SITE INVESTIGATION

BGS uncovers Britain's ancient valleys

Hundreds of ancient valleys buried beneath the surface of Great Britain have now been mapped for the first time by the British Geological Survey (BGS).

 A stylised example of a buried valley mapped by the British Geological Survey

A stylised example of a buried valley mapped by the British Geological Survey

The buried valleys occur across Britain, from a 162m deep valley in Grangemouth, Scotland, to a 22km long valley under Melton Mowbray, Leicestershire and a 50m deep valley under Swansea.

The valleys mostly date from the last ice age, which ended around 11,500 years ago, and are ancient drainage networks from rivers and glaciers that over the years have become partly or completely buried by more recent sediments.

Sometimes a part of the valley peeks above the surface, but more often than not they are completely hidden underground, with no way for hydrologists, civil engineers, planners or construction companies to tell what lies beneath.

BGS first identified a hidden valley in the 1870s, under the river Mersey, and since then has been collecting data from thousands of boreholes across Britain.

The digital age brought a new opportunity to collect and collate all the buried valley data in one place and make it publicly available online.

Dr Tim Kearsey, the BGS geologist who has been leading the project, said: "Britain's buried valleys might be underground, but they could and have had a huge impact on what happens above the surface.

"We need to know where these buried valleys are for a number of reasons. They could be a target area for shallow geothermal energy, like in Cardiff. They could be unsuitable places for skyscrapers or bridges to be constructed. They cause problems for groundwater supplies, as they already do in south-east England.

"We combined historical BGS survey activities with over 200,000 borehole records from our national borehole database to identify these previously hidden features across the UK.

"The buried valleys are all across Britain. The whole of the Cheshire basin looks flat as a pancake, but it has lots of features underneath it. These probably formed under an ice sheet that covered the area some 23,000 years ago.

"The deepest system is in the middle of Scotland, under Grangemouth. It's over 162m deep and absolutely full of clay.

"Now that we know where they are, the next stage of the work is to find out what's in all of them, and whether they could be useful for providing geothermal energy or as a groundwater source for the whisky or manufacturing sectors."

The Buried Valleys dataset is online at www.bgs.ac.uk.

 

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