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Geodiversity of the Loch Lomond and the Trossachs National Park

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Geodiversity of the Loch Lomond and the Trossachs National Park Geodiversity of the Loch Lomond and The Trossachs National Park: Statement of Significance and Identification of Opportunities Geology and Landscape (Northern Britain) Programme Open File Report OR/07/036 BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE (NORTHERN BRITAIN) PROGRAMME OPEN FILE REPORT OR/07/036 Geodiversity of the Loch Lomond and The Trossachs National Park: Statement of Significance and Identification of Opportunities K M Goodenough, A Finlayson and H F Barron Front cover Loch Lomond from Duncryne Hill, showing the contrasting landscapes across the Highland Border. BGS photo P001223. Bibliographical reference GOODENOUGH, K M, FINLAYSON, A AND BARRON, H F. 2008. Geodiversity of the Loch Lomond and The Trossachs National Park: Statement of Significance and Identification of Opprtunities. British Geological Survey Open File Report, OR/07/036. 26pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and the authority that commissioned the work. Maps and diagrams in this report use topography based on Ordnance Survey mapping. © NERC 2008. All rights reserved Keyworth, Nottingham British Geological Survey 2008 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. email [email protected] We publish an annual catalogue of our maps and other publications; this catalogue is available online or from any of the Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG BGS shops. Tel 0115 936 3241 Fax 0115 936 3488 email [email protected] The British Geological Survey carries out the geological survey of Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the Murchison House, West Mains Road, Edinburgh EH9 3LA surrounding continental shelf, as well as basic research projects. Tel 0131 667 1000 Fax 0131 668 2683 It also undertakes programmes of technical aid in geology in email [email protected] developing countries. The British Geological Survey is a component body of the Natural Environment Research Council. London Information Office at the Natural History Museum (Earth Galleries), Exhibition Road, South Kensington, London SW7 2DE Tel 020 7589 4090 Fax 020 7584 8270 Tel 020 7942 5344/45 email [email protected] Columbus House, Greenmeadow Springs, Tongwynlais, Cardiff CF15 7NE Tel 029 2052 1962 Fax 029 2052 1963 Forde House, Park Five Business Centre, Harrier Way, Sowton EX2 7HU Tel 01392 445271 Fax 01392 445371 Maclean Building, Crowmarsh Gifford, Wallingford OX10 8BB Tel 01491 838800 Fax 01491 692345 Geological Survey of Northern Ireland, Colby House, Stranmillis Court, Belfast BT9 5BF Tel 028 9038 8462 Fax 028 9038 8461 www.bgs.ac.uk/gsni/ Parent Body Natural Environment Research Council, Polaris House, North Star Avenue, Swindon SN2 1EU Tel 01793 411500 Fax 01793 411501 www.nerc.ac.uk Website www.bgs.ac.uk Shop online at www.geologyshop.com Created on 21/01/2008 09:16:00 Acknowledgements Mike Browne, Graham Leslie, Nick Golledge, and Chris Thomas, all of BGS, provided valuable advice on aspects of this report. Contents Acknowledgements........................................................................................................................ 1 Contents.......................................................................................................................................... 1 1 Introduction............................................................................................................................ 2 2 Geological history of the National Park............................................................................... 2 3 Key bedrock features and localities in the National Park.................................................. 7 3.1 The Dalradian Supergroup.............................................................................................. 7 3.2 The Highland Border ...................................................................................................... 8 3.3 Mineralisation................................................................................................................. 9 3.4 Igneous rocks.................................................................................................................. 9 3.5 Devonian sedimentary rocks........................................................................................... 9 4 Key geomorphological features and localities in the National Park................................ 10 5 Suggestions for geological management in the National Park......................................... 13 5.1 Geodiversity Sites......................................................................................................... 13 5.2 Geodiversity and Planning............................................................................................ 14 5.3 Management Issues....................................................................................................... 15 5.4 Geodiversity Audit........................................................................................................ 18 6 Opportunities for interpretation of geodiversity in the National Park........................... 18 6.1 Single localities for fixed interpretation ....................................................................... 19 6.2 Suggested walking routes that would benefit from geological interpretation .............. 20 7 Further Reading................................................................................................................... 21 Appendix 1 Geological Conservation Review sites in the National Park......................... 22 1 Created on 21/01/2008 09:16:00 1 Introduction The natural beauty and striking landscapes of the Loch Lomond and The Trossachs National Park are a direct product of its geological history. A major landscape feature within the Park is the Highland Border, which separates the rugged peaks and deep glens of the Highlands from the lower, rolling hills and broad straths of the Lowlands. This landscape feature follows a geological structure known as the Highland Boundary fault zone, which separates ancient Precambrian metamorphic rocks in the Highlands from younger, softer, sedimentary rocks to the south. These geological differences have been exploited over time by the erosive power of wind, water and ice to produce the present-day landscape of the National Park. This report has been prepared for the Loch Lomond and The Trossachs National Park authority, to provide an overview of the park’s geodiversity. Section 2 of the report describes the geological history of the National Park. Sections 3 and 4 pick out key localities of interest for their geology and geomorphology, and opportunities for management and interpretation of the park’s geological heritage are discussed in sections 5 and 6. 2 Geological history of the National Park The geological history of the Loch Lomond and The Trossachs National Park begins around 700 million years ago, in the Precambrian era. At that time, Scotland lay within a major supercontinent, which was positioned close to the South Pole. However, then as now, continents could move gradually across the Earth’s surface through the process of plate tectonics. Such tectonic processes led to the crust of the supercontinent being gradually stretched and thinned, until eventually it split, and a new ocean began to grow. This is known as the Iapetus Ocean, and it separated Laurentia (a continent containing Scotland, Greenland and parts of North America) from the continent of Gondwana to the south. The continent of Laurentia moved northwards as the Iapetus Ocean widened. Around the margins of the continent, sediments were laid down on the ocean floor; these sediments would eventually become the rocks of the ‘Highland’ part of the Loch Lomond and The Trossachs National Park. In Scotland, the rocks that were originally deposited in the developing Iapetus Ocean are known as the Dalradian Supergroup. They underlie the southern and central Highlands, extending from the Great Glen in the north to the Highland Border in the south. The oldest rocks in the National Park belong to the earlier part of the Dalradian Supergroup; most of them are part of a unit known as the Argyll Group. They occur along the park’s northern margin, from Ben Lui to Killin, and they also stretch southwards along Glen Ogle to Loch Lubnaig. These rocks were originally formed as sands and muds, deposited on the sea-bed before 600 million years ago. 600 million years ago, sub-sea volcanic eruptions culminated in the development of new ocean floor and signalled the final split of Laurentia from Gondwana. Some of the volcanic rocks formed at this time are commonly associated with limestones, which were laid down in relatively shallow waters, and they form a marker unit that runs along the north side of Glen Dochart, then southwards towards Strathyre. This unit is known as the Loch Tay Limestone Formation. Associated with the volcanic activity were submarine hot springs, through which mineral-rich, heated fluids circulated to form mineral deposits within the older
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