See also:LONDON See also:CLAY
, in See also:geology, the most important member of the See also:Lower See also:Eocene strata in the See also:south of See also:England
.
It is well See also:developed in the See also:London See also:basin, though not frequently exposed, partly because it is to a See also:great extent covered by more See also:recent gravels and partly because it is not often worked on a large See also:scale
.
It is a stiff, tenacious, bluish See also:clay that becomes See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
brown on weathering, occasionally it becomes distinctly sandy, some-times glauconitic, especially towards the See also:top; large calcareous septarian concretions are See also:common, and have been used in the manufacture of See also:cement, being dug for this purpose at See also:Sheppey, near Southend, and at See also:Harwich, and dredged off the See also:Hampshire See also:coast
.
Nodular lumps of See also:pyrites and crystals of selenite are of frequent occurrence
.
The clay has been employed for making bricks, tiles and coarse pottery, but it is usually too tenacious for this purpose except in well-weathered or sandy portions
.
The See also:base of the clay is very regularly indicated by a few inches of rounded See also:flint pebbles with See also:green and yellowish See also:sand, parts of this layer being frequently cemented by carbonate of See also:lime
.
The See also:average thickness of the London Clay in the London basin is about 450 ft.; at See also:Windsor it is 400 ft. thick; beneath London it is rather thicker, while in the south of See also:Essex it is over 48o ft
.
In See also:Wiltshire it only reaches a few feet in thickness, while in See also:Berkshire it is some 50 or 6o ft
.
It is found in the Isle of See also:Wight, where it is 300 ft. thick at Whitecliff See also:Bay—here the beds are See also:vertical and even slightly reversed—and in See also:Alum Bay it is 220 ft. thick
.
In Hampshire it is sometimes known as the See also:Bognor Beds, and certain layers of calcareous See also:sandstone within the See also:clays are called See also:Barnes or Bognor See also:Rock
.
In the eastern See also:part of the London basin in See also:east See also:Kent the pebbly
the Oldhaven and See also:Blackheath Beds
.
The London Clay is a marine See also:deposit, and its fossils indicate a moderately warm See also:climate, the See also:flora having a tropical aspect
.
Among the fossils may be mentioned Panopoea intermedia, Ditrupa Plana, Teredina personata, Conus concinnus, Rostellaria ampla, See also:Nautilus centralis, Belosepia, See also:foraminifera and diatoms
.
See also:Fish remains include Otodus obliquus, Sphyroenodus crassidens; birds are represented by Halcyornis Toliapicus, Lithornis and Odontopteryx, and See also:reptiles by Chelone gigas, and other turtles, Palaeophis, a See also:serpent and crocodiles
.
Hyracotherium leporinum, See also:Palaeotherium and a few other mammals are recorded
.
Plant remains in a pyritized See also:condition are found in great abundance and perfection on the See also:shore of Sheppey; numerous See also:species of palms, See also:- SCREW (O.E. scrue, from O. Fr. escroue, mod. ecrou; ultimate origin uncertain; the word, or a similar one, appears in Teutonic languages, cf. Ger. Schraube, Dan. skrue, but Skeat, following Diaz, finds the origin in Lat. scrobs, a ditch, hole, particularl
screw pines, See also:water lilies, cypresses, yews, leguminous See also:plants and many others occur; logs of coniferous See also:wood bored through by annelids and See also:Teredo are common, and fossil See also:resin has been found at See also:Highgate
.
See EOCENE ; also W
.
See also:Whitaker, " The Geology of London and part of the See also:Thames Valley," Mem
.
Geol
.
Survey (1889)., and See also:Sheet See also:Memoirs of the Geol
.
Survey, London, Nos
.
314, 315, 268, 329, 332, and Memoirs on the Geology of the Isle of Wight (1889)
.
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