Exposure in Gilbert's Pit. Dark grey clays, and light grey shelly clays of the Woolwich Formation overlying yellow-brown weathering sands of the Upnor Formation
The Lambeth Group is a stratigraphic group, a set of geological rock strata in the London and Hampshirebasins of southern England. It comprises a complex of vertically and laterally varying gravels, sands, silts and clays deposited between 56-55 million years before present during the Ypresianage (lower Eocene). It is found throughout the London Basin with a thickness between 10m and 30m, and the Hampshire Basin with a thickness between 50m and less than 25m. Although this sequence only crops out in these basins, the fact that it underlies 25% of London at a depth of less than 30m means the formation is of engineering interest for tunnelling and foundations.
History
The formation was first known as the Plastic Clay by Thomas Webster in 1816 after the Argile plastique of Georges Cuvier and Alexandre Brongniart. It was called the Mottled Clay by Joseph Prestwich in 1846, but in 1853 he proposed the name Woolwich-and-Reading Beds to emphasise the differing local aspects of the series.[1] This name received widespread usage, but it was in turn deprecated in 1994 in favour of the Lambeth Group by the British Geological Survey, to conform with new standards and to allow scope for more detailed subdivisions.
The Reading Formation: a series of lenticular mottled clays and sands, here and there with pebbly beds and masses of fine sand converted into sandstone. These beds are generally unfossiliferous.[citation needed] They are found in the north of the London Basin, mid-west of the Thames Basin and in the Hampshire Basin.
The Woolwich Formation: grey clays and pale sands, often estuarine shells comprise a great deal, in places including a well-marked oyster bed (strata). It overspills borders of west Kent, is found in edges of east Kent, in south Essex and at Newhaven, Sussex. At the base of the shell-rich clayer lay in southeast London are pebble beds and lignitic layers.
The Upnor Formation: light-coloured false-bedded sands with marine fossils occurs in east Kent. Where it rests on the Thanet beds it is an argillaceous greensand with rounded flint pebbles; where it rests on the chalk it is more clayey and the flints are less rounded and are green-coated.[1]
In Dorset the Reading Formation appears on the coast at Studland Bay and at other points inland. The Hertfordshire puddingstone is a distinctive rock from near the base of the formation; a flint pebbly conglomerate in a siliceous matrix. The fossils, estuarine, freshwater and marine, include Corbicula cuneiformis, C. tellinella, Ostrea bellovacina, Viva parus lentus, Planorbis hemistoma, Melania (Melanatria) inquinata, Neritina globulus, and the remains of turtles, crocodiles, sharks, birds (Gastornis) and the mammal Coryphodon. Bricks, tiles and coarse pottery and occasionally firebricks have been made from the clay beds in this formation.[1]
Hight, D.W.; Ellison, R.A.; Page, D.P. (2004). "Engineering in the Lambeth Group". Construction Industry Research and Information Association (Report C583).
Jackson, A.A. (2007). Bedrock geology UK south. An explanation of the bedrock geology map of England and Wales – 1:625,000 fifth edition. Keyworth, Nottingham: British Geological Survey. ISBN978-0-85272-586-3. OCLC243694452.
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