See also:LINLITHGOWSHIRE, or See also:WEST See also:LOTHIAN
, a See also:south-eastern See also:county of See also:Scotland, bounded N. by the See also:Firth of Forth, E. and S.E. by See also:Edinburghshire, S.W. by See also:Lanarkshire and N.W. by See also:Stirlingshire
.
It has an See also:area of 76,861 acres, or 120 sq. m., and a See also:coast See also:line of 17 M
.
The See also:surface rises very gradually from the Firth to the hilly See also:district in the south
.
A few See also:miles from the Forth a valley stretches from See also:east to See also:west
.
Between the county See also:town and See also:Bathgate are several hills, the See also:chief being Knock (1017 ft.), Cairnpapple, or Cairnnaple (1000), Cocklerue (said to be a corruption of Cuckold-le-Roi, 912), Riccarton Hills (832) terminating eastwards in Binny See also:Craig, a striking See also:eminence similar to those of See also:Stirling and See also:Edinburgh, Torphichen Hills (777) and Bowden (749)
.
In the coast district a few bold rocks are found, such as Dalmeny, Dundas (well wooded and with a precipitous front), the Binns and a rounded eminence of 559 ft. named Glower-o'er-'em or Bonnytoun, bearing on its See also:summit a See also:monument to See also:General See also:Adrian See also:Hope, who See also:fell in the See also:Indian See also:Mutiny
.
The See also:river See also:Almond, rising in Lanarkshire and pursuing a See also:north-easterly direction, enters the Firth at Cramond after a course of 24 m., during a See also:great See also:part of which it forms the boundary between West and See also:Mid See also:Lothian
.
Its right-See also:hand tributary, Breich See also:Water, constitutes another portion of the line dividing the same counties
.
The See also:Avon, rising in the detached portion of See also:Dumbartonshire, flows eastwards across south Stirlingshire and then, following in the See also:main a northerly direction, passes the county town on the west and reaches the Firth about midway between See also:Grangemouth and Bo'ness, having served as the boundary of Stirlingshire, during rather more than the latter See also:half of its course
.
The only See also:loch is See also:Linlithgow See also:Lake (102 acres), immediately adjoining the county town on the north, a favourite resort of curlers and skaters
.
It is to ft. deep at the east end and 48 ft. at the west
.
Eels, See also:perch and braise (a See also:species of See also:roach) are abundant
.
See also:Geology.—The rocks of See also:Linlithgowshire belong almost without exception to the Carboniferous See also:system
.
At the See also:base is the Calciferous See also:Sandstone See also:series, most of which lies between the Bathgate Hills and the eastern boundary of the county
.
In this series are the See also:Queensferry See also:limestone, the See also:equivalent of the Burdiehouse limestone of Edinburgh, and the Binny sandstone See also:group with shales and See also:clays and the See also:Houston See also:coal See also:bed
.
At more than one See also:horizon in this series oil shales are found
.
The Bathgate Hills are formed of basaltic lavas and tuffs—an interbedded volcanic group possibly 2000 ft. thick in the Calciferous Sandstone and Carboniferous Limestone series
.
A See also:peculiar serpentinous variety of the prevailing See also:rock ,is quarried at See also:Blackburn for See also:oven floors; it is known as " lakestone." Binns 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 is the site of one of the volcanic cones of the See also:period
.
The Carboniferous Limestone series consists of an upper and See also:low& limestone group—including the Petershill, See also:Index, Dykeneuk and Craigenbuck limestones—and a See also:middle group of shales, ironstones and coals; the Smithy, See also:Easter Main, Foul, Red and Splint coals belong to this horizon
.
Above the Carboniferous Limestone ,the
Millstone grit series crops in a See also:belt which may be traced from the mouth of the Avon southwards to Whitburn
.
This is followed by .the true coal-See also:measures with the Boghead or Torbanehill coal, the Colinburn, Main, See also:Ball, See also:- MILL
- MILL (O. Eng. mylen, later myln, or miln, adapted from the late Lat. molina, cf. Fr. moulin, from Lat. mola, a mill, molere, to grind; from the same root, mol, is derived " meal;" the word appears in other Teutonic languages, cf. Du. molen, Ger. muhle)
- MILL, JAMES (1773-1836)
- MILL, JOHN (c. 1645–1707)
- MILL, JOHN STUART (1806-1873)
Mill and Upper Cannel or See also:Shotts get_ coals of Armadale, Torbanehill and Fauldhouse
.
See also:Climate and See also:Agriculture.—The See also:average rainfall for the See also:year is 29.9 in., and the average temperature 47.5° F
.
(See also:January 38° F.; See also:July 59.5° F.)
.
More than three-fourths of the county, the agriculture of which is highly See also:developed, is under cultivation
.
The best See also:land is found along the coast, as at Carriden and Dalmeny
.
The farming is mostly arable, permanent pasture being practically stationary (at about 22,000 acres)
.
Oats is the See also:principal See also:grain See also:crop, but See also:barley and See also:wheat are also cultivated
.
Farms between too and 300 acres are the most See also:common
.
Turnips and potatoes are the leading See also:green crops
.
Much land has been reclaimed; the See also:parish of See also:Livingston, for example, which in the beginning of the 18th See also:century was covered with See also:heath and See also:juniper, is now under rotation
.
In Torphichen and Bathgate, however, patches of See also:peat See also:moss and swamp occur, and in the south there are extensive See also:moors at Fauldhouse and Polkemmet
.
Live stock does not See also:count for so much in West Lothian as in other Scottish counties, though a considerable number of See also:cattle are fattened and See also:dairy farming is followed success-fully, the fresh See also:butter and See also:milk finding a See also:market in Edinburgh
.
There is some See also:sheep-farming, and horses and pigs are reared
.
The wooded land occurs principally in the parks and " policies " surrounding the many noblemen's mansions and private estates
.
Other See also:Industries.—The shale-oil See also:trade flourishes at Bathgate, Broxburn, Armadale, Uphall, Winchburgh, Philpstoun and Dalmeny
.
There are important See also:iron-See also:works with blast furnaces at Bo'ness, Kiiineil, Whitburn and Bathgate, and coal is also largely See also:mined at these places
.
Coal-See also:mining is supposed to have been followed since See also:Roman times, and the earliest document extant regarding coalpits in Scotland is a See also:charter granted about the end of the 12th century to 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 Oldbridge of Carriden
.
See also:Fire-See also:clay is extensively worked in connexion with the coal, and ironstone employs many hands
.
Limestone, freestone and whinstone are all quarried
.
Binny See also:free-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 was used for the Royal Institution and the See also:National See also:Gallery in Edinburgh, and many important buildings in See also:Glasgow
.
Some fishing is carried on from Queensferry, and Bo'ness is the principal See also:port
.
Communications.—The North See also:British Railway See also:Company's line from Edinburgh to Glasgow runs across the north of the county, it controls the approaches to the Forth See also:Bridge, and serves the See also:rich See also:mineral district around See also:Airdrie and See also:Coatbridge in Lanarkshire via Bathgate
.
The Caledonian Railway Company's line from Glasgow to Edinburgh touches the extreme south of the See also:shire
.
The See also:Union See also:Canal, constructed in 1818-1822 to connect Edinburgh with the Forth and See also:Clyde Canal near Camelon in Stirlingshire, crosses the county, roughly following the N.B.R. line to See also:Falkirk
.
The Union Canal, which is 31 M. See also:long and belongs to the North British railway, is carried across the Almond and Avon on aqueducts designed by See also:- THOMAS
- THOMAS (c. 1654-1720)
- THOMAS (d. 110o)
- THOMAS, ARTHUR GORING (1850-1892)
- THOMAS, CHARLES LOUIS AMBROISE (1811-1896)
- THOMAS, GEORGE (c. 1756-1802)
- THOMAS, GEORGE HENRY (1816-187o)
- THOMAS, ISAIAH (1749-1831)
- THOMAS, PIERRE (1634-1698)
- THOMAS, SIDNEY GILCHRIST (1850-1885)
- THOMAS, ST
- THOMAS, THEODORE (1835-1905)
- THOMAS, WILLIAM (d. 1554)
Thomas See also:Telford, and near Falkirk is conveyed through a See also:tunnel 2100 ft. long
.
See also:Population and See also:Administration.—In 1891 the population amounted to 52,808, and in 1901 to 65,708, showing an increase of 24.43% in the decennial period, the highest of any Scottish county for that See also:decade, and a See also:density of 547 persons to the sq. m
.
In 1901 five persons spoke Gaelic only, and 575 Gaelic and See also:English
.
The chief towns, with populations in 1901, are Bathgate (7549), Borrowstounness (9306), Broxburn (7099) and Linlithgow (4279)
.
The shire returns one member to See also:parliament
.
Linlithgowshire is part of the sheriffdom of the Lothians and See also:Peebles, and a See also:resident See also:sheriff-substitute sits at Linlithgow and Bathgate
.
The county is under school-See also:board See also:jurisdiction, and there are See also:academies at Linlithgow, Bathgate and Bo'ness
.
The See also:local authorities entrust the bulk of the " See also:residue " See also:- GRANT (from A.-Fr. graunter, O. Fr. greanter for creanter, popular Lat. creantare, for credentare, to entrust, Lat. credere, to believe, trust)
- GRANT, ANNE (1755-1838)
- GRANT, CHARLES (1746-1823)
- GRANT, GEORGE MONRO (1835–1902)
- GRANT, JAMES (1822–1887)
- GRANT, JAMES AUGUSTUS (1827–1892)
- GRANT, ROBERT (1814-1892)
- GRANT, SIR ALEXANDER
- GRANT, SIR FRANCIS (1803-1878)
- GRANT, SIR JAMES HOPE (1808–1895)
- GRANT, SIR PATRICK (1804-1895)
- GRANT, U
- GRANT, ULYSSES SIMPSON (1822-1885)
grant to the County Secondary See also:Education See also:Committee, which subsidizes elementary technical classes (See also:cookery, See also:laundry and dairy) and See also:science and See also:art and technological classes, including their equipment
.
See also:History.—Traces of the Pictish inhabitants still exist
.
Near Inveravon is an See also:accumulation of shells—mostly oysters, which have long ceased to be found so far up the Forth--considered by geologists to be a natural bed, but pronounced by antiquaries to be a See also:kitchen midden
.
Stone cists have been discovered at Carlowrie, Dalmeny, Newliston and elsewhere; on Cairnnaple is a circular structure of remote but unknown date; and at Kipps is a cromlech that was once surrounded by stones
.
The See also:wall of See also:Antoninus lies for several miles in the shire
.
The See also:discovery of a See also:fine legionary tablet at Bridgeness in 1868 is held by some to be conclusive See also:evidence that the great rampart terminated at that point and not at Carriden
.
Roman campscan be distinguished at several, spots
.
On the hill of Bowden is an earthwork, which J
.
See also:Stuart Glennie and others connect with the struggle of the See also:ancient Britons against the See also:Saxons of See also:Northumbria
.
The See also:historical associations of the county mainly cluster See also:round the town of Linlithgow (q.v.)
.
Kingscavil (pop
.
629) disputes with Stonehouse in Lanarkshire the See also:honour of being the birthplace of See also:Patrick See also:- HAMILTON
- HAMILTON (GRAND or ASHUANIPI)
- HAMILTON, ALEXANDER (1757-1804)
- HAMILTON, ANTHONY, or ANTOINE (1646-1720)
- HAMILTON, ELIZABETH (1758–1816)
- HAMILTON, EMMA, LADY (c. 1765-1815)
- HAMILTON, JAMES (1769-1831)
- HAMILTON, JAMES HAMILTON, 1ST DUKE OF (1606-1649)
- HAMILTON, JOHN (c. 1511–1571)
- HAMILTON, MARQUESSES AND DUKES OF
- HAMILTON, PATRICK (1504-1528)
- HAMILTON, ROBERT (1743-1829)
- HAMILTON, SIR WILLIAM
- HAMILTON, SIR WILLIAM (1730-1803)
- HAMILTON, SIR WILLIAM ROWAN (1805-1865)
- HAMILTON, THOMAS (1789-1842)
- HAMILTON, WILLIAM (1704-1754)
- HAMILTON, WILLIAM GERARD (1729-1796)
Hamilton, the See also:martyr (15o4-1528)
.
See See also:Sir R
.
See also:Sibbald, History of the Sheriffdoms of Linlithgow and Stirlingshire (Edinburgh, 1710) G
.
Waldie, Walks along the See also:Northern Roman Wall (Linlithgow, 1883); R
.
J
.
H
.
See also:Cunningham, Geology of the Lothians (Edinburgh, 1838)
.
End of Article: