Page:The National Gazetteer - A Topographical Dictionary of the British Islands, Volume 2.djvu/712

Rh LONGFORD. 704 LONGFORD. king's use by virtue of the Act of Absentees, and dis- posed of to patentees. The plantation did not take effect to any great extent ; and when the civil war commenced in 1641, the entire county appears to have been in the possession of the O'Farrels, except Longford Castle and Castle Forbes, both of which were then besieged and taken by the Irish for the O'Favrels. But the ultimate triumph of Cromwell's forces entirely reversed the fate of the country, and the O'Farrels lost both their pro- perty and influence. The confiscations which ensued extended over nearly the entire county, and introduced a new proprietary, most of whom were of English de- scent. The population in 1851 was 85,350, and, in 1861 , 71,69-i, and the net annual value of property in the county under the Tenement Valuation Act, is 151,598. The surface is for the most part flat, and, in many places, overspread with large 'tracts of bog.. Towards the N., where Longford borders on the county of Leitrim, it rises into bleak and sterile mountains ; but towards the S., it is much more fertile and well cultivated, espe- cially in the valley of the Inny. In the S. the_ only considerable eminence is Slieve Gauldry, which rises to the height of 650 feet, and consists of a mass of sand- stone, resting upon a stratum of stratified limestone, which constitutes the prevailing formation of the southern portion of the county and the tract in the north- eastern part of it. The hilly district in the N.W. is chiefly clay slate, of the graywacke formation, so pre- valent in the adjoining county of Cavan. The principal range of hills is the Clonhugh, which extends for about 10 miles in a south-westerly direction, attaining an alti- tude of 912 feet at Cairn Clonhugh. The line of division between the limestone and clay-slate proceeds from the Camlin river, near Longford, by St. Johnstown, between Lough Kinale and Lough Gownagh, to the head of Lough Sheelin. To the W. of the clay-slate formation in the north-western extremity of the county, is a considerable tract of sandstone, which stretches on both sides of the Shannon into the counties of Roscommon and Leitrim. Marly clay in beds, from 1 foot to 10 feet thick, under- lies many of the boggy tracts, which are of great extent, and have an average depth of 30 feet. In these bogs the scented myrtle, and many rare species of plants, are found, particularly in the barony of Longford. Near Ballymahon, a marble of a deep grey colour is raised, and near Lough Gownagh is a small tract of millstone grit. The only mineral treasures at present discovered are lead ore and ironstone rock. .This latter, mixed with coal shale, is abundant in the vicinity of Lough Gownagh and Beulaghy, not in thin layers like those of the Arigna district, but regular in formation and of a deep red colour. No systematic attempts have, however, yet been made to work either of these minerals ; ochres of .various colours are common. Notwithstanding the abundance of lime- stone, sandstone, and gravel, pure water is rather scarce and the streams few. The whole drainage of the county, except a few streams that fall into Lough Gownagh, is towards the Shannon. This noble river connects the county with the important line of navigation, extending from Lough Allen to the city of Limerick ; and, by an- other line, through Longford, with the city, of Dublin. On first entering the county, the Shannon expands into Lough Forbes, about 3 miles long by 1J mile broad, and here receives the waters of the Ehinn flowing out of Leitrim ; about 2 miles farther on it receives the waters of the Camlin, which rises near the eastern boundary of the county, and pursues a winding course of 20 miles towards the W. After passing the county town, it receives the waters of the Keenagh and an- other stream from the S. ; then those of the Fallen and O wnamount, two insignificant streams. The Shan- non then expands into the extensive lake of Lough Ree, the banks of which are diversified by deep bays, rugged headlands, and numerous islands. At this point itis joined by the Inny, which flows through a rich country in a winding course by Ballymahon, and forms part of the southern boundary of the county. Few rivers present so many facilities for water carriage as the Inny, the total fall from Finea to the Shannon being only 90 feet, and the main obstructions to its navigation the two shallows between the Shannon and Ballymahon, and the ridge of rocks between the latter and Newcastle. The waters of Lough Ree, swollen by numerous streams in winter, rise to an 'average height of 7 feet above the summer level, and inundate the country to a wide extent on its banks. The islands of this lake are numerous, and some of them large : those within the coiinty of Longford are All Saints, Inchban, Innis-bofin, Innisdoran, Inchy- nough, and Quakers' Island. Besides the loughs already mentioned, many smaller lakes diversify the surface of the county, as Loughs Gownagh and Kinale, between this county and Cavan ; also, Loughs Bon, Bonnow,' Drum, Derry, Drumurry, Doogary, Gurteen, 'fully, and Glin. The Royal Canal passes through, the county in a westerly direction, entering from Westmeath by an aqueduct over the Inny, near Tinellick, and joins tho Shannon at Richmond Harbour, in its course having sent out a branch northwards to the town of Longford." Two branches of the Midland Great .Western railway, pass through the county from Mullingar to Longford and Cavan. The roads are numerous and well made, but aro in general wet, owing .to the watercourses being neg- lected. The soil varies .very considerably both in* quality, and composition, being in parts a. light thin mould, 'in others a .deep loamy clay, alternating with' bog and marl, while the best lands in the south are a rich vegetable mould, resting on blue clay or limestone gravel." Largo tracts in the north are still in a state of nature, 1 and are of little value except as sheep walks, while tho rich lands of the south, especially in the barony of Gra- nard, produce herbage of the finest quality for grazing,' and the high lands between Edgeworthstown and Long- ford yield heavy grain crops. The climate, however, of this part of Ireland being mild and damp, is, on tho whole, better adapted for pastures and green-crops, and, under a better system of drainage, would rank with the' best grazing lands in the kingdom. The lower grounds,- which are chiefly in pasture, produce great .varieties of acidulous plants,' occasioned by the overflowing of the rivers and by the accumulation of the surface .waters, which have at present no sufficient outlets. The occupations are tillage and grazing, chiefly the latter. : A few manu- factures only, as linen cloth, linen yarn, flannels, friezes, and coarse woollens, are carried on chiefly for domestic consumption. The county returns two members to the Imperial Parliament, and had a constituency in 1859 of 2,869. It is in Ardagh diocese, with a small portion in Meath. It is divided into 6 baronies, Ardagh, Granard, Longford, Moydow, Rathcline, and Shrule, comprising 26 parishes. The principal towns are Longford, the county town, where the Assizes arc held, and where are the county prison and county infirmary, with a popula- tion in 1861, of 4,535, Granard with a population of 1,665, and Ballymahon, at all these quarter sessions are held, and each is tho seat of a Poor-law. Union. The county is within the N.W.- circuit, and forms part of tho military district of Dublin, where are barracks fur cavalry and military. The ' constabulary force has its headquarters at Longford, but the staff of the cun militia is stationed at Newtown-Forbes. Fossil ren, of many extinct animals have been discovered in the limestone caverns and fissures ; also, bones and hoi ; the elk and red deer in the marl at the foot of the L"s< and beneath several of the bogs. Tho remains of anti- quity are .very few. .A large rath, usually called th Moat of Granard, stands at one end of the main that town ; another, called Lisardowlin, situate near thu road from Longford to Edgeworthstown, was prob connected with the rampart of Dunela, which runs i . Lough Kinale to Lough Gownagh, about 8 miles, an supposed to have formed part of the division between the ancient kingdoms of Meath and "Ulster. Monastic insti- tutions were numerous and well endowed ; the Abbey ( 'f Longford is said to have been originally founded by St. Patrick, and was afterwards rebuilt by O'l'V Prince of Annaly, in 1100. There were also abbr priories, at Abbeyshrule, Ardagh, Clone, Clonebrone. Dery, Druimchci, Granard, where are ruins of a round