Editorial This Linnean Is Mainly Concerned with the Welsh Marches
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Vol 8, Issue 2, June 2009
mag30.qxd 05/05/2009 17:46 Page 1 MAGAZINE OF THE GEOLOGISTS’ ASSOCIATION Volume 8 No. 2 June 2009 Appeal for the Archives WSGS Study Tour of Guernsey Meetings July/October ROCKWATCH News Awards Proceedings of the GA Bernard Leake Retires Getting the most from the PGA Dates for your Diary Presidential Address/Lecture Reports GA Trip to Chafford Hundred Book Reviews CIRCULAR 979 mag30.qxd 05/05/2009 17:45 Page 2 Magazine of the Geologists’ Association From the President Volume 8 No.2, 2009 In writing the June presidential report, I am reminded of the vital role that the GA Published by the plays in upholding the importance of geology on a range of scales, from local Geologists’ Association. to international. For example, the GA can serve as a point of contact to provide Four issues per year. CONTENTS critical information on key geological ISSN 1476-7600 sequences that are under threat from 3. The Association insensitive development plans - in short, Production team: JOHN CROCKER, acting as an expert witness. This does Paula Carey, John Cosgrove, New GA Awards not necessarily entail opposing develop- Vanessa Harley, Bill French 4. GA Meetings July/October ment but rather looking for opportunities to enhance geological resources for 5. Awards Printed by City Print, Milton Keynes future study while ensuring that they are 6. Bernard Leake Retires appropriately protected. In addition, a major part of our national earth heritage The GEOLOGISTS’ ASSOCIATION 7. Dates for your Diary is preserved within our museums and in does not accept any responsibility for 8. -
Wales Regional Geology RWM | Wales Regional Geology
Wales regional geology RWM | Wales Regional Geology Contents 1 Introduction Subregions Wales: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks Older sedimentary rocks 3 Basement rocks Rock structure 4 Groundwater 5 Resources 6 Natural processes Further information 7 - 21 Figures 22 - 24 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Wales Regional Geology Introduction This region comprises Wales and includes the adjacent inshore area which extends to 20km from the coast. Subregions To present the conclusions of our work in a concise and accessible way, we have divided Wales into 6 subregions (see Figure 1 below). We have selected subregions with broadly similar geological attributes relevant to the safety of a GDF, although there is still considerable variability in each subregion. The boundaries between subregions may locally coincide with the extent of a particular Rock Type of Interest, or may correspond to discrete features such as faults. -
Herefordshire
114 KIXSH.•UI. HEREFORDSHIRE, Great Western railway, about 12 north-west from Leo- landowner: the place is of interest as having"once been the resi minster, 7 north-east from Kington and about 23 north- dence of the family of Miss Florence Nightingale: Lord Byron west from Hereford, in the Northern division of the county, stayed some time at the Court. A room in the house is still Wigmore hundred, Kington union and petty sessional called Byron's room, and there is a seat under a large cedar division and Presteigne county court district. Upper Kins- tree in the grounds, where he is said to have written "Childe ham and Lower Kinsham were amalgamated March 25, Harold": the scenery is exquisite and the fishing abundant. 1886, and the parish designated Kinsham. All Saints Immediately below Kinsham Court is Kinsham Dingle, one church is a building of stone, in the Early English style, of the most pi,cturesque spots in the county, at the bottom of consisting of chancel, nave and a small belfry containing which runs the river Lugg. Itwas through this dingle that the one bell: the chancel retains a piscina and there is a hagio- defeated Lancastriansfled after the battle of Mortimer's.Cross. scope with shutter: in the chancel is also a fine marble The soil is of a clayey description; subsoil, the same. The tablet to Thomas Harleyesq. and on the floor an old altar- chief crops are wheat, barley and turnips. The area is slab, 4 by 9 feet, some of the crosses on which are still 1,538 acres; rateable value, £1,752 j the population in 1891 visible. -
Hydrogeology of Wales
Hydrogeology of Wales N S Robins and J Davies Contributors D A Jones, Natural Resources Wales and G Farr, British Geological Survey This report was compiled from articles published in Earthwise on 11 February 2016 http://earthwise.bgs.ac.uk/index.php/Category:Hydrogeology_of_Wales BRITISH GEOLOGICAL SURVEY The National Grid and other Ordnance Survey data © Crown Copyright and database rights 2015. Hydrogeology of Wales Ordnance Survey Licence No. 100021290 EUL. N S Robins and J Davies Bibliographical reference Contributors ROBINS N S, DAVIES, J. 2015. D A Jones, Natural Rsources Wales and Hydrogeology of Wales. British G Farr, British Geological Survey Geological Survey 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. Maps and diagrams in this book use topography based on Ordnance Survey mapping. Cover photo: Llandberis Slate Quarry, P802416 © NERC 2015. All rights reserved KEYWORTH, NOTTINGHAM BRITISH GEOLOGICAL SURVEY 2015 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS British Geological Survey offices shops at Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or BGS Central Enquiries Desk shop online at www.geologyshop.com Tel 0115 936 3143 Fax 0115 936 3276 email [email protected] The London Information Office also maintains a reference collection of BGS publications, including Environmental Science Centre, Keyworth, maps, for consultation. -
NLCA06 Snowdonia - Page 1 of 12
National Landscape Character 31/03/2014 NLCA06 Snowdonia Eryri – Disgrifiad cryno Dyma fro eang, wledig, uchel, sy’n cyd-ffinio’n fras â Pharc Cenedlaethol Eryri. Ei nodwedd bennaf yw ei mynyddoedd, o ba rai yr Wyddfa yw mynydd uchaf Cymru a Lloegr, yn 3560’ (1085m) o uchder. Mae’r mynyddoedd eraill yn cynnwys y Carneddau a’r Glyderau yn y gogledd, a’r Rhinogydd a Chadair Idris yn y de. Yma ceir llawer o fryndir mwyaf trawiadol y wlad, gan gynnwys pob un o gopaon Cymru sy’n uwch na 3,000 o droedfeddi. Mae llawer o nodweddion rhewlifol, gan gynnwys cribau llymion, cymoedd, clogwyni, llynnoedd (gan gynnwys Llyn Tegid, llyn mwyaf Cymru), corsydd, afonydd a rhaeadrau. Mae natur serth y tir yn gwneud teithio’n anodd, a chyfyngir mwyafrif y prif ffyrdd i waelodion dyffrynnoedd a thros fylchau uchel. Yn ddaearegol, mae’n ardal amrywiol, a fu â rhan bwysig yn natblygiad cynnar gwyddor daeareg. Denodd sylw rhai o sylfaenwyr yr wyddor, gan gynnwys Charles Darwin, a archwiliodd yr ardal ym 1831. Y mae ymhell, fodd bynnag, o fod yn ddim ond anialdir uchel. Am ganrifoedd, bu’r ardal yn arwydd ysbryd a rhyddid y wlad a’i phobl. Sefydlwyd bwrdeistrefi Dolgellau a’r Bala yng nghyfnod annibyniaeth Cymru cyn y goresgyniad Eingl-normanaidd. Felly, hefyd, llawer o aneddiadau llai ond hynafol fel Dinas Mawddwy. O’i ganolfan yn y Bala, dechreuodd y diwygiad Methodistaidd ar waith trawsffurfio Cymru a’r ffordd Gymreig o fyw yn y 18fed ganrif a’r 19eg. Y Gymraeg yw iaith mwyafrif y trigolion heddiw. -
THE SKYDMORES/ SCUDAMORES of ROWLESTONE, HEREFORDSHIRE, Including Their Descendants at KENTCHURCH, LLANCILLO, MAGOR & EWYAS HAROLD
Rowlestone and Kentchurch Skidmore/ Scudamore One-Name Study THE SKYDMORES/ SCUDAMORES OF ROWLESTONE, HEREFORDSHIRE, including their descendants at KENTCHURCH, LLANCILLO, MAGOR & EWYAS HAROLD. edited by Linda Moffatt 2016© from the original work of Warren Skidmore CITATION Please respect the author's contribution and state where you found this information if you quote it. Suggested citation The Skydmores/ Scudamores of Rowlestone, Herefordshire, including their Descendants at Kentchurch, Llancillo, Magor & Ewyas Harold, ed. Linda Moffatt 2016, at the website of the Skidmore/ Scudamore One-Name Study www.skidmorefamilyhistory.com'. DATES • Prior to 1752 the year began on 25 March (Lady Day). In order to avoid confusion, a date which in the modern calendar would be written 2 February 1714 is written 2 February 1713/4 - i.e. the baptism, marriage or burial occurred in the 3 months (January, February and the first 3 weeks of March) of 1713 which 'rolled over' into what in a modern calendar would be 1714. • Civil registration was introduced in England and Wales in 1837 and records were archived quarterly; hence, for example, 'born in 1840Q1' the author here uses to mean that the birth took place in January, February or March of 1840. Where only a baptism date is given for an individual born after 1837, assume the birth was registered in the same quarter. BIRTHS, MARRIAGES AND DEATHS Databases of all known Skidmore and Scudamore bmds can be found at www.skidmorefamilyhistory.com PROBATE A list of all known Skidmore and Scudamore wills - many with full transcription or an abstract of its contents - can be found at www.skidmorefamilyhistory.com in the file Skidmore/Scudamore One-Name Study Probate. -
A Template for an Improved Rock-Based Subdivision of the Pre-Cryogenian Timescale
Downloaded from http://jgs.lyellcollection.org/ by guest on September 28, 2021 Perspective Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2020-222 A template for an improved rock-based subdivision of the pre-Cryogenian timescale Graham A. Shields1*, Robin A. Strachan2, Susannah M. Porter3, Galen P. Halverson4, Francis A. Macdonald3, Kenneth A. Plumb5, Carlos J. de Alvarenga6, Dhiraj M. Banerjee7, Andrey Bekker8, Wouter Bleeker9, Alexander Brasier10, Partha P. Chakraborty7, Alan S. Collins11, Kent Condie12, Kaushik Das13, David A. D. Evans14, Richard Ernst15,16, Anthony E. Fallick17, Hartwig Frimmel18, Reinhardt Fuck6, Paul F. Hoffman19,20, Balz S. Kamber21, Anton B. Kuznetsov22, Ross N. Mitchell23, Daniel G. Poiré24, Simon W. Poulton25, Robert Riding26, Mukund Sharma27, Craig Storey2, Eva Stueeken28, Rosalie Tostevin29, Elizabeth Turner30, Shuhai Xiao31, Shuanhong Zhang32, Ying Zhou1 and Maoyan Zhu33 1 Department of Earth Sciences, University College London, London, UK 2 School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, UK 3 Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA, USA 4 Department of Earth and Planetary Sciences, McGill University, Montreal, Canada 5 Geoscience Australia (retired), Canberra, Australia 6 Instituto de Geociências, Universidade de Brasília, Brasilia, Brazil 7 Department of Geology, University of Delhi, Delhi, India 8 Department of Earth and Planetary Sciences, University of California, Riverside, -
A Dispute Over the Emerging Geology of Wales
g-327E Cambria versus Siluria: A Dispute over the Emerging Geology of Wales Colin Humphrey GEOLOGICAL HISTORY AND THE ORIGINS OF Sedgwick’s standing gradually recovered and today he is A DISPUTE generally regarded as having been unfairly treated by Murchison. The present review comes to a different One of the great scientific disputes of the mid-nineteenth conclusion: the early mistakes were due more to century concerned the partitioning of a large part of Wales Sedgwick’s preconceptions, uncooperative attitude, and into younger and older rocks. It started in the 1830s with lack of application and method, than they were to the work of two very different men, and the most important Murchison’s failings, but both men’s intransigence, and British geologists of the time. They began as close friends Sedgwick’s resentment, ensured that a lifelong dispute but eventually were bitterly estranged. Their failure to ensued. collaborate resulted in a big overlap between their scientific claims. Neither would concede. They argued over Regional geology and what the old geologists knew terminology, and priority - the right to name the hitherto More than 500 million years ago, in the Cambrian period, un-described rocks. This right was a treasured intellectual Mid Wales was an ancient sea, known rather property, more so then than it is now. There was more unimaginatively by geologists as the Welsh Basin, a sea interest in geology then because the age of steam had which probably extended north into another basin around begun, the industrial revolution was well under way, and the Lake District. The Welsh Basin (Figure 1) lay near the the realisation was dawning that geology pointed the way to edge of a supercontinent called Gondwana, situated near to coal.1 Over a period of nearly forty years their differences where Australia is now. -
Curator 9-2 Cover.Qxd
Volume 9 Number 2 GEOLOGICAL CURATORS’ GROUP Registered Charity No. 296050 The Group is affiliated to the Geological Society of London. It was founded in 1974 to improve the status of geology in museums and similar institutions, and to improve the standard of geological curation in general by: - holding meetings to promote the exchange of information - providing information and advice on all matters relating to geology in museums - the surveillance of collections of geological specimens and information with a view to ensuring their well being - the maintenance of a code of practice for the curation and deployment of collections - the advancement of the documentation and conservation of geological sites - initiating and conducting surveys relating to the aims of the Group. 2009 COMMITTEE Chairman Helen Fothergill, Plymouth City Museum and Art Gallery: Drake Circus, Plymouth, PL4 8AJ, U.K. (tel: 01752 304774; fax: 01752 304775; e-mail: [email protected]) Secretary David Gelsthorpe, Manchester Museum, Oxford Road, Manchester M13 9PL, U.K. (tel: 0161 3061601; fax: 0161 2752676; e-mail: [email protected] Treasurer John Nudds, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Oxford Road, Manchester M13 9PL, U.K. (tel: +44 161 275 7861; e-mail: [email protected]) Programme Secretary Steve McLean, The Hancock Museum, The University, Newcastle-upon-Tyne NE2 4PT, U.K. (tel: 0191 2226765; fax: 0191 2226753; e-mail: [email protected]) Editor of Matthew Parkes, Natural History Division, National Museum of Ireland, Merrion Street, The Geological Curator Dublin 2, Ireland (tel: 353 (0)87 1221967; e-mail: [email protected]) Editor of Coprolite Tom Sharpe, Department of Geology, National Museums and Galleries of Wales, Cathays Park, Cardiff CF10 3NP, Wales, U.K. -
CAMBRIDGE LIBRARY COLLECTION Books of Enduring Scholarly Value
Cambridge University Press 978-1-108-08122-1 - A Monograph of British Trilobites from the Cambrian, Silurian, and Devonian Formations John William Salter Frontmatter More information CAMBRIDGE LIBRARY COLLECTION Books of enduring scholarly value Monographs of the Palaeontographical Society The Palaeontographical Society was established in 1847, and is the oldest Society devoted to study of palaeontology worldwide. Its primary role is to promote the description and illustration of the British fossil flora and fauna, via publication of an authoritative monograph series. These monographs cover a wide range of taxonomic groups, from microfossils, trilobites and ammonites through to Coal Measure plants, mammals and reptiles, and from all ages from Cambrian to Pleistocene. They form a benchmark for understanding the past life of the British Isles and many include the original descriptions of numerous key species. The first monograph (on the Crag Mollusca) was published in March 1848 and the Society still continues this work today. Notable authors in the series include Charles Darwin (fossil barnacles) and Richard Owen (dinosaurs and other extinct reptiles). Beginning in 2014, the Cambridge Library Collection and the Society are collaborating to reissue the earlier publications, focusing on monographs completed between 1848 and 1918. A Monograph of British Trilobites from the Cambrian, Silurian, and Devonian Formations At the time of his death, John William Salter (1820–69) was dubbed ‘the prince of palaeontologists’. A true naturalist with a particular interest in Trilobita, he started publishing this monograph in 1864, and three further parts were issued in 1865–7. But his heath failed and he died, leaving around half of the trilobites then known from Britain untreated; the work was wound up in 1883. -
Coastal Cliff Failures at Colhuw Beach, Wales, UK
Transactions on Ecology and the Environment vol 9, © 1996 WIT Press, www.witpress.com, ISSN 1743-3541 Coastal cliff failures at Colhuw beach, Wales, UK A.T. Williams, P. Davies, A.P. Belov Centre for Science and Technology, University of Glamorgan, Pontypridd, Mid-Glamorgan, CF371DL, Wales, UK Abstract Several numerical models of cliff failure have been utilised in an attempt to understand failure mechanisms at Colhuw beach located in the Glamorgan Heritage Coast, Wales, UK. An understanding as to why falls occur is pre requisite for any management scheme, particularly with the current concern for public safety and consequent financial liabilities Translation failure was common at heavily limestone buttressed cliff sites of Jurassic bucklandi - limestone dominated cliffs and in areas where mudstone dominated angulata series outcropped. Toppling was common at vertical and overhanging cliff sites which exhibited basal undercutting and/or where a hard, thick limestone fulcrum existed in the cliff face on which the block could rotate and topple. The factor of safety reduced as the ratio of undercutting depth (d) to tension fracture distance (D) in the cliff face increased. Instability forces can be modest ranging from 1.7 to 2.7 MNm"2, but this is enough to exceed cross joint strength as weathering takes place. Sea notching is evidenced at many sites and is a result of wave hydraulic forces, pebble impact, clay expansion and contraction and joint weakening by water movement /seepage and ice. Introduction Cliff instability has been long associated with Colhuw beach, Llantwit Major, UK (Williams and Davies, [7,10]; Williams et al, [11,12], Davies and Williams, [2], Davies et #/, [3]). -
Obits in Year Book 2013 FINAL
BSBI Yearbook 2013: 85-87 DAVID RIDLEY HUMPHREYS, MD, FRCP (1916 – 2011) David was born in Birmingham, the eldest of Calcutta and in Darjeeling and was once heard three, to a father who was an insurance to casually mention dining, under the stars in company manager. He was educated in Small a Maharaja’s palace, in the company of the Heath and Kings Heath, attending King writer E M Forster. Edward’s Boys School where his academic On his return from India in 1948, just in time talents won him a scholarship to Birmingham for the birth of the NHS, David was appointed Medical School when he was seventeen. After as chest consultant at his beloved Queen Eliza- further awards and prizes, he qualified as a beth Hospital and was introduced into the lives doctor in 1938. His first post was at the Queen of his two year old daughters, who did not Elizabeth Hospital in Birmingham, starting as know the strange man suddenly living in their a house physician, becoming the Resident home. After the birth of two further daugh- Medical Officer in 1939 and running the ters, Philippa and Nicola, family and working pneumothorax clinic. With the outbreak of life left little time for botany, but it was always World War II he took on the admission of air there on the sidelines. When Philippa was raid casualties as well as teaching students and asked to take wild flowers to school there was night-time fire-watching duties on the roof of a rather high standard, as David vied with the hospital.