider the course of the River Esk and compare the geology of the two sides of the town. Meet: outside the Tourist Info. Centre Park: Harbour car park Itinerary Low tide at Whitby will be at about 1.15pm. For logistical reasons we will first visit an exposure of Middle Jurassic rocks west of West Pier before walking through Whitby to access the wave- cut platform at East Pier. The Lower Jurassic Whitby Mudstones are preserved in a syncline which also brings the overlying Saltwick Formation (Middle Jurassic) down to almost beach level. Here the Lower – Middle Jurassic boundary is represented by the Dogger Formation, a complex unit worthy of attention. There will be ample opportunity to look for and collect representative fossils which will include: ammonites (Dactylioceras sp. and Hildoceras sp.), bivalves, belemnites, plants (stems, leaves, rootlets) ichnofossils and, maybe, dinosaur footprints. On the day 12 of us met Paul at the car park near the railway station on a sunny but cold day after some had an exciting detour as the A64 was closed at York.
  • Opengeoscience 1: Igneous Intrusions and Lavas Opening Geological Maps to the World

    Opengeoscience 1: Igneous Intrusions and Lavas Opening Geological Maps to the World

    Earthlearningidea - http://www.earthlearningidea.com/ Opengeoscience 1: igneous intrusions and lavas Opening geological maps to the world Open the British Geological Survey ‘OpenGeoscience’ A dyke – see a vertical dyke cutting straight website at http://www.bgs.ac.uk/OpenGeoscience/ In the across the countryside and the geology by typing section ‘What is OpenGeoscience’, click on ‘Geology of ‘Goathland’ into the search box, as below. Britain’ to open the BGS ‘Geology of Britain viewer’. You can use this to see how geological formations appear on Derived from the 1:50 000 maps and also how they affect the shape of the land – scale BGS and apply this understanding anywhere in the world. digital geological The viewer is part of the BGS’s ‘Opengeoscience’ map, British Geological website showing geological maps down to 1:50,000 Survey © scale, of the whole of Britain. The BGS viewer uses NERC. different basemaps; by clicking ‘Switch basemap’ and All rights ‘Imagery’ you can choose an aerial view for one end of reserved. the scale and a geological map at the other – with all IPR/145-63CT gradations in between. So you can choose a geological This is the Cleveland Dyke which cuts across feature on the map and then slide the slider, then click much of Northern England, but is covered over by the location again to see how it affects the landscape. the glacial till (boulder clay), a superficial deposit shown in pale blue on the left of the map extract. Follow the instructions to find the examples of igneous features below – and much more.
  • Voice of the Moors

    Voice of the Moors

    VOICE OF THE MOORS NYMA – PROTECTING THE NORTH YORKSHIRE MOORS FOR PRESENT AND FUTURE GENERATIONS THE MAGAZINE OF ISSUE 133 THE NORTH YORKSHIRE AUTUMN 2018 MOORS ASSOCIATION (NYMA) £2.75 CONTENTS CHAIRMAN’S 2 Chairman’s foreword FOREWORD 4 Botany NAN SYKES: NORTH YORKSHIRE’S BOTANICAL TREASURE 6 Botany FOUR MORE FROM THE BOG 7 President’s piece THOUGHTS FROM GOVERNMENT POLICY ON NATIONAL PARKS A SPECIAL SEAT 8 Arts & Crafts REVIVING A CRAFT FROM In the last issue of Voice , I mentioned that the government had A BYGONE ERA announced a Review of National Parks and Areas of Outstanding 10 Geology PARDON THE INTRUSION Natural Beauty. In June, the terms of reference were published 11 Birds in your garden LONG TAILED TITS and the aims of the review were set out as follows: 12 Transport GETTING TO THE NATIONAL PARK BY “The review aims not to diminish the character or independence of PUBLIC TRANSPORT IN THE WINTER MONTHS our designated landscapes, or to impose new burdens on them and 12 Book THE HISTORY TREE the people who live and work in the areas they cover. Instead, its 13 Mycology IT WAS THE BEST OF TIMES … IT WAS purpose is to ask what might be done better, what changes could THE WORST OF TIMES assist them, and whether definitions and systems - which in many 13 Literature ALICE AND DRACULA cases date back to their original creation - are still sufficient”. 15 Skylarks / Crossword Amongst the objectives of the review are two especially 16 NYMA News / NYMA Walks important considerations: Cover Photo: Nan Sykes © Margaret Atherden • how to enhance the environment and biodiversity in existing designated landscapes, and • how to build on the existing eight-point plan for National Parks and to connect more people with the natural environment from all sections of society and improve health and wellbeing.
  • Northumbria Rocks

    Northumbria Rocks

    Open University Geological Society Journal Symposium Edition 2003 Northumbria Rocks University of Durham Contents Setting the scene: the geological framework and history of Northumbria 1 Paul F V Williams, Staff Tutor in Earth Science, The Open University in the North The Yoredale Cycles of Northumbria: High-Frequency Clastic-Carbonate Sequences 5 of the Mid-Carboniferous Icehouse World Maurice Tucker1, James Gallagher1, Kirstin Lemon1 & Melanie Leng2 1Department of Earth Sciences, University of Durham 2NIGL, British Geological Survey, Nottingham, The Caledonian Orogeny in northern Britain – a state of the arc 11 Howard A Armstrong, Department of Earth Sciences, University of Durham. Alan W Owen, Division of Earth Sciences, University of Glasgow. The Hydrogeology of the Great Northern Coalfield 19 Paul Younger, School of Civil Engineering & Geosciences, University of Newcastle Fissuring in the Magnesian Limestone of County Durham 25 Brian Young, BGS District Geologist – Northern England, British Geological Survey, Edinburgh The Fossil Collections at the Hancock Museum, Newcastle upon Tyne 27 Steve McLean, Hancock Museum, Barras Bridge, Newcastle upon Tyne Early Palaeozoic magmatism in northern England 34 David Millward, British Geological Survey, Edinburgh The Story of the Weardale Granite 39 Martin Bott, Emeritus Professor of Geophysics, University of Durham Northumberland Rocks - a story that has to be told 44 Stuart Monro, Scientific Director, Our Dynamic Earth, Edinburgh -------------------------------- A Taste of Namibia 45 Chris Crivelli Seven unconformaties and a thrust fault: north west Highlands excursion 4-11 May 2002 51 Margaret Donnelly, Lynn Everson, Stuart Fairley, Margaret Kennedy, complied by Jane Hickman Book reviews 18, 26, 33,58 It is the responsibility of authors to obtain the necessary permission to reproduce any copyright material they wish to use in their article.
  • To Volume 56

    To Volume 56

    PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 273 INDEX TO VOLUME 56 General index Carboniferous System new official names dykes, Palaeogene Hebridean swarm 1-4 Boreholes 57-58 Chronostratigraphy Cardioceras spp. 65-75,168,170 East Fife Coalfield 20 Lithostratigraphy Carreg Cennen Disturbance 21 East Lothian Syncline 19 Localities Castleton Reef Belt 111-150 East Midlands Shelf 254,259 Minerals Celtia 267 Ectocrinus spp. 102 New Taxa Cervus elaphus 197 Edapocrinus rugosus 104 charcoal analysis, Pasture Beck valley debris Enascocrinus redesdalensis 105 GENERAL cone 237,238-240 Equus ferus 197 Cheshire Basin 43 Erymoceras 168 Abrachiocrinus clausus 103 Chlamys (Radulospecten) drewtonensis 271 Escrick Moraine 194, 201, 202 Acetabulastoma 268 Cinderhill Fault 21 estuarine silts, interglacial, Kirmington, Lines. acritarchs 209,211,212, 213 Clackmannan Syncline 20,27 246-249 Acrocrinus alvestonensis 99,101 classification, new official names for Eubrontes 79 Actinocrinites spp. 89, 91, 93,101 Carboniferous System 57-58 Eumorphocrinus spp. 99,102 Aexithrophocrinus swaledalensis 99,105 'clastic dykes' 42 Euryocrinus spp. 94,105 algae 209-214,245 cleats (joints) in British Carboniferous coals Alligaticeras (A.) rotifer 165 15-30 FAULKNER, Michael, Moore medallist Alston Block 151-154, 223, 226, 230 cleavage, and new isochron ages, Ingleton 61-62 amber, black 264 Group 81-85 Fearnsides Prize 62 ammonites Cleveland Basin 77-80,173,174 Ferriby-Winterton Moraine 202 assemblages from Peak District buildups Cleveland Dyke \-A Flamborough Moraine 186-187, 202 111-150 cliffs, landscape geomorphology at Cayton flint artefacts, Kirmington, Lines. 200,248 Cambridgeshire 65-75 Bay 5-14 flint in chalk-rich diamictons, Garret Hill, and jet 261,262-263 climate change, and slope destabilization 12, Norfolk 32, 35-39 John William Neale's studies 271 235-236, 241 flint-rich sand and gravel, Garret Hill, South Cave Quarry 159-176 Cluthia 267 Norfolk 32-35 Ammonites spp.
  • Cleveland Naturalists' Field Club

    Cleveland Naturalists' Field Club

    CLEVELAND NATURALISTS’ FIELD CLUB RECORD OF PROCEEDINGS 1928 TO 1932 VOL.IV. Part 2 Edited by T.A. LOFTHOUSE F.R.I.B.A., F.E.S AND M. ODLING M.A., B.Sc.,F.G.S. PRICE THREE SHILLINGS (FREE TO MEMBERS) MIDDLESBROUGH; H & F STOKELD 1932 CONTENTS Officers Elected at the 48th – 51st Annual Meeting - 85 - 86 48th-51st Annual Reports - 87 - 94 Excavations at Eston Camp 1929 – F Elgee - 95 Field Meetings and Lectures 1928-32 - 96 - 98 History of Natural History Societies in Middlesbrough - J.W.R Punch F.R.A.S. - 99 - 106 In Memoriam J.J. Burton O.B.E., J.P., F.R.A.S J.W.R.PUNCH, F.R.A.S. -107 - 110 In Memorium H. Frankland F.I.C. E.W.Jackson F.I.C., F.G.S -110 - 111 A Few Cleveland Place Names Major R.B.Turton - 112 - 118 The Cleveland Whin Dyke J J Burton O.B.E., J.P., F.G.S., M.I.M.E - 119 -136 Notes on Wild Flowers Chas. Postgate & M Odling - 136 Report on Cleveland Lepidoptera T.A. Lofthouse, F.E.S. - 137 – 142 Coleoptera observed in Cleveland M.L. Thompson F.E.S. - 143 - 145 A Preliminary list of Cleveland Hemiptera M.L. Thompson F.E.S. - 146 – 156 Floods in the Esk Valley July 1930 and Sept 1931 – J.W.R.Punch F.R.A.S. - 156 – 166 Ornithological Notes in Yorkshire and South Durham – C E Milburn - 167 – 171 Meteorological Observations at Marton-in- Cleveland 1928-31 – M Odling M.A.,B.SC.,F.G.S - 172 – 176 Notes on the Alum Industry – H N Wilson F.I.C.