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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.
289:
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, but it was in turn deprecated in 1994 in favour of the
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249:. It comprises a complex of vertically and laterally varying gravels, sands, silts and clays deposited between 56-55 million years before present during the
424:
712:
373:
653:
707:
673:
Bedrock geology UK south. An explanation of the bedrock geology map of
England and Wales – 1:625,000 fifth edition
376:
sands with marine fossils occurs in east Kent. Where it rests on the Thanet beds it is an argillaceous greensand with rounded
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717:
616:
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473:. Bricks, tiles and coarse pottery and occasionally firebricks have been made from the clay beds in this formation.
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330:. They are found in the north of the London Basin, mid-west of the Thames Basin and in the Hampshire Basin.
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pebbly conglomerate in a siliceous matrix. The fossils, estuarine, freshwater and marine, include
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260:). It is found throughout the London Basin with a thickness between 10m and 30m, and the
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361:. At the base of the shell-rich clayer lay in southeast London are pebble beds and
662:
Hight, D.W.; Ellison, R.A.; Page, D.P. (2004). "Engineering in the
Lambeth Group".
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298:, to conform with new standards and to allow scope for more detailed subdivisions.
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and sands, here and there with pebbly beds and masses of fine sand converted into
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Exposure in
Gilbert's Pit. Dark grey clays, and light grey shelly clays of the
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657:. Vol. 28 (11th ed.). Cambridge University Press. p. 819.
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it is more clayey and the flints are less rounded and are green-coated.
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This article incorporates text from a publication now in the
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shells comprise a great deal, in places including a well-marked
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is a distinctive rock from near the base of the formation; a
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Construction
Industry Research and Information Association
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The formation was first known as the
Plastic Clay by
675:. Keyworth, Nottingham: British Geological Survey.
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62:overlying yellow-brown weathering sands of the
485:Basin, the Lambeth Group usually rests on the
392:the Reading Formation appears on the coast at
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345:bed (strata). It overspills borders of west
349:, is found in edges of east Kent, in south
52:
617:Learn how and when to remove this message
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580:This article includes a list of general
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713:Geological groups of the United Kingdom
14:
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277:in 1816 after the Argile plastique of
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306:The Lambeth Group consists of three
285:. It was called the Mottled Clay by
337:: grey clays and pale sands, often
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586:it lacks sufficient corresponding
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318:: a series of lenticular mottled
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396:and at other points inland. The
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517:. It is usually covered by the
380:pebbles; where it rests on the
708:Geologic formations of England
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326:. These beds are generally un
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718:Paleocene Series of Europe
477:Stratigraphic relationship
398:Hertfordshire puddingstone
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649:Woolwich-and-Reading Beds
296:British Geological Survey
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654:Encyclopædia Britannica
601:more precise citations.
671:Jackson, A.A. (2007).
493:, but is found on the
440:(Melanatria) inquinata
233:, a set of geological
449:, and the remains of
738:Geology of Hampshire
231:stratigraphic group
38:Stratigraphic range
335:Woolwich Formation
93:Woolwich Formation
60:Woolwich Formation
743:Geology of London
723:Paleogene England
682:978-0-85272-586-3
627:
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519:Harwich Formation
467:) and the mammal
425:Viva parus lentus
372:: light-coloured
316:Reading Formation
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89:Reading Formation
16:(Redirected from
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487:Thanet Formation
287:Joseph Prestwich
243:Hampshire Basins
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370:Upnor Formation
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262:Hampshire Basin
218:Hampshire Basin
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666:(Report C583).
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283:A. Brongniart
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527:Thames Group
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394:Studland Bay
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374:false-bedded
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245:of southern
226:
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214:London Basin
170:Conglomerate
103:Thames Group
26:
18:Reading Beds
599:introducing
495:Chalk Group
420:bellovacina
409:cuneiformis
302:Subdivision
235:rock strata
117:Chalk Group
113:Thanet Sand
702:Categories
582:references
563:References
507:Hungerford
470:Coryphodon
455:crocodiles
308:formations
275:T. Webster
126:Up to 39 m
691:243694452
523:formation
483:Hampshire
464:Gastornis
461:, birds (
433:hemistoma
431:Planorbis
407:Corbicula
339:estuarine
324:sandstone
184:southern
166:Sandstone
158:Limestone
131:Lithology
123:Thickness
99:Underlies
81:Sub-units
42:Thanetian
511:Hertford
503:Charlton
447:globulus
445:Neritina
363:lignitic
355:Newhaven
251:Ypresian
176:Location
109:Overlies
46:Ypresian
642::
595:improve
525:of the
515:Reading
499:Bromley
489:of the
451:turtles
438:Melania
365:layers.
353:and at
294:by the
269:History
256:(lower
247:England
237:in the
192:Country
186:England
162:Lignite
136:Primary
689:
679:
636:
584:, but
459:sharks
418:Ostrea
390:Dorset
359:Sussex
343:oyster
258:Eocene
239:London
210:Extent
201:
181:Region
154:Gravel
533:Notes
497:near
402:flint
382:chalk
378:flint
351:Essex
320:clays
229:is a
146:Other
75:Group
687:OCLC
677:ISBN
513:and
368:The
347:Kent
333:The
314:The
281:and
241:and
225:The
216:and
150:Sand
140:Clay
71:Type
651:".
388:In
310::
254:age
704::
685:.
541:^
529:.
509:,
505:,
501:,
457:,
453:,
442:,
435:,
428:,
422:,
415:,
411:,
357:,
204:UK
168:,
164:,
160:,
156:,
152:,
115:,
91:,
87:,
40::
693:.
620:)
614:(
609:)
605:(
591:.
555:.
44:-
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.