Chapter 4

(J. S. F.)

1I. Minette (Weiler, Alsace). II. Kersantite (Neubrunn, Thuringia). III. Vogesite (Castle Mountain, Montana). IV. Spessartite (Waldmichael, Spessart). V. Camptonite (Campton Falls). VI. Monchiquite (Ria do Ouro, Serra de Tingua). VII. Alnöite (Alnö, Sweden).

1I. Minette (Weiler, Alsace). II. Kersantite (Neubrunn, Thuringia). III. Vogesite (Castle Mountain, Montana). IV. Spessartite (Waldmichael, Spessart). V. Camptonite (Campton Falls). VI. Monchiquite (Ria do Ouro, Serra de Tingua). VII. Alnöite (Alnö, Sweden).

LAMPSACUS,an ancient Greek colony in Mysia, Asia Minor, known as Pityusa or Pityussa before its colonization by Ionian Greeks from Phocaea and Miletus, was situated on the Hellespont, opposite Callipolis (Gallipoli) in Thrace. It possessed a good harbour; and the neighbourhood was famous for its wine, so that, having fallen into the hands of the Persians during the Ionian revolt, it was assigned by Artaxerxes I. to Themistocles to provide him with wine, as Percote did with meat and Magnesia with bread. After the battle of Mycale (479B.C.), Lampsacus joined the Athenians, but, having revolted from them in 411, was reduced by force. It was defended in 196B.C.against Antiochus the Great of Syria, after which its inhabitants were received as allies of Rome. Lampsacus was the chief seat of the worship of Priapus, a gross nature-god closely connected with the culture of the vine. The ancient name is preserved in that of the modern village of Lapsaki, but the Greek town possibly lay at Chardak immediately opposite Gallipoli.

See A. L. Castellan,Lettres sur la Morée, l’Hellespont, &c.(Paris, 1820); Choiseul Gouffier,Voyage pittoresque dans l’empire ottoman(1842).

See A. L. Castellan,Lettres sur la Morée, l’Hellespont, &c.(Paris, 1820); Choiseul Gouffier,Voyage pittoresque dans l’empire ottoman(1842).

LAMPSTAND,a pillar, tripod or figure extending to the floor for supporting or holding a lamp. The lampstand (lampadère) is probably of French origin; it appears to have been in use in France before the end of the 17th century.

LANARK,a royal, municipal and police burgh, and county town of Lanarkshire, Scotland, standing on high ground about half a mile from the right bank of the Clyde, 31 m. S.E. of Glasgow by the Caledonian railway. Pop. (1901) 6440. It is a favourite holiday resort, being the point from which the falls of the Clyde are usually visited. The principal buildings are the town hall, the county buildings, the assembly rooms, occupying the site of an old Franciscan monastery, three hospitals, a convalescent home, the Smyllum orphanage and the Queen Victoria Jubilee fountain. The industries include cotton-spinning, weaving, nail-making and oilworks, and there are frequent markets for cattle and sheep. Lanark is a place of considerable antiquity. Kenneth II. held a parliament here in 978, and it was sometimes the residence of the Scottish kings, one of whom, William the Lion (d. 1214), granted it a charter. Several of the earlier exploits of William Wallace were achieved in the neighbourhood. He burned the town and slew the English sheriff William Hezelrig. About 1 m. N.W. are Cartland Craigs, where Mouse Water runs through a precipitous red sandstone ravine, the sides of which are about 400 ft. high. The stream is crossed by a bridge of single span, supposed to be Roman, and by a three-arched bridge, designed by Thomas Telford and erected in 1823. On the right bank, near this bridge, is the cave in which Wallace concealed himself after killing Hezelrig and which still bears his name. Lanark was the centre of much activity in the days of the Covenanters. William Lithgow (1582-1645), the traveller, William Smellie (1697-1763), the obstetrician and Gavin Hamilton (1730-1797), the painter, were born at Lanark. The town is one of the Falkirk district group of parliamentary burghs, the other constituents being Airdrie, Hamilton, Falkirk and Linlithgow.

New Lanark (pop. 795), 1 m. S., is famous in connexion with the socialist experiments of Robert Owen. The village was founded by David Dale (1739-1806) in 1785, with the support of Sir Richard Arkwright, inventor of the spinning-frame, who thought the spot might be made the Manchester of Scotland. In ten years four cotton mills were running, employing nearly 1400 hands. They were sold in 1799 to a Manchester company, who appointed Owen manager. In the same year he married Dale’s daughter. For many years the mills were successfully conducted, but friction ultimately arose and Owen retired in 1828. The mills, however, are still carried on.

There are several interesting places near Lanark. Braxfield, on the Clyde, gave the title of Lord Braxfield to Robert Macqueen (1722-1799), who was born in the mansion and acquired on the bench the character of the Scottish Jeffreys. Robert Baillie, the patriot who was executed for conscience’ sake (1684), belonged to Jerviswood, an estate on the Mouse. Lee House, the home of the Lockharts, is 3 m. N.W. The old castle was largely rebuilt in the 19th century. It contains some fine tapestry and portraits, and the Lee Penny—familiar to readers of Sir Walter Scott’sTalisman—which was brought from Palestine in the 14th century by the Crusading knight, Sir Simon Lockhart. It is described as a cornelian encased in a silver coin. Craignethan Castle on the Nethan, a left-hand tributary joining the Clyde at Crossford, is said to be the original of the “Tillietudiem” of Scott’sOld Mortality.

There are several interesting places near Lanark. Braxfield, on the Clyde, gave the title of Lord Braxfield to Robert Macqueen (1722-1799), who was born in the mansion and acquired on the bench the character of the Scottish Jeffreys. Robert Baillie, the patriot who was executed for conscience’ sake (1684), belonged to Jerviswood, an estate on the Mouse. Lee House, the home of the Lockharts, is 3 m. N.W. The old castle was largely rebuilt in the 19th century. It contains some fine tapestry and portraits, and the Lee Penny—familiar to readers of Sir Walter Scott’sTalisman—which was brought from Palestine in the 14th century by the Crusading knight, Sir Simon Lockhart. It is described as a cornelian encased in a silver coin. Craignethan Castle on the Nethan, a left-hand tributary joining the Clyde at Crossford, is said to be the original of the “Tillietudiem” of Scott’sOld Mortality.

LANARKSHIRE,a south-western county of Scotland, bounded N. by the shires of Dumbarton and Stirling, E. by Linlithgowshire, Mid-Lothian and Peeblesshire, S. by Dumfriesshire and W. by the counties of Ayr, Renfrew and Dumbarton. Its area is 879 sq. m. (562,821 acres). It may be described as embracing the valley of the Clyde; and, in addition to the gradual descent from the high land in the south, it is also characterized by a gentle slope towards both banks of the river. The shire is divided into three wards, the Upper, comprising all the southern section, or more than half the whole area (over 330,000 acres); the Middle, with Hamilton for its chief town, covering fully 190,000 acres; and the Lower, occupying the northern area of about 40,000 acres. The surface falls gradually from the uplands in the south to the Firth of Clyde. The highest hills are nearly all on or close to the borders of Peeblesshire and Dumfriesshire, and include Culter Fell (2454 ft.) and Lowther Hill (2377). The loftiest heights exclusively belonging to Lanarkshire are Green Lowther (2403), Tinto (2335), Ballencleuch Law (2267), Rodger Law (2257), Dun Law (2216), Shiel Dod (2190), Dungrain Law (2186) and Comb Law (2107). The principal rivers are the Clyde and its head waters and affluents (on the right, the Medwin, Mouse, South Calder, NorthCalder and Kelvin; on the left, the Douglas, Nethan, Avon, Rotten Calder and Cart). There are no lochs of considerable size, the few sheets of water in the north—Woodend Reservoir, Bishop Loch, Hogganfield Loch, Woodend Loch, Lochend Loch—mainly feeding the Monkland and the Forth and Clyde Canals. The most famous natural features are the Falls of Clyde at Bonnington, Corra, Dundaff and Stonebyres.

Geology.—The southern upland portion is built up of Silurian and Ordovician rocks; the northern lower-lying tracts are formed of Carboniferous and Old Red Sandstone rocks. Ordovician strata cross the county from S.W. to N.E. in a belt 5-7 m. in breadth which is brought up by a fault against the Old Red and the Silurian on the northern side. This fault runs by Lamington, Roberton and Crawfordjohn. The Ordovician rocks lie in a synclinal fold with beds of Caradoc age in the centre flanked by graptolitic shales, grits and conglomerates, including among the last-named the local “Haggis-rock”; the well-known lead mines of Leadhills are worked in these formations. Silurian shales and sandstones, &c., extend south of the Ordovician belt to the county boundary; and again, on the northern side of the Ordovician belt two small tracts appear through the Old Red Sandstone on the crests of anticlinal folds. The Old Red Sandstone covers an irregular tract north of the Ordovician belt; a lower division consisting of sandstone, conglomerates and mud-stones is the most extensively developed; above this is found a series of contemporaneous porphyrites and melaphyres, conformable upon the lower division in the west of the county but are not so in the east. An upper series of sandstones and grits is seen for a short distance west of Lamington. Lanark stands on the Old Red Sandstone and the Falls of Clyde occur in the same rocks. Economically the most important geological feature is the coal basin of the Glasgow district. The axis of this basin lies in a N.E.-S.W. direction; in the central part, including Glasgow, Airdrie, Motherwell, Wishaw, Carluke, lie the coal-measures, consisting of sandstones, shales, marls and fireclays with seams of coal and ironstone. There are eleven beds of workable coal, the more important seams being the Ell, Main, Splint, Pyotshaw and Virtuewell. Underlying the coal-measures is the Millstone Grit seen on the northern side between Glenboig and Hogganfield—here the fireclays of Garnkirk, Gartcosh and Glenboig are worked—and on the south and south-east of the coal-measures, but not on the western side, because it is there cut out by a fault. Beneath the last-named formation comes the Carboniferous Limestone series with thin coals and ironstones, and again beneath this is the Calciferous Sandstone series which in the south-east consists of sandstones, shales, &c., but in the west the greater part of the series is composed of interbedded volcanic rocks—porphyrites and melaphyres. It will be observed that in general the younger formations lie nearer the centre of the basin and the older ones crop out around them. Besides the volcanic rocks mentioned there are intrusive basalts in the Carboniferous rocks like that in the neighbourhood of Shotts, and the smaller masses at Hogganfield near Glasgow and elsewhere. Volcanic necks are found in the Carluke and Kilcadzow districts, marking the vents of former volcanoes and several dikes of Tertiary age traverse the older rocks. An intrusion of pink felsite in early Old Red times has been the cause of Tinto Hill. Evidences of the Glacial period are abundant in the form of kames and other deposits of gravel, sand and boulder clay. The ice in flowing northward and southward from the higher ground took an easterly direction when it reached the lower ground. In the lower reaches of the Clyde the remains of old beaches at 25, 50 and 100 ft. above the present sea-level are to be observed.Climate and Agriculture.—The rainfall averages 42 in. annually, being higher in the hill country and lower towards the north. The temperature for the year averages 48° F., for January 38° and for July 59°. The area under grain has shown a downward tendency since 1880. Oats is the principal crop, but barley and wheat are also grown. Potatoes and turnips are raised on a large scale. In the Lower Ward market-gardening has increased considerably, and the quantity of vegetables, grapes and tomatoes reared under glass has reached great proportions. An ancient industry in the vale of the Clyde for many miles below Lanark is the cultivation of fruit, several of the orchards being said to date from the time of Bede. The apples and pears are of good repute. There has been a remarkable extension in the culture of strawberries, hundreds of acres being laid down in beds. The sheep walks in the upper and middle wards are heavily stocked and the herds of cattle are extensive, the favoured breeds being Ayrshire and a cross between this and “improved Lanark.” Dairy-farming flourishes, the cheeses of Carnwath and Lesmahagow being in steady demand. Clydesdale draught-horses are of high class. They are supposed to have been bred from Flanders horses imported early in the 18th century by the 5th duke of Hamilton. Most of the horses are kept for agricultural work, but a considerable number of unbroken horses and mares are maintained for stock. Pigs are numerous, being extensively reared by the miners. The largest farms are situated in the Upper Ward, but the general holding runs from 50 to 100 acres. More than 21,000 acres are under wood.Other Industries.—The leading industries are those in connexion with the rich and extensive coal and iron field to the east and southeast of Glasgow; the shipbuilding at Govan and Partick and in Glasgow harbour; the textiles at Airdrie, Blantyre, Hamilton, Lanark, New Lanark, Rutherglen and Glasgow; engineering at Cambuslang, Carluke, Coatbridge, Kinning Park, Motherwell and Wishaw, and the varied and flourishing manufactures centred in and around Glasgow.Communications.—In the north of the county, where population is most dense and the mineral field exceptionally rich, railway facilities are highly developed, there being for 10 or 12 m. around Glasgow quite a network of lines. The Caledonian Railway Company’s main line to the south runs through the whole length of the shire, sending off branches at several points, especially at Carstairs Junction. The North British Railway Company serves various towns in the lower and middle wards and its lines to Edinburgh cross the northwestern corner and the north of the county. Only in the immediate neighbourhood of Glasgow does the Glasgow and South Western system compete for Lanarkshire traffic, though it combines with the Caledonian to work the Mid-Lanarkshire and Ayrshire railway. The Monkland Canal in the far north and the Forth and Clyde Canal in the north and north-west carry a considerable amount of goods, and before the days of railways afforded one of the principal means of communication between east and west.Population and Administration.—The population amounted in 1891 to 1,105,899 and in 1901 to 1,339,327, or 1523 persons to the sq. m. Thus though only tenth in point of extent, it is much the most populous county in Scotland, containing within its bounds nearly one-third of the population of the country. In 1901 there were 104 persons speaking Gaelic only, and 26,905 speaking Gaelic and English. The chief towns, with populations in 1901, apart from Glasgow, are Airdrie (22,288), Cambuslang (12,252), Coatbridge (36,991), Govan (82,174), Hamilton (32,775), Kinning Park (13,852), Larkhall (11,879), Motherwell (30,418), Partick (54,298), Rutherglen (17,220), Shettleston (12,154), Wishaw (20,873). Among smaller towns are Bellshill, Carluke, Holytown, Lanark, Stonefield, Tollcross and Uddingston; and Lesmahagow and East Kilbride are populous villages and mining centres. The county is divided into six parliamentary divisions:—North-east, North-west, Mid and South Lanark, Govan and Partick each returning one member. The royal burghs are Glasgow, Lanark and Rutherglen; the municipal and police burghs Airdrie, Biggar, Coatbridge, Glasgow, Govan, Hamilton, Kinning Park, Lanark, Motherwell, Partick, Rutherglen and Wishaw. Glasgow returns seven members to Parliament; Airdrie, Hamilton and Lanark belong to the Falkirk group and Rutherglen to the Kilmarnock group of parliamentary burghs. Lanarkshire is a sheriffdom, whose sheriff-principal is confined to his judicial duties in the county, and he has eight substitutes, five of whom sit constantly in Glasgow, and one each at Airdrie, Hamilton and Lanark. The shire is under school-board jurisdiction, many schools earning grants for higher education. For advanced education, besides the university and many other institutions in Glasgow there are a high school in Hamilton, and technical schools at Coatbridge and Wishaw. The county council expends the “residue” grant in supporting lectures and classes in agriculture and agricultural chemistry, mining, dairying, cookery, laundry work, nursery and poultry-keeping, in paying fees and railway fares and providing bursaries for technical students, and in subsidizing science and art and technical classes in day and evening schools. A director of technical education is maintained by the council. Lanark, Motherwell and Biggar entrust their shares of the grant to the county council, and Coatbridge and Airdrie themselves subsidize science and art and evening classes and continuation schools.

Geology.—The southern upland portion is built up of Silurian and Ordovician rocks; the northern lower-lying tracts are formed of Carboniferous and Old Red Sandstone rocks. Ordovician strata cross the county from S.W. to N.E. in a belt 5-7 m. in breadth which is brought up by a fault against the Old Red and the Silurian on the northern side. This fault runs by Lamington, Roberton and Crawfordjohn. The Ordovician rocks lie in a synclinal fold with beds of Caradoc age in the centre flanked by graptolitic shales, grits and conglomerates, including among the last-named the local “Haggis-rock”; the well-known lead mines of Leadhills are worked in these formations. Silurian shales and sandstones, &c., extend south of the Ordovician belt to the county boundary; and again, on the northern side of the Ordovician belt two small tracts appear through the Old Red Sandstone on the crests of anticlinal folds. The Old Red Sandstone covers an irregular tract north of the Ordovician belt; a lower division consisting of sandstone, conglomerates and mud-stones is the most extensively developed; above this is found a series of contemporaneous porphyrites and melaphyres, conformable upon the lower division in the west of the county but are not so in the east. An upper series of sandstones and grits is seen for a short distance west of Lamington. Lanark stands on the Old Red Sandstone and the Falls of Clyde occur in the same rocks. Economically the most important geological feature is the coal basin of the Glasgow district. The axis of this basin lies in a N.E.-S.W. direction; in the central part, including Glasgow, Airdrie, Motherwell, Wishaw, Carluke, lie the coal-measures, consisting of sandstones, shales, marls and fireclays with seams of coal and ironstone. There are eleven beds of workable coal, the more important seams being the Ell, Main, Splint, Pyotshaw and Virtuewell. Underlying the coal-measures is the Millstone Grit seen on the northern side between Glenboig and Hogganfield—here the fireclays of Garnkirk, Gartcosh and Glenboig are worked—and on the south and south-east of the coal-measures, but not on the western side, because it is there cut out by a fault. Beneath the last-named formation comes the Carboniferous Limestone series with thin coals and ironstones, and again beneath this is the Calciferous Sandstone series which in the south-east consists of sandstones, shales, &c., but in the west the greater part of the series is composed of interbedded volcanic rocks—porphyrites and melaphyres. It will be observed that in general the younger formations lie nearer the centre of the basin and the older ones crop out around them. Besides the volcanic rocks mentioned there are intrusive basalts in the Carboniferous rocks like that in the neighbourhood of Shotts, and the smaller masses at Hogganfield near Glasgow and elsewhere. Volcanic necks are found in the Carluke and Kilcadzow districts, marking the vents of former volcanoes and several dikes of Tertiary age traverse the older rocks. An intrusion of pink felsite in early Old Red times has been the cause of Tinto Hill. Evidences of the Glacial period are abundant in the form of kames and other deposits of gravel, sand and boulder clay. The ice in flowing northward and southward from the higher ground took an easterly direction when it reached the lower ground. In the lower reaches of the Clyde the remains of old beaches at 25, 50 and 100 ft. above the present sea-level are to be observed.

Climate and Agriculture.—The rainfall averages 42 in. annually, being higher in the hill country and lower towards the north. The temperature for the year averages 48° F., for January 38° and for July 59°. The area under grain has shown a downward tendency since 1880. Oats is the principal crop, but barley and wheat are also grown. Potatoes and turnips are raised on a large scale. In the Lower Ward market-gardening has increased considerably, and the quantity of vegetables, grapes and tomatoes reared under glass has reached great proportions. An ancient industry in the vale of the Clyde for many miles below Lanark is the cultivation of fruit, several of the orchards being said to date from the time of Bede. The apples and pears are of good repute. There has been a remarkable extension in the culture of strawberries, hundreds of acres being laid down in beds. The sheep walks in the upper and middle wards are heavily stocked and the herds of cattle are extensive, the favoured breeds being Ayrshire and a cross between this and “improved Lanark.” Dairy-farming flourishes, the cheeses of Carnwath and Lesmahagow being in steady demand. Clydesdale draught-horses are of high class. They are supposed to have been bred from Flanders horses imported early in the 18th century by the 5th duke of Hamilton. Most of the horses are kept for agricultural work, but a considerable number of unbroken horses and mares are maintained for stock. Pigs are numerous, being extensively reared by the miners. The largest farms are situated in the Upper Ward, but the general holding runs from 50 to 100 acres. More than 21,000 acres are under wood.

Other Industries.—The leading industries are those in connexion with the rich and extensive coal and iron field to the east and southeast of Glasgow; the shipbuilding at Govan and Partick and in Glasgow harbour; the textiles at Airdrie, Blantyre, Hamilton, Lanark, New Lanark, Rutherglen and Glasgow; engineering at Cambuslang, Carluke, Coatbridge, Kinning Park, Motherwell and Wishaw, and the varied and flourishing manufactures centred in and around Glasgow.

Communications.—In the north of the county, where population is most dense and the mineral field exceptionally rich, railway facilities are highly developed, there being for 10 or 12 m. around Glasgow quite a network of lines. The Caledonian Railway Company’s main line to the south runs through the whole length of the shire, sending off branches at several points, especially at Carstairs Junction. The North British Railway Company serves various towns in the lower and middle wards and its lines to Edinburgh cross the northwestern corner and the north of the county. Only in the immediate neighbourhood of Glasgow does the Glasgow and South Western system compete for Lanarkshire traffic, though it combines with the Caledonian to work the Mid-Lanarkshire and Ayrshire railway. The Monkland Canal in the far north and the Forth and Clyde Canal in the north and north-west carry a considerable amount of goods, and before the days of railways afforded one of the principal means of communication between east and west.

Population and Administration.—The population amounted in 1891 to 1,105,899 and in 1901 to 1,339,327, or 1523 persons to the sq. m. Thus though only tenth in point of extent, it is much the most populous county in Scotland, containing within its bounds nearly one-third of the population of the country. In 1901 there were 104 persons speaking Gaelic only, and 26,905 speaking Gaelic and English. The chief towns, with populations in 1901, apart from Glasgow, are Airdrie (22,288), Cambuslang (12,252), Coatbridge (36,991), Govan (82,174), Hamilton (32,775), Kinning Park (13,852), Larkhall (11,879), Motherwell (30,418), Partick (54,298), Rutherglen (17,220), Shettleston (12,154), Wishaw (20,873). Among smaller towns are Bellshill, Carluke, Holytown, Lanark, Stonefield, Tollcross and Uddingston; and Lesmahagow and East Kilbride are populous villages and mining centres. The county is divided into six parliamentary divisions:—North-east, North-west, Mid and South Lanark, Govan and Partick each returning one member. The royal burghs are Glasgow, Lanark and Rutherglen; the municipal and police burghs Airdrie, Biggar, Coatbridge, Glasgow, Govan, Hamilton, Kinning Park, Lanark, Motherwell, Partick, Rutherglen and Wishaw. Glasgow returns seven members to Parliament; Airdrie, Hamilton and Lanark belong to the Falkirk group and Rutherglen to the Kilmarnock group of parliamentary burghs. Lanarkshire is a sheriffdom, whose sheriff-principal is confined to his judicial duties in the county, and he has eight substitutes, five of whom sit constantly in Glasgow, and one each at Airdrie, Hamilton and Lanark. The shire is under school-board jurisdiction, many schools earning grants for higher education. For advanced education, besides the university and many other institutions in Glasgow there are a high school in Hamilton, and technical schools at Coatbridge and Wishaw. The county council expends the “residue” grant in supporting lectures and classes in agriculture and agricultural chemistry, mining, dairying, cookery, laundry work, nursery and poultry-keeping, in paying fees and railway fares and providing bursaries for technical students, and in subsidizing science and art and technical classes in day and evening schools. A director of technical education is maintained by the council. Lanark, Motherwell and Biggar entrust their shares of the grant to the county council, and Coatbridge and Airdrie themselves subsidize science and art and evening classes and continuation schools.

History.—At an early period Lanarkshire was inhabited by a Celtic tribe, the Damnonii, whose territory was divided by the wall of Antoninus between the Forth and Clyde (remains of which are found in the parish of Cadder), but who were never wholly subjugated by the Romans. Traces of their fortifications, mounds and circles exist, while stone axes, bronze celts, querns and urns belonging to their age are occasionally unearthed. Of the Romans there are traces in the camp on Beattock summit near Elvanfoot, in the fine bridge over the Mouse near Lanark, in the road to the south of Strathaven, in the wall already mentioned and in the coins and other relics that have been dug up. After their departure the country which included Lanarkshire formed part of the kingdom of Strathclyde, which, in the 7th century, was subdued by Northumbrian Saxons, when great numbers of the Celts migrated into Wales. The county once embraced a portion of Renfrewshire, but this was disjoined in the time of Robert III. The shire was then divided into two wards, the Over (with Lanark as its chief town) and the Nether (with Rutherglen as its capital). The present division into three wards was not effected till the 18th century. Independently of Glasgow, Lanarkshire has not borne any part continuously in the general history of Scotland, but has been the scene ofseveral exciting episodes. Many of Wallace’s daring deeds were performed in the county, Queen Mary met her fate at Langside (1568) and the Covenanters received constant support from the people, defeating Claverhouse at Drumclog (1679), but suffering defeat themselves at Bothwell Brig (1679).

See W. Hamilton,Description of the Sheriffdoms of Lanark and Renfrew, Maitland Club (1831); C. V. Irving and A. Murray,The Upper Ward of Lanarkshire(Glasgow, 1864);The Clydesdale Stud Book(Glasgow); W. A. Cowan,History of Lanark(Lanark, 1867);Extracts from the Records of the Burgh of Lanark(Glasgow, 1893).

See W. Hamilton,Description of the Sheriffdoms of Lanark and Renfrew, Maitland Club (1831); C. V. Irving and A. Murray,The Upper Ward of Lanarkshire(Glasgow, 1864);The Clydesdale Stud Book(Glasgow); W. A. Cowan,History of Lanark(Lanark, 1867);Extracts from the Records of the Burgh of Lanark(Glasgow, 1893).

LANCASHIRE,a north-western county of England, bounded N.E. by Westmorland, E. by Yorkshire, S. by Cheshire, W. by the Irish Sea and N.W. by Cumberland. The area is 1880.2 sq. m., the county being the sixth in size in England. The coast is generally flat, and broken by great inlets, with wide expanses of sandy foreshore at low tide. The chief inlets, from N. to S., are—the estuary of the river Duddon, which, with the river itself, separates the county from Cumberland; Morecambe Bay; and the estuaries of the Ribble and the Mersey. Morecambe Bay receives the rivers Crake and Leven in a common estuary, and the Kent from Westmorland; while the Lune and the Wyre discharge into Lancaster Bay, which is only partially separated from Morecambe Bay by the promontory of Red Nab. Morecambe Bay also detaches from the rest of the county the district of Furness (q.v.), extending westward to the Duddon, and having off its coast the island of Walney, 8 m. in length, and several small isles within the strait between Walney and the mainland. The principal seaside resorts and watering-places, from S. to N., are Southport, Lytham, St Anne’s-on-the-Sea, Blackpool, Fleetwood and Morecambe; while at the head of Morecambe Bay are several pleasant villages frequented by visitors, such as Arnside and Grange. Of the rivers the Mersey (q.v.), separating the county from Cheshire, is the principal, and receives from Lancashire the Irwell, Sankey and other small streams. The Ribble, which rises in the mountains of the West Riding of Yorkshire, forms for a few miles the boundary with that county, and then flows S.W. to Preston, receiving the Hodder from the N. and the Calder and Darwen from the S. Lancashire has a share in two of the English districts most famous for their scenery, but does not include the finest part of either. Furness, entirely hilly except for a narrow coastal tract, extends N. to include the southern part of the Lake District (q.v.); it contains Coniston Lake and borders Windermere, which are drained respectively by the Leven and Crake, with some smaller lakes and such mountains as the Old Man and Wetherlam. Another elevated district, forming part of a mountainous chain stretching from the Scottish border, covered by the name of Pennine uplands in its broader application, runs along the whole eastern boundary of the main portion of the county, and to the south of the Ribble occupies more than half the area, stretching west nearly to Liverpool. The moorlands in the southern district are generally bleak and covered with heather. Towards the north the scenery is frequently beautiful, the green rounded elevated ridges being separated by pleasant cultivated valleys variegated by woods and watered by rivers. None of the summits of the range within Lancashire attains an elevation of 2000 ft., the highest being Blackstone Edge (1523ft.), Pendle Hill (1831 ft.) and Boulsworth Hill (1700 ft.).

Along the sea-coast from the Mersey to Lancaster there is a continuous plain formerly occupied by peat mosses, many of which have been reclaimed. The largest is Chat Moss between Liverpool and Manchester. In some instances these mosses have exhibited the phenomenon of a moving bog. A large district in the north belonging to the duchy of Lancaster was at one time occupied by forests, but these have wholly disappeared, though their existence is recalled in nomenclature, as in the Forest of Rossendale, near the Yorkshire boundary somewhat south of the centre.

Geology.—The greater part of Lancashire, the central and eastern portions, is occupied by Carboniferous rocks; a broad belt of Triassic strata fringes the west and south; while most of the detached northern portion is made up of Silurian and Ordovician formations. The Carboniferous system includes the great coal-field in which are gathered all the principal manufacturing towns, Colne, Burnley, Blackburn, Chorley, Wigan, Bolton, Preston, Oldham, Rochdale and Manchester. In the centre of the coal-field is an elevated moorland tract formed of the grits and shales of the Millstone Grit series. Part of the small coal-field of Ingleton also lies within the county. Between these two coal basins there is a moderately hilly district in which grits and black shales predominate, with a broad tract of limestone and shales which are well exposed in the quarries at Clitheroe and at Longridge, Chipping, Whalley and Downham. The limestone again appears in the north at Bolton-le-Sands, Burton-in-Kendall, Grange, Ulverston and Dalton-in-Furness. Large pockets of rich iron ore are worked in the limestone in the Furness district. The belt of Trias includes the Bunter sandstone and conglomerate, which ranges from Barrow-in-Furness, through Garstang, Preston, Ormskirk, Liverpool, Warrington and Salford; and Keuper marls, which underlie the surface between the Bunter outcrop and the sea. On the coast there is a considerable development of blown sand between Blackpool and Lytham and between Southport and Seaforth. North of Broughton-in-Furness, Ulverston and Cartmel are the Silurian rocks around Lakes Windermere and Coniston Water, including the Coniston grits and flags and the Brathay flags. These rocks are bounded by the Ordovician Coniston limestone, ranging north-east and south-west, and the volcanic series of Borrowdale. A good deal of the solid geology is obscured in many places by glacial drift, boulder clay and sands.The available coal supply of Lancashire has been estimated at about five thousand millions of tons. In 1852 the amount raised was 8,225,000 tons; in 1899 it was 24,387,475 tons. In the production of coal Lancashire vies with Yorkshire, but each is about one-third below Durham. There are also raised in large quantities—fireclay, limestone, sandstone, slate and salt, which is also obtained from brine. The red hematitic iron obtained in the Furness district is very valuable, but is liable to decrease. The district also produces a fine blue slate. Metals, excepting iron, are unimportant.Climate and Agriculture.—The climate in the hilly districts is frequently cold, but in the more sheltered parts lying to the south and west it is mild and genial. From its westerly situation and the attraction of the hills there is a high rainfall in the hilly districts (e.g.at Bolton the average is 58.71 in.), while the average for the other districts is about 35. The soil after reclamation and drainage is fertile; but, as it is for the most part a strong clayey loam it requires a large amount of labour. In some districts it is more of a peaty nature, and in the Old Red Sandstone districts of the Mersey there is a tract of light sandy loam, easily worked, and well adapted for wheat and potatoes. In many districts the ground has been rendered unfit for agricultural operations by the rubbish from coal-pits. A low proportion (about seven-tenths) of the total area is under cultivation, and of this nearly three-fourths is in permanent pasture, cows being largely kept for the supply of milk to the towns, while in the uplands many sheep are reared. In addition to the cultivated area, about 92,000 acres are under hill pasturage. A gradual increase is noticeable in the acreage under oats, which occupy more than seven-tenths of the area under grain crops, and in that under wheat, to the exclusion of the cultivation of barley. Of green crops the potato is the chief.

Geology.—The greater part of Lancashire, the central and eastern portions, is occupied by Carboniferous rocks; a broad belt of Triassic strata fringes the west and south; while most of the detached northern portion is made up of Silurian and Ordovician formations. The Carboniferous system includes the great coal-field in which are gathered all the principal manufacturing towns, Colne, Burnley, Blackburn, Chorley, Wigan, Bolton, Preston, Oldham, Rochdale and Manchester. In the centre of the coal-field is an elevated moorland tract formed of the grits and shales of the Millstone Grit series. Part of the small coal-field of Ingleton also lies within the county. Between these two coal basins there is a moderately hilly district in which grits and black shales predominate, with a broad tract of limestone and shales which are well exposed in the quarries at Clitheroe and at Longridge, Chipping, Whalley and Downham. The limestone again appears in the north at Bolton-le-Sands, Burton-in-Kendall, Grange, Ulverston and Dalton-in-Furness. Large pockets of rich iron ore are worked in the limestone in the Furness district. The belt of Trias includes the Bunter sandstone and conglomerate, which ranges from Barrow-in-Furness, through Garstang, Preston, Ormskirk, Liverpool, Warrington and Salford; and Keuper marls, which underlie the surface between the Bunter outcrop and the sea. On the coast there is a considerable development of blown sand between Blackpool and Lytham and between Southport and Seaforth. North of Broughton-in-Furness, Ulverston and Cartmel are the Silurian rocks around Lakes Windermere and Coniston Water, including the Coniston grits and flags and the Brathay flags. These rocks are bounded by the Ordovician Coniston limestone, ranging north-east and south-west, and the volcanic series of Borrowdale. A good deal of the solid geology is obscured in many places by glacial drift, boulder clay and sands.

The available coal supply of Lancashire has been estimated at about five thousand millions of tons. In 1852 the amount raised was 8,225,000 tons; in 1899 it was 24,387,475 tons. In the production of coal Lancashire vies with Yorkshire, but each is about one-third below Durham. There are also raised in large quantities—fireclay, limestone, sandstone, slate and salt, which is also obtained from brine. The red hematitic iron obtained in the Furness district is very valuable, but is liable to decrease. The district also produces a fine blue slate. Metals, excepting iron, are unimportant.

Climate and Agriculture.—The climate in the hilly districts is frequently cold, but in the more sheltered parts lying to the south and west it is mild and genial. From its westerly situation and the attraction of the hills there is a high rainfall in the hilly districts (e.g.at Bolton the average is 58.71 in.), while the average for the other districts is about 35. The soil after reclamation and drainage is fertile; but, as it is for the most part a strong clayey loam it requires a large amount of labour. In some districts it is more of a peaty nature, and in the Old Red Sandstone districts of the Mersey there is a tract of light sandy loam, easily worked, and well adapted for wheat and potatoes. In many districts the ground has been rendered unfit for agricultural operations by the rubbish from coal-pits. A low proportion (about seven-tenths) of the total area is under cultivation, and of this nearly three-fourths is in permanent pasture, cows being largely kept for the supply of milk to the towns, while in the uplands many sheep are reared. In addition to the cultivated area, about 92,000 acres are under hill pasturage. A gradual increase is noticeable in the acreage under oats, which occupy more than seven-tenths of the area under grain crops, and in that under wheat, to the exclusion of the cultivation of barley. Of green crops the potato is the chief.

Industries and Trade.—South Lancashire is the principal seat of the cotton manufacture in the world, the trade centring upon Manchester, Oldham and the neighbouring densely populated district. It employs upwards of 400,000 operatives. The worsted, woollen and silk manufactures, flax, hemp and jute industries, though of less importance, employ considerable numbers. Non-textile factories employ about 385,000 hands. The manufacture of machines, appliances, conveyances, tools, &c., are very important, especially in supplying the needs of the immense weaving and spinning industries. For the same purpose there is a large branch of industry in the manufacture of bobbins from the wood grown in the northern districts of the county. Of industries principally confined to certain definite centres there may be mentioned—the manufacture of iron and steel at Barrow-in-Furness, a town of remarkably rapid growth since the middle of the 19th century; the great glass works at St Helens; the watch-making works at Prescot and the leather works at Warrington. Printing, bleaching and dyeing works, paper and chemical works, india-rubber and tobacco manufactures are among the chief of the other resources of this great industrial region. Besides the port of Liverpool, of worldwide importance, the principal ports are Manchester, brought into communication with the sea by the Manchester Ship Canal opened in 1894, Barrow-in-Furness and Fleetwood, while Preston and Lancaster have docks and a considerable shipping trade by the rivers Lune and Ribble respectively. The sea fisheries, for which Fleetwood and Liverpool are the chief ports, are of considerable value.

Communications.—Apart from the Manchester Ship Canal, canal-traffic plays an important part in the industrial region. In 1760 the Sankey canal, 10 m. long, the first canal opened in Britain (apart from very early works), was constructed to carry coal from St Helens to Liverpool. Shortly afterwards the duke of Bridgewater projected the great canal from Manchester across the Irwell to Worsley, completed in 1761 and bearing the name of its originator. The Leeds and Liverpool canal, begun in 1770, connects Liverpool and other important towns with Leeds by a circuitous route of 130 m. The other principal canals are the Rochdale, the Manchester (to Huddersfield) and the Lancaster, connecting Preston and Kendal. A short canal connects Ulverston with Morecambe Bay. A network of railways covers the industrial region. The main line of the London and North Western railway enters the county at Warrington, and runs north through Wigan, Preston, Lancaster and Carnforth. It also serves Liverpool and Manchester, providing the shortest route to each of these cities from London, and shares with the Lancashire and Yorkshire company joint lines to Southport, to Blackpool and to Fleetwood, whence there is regular steamship communication with Belfast. The Lancashire and Yorkshire line serves practically all the important centres as far north as Preston and Fleetwood. All the northern trunk lines from London have services to Manchester and Liverpool. The Cheshire Lines system, worked by a committee of the Great Northern, Great Central and Midland companies, links their systems with the South Lancashire district generally, and maintains lines between Liverpool and Manchester, both these cities with Southport, and numerous branches. Branches of the Midland railway from its main line in Yorkshire serve Lancaster, Morecambe, and Heysham and Carnforth, where connexion is made with the Furness railway to Ulverston, Barrow, Lake Side, Coniston, &c.

Communications.—Apart from the Manchester Ship Canal, canal-traffic plays an important part in the industrial region. In 1760 the Sankey canal, 10 m. long, the first canal opened in Britain (apart from very early works), was constructed to carry coal from St Helens to Liverpool. Shortly afterwards the duke of Bridgewater projected the great canal from Manchester across the Irwell to Worsley, completed in 1761 and bearing the name of its originator. The Leeds and Liverpool canal, begun in 1770, connects Liverpool and other important towns with Leeds by a circuitous route of 130 m. The other principal canals are the Rochdale, the Manchester (to Huddersfield) and the Lancaster, connecting Preston and Kendal. A short canal connects Ulverston with Morecambe Bay. A network of railways covers the industrial region. The main line of the London and North Western railway enters the county at Warrington, and runs north through Wigan, Preston, Lancaster and Carnforth. It also serves Liverpool and Manchester, providing the shortest route to each of these cities from London, and shares with the Lancashire and Yorkshire company joint lines to Southport, to Blackpool and to Fleetwood, whence there is regular steamship communication with Belfast. The Lancashire and Yorkshire line serves practically all the important centres as far north as Preston and Fleetwood. All the northern trunk lines from London have services to Manchester and Liverpool. The Cheshire Lines system, worked by a committee of the Great Northern, Great Central and Midland companies, links their systems with the South Lancashire district generally, and maintains lines between Liverpool and Manchester, both these cities with Southport, and numerous branches. Branches of the Midland railway from its main line in Yorkshire serve Lancaster, Morecambe, and Heysham and Carnforth, where connexion is made with the Furness railway to Ulverston, Barrow, Lake Side, Coniston, &c.

Population and Administration.—The area of the ancient county is 1,203,365 acres. Its population in 1801 was 673,486; in 1891, 3,926,760; and in 1901, 4,406,409. The area of the administrative county is 1,196,753 acres. The distribution of the industrial population may be best appreciated by showing the parliamentary divisions, parliamentary, county and municipal boroughs and urban districts as placed among the four divisions of the ancient county. In the case of urban districts the name of the great town to which each is near or adjacentfollows where necessary. The figures show population in 1901.

Northern Division.—This embraces almost all the county N. of the Ribble, including Furness, and a small area S. of the Ribble estuary. It is considerably the largest of the divisions.Parliamentary divisions, from N. to S.—North Lonsdale, Lancaster, Blackpool, Chorley.Parliamentary, county and municipal boroughs—Barrow-in-Furness (57,586; one member); Preston (112,989; two members).Municipal boroughs—Blackpool (county borough; 47,348), Chorley (26,852), Lancaster (40,329; county town), Morecambe (11,798).Urban districts—Adlington (4523; Chorley), Bispham-with-Norbreck (Blackpool), Carnforth (3040; Lancaster), Croston (2102; Chorley), Dalton-in-Furness (13,020), Fleetwood (12,082), Fulwood (5238; Preston), Grange (1993), Heysham (3381; Morecambe), Kirkham (3693; Preston), Leyland (6865; Chorley), Longridge (4304; Preston), Lytham (7185), Poulon-le-Fylde (2223; Blackpool). Preesall-with-Hackinsall (1423; Fleetwood), St Anne’s-on-the-Sea (6838, a watering-place between Blackpool and Lytham), Thornton (3108; Fleetwood), Ulverston (10,064, in Furness), Withnell (3349; Chorley).North-Eastern-Division.—This lies E. of Preston, and is the smallest of the four.Parliamentary divisions—Accrington, Clitheroe, Darwen, Rossendale.Parliamentary, county and municipal boroughs—Blackburn (127,626; two members); Burnley (97,043; one member).Municipal boroughs—Accrington (43,122), Bacup (22,505), Clitheroe (11,414), Colne (23,000), Darwen (38,212), Haslingden (18,543, extending into South-Eastern division), Nelson (32,816), Rawtenstall (31,053).Urban districts—Barrowford (4959; Colne), Brierfield (7288; Burnley), Church (6463; Accrington), Clayton-le-Moors (8153; Accrington), Great Harwood (12,015; Blackburn), Oswaldtwistle (14,192; Blackburn), Padiham (12,205; Burnley), Rishton (7031; Blackburn), Trawden (2641; Colne), Walton-le-Dale (11,271; Preston).South-Western Division.—This division represents roughly a quadrant with radius of 20 m. drawn from Liverpool.Parliamentary divisions—Bootle, Ince, Leigh, Newton, Ormskirk, Southport, Widnes.Parliamentary boroughs—the city and county and municipal borough of Liverpool (684,958; nine members); the county and municipal boroughs of St Helens (84,410; one member); Wigan (60,764; one member), Warrington (64,242; a part only of the parliamentary borough is in this county).Municipal boroughs—Bootle (58,566), Leigh (40,001), Southport (county borough; 48,083), Widnes (28,580).Urban districts—Abram (6306; Wigan), Allerton (1101; Liverpool), Ashton-in-Makerfield (18,687), Atherton (16,211), Billinge (4232; Wigan), Birkdale (14,197; Southport), Childwall (219; Liverpool), Formby (6060), Golborne (6789; St Helens), Great Crosby (7555; Liverpool), Haydock (8575; St Helens), Hindley (23,504; Wigan), Huyton-with-Roby (4661; St Helens), Ince-in-Makerfield (21,262), Lathom-and-Burscough (7113; Ormskirk), Litherland (10,592; Liverpool), Little Crosby (563; Liverpool), Little Woolton (1091; Liverpool), Much Woolton (4731; Liverpool), Newton-in-Makerfield (16,699), Ormskirk (6857), Orrell (5436; Wigan), Prescot (7855; St Helens), Rainford (3359; St Helens), Skelmersdale (5699; Ormskirk), Standish-with-Langtree (6303; Wigan), Tyldesley-with-Shakerley (14,843), Upholland (4773; Wigan), Waterloo-with-Seaforth (23,102; Liverpool).South-Eastern Division.—This is of about the same area as the South-Western division, and it constitutes the heart of the industrial region.Parliamentary divisions—Eccles, Gorton, Heywood, Middleton, Prestwich, Radcliffe-cum-Farnworth, Stretford, Westhoughton.Parliamentary boroughs—the city and county of a city of Manchester (543,872; six members); with which should be correlated the adjoining county and municipal borough of Salford (220,957; three members), also the county and municipal boroughs of Bolton (168,215; two members), Bury (58,029; one member), Rochdale (83,114; one member), Oldham (137,246; two members), and the municipal borough of Ashton-under-Lyne (43,890). Part only of the last parliamentary borough is within the county, and this division also contains part of the parliamentary boroughs of Stalybridge and Stockport.Municipal boroughs—Eccles (34,369), Heywood (25,458), Middleton (25,178), Mossley (13,452).Urban districts—Aspull (8388; Wigan), Audenshaw (7216; Ashton-under-Lyne), Blackrod (3875; Wigan), Chadderton (24,892; Oldham), Crompton (13,427; Oldham), Denton (14,934; Ashton-under-Lyne), Droylsden (11,087; Manchester), Failsworth (14,152; Manchester), Farnworth (25,925; Bolton), Gorton (26,564; Manchester), Heaton Norris (9474; Stockport). Horwich (15,084; Bolton), Hurst (7145; Ashton-under-Lyne), Irlam (4335; Eccles), Kearsley (9218; Bolton), Lees (3621; Oldham), Levenshulme (11,485; Manchester), Littleborough (11,166; Rochdale), Little Hulton (7294; Bolton), Little Lever (5119; Bolton), Milnrow (8241; Rochdale), Norden (3907; Rochdale), Prestwich (12,839; Manchester), Radcliffe (25,368; Bury), Ramsbottom (15,920; Bury), Royton (14,881; Oldham), Stretford (30,436; Manchester), Swinton-and-Pendlebury (27,005; Manchester), Tottington (6118; Bury), Turton (12,355; Bolton), Urmston (6594; Manchester), Wardle (4427; Rochdale), Westhoughton (14,377; Bolton), Whitefield or Stand (6588; Bury), Whitworth (9578; Rochdale), Worsley (12,462; Eccles).

Northern Division.—This embraces almost all the county N. of the Ribble, including Furness, and a small area S. of the Ribble estuary. It is considerably the largest of the divisions.Parliamentary divisions, from N. to S.—North Lonsdale, Lancaster, Blackpool, Chorley.Parliamentary, county and municipal boroughs—Barrow-in-Furness (57,586; one member); Preston (112,989; two members).Municipal boroughs—Blackpool (county borough; 47,348), Chorley (26,852), Lancaster (40,329; county town), Morecambe (11,798).Urban districts—Adlington (4523; Chorley), Bispham-with-Norbreck (Blackpool), Carnforth (3040; Lancaster), Croston (2102; Chorley), Dalton-in-Furness (13,020), Fleetwood (12,082), Fulwood (5238; Preston), Grange (1993), Heysham (3381; Morecambe), Kirkham (3693; Preston), Leyland (6865; Chorley), Longridge (4304; Preston), Lytham (7185), Poulon-le-Fylde (2223; Blackpool). Preesall-with-Hackinsall (1423; Fleetwood), St Anne’s-on-the-Sea (6838, a watering-place between Blackpool and Lytham), Thornton (3108; Fleetwood), Ulverston (10,064, in Furness), Withnell (3349; Chorley).

North-Eastern-Division.—This lies E. of Preston, and is the smallest of the four.Parliamentary divisions—Accrington, Clitheroe, Darwen, Rossendale.Parliamentary, county and municipal boroughs—Blackburn (127,626; two members); Burnley (97,043; one member).Municipal boroughs—Accrington (43,122), Bacup (22,505), Clitheroe (11,414), Colne (23,000), Darwen (38,212), Haslingden (18,543, extending into South-Eastern division), Nelson (32,816), Rawtenstall (31,053).Urban districts—Barrowford (4959; Colne), Brierfield (7288; Burnley), Church (6463; Accrington), Clayton-le-Moors (8153; Accrington), Great Harwood (12,015; Blackburn), Oswaldtwistle (14,192; Blackburn), Padiham (12,205; Burnley), Rishton (7031; Blackburn), Trawden (2641; Colne), Walton-le-Dale (11,271; Preston).

South-Western Division.—This division represents roughly a quadrant with radius of 20 m. drawn from Liverpool.Parliamentary divisions—Bootle, Ince, Leigh, Newton, Ormskirk, Southport, Widnes.Parliamentary boroughs—the city and county and municipal borough of Liverpool (684,958; nine members); the county and municipal boroughs of St Helens (84,410; one member); Wigan (60,764; one member), Warrington (64,242; a part only of the parliamentary borough is in this county).Municipal boroughs—Bootle (58,566), Leigh (40,001), Southport (county borough; 48,083), Widnes (28,580).Urban districts—Abram (6306; Wigan), Allerton (1101; Liverpool), Ashton-in-Makerfield (18,687), Atherton (16,211), Billinge (4232; Wigan), Birkdale (14,197; Southport), Childwall (219; Liverpool), Formby (6060), Golborne (6789; St Helens), Great Crosby (7555; Liverpool), Haydock (8575; St Helens), Hindley (23,504; Wigan), Huyton-with-Roby (4661; St Helens), Ince-in-Makerfield (21,262), Lathom-and-Burscough (7113; Ormskirk), Litherland (10,592; Liverpool), Little Crosby (563; Liverpool), Little Woolton (1091; Liverpool), Much Woolton (4731; Liverpool), Newton-in-Makerfield (16,699), Ormskirk (6857), Orrell (5436; Wigan), Prescot (7855; St Helens), Rainford (3359; St Helens), Skelmersdale (5699; Ormskirk), Standish-with-Langtree (6303; Wigan), Tyldesley-with-Shakerley (14,843), Upholland (4773; Wigan), Waterloo-with-Seaforth (23,102; Liverpool).

South-Eastern Division.—This is of about the same area as the South-Western division, and it constitutes the heart of the industrial region.Parliamentary divisions—Eccles, Gorton, Heywood, Middleton, Prestwich, Radcliffe-cum-Farnworth, Stretford, Westhoughton.Parliamentary boroughs—the city and county of a city of Manchester (543,872; six members); with which should be correlated the adjoining county and municipal borough of Salford (220,957; three members), also the county and municipal boroughs of Bolton (168,215; two members), Bury (58,029; one member), Rochdale (83,114; one member), Oldham (137,246; two members), and the municipal borough of Ashton-under-Lyne (43,890). Part only of the last parliamentary borough is within the county, and this division also contains part of the parliamentary boroughs of Stalybridge and Stockport.Municipal boroughs—Eccles (34,369), Heywood (25,458), Middleton (25,178), Mossley (13,452).Urban districts—Aspull (8388; Wigan), Audenshaw (7216; Ashton-under-Lyne), Blackrod (3875; Wigan), Chadderton (24,892; Oldham), Crompton (13,427; Oldham), Denton (14,934; Ashton-under-Lyne), Droylsden (11,087; Manchester), Failsworth (14,152; Manchester), Farnworth (25,925; Bolton), Gorton (26,564; Manchester), Heaton Norris (9474; Stockport). Horwich (15,084; Bolton), Hurst (7145; Ashton-under-Lyne), Irlam (4335; Eccles), Kearsley (9218; Bolton), Lees (3621; Oldham), Levenshulme (11,485; Manchester), Littleborough (11,166; Rochdale), Little Hulton (7294; Bolton), Little Lever (5119; Bolton), Milnrow (8241; Rochdale), Norden (3907; Rochdale), Prestwich (12,839; Manchester), Radcliffe (25,368; Bury), Ramsbottom (15,920; Bury), Royton (14,881; Oldham), Stretford (30,436; Manchester), Swinton-and-Pendlebury (27,005; Manchester), Tottington (6118; Bury), Turton (12,355; Bolton), Urmston (6594; Manchester), Wardle (4427; Rochdale), Westhoughton (14,377; Bolton), Whitefield or Stand (6588; Bury), Whitworth (9578; Rochdale), Worsley (12,462; Eccles).

Lancashire is one of the counties palatine. It is attached to the duchy of Lancaster, a crown office, and retains the chancery court for the county palatine. The chancery of the duchy of Lancaster was once a court of appeal for the chancery of the county palatine, but now even its jurisdiction in regard to the estates of the duchy is merely nominal. The chancery of the county palatine has concurrent jurisdiction with the High Court of Chancery in all matters of equity within the county palatine, and independent jurisdiction in regard to a variety of other matters. The county palatine comprises six hundreds.

Lancashire is in the northern circuit, and assizes are held at Lancaster for the north, and at Liverpool and Manchester for the south of the county. There is one court of quarter sessions, and the county is divided into 33 petty sessional divisions. The boroughs of Blackburn, Bolton, Burnley, Liverpool, Manchester, Oldham, Salford and Wigan have separate commissions of the peace and courts of quarter sessions; and those of Accrington, Ashton-under-Lyne, Barrow-in-Furness, Blackpool, Bolton, Bury, Clitheroe, Colne, Darwen, Eccles, Heywood, Lancaster, Middleton, Mossley, Nelson, Preston, Rochdale, St Helens, Southport and Warrington have separate commissions of the peace only. There are 430 civil parishes. Lancashire is mainly in the diocese of Manchester, but parts are in those of Liverpool, Carlisle, Ripon, Chester and Wakefield. There are 787 ecclesiastical parishes or districts wholly or in part within the county.Manchester and Liverpool are each seats of a university and of other important educational institutions. Within the bounds of the county there are many denominational colleges, and near Clitheroe is the famous Roman Catholic college of Stonyhurst. There is a day training college for schoolmasters in connexion with University College, Liverpool, and a day training college for both schoolmasters and schoolmistresses in connexion with Owens College, Manchester. At Edgehill, Liverpool, there is a residential training college for schoolmistresses which takes day pupils, at Liverpool a residential Roman Catholic training college for schoolmasters, and at Warrington a residential training college (Chester, Manchester and Liverpool diocesan) for schoolmistresses.

Lancashire is in the northern circuit, and assizes are held at Lancaster for the north, and at Liverpool and Manchester for the south of the county. There is one court of quarter sessions, and the county is divided into 33 petty sessional divisions. The boroughs of Blackburn, Bolton, Burnley, Liverpool, Manchester, Oldham, Salford and Wigan have separate commissions of the peace and courts of quarter sessions; and those of Accrington, Ashton-under-Lyne, Barrow-in-Furness, Blackpool, Bolton, Bury, Clitheroe, Colne, Darwen, Eccles, Heywood, Lancaster, Middleton, Mossley, Nelson, Preston, Rochdale, St Helens, Southport and Warrington have separate commissions of the peace only. There are 430 civil parishes. Lancashire is mainly in the diocese of Manchester, but parts are in those of Liverpool, Carlisle, Ripon, Chester and Wakefield. There are 787 ecclesiastical parishes or districts wholly or in part within the county.

Manchester and Liverpool are each seats of a university and of other important educational institutions. Within the bounds of the county there are many denominational colleges, and near Clitheroe is the famous Roman Catholic college of Stonyhurst. There is a day training college for schoolmasters in connexion with University College, Liverpool, and a day training college for both schoolmasters and schoolmistresses in connexion with Owens College, Manchester. At Edgehill, Liverpool, there is a residential training college for schoolmistresses which takes day pupils, at Liverpool a residential Roman Catholic training college for schoolmasters, and at Warrington a residential training college (Chester, Manchester and Liverpool diocesan) for schoolmistresses.

History.—The district afterwards known as Lancashire was after the departure of the Romans for many years apparently little better than a waste. It was not until the victory of Æthelfrith, king of Deira, near Chester in 613 cut off the Britons of Wales from those of Lancashire and Cumberland that even Lancashire south of the Ribble was conquered. The part north of the Ribble was not absorbed in the Northumbrian kingdom till the reign of Ecgfrith (670-685). Of the details of this long struggle we know nothing, but to the stubborn resistance made by the British leaders are due the legends of Arthur; and of the twelve great battles he is supposed to have fought against the English, four are traditionally, though probably erroneously, said to have taken place on the river Douglas near Wigan. In the long struggle for supremacy between Mercia and Northumbria, the country between the Mersey and Ribble was sometimes under one, sometimes under the other kingdom. During the 9th century Lancashire was constantly invaded by the Danes, and after the peace of Wedmore (878) it was included in the Danish kingdom of Northumbria. TheA.S. Chroniclerecords the reconquest of the district between the Ribble and Mersey in 923 by the English king, when it appears to have been severed from the kingdom of Northumbria and united to Mercia, but the districts north of the Ribble now comprised in the county belonged to Northumbria until its incorporation with the kingdom of England. The names on the Lancashire coast ending inby, such as Crosby, Formby, Roby, Kirkby, Derby, show where the Danish settlements were thickest. William the Conqueror gave the lands between the Ribble and Mersey, and Amounderness to Roger de Poictou, but at the time of Domesday Book these had passed out of his hand and belonged to the king.

The name Lancashire does not appear in Domesday; the lands between the Ribble and Mersey were included in Cheshire and those north of the Ribble in Yorkshire. Roger de Poictou soon regained his lands, and Rufus added to his possessions the rest of Lonsdale south of the Sands, of which he already held a part; and as he had the Furness fells as well, he owned all that is now known as Lancashire. In 1102 he finally forfeited all his lands, which Henry I. held till, in 1118, he created the honour of Lancaster by incorporating with Roger’s forfeitedlands certain escheated manors in the counties of Nottingham, Derby and Lincoln, and certain royal manors, and bestowed it upon his nephew Stephen, afterwards king. During Stephen’s reign the history of the honour presents certain difficulties, for David of Scotland held the lands north of the Ribble for a time, and in 1147 the earl of Chester held the district between the Ribble and Mersey. Henry II. gave the whole honour to William, Stephen’s son, but in 1164 it came again into the king’s hands until 1189, when Richard I. granted it to his brother John. In 1194, owing to John’s rebellion, it was confiscated and the honour remained with the crown till 1267. In 1229, however, all the crown demesne between the Ribble and Mersey was granted to Ranulf, earl of Chester, and on his death in 1232 came to William Ferrers, earl of Derby, in right of his wife Agnes, sister and co-heir of Ranulf. The Ferrers held it till 1266, when it was confiscated owing to the earl’s rebellion. In 1267 Henry III. granted the honour and county and all the royal demesne therein to his son Edmund, who was created earl of Lancaster. His son, Earl Thomas, married the heiress of Henry de Lacy, earl of Lincoln, and thus obtained the great estates belonging to the de Lacys in Lancashire. On the death of Henry, the first duke of Lancaster, in 1361, the estates, title and honour fell to John of Gaunt in right of his wife Blanche, the duke’s elder daughter, and by the accession of Henry IV., John of Gaunt’s only son, to the throne, the duchy and honour became merged in the crown.

The county of Lancaster is first mentioned in 1169 as contributing 100 marks to the Royal Exchequer for defaults and fines. The creation of the honour decided the boundaries, throwing into it Furness and Cartmel, which geographically belong to Westmorland; Lonsdale and Amounderness, which in Domesday had been surveyed under Yorkshire; and the land between the Ribble and Mersey. In Domesday this district south of the Ribble was divided into the six hundreds of West Derby, Newton, Warrington, Blackburn, Salford and Leyland, but before Henry II.’s reign the hundreds of Warrington and Newton were absorbed in that of West Derby. Neither Amounderness nor Lonsdale was called a hundred in Domesday, but soon after that time the former was treated as a hundred. Ecclesiastically the whole of the county originally belonged to the diocese of York, but after the reconquest of the district between the Ribble and Mersey in 923 this part was placed under the bishop of Lichfield in the archdeaconry of Chester, which was subdivided into the rural deaneries of Manchester, Warrington and Leyland. Up to 1541 the district north of the Ribble belonged to the archdeaconry of Richmond in the diocese of York, and was subdivided into the rural deaneries of Amounderness, Lonsdale and Coupland. In 1541 the diocese of Chester was created, including all Lancashire, which was divided into two archdeaconries: Chester, comprising the rural deaneries of Manchester, Warrington and Blackburn, and Richmond, comprising the deaneries of Amounderness, Furness, Lonsdale and Kendal. In 1847 the diocese of Manchester was created, which included all Lancashire except parts of West Derby, which still belonged to the diocese of Chester, and Furness and Cartmel, which were added to Carlisle in 1856. In 1878 by the creation of the diocese of Liverpool the south-eastern part of the county was subtracted from the Manchester diocese.

No shire court was ever held for the county, but as a duchy and county palatine it has its own special courts. It may have enjoyed palatine jurisdiction under Earl Morcar before the Conquest, but these privileges, if ever exercised, remained in abeyance till 1351, when Henry, duke of Lancaster, received power to have a chancery in the county of Lancaster and to issue writs therefrom under his own seal, as well touching pleas of the crown as any other relating to the common laws, and to have allJura Regaliabelonging to a county palatine. In 1377 the county was erected into a palatinate for John of Gaunt’s life, and in 1390 these rights of jurisdiction were extended and settled in perpetuity on the dukes of Lancaster. The county palatine courts consist of a chancery which dates back at least to 1376, a court of common pleas, the jurisdiction of which was transferred in 1873 by the Judicature Act to the high court of justice, and a court of criminal jurisdiction which in no way differs from the king’s ordinary court. In 1407 the duchy court of Lancaster was created, in which all questions of revenue and dignities affecting the duchy possessions are settled. The chancery of the duchy has been for years practically obsolete. The duchy and county palatine each has its own seal. The office of chancellor of the duchy and county palatine dates back to 1351.

Lancashire is famed for the number of old and important county families living within its borders. The most intimately connected with the history of the county are the Stanleys, whose chief seat is Knowsley Hall. Sir John Stanley early in the 15th century married the heiress of Lathom and thus obtained possession of Lathom and Knowsley. In 1456 the head of the family was created a peer by the title of Baron Stanley and in 1485 raised to the earldom of Derby. The Molyneuxes of Sephton and Croxteth are probably descended from William de Molines, who came to England with William the Conqueror, and is on the roll of Battle Abbey. Roger de Poictou gave him the manor of Sephton, and Richard de Molyneux who held the estate under Henry II. is undoubtedly an ancestor of the family. In 1628 Sir Richard Molyneux was advanced to the peerage of Ireland by the title of Viscount Maryborough, and in 1771 Charles, Lord Maryborough, became earl of Sefton in the peerage of Ireland. His son was created a peer of the United Kingdom as Baron Sefton of Croxteth. The Bootle Wilbrahams, earls of Lathom, are, it is said, descended from John Botyll of Melling, who was alive in 1421, and from the Wilbrahams of Cheshire, who date back at least to Henry III.’s reign. In 1755 the two families intermarried. In 1828 the title of Baron Skelmersdale was bestowed on the head of the family and in 1880 that of earl of Lathorn. The Gerards of Bryn are said to be descended from an old Tuscan family, one of whom came to England in Edward the Confessor’s time, and whose son is mentioned in Domesday. Bryn came into this family by marriage early in the 14th century. Sir Thomas Gerard was created a baronet by James I. in 1611, and in 1876 a peerage was conferred on Sir Robert Gerard. The Gerards of Ince were a collateral branch. The Lindsays, earls of Crawford and Balcarres, are representative on the female side of the Bradshaighs of Haigh Hall, who are said to be of Saxon origin. Other great Lancashire families are the Hoghtons of Hoghton Tower, dating back to the 12th century, the Blundells of Ince Blundell, who are said to have held the manor since the 12th century, now represented by the Weld-Blundells, the Tyldesleys of Tyldesley, now extinct, and the Butlers of Bewsey, barons of Warrington, of whom the last male heir died in 1586.

Lancashire is famed for the number of old and important county families living within its borders. The most intimately connected with the history of the county are the Stanleys, whose chief seat is Knowsley Hall. Sir John Stanley early in the 15th century married the heiress of Lathom and thus obtained possession of Lathom and Knowsley. In 1456 the head of the family was created a peer by the title of Baron Stanley and in 1485 raised to the earldom of Derby. The Molyneuxes of Sephton and Croxteth are probably descended from William de Molines, who came to England with William the Conqueror, and is on the roll of Battle Abbey. Roger de Poictou gave him the manor of Sephton, and Richard de Molyneux who held the estate under Henry II. is undoubtedly an ancestor of the family. In 1628 Sir Richard Molyneux was advanced to the peerage of Ireland by the title of Viscount Maryborough, and in 1771 Charles, Lord Maryborough, became earl of Sefton in the peerage of Ireland. His son was created a peer of the United Kingdom as Baron Sefton of Croxteth. The Bootle Wilbrahams, earls of Lathom, are, it is said, descended from John Botyll of Melling, who was alive in 1421, and from the Wilbrahams of Cheshire, who date back at least to Henry III.’s reign. In 1755 the two families intermarried. In 1828 the title of Baron Skelmersdale was bestowed on the head of the family and in 1880 that of earl of Lathorn. The Gerards of Bryn are said to be descended from an old Tuscan family, one of whom came to England in Edward the Confessor’s time, and whose son is mentioned in Domesday. Bryn came into this family by marriage early in the 14th century. Sir Thomas Gerard was created a baronet by James I. in 1611, and in 1876 a peerage was conferred on Sir Robert Gerard. The Gerards of Ince were a collateral branch. The Lindsays, earls of Crawford and Balcarres, are representative on the female side of the Bradshaighs of Haigh Hall, who are said to be of Saxon origin. Other great Lancashire families are the Hoghtons of Hoghton Tower, dating back to the 12th century, the Blundells of Ince Blundell, who are said to have held the manor since the 12th century, now represented by the Weld-Blundells, the Tyldesleys of Tyldesley, now extinct, and the Butlers of Bewsey, barons of Warrington, of whom the last male heir died in 1586.

At the close of the 12th and during the 13th century there was a considerable advance in the importance of the towns; in 1199 Lancaster became a borough, in 1207 Liverpool, in 1230 Salford, in 1246 Wigan, and in 1301 Manchester. The Scottish wars were a great drain to the county, not only because the north part was subject to frequent invasions, as in 1322, but because some of the best blood was taken for these wars. In 1297 Lancashire raised 1000 men, and at the battle of Falkirk (1298) 1000 Lancashire soldiers were in the vanguard, led by Henry de Lacy, earl of Lincoln. In 1349 the county was visited by the Black Death and a record exists of its ravages in Amounderness. In ten parishes between September 1349 and January 1350, 13,180 persons perished. At Preston 3000 died, at Lancaster 3000, at Garstang 2000 and at Kirkham 3000. From the effects of this plague Lancashire was apparently slow to recover; its boroughs ceased to return members early in the 14th century and trade had not yet made any great advance. The drain of the Wars of the Roses on the county must also have been heavy, although none of the battles was fought within its borders; Lord Stanley’s force of 5000 raised in Lancashire and Cheshire virtually decided the battle of Bosworth Field. The poverty of the county is shown by the fact that out of £40,000 granted in 1504 by parliament to the king, Lancashire’s share was only £318. At the battle of Flodden (1513) the Lancashire archers led by Sir Edward Stanley almost totally destroyed the Highlanders on the right Scottish wing and greatly contributed to the victory. Under the Tudors the county prospered; the parliamentary boroughs once more began to return members, the towns increased in size, many halls were built by the gentry and trade increased.


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