Holmes, Samuel John (2019) the Pre-Depositional History of the Applecross Formation, Northwest Highlands, Scotland

Total Page:16

File Type:pdf, Size:1020Kb

Holmes, Samuel John (2019) the Pre-Depositional History of the Applecross Formation, Northwest Highlands, Scotland Holmes, Samuel John (2019) The pre-depositional history of the Applecross Formation, Northwest Highlands, Scotland. MSc(R) thesis. http://theses.gla.ac.uk/41219/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten: Theses https://theses.gla.ac.uk/ [email protected] The pre-depositional history of the Applecross Formation, Northwest Highlands, Scotland. Samuel John Holmes BSc (Hons) Submitted in fulfilment of the requirements for the Degree of Master of Science School of Geographical and Earth Sciences College of Science and Engineering University of Glasgow November 2018 Abstract The provenance of Applecross Formation sedimentary rocks (Torridon Group, Northwest Scotland) is a topic of significant debate owing to difficulties in clearly correlating various datasets for the region (detrital mineral studies, sedimentology, and palinspastic restorations) to create an accepted palaeogeographic reconstruction. This study aims to elucidate the source area of Applecross sedimentary rocks and modes of deposition and transportation. LA-ICP-MS 206Pb/238U dating of detrital zircon samples from various stratigraphic levels within the Applecross Formation type area is utilised to assess variations in the source over time. Sampling is spread through ~2000m of stratigraphy, along a ~15km outcrop parallel transect between Applecross and Loch Kishorn. Data reduction is undertaken using Iolite data reduction software. U-Pb detrital zircon peaks of Mesoproterozoic (1280-1520Ma) and late Palaeoproterozoic (1680-1980Ma) age are dominant throughout the Applecross Formation. Minor early Palaeoproterozoic (2191-2265Ma) and Archean components up to 3346±43Ma are present. These data are in broad agreement with detrital zircon data from elsewhere in the Applecross Formation presented by Rainbird, Hamilton and Young (2001) and Krabbendam et al. (2017), suggesting a uniform input of well mixed sediment from a single source. Terranes in the foreland basin of the Grenville Orogen are favoured as source areas, with transport in an orogen axial foreland trunk system. Detrital Zircon U- Pb geochronology is combined with sedimentological context to determine depositional style. Deposition is interpreted to occur in a large scale distributive system similar to the Okavango Delta, Botswana, with unconfinement occurring during an extensional phase of the Grenville Orogen associated with rotation of Baltica relative to Laurentia at the time of deposition (see Rivers, 1997; Cawood et al., 2007). This proposal correlates known detrital mineral and sedimentological datasets. Further work is required to support the model; additional detrital zircon datasets are required to confirm the validity of a single sediment input. Further evidence for localised extension in the Applecross region is required to substantiate unconfinement of an established foreland trunk river system. I Chapter 1-Introduction Table of Contents The pre-depositional history of the Applecross Formation, Northwest Highlands, Scotland. ...................................................................................... I Abstract ....................................................................................... I List of Tables and Figures ................................................................. VI Acknowledgements ....................................................................... VIII Author’s Declaration ....................................................................... IX Chapter 1 Introduction .................................................................. 1 1.1 Objectives ......................................................................... 1 1.2 Setting .............................................................................. 2 1.3 Detrital zircon geochronology .................................................. 6 1.4 Previous work ..................................................................... 7 1.5 Rodinia configuration ........................................................... 11 1.6 Grenville configuration and basements ...................................... 14 1.6.1 Rockall Plateau ............................................................. 18 1.7 Palaeocurrents and sedimentology ........................................... 19 1.7.1 Torridon Group setting ..................................................... 19 1.7.2 Diabaig Formation .......................................................... 20 1.7.3 Applecross Formation ...................................................... 20 1.7.4 Aultbea Formation .......................................................... 21 1.7.5 Cailleach Head Formation ................................................. 21 Chapter 2 Methodology ................................................................. 22 2.1 Preliminary fieldwork and sample collection ................................ 22 2.1.1 Study area ................................................................... 22 2.1.2 Sampling regime ............................................................ 22 2.2 Laboratory protocol ............................................................. 23 2.2.1 Mineral separation .......................................................... 23 2.2.1.1 Crushing ................................................................. 23 2.2.1.2 Washing ................................................................. 23 II Chapter 1-Introduction 2.2.1.3 Sieving ................................................................... 23 2.2.1.4 Magnetic separation ................................................... 23 2.2.1.5 Density separation ..................................................... 25 2.2.1.6 Sample assessment, picking, and mounting ....................... 25 2.2.2 Analysis ....................................................................... 27 2.2.2.1 SEM cathodoluminescence and secondary electron imaging .... 27 2.2.2.2 Sample mapping ....................................................... 28 2.2.3 Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry (LA- ICP-MS) 29 2.2.3.1 Laser setup ............................................................. 29 2.2.3.2 ICP-MS setup ............................................................ 30 2.2.3.3 Standards ............................................................... 31 2.2.4 Data reduction .............................................................. 31 2.2.4.1 Kernel density estimates and probability density plots .......... 33 Chapter 3 Results........................................................................ 36 3.1.1 Zircon textures in Cathodoluminescence ............................... 36 3.1.1.1 Zoning ................................................................... 36 3.1.1.2 Metamorphic overgrowths ............................................ 36 3.1.1.3 Metamictization ........................................................ 37 3.1.1.4 Fracturing ............................................................... 37 3.1.1.5 Inclusions ............................................................... 37 3.1.1.6 Ablation pit morphology .............................................. 37 3.1.2 Plesovice Zircon standards ................................................ 38 3.1.2.1 Standards data ......................................................... 38 3.2 LA-ICP-MS ages: Applecross Peninsula ........................................ 39 3.2.1 Kernel Density Estimates (KDE) ........................................... 39 3.2.1.1 SA2 – SA 3.1 ............................................................. 39 3.2.1.2 SA4 - SA7 ................................................................ 40 3.2.1.3 SA5 ....................................................................... 41 III Chapter 1-Introduction 3.2.1.4 SA8 ....................................................................... 42 3.2.1.5 SA10 - SA21C ........................................................... 43 3.2.2 Stratigraphic succession ................................................... 44 3.2.2.1 Age variation through stratigraphy .................................. 48 3.2.2.2 Age variation through stratigraphy summary ...................... 54 3.3 Ablation spots .................................................................... 56 3.3.1 Ablation sites ................................................................ 56 3.3.2 Table of ablated spots ..................................................... 57 3.3.3 Analysis quality ............................................................. 58 Chapter 4 Discussion .................................................................... 61 4.1 Detrital zircon age data ........................................................ 61 4.2 Source areas ...................................................................... 67 4.2.1 Archean-early Palaeoproterozoic ........................................ 69 4.2.2 Palaeoproterozoic .......................................................... 69 4.2.3 Early Mesoproterozoic age gap ..........................................
Recommended publications
  • James Hawkins 2009 the Chronicles of the Straight Line Ramblers Club
    The Chronicles of the Straight Line Ramblers Club James Hawkins 2009 The Chronicles of the Straight Line Ramblers Club James Hawkins SW1 GALLERY 12 CARDINAL WALK LONDON SW1E 5JE James and Flick Hawkins would like to thank The John Muir Trust (www.jmt.org) and Knoydart Foundation (www.knoydart-foundation.com) for their support Design Peter A Welch (www.theworkhaus.com) MAY 2009 Printed J Thomson Colour Printers, Inverness, IV3 8GY The Straight Line Ramblers Club Don’t get me wrong, I am most enthusiastic about technology and its development; I am very happy to be writing this on my new PC that also helps me enormously with many aspects of my visual work. No it is more that, in our long evolution, at this point there now seems a danger of disconnection from The Straight Line Ramblers Club was first conceived when we were teenagers walking our parents the natural world. We have always been controlled by Nature, now we think that we can control it. dogs around the Oxfordshire countryside, membership was flexible, anyone could join and of course the one thing we didn’t do was walk in a straight line. Many of us have kept in touch and when John Muir, whose writings I have discovered during the research for this exhibition, felt that he needed we meet up that spirit of adventure still prevails, there aren’t any rules, but if there were they would to experience the wilderness “to find the Law that governs the relations subsisting between human be that spontaneity is all, planned routes exist to be changed on a whim and that its very impor- beings and Nature.” After many long and often dangerous journeys into wild places he began to tant to see what’s around the next corner or over the next top.
    [Show full text]
  • Scotland's Geodiversity, Provides a Source of Basic Raw Materials: Raw Basic of Source a Provides Geodiversity, Scotland's
    ROCKS,FOSSILS, LANDFORMS AND SOILS AND LANDFORMS ROCKS,FOSSILS, Cover photograph:Glaciatedmountains,CoireArdair,CreagMeagaidh. understanding. e it and promote its wider its promote and it e conserv to taken being steps the and it upon pressures the heritage, Earth Scotland's of diversity the illustrates leaflet This form the foundation upon which plants, animals and people live and interact. interact. and live people and animals plants, which upon foundation the form he Earth. They also They Earth. he t of understanding our in part important an played have soils and landforms fossils, rocks, Scotland's surface. land the alter the landscapes and scenery we value today, how different life-forms have evolved and how rivers, floods and sea-level changes a changes sea-level and floods rivers, how and evolved have life-forms different how today, value we scenery and landscapes the re continuing to continuing re CC5k0309 mates have shaped have mates cli changing and glaciers powerful volcanoes, ancient continents, colliding how of story wonderful a illustrates It importance. Printed on environmentally friendly paper friendly environmentally on Printed nternational i and national of asset heritage Earth an forms and istence, ex Earth's the of years billion 3 some spanning history, geological For a small country, Scotland has a remarkable diversity of rocks, fossils, landforms and soils. This 'geodiversity' is the res the is 'geodiversity' This soils. and landforms fossils, rocks, of diversity remarkable a has Scotland country, small a For ult of a rich and varied and rich a of ult Leachkin Road, Inverness, IV3 8NW. Tel: 01463 725000 01463 Tel: 8NW.
    [Show full text]
  • The Minor Intrusions of Assynt, NW Scotland: Early Development of Magmatism Along the Caledonian Front
    Mineralogical Magazine, August 2004, Vol. 68(4), pp. 541–559 The minor intrusions of Assynt, NW Scotland: early development of magmatism along the Caledonian Front 1, 2,3 4 K. M. GOODENOUGH *, B. N. YOUNG AND I. PARSONS 1 British Geological Survey, West Mains Road, Edinburgh EH9 3LA, UK 2 Department of Geology and Mineralogy, University of Aberdeen, Marischal College, Broad Street, Aberdeen AB24 3UE, UK 3 Baker Hughes Inteq, Barclayhill Place, Portlethen, Aberdeen AB12 4PF, UK 4 Grant Institute of Earth Science, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK ABSTRACT The Assynt Culmination of the Moine Thrust Belt, in the northwest Scottish Highlands, contains a variety of Caledonian alkaline and calc-alkaline intrusions that are mostly of Silurian age. These include a significant but little-studied suite of dykes and sills, the Northwest Highlands Minor Intrusion Suite. We describe the structural relationships of these minor intrusions and suggest a classification into seven swarms. The majority of the minor intrusions can be shown to pre-date movement in the Moine Thrust Belt, but some appear to have been intruded duringthe period of thrusting.A complex history of magmatism is thus recorded within this part of the Moine Thrust Belt. New geochemical data provide evidence of a subduction-related component in the mantle source of the minor intrusions. KEYWORDS: Assynt, Caledonian, minor intrusion, Moine Thrust, Scotland. Introduction north of Assynt, to the Achall valley near Ullapool, but they are most abundant in the Assynt area. The WITHIN the Assynt Culmination of the Moine minor intrusions constitute a significant part of the Thrust Belt of NW Scotland (Fig.
    [Show full text]
  • WESTER ROSS Wester Ross Ross Wester 212 © Lonelyplanet Walk Tooneofscotland’Sfinestcorries, Coire Mhicfhearchair
    © Lonely Planet 212 Wester Ross Wester Ross is heaven for hillwalkers: a remote and starkly beautiful part of the High- lands with lonely glens and lochs, an intricate coastline of rocky headlands and white-sand beaches, and some of the finest mountains in Scotland. If you are lucky with the weather, the clear air will provide rich colours and great views from the ridges and summits. In poor conditions the remoteness of the area makes walking a much more serious proposition. Whatever the weather, the walking can be difficult, so this is no place to begin learning mountain techniques. But if you are fit and well equipped, Wester Ross will be immensely rewarding – and addictive. The walks described here offer a tantalising taste of the area’s delights and challenges. An Teallach’s pinnacle-encrusted ridge is one of Scotland’s finest ridge walks, spiced with some scrambling. Proving that there’s much more to walking in Scotland than merely jumping out of the car (or bus) and charging up the nearest mountain, Beinn Dearg Mhór, in the heart of the Great Wilderness, makes an ideal weekend outing. This Great Wilderness – great by Scottish standards at least – is big enough to guarantee peace, even solitude, during a superb two-day traverse through glens cradling beautiful lochs. Slioch, a magnificent peak overlooking Loch Maree, offers a comparatively straightforward, immensely scenic ascent. In the renowned Torridon area, Beinn Alligin provides an exciting introduction to its consider- WESTER ROSS able challenges, epitomised in the awesome traverse of Liathach, a match for An Teallach in every way.
    [Show full text]
  • Towards a Greener Applecross
    Towards March 20 a Greener 2014 Applecross Developed by: Michelle Akute Derina Paramitasari Waliullah Bhuiyan Emmanuel Nii Ankrah Alejandra Claure Tripti Prajapati Paul Boateng Darge Adenew Kristine Lim María Mercedes Vanegas Shadman Shukry Kayvan Maysami Supervisors Prof.Dr.Bernd Möller Dipl.Ing.Wulf Boie, Dipl.Soz. Dorsi Germann Towards a Greener Applecross ACKNOWLEDGEMENT We would like to express our gratitude to all individuals and organizations that have assisted us throughout the course of this study. This research wouldn’t have been possible without the support of the Applecross Estate Trust, the Applecross Community Company and the Applecross Energy Efficiency program. Our special thanks goes to Allison Macleod, Valerie Hodkingson, Alasdair Macleod, Gordon Cameron, Donald Ferguson, Barry Marsh, Alistair Brown, Ian Gillies, Archie Maclellan, David Newmanand their families for their unconditional support. We would also like to express our sincere appreciation to all residents of Applecross for the warm welcome we received. We loved learning about your culture and traditional Scottish dances. Our special thanks to all the people who participated in the interviews for making time to answer our questionnaires. The research team is very grateful to our supervisors from the University of Flensburg, Prof.Dr.Bernd Möller, Dipl.Ing.Wulf Boie, Dipl.Soz. DorsiGermann for their moral support, academic guidance, and the hours spent proof-reading and reviewing the present document. Our particular appreciation to the DeutscherAkademischerAustauschDienst (DAAD, German Academic Exchange Service) and the Global Electricity Partnership for their financial support without which this experience of the International Class 2014 would not have been possible. Towards a Greener Applecross Disclaimer Although the contents were reviewed several times before being part of this report, the accuracy of the results cannot be guaranteed.
    [Show full text]
  • NORTHWEST © Lonelyplanetpublications Northwest Northwest 256 and Thedistinctive, Seeminglyinaccessiblepeakstacpollaidh
    © Lonely Planet Publications 256 www.lonelyplanet.com NORTHWEST •• Information 257 0 10 km Northwest 0 6 miles Northwest – Maps Cape Wrath 1 Sandwood Bay & Cape Wrath p260 Northwest Faraid 2 Ben Loyal p263 Head 3 Eas a' Chùal Aluinn p266 H 4 Quinag p263 Durness C Sandwood Creag Bay S Riabach Keoldale t (485m) To Thurso The north of Scotland, beyond a line joining Ullapool in the west and Dornoch Firth in r Kyle of N a (20mi) t Durness h S the east, is the most sparsely populated part of the country. Sutherland is graced with a h i n Bettyhill I a r y 1 Blairmore A838 Hope of Tongue generous share of the wildest and most remote coast, mountains and glens. At first sight, Loch Eriboll M Kinlochbervie Tongue the bare ‘hills’, more rock than earth, and the maze of lochs and waterways may seem Loch Kyle B801 Cranstackie Hope alien – part of another planet – and unattractive. But the very wildness of the rockscapes, (801m) r Rudha Rhiconich e Ruadh An Caisteal v the isolation of the long, deep glens, and the magnificence of the indented coastline can E (765m) a A838 Foinaven n Laxford (911m) Ben Hope h Loch t exercise a seductive fascination. The outstanding significance of the area’s geology has Bridge (927m) H 2 Loyal a r been recognised by the designation of the North West Highlands Geopark (see the boxed t T Scourie S Loch Ben Stack Stack A836 text on p264 ), the first such reserve in Britain. Intrusive developments are few, and many (721m) long-established paths lead into the mountains and through the glens.
    [Show full text]
  • Free Church Lochcarron & Applecross
    AN CARRANNACH The General Interest Magazine of Lochcarron, Shieldaig, Applecross, Kishorn and Torridon & Kinlochewe Districts NO: 351 MARCH 2017 £1.00 Our AGM was held on the 13th January and saw some changes to the committee. George Hendry is staying on as Chieftain, Henry Dalgety is also staying on as Club President with Anne MacCuish as Vice President. Janet Price is continuing to be our Secretary. Neil Ross from Kishorn has taken on the role of Treasurer from Fionnuala Stark. Fionnuala will continue as a committee member after a number of years being Treasurer. Fiona McLeod is staying on as Publicity Officer, completing articles and updating Facebook. Andrew Slaughter is going to continue as Team Manager on his own. We thank Alan Mackay for his joint management team last season with Andrew. Bob Munro will continue as Team Coach and our Youth Coaches will be Laura Mackay and Douglas Mackenzie. Further committee members are: Liam Arnott, Lachlan Dean Morrice, Crisdean Finlayson, Peter Mackenzie, Katrine Fogt, David MacCuish and Fionnuala Stark. We would also like to thank Helen Stewart who has stepped down from the committee this year after a number of years loyal service. On the 11th February, we had our first preseason friendly against Skye 2nds. It was a beautiful day for our first game at The Battery Park. Skye started strongly and kept the Lochcarron defence busy for the opening thirty minutes going 3-nil up. Lochcarron got back into the game, just before half time, through a well worked free hit which was finished well with Crisdean Finlayson finding the back of the Skye net.
    [Show full text]
  • Applecross Community Land Use Plan
    APPLECROSS COMMUNITY LAND USE PLAN Plana Cleachdadh Fearainn Coimhearsnachd na Comraich JULY 2019 Caroline Appleyard - www.appleyard-art.co.uk FOREWORD CONTENTS PAS (www.pas.org.uk) was commissioned by the Applecross Community 1 INTRODUCTION 3 Company (ACC) to produce this land use plan with a focus on identifying geographical areas which are suitable for future development. Such 1.1 PURPOSE 3 developments may include new homes, recreational areas, community 1.2 CONTEXT 3 and commercial buildings, and walking routes. The methodology of the Charretteplus® model was adapted to deliver this process, this being 1.3 PLAN AREA 4 a series of community conversations and workshops where people are encouraged to come together to discuss and share ideas for the future of Applecross. 2 APPROACH & EVIDENCE GATHERING 4 This plan has been developed by the ACC and Applecross Trust and is a community plan, to be shared and delivered by all members of the 2.1 METHODOLOGY 4 Applecross Community. 2.2 CONTEXT SETTING 4 2.3 VISIONING 4 2.4 COMMUNITY PRIORITIES 5 2.5 ACTION 5 3 STRATEGIC VISION 7 3.1 AIM 7 3.2 VISION 7 3.3 PLACEMAKING PRIORITIES 7 4 PLACE 8 4.1 NORTH APPLECROSS - ZONE 1 9 WHAT’S IN A LOGO? 4.2 ESTATE AND SHORE ST - ZONE 2 15 4.3 SOUTH APPLECROSS - ZONE 3 44 This land use plan has been named Plan It Applecross, and the logo has been designed by pupils of Applecross Primary. The logo is intended to 5 SUMMARY / NEXT STEPS 48 represent the Applecross Peninsula with houses for everyone who needs them.
    [Show full text]
  • “MAPPING MOUNTAINS” – CELEBRATING SCIENCE THROUGH CULTURAL HERITAGE: REFLECTIONS on CURATING an EXHIBITION of 1880S GEOLOGICAL MAPS
    OUTREACH “MAPPING MOUNTAINS” – CELEBRATING SCIENCE THROUGH CULTURAL HERITAGE: REFLECTIONS ON CURATING AN EXHIBITION OF 1880s GEOLOGICAL MAPS The mountainous Northwest Highlands of Scotland have an interna- tional reputation for their geology. The Lewisian Gneiss is perhaps the most intensely studied piece of Precambrian crust in the world, worked on by generations of geologists and used as a testing ground for geochronological techniques. The area is best known for the Moine Thrust Zone, which carries the western edge of the Caledonian fold belt over the Archaean and Proterozoic ‘Foreland’, which is a remnant of Lau- rentia. For over a century geologists have studied the internal structure of mountain ranges to decipher their formation, and the Moine Thrust Zone, along with classic sites in the Alps, has played a key part in the history of our understanding of mountains and thrust tectonics. It was Part of the Ben More Assynt map surveyed by B.N. Peach and C.T. Clough, c. 1886–1888. The heavy boundary on the right is the Moine thrust itself; that on the left is one of the mapped, over 100 years ago, by geologists of the Geological Survey, led lower movement planes, the Ben More thrust. Copyright BGS, reprinted with permission by the great Ben Peach and John Horne, to solve a debate about the sequence of rocks. The resulting map formed the basis for what is known as ‘The Northwest Highlands Memoir’ (Peach et al. 1907)1. Initiatives in the Northwest Highlands to celebrate the geological her- itage of the area resulted in the formation of the Northwest Highlands Geopark in 2004.
    [Show full text]
  • Structural, Petrological, and Tectonic Constraints on the Loch Borralan and Loch Ailsh Alkaline Intrusions, Moine Thrust Zone, GEOSPHERE, V
    Research Paper GEOSPHERE Structural, petrological, and tectonic constraints on the Loch Borralan and Loch Ailsh alkaline intrusions, Moine thrust zone, GEOSPHERE, v. 17, no. 4 northwestern Scotland https://doi.org/10.1130/GES02330.1 Robert Fox and Michael P. Searle 24 figures Department of Earth Sciences, Oxford University, South Parks Road, Oxford OX1 3AN, UK CORRESPONDENCE: [email protected] ABSTRACT during ductile shearing. The minerals pseudomor- Grit Members of the An t-Sron Formation) and the phing leucites show signs of ductile deformation Ordovician Durness Group dolomites and lime- CITATION: Fox, R., and Searle, M.P., 2021, Structural, petrological, and tectonic constraints on the Loch Bor- During the Caledonian orogeny, the Moine indicating that high-temperature (~500 °C) defor- stones (Woodcock and Strachan, 2000; Strachan ralan and Loch Ailsh alkaline intrusions, Moine thrust thrust zone in northwestern Scotland (UK) mation acted upon pseudomorphed leucite crystals et al., 2010; British Geological Survey, 2007). zone, northwestern Scotland: Geosphere, v. 17, no. 4, emplaced Neoproterozoic Moine Supergroup rocks, that had previously undergone subsolidus break- The hinterland of the Caledonian orogenic p. 1126– 1150, https:// doi.org /10.1130 /GES02330.1. meta morphosed during the Ordovician (Grampian) down. New detailed field mapping and structural wedge comprises schists of the Moine Super- and Silurian (Scandian) orogenic periods, westward and petrological observations are used to constrain group with structural inliers of Lewisian basement Science Editor: Andrea Hampel Associate Editor: Robert S. Hildebrand over the Laurentian passive margin in the north- the geological evolution of both the Loch Ailsh gneisses and intrusive Caledonian granites (Geikie, ern highlands of Scotland.
    [Show full text]
  • Download Transcript
    Transcript – The future of mountain regions – International Mountain Day 2020 Host: John McLuckie Guest Speakers: Leonie Schulz, Mike Pescod John McLuckie: 0:16 This podcast has been brought to you by the University of the Highlands and Islands Careers and Employability Centre. In this episode, to mark International Mountain Day 2020, we'll be talking to Leoni Schulz, PhD student at UHI’s Centre for Mountain Studies and Mike Pescod, Mountain guide and instructor at the School of Adventure Studies at West Highland College UHI, about the future of mountain regions with a focus on the Highlands. My name is John McLuckie and I'm joined today by Leonie Schulz and Mike Pescod, welcome both to the podcast. Leonie Schulz: 0:47 Yeah, good morning. Thanks for having me today. Mike Pescod: 0:50 Thank you very much. John McLuckie: 0:51 Can I start by asking you both to tell us a bit about your route into your current role? Leonie Schulz: 0:55 Yeah sure. My name is Leonie, I'm originally from Germany, but I've lived and studied and worked in lots of different countries including New Zealand, South Africa and the Netherlands. I've lived in Scotland for five years now and I initially moved here to complete my Master's in ecotourism. After completing my Master's, I started a job with a tour company and I was responsible for the online marketing, product management and I also worked as a tour guide. I was mainly doing the walking tours, which take people to different parts in Scotland, for longer and shorter walks around the countryside, and my favourite tour was called the Highlands and Islands tour.
    [Show full text]
  • Scotland – the Splendours of Wester Ross 10 – 15 June 2019
    Tour Report Scotland – The Splendours of Wester Ross 10 – 15 June 2019 Merlin Black-throated diver Otter White-tailed eagle Compiled by Louise Hughes 01962 302086 [email protected] www.wildlifeworldwide.com Tour Leader: Louise Hughes Day 1: Monday 10 June 2019 Weather: Overcast with bursts of sunshine After picking everyone up from Inverness, we made our way to North Kessock. Sitting on the Beauly Firth, it was a nice spot to have our lunch whilst watching the water, and some of us managed to catch a glimpse of a male otter swimming towards the bridge. Our next stop was Black Water/Silverbridge, where we admired the Thomas Telford Bridge and the waterfalls. At Loch Droma, a black-throated diver was visible but kept diving for fish. We made a brief stop in Ullapool to scan the water, seeing a bottling grey seal some way offshore. Our final stop was Knockan Crag, where we not only admired the geology – where you can see the evidence of old rock sitting on top of younger rock – known as the Moine Thrust zone, but also saw a male ring ouzel that perched on the rock face before flying right over the top of us. We also had a lovely view of a male wheatear as well as another black-throated diver on the loch below the Crag. Another 25 minutes up the road and we arrived at our accommodation for the next three nights, the Eddrachilles Hotel, which has a beautiful view over Eddrachilles Bay. Day 2: Tuesday 11 June 2019 Weather: Drizzle on & off through the day with strong winds! Today we made for Handa Island, a small private island managed by the Scottish Wildlife Trust.
    [Show full text]