OXFORDIAN
, in See also:geology, the name given to a See also:series of strata in the See also:middle Oolites which occur between the See also:Corallian beds and the See also:Cornbrash; the See also:division is now taken to include the See also:- OXFORD
- OXFORD, EARLS OF
- OXFORD, EDWARD DE VERE, 17TH EARL
- OXFORD, JOHN DE VERE, 13TH EARL OF (1443-1513)
- OXFORD, PROVISIONS OF
- OXFORD, ROBERT DE VERE, 9TH EARL OF (1362-1392)
- OXFORD, ROBERT HARLEY, 1ST
Oxford See also:Clay with the underlying See also:Callovian See also:stage (q.v.)
.
The argillaceous beds were called " Clunch Clay and Shale " by See also:- WILLIAM
- WILLIAM (1143-1214)
- WILLIAM (1227-1256)
- WILLIAM (1J33-1584)
- WILLIAM (A.S. Wilhelm, O. Norse Vilhidlmr; O. H. Ger. Willahelm, Willahalm, M. H. Ger. Willehelm, Willehalm, Mod.Ger. Wilhelm; Du. Willem; O. Fr. Villalme, Mod. Fr. Guillaume; from " will," Goth. vilja, and " helm," Goth. hilms, Old Norse hidlmr, meaning
- WILLIAM (c. 1130-C. 1190)
- WILLIAM, 13TH
William See also:- SMITH
- SMITH, ADAM (1723–1790)
- SMITH, ALEXANDER (183o-1867)
- SMITH, ANDREW JACKSON (1815-1897)
- SMITH, CHARLES EMORY (1842–1908)
- SMITH, CHARLES FERGUSON (1807–1862)
- SMITH, CHARLOTTE (1749-1806)
- SMITH, COLVIN (1795—1875)
- SMITH, EDMUND KIRBY (1824-1893)
- SMITH, G
- SMITH, GEORGE (1789-1846)
- SMITH, GEORGE (184o-1876)
- SMITH, GEORGE ADAM (1856- )
- SMITH, GERRIT (1797–1874)
- SMITH, GOLDWIN (1823-191o)
- SMITH, HENRY BOYNTON (1815-1877)
- SMITH, HENRY JOHN STEPHEN (1826-1883)
- SMITH, HENRY PRESERVED (1847– )
- SMITH, JAMES (1775–1839)
- SMITH, JOHN (1579-1631)
- SMITH, JOHN RAPHAEL (1752–1812)
- SMITH, JOSEPH, JR
- SMITH, MORGAN LEWIS (1822–1874)
- SMITH, RICHARD BAIRD (1818-1861)
- SMITH, ROBERT (1689-1768)
- SMITH, SIR HENRY GEORGE WAKELYN
- SMITH, SIR THOMAS (1513-1577)
- SMITH, SIR WILLIAM (1813-1893)
- SMITH, SIR WILLIAM SIDNEY (1764-1840)
- SMITH, SYDNEY (1771-1845)
- SMITH, THOMAS SOUTHWOOD (1788-1861)
- SMITH, WILLIAM (1769-1839)
- SMITH, WILLIAM (c. 1730-1819)
- SMITH, WILLIAM (fl. 1596)
- SMITH, WILLIAM FARRAR (1824—1903)
- SMITH, WILLIAM HENRY (1808—1872)
- SMITH, WILLIAM HENRY (1825—1891)
- SMITH, WILLIAM ROBERTSON (1846-'894)
Smith (1815-1816); in 1818 W
.
See also:Buckland described them under the unwieldy See also:title " Oxford, See also:Forest or Fen Clay." The See also:term Oxfordian was introduced by d'See also:Orbigny in 1844
.
The name is derived from the See also:English See also:county of Oxford, where the beds are well See also:developed, but they See also:crop out almost continuously from See also:Dorsetshire to the See also:coast of See also:Yorkshire, generally forming See also:low, broad valleys
.
They are well exposed at See also:Weymouth, Oxford, See also:Bedford, See also:Peterborough, and in the cliffs at Scar-See also:- BOROUGH (A.S. nominative burh, dative byrig, which produces some of the place-names ending in bury, a sheltered or fortified place, the camp of refuge of a tribe, the stronghold of a chieftain; cf. Ger. Burg, Fr. bor, bore, bourg)
- BOROUGH [BURROUGH, BURROWE, BORROWS], STEVEN (1525–1584)
borough, Red Cliff and Gristhorpe See also:Bay
.
Rocks of this See also:age are found also in Uig and See also:Skye
.
The Oxford Clay is usually bluish or greenish-See also:grey in See also:colour, weathering 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 or yellow; In the See also:lower portions it is somewhat more shaly
.
The beds frequently tend to be calcareous and bituminous, while in places there is a considerable amount of See also:lignite
.
Septaria of large See also:size are See also:common, they have been cut and polished at Radipole and Melbury Osmund in Dorsetshire, where they are known as Melbury See also:marble or "turtle-stones "; they were used to See also:form table-tops, &c
.
In Yorkshire the Oxford Clay is usually a grey sandy shale
.
In the central and See also:southern English counties the Oxford Clay is divisible as follows:
Upper See also:zone of S See also:Clays with septaria and ironstone nodules
.
Clays with
Cardsoceras cordalum pyritized fossils (subzone of Quenstedloceras kamberli)
.
Lower zone of 1 Shales with pyritized fossils (subzone of Cosmoceras See also:Jason)
.
Cosmoccras ornatum
The upper zone contains also Gryphaea dilatata (large forms), Serpula vertebralis, Belemnites hastatus, Aspidoceras perarmatum, Cardioceras vertebrale
.
The lower zone yields Reineckia anceps, Peltoceras at hl eta, Quenstedtoceras Mariae, Cosmoceras Jason, Cerithium muricatum, and a small form of Gryphaea dilatata
.
The remains of fishes and saurian See also:reptiles have been found
.
The Oxford Clay is dug for See also:brick-making at Weymouth, See also:Trowbridge, See also:Chippenham, Oxford, Bedford, Peterborough and Fletton
.
The " Oxfordian " of the See also:continent of See also:Europe is divided accordin to A. de See also:Lapparent into an upper (Argovian) and a lower (Neuvizyen) substage
.
In the former he includes See also:part of the English Coralline Oolite and in the latter the lower Calcareous Grit, while a portion of the lower Oxford Clay is placed in the Divesian or upper substage of the Callovian
.
In See also:north-See also:west See also:Germany the Oxford Clay is re-presented by the Hersumer beds
.
Most of the See also:European formations on this See also:horizon are clays and marls with occasional See also:limestone and ironstone beds
.
See See also:JURASSIC, CALLOVIAN, CORALLIAN
.
(J
.
A
.
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