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Celtic Tours 2022 Brochure
TRIED AND TRUE SINCE 1972 – We are proud of the relationships we have earned over the years with our dedicated travel advisors, and we will promise to continue to bring you the best in service, products, and value. VALUE – Time and time again our tours and pack- ages offer more value for your clients. We have built long and strong relationships with our Irish suppli- ers, allowing us to package our tours at the best prices and inclusions. Call us for your customer tour requests and give us the opportunity to provide you with Celtic Value! 100% CUSTOMER SERVICE – Celtic Tours is driven by providing the best customer service to you, so you can relax and have piece of mind when booking with us. Our agents have a wealth of knowledge and are at your service to help you navigate through putting the perfect Irish vacation together for your clients. TRUST – You know when you are booking with Celtic Tours you are booking with a financially sound and secure company. A fiscally responsible company since 1972! We are also proud members of the United States Tour Operators Association (USTOA). Protecting you and your customers. NO HIDDEN FEES – At Celtic Tours, we do not want to surprise your clients with extras and add-ons. All touring and meals as noted on the itinerary are included. Our group arrival and departure transfers THE are always included no matter if you book air & land or land only with us (note: transfers are scheduled for CELTIC TOURS specific times.) EARN MORE – We know how hard travel agents work, and we want you rewarded. -
Scottish Highlands Hillwalking
SHHG-3 back cover-Q8__- 15/12/16 9:08 AM Page 1 TRAILBLAZER Scottish Highlands Hillwalking 60 DAY-WALKS – INCLUDES 90 DETAILED TRAIL MAPS – INCLUDES 90 DETAILED 60 DAY-WALKS 3 ScottishScottish HighlandsHighlands EDN ‘...the Trailblazer series stands head, shoulders, waist and ankles above the rest. They are particularly strong on mapping...’ HillwalkingHillwalking THE SUNDAY TIMES Scotland’s Highlands and Islands contain some of the GUIDEGUIDE finest mountain scenery in Europe and by far the best way to experience it is on foot 60 day-walks – includes 90 detailed trail maps o John PLANNING – PLACES TO STAY – PLACES TO EAT 60 day-walks – for all abilities. Graded Stornoway Durness O’Groats for difficulty, terrain and strenuousness. Selected from every corner of the region Kinlochewe JIMJIM MANTHORPEMANTHORPE and ranging from well-known peaks such Portree Inverness Grimsay as Ben Nevis and Cairn Gorm to lesser- Aberdeen Fort known hills such as Suilven and Clisham. William Braemar PitlochryPitlochry o 2-day and 3-day treks – some of the Glencoe Bridge Dundee walks have been linked to form multi-day 0 40km of Orchy 0 25 miles treks such as the Great Traverse. GlasgowGla sgow EDINBURGH o 90 walking maps with unique map- Ayr ping features – walking times, directions, tricky junctions, places to stay, places to 60 day-walks eat, points of interest. These are not gen- for all abilities. eral-purpose maps but fully edited maps Graded for difficulty, drawn by walkers for walkers. terrain and o Detailed public transport information strenuousness o 62 gateway towns and villages 90 walking maps Much more than just a walking guide, this book includes guides to 62 gateway towns 62 guides and villages: what to see, where to eat, to gateway towns where to stay; pubs, hotels, B&Bs, camp- sites, bunkhouses, bothies, hostels. -
Protected Landscapes: the United Kingdom Experience
.,•* \?/>i The United Kingdom Expenence Department of the COUNTRYSIDE COMMISSION COMMISSION ENVIRONMENT FOR SCOTLAND NofChern ireianc •'; <- *. '•ri U M.r. , '^M :a'- ;i^'vV r*^- ^=^l\i \6-^S PROTECTED LANDSCAPES The United Kingdom Experience Digitized by the Internet Archive in 2010 with funding from UNEP-WCIVIC, Cambridge http://www.archive.org/details/protectedlandsca87poor PROTECTED LANDSCAPES The United Kingdom Experience Prepared by Duncan and Judy Poore for the Countryside Commission Countryside Commission for Scotland Department of the Environment for Northern Ireland and the International Union for Conservation of Nature and Natural Resources Published for the International Symposium on Protected Landscapes Lake District, United Kingdom 5-10 October 1987 * Published in 1987 as a contribution to ^^ \ the European Year of the Environment * W^O * and the Council of Europe's Campaign for the Countryside by Countryside Commission, Countryside Commission for Scotland, Department of the Environment for Northern Ireland and the International Union for Conservation of Nature and Natural Resources © 1987 International Union for Conservation of Nature and Natural Resources Avenue du Mont-Blanc, CH-1196 Gland, Switzerland Additional copies available from: Countryside Commission Publications Despatch Department 19/23 Albert Road Manchester M19 2EQ, UK Price: £6.50 This publication is a companion volume to Protected Landscapes: Experience around the World to be published by the International Union for Conservation of Nature and Natural Resources, -
37 Foinaven - Ben Hee Wild Land Area
Description of Wild Land Area – 2017 37 Foinaven - Ben Hee Wild Land Area 1 Description of Wild Land Area – 2017 Context This large Wild Land Area (WLA) extends 569 km2 across north west Sutherland, extending from the peatlands of Crask in the south east to the mountain of Foinaven in the north west. The northern half of the WLA mainly comprises a complex range of high mountains in addition to a peninsula of lower hills extending towards Durness. In contrast, the southern half of the WLA includes extensive peatlands and the isolated mountain of Ben Hee. One of a cluster of seven WLAs in the north west of Scotland, flanked by main (predominantly single track) roads to the north, west and south, it is relatively distant from large population centres. The geology of the area has a strong influence on its character. Along the Moine Thrust Belt that passes through the north west, rocky mountains such as Foinaven and Arkle are highly distinctive with their bright white Cambrian quartzite and scree, with little vegetation. The geological importance of this area is recognised by its inclusion within the North West Highlands Geoparki. Land within the WLA is used mainly for deer stalking and fishing and, except for a few isolated estate lodges and farms, is uninhabited. Many people view the area from outside its edge as a visual backdrop, particularly when travelling along the A838 between Lairg and Laxford Bridge and Durness, and along the A836 between Lairg and Altnaharra, through Strath More, and around Loch Eriboll. The mountains within this WLA typically draw fewer hillwalkers than some other areas, partly due to the lack of Munros. -
Description Geological Map of Sutherland
DESCRIPTION OF THE GEOLOGICAL MAP OF SUTHERLAND. Br Pxo~.ssoa H~DD~. T was with considerable reluctance that I felt myself' compelled to I discard the system of coloration adopted in the Geological Survey Maps ; and rids I did only after the strongly expressed opinion of several geologists. ~t was not that I have any very intense desire to colour rocks after their natural tints, but I have an aversion to adopting a eolour suite which departs markedly therefrom ; or one which is in discordance instead of harmony therewith. One friend, a man of great scientific discretion, and himself an artist, writes me that when he looks at a recently published geological Map of Scotland, with its grey Torridon and its red Lauren- tian, he does not know whether he i~ standing on his head or his heels. I must say that I share the feeling intended to be therein expressed ; and hold that, if there is to he an absolute departure from the tone presented by the rocks themselves, we, at ]east, should not have the incongruity of a bed of a sombre or dark hue, reposing upon one of a markedly lighter tint. The co]ours, then, which have been adopted, if they differ from such as were formerly in use, have been selected upon the foregoing principles ; namely, some resemblance to nature, and the keeping the graver tints for the more profound rocks. There is what may be considered a departure from this, in the c~se of the lively tint given to the so-called "igneous rock." As this rock much resembles in many ways the Hebridian gneiss,--being only of a lighter tint,--a green was also chosen for it. -
Ainmean-Àite Na Cuinneige |The Place-Names of Quinag
Ainmean-Àite na Cuinneige |The Place-names of Quinag Quinag from the Ardroe path (photo by Gemma Smith, August 2020) Gemma Smith Roinn na Ceiltis is na Gàidhlig | Celtic and Gaelic Oilthigh Ghlaschu | University of Glasgow An Giblean 2021 | April 2021 Contents Introduction 2 Key to entries 4 Gazetteer 5 Bibliography 35 1 Introduction Area This toponymic survey covers the area currently designated as the Quinag Estate, Assynt, as delineated in the John Muir Trust’s map below. Names from the immediate environs of the survey area have been included where relevant or interesting. Map © John Muir Trust 2012 Land Use In order to understand historic land use in this area it is necessary to look past any idea of ‘the estate’, as Quinag was in the past a shared resource, with each farm that backed onto the hill having grazing rights to their own particular portion. Therefore any shielings, etc. must be understood in relation to the farm of which they were an integral part. The hinterland of each home baile also included peat bogs, woodlands, burns and lochs which would have supplied a variety of valuable resources year-round – see pg. 184 of the Old Statistical Account for ‘The ancient Divisions of the Land of the whole Parish’. As the saying goes regarding the rights of the Gàideil, breac à linne, slat à coille ‘s fiadh à fìreach – ‘a fish 2 from the burn, a staff from the wood and a deer from the moor’ – wild resources were just as important as farmed. John Home’s 1774 maps of the individual farms are readily available on the National Library of Scotland website, and should be consulted wherever necessary, as they are an unparalleled and invaluable resource in the context of the wider north-west area, and provide a uniquely detailed snapshot of pre-‘Improvement’ land use. -
Letter from Scotland Alex Mcleod of South Australia, 2010
A Letter from Scotland Alex McLeod of South Australia, 2010 EDITOR’S EXCURSION A Letter from Scotland.. Alex McLeod In 2010 we had 8 representatives from SA to the 4 yearly Clan MacLeod Societies’ Parliament. Not so much of a Parliament; but a Gathering with some Clan business. I was thrilled by the strong attendance of Merawyn, Alexa, Stefan & Doreen, Bronwyn and Bill & Jenny Hunt who were warmly greeted. The Raasay MacLeods especially acknowledged the Hunts for preserving the Raasay MacLeod history at their farming property “Nalang”, near Bordertown. Our pre Parliament gathering in Scotland is usually about regional culture and history, and this time it was held in the parish of Assynt, by Inchnadamph, in the northwest highlands and coast. That required some traveling, which we also continued later. So here is a spray of traveler’s impressions. Glasgow Yin and Yang. Clydebank shipyards ‘lang gang’ Architecture old and new. What rain can’t clean, steam may do. Edinburgh, Fringe - both witty and rank. Every building LOOKS like a bank; but ATM’s are hard to find. Military Tattoo was slick, refined. Stirling Castle renovation. Brooch of Scotland. History of a nation. The Wallace monument, -stand and linger. Still Wallace gives England the finger. Culloden battlefield Visitor Centre, Highland Charge & Helter Skelter. Aberdeen; granite grey upon grey; -couldn’t find it on a cloudy day. What were they thinking? Missed Perth, I was blinking. Bright Dundee on the Tay, Scot’s ship Discovery, St. Andrews, golfing town of ‘eagles, birdies and pars’, ‘Triple bogey’ traffic jams for travelers in cars. -
Geodiversity Audit and Action Plan 2013 - 2016
GEODIVERSITY AUDIT AND ACTION PLAN 2013 - 2016 THIS PROJECT IS BEING PART FINANCED BY THE SCOTTISH GOVERNMENT AND THE EUROPEAN COMMUNITY HIGHLAND LEADER 2007-2013 PROGRAMME. CONTENTS FOREWORD.................................................................................................................. 1 ROCKS FROM THE DAWN OF TIME……………………………………………………….2 INTRODUCTION............................................................................................................ 3 The North West Highlands Geopark........................................................................... 3 The Geology and Geological Structure of the NWHG................................................. 3 The Purpose of the Audit and Action Plan .................................................................. 5 Geodiversity................................................................................................................ 5 Part 1 – THE GEODIVERSITY AUDIT........................................................................... 7 North West Highland Geopark : Location Maps ............................................................. 9 NWHG REF. 001 - BEN HUTIG................................................................................ 13 NWHG REF. 002 - CLEIT AN T-SEABHAIG ............................................................ 15 NWHG REF. 003 - ERIBOLL.................................................................................... 17 NWHG REF. 004 - AN T-SRON .............................................................................. -
Geological Notes and Location Descriptions for Field Excursions
Inverness: 30 April - 7 May Inverness: 30 Geological notes and location descriptions for field excursions Deformation mechanisms, Rheology and Tectonics 2017 Deformation mechanisms, Rheology and Tectonics 1 Geological notes* The crustal evolution and geology of NW Scotland can be considered with reference to the Palaeozoic Caledonian orogeny. This major episode of crustal reworking was associated with the formation of a North Atlantic Craton – suturing the Proterozoic and older crustal blocks of Laurentian and Baltica (together with Avalonia, further south). NW Scotland contains part of the western margin of this orogen (or at least its more intense parts), a tectonic feature termed the Moine Thrust Belt. The foreland to the thrust belt preserves much older geology, exhumed from up to 35-40km depth, that give insight to processes that form, rework and reassemble the continental crust. The Caledonian rocks allow us to follow a transect from exhumed middle crustal sections within the orogen out into the foreland. Collectively these outcrops provide arrays of analogues for crustal geology and deformation structures, and we can use these to promote discussion of their geophysical characteristics when targeted in situ. However, the Caledonian crust, together with its foreland, has seen later deformation associated with the formation of sedimentary basins, chiefly in the immediate offshore. We can also access basin faults and examine not only their individual characteristics but also debate how they may have been influenced by pre-existing structures. Pre-Caledonian geology The Lewisian. The Lewisian forms the oldest basement to the British Isles and has classic Laurentian geology. The key geological markers in the field used to build up a sequence of geological events are a suite of NW-SE-trending metabasic sheets – the Scourie dykes. -
The Quaternary Deposits and Glacial History of the Area Around Inchnadamph, Sutherland
The Quaternary deposits and glacial history of the area around Inchnadamph, Sutherland Integrated Geoscience Surveys (Northern Britain) Internal Report IR/03/120 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/120 The Quaternary deposits and glacial history of the area around Inchnadamph, Sutherland Tom Bradwell 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 272191/2003 Key words NC22; Quaternary; glaciation Front cover Quinag, Sutherland [P513692] Bibliographical reference BRADWELL, T. 2003. The Quaternary deposits and glacial history of the area around Inchnadamph, Sutherland. British Geological Survey Internal Report, IR/03/1200. 25pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects. -
Mapping Glacial Bedforms and Erosion Zones in NW Scotland
*Manuscript Click here to view linked References 1 Identifying palaeo-ice-stream tributaries on hard beds: mapping glacial bedforms 2 and erosion zones in NW Scotland 3 4 Tom Bradwell* 5 British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA, UK 6 *Tel.: +44 131 6671000; Fax: +44 6681535; E-mail: [email protected] 7 8 Abstract 9 Ice streams are fed by tributaries that can extend deep into the heart of ice sheets. These tributaries are born 10 at onset zones — the abrupt transitions from slow sheet flow to fast streaming flow that often occur at 11 significant topographic steps on hard beds (bedrock-dominated beds). For this reason, tributary onset zones 12 leave only a subtle erosional geomorphic signature in the landscape record that is rarely studied. This paper 13 examines, in detail, the geomorphic signature of ice-sheet flow on a hard bed at the head of a palaeo-ice 14 stream. We use field survey techniques to map glacial bedforms within an ~ 200-km2 area of hard crystalline 15 bedrock in a landscape of ‘areal scour’ around Loch Laxford in NW Scotland. The bedrock bedforms range from 16 plastically moulded (p-forms) and wholly abraded forms, to stoss-lee forms and plucked surfaces all on an 17 outcrop scale (1-100 m). We devise a five-zone classification system to map (in a GIS) the presence, absence, 18 and abundance of glacial erosional forms within 619 (500-m square) grid cells. We go on to use these erosional 19 bedform zones, along with known glaciological relationships to interpret the spatial and altitudinal pattern of 20 palaeo-ice sheet processes and glacier dynamics in this part of NW Scotland. -
Area Lft2-Wildlife.Indd
Watch and wait The power of plants The diversity of wildlife within the Geopark is breathtaking. Ask Sweet gale or bog myrtle grows naturally in the Geopark and has local guides or consult our website to fi nd out about the best a long history of human use. Vikings were reputed to have used it places and seasons for watching animals and birds in their natural as a stimulant before battle, it’s been used instead of hops to make environment. You can also catch your own wild game such as beer and it’s even said to cure ulcers, intestinal worms, aching salmon or brown trout – but make sure you obtain the necessary muscles – and ward off insects. Now the antibacterial qualities of permits fi rst. Animals and birds you may see around the Geopark: the plant’s essential oils are being researched and developed to badger, stoat, weasel, pine marten, fox, hare, otter, red deer create skin products. and roe deer The geology of the north west Highlands provides the right whale species, porpoise, seal, basking shark and dolphin conditions for certain rare pants to thrive. Limestone encourages golden eagle, peregrine falcon, osprey, heron, willow warbler, the growth of mountain avens and globe fl ower while peatland wren, redpoll, redwing, sandpiper, oystercatcher, black- areas such as the classic ‘cnoc and lochan’ landscapes found throated diver around Eddrachilles support sphagnum mosses, sundew, cranberry European Geoparks Network North West Highlands Geopark is and bogbean. part of a global network of territories defi ned by their outstanding To fi nd out more about rare species and the way plants have geological features, forward-thinking local communities and unique natural and cultural heritage.