Lyell Collection

Quarterly Journal of Engineering Geology and Hydrogeology

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Winter, M.G.
Right arrow Articles by Macgregor, F.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Quarterly Journal of Engineering Geology and Hydrogeology; 2006; v. 39; issue.1; p. 73-78;
DOI: 10.1144/1470-9236/05-049
© 2006 Geological Society of London

Photographic Feature

Scottish debris flow events of August 2004

M.G. Winter1, A.P. Heald2, J.A. Parsons2, L. Shackman3 & F. Macgregor4

1 1TRL Limited, Sighthill Campus, Sighthill Court, Edinburgh, EH11 4BN, United Kingdom.(e-mail: mwinter@trl.co.uk)
2 2Jacobs Babtie, 95 Bothwell Street, Glasgow, G2 7HX. United Kingdom.
3 3Scottish Executive, Victoria Quay, Edinburgh, EH6 6QQ, United Kingdom.
4 4Consultant to the Scottish Executive, Victoria Quay, Edinburgh, EH6 6QQ, United Kingdom.

Received for publication 15 September 2005. Accepted for publication 13 October 2005.

The first 250 words of the full text of this article appear below. Images appear only in PDF or full-text views.


    Introduction
 
In August 2004 Scotland experienced rainfall substantially in excess of the norm. Some areas of Scotland received more than 300% of the 30-year average August rainfall, while in the Perth & Kinross area figures of the order of between 250% and 300% were typical. Although the percentage rainfall during August reduced to the west, parts of Stirling and Argyll & Bute still received between 200% and 250% of the monthly average (Source: http://www.metoffice.com/climate/uk/2004/august/maps.html). The 30-year average rainfall for August in Scotland varies between 67 mm on the east coast and 150 mm in the west of Scotland (Anon 1989).

The rainfall was both intense and long lasting and a large number of landslides, in the form of debris flows, were experienced in the hills of Scotland. A small number of these intersected the trunk or strategic, road network, notably the A83 between Glen Kinglas and to the north of Cairndow (9 August), the A9 to the north of Dunkeld (11 August), and the A85 at Glen Ogle (18 August). These locations are illustrated in Figure 1.


Figure Removed (Available Only in the Full Text)
View larger version (46K):
[in this window]
[in a new window]
 
Fig. 1 Map showing the trunk and motorway network in Scotland (© Crown Copyright). The locations of the three main debris flow event areas in Scotland in August 2004 are also shown.

 
While there were no major injuries to those affected, 57 people had to be airlifted to safety when they became trapped between the two main debris flows at Glen Ogle. However, the real impacts of the events were economic and social, . . . [Full Text of this Article]