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See also:BARTON BEDS , in See also:geology, the name given to a See also:series of softish See also:grey and 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 See also:clays, with layers of See also:sand, of Upper See also:Eocene See also:age, which are found in the See also:Hampshire See also:Tertiary See also:basin, where they are particularly well exposed in the cliffs of Barton, Hordwell, and in the Isle of See also:Wight. Above the highly fossiliferous Barton See also:Clay there is a sandy series with few fossils; these are the Headon See also:- HILL
- HILL (0. Eng. hyll; cf. Low Ger. hull, Mid. Dutch hul, allied to Lat. celsus, high, collis, hill, &c.)
- HILL, A
- HILL, AARON (1685-175o)
- HILL, AMBROSE POWELL
- HILL, DANIEL HARVEY (1821-1889)
- HILL, DAVID BENNETT (1843–1910)
- HILL, GEORGE BIRKBECK NORMAN (1835-1903)
- HILL, JAMES J
- HILL, JOHN (c. 1716-1775)
- HILL, MATTHEW DAVENPORT (1792-1872)
- HILL, OCTAVIA (1838– )
- HILL, ROWLAND (1744–1833)
- HILL, SIR ROWLAND (1795-1879)
Hill or Barton Sands. Either of these names is preferable to the See also:term " Upper Bagshot Beds," which has been applied to these sands. The Barton Beds are absent from the See also:London basin, and the Upper Bagshot Sands of that See also:area are probably of a See also:lower See also:horizon than the Barton Sands. The term "Bartonien " was introduced by See also:Mayer-Eymar in 1857 for the See also:continental equivalents of the series.
Hampshire basin and See also:Paris basin. Isle of Wight.
Barton Sands 140-200 ft. See also:Limestone of St Ouen.
Barton Clay 162-255 ft. Bartonien Sands of See also:Beauchamp (sables moyen).
Fusus longaevus,Volutilithes luctatrix, Ostrea gigantea, Pectunculus (Glycimeris) deleta are characteristic fossils; fishes (Lamna, See also:Arius, &c.) and a See also:crocodile (Diplocynodon) are also found in the Barton Clay.
The sands are very pure and are used in See also:glass making.
See " Geology of the Isle of Wight," Mem. Geol. Survey (2nd ed., 1889) ; and " The Geology of the See also:Country around See also:Southampton," Mem. Geol. Survey (1902). (J. A. H.)
BARTON-UPON-See also:HUMBER, a See also:market See also:town in the N. See also:Lindsey or See also:Brigg See also:parliamentary See also:division of See also:Lincolnshire, See also:England, the See also:terminus of a See also:branch of the See also:Great Central railway, 44 M. N. by E. of See also:Lincoln. Pop. of See also:urban See also:district (1901) 5671.
It lies beneath See also:low hills, on See also:flat ground bordering the Humber, but the centre of the town is a mile from the See also:river. The See also:- CHURCH
- CHURCH (according to most authorities derived from the Gr. Kvpcaxov [&wµa], " the Lord's [house]," and common to many Teutonic, Slavonic and other languages under various forms—Scottish kirk, Ger. Kirche, Swed. kirka, Dan. kirke, Russ. tserkov, Buig. cerk
- CHURCH, FREDERICK EDWIN (1826-1900)
- CHURCH, GEORGE EARL (1835–1910)
- CHURCH, RICHARD WILLIAM (1815–189o)
- CHURCH, SIR RICHARD (1784–1873)
church of St See also:- PETER
- PETER (Lat. Petrus from Gr. irfpos, a rock, Ital. Pietro, Piero, Pier, Fr. Pierre, Span. Pedro, Ger. Peter, Russ. Petr)
- PETER (PEDRO)
- PETER, EPISTLES OF
- PETER, ST
Peter has a remarkable See also:west See also:tower of pre-See also:Conquest workman-See also:ship, excepting the See also:early See also:Norman See also:top. See also:storey. Against the western See also:face is a low See also:building of the date of the lower tower-storeys, measuring 15 ft. by 12, with See also:rude, deeply-splayed windows. The tower itself is arcaded in the two lower storeys, having See also:round See also:arches in the lower and triangular in the upper, and there is a round-headed S. See also:doorway and a triangular-headed N. doorway. The See also:rest of the church is Decorated and Perpendicular. The church of St See also:Mary is See also:fine Early See also:English with Perpendicular See also:clerestory. See also:Industries include See also:brick-making, malting, and rope-making. Barton appears in Domesday, when the See also:ferry over the Humber existed. As a See also:port, moreover, it subsequently See also:rose into some importance, for it was able to See also:supply eight See also:ships and men to the expedition of See also:Edward III. to See also:Brittany.
End of Article: BARTON BEDS
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