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See also:WILTSHIRE [WILTS]
, a See also:south-western See also:county of See also:England, bounded N.W. and N. by See also:Gloucestershire, N.E. and E. by See also:Berkshire, S.E. by See also:Hampshire, S.W. and S. by See also:Dorsetshire, and W. by See also:Somersetshire
.
The See also:area is 1374.9 sq. m
.
A See also:great upland covers two-thirds of the county, comprising, in the See also:north-See also:east, See also:Marlborough See also:Downs, with Savernake See also:Forest; in the centre, the broad undulating sweep of See also:Salisbury See also:Plain; and in the south, the more varied hills and dales of the Nadder See also:watershed, the vale of See also:Chalk and Cranborne See also:Chase
.
Large tracts of the Chalk are over 600 ft. above the See also:sea, rising in many parts into steep and picturesque escarpments
.
Several peaks attain an See also:altitude of 900 ft., and Inkpen See also:Beacon, on the See also:borders of Berkshire, See also:Wiltshire and Hampshire, reaches ro11 ft
.
Scattered in thousands over the downs See also:lie huge blocks of silicious See also:Tertiary grits, called sarsen stones or See also:grey wethers, which were used by the See also:primitive builders of See also:Stonehenge and See also:Avebury
.
The underlying See also:Greensand is exposed in the deeper valleys of the Chalk, such as the vale of Pewsey, dividing Salisbury Plain from Marlborough Downs, and the vale of Chalk, dividing the Nadder westward from the heights of Cranborne Chase
.
One of the most charming features of the county is its fertile and well-wooded valleys
.
Three See also:ancient forests remain: Cranborne Chase, which extends into See also:Dorset, was a royal See also:deer-See also:park as See also:early as the reign of See also:
There is no great See also:sheet of See also:water, but the See also:reservoir near See also:Swindon, and the lakes of Longleat, Stourton and Fonthill in the south-See also:west of See also:Earl Stoke near See also:Westbury, and of Bowood, Corsham and Seagry near See also:Chippenham, deserve mention for the beauty of their scenery
.
The upper reaches of the See also:Thames skirt the north-eastern border, and three other considerable See also:rivers drain the Wiltshire Downs
.
The Kennet, rising west of Marlborough, winds eastward into Berkshire and meets the Thames at See also:Reading
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The See also:Lower or See also:Bristol See also:Avon flows from its source among the Cotteswolds in See also:southern Gloucestershire, past See also:Malmesbury, Chippenham, See also:Melksham and See also:Bradford, where it curves north-eastward into See also:Somerset, finally falling into the Bristol Channel
.
Besides many lesser tributaries it receives from the south the See also:Frome, which forms for about 5 M. the boundary between Wilts and Somerset
.
The East or See also:Christchurch Avon, which rises near Bishops Cannings in the centre of the county, flows east and south into Hampshire, and enters the sea at Christchurch
.
See also:Close to Salisbury it is joined by the See also:united streams of the Nadder and the Wylye; by the Ebble, which drains the vale of Chalk; and by the See also:Bourne, which flows south by west from its See also:head near Ludgershall
.
See also:Geology.—As has been said, about two-thirds of the See also:surface of Wilts is occupied by a great Chalk upland
.
Cropping out from beneath the Chalk is a fringe of the Selbornian—Upper Greensand and See also:Gault—the former is well exposed in the vale of Pewsey, west of See also:Devizes, and along the margins of the vale of Wardour; it forms a broad, hilly See also:tract from See also:Mere through Stourton to See also:Warminster
.
The Gault See also:Clay runs regularly at the See also:foot of the Upper Greensand; it is excavated in several places for See also:brick-making
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The Lower Greensand, which oversteps the underlying formations, appears from beneath the Gault at Poulshot and follows the same See also:line of outcrop northwards; a small outlier at Seend is worked for the See also:iron it contains
.
About one-third of the county lying on the north-west See also:side of the Chalk downs, including a portion of the vale of the See also: The Upper See also:Lias—the See also:oldest formation in the county—forms the See also:floor of the valley near See also:Box; it is followed by the overlying Inferior Oolite and See also:Fuller's See also:Earth . Then succeeds the Great Oolite See also:Series, which includes the famous See also:building-stones of See also:Bath, quarried at Winsley Down, near Bradford, and at Box, Corsham Down and other places in the neighbourhood . Above the freestones near Bradford comes the Bradford clay, with the well-known fossil A piocrinus or See also:pear-encrinite, followed by the Forest See also:Marble limestones and See also:clays . The rubbly See also:Cornbrash crops at Westwood, See also:Trowbridge, and Malmesbury . Further east lies the outcrop of See also:Oxfordian strata, comprising the sandy Keilaways beds and overlying See also:Oxford Clay, together forming a broad See also:low-lying tract in which stand Trowbridge, Melksham, Chippenham and See also:Cricklade . Rising up from the eastern margin of the Oxfordian vale is the irregular scarp formed by the See also:Corallian oolitic Iimestones and marls . The iron ores of Westbury are obtained in this formation . Another clay-bottomed vale lies on the eastern side of the Corallian ground, from near See also:Calne to Swindon, where it is exploited for bricks . It appears also between Seend, Coniston and West-See also:bury; also between Mere and Semley . About the former See also:place it is brought into apposition with Cretaceous rocks through the agency of an east to west See also:fault . At Tisbury and near Potterne are small outcrops of See also:Portlandian rocks which yield the See also:familiar building-stones of Tisbury and Chilmark . Limestones and clays of Purbeck See also:age lie in the vale of Wardour about Teffont Evias .
At Dinton in the same vale the See also:Wealden formation just makes its See also:appearance
.
In the south-eastern corner of the county there are tracts of Tertiary Reading Beds and See also:London Clay east of Downton and on the See also:Clarendon Hills; these are covered by Bagshot Beds at See also:Alder-bury and Grinstead, also on Hampworth Common
.
Outliers of Reading Beds and London Clay occur about Great Bedwin; the sarsen stones previously referred to represent the last remnants of a See also:mantle of Tertiary rocks which formerly covered the See also:district
.
Here and there See also:drift gravels and brick earths, besides low-level See also:river gravels, See also:rest upon the older rocks
.
See also:Agriculture.—Some five-sixths of the See also:total area, a high proportion, is under cultivation, but a large amount of this is in permanent pasture
.
The See also:soil, a heavy reddish See also:loam, with a subsoil of broken stones, in the north-west, but lighter in the chalk region, is essentially that of a See also:pastoral See also:country, although there are wide tracts of richer land, suitable for See also:wheat and beans
.
Oats, however, are the largest See also:grain See also:crop
.
There is a small acreage classified as See also:
An agricultural See also:college is established at Downton
.
Manufactures.—A See also:majority of the hands employed in factories and workshops are occupied in the See also:locomotive See also:works of the Great Western railway at Swindon
.
There are also large See also:engineering works at Devizes
.
See also:Cloth is still See also:woven, though in greatly diminished quantities, at Trowbridge, Melksham, Chippenham and other places where water-See also:power is available
.
Carpets are woven at See also:Wilton, haircloth and coco-See also:nut fibre at Melksham, See also:silk at Malmesbury, Mere and Warminster
.
See also:Portland and Bath See also: Swindon, Salisbury and Westbury are the three centres of railway See also:traffic . The Avon is navigable as far as Salisbury, and goods are carried on the Thames & See also:Severn See also:Canal in the N.E., and on the Kennet & Avon Canal across Salisbury Plain . These waterways were formerly connected by a branch of the Berks & Wilts Canal, which runs S.W. from Berkshire, through Swindon and Melksham, but was closed in 1899 . The area of the ancient county is 879,943 acres, with a See also:population in 1891 of 264,997 and in 1901 of 273,869 . The area of the administrative county is 864,105 acres . The county contains 29 hundreds . The municipal boroughs are—See also:Calve (pop . 3457), Chippenham (5o74), Devizes (6532), Malmesbury (2854), See also:Marl-See also:borough (3887), Salisbury, a See also:city and the county town (17,117), Swindon (45,006), Wilton (2203) . The See also:urban districts are—Bradford-on-Avon (4514), Melksham (2450) ,Trowbridge (11,526), Warminster (5547), Westbury (33o5) . Other small towns are Cricklade (1517), Downton (1786), Highworth (2047), Mere (1977), Pewsey (1722), Wootton Bassett (2258) . The county is in the western See also:circuit, and assizes are held at Salisbury and Devizes . It has one See also:court of quarter sessions, and is divided into 16 See also:petty sessional divisions . The boroughs of Devizes and Salisbury have See also:separate courts of quarter sessions and commissions of the See also:peace, and the borough of Marlborough has a separate See also:commission of the peace . There are 33 5 See also:civil parishes . Wiltshire is mainly in the See also:diocese of Salisbury, but a considerable part is in that of Bristol, and small parts in those of See also:Gloucester, Oxford and See also:Winchester . It contains 322 ecclesiastical parishes or districts, wholly or in part . The county is divided into five See also:parliamentary divisions, each returning one member—See also:Northern or Cricklade, North-western or Chippenham, Western or West- bury, Eastern or Devizes and Southern or Wilton . It also contains the parliamentary borough of Salisbury, returning one member . See also:History.—The See also:English See also:conquest of the district now known as Wiltshire began in 552 with the victory of Cynric at Old Sarum, by which the way was opened to Salisbury Plain . Four years later, pushing his way through the vale of Pewsey, Cynric extended the limits of the West Saxon See also:kingdom to the Marl-borough Downs by a victory at Barbury Hill At this See also:period the district south of the Avon and the Nadder was occupied by dense woodland, the See also:relics of which survive in Cranborne Chase, and the first See also:wave of West Saxon colonization was chiefly confined to the valleys of the Avon and the Wylye, the little township of Wilton which arose in the latter giving the name of Wilsaetan to the new settlers . By the 9th See also:century the district had acquired a definite administrative and territorial organization, Walstan, ealdorman of the Wilsaetan, being mentioned as early as Soo as repelling an attempted invasion of the Mercians . Moreover, " Wiltunscire " is mentioned by See also:Asser in 878, in which See also:year the Danes established their head-quarters at Chippenham and remained there a year, plundering the surrounding country . In the See also:time of IEthelstan mints existed at Old Sarum, Malmesbury, Wilton, Cricklade and Marlborough . Wilton and Salisbury were destroyed by the Danish invaders under Sweyn in 1003, and in 1015 the district was harried by Canute .
With the redistribution of estates after the Conquest more than two-fifths of the county See also:fell into the hands of the See also:
On the See also:division of the West Saxon see in 703 Wiltshire was included in the diocese of See also:Sherborne, but in 905 a separate diocese of Wilton was founded, the see being fixed alternately at Ramsbury, Wilton and Sunning in Berkshire
.
Shortly before the Conquest Wilton was reunited to the Sherborne diocese, and by the See also:synod of 1075–1076 the see was transferred to Salisbury
.
The archdeaconrics of Wiltshire and Salisbury are mentioned in 1180; in 1291 the former included the deaneries of Avebury, Malmesbury, Marlborough and Cricklade within this county, and the latter the deaneries of Amesbury, Potterne, Wilton, Chalke and Wylye
.
In 1535 the archdeaconry of Salisbury included the additional deanery of Salisbury, while Potterne deanery had been transferred to the archdeaconry of Wiltshire
.
The deaneries of the archdeaconry of Salisbury have remained unaltered; Wiltshire archdeaconry now includes the deaneries of Avebury, Marlborough and Potterne; and the deaneries of Chippenham, Cricklade and Malmesbury form part of the archdeaconry and diocese of Bristol
.
The inhabitants of Wiltshire have always been addicted to See also:industrial rather than warlike pursuits, and the See also:political history of the county is not remarkable
.
In 1686, after the completion of the Domesday Survey, Salisbury was the See also:scene of a great See also:council, in which all the landholders took oaths of See also:allegiance to the king; and a council for the same purpose assembled at Salisbury in 1116
.
At Clarendon in 1166 was See also:drawn up the See also:assize which remodelled the provincial See also:administration of See also:justice
.
Parliaments were held at Marlborough in 1267 and at Salisbury in 1328 and 1384
.
During the See also:wars of See also:Stephen's reign Salisbury, Devizes and Malmesbury were garrisoned by See also:Roger, bishop of Salisbury, for the empress, but in 1138 Stephen seized the bishop and captured Devizes See also:Castle
.
In 1216 Marl-borough Castle was surrendered to See also:
In the Civil See also:War of the 17th century Wiltshire actively supported the parliamentary cause, displaying a spirit of violent See also:anti-Catholicism, and the efforts of the See also:marquess of See also:Hertford and of See also:Lord See also:Seymour to raise a party for the king met with vigorous resistance from the inhabitants
.
The Royalists, however, made some progress in the early See also:stage of the struggle, Marlborough being captured for the king in 1642, while in 1643 the forces of the earl of See also:Essex were routed by See also: |