The Lambeth Group is a stratigraphic group, a set of geological rock strata in the London and Hampshire Basins 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 Ypresian age. 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 on the edges of these basins, the fact that the Lambeth Group underlies some 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 T. Webster in 1816 after the Argile plastique of Georges Cuvier and A. 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. This name received widespread usage, however, has in turn been recently 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.
Subdivision
The Lambeth Group consists of three formations:
The Reading Formation, a series of lenticular mottled clays and sands, here and there with pebbly beds and masses of fine sandconverted into sandstone. These beds are generally unfossiliferous. They are found in the north and west portions of the London Basin and in the Hampshire Basin.
The Woolwich Formation, grey clays and pale sands, often estuarine shells comprise a very substsantial component and in places with a well-marked oyster bed. At the base of the shell-bearing clays in southeast London there are pebble beds and lignitic layers. The WoolwichFormation occurs in west Kent, the east borders of Surrey, the borders of east Kent, in south Essex and at Newhaven in Sussex.
The Upnor Formation, consisting of 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.
In Dorset the Reading Formation appears on the coast at Studland Bay and at other points inland. The Hertfordshire puddingstone is a well-known rock from near the base of the formation; it is 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 inquinata, Neritina globulus, and the remains of turtles, crocodiles, sharks, birds and the mammal Coryphodon. Bricks, tiles and coarse pottery and occasionally firebricks have been made from the clay beds in this formation.
