North West England and South West Scotland - November 2009 flooding
The British Geological Survey took to the air on 20 November 2009 in the aftermath of the flooding, which devastated homes and businesses in the North West England and South West Scotland, to find out how modern flooding compares to ancient flood areas. BGS photographer Fergus MacTaggart observed flooding from 600m (2000 ft) as he flew over the worst affected areas around Cockermouth, Lockerbie, Dumfries and Workington.
Why do geological maps reflect areas prone to flooding?
Areas which have been flooded in the past have deposits of clay, silt and sand left by the flood water. These areas are called floodplains and coastal plains and can be extracted from geological maps indicating areas with a potential to flood in the future.
More photographs and information on geology and flooding
Cockermouth
The River Annan at Shillahill Bridge, A709, WSW of Lockerbie
Dumfries
The Geological Indicators of Flooding Team have compared photographs from the flight with the new BGS Geological Indicators of Flooding Map. A comparison of the photograph and geological maps shows a correlation between areas which have flooded and areas marked as alluvial deposits (with a potential to flood).
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