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Management Plan 2014 - 2019
Management Plan 2014 - 2019 Part One STRATEGY Introduction 1 AONB Designation 3 Setting the Plan in Context 7 An Ecosystem Approach 13 What makes the Clwydian Range and Dee Valley Special 19 A Vision for the Clwydian Range and Dee Valley AONB 25 Landscape Quality & Character 27 Habitats and Wildlife 31 The Historic Environment 39 Access, Recreation and Tourism 49 Culture and People 55 Introduction The Clwydian Range and Dee lies the glorious Dee Valley Valley Area of Outstanding with historic Llangollen, a Natural Beauty is the dramatic famous market town rich in upland frontier to North cultural and industrial heritage, Wales embracing some of the including the Pontcysyllte country’s most wonderful Aqueduct and Llangollen Canal, countryside. a designated World Heritage Site. The Clwydian Range is an unmistakeable chain of 7KH2DȇV'\NH1DWLRQDO heather clad summits topped Trail traverses this specially by Britain’s most strikingly protected area, one of the least situated hillforts. Beyond the discovered yet most welcoming windswept Horseshoe Pass, and easiest to explore of over Llantysilio Mountain, %ULWDLQȇVȴQHVWODQGVFDSHV About this Plan In 2011 the Clwydian Range AONB and Dee Valley and has been $21%WRZRUNWRJHWKHUWRDFKLHYH was exteneded to include the Dee prepared by the AONB Unit in its aspirations. It will ensure Valley and part of the Vales of close collaboration with key that AONB purposes are being Llangollen. An interim statement partners and stake holders GHOLYHUHGZKLOVWFRQWULEXWLQJWR for this Southern extension including landowners and WKHDLPVDQGREMHFWLYHVRIRWKHU to the AONB was produced custodians of key features. This strategies for the area. in 2012 as an addendum to LVDȴYH\HDUSODQIRUWKHHQWLUH the 2009 Management Plan community of the AONB not just 7KLV0DQDJHPHQW3ODQLVGLHUHQW for the Clwydian Range. -
Aerial Archaeology Research Group - Conference 1996
AERIAL ARCHAEOLOGY RESEARCH GROUP - CONFERENCE 1996 PROGRAMM.E Wednesday 18 September 10.00 Registration 12.30 AGM 13.00 Lunch 114.00 Welcome and Introduction to Conference - Jo EIsworthIM Brown Aerial Archaeology in the Chester Area t'14.10 Archaeology in Cheshire and Merseyside: the view from the ground Adrian Tindall /14.35 The impact of aerial reconnaissance on the archaeology of Cheshire and Merseyside - Rob Philpot . {/15.05 Aerial reconnaissance in Shropshire; Recent results and changing perceptions Mike Watson 15.35 ·~ 5The Isle of Man: recent reconnaissance - Bob Bewley 15.55 Tea News and Views V16.l0 The MARS project - Andrew Fulton 16.4(}1~Introduction to GIS demonstrations 10/17.15 North Oxfordshire: recent results in reconnaissance - Roger Featherstone 17.30 Recent work in Norfolk - Derek Edwards 19.30 Conference Dinner 21 .30 The aerial photography training course, Hungary, June 1996 - Otto Braasch Historical Japan from the air - Martin Gojda Some problems from the Isle ofWight - David Motkin News and Views from Wales - Chris Musson Parchmarks in Essex - David Strachan Thursday 19 September International Session 9.00 From Arcane to Iconic - experience of publishing and exhibiting aerial photographs in New Zealand - Kevin Jones 9.40 The combined method of aerial reconnaissance and sutface collection - Martin Gojda "c j\ 10.00. Recent aerial reconnaissance in Po1and ·"Bf1uL,fi~./ 10.10'1 CtThirsty Apulia' 1994 - BaITi Jones 10.35 The RAPHAEL Programme of the European Union and AARG - Otto Braasch 10.45 Coffee 11.00 TechnicaJ -
A Short Guide to Castell Dinas Bran
11/12/2018 Clwyd-Powys Archaeological Trust - Education - Guides - Dinas Bran Cymraeg / English A short guide to Castell Dinas Bran by the Clwyd Powys Archaeological Trust Castell Dinas Bran (OS national grid reference SJ222430) is both a hillfort and medieval castle. The Iron Age defences and medieval castle are located high above the valley of the Dee overlooking Llangollen. The castle is sited on a long rectangular platform which may have been artificially levelled. The ground drops away steeply on all sides but particularly to the north with its crags and cliffs. The site is a scheduled ancient monument. The hillfort has a single bank and ditch enclosing an area of about 1.5 hectares. To the south and west the defences are most considerable being up to 8 metres high in places. The entrance lies in the south-west corner of the fort and is defended by an inward curving bank. To the north the fort is defended by the natural steepness of the land and no earthwork defences were required. The castle was built towards the later part of the 13th century by the princes of Powys Fadog and was the site of a meeting between the sons of Gryffydd Maelor in 1270 when they granted the lands of Maelor Saesneg for the upkeep of their mother, Emma Audley. During the wars between Llywelyn ap Gruffydd, Prince of Wales and Edward I of England the castle was burnt by the Welsh before it was captured in 1277 by Henry de Lacy, earl of Lincoln. It was not repaired and ceased to be used after the 1280s. -
Table of Contents. Letter of Transmittal. Officers 1910
TWELFTH REPORT OFFICERS 1910-1911. OF President, F. G. NOVY, Ann Arbor. THE MICHIGAN ACADEMY OF SCIENCE Secretary-Treasurer, GEO. D. SHAFER, East Lansing. Librarian, A. G. RUTHVEN, Ann Arbor. CONTAINING AN ACCOUNT OF THE ANNUAL MEETING VICE-PRESIDENTS. HELD AT Agriculture, CHARLES E. MARSHALL, East Lansing. Geography and Geology, W. H. SHERZER, Ypsilanti. ANN ARBOR, MARCH 31, APRIL 1 AND 2, 1910. Zoology, A. S. PEARSE, Ann Arbor. Botany, C. H. KAUFFMAN, Ann Arbor. PREPARED UNDER THE DIRECTION OF THE Sanitary and Medical Science, GUY KIEFER, Detroit. COUNCIL Economics, H. S. SMALLEY, Ann Arbor. BY PAST-PRESIDENTS. GEO. D. SHAFER DR. W. J. BEAL, East Lansing. Professor W. H. SHERZER, Ypsilanti. BRYANT WALKER, ESQ. Detroit. BY AUTHORITY Professor V. M. SPALDING, Tucson, Arizona. LANSING, MICHIGAN DR. HENRY B. BAKER, Holland. WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Professor JACOB REIGHARD, Ann Arbor. 1910 Professor CHARLES E. BARR, Albion. Professor V. C. VAUGHAN, Ann Arbor. Professor F. C. NEWCOMBE, Ann Arbor. TABLE OF CONTENTS. DR. A. C. LANE, Tuft's College, Mass. Professor W. B. BARROWS, East Lansing. DR. J. B. POLLOCK, Ann Arbor. Letter of Transmittal .......................................................... 1 Professor M. H. W. JEFFERSON, Ypsilanti. DR. CHARLES E. MARSHALL, East Lansing. Officers for 1910-1911. ..................................................... 1 Professor FRANK LEVERETT, Ann Arbor. Life of William Smith Sayer. .............................................. 1 COUNCIL. Life of Charles Fay Wheeler.............................................. 2 The Council is composed of the above named officers Papers published in this report: and all Resident Past-Presidents. President's Address—Outline of the History of the Great Lakes, Frank Leverett.......................................... 3 On the Glacial Origin of the Huronian Rocks of WILLIAM SMITH SAYER. -
Opening Article Is an Edition of Her Journals 1923-48 (1973)
The Powys Review NUMBER EIGHT Angus Wilson SETTING THE WORLD ON FIRE "A very distinguished novel ... It is superb entertain- ment and social criticism but it is also a poem about the life of human beings - a moving and disturbing book and a very superior piece of art.'' Anthony Burgess, Observer "Wonderfully intricate and haunting new novel. The complex relationships between art and reality . are explored with a mixture of elegance, panache and concern that is peculiarly his ... magnificent." Margaret Drabble, Listener "As much for the truth and pathos of its central relation- ships as for the brilliance of the grotesques who sur- round them, I found Setting the World on Fire the most successful Wilson novel since Late Call. I enjoyed it very much indeed.'' Michael Ratcliffe, The Times "A novel which will give much pleasure and which exemplifies the civilised standards it aims to defend." Thomas Hinde, Sunday Telegraph "A book which I admire very much . this is an immensely civilised novel, life enhancing, with wonder- fully satirical moments.'' David Holloway, Daily Telegraph "... an exceptionally rich work . the book is witty, complex and frightening, as well as beautifully written.'' Isobel Murray, Financial Times Cover: Mary Cowper Powys with (1. to r.) Llewelyn, Marian and Philippa, c. 1886. The Powys Review Editor Belinda Humfrey Reviews Editor Peter Miles Advisory Board Glen Cavaliero Ben Jones Derrick Stephens Correspondence, contributions, and books for review may be addressed to the Editor, Department of English, Saint David's University College, Lampeter, Dyfed, SA48 7ED Copyright ©, The Editor The Powys Review is published with the financial support of the Welsh Arts Council. -
Medieval, Bibliography 22/12/2003
A Research Framework for the Archaeology of Wales Select Bibliography, Northeast Wales Medieval A Research Framework for the Archaeology of Wales East and Northeast Wales – Medieval, bibliography 22/12/2003 Adams. B. 1999. 'The Latin Epitaphs in Brecon Cathedral’. Brycheiniog 31. 31-42. Adams. M. 1988. Abbeycwmhir: a survey of the ruins. CPAT report 1. August 1988. Alban. J & Thomas. W S K. 1993. 'The charters of the borough of Brecon 1276- 1517’. Brycheiniog 25. 31-56. Alcock. L. 1961. 'Beili Bedw Farm. St Harmon’. Archaeology in Wales 1. 14-15. Alcock. L. 1962. 'St Harmon’. Archaeology in Wales 2. 18. Allcroft. A H. 1908. Earthwork of England. London. Anon. 1849. 'Account of Cwmhir Abbey. Radnorshire’. Archaeologia Cambrensis 4. 229-30. Anon. 1863. ‘Brut y Saeson (translation)’. Archaeologia Cambrensis 9. 59-67. Anon. 1884. ‘Inscription on a grave-stone in Llanwddyn churchyard’. Archaeologia Cambrensis 1. 245. Anon. 1884. 'Llanfechain. Montgomeryshire’. Archaeologia Cambrensis 1. 146. Anon. 1884. 'Nerquis. Flintshire’. Archaeologia Cambrensis 1. 247. Anon. 1884. ‘Oswestry. Ancient and Modern. and its Local Families’. Archaeologia Cambrensis 1. 193-224. Anon. 1884. 'Report of Meeting’. Archaeologia Cambrensis 1. 324-351. Anon. 1884. 'Restoration of Llanynys Church’. Archaeologia Cambrensis 1. 318. Anon. 1884. ‘Restoration of Meliden Church’. Archaeologia Cambrensis 1. 317-8. Anon. 1885. 'Review - Old Stone Crosses of the Vale of Clwyd and Neighbouring Parishes’. Archaeologia Cambrensis 6. 158-160. Anon. 1887. 'Report of the Denbigh meeting of the Cambrian Archaeological Association’. Archaeologia Cambrensis 4. 339. Anon. 1887. 'The Carmelite Priory. Denbigh’. Archaeologia Cambrensis 16. 260- 273. Anon. 1891. ‘Report of the Holywell Meeting’. -
A Short History of the Dudley & Midland
A Short History of the Dudley & Midland Geological Societies A Cutler Summary The history and development of the Dudley Geological Societies is traced with the aid of published transactions and other manuscript material. Both Societies established geological museums in Dudley, the surviving collections of which are now in the care of the Local Authority. Introduction It is not common knowledge that a geological society existed in the Black Country during the nineteenth century and probably even less so that there were two societies at different periods, which shared similar titles. That these societies existed at all should come as no surprise. The nineteenth century was a period of great scientific advancement and popular interest in all sciences was high. The period too was one of great industrial activity particularly in the Black Country and geological problems of a very practical nature relating to mining served to make the societies ideal forums for all interested parties. They were both typical nineteenth century scientific societies and possessed many essentially amateur members. But their contribution to Black Country geology was certainly not amateur and has proved to be of lasting value. The Original Society The original or first society (even referred to as the parent society in later references) was formed in 1841 and quickly attracted a most impressive total of 150 subscribing members. Lord Ward accepted the office of President and some thirty local industrialists, geologists and Members of Parliament became Vice- Presidents. The list of patrons included no less than thirteen peers of the realm, three Lord Bishops and Sir Robert Peel who is perhaps more well known for his association with the first constabularies. -
Open Kosei.Pdf
The Pennsylvania State University The Graduate School Department of Geosciences GEOCHEMISTRY OF ARCHEAN–PALEOPROTEROZOIC BLACK SHALES: THE EARLY EVOLUTION OF THE ATMOSPHERE, OCEANS, AND BIOSPHERE A Thesis in Geosciences by Kosei Yamaguchi Copyright 2002 Kosei Yamaguchi Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2002 We approve the thesis of Kosei Yamaguchi Date of Signature ____________________________________ _______________________ Hiroshi Ohmoto Professor of Geochemistry Thesis Advisor Chair of Committee ____________________________________ _______________________ Michael A. Arthur Professor of Geosciences ____________________________________ _______________________ Lee R. Kump Professor of Geosciences ____________________________________ _______________________ Raymond G. Najjar Associate Professor of Meteorology ____________________________________ _______________________ Peter Deines Professor of Geochemistry Associate Head for Graduate Program and Research in Geosciences iii ABSTRACT When did the Earth's surface environment become oxic? The timing and mechanism of the rise of atmospheric pO2 level in the early Precambrian have been long debated but no consensus has been reached. The oxygenation of the atmosphere and oceans has significant impacts on the evolution of the biosphere and the geochemical cycles of redox-sensitive elements. In order to constrain the evolution of the atmosphere, oceans, biosphere, and geochemical cycles of elements, a systematic and multidisciplinary -
Chemical Weathering in Highsedimentyielding Watersheds
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, F01008, doi:10.1029/2003JF000088, 2005 Chemical weathering in high-sediment-yielding watersheds, New Zealand W. Berry Lyons and Anne E. Carey Department of Geological Sciences and Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA D. Murray Hicks NIWA Research, Christchurch, New Zealand Carmen A. Nezat1 Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA Received 3 September 2003; revised 14 September 2004; accepted 30 November 2004; published 15 February 2005. [1] We have determined the chemical erosion yields for fifteen watersheds in New Zealand, ranging in size from 12.2 to 2928 km2. These rates, coupled with previously measured physical erosion yields, allow us to compare these two modes of landscape denudation. The physical erosion yields are some of the highest measured in the world. Although in most instances the chemical erosion yields are only a small fraction of the total erosion yields, the absolute values are very high. Our data strongly support the notion that chemical erosion rates are greatly influenced by the yield of physical erosion and that the rapid production of fresh surfaces as a result of high physical erosion rates and subsequent denudation is critical to the high chemical erosion yields observed. Citation: Lyons, W. B., A. E. Carey, D. M. Hicks, and C. A. Nezat (2005), Chemical weathering in high-sediment-yielding watersheds, New Zealand, J. Geophys. Res., 110, F01008, doi:10.1029/2003JF000088. 1. Introduction Vance et al., 2003]. In general, the net, large-scale erosional potential of a landscape is thought to increase with precip- [2] Over the past decade, a debate has occurred regard- itation, drainage area and slope [Montgomery et al., 2001]. -
Other Wildlife Sites in Denbighshire
Welcome Making sense of the jargon Some sites have local, national or international designations. This means that the sites have to be managed and preserved in a special way to safeguard the animals, habitats, archaeology or landscapes that are rare or in danger. LNR - Local Nature Reserve SSSI - Site of Special Scientific Interest SAC - Special Area of Conservation AONB - Area of Outstanding Natural Beauty SAM - Scheduled Ancient Monument WS - County Wildlife Sites These symbols show what facilities are available on the sites: This leaflet is designed to show you the Café or restaurant nearby room for hire managed countryside sites in the area, how shop events to get to them, what you can do when you picnic tables hang/para gliding get there and why they are such valuable toilets & model flying places to visit and protect. The centre map disabled facilities historic remains shows the location of the sites; please refer to (parking, toilets, view) the map reference to help you to your leaflet cycling route destination. Information panels bridlepath ()limited coach parking parking on site 1 We hope you enjoy exploring these beautiful public bus route parking within /2 mile countryside sites. schools resources views Sites are graded according to how accessible the main paths are, please look for these symbols: Whilst every effort has been made to make this booklet as 1 accurate as possible, - Most paths are flat with hard surface. neither authors nor 2 publishers accept any - Some gradients and hard surfaces. responsibility for the 3 consequence of any - Gradients with surfaces of loose stones and grass. -
Sedimentology, Petrography, and Depositional Environment of Dore
SEDIMENTOLOGY, PETROGRAPHY, AND DEPOSITIONAL ENVIRONMENT OF DORE SEDIMENTS ABOVE THE HELEN-ELEANOR IRON RANGE, WAHA, ONTARIO ' SEDIMENTOLOGY, PETROGRAPHY, AND DEPOSITIONAL ENVIRONMENT OF DORE SEDIMENTS AHOVE THE HELEN-ELEANOR IRON RANGE, WAWA, ONTARIO By KATHRYN L. NEALE Submitted to the Department of Geology in Partial Fulfilment of the Requirements for the Degree Bachelor of Science McMaster University April, 1981 BACHELOR OF SCIENCE (1981) McMASTER UNIVERSITY (Geology) Hamilton, Ontario TITLE: Sedimentology, Petrography, and Depositional Environment of Dore Sediments above the Helen Eleanor Iron Range, Wawa, Ontario AUTHOR: Kathryn L. Neale SUPERVISOR: Dr. R. G. Walker NUMBER OF PAGES: ix, 54 ii ABSTRACT Archean sediments of the Dare group, located in the 1-Jawa green stone belt, were studied. The sediments are stratigraphically above the carbonate facies Helen-Eleanor secti on of the Michipicoten Iron Forma tion. A mafic volcanic unit, 90 m thick, lies between the iron range and the sediments. Four main facies have been i dentified in the first cycle of clastic sedimentation above the maf i c flow rocks. A 170 ro break in stratigraphy separates the volcanics from the first facies. The basal sedimentary facies is an unstratified and poorly sorted granule-cobble conglomerate, 200m thick, interpreted as an alluvial mass flow deposit. Above the conglomerate, there is a 20 m break in the stratigraphic column. The second facies, 220m to 415 m thick, consists of laminated (0.1- 2 em) argillites and siltstones, together with massive, thick bedded (8-10 m) greywackes. The argillites and siltstones are interpre ted as interchannel deposits on an upper submarine fan, and the grey wackes are explained as in-channel turbidity current deposition. -
And How the Gold Got There
BLUE LAKE and how the gold got there Geology Department Geology by Dave Craw Presentation by Anna Craw Blue Lake, at the foot of Mt St Bathans in Central Otago, is one of several important historical gold mines in the area. Mt St Bathans is made up of 200 million year old greywacke and that continues deep under the Blue Lake area. It is unusual to find gold associated with greywacke, and it was a long and complicated geological journey that ended with the large concentrations of gold where St Bathans town now stands. 20 million years ago Gold in quartz Gold typically occurs in quartz vein veins in schist (see diagram above). Schist bedrock and gold-bearing veins occur tens of kilometres to the southwest of the St Bathans area. Greywacke was faulted against schist about 100 million years ago. About 20 million years ago, erosion of schist hills produced river sediments rich in quartz pebbles. The quartz Schist Greywacke Quartz pebbles result when the white gravel quartz layers in schist break up and become rounded during river transport. Some of the quartz came from gold-bearing veins, and the gold was transported at the same time. The quartz pebbles and gold were transported northeast and deposited on greywacke bedrock. Some greywacke pebbles entered this river, but they are not resistent to abrasion like quartz and most of them ground away. 1 10 million years ago Lake Manuherikia Greywacke Schist Gold-bearing quartz veins Lake mudstone with fossil leaves and twigs Quartz gravel river deposits Ten million years ago, the quartz river sediments were buried by a large shallow lake, Lake Manuherikia, which covered most of Central Otago.