The Lambeth Group, formerly known as the Woolwich and Reading Beds, occurs in the London and Hampshire Basins, where it directly overlies the Chalk or Thanet Sand Formation, and is succeeded by the Harwich and London Clay Formations.
Although generally less than 50 m thick, its lithological variability and position beneath much of London has concerned tunnelling engineers since the early nineteenth century.
Geotechnical data from over 50 ground investigations, held in the National Geotechnical Properties Database have been analysed to assess the spatial variation in geotechnical properties across the main formations of the Lambeth Group. An example of the undrained shear strength with depth is presented below.
The BGS gratefully acknowledges the contribution made to parts of this study by Dr Jackie Skipper (Engineering Stratigrapher, Natural History Museum) based on her extensive experience of the Lambeth Group geology and its associated engineering problems.
The Engineering Geology of British Rocks and Soils: Lambeth Group provides an in-depth study of formations within the Lambeth Group using data held in the National Geotechnical Properties Database.
The geological, lithological, geotechnical, and mineralogical features within the Lambeth Group have been described in detail including applicable geophysical methods for ground investigation.
Entwisle, D C, Hobbs, P R N, Northmore, K J, Skipper, J, Raines, M R, Self, S J, Ellison, R A, Jones, L D. 2013. Engineering Geology of British Rocks and Soils: Lambeth Group. British Geological Survey Report, OR/13/006.
Jones, L D, and Hobbs, P R N. 2004. The shrinkage and swelling behaviour of UK soils: the clays of the Lambeth Group. British Geological Survey Report, RR/04/001.
Jones, L D. 2001. Determination of the shrinking and swelling properties of the clays of the Lambeth Group. British Geological Survey Report, IR/01/054.
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