A Stratigraphical Framework for the Lower Cretaceous of England

Total Page:16

File Type:pdf, Size:1020Kb

A Stratigraphical Framework for the Lower Cretaceous of England A stratigraphical framework for the Lower Cretaceous of England Research Report RR/08/03 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are book- marked enabling direct links to be followed to the principal section headings and sub- headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/08/03 The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2008. Keywords A stratigraphical framework for the United Kingdom, England, Yorkshire, Lincolnshire, East Anglia, Southern England. Lower Cretaceous of England Geology, Stratigraphy, Lower Cretaceous, Early Cretaceous. P M Hopson, I P Wilkinson and M A Woods Front cover Ferruginous Sand Formation exposed above a significant landslide founded in the Atherfield Clay Formation, Red Cliff, Sandown Bay, Isle of Wight (P683788). Bibliographical reference HOPSON , P M, WILKINSON , I P, and WOODS , M A. 2008. A stratigraphical framework for the Lower Cretaceous of England. British Geological Survey. British Geological Survey Research Report, RR/08/03. ISBN 0 85272 623 5 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. Your use of any information provided by the British Geological Survey (BGS) is at your own risk. Neither BGS nor the Natural Environment Research Council gives any warranty, condition or representation as to the quality, accuracy or completeness of the information or its suitability for any use or purpose. All implied conditions relating to the quality or suitability of the information, and all liabilities arising from the supply of the information (including any liability arising in negligence) are excluded to the fullest extent permitted by law. © NERC 2008. All rights reserved Keyworth, Nottingham British Geological Survey 2008 BRITISH GEOLOGICAL SURVEY British Geological Survey offices The full range of our publications is available from BGS BGS Central Enquiries Desk shops at Nottingham, Edinburgh, London and Cardiff (Welsh Tel 0115 936 3143 Fax 0115 936 3276 publications only) see contact details below or shop online at email [email protected] www.geologyshop.com Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG The London Information Office also maintains a reference Tel 0115 936 3241 Fax 0115 936 3488 collection of BGS publications, including maps, for consultation. email [email protected] We publish an annual catalogue of our maps and other publications; this catalogue is available online or from any of the Murchison House, West Mains Road, Edinburgh EH9 3LA BGS shops. Tel 0131 667 1000 Fax 0131 668 2683 email [email protected] The British Geological Survey carries out the geological survey of Great Britain and Northern Ireland (the latter as an agency London Information Office at the Natural History Museum service for the government of Northern Ireland), and of the (Earth Galleries), Exhibition Road, South Kensington, surrounding continental shelf, as well as basic research projects. London SW7 2DE It also undertakes programmes of technical aid in geology in Tel 020 7589 4090 Fax 020 7584 8270 developing countries. Tel 020 7942 5344/45 email [email protected] The British Geological Survey is a component body of the Natural Environment Research Council. Columbus House, Greenmeadow Springs, Tongwynlais, Cardiff CF15 7NE Tel 029 2052 1962 Fax 029 2052 1963 Maclean Building, Crowmarsh Gifford, Wallingford OX10 8BB Tel 01491 838800 Fax 01491 692345 Geological Survey of Northern Ireland, Colby House, Stranmillis Court, Belfast BT9 5BF Tel 028 9038 8462 Fax 028 9038 8461 www.bgs.ac.uk/gsni/ Parent Body Natural Environment Research Council, Polaris House, North Star Avenue, Swindon SN2 1EU Tel 01793 411500 Fax 01793 411501 www.nerc.ac.uk Website www.bgs.ac.uk Shop online at www.geologyshop.com Acknowledgements The authors would like to thank numerous colleagues of Wales is thanked for his proof reading and additional within BGS who appraised parts of this document and who corrections to the text. created many of the lexicon entries on which this document Thanks are also due to the Geological Society draws. Stratigraphy Commission and their reviewers for comment Peter Rawson formerly of University College London and suggestions incorporated in this document. is thanked for his views and comments of various early drafts of this document. John Cope of the National Museum Peter Hopson, Ian Wilkinson and Mark Woods. iii British Geological Survey Research Report RR/08/04 Contents Summary vi 5.16 Wealden Group 56 5.17 Lower Greensand Group 56 1 Introduction 1 5.18 Selborne Group 61 1.1 The base of the Cretaceous in onshore basins 1 1.2 Offshore correlation 2 6 Cleveland/Yorkshire Basin 62 1.3 Other considerations 2 6.1 Speeton Clay Formation 62 2 Palaeogeography and Basin Definition 3 6.2 Hunstanton Formation 64 3 Wessex Basin (Wealden Basin) 5 Overview 67 3.1 Purbeck Basin 5 References 69 3.2 Wealden Group 8 3.3 Lower Greensand Group 14 3.4 Selborne Group 22 FIGURES 4 Wessex Basin (Vectian Basin) 25 4.1 Purbeck Group 25 1 The palaeogeography at various times throughout the 4.2 Wealden Group 28 Early Cretaceous 4 4.3 Lower Greensand Group 31 2 The relationship of the lithologies within the East 4.4 Selborne Group 35 Midlands Shelf area 42 5 East Midlands Shelf (including ‘Bedfordshire Straits’) 41 5.1 Sandringham Sands Formation 45 TABLES 5.2 Dersingham Formation 48 5.3 Roach Formation 49 1 The relationship between the Boreal and Tethyan 5.4 Carstone Formation 49 stages 1 5.5 Selborne Group 50 2 Lithostratigraphical scheme for the Wealden 5.6 Spilsby Sandstone Formation 50 Basin 6 5.7 Claxby Ironstone Formation 51 3 Lithostratigraphical scheme for the Vectian 5.8 Tealby Formation 52 Basin 26 5.9 Roach Formation 53 4 Lithostratigraphical scheme for the East Midlands 5.10 Skegness Clay Formation 53 Shelf 43 5.11 Sutterby Marl Formation 54 5 Deposits of the ‘Bedfordshire Straits’ and related 5.12 Carstone Formation 54 areas 44 5.13 Hunstanton Formation 55 6 Lithostratigraphical scheme for the Cleveland/ 5.14 Sandringham Sands Formation 55 Yorkshire Basin 63 5.15 Purbeck Group 55 7 Overview of the Lower Cretaceous 68 v British Geological Survey Research Report RR/08/03 Summary This report describes the Lower Cretaceous strata of Clear terminology and relationships exist over the East England appearing on maps and major texts from the British Midlands Shelf and needs little adjustment at formation and Geological Survey and seeks to clarify the lithostratigraphical member level. terminology, relationships and distribution of the various In the marginal area of the Wessex Basin from north units. The report considers the successions in England Wiltshire to Bedfordshire, a number of new terms (at formation within defined sedimentological basins: the Wessex Basin level) are proposed for the thin isolated units encountered; more (including the Wealden Basin and Vectian Basin — sub- research may clarify their relationships and require a further basins of some authors), the East Midlands Shelf covering reappraisal of these terms used herein and in the literature. Lincolnshire, South Yorkshire and Norfolk (strictly not a The Whitchurch Sand Formation is now considered to be of basin in its own right) and the Cleveland–Yorkshire Basins Valanginian age and includes those beds formerly described are described. The marginal basin successions of north as the Shotover Ironsands. The isolated outcrops attributed to Wiltshire to Bedfordshire (the ‘Bedfordshire Straits’) are the Lower Greensand Group are all given formation status. included in the descriptions for the East Midlands Shelf The terms ‘Calne Sand’ and ‘Seend Ironstone (Ironsand of area. some authors)’ are firmly emplaced within the literature The base of the Lower Cretaceous is taken at the base and are retained. The Faringdon Sand Formation has been of the Berriasian Stage that occurs in the lower part of the introduced and includes the Faringdon Sponge Gravels Purbeck Group of the English succession. Consequently the Member, Baulking Sand Member and Fernham Sand Member. Lulworth Formation is described herein as it is principally Terms such as the ‘Red Sands’ of Uffington, ‘Junction Beds’ of Berriasian age. The Haddenham Formation, a new term and ‘Transition Beds’ have been abandoned and the unnamed proposed herein, covers those beds formerly called the outcrops around Clifton Hampden incorporated into the newly Purbeck Limestone Formation within the marginal basin defined Baulking Sand Member, Fernham Sand Member and areas in Wiltshire, Oxfordshire and Buckinghamshire. Munday’s Hill Phosphatic Sandstone Formation; the latter These are probably of latest Jurassic, Portlandian Stage, but including the Shenley Limestone Member. show strong lithological affinities to the restricted salinity The term ‘Selborne Group’ is formally introduced environments of the Purbeck Group rather than the open to include the Gault Formation and Upper Greensand marine conditions of the Portland Group. The Purbeck Formation.
Recommended publications
  • A Fragment of the Geography of England. South West Sussex Author(S): Hugh Robert Mill Source: the Geographical Journal, Vol
    A Fragment of the Geography of England. South West Sussex Author(s): Hugh Robert Mill Source: The Geographical Journal, Vol. 15, No. 3 (Mar., 1900), pp. 205-227 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774689 Accessed: 27-06-2016 19:49 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 165.193.178.102 on Mon, 27 Jun 2016 19:49:48 UTC All use subject to http://about.jstor.org/terms The Geographical Journal. No. 3. MARPCH, 1900. VOL. XV. A FRAGMENT OF THE GEOGRAPHY OF ENGLAND. SOUTH WEST SUSSEX.' By HUGH ROBERT MILL, D.Sc., F.R.S.E. Introductory.-In 1896 I proposed a scheme for a geographical description of the United Kingdom, based on the maps of the Ordnance Survey, and consisting of a separate memoir for every sheet of the map on the scale of 1 inch to a mile.t I was requested by the Royal Geographical Society to prepare a specimen memoir, and, by the advice of Sir John Farquharson, then Director-General of the Ordnance Survey, chose Sheet No.
    [Show full text]
  • Conceptualising Groundwater Flow Systems at a National (British Mainland) Scale
    Conceptualising groundwater flow systems at a national (British mainland) scale Brighid Ó Dochartaigh and BGS Hydro-JULES team 11 September 2019 Seeking answers to 2 questions: How can an integrated & holistic approach to modelling terrestrial hydrology – including groundwater – improve: 1. Simulation of major flooding events, such as 2013-14 floods? 2. Assessment of water resources under drought conditions? Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 2 British mainland (WP4.1) 3D Parameterising Deep geological Saturated GW domain – Unsaturated framework Zone code technique Zone code model Conceptual FY18/19 models of groundwater (GW) flow Parameterising Model Sub-surface GW domain – instance code application FY19/20 Results Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 3 Britain’s diverse geology and hydrogeology Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 4 3D Geological Framework Model +1.5 km to -15 km 1:625,000 scale mapping Newell 2019 Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 5 Model includes 3D information from: borehole geology & geophysics; pre-existing cross sections; geological history & structure; seismic data Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 6 Geology: a physical framework for groundwater flow Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 7 Key groundwater conceptual model parameters Geology Geography Surface water Groundwater Aquifer Chemistry Flow Aquifer Topographic relief Recharge quantity, Groundwater flow Aquifer properties: e.g.
    [Show full text]
  • Back Matter (PDF)
    PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 309 INDEX TO VOLUME 55 General index unusual crinoid-coral association 301^ Lake District Boreholes Craven inliers, Yorkshire 241-61 Caradoc volcanoes 73-105 Chronostratigraphy Cretoxyrhinidae 111, 117 stratigraphical revision, Windermere Lithostratigraphy crinoid stems, N Devon 161-73 Supergroup 263-85 Localities crinoid-coral association 301-4 Lake District Batholith 16,73,99 Minerals crinoids, Derbiocrinus diversus Wright 205-7 Lake District Boundary Fault 16,100 New Taxa Cristatisporitis matthewsii 140-42 Lancashire Crummock Fault 15 faunal bands in Lower Coal Measures 26, Curvirimula spp. 28-9 GENERAL 27 Dale Barn Syncline 250 unusual crinoid-coral association 3Q1-A Acanthotriletes sp. 140 Dent Fault 257,263,268,279 Legburthwaite graben 91-2 acritarchs 243,305-6 Derbiocrinus diversus Wright 205-7 Leiosphaeridia spp. 157 algae Derbyshire, limestones 62 limestones late Triassic, near York 305-6 Diplichnites 102 foraminifera, algae and corals 287-300 in limestones 43-65,287-300 Diplopodichnus 102 micropalaeontology 43-65 origins of non-haptotypic palynomorphs Dumfries Basin 1,4,15,17 unusual crinoid-coral association 301-4 145,149,155-7 Dumfries Fault 16,17 Lingula 22,24 Alston Block 43-65 Dunbar-Oldhamstock Basin 131,133,139, magmatism, Lake District 73-105 Amphoracrinus gilbertsoni (Phillips 1836) 145,149 Manchester Museum, supplement to 301^1 dykes, Lake District 99 catalogue of fossils in Geology Dept. Anacoracidae 111-12 East Irish Sea Basin 1,4-7,8,10,12,13,14,15, 173-82 apatite
    [Show full text]
  • Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
    A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C.
    [Show full text]
  • Greensand.Pdf
    www.natureswayresources.com GREENSAND Greensand is a naturallyoccurring mineral mined from ocean deposits from a sedimentary rock known as “Glauconite”. It is often an olive-green colored sandstonerock found in layers in many sedimentary rock formations. Origin of Greensand Greensand forms in anoxic (without oxygen) marine environments that are rich in organic detritus and low in sedimentary inputs. Some greensands contain marine fossils (i.e. New Jersey Greensand). Greensand has been found in deposits all over the world. The greenish color comes from the mineral glauconite and iron potassiumsilicate that weathers and breaks down releasing the stored minerals. The color may range from a dark greenish gray, green-black to blue-green dependingon the minerals and water content. It often weatherseasilyand forms nodules that have been oxidized with iron bearing minerals that has a reddish brown or rust color. +3 The major chemical description is ((K,Na)(Fe , Al, Mg)2(Si,Al)4O10(OH)2) General chemical information: Iron (Fe) 12-19% Potassium (K) 5-7 % Silicon (Si) 25.0% Oxygen (O) 45% Magnesium (Mg) 2-3 % Aluminum (Al) 1.9 % Sodium (Na) 0.27% Hydrogen (H) 0.47% Over 30 other trace minerals and many micronutrients. Types of Greensand Glauconite is the namegiven to a group of naturally occurring iron rich silica minerals that may be composed of pellets or grains. When glauconite is mined the upper layers that have weathered and become oxidizedand minerals are released.These sometimes form pyrite a iron sulfide (FeS2) when oxygen is www.natureswayresources.com absent. In the deeper layers or reduced zone pyrite crystals often form.
    [Show full text]
  • Geology and the Landscape of the North Wessex Downs Factsheet
    Factsheet Geology and the Landscape of the North Wessex Downs The majority of the North Wessex Downs is underlain by chalk resulting in the beautiful gentle rolling topography which is so characteristic of the North Wessex Downs. The area is influenced by geological formations from the Cretaceous, Palaeogene and Quaternary periods. There is also a direct link between the building materials used in the AONB and the local underlying geology. This is explored in the leaflet 'Diversity in Stone' Geological History of the North Wessex Downs Lower Cretaceous (145 – 99 million years ago) Only the top most part of the Lower Cretaceous (the Gault Clay and the Upper Greensand) are found in the AONB. The Gault Clay is restricted to a narrow band marking the foot of the Downs on the northern margin. This blue-grey mudstone has historically been extracted from the Swindon and Devizes area for brick making. The junction between the Gault Clay and the overlying Upper Greensand is marked on the northern edge of the AONB by a spring line which gave rise to the development of the villages such as Cherhill and Uffington. The sands and silts of the Upper Greensand are rich in a mineral called glauconite, giving them their green colour. As well as tracing the northern scarp of the AONB the Upper Greensand is also seen at the surface in the Vale of Pewsey, as a result of the uplift of the basin. Towards the top of the Upper Greensand is a bed known as the Malmstone. This is a hard sandstone composed of siliceous spicules held together with a silica rich cement.
    [Show full text]
  • Chapter 2 Physical Characteristics of the Study Area
    CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area.
    [Show full text]
  • WALKING EXPERIENCES: TOP of the WIGHT Experience Sustainable Transport
    BE A WALKING EXPERIENCES: TOP OF THE WIGHT Experience sustainable transport Portsmouth To Southampton s y s rr Southsea Fe y Cowe rr Cowe Fe East on - ssenger on - Pa / e assenger l ampt P c h hi Southampt Ve out S THE EGYPT POINT OLD CASTLE POINT e ft SOLENT yd R GURNARD BAY Cowes e 5 East Cowes y Gurnard 3 3 2 rr tsmouth - B OSBORNE BAY ishbournFe de r Lymington F enger Hovercra Ry y s nger Po rr as sse Fe P rtsmouth/Pa - Po e hicl Ve rtsmouth - ssenger Po Rew Street Pa T THORNESS AS BAY CO RIVE E RYDE AG K R E PIER HEAD ERIT M E Whippingham E H RYDE DINA N C R Ve L Northwood O ESPLANADE A 3 0 2 1 ymington - TT PUCKPOOL hic NEWTOWN BAY OO POINT W Fishbourne l Marks A 3 e /P Corner T 0 DODNOR a 2 0 A 3 0 5 4 Ryde ssenger AS CREEK & DICKSONS Binstead Ya CO Quarr Hill RYDE COPSE ST JOHN’S ROAD rmouth Wootton Spring Vale G E R CLA ME RK I N Bridge TA IVE HERSEY RESERVE, Fe R Seaview LAKE WOOTTON SEAVIEW DUVER rr ERI Porcheld FIRESTONE y H SEAGR OVE BAY OWN Wootton COPSE Hamstead PARKHURST Common WT FOREST NE Newtown Parkhurst Nettlestone P SMALLBROOK B 4 3 3 JUNCTION PRIORY BAY NINGWOOD 0 SCONCE BRIDDLESFORD Havenstreet COMMON P COPSES POINT SWANPOND N ODE’S POINT BOULDNOR Cranmore Newtown deserted HAVENSTREET COPSE P COPSE Medieval village P P A 3 0 5 4 Norton Bouldnor Ashey A St Helens P Yarmouth Shaleet 3 BEMBRIDGE Cli End 0 Ningwood Newport IL 5 A 5 POINT R TR LL B 3 3 3 0 YA ASHEY E A 3 0 5 4Norton W Thorley Thorley Street Carisbrooke SHIDE N Green MILL COPSE NU CHALK PIT B 3 3 9 COL WELL BAY FRES R Bembridge B 3 4 0 R I V E R 0 1
    [Show full text]
  • DAW 2018 Brochure
    DAW_2018_BROCHURE_COVER [3]_Layout 1 14/03/2018 15:49 Page 1 DORSET ART WEEKS 2018 DORSET ART FREE GUIDE OPEN STUDIOS, EXHIBITIONS, EVENTS 26 MAY –26 MAY 10 JUNE 26 MAY – 10 JUNE 2018 26 MAY – 10 JUNE 2018 OPEN STUDIOS, EXHIBITIONS, EVENTS DORSET VISUAL ARTS DORSET COTTAGES DORSET VISUAL ARTS DAW_2018_BROCHURE_COVER [3]_Layout 1 14/03/2018 15:49 Page 2 DORSET VISUAL ARTS DVA is a not for profit organisation and registered charity. It has a membership of some 300 artists, designers and makers living and practising in the county, some with national and international reputations. We are currently developing a number of opportunities for our members working across the spectrum of the visual arts with a focus on creative and professional development. Making Dorset www.dorsetvisualarts.org The driving ambition behind this grouping is to bring high quality design and making to new markets within and beyond Dorset. We aim to develop the group’s identity further to become recognised nationally and Dorset Art Weeks internationally. Membership of the OPEN STUDIOS group is by selection. EXHIBITIONS EVENTS DORSET DAW is an open studio event open to all artists practising in Dorset, regardless of DVA membership. VISUAL Produced by DVA, it is its biennial, Membership Groups flagship event. Reputedly the largest biennial open studios event in the ARTS INTERROGATING PROJECTS country. The event attracts around For those wanting to benefit from 125,000 studio visits. Visitors are interaction with other artists. The focus fascinated by seeing how artists work of group sessions is on creative and and the varied types of environment professional development.
    [Show full text]
  • (Foram in Ifers, Algae) and Stratigraphy, Carboniferous
    MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract
    [Show full text]
  • RWM Eastern England Subregion 1
    Eastern England SUBREGION 1 RWM | Eastern England Subregion 1 Contents 1 Eastern England Subregion 1 Introduction 2 Rock type 3 Rock structure Groundwater 4 Resources Natural processes 5 - 12 Figures 13 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 | Eastern England Subregion 1 Our work shows that we may find a suitable geological setting for a GDF in most of this subregion. Rock can be seen at the surface in some of this subregion such as the sea cliffs, cliffs in the North York Moors and in man-made excavations such as quarries or road cuttings. Combined with numerous deep boreholes and some geophysical investigations, this gives us an understanding of the rocks present and their distribution. There are clay-rich rock layers under most of the subregion in which we may be able to site a GDF. There are also layers of rock salt under most of the eastern coastal half of the subregion and extending off the coast, in which we may be able to site a GDF.
    [Show full text]
  • Review of the Pterodactyloid Pterosaur Coloborhynchus 219
    Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W.
    [Show full text]