The Parallel Roads of Glen Roy, Scotland : geoconservation history and challenges
MetadataShow full item record
Glen Roy is a classic geosite for ice-dammed lake shorelines, the Parallel Roads, and associated features formed during the Loch Lomond (Younger Dryas) Stade (12.9–11.7 ka). The area played a key part in the development of the glacial theory in the early 19th century and continues today to have outstanding scientific value for understanding the processes and timing of events at the end of the last glaciation. Glen Roy has also been long-appreciated as an awe-inspiring visitor attraction, and is now a flagship site for geotourism within Lochaber Geopark. Statutory geoconservation in Glen Roy, beginning in the second half of the 20th century, was founded on the exceptional scientific value of the area. The history and practice of geoconservation in Glen Roy illustrate the contested values of geoheritage and the evolving approaches adopted. Important lessons include the need for open dialogue and partnership working among the local community, land owners and managers, the statutory conservation agency (Scottish Natural Heritage), Lochaber Geopark and the scientific community.
Brazier , V , Gordon , J E , Faulkner , M , Warner , D , Hoole , K & Blair , J 2017 , ' The Parallel Roads of Glen Roy, Scotland : geoconservation history and challenges ' Proceedings of the Geologists' Association , vol. 128 , no. 1 , pp. 151-162 . https://doi.org/10.1016/j.pgeola.2016.11.008
Proceedings of the Geologists' Association
© 2017 Elsevier Ltd. All rights reserved. This work has been made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1016/j.pgeola.2016.11.008
Items in the St Andrews Research Repository are protected by copyright, with all rights reserved, unless otherwise indicated.