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STRATEGIC STONE STUDY a Building Stone Atlas of NORTH-EAST YORKSHIRE
STRATEGIC STONE STUDY A Building Stone Atlas of NORTH-EAST YORKSHIRE Published May 2012 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © NE Yorkshire Bedrock Geology NERC. All rights reserved Click on this link to visit NE Yorkshire’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window http://maps.bgs.ac.uk/buildingstone?County=North-EastYorkshire ) NE Yorkshire Strategic Stone Study 1 Stratigraphical column of the Permian (in part),Triassic, Jurassic and Cretaceous rocks and Quaternary deposits in North-east Yorkshire showing the common buildings stones (bold) and alternative stone names. The oldest rocks are at the bottom of the table. Gp., Group; Fm., Formation; Mbr., Member. North East Yorkshire: Permian, Triassic, Jurassic, Cretaceous & Quaternary Building Stones PERIOD GROUP FORMATION MEMBER Common/alternative Stone Name Calcareous Tufa; Aquarium Stone Till (Boulder Clay) and Fluvio-glacial sand Quaternary and gravel; boulders Tertiary Cleveland Dyke Whinstone Flamborough Chalk Fm. Flamborough Chalk; White Chalk Burnham Chalk Fm. Burnham Chalk; White chalk Chalk Group Welton ChalkFm. Cretaceous Ferriby Chalk Fm. Grey chalk ungrouped Hunstanton Fm. Speeton Clay Kimmeridge Clay ungrouped Ampthill Clay North Grimston Upper Calcareous Grit Upper Calcareous Grit Cementstone North Grimston Cementstone Formation Coral Rag Member Coral Rag Malton Oolite Member Malton Oolite; Hildenley Limestone; Corallian Hildenley Stone Group Middle Calcareous Grit Middle Calcareous Grit Coralline Oolite Formation Member Birdsall Calcareous Grit Birdsall Calcareous Grit Member Hambleton Oolite Hambleton Oolite Member Yedmandale Member Passage Beds; Wallstone Lower Calcareous Grit Fm. Lower Calcareous Grit Oxford Clay Fm. -
The Magnetic Ironstone Conundrum
The genesis of geology in York and beyond HOGG 25th Anniversary Meeting Thursday 24th October Field Excursion Notes Rosedale - the magnetic ironstone conundrum Rosedale – the magnetic ironstone conundrum Afternoon Rosedale – the magnetic ironstone conundrum Practical Men “The practice of geology, through the search for mines and minerals, has been much less attended to by historians than has the geology undertaken by leisured amateurs - even though practical geology was as important in the past as the oil industry is today.” Hugh Torrens (2002) The Practice of British Geology, 1750–1850. London: Routledge. Introduction At its peak in the mid 1870s-mid 1880s the ironstone industries in the area (alongside the remainder of the Cleveland Hills) provided 38% of Britain’s need for iron, which equated to 20% of world demand. The area contributed to the shifting industries in North East England and the establishment of Middlesbrough as a centre of iron-making and its impact on the nation and the world beyond. Iron was in much demand - investment in construction of railways, in Britain and abroad started around 1835 and continued apace for the next three decades creating a significant demand for rails made from iron. In 1835 ironstone was first identified and the first underground ironstone mining commenced in the Cleveland Hills ironstone mining district. Ironstone was identified in stream near tunnel works at Grosmont when building the new railway between Whitby and Pickering and was subsequently worked along the Murk Esk Valley at Beck Hole and Esk Valley, then at Kildale. In 1853 a magnetic ironstone with a significantly high iron content was discovered in Rosedale. -
A Detailed Record of Deglacial and Early Post-Glacial Fluvial Evolution: the River Ure in North Yorkshire, UK
quaternary Article A Detailed Record of Deglacial and Early Post-Glacial Fluvial Evolution: The River Ure in North Yorkshire, UK James Innes 1,*, Wishart Mitchell 2, Charlotte O’Brien 3, David Roberts 1, Mairead Rutherford 4 and David Bridgland 1 1 Geography Department, Durham University, Science Labs, South Road, Durham DH1 3LE, UK; [email protected] (D.R.); [email protected] (D.B.) 2 Division of Geography, University of Dundee, Dundee DD1 4HN, UK; [email protected] 3 Archaeology Department, Durham University, Science Labs, South Road, Durham DH1 3LE, UK; charlotte.o’[email protected] 4 Oxford Archaeology North, Mill 3, Moor Lane Mills, Moor Lane, Lancaster LA1 1GF, UK; [email protected] * Correspondence: [email protected] Abstract: The lower reaches of the River Ure, on the flanks of the Pennine Hills in northern England, contain sedimentary and erosional landforms that are a record of fluvial activity during deglaciation and valley-glacier retreat at the end of the last (Devensian) glacial period, and in the subsequent post- glacial Holocene. Terraces and channels, most of which are now relict features well above the altitude of the present river, attest to the impacts of massive meltwater discharge and deposition of sand and gravel outwash, and dynamic river regimes with rapid incision. Through field survey, we have created a detailed geomorphological map of these landforms and glacial and fluvioglacial surface deposits, as well as the terraces and palaeochannels that were abandoned by the river due to avulsion Citation: Innes, J.; Mitchell, W.; and incision-driven course changes. -
Scarborough Geological Watching Brief: Toll House Shaft Site, Castle Hill SSSI
Scarborough Geological Watching Brief: Toll House Shaft Site, Castle Hill SSSI Geology and Regional Geophysics Internal Report IR/13/025 BRITISH GEOLOGICAL SURVEY Geology and Regional Geophysics INTERNAL REPORT IR/13/025 Scarborough Geological The National Grid and other Watching Brief: Toll House Shaft Ordnance Survey data © Crown Copyright and database rights 2013. Ordnance Survey Licence Site, Castle Hill SSSI No. 100021290. Keywords Scarborough; Castle Hill, Toll J H Powell and J B Riding House Shaft; Geology; Callovian-Oxfordian, Middle Jurassic, SSSI Contributor National Grid Reference Centre point: E 505209.71 B M Cox N. 488927.96 Map Editors Sheet 54, 1:50 000 scale, Scarborough A S Howard & J Ford Front cover Oblique aerial view of Castle Hill looking NW; courtesy of Arup (photograph courtesy of www.petersmith.com) Bibliographical reference Powell, J H and Riding, J B. 2013. Scarborough Geological Watching Brief; Toll House Shaft Site, Castle Hill SSSI British Geological Survey Internal Report, IR/13/025. 48 pp + figures. 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. © NERC 2013. All rights reserved Keyworth, Nottingham British Geological Survey 2013 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. -
Yorkshire Geology As Seen Through the Eyes of Notable British Geological Survey Geologists 1862-2000 46-67 in Myerscough, R and Wallace, V
Yorkshire geology as seen through the eyes of notable British Geological Survey geologists 1862-2000 46-67 in Myerscough, R and Wallace, V. Famous Geologists of Yorkshire. PLACE, York. ISBN 978-1-906604-58-5. By Anthony H. Cooper Honorary Research Associate, British Geological Survey, Nottingham, NG12 5GG, UK This paper was presented at the PLACE (People, Landscape & Cultural Environment Education and Research Centre) conference 3rd October 2015. The printed version along with 5 other papers on the theme of Famous Yorkshire Geologists can be obtained from PLACE; details at www.place.uk.com e-mail [email protected] The first pieces in the puzzle Making a geological map is like doing a 3-dimensional jigsaw puzzle, but with 99% of the pieces missing and without the picture on the box to help. It involves looking at the lie of the land and piecing together various sources of evidence to put the rocks in order and visualise the result as a 3-dimensional model of what is hidden below the surface. It is “landscape literacy” and unlike a topographical map, such as those produced by the Ordnance Survey, it is largely an interpretation rather than the map of observable features. Each geologist and each new map update builds on what has gone before. Some geologists add more than others and some make ground-breaking observations. A few geologists have great insights in fitting the pieces together and fundamentally change the way we interpret Earth history, an example being the recognition of continental drift, a major advance built on many diverse observations. -
Stratigraphy, Sedimentology and Structure of the Jurassic (Callovian to 2 Lower Oxfordian) Succession at Castle Hill, Scarborough, North 3 Yorkshire, UK
1 Stratigraphy, sedimentology and structure of the Jurassic (Callovian to 2 Lower Oxfordian) succession at Castle Hill, Scarborough, North 3 Yorkshire, UK 4 5 John H. Powell* & James B. Riding 6 British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, UK 7 * Correspondence: [email protected] 8 9 Abstract: Site investigation borehole cores and temporary shaft exposures at the Toll House Pumping Station 10 shaft site, Castle Hill, Scarborough, North Yorkshire, have revealed new data on the Callovian to Lower 11 Oxfordian (Jurassic) succession. The condensed transgressive marine unit, the Lower Callovian Cornbrash 12 Formation, rich in berthierine ooids and abundant shelly fossils, and the attenuated Cayton Clay Formation 13 represent the Early Callovian marine transgression that flooded the low-gradient alluvial plain which is 14 represented by the underlying Scalby Formation. The Callovian Osgodby Formation (Red Cliff Rock and 15 Langdale members) is an extensively bioturbated, silty sandstone with abundant berthierine-pyrite ooids in the 16 lower part. It was deposited in lower- to upper-shoreface settings. Slow sedimentation rates, with long sediment 17 residence time, resulted in a diverse ichnofauna and a high bioturbation index. Framboidal pyrite ooids in the 18 lower Osgodby Formation sandstones are interpreted as being formed in anoxic lagoons in the nearshore zone; 19 ooids were subsequently swept offshore during storm surge-ebb events. Cold water dinoflagellate cysts of 20 Boreal affinity such as Gonyaulacysta dentata in the lower part of the Oxford Clay Formation indicate an Early 21 Oxfordian age. This is confirmed by the presence of the zonal ammonite species Quenstedoceras mariae and is 22 consistent with a relatively cold, but warming, palaeoclimate at this time. -
Geology of the Yorkshire Coast Sedimentary Rock Types
05/03/2013 Geology of the Yorkshire Coast Dr Liam Herringshaw - [email protected] Sedimentary rock types 1 05/03/2013 Sedimentary grain size Grain size reflects energy: – - Strong currents pick up larger grains – - Proxy for environment (& sea level) Geology of Yorkshire 2 05/03/2013 Coastal geology of North- East Permian England Triassic Permian on the Yorkshire coast Boulby Potash Mine 3 05/03/2013 Salts from the Zechstein Sea Large, arid, northern European basin Drilling for salts Permian polyhalites 4 05/03/2013 Magnesian Limestone Permian at the coast Caythorpe gas field, near Bridlington 5 05/03/2013 Geology of the Yorkshire Coast - The Cleveland Basin 6 05/03/2013 The Early Jurassic: Redcar – Ravenscar Redcar Mudstone Formation Staithes Sandstone Formation Cleveland Ironstone Formation Whitby Mudstone Formation Lias Group Lias = Old term for lower Jurassic; In Yorkshire (after Powell 1984): - Lower Lias = Redcar Mudstone Formation; - Middle Lias = Staithes Sandstone Formation, Cleveland Ironstone Formation; - Upper Lias = Whitby Mudstone Formation 7 05/03/2013 Lias of Yorkshire Redcar Mudstone Formation Robin Hood's Bay Redcar Earliest Jurassic unit on Yorkshire Coast – - Divided into 4 members 8 05/03/2013 Redcar Rocks Redcar Rocks geological map (Rawson & Wright 1992) 9 05/03/2013 Hummersea Image © Dave Eagle, geograph.org.uk Common fossils Gryphaea arcuata, an Early Jurassic 'oyster' 10 05/03/2013 Trace fossils Rhizocorallium, Boggle Hole Robin Hood's Bay 11 05/03/2013 Robin Hood's Bay Why does Redcar Mudstone Fm reappear so -
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. -
Welsh Geology's
Putting fossil forest Spreading the word treasures on display E about geodiversity U S S I 46 Importance of South Autumn 2016 Welsh geology’s Downs geology global significance OUTCROPS INSIDE EDITORIAL OUTCROPS 3-6 Why conserving South Downs geology is so important 7 With enduring pressure on budgets, and with the great unknown of ‘Brexit’ ahead Skye’s extraordinary of us, it is more important than ever for everyone engaged in geoconservation dinosaur discoveries 11 and geodiversity to work together to keep our subjects at the forefront of Field trip signals global agendas. importance of Wales 14 HAVE YOUR SAY! How do we With this in mind, our packed issue 46 ranges widely over many of the strands of work control damage to vital sites? 15 that make conserving Britain’s geodiversity perenially worthwhile. There are articles on Checking and managing the importance of sites for scientific study; practical site management; site Scotland’s geo-heritage 16 interpretation and promotion to the public; the use of geotourism to boost local Re-exposing the Carboniferous economies; geology within education; building geoconservation issues into planning; of Northern England 17 and even a request for ideas on how best to limit damage to sites. The writers of these 30 years of funding Earth articles also illustrate the diversity of people and organisations active in our subject – science projects 19 national conservation agencies, geoparks, societies, academics and volunteers. Miller’s spirit lives on in writing competition 21 As ever, we want to hear your views and to learn of new projects. Please contact the Saltscape builds new awareness most appropriate editor (below). -
How to Navigate This Document How to Navigate This Document
BRITISH GEOLOGICAL SURVEY RESEARCH REPORT NUMBER RR/99/01 A formational framework for the Lower Jurassic of England and Wales (onshore area) B M Cox, M G Sumbler and H C Ivimey-Cook Geographical index England and Wales Subject index Geology, stratigraphy, lithostratigraphy, Lias Group, Triassic, Jurassic Bibliographical Reference Cox, B M, Sumbler, M G and Ivimey-Cook, H C. 1999. A formational framework for the Lower Jurassic of England and Wales (onshore area) British Geological Survey Research Report, RR/99/01 © 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 Figures 2 Preface Figure 1a Generalised outcrop map of the Lias Group 3 Introduction in England and Wales showing the structural elements that controlled deposition 4 Stratigraphical framework Figure 1b Inferred distribution of land and sea during 4.1 Supraformational classification deposition of the Lias Group –– based on 4.2 Cleveland Basin Donovan and Howarth in Cope et al. -
Yorkshire Geological So
Downloaded from http://pygs.lyellcollection.org/ by guest on September 26, 2021 Yorkshire Geological So 150TH ANNIVERSARY YEAR A message from the President This year has been one of celebration for the Society and give opportunity for discussion, but no one was lost in we have marked it with a special programme of the mist". Mercifully the weather was superb for our trip meetings. Here I mention some of these meetings with on the slopes of Ingleborough in 1988. special bearing on the anniversary celebrations. At the centenary meeting Dr W. S. Bisat, a former Firstly, the Annual Dinner in December 1987 was President of our Society, was given an Honorary Master held on a date very close to that of the original of Science degree by Leeds University. One of our field inauguration of the Society. The spacious Assembly trips this year, led by Dr N. J. Riley, was designed as a Rooms in York were the venue for the dinner. A short tribute to the work of Dr Bisat on goniatites as zonal account and two of the speeches are quoted in the fossils. following pages. The Yorkshire Geological Society was founded (as The four full weekend field meetings included a the Geological and Polytechnic Society of the West Grand Reunion field meeting at Cober Hill, Cloughton Riding of Yorkshire) by coal owners and managers. It near Scarborough. This took place in superb weather, was particularly appropriate, therfore, that the subject and included a visit to the home of Lord Derwent at of 'Recent Advances in British Coalfield Geology and Hackness Hall, where William Smith, the founder of Geophysics1 was chosen as our topic for the session British geology, was land agent. -
New Field Observations and U-Pb Calcite Dating Constraints Nick M W Roberts1, Jack K Lee1, 2, Robert E Holdsworth2, Christopher Jeans3, Andrew R
https://doi.org/10.5194/se-2020-73 Preprint. Discussion started: 6 May 2020 c Author(s) 2020. CC BY 4.0 License. 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 was active at ca. 63 Ma, with protracted fluid activity occurring as young as ca. 55 Ma. Other dated tensile fractures overlap this timeframe, and also cross-cut earlier formed 15 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, and exhibiting a protracted history of several million years. Most structures at Selwicks Bay may have formed in a deformation history that is simpler than previously interpreted, with a protracted phase of extensional and strike-slip motion along the FHFZ.