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From Wikipedia, the free encyclopedia

Lambeth Group
Type Group
Age Thanetian-Ypresian
Underlies Thames Group
Overlies Thanet Sand, Chalk Group
Region southern England

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 (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. Surface outcrops are present only on the outskirts of these, however, that the Lambeth Group underlies some 25% of London at a depth of less than 30m means the formation is of great engineering interest for tunnelling and foundations.



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 J. 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 in order to conform with new standards and to allow scope for more detailed subdivisions.


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 sand converted into quartzite. 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 full of estuarine shells 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 Woolwich Formation 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-colored 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 (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.

Stratigraphic relationship

Except in the Hampshire basin the Lambeth Group usually rests on the Thanet Sand Formation, but they are found on the Chalk Group near Bromley, Charlton, Hungerford, Hertford, Reading, etc. It is usually covered by the Harwich Formation, the oldest formation of the Thames Group.


  • This article incorporates text from the Encyclopædia Britannica, Eleventh Edition, a publication now in the public domain.
  • 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.; 2008: Bedrock Geology UK South. An explanation of the bedrock geology map of England and Wales - 1:625,000 fifth edition, British Geological Survey, ISBN 978-085272-586-3.

Redirecting to Lambeth Group

1911 encyclopedia

Up to date as of January 14, 2010

From LoveToKnow 1911

READING BEDS, in geology, a series of marine and estuarine beds consisting of variegated plastic clays and bright-coloured sands, which form, with the Woolwich beds, a subdivision of the Lower Eocene (see Woolwich And Reading Beds).

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