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Scottish Road Network Landslides Study - University of Glasgow

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32<br />

INFORMATION SOURCES<br />

Second, information on past landslide locations that have affected the road network, their type<br />

<strong>of</strong> movement, their date <strong>of</strong> occurrence and, if relevant, reactivation dates may help to identify<br />

sites <strong>of</strong> current landslide activity and the factors that control their occurrence under present<br />

climatic conditions. Such data are contained within geological maps, landslide databases,<br />

ground investigation reports, PhD theses, and papers in technical/scientific journals.<br />

3.3.1 Geological/Geotechnical Information<br />

The British Geological Survey (BGS) holds a large amount <strong>of</strong> geological, engineering<br />

geological and geotechnical data. These data are increasingly being held in digital form and<br />

are being accessed, viewed, analysed and presented using sophisticated computer systems<br />

(relational databases and Geographical Information Systems, or GIS) that enable them to be<br />

combined in different ways. Thus BGS <strong>of</strong>fers not only large relevant data holdings but also<br />

the ability to manipulate the data to user needs incorporating new types <strong>of</strong> data into the<br />

system as the need arises.<br />

6"/1:10,000 scale geological maps: The area covered by modern 1:10,000 scale and older<br />

1:10,560 scale maps is shown on Figures 3.1 and 3.2. However, this gives no indication <strong>of</strong> the<br />

geological content <strong>of</strong> each sheet. Every geological map is to some extent a personal product,<br />

with a content reflecting the experience and pr<strong>of</strong>essional interests <strong>of</strong> the geologist. The age <strong>of</strong><br />

the mapping is not necessarily a guide to content or quality. Primary survey field slips<br />

(1:10,560 scale) <strong>of</strong>ten contain a wealth <strong>of</strong> data compared to those produced during more<br />

modern mapping when a more focused and time constrained mapping style was the normal<br />

procedure.<br />

Figure 3.1 – Availability <strong>of</strong> 1:10,000 geological maps.

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