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Conservation of the Wildcat (Felis Silvestris) in Scotland: Review of the Conservation Status and Assessment of Conservation Activities
Conservation of the wildcat (Felis silvestris) in Scotland: Review of the conservation status and assessment of conservation activities Urs Breitenmoser, Tabea Lanz and Christine Breitenmoser-Würsten February 2019 Wildcat in Scotland – Review of Conservation Status and Activities 2 Cover photo: Wildcat (Felis silvestris) male meets domestic cat female, © L. Geslin. In spring 2018, the Scottish Wildcat Conservation Action Plan Steering Group commissioned the IUCN SSC Cat Specialist Group to review the conservation status of the wildcat in Scotland and the implementation of conservation activities so far. The review was done based on the scientific literature and available reports. The designation of the geographical entities in this report, and the representation of the material, do not imply the expression of any opinion whatsoever on the part of the IUCN concerning the legal status of any country, territory, or area, or its authorities, or concerning the delimitation of its frontiers or boundaries. The SWCAP Steering Group contact point is Martin Gaywood ([email protected]). Wildcat in Scotland – Review of Conservation Status and Activities 3 List of Content Abbreviations and Acronyms 4 Summary 5 1. Introduction 7 2. History and present status of the wildcat in Scotland – an overview 2.1. History of the wildcat in Great Britain 8 2.2. Present status of the wildcat in Scotland 10 2.3. Threats 13 2.4. Legal status and listing 16 2.5. Characteristics of the Scottish Wildcat 17 2.6. Phylogenetic and taxonomic characteristics 20 3. Recent conservation initiatives and projects 3.1. Conservation planning and initial projects 24 3.2. Scottish Wildcat Action 28 3.3. -
2020 Cruise Directory Directory 2020 Cruise 2020 Cruise Directory M 18 C B Y 80 −−−−−−−−−−−−−−− 17 −−−−−−−−−−−−−−−
2020 MAIN Cover Artwork.qxp_Layout 1 07/03/2019 16:16 Page 1 2020 Hebridean Princess Cruise Calendar SPRING page CONTENTS March 2nd A Taste of the Lower Clyde 4 nights 22 European River Cruises on board MS Royal Crown 6th Firth of Clyde Explorer 4 nights 24 10th Historic Houses and Castles of the Clyde 7 nights 26 The Hebridean difference 3 Private charters 17 17th Inlets and Islands of Argyll 7 nights 28 24th Highland and Island Discovery 7 nights 30 Genuinely fully-inclusive cruising 4-5 Belmond Royal Scotsman 17 31st Flavours of the Hebrides 7 nights 32 Discovering more with Scottish islands A-Z 18-21 Hebridean’s exceptional crew 6-7 April 7th Easter Explorer 7 nights 34 Cruise itineraries 22-97 Life on board 8-9 14th Springtime Surprise 7 nights 36 Cabins 98-107 21st Idyllic Outer Isles 7 nights 38 Dining and cuisine 10-11 28th Footloose through the Inner Sound 7 nights 40 Smooth start to your cruise 108-109 2020 Cruise DireCTOrY Going ashore 12-13 On board A-Z 111 May 5th Glorious Gardens of the West Coast 7 nights 42 Themed cruises 14 12th Western Isles Panorama 7 nights 44 Highlands and islands of scotland What you need to know 112 Enriching guest speakers 15 19th St Kilda and the Outer Isles 7 nights 46 Orkney, Northern ireland, isle of Man and Norway Cabin facilities 113 26th Western Isles Wildlife 7 nights 48 Knowledgeable guides 15 Deck plans 114 SuMMER Partnerships 16 June 2nd St Kilda & Scotland’s Remote Archipelagos 7 nights 50 9th Heart of the Hebrides 7 nights 52 16th Footloose to the Outer Isles 7 nights 54 HEBRIDEAN -
The Thor Suture Zone: from Subduction to Intraplate Basin Setting
The Thor suture zone: From subduction to intraplate basin setting Jeroen Smit1, Jan-Diederik van Wees1,2, and Sierd Cloetingh1 1Department of Earth Sciences, Faculty of Geosciences, Utrecht University, PO Box 80.021, 3508 TA Utrecht, Netherlands 2TNO Energy, PO Box 80015, 3508 TA Utrecht, Netherlands ABSTRACT deep crustal structures and their boundaries, such The crustal seismic velocity structure of northwestern Europe shows a low P-wave veloc- as the northwest European Caledonian suture ity zone (LVZ) in the lower crust along the Caledonian Thor suture zone (TSZ) that cannot zones (e.g., Barton, 1992; MONA LISA Work- be easily attributed to Avalonia or Baltica plates abutting the TSZ. The LVZ appears to cor- ing Group, 1997; Pharaoh, 1999; England, 2000; respond to a hitherto unrecognized crustal segment (accretionary complex) that separates Fig. 1; Fig. DR1 in the GSA Data Repository1). Avalonia from Baltica, explaining well the absence of Avalonia further east. Consequently, Reflection seismic profiles in the southern North the northern boundary of Avalonia is shifted ~150 km southward. Our interpretation, based Sea and the North German Basin generally show on analysis of deep seismic profiles, places the LVZ in a consistent crustal domain inter- poor resolution at deeper crustal levels due to pretation. A comparison with present-day examples of the Kuril and Cascadia subduction the presence of evaporites, one of the reasons to zones suggests that the LVZ separating Avalonia from Baltica is composed of remnants of record refraction seismic profiles (e.g., Rabbel the Caledonian accretionary complex. If so, the present-day geometry probably originates et al., 1995; Krawczyk et al., 2008). -
Homewarts-Movie-Map-Guide2.Pdf
1 This guide will provide you with more detailed information such as addresses, route descriptions and other useful information for a convenient homewarts journey. As we did on homewarts.com, we will start in London. 2 Alohomora London .................................................................................................................................................. 6 London City ........................................................................................................................................ 7 Lambeth Bridge .................................................................................................................................... 9 Horse Guards Avenue ....................................................................................................................... 11 Great Scotland Yard....................................................................................................................... 13 Piccadilly Circus ............................................................................................................................. 15 Charing Cross Road ......................................................................................................................... 17 Australian High Commission ........................................................................................................ 18 St. Pancras and King’s Cross ........................................................................................................ 20 Claremont Square ........................................................................................................................... -
Ipas in Scotland • 2
IPAs in Scotland • 2 • 5 • 6 • 3 • 4 • 15 • 10 • 11 • 14 • 16 • 12 • 13 • 9 • 7 • 8 • 17 • 19 • 21 • 26 • 29 • 23 • 25 • 27 31 • • 33 • 18 • 28 • 32 • 24 • 20 • 22 • 30 • 40 • 34 • 39 • 41 • 45 • 35 • 37 • 38 • 44 • 36 • 43 • 42 • 47 • 46 2 Contents Contents • 1 4 Foreword 6 Scotland’s IPAs: facts and figures 12 Protection and management 13 Threats 14 Land use 17 Planning and land use 18 Land management 20 Rebuilding healthy ecosystems 21 Protected areas Code IPA name 22 Better targeting of 1 Shetland 25 Glen Coe and Mamores resources and support 2 Mainland Orkney 26 Ben Nevis and the 24 What’s next for 3 Harris and Lewis Grey Corries Scotland’s IPAs? 4 Ben Mor, Assunt/ 27 Rannoch Moor 26 The last word Ichnadamph 28 Breadalbane Mountains 5 North Coast of Scotland 29 Ben Alder and Cover – Glen Coe 6 Caithness and Sutherland Aonach Beag ©Laurie Campbell Peatlands 30 Crieff Woods 7 Uists 31 Dunkeld-Blairgowrie 8 South West Skye Lochs 9 Strathglass Complex 32 Milton Wood 10 Sgurr Mor 33 Den of Airlie 11 Ben Wyvis 34 Colonsay 12 Black Wood of Rannoch 35 Beinn Bheigier, Islay 13 Moniack Gorge 36 Isle of Arran 14 Rosemarkie to 37 Isle of Cumbrae Shandwick Coast 38 Bankhead Moss, Beith 15 Dornoch Firth and 39 Loch Lomond Woods Morrich More 40 Flanders Moss 16 Culbin Sands and Bar 41 Roslin Glen 17 Cairngorms 42 Clearburn Loch 18 Coll and Tiree 43 Lochs and Mires of the 19 Rum Ale and Ettrick Waters 20 Ardmeanach 44 South East Scotland 21 Eigg Basalt Outcrops 22 Mull Oakwoods 45 River Tweed 23 West Coast of Scotland 46 Carsegowan Moss 24 Isle of Lismore 47 Merrick Kells Citation Author Plantlife (2015) Dr Deborah Long with editorial Scotland’s Important comment from Ben McCarthy. -
The Biology and Management of the River Dee
THEBIOLOGY AND MANAGEMENT OFTHE RIVERDEE INSTITUTEofTERRESTRIAL ECOLOGY NATURALENVIRONMENT RESEARCH COUNCIL á Natural Environment Research Council INSTITUTE OF TERRESTRIAL ECOLOGY The biology and management of the River Dee Edited by DAVID JENKINS Banchory Research Station Hill of Brathens, Glassel BANCHORY Kincardineshire 2 Printed in Great Britain by The Lavenham Press Ltd, Lavenham, Suffolk NERC Copyright 1985 Published in 1985 by Institute of Terrestrial Ecology Administrative Headquarters Monks Wood Experimental Station Abbots Ripton HUNTINGDON PE17 2LS BRITISH LIBRARY CATALOGUING-IN-PUBLICATIONDATA The biology and management of the River Dee.—(ITE symposium, ISSN 0263-8614; no. 14) 1. Stream ecology—Scotland—Dee River 2. Dee, River (Grampian) I. Jenkins, D. (David), 1926– II. Institute of Terrestrial Ecology Ill. Series 574.526323'094124 OH141 ISBN 0 904282 88 0 COVER ILLUSTRATION River Dee west from Invercauld, with the high corries and plateau of 1196 m (3924 ft) Beinn a'Bhuird in the background marking the watershed boundary (Photograph N Picozzi) The centre pages illustrate part of Grampian Region showing the water shed of the River Dee. Acknowledgements All the papers were typed by Mrs L M Burnett and Mrs E J P Allen, ITE Banchory. Considerable help during the symposium was received from Dr N G Bayfield, Mr J W H Conroy and Mr A D Littlejohn. Mrs L M Burnett and Mrs J Jenkins helped with the organization of the symposium. Mrs J King checked all the references and Mrs P A Ward helped with the final editing and proof reading. The photographs were selected by Mr N Picozzi. The symposium was planned by a steering committee composed of Dr D Jenkins (ITE), Dr P S Maitland (ITE), Mr W M Shearer (DAES) and Mr J A Forster (NCC). -
2019 Scotch Whisky
©2019 scotch whisky association DISCOVER THE WORLD OF SCOTCH WHISKY Many countries produce whisky, but Scotch Whisky can only be made in Scotland and by definition must be distilled and matured in Scotland for a minimum of 3 years. Scotch Whisky has been made for more than 500 years and uses just a few natural raw materials - water, cereals and yeast. Scotland is home to over 130 malt and grain distilleries, making it the greatest MAP OF concentration of whisky producers in the world. Many of the Scotch Whisky distilleries featured on this map bottle some of their production for sale as Single Malt (i.e. the product of one distillery) or Single Grain Whisky. HIGHLAND MALT The Highland region is geographically the largest Scotch Whisky SCOTCH producing region. The rugged landscape, changeable climate and, in The majority of Scotch Whisky is consumed as Blended Scotch Whisky. This means as some cases, coastal locations are reflected in the character of its many as 60 of the different Single Malt and Single Grain Whiskies are blended whiskies, which embrace wide variations. As a group, Highland whiskies are rounded, robust and dry in character together, ensuring that the individual Scotch Whiskies harmonise with one another with a hint of smokiness/peatiness. Those near the sea carry a salty WHISKY and the quality and flavour of each individual blend remains consistent down the tang; in the far north the whiskies are notably heathery and slightly spicy in character; while in the more sheltered east and middle of the DISTILLERIES years. region, the whiskies have a more fruity character. -
Edinburgh Departures: 2017/18 Award Winning Small Group Tours
Edinburgh Departures: 2017/18 Award Winning Small Group Tours Go beyond the guidebooks Travel the local way on small group tours of 16 people or less You’ll have a guaranteed experience, or your money back Guaranteed departures: you book, you go +44 (0)131 212 5005 (8am to 10pm) www.rabbies.com 1 ENTREPRENEUR OF THE YEAR TOURISM EVERYONE’S BUSINESS Kleingruppengarantie – Garanzia di piccoli gruppi - Grupos Reducidos Garantizados - La garantie de petits groupes - mit maximal 16 Mitreisenden. Massimo 16 passeggeri. Máximo de 16 pasajeros. 16 passagers maximum. Durchführungsgarantie – wenn Sie Partenze garantite - Salida Garantizada - La garantie des départs - gebucht haben, dann reisen Sie auch! Prenotate, Partite! ¡Si Reserva, Viaja! Vous avez réservé, vous partez! Wir garantieren eine einzigartige Esperienza Garantita - Experiencia Garantizada - La Guarantie de L’Expérience - Reise – oder erhalten Sie Ihr Geld Soddisfatti o rimborsati! ¡O le devolvemos su dinero! Ou on vous rembourse! zurück. Escursioni con un massimo Viajando con un máximo de Ses tours d’un maximum de 16 Da unsere Gruppen aus maximal 16 di 16 passeggeri per offrire il 16 pasajeros, le garantizamos passagers, vous permettront de Personen bestehen, bekommen Sie massimo valore, più attenzione mayor beneficio, más atención profiter d’une attention plus viel mehr Leistung für Ihr Geld. personale, più tempo con le personalizada, más tiempo con personnalisée, plus de temps de Mehr persönliche Aufmerksamkeit, persone del posto, meno tempo los habitantes locales, menos rencontre avec les gens locaux, mehr Zeit mit den Einheimischen, sull’autobus, più tempo nelle tiempo en el autobús y más en moins de temps dans l’autocar, mehr Zeit auf wenig befahrenen stradine meno conosciute e, nel rutas apartadas. -
Orcadian Basin Devonian Extensional Tectonics Versus Carboniferous
Journal of the Geological Society Devonian extensional tectonics versus Carboniferous inversion in the northern Orcadian basin M. SERANNE Journal of the Geological Society 1992; v. 149; p. 27-37 doi:10.1144/gsjgs.149.1.0027 Email alerting click here to receive free email alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Journal of the Geological Society or the Lyell Collection Notes Downloaded by INIST - CNRS trial access valid until 31/05/2008 on 31 March 2008 © 1992 Geological Society of London Journal of the Geological Society, London, Vol. 149, 1992, pp. 21-31, 14 figs, Printed in Northern Ireland Devonian extensional tectonics versus Carboniferous inversion in the northern Orcadian basin M. SERANNE Laboratoire de Gdologie des Bassins, CNRS u.a.1371, 34095 Montpellier cedex 05, France Abstract: The Old Red Sandstone (Middle Devonian) Orcadian basin was formed as a consequence of extensional collapse of the Caledonian orogen. Onshore study of these collapse-basins in Orkney and Shetland provides directions of extension during basin development. The origin of folding of Old Red Sandstone sediments, that has generally been related to a Carboniferous inversion phase, is discussed: syndepositional deformation supports a Devonian age and consequently some of the folds are related to basin formation. Large-scale folding of Devonian strata results from extensional and left-lateral transcurrent faulting of the underlying basement. Spatial variation of extension direction and distribution of extensional and transcurrent tectonics fit with a model of regional releasing overstep within a left- lateral megashear in NW Europe during late-Caledonian extensional collapse. -
Geology: Ordovician Paleogeography and the Evolution of the Iapetus Ocean
Ordovician paleogeography and the evolution of the Iapetus ocean Conall Mac Niocaill* Department of Geological Sciences, University of Michigan, 2534 C. C. Little Building, Ben A. van der Pluijm Ann Arbor, Michigan 48109-1063. Rob Van der Voo ABSTRACT thermore, we contend that the combined paleomagnetic and faunal data ar- Paleomagnetic data from northern Appalachian terranes identify gue against a shared Taconic history between North and South America. several arcs within the Iapetus ocean in the Early to Middle Ordovi- cian, including a peri-Laurentian arc at ~10°–20°S, a peri-Avalonian PALEOMAGNETIC DATA FROM IAPETAN TERRANES arc at ~50°–60°S, and an intra-oceanic arc (called the Exploits arc) at Displaced terranes occur along the extent of the Appalachian-Cale- ~30°S. The peri-Avalonian and Exploits arcs are characterized by Are- donian orogen, although reliable Ordovician paleomagnetic data from Ia- nigian to Llanvirnian Celtic fauna that are distinct from similarly aged petan terranes have only been obtained from the Central Mobile belt of the Toquima–Table Head fauna of the Laurentian margin, and peri- northern Appalachians (Table 1). The Central Mobile belt separates the Lau- Laurentian arc. The Precordillera terrane of Argentina is also charac- rentian and Avalonian margins of Iapetus and preserves remnants of the terized by an increasing proportion of Celtic fauna from Arenig to ocean, including arcs, ocean islands, and ophiolite slivers (e.g., Keppie, Llanvirn time, which implies (1) that it was in reproductive communi- 1989). Paleomagnetic results from Arenigian and Llanvirnian volcanic units cation with the peri-Avalonian and Exploits arcs, and (2) that it must of the Moreton’s Harbour Group and the Lawrence Head Formation in cen- have been separate from Laurentia and the peri-Laurentian arc well tral Newfoundland indicate paleolatitudes of 11°S (Table 1), placing them before it collided with Gondwana. -
OUGS Journal 32
Open University Geological Society Journal Volume 32 (1–2) 2011 Editor: Dr David M. Jones e-mail: [email protected] The Open University Geological Society (OUGS) and its Journal Editor accept no responsibility for breach of copyright. Copyright for the work remains with the authors, but copyright for the published articles is that of the OUGS. ISSN 0143-9472 © Copyright reserved OUGS Journal 32 (1–2) Edition 2011, printed by Hobbs the Printers Ltd, Totton, Hampshire Committee of the Open University Geological Society 2011 Society Website: ougs.org Executive Committee President: Dr Dave McGarvie, Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA Chairman: Linda Fowler Secretary: Sue Vernon, Treasurer: John Gooch Membership Secretary: Phyllis Turkington Newsletter Editor: Karen Scott Events Officer: Chris Arkwright Information Officer: vacant at time of going to press Branch Organisers East Anglia (EAn): Wendy Hamilton East Midlands (EMi): Don Cameron East Scotland (ESc): Stuart Swales Ireland (Ire): John Leahy London (Lon): Jenny Parry Mainland Europe (Eur): Elisabeth d'Eyrames Northumbria (Nor): Paul Williams North West (NWe): Mrs Jane Schollick Oxford (Oxf): Sally Munnings Severnside (Ssi): Janet Hiscott South East (SEa): Elizabeth Boucher South West (SWe): Chris Popham Walton Hall (WHa): Tom Miller Wessex (Wsx): Sheila Alderman West Midlands (WMi): Linda Tonkin West Scotland (WSc): Jacqueline Wiles Yorkshire (Yor): Geoff Hopkins Other officers (non-OUGSC voting unless otherwise indicated) Sales Administrator (voting OUGSC member ): vacant at time of going to press Administrator: Don Cameron Minutes Secretary: Pauline Kirtley Journal Editor: Dr David M. Jones Archivist/Reviews: Jane Michael Webmaster: Stuart Swales Deputy Webmaster: Martin Bryan Gift Aid Officer: Ann Goundry OUSA Representative: Capt. -
Stratigraphical Framework for the Devonian (Old Red Sandstone) Rocks of Scotland South of a Line from Fort William to Aberdeen
Stratigraphical framework for the Devonian (Old Red Sandstone) rocks of Scotland south of a line from Fort William to Aberdeen Research Report RR/01/04 NAVIGATION HOW TO NAVIGATE THIS DOCUMENT ❑ The general pagination is designed for hard copy use and does not correspond to PDF thumbnail pagination. ❑ The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub-headings, figures, 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 sub-section 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 NATURAL ENVIRONMENT RESEARCH COUNCIL BRITISH GEOLOGICAL SURVEY Research Report RR/01/04 Stratigraphical framework for the Devonian (Old Red Sandstone) rocks of Scotland south of a line from Fort William to Aberdeen Michael A E Browne, Richard A Smith and Andrew M Aitken Contributors: Hugh F Barron, Steve Carroll and Mark T Dean Cover illustration Basal contact of the lowest lava flow of the Crawton Volcanic Formation overlying the Whitehouse Conglomerate Formation, Trollochy, Kincardineshire. BGS Photograph D2459. The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/2002.