BATHONIAN SERIES
, in geology
.
The typical Bathonian is the Great Oolite series of England, and the name was derived from the " Bath Oelite," so extensively mined and quarried in the vicinity of that city, where the principal strata were first studied by W
.
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
.
The term was first used by J. d' Omalius d'ilalloy in 1843 (Precis Geol.) as a synonym for " Dogger "; but it was limited in 1849 by A. d' Orbigny ( Pal
.
Franc
.
Jun. i. p
.
607)
.
In 1864 Mayer-Eymar ( Tabl
.
Synchron.) used the word " Bathien "= Bajocian+Bathonian (sen. str.)
.
According to English practice, the Bathonian includes the,following formations in descending See also: - ORDER
- ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
- ORDER, HOLY
order: Cornbrash, Forest Marble with Bradford Clay, Great or Bath Oolite, Stonesfield Slate and Fullers' Earth
.
(The Fullers' Earth is sometimes regarded as constituting a separate stage, the " Fullonian.") The " Bathonien " of some French geologists differs from the English Bathonian in that it includes at the base the zone of the ammonite Parkinsonia Parkinso-ni, which in England is placed at the summit of the Inferior Oolite
.
The Bathonian is the equivalent of the upper part of the " Dogger " ( Middle Jurassic) of Germany, or to the base of the Upper 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 Jura (substage " E " of Quenstedt)
.
Rocks of Bathonian age arc well developed in Europe: in the N.W. and S.W. polite limestones are characteristically associated with coral- hearing, crinoidal and other varieties, and with certain beds of clay
.
In the N. and N.E., Russia, &c., clays, sandstones and ferruginous oolites prevail, some of the last being exploited for iron
.
They occur also in the extreme north of America and in the Arctic regions, Greenland, Franz Josef Land, &c.; in Africa, Algeria, German East Africa, Madagascar and near the Cape (Enon Beds); in India, Rajputana and Gulf of Cutch, and in South America
.
The well-known Caen See also: - STONE
- STONE (0. Eng. shin; the word is common to Teutonic languages, cf. Ger. Stein, Du. steen, Dan. and Swed. sten; the root is also seen in Gr. aria, pebble)
- STONE, CHARLES POMEROY (1824-1887)
- STONE, EDWARD JAMES (1831-1897)
- STONE, FRANK (1800-1859)
- STONE, GEORGE (1708—1764)
- STONE, LUCY [BLACKWELL] (1818-1893)
- STONE, MARCUS (184o— )
- STONE, NICHOLAS (1586-1647)
stone of Normandy and " Hauptrogenstein" of Swabia, as well as the "Eisenkalk" of N.W
.
Germany, and " Klaus-Schichten " of the Austrian Alps, are of Bathonian age
.
For a general account, see A. de Lapparent, Traite de g'ologie (5th ed., 1906), vol. ii.; see also the article JURASSIC
.
(J
.
A
.
End of Article: BATHONIAN SERIES
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