OUGS Journal 30 (1) 2009
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PEMBROKESHIRE © Lonelyplanetpublications Biggest Megalithicmonumentinwales
© Lonely Planet Publications 162 lonelyplanet.com PEMBROKESHIRE COAST NATIONAL PARK •• Information 163 porpoises and whales are frequently spotted PEMBROKESHIRE COAST in coastal waters. Pembrokeshire The park is also a focus for activities, from NATIONAL PARK hiking and bird-watching to high-adrenaline sports such as surfing, coasteering, sea kayak- The Pembrokeshire Coast National Park (Parc ing and rock climbing. Cenedlaethol Arfordir Sir Benfro), established in 1952, takes in almost the entire coast of INFORMATION Like a little corner of California transplanted to Wales, Pembrokeshire is where the west Pembrokeshire and its offshore islands, as There are three national park visitor centres – meets the sea in a welter of surf and golden sand, a scenic extravaganza of spectacular sea well as the moorland hills of Mynydd Preseli in Tenby, St David’s and Newport – and a cliffs, seal-haunted islands and beautiful beaches. in the north. Its many attractions include a dozen tourist offices scattered across Pembro- scenic coastline of rugged cliffs with fantas- keshire. Pick up a copy of Coast to Coast (on- Among the top-three sunniest places in the UK, this wave-lashed western promontory is tically folded rock formations interspersed line at www.visitpembrokeshirecoast.com), one of the most popular holiday destinations in the country. Traditional bucket-and-spade with some of the best beaches in Wales, and the park’s free annual newspaper, which has seaside resorts like Tenby and Broad Haven alternate with picturesque harbour villages a profusion of wildlife – Pembrokeshire’s lots of information on park attractions, a cal- sea cliffs and islands support huge breeding endar of events and details of park-organised such as Solva and Porthgain, interspersed with long stretches of remote, roadless coastline populations of sea birds, while seals, dolphins, activities, including guided walks, themed frequented only by walkers and wildlife. -
Welsh Bulletin
BOTANICAL SOCIETY OF THE BRITISH ISLES WELSH BULLETIN Editor: R. D. Pryce No. 64, WINTER 1998 Photocopy of specimens of Asplenium trichomanes subsp. pachyrachis al NMW. enlarged (xl.S) 10 show Ihe often haslate pinnae of Ihis subspecies. It is new 10 Brecs. (v.c.42); see Welsh Plant Records. 2 Contents . -.--~----- ------CO-N-TE-NT-S----~-·~~- Editorial ...................................................................................................................... 3 Progress with Atlas 2000 - the Welsh perspective Atlas 2000: Progress in v.c. 35 as November 1998 .................................................. .4 Atlas 2000: Recording in Glamorgan ........................................................................ .4 Atlas 2000: Breconshire (v.c. 42) .............................................................................. 5 Atlas 2000: 1998 recording in v.c. 43 .........................................................................6 Atlas 2000: Carmarthenshire - report on recording progress 1996 to 1998 .............. 7 Atlas 2000: Botanical recording in Pembrokeshire since 1995 .................................. 8 Atlas 2000: v.c. 46, Cardoganshire .......................................................................... 10 Atlas 2000: v.c. 47, Montgomeryshire ...................................................................... 10 Atlas 2000: Recording in Caernarfonshire (v.c. 49) ................................................. 11 Atlas 2000: v.c. 50, Denbighshire ........................................................................... -
Morloi Ble I Fynd, Beth I'w Wybod
Morlo bychan Seliwch gwylio yn llawer o hwyl, ond cadwch dawel felly rydym peidiwch â'u tarfu Morloi ble i fynd, beth i'w wybod Côd Ymddygiad Caiff Morloi eu hamddiffyn gan y gyfraith. Rydym yn ffodus i gael Morlo ifanc rhannu’r ardal arbennig yma â nhw. O’r tir: • Mae’n well gwylio’r morloi oddi ar lwybr yr arfordir – mae’n ddefnyddiol bod â sbienddrych gyda chi. Cymerwch ofal ar y clogwyni ac yn cadw proffil isel. • Cadwch draw o’r traethau ble fo morloi bychain • Gall cwˆn darfu’n fawr iawn ar y morloi • Cadwch mor dawel â phosibl • Cadwch draw os y sylwch ar arwyddion bod y morloi’n aflonyddu O’r dwˆr: • Dylech osgoi glanio ar draethau geni’r morloi bychain neu ar draethau ble fo morloi’n ymlacio • Dylech osgoi dod rhwng mam a’i un bach • Cadwch gyflymder eich cwch yn araf wrth gyrraedd a gadael y lan, a chofiwch sicrhau mai dim ond un cwch sy’n gwylio’r morloi ar y Oedolyn benyw tro • Cadwch o leiaf 20 metr i ffwrdd, ond yn ddelfrydol cadwch 50 metr i ffwrdd • Symudwch draw os y sylwch ar unrhyw arwyddion bod y morloi’n aflonyddu • Peidiwch â cheisio nofio gyda’r morloi na’u cyffwrdd na’u bwydo Nodiadau • Os oes morlo bychan ar ei ben ei hun ar draeth, fel arfer mae’n golygu bod ei fam yn y dwˆr gerllaw. Gwnewch yn siwˆr eich bod yn cadw’n ddigon pell i ffwrdd fel y gall ddod yn ôl at yr un bach pan fydd angen. -
During Neoproterozoic Glaciations with Evolutionary Implications
Geosciences 2012, 2, 90-108; doi:10.3390/geosciences2020090 OPEN ACCESS geosciences ISSN 2076-3263 www.mdpi.com/journal/geosciences Review The Location and Styles of Ice-Free “Oases” during Neoproterozoic Glaciations with Evolutionary Implications Daniel Paul Le Heron Department of Earth Sciences, Royal Holloway University of London, Queen’s Building, Egham TW200EX, UK; E-Mail: [email protected]; Tel.: +0044-1784-443615; Fax: +0044-1784-471780 Received: 13 March 2012; in revised form: 10 April 2012 / Accepted: 17 May 2012 / Published: 29 May 2012 Abstract: Evidence based on molecular clocks, together with molecular evidence/biomarkers and putative body fossils, points to major evolutionary events prior to and during the intense Cryogenian and Ediacaran glaciations. The glaciations themselves were of global extent. Sedimentological evidence, including hummocky cross-stratification (representing ice-free seas affected by intra-glacial storms), dropstone textures, microbial mat-bearing ironstones, ladderback ripples, and wave ripples, militates against a “hard” Snowball Earth event. Each piece of sedimentological evidence potentially allows insight into the shape and location, with respect to the shoreline, of ice-free areas (“oases”) that may be viewed as potential refugia. The location of such oases must be seen in the context of global paleogeography, and it is emphasized that continental reconstructions at 600 Ma (about 35 millions years after the “Marinoan” ice age) are non-unique solutions. Specifically, whether continents such as greater India, Australia/East Antarctica, Kalahari, South and North China, and Siberia, were welded to a southern supercontinent or not, has implications for island speciation, faunal exchange, and the development of endemism. -
Neoproterozoic Glaciations in a Revised Global Palaeogeography from the Breakup of Rodinia to the Assembly of Gondwanaland
Sedimentary Geology 294 (2013) 219–232 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Invited review Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland Zheng-Xiang Li a,b,⁎, David A.D. Evans b, Galen P. Halverson c,d a ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia b Department of Geology and Geophysics, Yale University, New Haven, CT 06520-8109, USA c Earth & Planetary Sciences/GEOTOP, McGill University, 3450 University St., Montreal, Quebec H3A0E8, Canada d Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia article info abstract Article history: This review paper presents a set of revised global palaeogeographic maps for the 825–540 Ma interval using Received 6 January 2013 the latest palaeomagnetic data, along with lithological information for Neoproterozoic sedimentary basins. Received in revised form 24 May 2013 These maps form the basis for an examination of the relationships between known glacial deposits, Accepted 28 May 2013 palaeolatitude, positions of continental rifting, relative sea-level changes, and major global tectonic events Available online 5 June 2013 such as supercontinent assembly, breakup and superplume events. This analysis reveals several fundamental ’ Editor: J. Knight palaeogeographic features that will help inform and constrain models for Earth s climatic and geodynamic evolution during the Neoproterozoic. First, glacial deposits at or near sea level appear to extend from high Keywords: latitudes into the deep tropics for all three Neoproterozoic ice ages (Sturtian, Marinoan and Gaskiers), al- Neoproterozoic though the Gaskiers interval remains very poorly constrained in both palaeomagnetic data and global Rodinia lithostratigraphic correlations. -
Southern Snowdon Horseshoe
ROUTE 3 JUNE 2017 Snowdonia 14.6km/8¾ miles 7-8 hours Strenuousness lllll Navigation lllll Technicality lllll TrailROUTE 100s STATS2 Welsh 3000s 1 Looking to Crib Goch from Y Lliwedd. Southern Snowdon Horseshoe WORTHINGTON KATE Check out Wales’ main attraction using some Descending Bwlch Main. quieter ascents and descents to enjoy Yr Wyddfa’s fine ridges and peaks, says Kate Worthington. his is a very fine outing indeed, height towards Snowdon’s summit on and hitting Wales’ highest peak the steep, upper section of the Watkin TSnowdon (Yr Wyddfa) is the cherry Path. Regardless of your relationship on the top. On your way, take in the glory with the summit cairn on Snowdon, it’s of finding a quiet way onto the majestic a breathtaking vista on a clear day – to peaks of Y Lliwedd and work hard to gain the Glyderau in the north, Moel Hebog and the Nantlle range to the south-west and the Moelwynion to the south-east. And whisk yourself away along the mountain’s attractive Bwlch Main and southern ridge, towards your final triumph, Yr Aran. This beautifully shaped peak stands guard over Snowdon’s southern hemisphere, protecting the beguiling Cwm Llan below a great route for a dry, calm, long from the worst of weather coming in summer’s day. And why not try an ‘alpine from the coast. This final peak is a fitting start’ to get ahead of others heading to finale to a robust route over rocky ground Snowdon’s summit from other directions? Heading to waterfalls. and slender, enticing rocky ridges. -
Integrated Upper Ordovician Graptolite–Chitinozoan Biostratigraphy of the Cardigan and Whitland Areas, Southwest Wales
Geol. Mag. 145 (2), 2008, pp. 199–214. c 2007 Cambridge University Press 199 doi:10.1017/S0016756807004232 First published online 17 December 2007 Printed in the United Kingdom Integrated Upper Ordovician graptolite–chitinozoan biostratigraphy of the Cardigan and Whitland areas, southwest Wales THIJS R. A. VANDENBROUCKE∗†, MARK WILLIAMS‡, JAN A. ZALASIEWICZ‡, JEREMY R. DAVIES§ & RICHARD A. WATERS¶ ∗Research Unit Palaeontology, Ghent University, Krijgslaan 281/S8, 9000 Ghent, Belgium ‡Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK §British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK ¶Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, UK (Received 26 January 2007; accepted 26 June 2007) Abstract – To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonation in the Anglo-Welsh, historical type basin, the graptolite-bearing Caradoc– Ashgill successions between Fishguard and Cardigan, and at Whitland, SW Wales, have been collected for chitinozoans. In the Cardigan district, finds of Armoricochitina reticulifera within strata referred to the clingani graptolite Biozone (morrisi Subzone), together with accessory species, indicate the Fungochitina spinifera chitinozoan Biozone, known from several Ordovician sections in northern England that span the base of the Ashgill Series. Tanuchitina ?bergstroemi, eponymous of the succeeding chitinozoan biozone, has tentatively been recovered from strata of Pleurograptus linearis graptolite Biozone age in the Cardigan area. The T. ?bergstroemi Biozone can also be correlated with the type Ashgill Series of northern England. Chitinozoans suggest that the widespread Welsh Basin anoxic–oxic transition at the base of the Nantmel Mudstones Formation in Wales, traditionally equated with the Caradoc–Ashgill boundary, is of Cautleyan (or younger Ashgill) age in the Cardigan area. -
Dyfed Final Recommendations News Release
NEWS RELEASE Issued by the Telephone 02920 395031 Boundary Commission for Wales Caradog House Fax 02920 395250 1-6 St Andrews Place Cardiff CF10 3BE Date 25 August 2004 FINAL RECOMMENDATIONS FOR THE PARLIAMENTARY CONSTITUENCIES IN THE PRESERVED COUNTY OF DYFED The Commission propose to make no change to their provisional recommendations for five constituencies in the preserved county of Dyfed. 1. Provisional recommendations in respect of Dyfed were published on 5 January 2004. The Commission received eleven representations, five of which were in support of their provisional recommendations. Three of the representations objected to the inclusion of the whole of the Cynwyl Elfed electoral division within the Carmarthen West and South Pembrokeshire constituency, one objected to the name of the Carmarthen West and South Pembrokeshire constituency and one suggested the existing arrangements for the area be retained. 2. The Commission noted that, having received no representation of the kind mentioned in section 6 (2) of the Parliamentary Constituencies Act 1986, there was no statutory requirement to hold a local inquiry. The Commission further decided that in all the circumstances they would not exercise their discretion under section 6 (1) to hold an inquiry. Final recommendations 3. The main objection to the provisional recommendations was in respect of the inclusion of the Cynwyl Elfed electoral division in the Carmarthen West and South Pembrokeshire constituency. It was argued that the division should be included in Carmarthen East and Dinefwr on the grounds that the majority of the electorate in the division fell within that constituency and that inclusion in Carmarthen East and Dinefwr rather than Carmarthen West and South Pembrokeshire would reduce the disparity between the electorates of the two constituencies and would bring them closer to the electoral quota. -
The Snowdon Horseshoe
Contextualised task 34 The Snowdon Horseshoe Teaching Notes This task is based on the mathematics involved in creating a route card for a journey in the mountains. In particular students will investigate methods of estimating timings. This will involve using worded formulae and, ultimately, trigonometry. While not essential, the whole task could be completed using a spreadsheet. If this approach is to be used, all the data is provided in an accompanying file. Task A: Naismith’s Rule Outline Students are presented with information about the route known as the Snowdon Horseshoe. They use Naismith’s Rule to calculate an estimate of the time taken on sections of the route. They have the option of creating a route profile. You will need: Teachers’ script PowerPoint Question sheet Spreadsheet (optional) Mark scheme Task B: Langmuir’s Refinements Outline Students consider a refinement to Naismith’s Rule which provides an improved model for estimating timings. They calculate angles of elevation that are needed to enable ‘Langmuir’s Refinement’ to be used. You will need: Question sheet Spreadsheet (optional) Mark scheme Task A: Teachers’ script for PowerPoint presentation The text in the right-hand boxes provides a possible script to be read to students. However, it is probably preferable to use your own words and elaboration. When questions are asked, time for discussion in pairs / groups should be provided. Ensure that students are given opportunity to explain their reasoning in response to these questions. All students need to understand the concepts in order to make progress with the task. Slide Keep this slide on the screen until you are ready 1 to start the presentation The Snowdon Horseshoe Slide Has anyone ever climbed Snowdon? Do they 2 know which way they climbed it? There are a number of different ways to reach the top of Snowdon – the highest point in Wales. -
The Pembrokeshire (Communities) Order 2011
Status: This is the original version (as it was originally made). This item of legislation is currently only available in its original format. WELSH STATUTORY INSTRUMENTS 2011 No. 683 (W.101) LOCAL GOVERNMENT, WALES The Pembrokeshire (Communities) Order 2011 Made - - - - 7 March 2011 Coming into force in accordance with article 1(2) and (3) The Local Government Boundary Commission for Wales has, in accordance with sections 54(1) and 58(1) of the Local GovernmentAct 1972(1), submitted to the Welsh Ministers a report dated April 2010 on its review of, and proposals for, communities within the County of Pembrokeshire. The Welsh Ministers have decided to give effect to those proposals with modifications. More than six weeks have elapsed since those proposals were submitted to the Welsh Ministers. The Welsh Ministers make the following Order in exercise of the powers conferred on the Secretary of State by sections 58(2) and 67(5) of the Local Government Act 1972 and now vested in them(2). Title and commencement 1.—(1) The title of this Order is The Pembrokeshire (Communities) Order 2011. (2) Articles 4, 5 and 6 of this Order come into force— (a) for the purpose of proceedings preliminary or relating to the election of councillors, on 15 October 2011; (b) for all other purposes, on the ordinary day of election of councillors in 2012. (3) For all other purposes, this Order comes into force on 1 April 2011, which is the appointed day for the purposes of the Regulations. Interpretation 2. In this Order— “existing” (“presennol”), in relation to a local government or electoral area, means that area as it exists immediately before the appointed day; “Map A” (“Map A”), “Map B” (“Map B”), “Map C” (“Map C”), “Map D” (“Map D”), “Map E” (“Map E”), “Map F” (“Map F”), “Map G” (“Map G”), “Map H” (“Map H”), “Map I” (“Map (1) 1972 c. -
Wales: River Wye to the Great Orme, Including Anglesey
A MACRO REVIEW OF THE COASTLINE OF ENGLAND AND WALES Volume 7. Wales. River Wye to the Great Orme, including Anglesey J Welsby and J M Motyka Report SR 206 April 1989 Registered Office: Hydraulics Research Limited, Wallingford, Oxfordshire OX1 0 8BA. Telephone: 0491 35381. Telex: 848552 ABSTRACT This report reviews the coastline of south, west and northwest Wales. In it is a description of natural and man made processes which affect the behaviour of this part of the United Kingdom. It includes a summary of the coastal defences, areas of significant change and a number of aspects of beach development. There is also a brief chapter on winds, waves and tidal action, with extensive references being given in the Bibliography. This is the seventh report of a series being carried out for the Ministry of Agriculture, Fisheries and Food. For further information please contact Mr J M Motyka of the Coastal Processes Section, Maritime Engineering Department, Hydraulics Research Limited. Welsby J and Motyka J M. A Macro review of the coastline of England and Wales. Volume 7. River Wye to the Great Orme, including Anglesey. Hydraulics Research Ltd, Report SR 206, April 1989. CONTENTS Page 1 INTRODUCTION 2 EXECUTIVE SUMMARY 3 COASTAL GEOLOGY AND TOPOGRAPHY 3.1 Geological background 3.2 Coastal processes 4 WINDS, WAVES AND TIDAL CURRENTS 4.1 Wind and wave climate 4.2 Tides and tidal currents 5 REVIEW OF THE COASTAL DEFENCES 5.1 The South coast 5.1.1 The Wye to Lavernock Point 5.1.2 Lavernock Point to Porthcawl 5.1.3 Swansea Bay 5.1.4 Mumbles Head to Worms Head 5.1.5 Carmarthen Bay 5.1.6 St Govan's Head to Milford Haven 5.2 The West coast 5.2.1 Milford Haven to Skomer Island 5.2.2 St Bride's Bay 5.2.3 St David's Head to Aberdyfi 5.2.4 Aberdyfi to Aberdaron 5.2.5 Aberdaron to Menai Bridge 5.3 The Isle of Anglesey and Conwy Bay 5.3.1 The Menai Bridge to Carmel Head 5.3.2 Carmel Head to Puffin Island 5.3.3 Conwy Bay 6 ACKNOWLEDGEMENTS 7 REFERENCES BIBLIOGRAPHY FIGURES 1. -
The Hitch-Hiker Is Intended to Provide Information Which Beginning Adult Readers Can Read and Understand
CONTENTS: Foreword Acknowledgements Chapter 1: The Southwestern Corner Chapter 2: The Great Northern Peninsula Chapter 3: Labrador Chapter 4: Deer Lake to Bishop's Falls Chapter 5: Botwood to Twillingate Chapter 6: Glenwood to Gambo Chapter 7: Glovertown to Bonavista Chapter 8: The South Coast Chapter 9: Goobies to Cape St. Mary's to Whitbourne Chapter 10: Trinity-Conception Chapter 11: St. John's and the Eastern Avalon FOREWORD This book was written to give students a closer look at Newfoundland and Labrador. Learning about our own part of the earth can help us get a better understanding of the world at large. Much of the information now available about our province is aimed at young readers and people with at least a high school education. The Hitch-Hiker is intended to provide information which beginning adult readers can read and understand. This work has a special feature we hope readers will appreciate and enjoy. Many of the places written about in this book are seen through the eyes of an adult learner and other fictional characters. These characters were created to help add a touch of reality to the printed page. We hope the characters and the things they learn and talk about also give the reader a better understanding of our province. Above all, we hope this book challenges your curiosity and encourages you to search for more information about our land. Don McDonald Director of Programs and Services Newfoundland and Labrador Literacy Development Council ACKNOWLEDGMENTS I wish to thank the many people who so kindly and eagerly helped me during the production of this book.