International Appalachian Trail ~ Annual General Meeting ~ 18Th - 20Th Sept, 2013
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The Lands of Kincaid in Relation to the Highlands of Scotland
Peter Anthony Kincaid The lands of Kincaid in relation to the Highlands of Scotland. The physical boundary between the Lowlands and the Highlands of Scotland is the Highland boundary fault. The Highland boundary fault creates a visible change in the geology of the land. The fault comes ashore from the river Clyde near Helensburgh and continues in a north east direction towards Aberfoyle. It continues north east all the way to near Stonehaven on the coast of the North Sea.1 The islands of Inchmurrin, Creinch, Torrinch, and Inchcailloch in Loch Lomond all form visible parts of the Highland boundary Fault.2 The lands of Kincaid are at best about 15.3 English miles or about 24.6 kilometres from this fault (if one takes a direct line from the intersection of Campsie Road and Milton Road to summits north east of Conic Hill). Without doubt the lands of Kincaid are physically in Lowland Scotland. Some may argue that people may have considered a different boundary with regards to what one considered a Highlander. The evidence does not support this. It is not until the 1716 penal laws established against the Highlanders that this author could locate any official boundary. In what we refer to as the Disarming Act of 1716, the western bounds were established as "within the Shires of Dumbarton on the North-side of the Water of Leven, Stirling on the North-side of the River of Forth."3 At that time, Scots must have understood the Highlands to be north of the River Forth and north of the river Leven. -
Land to East of Montrose House, Balmaha
Agenda Item 3 PLANNING AND ACCESS COMMITTEE MEETING: 26 March 2018 SUBMITTED BY: Director of Rural Development and Planning APPLICATION NUMBER: 2016/0399/DET APPLICANT: Rural Stirling Housing Association LOCATION: Land to East of Montrose House, Balmaha PROPOSAL: 20 unit affordable housing development (comprising 12no. houses and 8no. flats), formation of 2 housing plots, access road and associated infrastructure NATIONAL PARK WARD: 7 COMMUNITY COUNCIL AREA: Buchanan Community Council CASE OFFICER: Name: Alison Williamson Tel: 01389 722 610 E-mail: [email protected] 1. SUMMARY AND REASON FOR PRESENTATION 1.1 Planning Permission is sought by Rural Stirling Housing Association for a 20 unit affordable housing development comprising 12 houses and 8 flats, the formation of 2 self-build house plots, access road and associated infrastructure. 1.2 The National Park Authority’s Scheme of Delegation, relative to planning, requires applications subject to a significant level of representation to be referred to the Planning and Access Committee. 115 letters of representation have been received to this application. 2. RECOMMENDATION That Members: Approve the application subject to the imposition of conditions as set out in Appendix 1 of the report. 1 Agenda Item 3 3. BACKGROUND 3.1 The current application was submitted on 23 December 2016. After a period of delay, as a result of discussions over foul drainage constraints, all information required to assess the application has now been submitted and considered. Given the significant level of representation (see section 4 of this report) received in relation to this application, it was agreed at a meeting of the Planning and Access Committee on 18th December 2017 that a special date would be convened, for a hearing, to allow the application to be determined. -
CITATION CONIC HILL SITE of SPECIAL SCIENTIFIC INTEREST Stirling Site Code: 397
CITATION CONIC HILL SITE OF SPECIAL SCIENTIFIC INTEREST Stirling Site code: 397 PLANNING AUTHORITY: Loch Lomond and The Trossachs National Park Authority NATIONAL GRID REFERENCE: NS 421916, NS 415912, NS 411918, NS413920 OS 1:50,000 SHEET NO: Landranger Series 56 1:25,000 SHEET NO: Explorer Series 347 AREA: 60.66 hectares NOTIFIED NATURAL FEATURES Geological: Igneous Petrology : Ordovician Igneous Biological: Woodlands : Upland oak woodland : Wet woodland Upland habitats : Subalpine calcareous grassland : Alkaline fen Invertebrates : Beetle assemblage : Moth assemblage DESCRIPTION Conic Hill Site of Special Scientific Interest (SSSI) is comprised of several detached areas and lies on the east side of Loch Lomond, immediately north of the village of Balmaha. The largest portion of the SSSI constitutes the upland part, whilst the lower areas, adjacent to the loch shore, support woodland. Conic Hill is a composite site supporting varying rocks and soils, and wildlife habitats. The Highland Border Complex is of national importance and consists of a number of narrow, fault-bounded exposures of Ordovician sediments and igneous rocks, which crop out intermittently along the Highland Boundary Fault Zone between Arran and Stonehaven. The ultramafic and mafic rocks of the complex are interpreted as incomplete fragments of a greatly dismembered obducted ophiolite. A narrow zone of rocks belonging to the Complex is exposed north of Balmaha, on the eastern side of Loch Lomond. Exposures extending from the lakeside to Druim nam Beurach consist of detrital rocks which have yielded a chitinozoan fauna of probable Arenig age. The rocks contain a wide variety of ophiolitic clasts including serpentinite, gabbro, dolerite and spilite, which by implication were derived from an ophiolite of early Arenig, or more likely pre-Arenig age. -
The Best of Walking in Scotland
1 The Best of Walking in Scotland Scotland is a land of contrasts—an ancient country with a modern outlook, where well-loved traditions mingle with the latest technology. Here you can tread on some of the oldest rocks in the world and wander among standing stones and chambered cairns erected 5,000 years ago. However, that little cottage you pass may have a high-speed Internet connection and be home to a jewelry designer or an architect of eco-friendly houses. Certainly, you’ll encounter all the shortbread and tartan you expect, though kilts are normally reserved for weddings and football matches. But far more traditional, although less obviously so, is the warm welcome you’ll receive from the locals. The farther you go from the big cities, the more time people have to talk—you’ll find they have a genuine interest in where you come from and what you do. Scotland’s greatest asset is its clean, green landscapes, where walkers can fill their lungs with pure, fresh air. It may only be a wee (small) country, but it has a variety of walks to rival anywhere in the world. As well as the splendid mountain hikes to be found in the Highlands, there’s an equal extent of Lowland terrain with gentle riverside walks and woodland strolls. The indented coastline and numerous islands mean that there are thousands of miles of shore to explore, while the many low hills offer exquisite views over the countryside. There’s walking to suit all ages and tastes. Some glorious countryside with rolling farmland, lush woods, and grassy hills can be reached within an hour’s drive of Edinburgh and Glasgow. -
Mountains and the People Project Delivers
Spring/Summer 2019 | No. 23 The The magazine of the Friends of Loch Lomond and the Trossachs Mountains and the People Project Delivers ALSO INSIDE Park News, Friends Updates, Mountains and the People, Events, Nature of the Park and more THIS ISSUE: TheVoiceSpring2019V1.indd 1 17/03/2019 19:39 ENJOY FRESH LOCAL PRODUCE Join us for seasonal menus with locally sourced ingredients, The finest Scottish seafood, served alongside a splendid a fantastic wine list and hand-pulled craft ales. wine list created by expert Matthew Jukes. 01436 860420 lochlomondarmshotel.com 01436 860420 luss-seafoodbar.com LOCH LOMOND ARMS HOTEL MAIN ROAD LUSS G83 8NY LUSS SEAFOOD BAR PIER ROAD LUSS SCOTLAND G83 8NY Traffic Design Consultants Email: [email protected] 1048 Govan Road, Web: www.traffic-design.co.uk Glasgow, G51 4XS Co. No. SC 210509 Tel: 0141 445 2174 VAT No. 829 372796 Loch Lomond Adventures Logo concepts - Logo option 4 - colour Suggestion for how colours could look. Subtle colours. 5* holiday park on the shores of Loch Lomond Book your adventure now at inverbeg.com T. 01436 860 267 [email protected] Join us on a BIKES GUIDED WALKS magical adventure through KAYAK & CANOE BOAT TICKETS the beautiful woodlands SPEEDBOAT CANYONING around Luss Village WATERSPORTS 4x4 ADVENTURE LOCH LOMOND FAERIE TRAIL, LUSS, G83 8PA LUSS CARPARK www.lochlomondfaerietrail.com WWW.LOCHLOMONDADVENTURES.COM 2 The Voice - Spring/Summer 2019 TheVoiceSpring2019V1.indd 2 17/03/2019 19:39 Chairman’s Introduction WELCOME TO THIS SPRING EDITION OF VOICE, which features interesting articles about different aspects of the Loch Lomond and The Trossachs National Park and news on recent activities of the Friends and others working to make the Park a better place for people and nature. -
Site Condition Monitoring for Otters (Lutra Lutra) in 2011-12
Scottish Natural Heritage Commissioned Report No. 521 Site condition monitoring for otters (Lutra lutra) in 2011-12 COMMISSIONED REPORT Commissioned Report No. 521 Site condition monitoring for otters (Lutra lutra) in 2011-12 For further information on this report please contact: Rob Raynor Scottish Natural Heritage Great Glen House INVERNESS IV3 8NW Telephone: 01463 725000 E-mail: [email protected] This report should be quoted as: Findlay, M., Alexander, L. & Macleod, C. 2015. Site condition monitoring for otters (Lutra lutra) in 2011-12. Scottish Natural Heritage Commissioned Report No. 521. This report, or any part of it, should not be reproduced without the permission of Scottish Natural Heritage. This permission will not be withheld unreasonably. The views expressed by the author(s) of this report should not be taken as the views and policies of Scottish Natural Heritage. © Scottish Natural Heritage 2015. COMMISSIONED REPORT Summary Site condition monitoring for otters (Lutra lutra) in 2011-12 Commissioned Report No. 521 Project No: 12557 and 13572 Contractor: Findlay Ecology Services Ltd. Year of publication: 2015 Keywords Otter; Lutra lutra; monitoring; Special Area of Conservation. Background 44 Special Areas of Conservation (SACs) for which otter is a qualifying interest were surveyed during 2011 and 2012 to collect evidence to inform an assessment of the condition of each SAC. 73 sites outside the protected areas network were also surveyed. The combined data were used to look for trends in the recorded otter population in Scotland since the first survey of 1977-79. Using new thresholds for levels of occupancy, and other targets agreed with SNH for the current report, the authors assessed 34 SACs as being in favourable condition, and 10 sites were assessed to be in unfavourable condition. -
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. -
Paddlemore in Loch Lomond and the Trossachs a Guide for Canoes, Kayaks and Sups Paddlemore in Loch Lomond and the Trossachs a Guide for Canoes, Kayaks and Sups
PaddleMore in LochTrossachs PaddleMore Lomond and the PaddleMore in Loch Lomond and the Trossachs a guide for canoes, kayaks and sups PaddleMore in Loch Lomond and the Trossachs a guide for canoes, kayaks and sups Whether you want hardcore white water, multi-day touring Kilpatrick Tom & Dolier Grant trips or a relaxing afternoon exploring sheltered water with your family, you’ll find all that and much more in this book. Loch Lomond & The Trossachs National Park is long estab- lished as a playground for paddlers and attracts visitors from all over the world. Loch Lomond itself has over eighty kilometres of shoreline to explore, but there is so much more to the park. The twenty-two navigable lochs range from the vast sea lochs around Loch Long to small inland Loch Lomond bodies such as Loch Chon. & the Trossachs The rivers vary from relaxed meandering waterways like the Balvaig to the steep white water of the River Falloch and 9 781906 095765 everything in between. Cover – Family fun on Loch Earn | PaddleMore Back cover – Chatting to the locals, River Balvaig | PaddleMore Grant Dolier & Tom Kilpatrick Loch an Daimh Loch Tulla Loch Also available from Pesda Press Bridge of Orchy Lyon Loch Etive Loch Tay Killin 21b Tyndrum River Dochart River Loch 21a Fillan Iubhair Loch Awe 20 LOCH LOMOND & Crianlarich Loch Lochearnhead Dochart THE TROSSACHS 19 Loch NATIONAL PARK Earn Loch 5 River Doine 17 River Falloch Loch 32 Voil Balvaig 23 Ardlui 18 Loch Loch Sloy Lubnaig Loch Loch Katrine Arklet 12 Glen Finglas Garbh 3 10 Reservoir Uisge 22 Callander -
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. -
Self Guided View Trip Dates the West Highland Way Book Now
Self Guided View Trip Dates The West Highland Way Book Now Trip Grade: Blue 6 Point to Point The West Highland Way The West Highland Way is a classic long distance walk, covering 152 kilometres (95 miles) from Milngavie on the outskirts of Glasgow, to Fort William in the Highlands. The route travels past the bonnie banks of Loch Lomond, across the atmospheric Rannoch Moor, past dramatic Glencoe and onwards to finish at the foot of Ben Nevis, Britain’s highest mountain. The West Highland Way is one of the classic treks of the world and is undertaken by many people of all ages from across the world, making it a fun and social trek. On this self- guided walk we arrange your accommodation each evening and baggage transfer, as well as providing you with detailed route notes and maps so that you get the most out of this wonderful trek. Highlights • Take on the challenge of Scotland’s most famous and one of the world’s greatest long distance trails - the West Highland Way. • Immerse yourself in the spectacular scenery as you walk through the beautiful landscapes of Loch Lomond, Rannoch Moor and Glencoe. • We will arrange all accommodation, luggage transfer and provide you with maps and comprehensive route notes. Book with confidence • You pick the dates that suit you – we make all the arrangements required. PLEASE NOTE – The itinerary may be subject to change at the discretion of the Wilderness Scotland Guide with regard to weather conditions and other factors. Planned Itinerary Day 1 | Arrive in Milngavie Day 2 | Milngavie to Drymen Day 3 | Drymen to Rowardennan Day 4 | Rowardennan to Inverarnan Day 5 | Inverarnan to Tyndrum Day 6 | Tyndrum to Glencoe* Day 7 | Glencoe to Kinlochleven Day 8 | Kinlochleven to Fort William Day 9 | Fort William and Depart Arrival Info Make your own transport arrangements to Milngavie and your first nights accommodation Departure Info From Fort William depart for home or onward travel after breakfast the day after completing the hike. -
Provisii)Nal Atlas of the Mammals
I I T PROVISII)NALATLAS I I OFTHE T MAMMALS I OFTHE BRITISH ISLES I I I Edited for the MammalSociety by I Henry R.ARNOLD I I NaturalEnvironment Research Council, The Instituteof TerrestrialEcology, t MonksWood Experimental Station, AbbotsRipton, I Huntingdon, T I 1978 I f,3.00 rsBN 0-9042A2-19-a I Producedby the Biological RecordsCentre, Institute of Te.rBstrialEcology under contract to the Nature ConservancyCouncil Copyright tsBN0.004282.19€ I INTRODUCTION In 1965the MammalSociety began the collectionof mammaldistribution records on a 10 km. squarebasis. The recordingscheme was co-ord inated by Dr G B Corbetat the British Museumof I Nitural History. In 1971a setof provisionaldistribution maps was published in MammalRetuiew (Corbet1971)io providea statementof distributionas then knownand to stimulatefurther recording I by showingiust how muchremained to be done. The dataused to producethe 1971maps have been transferred to MonksWood and will be entered into the BiologicalRecords Centre national data bank. The presentset of mapshas been prepared as a secondprogress report and a furtherstimulus to recording.The mapsare stillvery muchprovisional, I particularlythose of the smallermammals. I ACKNOWLEDGEMENTS I My primedebt is to Dr G B Corbet,who laid the foundationsfor this setof mapswith the work he did on the fifst ten yearsof the Survey, lam alsograteful tothe many recorders,both within andwithoutthe MammalSociety, who have continued to sendin records. I havealso receivedinvaluable assistance from the organisersof specialsurveys and the I Group referees:-Dr S Harris(Harvest Mice), Dr P Chanin(Otters), Miss E Hurrell(Dormice), M Clarke(Deer), R W Vaughan(Seals), E D Clementsand MissFarquharson (Badgers), and Dr R E Stebbings(Bats). -
Draft Management Plan for Loch Lomond NNR 2018-2028
Draft Management Plan for Loch Lomond NNR 2018-2028 PLAN DETAILS Start 01-APR-2018 End 31-MAR-2028 Site description Loch Lomond National Nature Reserve (NNR) lies in the southeast corner of Loch Lomond, in the southern part of the Loch Lomond and Trossachs National Park. Loch Lomond NNR as a whole is 430 hectares (ha) in size and is incredibly diverse. The reserve includes some of the woodlands for which Loch Lomond is renowned, including the wooded shores on the mainland, the islands of Inchcailloch, Clairinsh, Torrinch, Creinch and Aber Isle, and the wetlands at the mouth of the River Endrick. Oak woodlands cover the islands, and a mosaic of open water, wetland, grassland and woodland habitats occupy the Mainland. The diversity is high because of its geographical position; it sits on the dividing line between the Highlands and Lowlands so habitats and species at the limits of both their northern and southern ranges in Britain are found here. The climate at Loch Lomond is relatively oceanic with mild winters. The importance of the reserve is reflected by the number of habitats and species which are either legally protected or are covered by Biodiversity Action Plans. People have managed these habitats for a variety of different purposes over the centuries, but today these wonderful woodlands and wetlands are managed primarily for wildlife and for people to enjoy. Scottish Natural Heritage managed the whole reserve up to 2004 when the Loch Lomond and Trossachs National Park took on the management of Inchcailloch. In 2012 RSPB Scotland purchased the Wards estate on the south side of the Endrick and now manage this as the RSPB Loch Lomond part of the Loch Lomond NNR.