Physical properties and behaviour of UK rocks and soils

As part of the Geo-engineering properties and processes team, the British Geological Survey is characterising UK geological formations in terms of their lithological and engineering properties. These properties can provide information on potential engineering behaviour, such as problem ground conditions and geological hazards. This information may be used to assist ground engineers and planners in undertaking feasibility studies and site investigation design for engineering projects and land-use planning for regional development.
All geotechnical data from these studies are stored in the National Geotechnical Properties Database.

Formations selected for study to date comprise:

  • Bedrock geological formations
  • The Gault Formation is susceptible to landsliding and severe shrink-swell problems.Download available.
  • The Mercia Mudstone Group underlies many major urban areas and can present problems in the construction of foundations, earthworks and tunnelling. Download available.
  • The Lambeth Group underlies much of London, has a complex stratigraphy and lithological variation, which, can constrain underground development.
  • The Lias Group underlies many major urban areas, is susceptible to landsliding and, in some areas, reacts with concrete to form thaumasite leading to weakening of buried concrete foundations

The work on the Mercia Mudstone and Lambeth Groups compliments reports published by CIRIA (the Construction Industry Research and Information Association). The BGS is a contributor to both CIRIA reports.

Map showing general distribution of
bedrock formations studied to date
Map showing general distribution of bedrock formations studied to date

Superficial deposits

Map showing general distribution of loessic brickearth.
Map showing general distribution of loessic brickearth.

Loessic brickearth occurs as irregular spreads mainly across southern and south-eastern England; in places, under engineering loads, it is prone to rapid ‘collapse’ settlement when saturated.

Glacial till is widespread across the UK north of the southern limits of the Anglian and Devensian glaciations. It is of markedly variable thickness, lithological composition and engineering behaviour.

Map showing extent of glaciations.
Map showing extent of glaciations.

For further information contact: enquiries@bgs.ac.uk