ARMAGH (County of), an inland county, in the province of ULSTER, bounded on the north by Lough Neagh, on the east by the county of Down, on the south-east by that of Louth, on the south-west by Monaghan, and on the west and north-west by Tyrone: it is situated between 54° 3' and 54° 31' (N. Lat), and between 6° 14' and 6° 45' (W. Lon.); and comprises, according to the Ordnance survey, 328,076 statute acres, of which 267,317 acres are tillable, 17,941 are covered with water, and the remainder is mountain and bog. The population, in 1821, was 197,427; and, in 1831, 220,134.
This tract is supposed to have been part of that named by Ptolemy as the territories of the Vinderii and Voluntii: it afterwards formed part of the district called Orgial, which also comprised the counties of Louth and Monaghan. The formation of this part of Ireland into a separate dominion is said to have taken place so early as the year 332, after the battle of Achaighleth-derg, in Fermoy, in which, as recorded by Tigernach, abbot of Clonmacnois, who died in 1068, Fergus Feagha, sone of Froechair the Brave, the last of the Ultonian kings who resided in Eamania, was killed by the three Collas, who then expelled the Ultonians from that part of the province to the south of Lough Neagh, and formed it into an independent state, to which they gave the name of Orgial, afterwards corrupted into Oriel or Uriel, names by which it was distinguished to the beginning of the seventeenth century.
The county was made shire ground, under its present name, in 1586, by the lord-deputy, Sir John Perrott, who, not relying with confidence on the vigilance and care of Henry O'Nial and Sir Henry Bagnell, to whom the government of Ulster had been entrusted, projected the division of the greater part of that province into seven counties, of which Armagh was one, and took its name from the chief town in it. For each of these counties he appointed sheriffs, commissioners of the peace, coroners, and other officers. Previously to this arrangement, the chief part of the property of the county had centred in the families of the O'Nials, the MacCahans, and the O'Hanlons. At the commencement of the seventeenth century, it was principally vested in those of MacHenry, Acheson, O'Nial, Brownlow, and O'Hanlon, exclusively of the great territories settled on Moharty, which the Mac Cahans had forfeited in rebellioni, and a large tract of country called Oirther, afterwards Orior, a district in the southern part, which also escheated to the crown by rebellion of a branch of the O'Hanlons. According to a project for planting, by Jas. I., the whole of the arable and pasture land, amounting to 77,580 acres, was to be allotted in 61 proportions of three classes of 2000, 1500, and 1000 acres each, among the English and Scottish undertakers, the servitors, and the Irish natives. A portion was also assigned to the primate, another for glebes for the incumbents (of whom there was to be one for each proportion), another for the four corporate towns of Armagh, Mountnorris, Charlemont and Tanderagee, and a fourth for a free grammar school. The native Irish were to be distributed among a few of the several proportions, with the exception of the swordsmen, who were to migrate into waste lands in Connaught and Munster. The project, which was but partially effected, was not acted upon until 1609, when a royal commission was issued to inquire into the king's title to the escheated and forfeited lands in Ulster, with a view to the plantation there. Inquisitions were consequently held, the return of which for Armagh, made in August of the same year, states that the county was then divided into the five baronies of Armaghe, Toaghriny, Orier, Fuighes, and Onylane or O'Nealane, and enumerates with great particularity the names and tenures of the proprietors. In 1618, a second commission was issued to Captain Pynnar and others, to ascertain how far the settlers located there in the intervening period had fulfilled the terms of their agreement. It is somewhat remarkable that, although the inquisition names five baronies, three only are noticed in Pynnar's survey; those of Armaghe and Toaghriny being omitted, probably because they contained no forfeited property. The number of the proportions specified in the survey are but 22, eleven of which, situated in O'Neylan, were in the hands of English undertakers; five in the Fuighes, in those of Scottish undertakers; and seven in Orier were allotted to servitors and natives. The number of tenants and men amounted to 319 of the former, and 679 of the latter; the number in Orier is not given.
The county is partly in the diocese of Dromore, but chiefly in that of Armagh. For civil purposes it is now divided into the baronies of Armagh, Turaney, O'Neilland East, O'Neilland West, Upper Fews, Lower Fews, Upper Orior, and Lower Orior. It contains the city and borough of Armagh; part of the borough, sea-port, and market-town of Newry; the market and post-towns of Lurgan, Portadown, Tanderagee, Market-hill, and Newtown-Hamilton; the disfranchised borough of Charlemont; the post-towns of Richhill, Keady, Blackwatertown, Loughgall, Tynan, Forkhill, and Flurry-Bridge; and the market-towns of Middleton and Crossmeglan, which, with Killylea, have each a penny post. Prior to the Union it sent six members to the Irish parliament, two for the county at large, and two for each of the boroughs; but at present its representation consists of three members in the Imperial parliament, two for the county at large, and one for the borough of Armagh. The election takes place at Armagh; and the constituency, as registered in Oct. 1836, consisted of 384 £50, 324 £20, and 2384 £10 freeholders; 5 £50 and 19 £20 rent-chargers; and 122 £20 and 573 £10 leaseholders; making a total of 3811. It is in the north-east circuit: the assizes are held at Armagh where the county court-house and gaol are situated; and quarter sissions at Armagh, Lurgan, Market-hill, and Ballybott, of which the three last have each a court-house and bridewell. The number os persons charged with criminal offences and committed to the county gaol, in 1835, was 385, and of civil bill commitments, 111. The local government is vested in a lieutenant, vice-lieutenant, 13 deputy-lieutenants, and 63 other magistrates; besides whom there are the usual county officers, including three coroners. There are 17 constabulary police stations, having in the whole a force of a stipendiary magistrate, sub-inspector, paymaster, 5 chief and 19 subordinate constables, and 99 men, with 5 horses, maintained equally by Grand Jury presentments and by Government. The amount of Grand Jury presentments, for 1835, was £27,259. 2. 3½., of which £4704. 0. 3. was for the public roads of the county at large; £9974. 1. 7½. for the public roads, being the baronial charge; £1475. 11. 4. in repayment of loans advanced by Government; £2279. 10. 7. for the police, and £8825. 18. 6. for public establishments, officers' salaries, buildings, &c. The public charitable instutions are a district lunatic asylum, and the county infirmary and fever hospital at Armagh; and dispensaries at Crossmeglin, Forkhill, Market-hill, Jonesborough, Keady, Blackwatertown, Seagoe, Loughgall, Richhill, Lurgan, Newtown-Hamilton, Poyntz-Pass, Tynan, Portadown, Tanderagee and Ballybott, supported by equal Grad Jury presentments and private subscriptions. There are also dispensaries at Tanderagee, Portadown, and Tullyhappy, built and supported by the Earl and Countess of Mandeville; and a fever hospital at Middleton, built and supported by the Trustees of Bishop Sterne's munificent bequest. In the military arrangements this county is within the northern district, of which Armagh is the head-quarters, where there are an ordnance-depôt and an infantry barrack constructed to accommodate 12 officers, 174 men, and 5 horses: at Charlemont there is a fort, with an artillery barrack for 5 officers, 151 men, and 79 horses, to which is attached an hospital for 22 patients.
The northern verge of the county, near Lough Neagh, the north-western adjoining Tyrone, and the neighbourhoods of Armagh, Market-hill, and Tanderagee, are level; the remainder is hilly, rising in the sourthern parts into mountains of considerable elevation. The highest is Slieve Gullion, rising, according to the Ordnance survey, 1893 feet above the level of the sea; it is about seven miles from the southern border, and is considered to be the loftiest point of land in Ulster, except Slieve Donard, in the neighbouring county of Down. Slieve Gullion sinks on the east into the Fathom Hills, which skirt the Newry water. One of the finest and most extensive prospects in Ulster is obtained from its summit, which commands the bay of Dundalk; and the bold and picturesque features of mountain scenery are confined to this immediate vicinity, including the Doobrin mountains and the neighbourhood of Forkhill. Westward to the Fews, the country exhibits a chain of abrupt hills, the greater part of which can never be reduced to a state of profitable cultivation. Futher west are the Fews mountains, a subordinate range, lying in a direction from south-east to north-west. The fertility of the more level districts towards the eastern, northern and north-western confines is very remarkable, especially in the views from Richhill, the numerous demesnes being sufficiently wooded to ornament the whole county, and the surface generally varied by pleasing undulations. From the shores of Lough Neagh, however, extend considerable tracts of low, marshy, and boggy land. The other lakes are few and small: that of Camlough, romantically situated on the northern verge of Slieve Gullion, is the largest. Lough Clay, in the western part of the county, which gives rise to one of the branches of the Callen river, is the next in size; but neither of them would be noticed for extent or beauty if situated in some of the neighbouring counties. A chain of small lakes occupying the south-western boundary of the county is valuable from the supply of water afforded by them to the mills in their neighbourhood. Coney Island, near the southern shore of Lough Neagh, and between the mounts of the Blackwater and Bann rivers, is the only island in the county; it is uninhabited. The climate is more genial than most of the other counties in Ulster, as is evinced by the greater forwardness of the harvests: this advantage has been attributed to the nature of the soil and subsoil, the gentle undulation of the surface, the absence of moor or marshy land, and the protection by mountains from the cooling breezes of the sea.
The soil is generally very fertile, especially in the northern part, the surface of which is a rich brown loam, tolerable deep, on a substratum of clay or gravel. There is an abundance of limestone in the vicinity of Armagh, and in Kilmore and other places; and there are quarries near Lough Neagh, but the stone lies so deep, and they are subject to such a flow of water, as to be of little practical use. Towards Charlemont there is much bog, which yields red ashes, and is easily reclaimable; the substratum of this is a rich limestone. The eastern part of the county consists of a light friable soil. In the south the country is rocky and barren: huge rocks of granite are found on the surface promiscuously mixed with blocks of limestone, as if thrown together by some convulstion of nature. All the limestone districts make good tillage and meadow ground: the natural meadow found on the banks of the rivers, and formed of a very deep brown loam, yields great crops without manure. The hilly district is generally of a deep retentive soil on a gravelly but not calcareous substratum: a decayed freestone gravel, highly tinged with ferruginous ore, is partially found here: the subsoil is sometimes clay-slate. In these districts heath is peculiarly vigorous, except where the judicious application of lime has compelled it to give place to a more productive vegetation. Except neat Newtown-Hamilton, there is but little bog among these hills. The valleys which lie between them have a rich and loamy soil, which yields much grain, and does not abound in aquatic plants, although the poa fluitans grows in them in great luxuriance. The general inequality of surface which pervades the county affords great facilities for drainage. In consequence of the dense population the farms are generally very small, and much land is tilled with the spade. Wheat is a very general crop in the baronies of Armagh, The O'Neillands, and Turaney; the main crops in the other baronies are oats, flax, and potatoes. In the smaller farms potatoes constitute the first and second crops, sometimes even a third; and afterwards flax occupies a portion of the potatoe plot, and barley the remainder, if the soil be dry and fine, but if otherwise, crops of oats are taken in succession. The treatment of the wheat crop consists of one harrowing and one ploughing, to level the potatoe furrows; if two crops of potatoes have preceded, a small quantity of ashes is scattered over the surface. The seed most in use is the red Lammas wheat, and the quantity sown is about three bushels to the acre. Potatoe oats are commonly sown on the best lands; black oats, and sometimes white oats, on land manured with lime, in the mountainous districts; this latter species, when sown on mountain land not previously manured and drained, will degenerate into a black grain in two or three seasons. Flax is invariably sown on potatoe ground, the plot being tilled with the spade, but not rolled: Dutch seed is sown on heavy soils, American on light soils. The seed is not saved, and therefor the plant is pulled just before it changes colour, from an opinion that when thus prepared it makes finer yarn. More seed was sown in 1835 then was ever before known, in consequence of the increased demand from the spinners in England and Ireland. The pasturage is abundant and nutritious; and though there are no extensive dairies, cows are kept by all the small farmers of the rich northern districts, whence much butter is sent to the Belfast market: a considerable quantity of butter, generally made up in small firkins, is also sent to Armagh and Newry for exportation. The state of agriculture in modern times has very much improved; gentlemen and large farmers have introduced all the improved agricultural implements, with the practice of drainage, irrigation, and rotation crops. Mangel-wurzel, turnips, clover, and all other green crops are now generally cultivated even upon the smallest farms, particularly around Market-hill, Tanderagee, Banagher, and other places, where the greatest encouragement is given by Lords Gosford, Mandeville, and Charlemont, and by Col. Close and other resident gentlemen, who have established farming societies and expend large sums annually in premiums. The Durham, Hereford, North Devon, Leicester, Ayrshire, and other breeds of cattle have been introduced, and by judicious crosses a very superior stock has been raised: some farmers on good soils have also brought over the Alderney breed, which thrives remarkably well; but in some of the mountain districts the old long-horned breed of the country is still preferred, and a cross between it and the old Leicester appears to suit both soil and climate, as they grow to a large size, give great quantities of milk, and fatten rapidly. The breed of sheep and horses has also been greatly improved; the former kind of stock is chiefly in the possession of gentlemen and large farmers. The horses used in farming are mostly a light active kind; but the best hunters and saddle-horses are brought hither by dealers from other counties. Numerous herds of young cattle are reared on the Fews mountains, which are the only part of the county where grass farms are extensive. Goats are numerous, and are allowed to graze at liberty in the mountainous districts. Hogs are fattened in great numbers; the gentry prefer the Chinese breed, but the Berkshire is preferred by the country people, as being equally prolific and more profitable. Lime and dung are the general manures; the former is usually mixed with clay for the culture of potatoes, and is also applied to grass lands as a surface dressing preparatory to tillage, sometimes even three years before the sod is broken, as being deemed more effective than manuring the broken ground; the average quantity of lime laid on an acre is from 30 to 40 barrels. Thorn hedges well kept are the common fences in the richer districts, and with scattered timber trees and numerous orchards give them a rich woody appearance. In the mountainous district, too, the same fences are rising in every direction. Many parts of the county, particularly in the barony of Armagh, are decorated with both old and new timber: and in comparison with neighbouring districts it has a well-wooded appearance; but there are no extensive woodlands, although there is, near Armagh, a large public nursery of forest trees.
The geological features of the county are various and interesting. The mountain of Slieve Gullion, in its south-eastern extremity, is an offset of the granite district of Down, and is remarkable for the varieties of which it is composed. It is in the form of a truncated cone, and presents on some sides mural precipices several hundred feet in height, from which it acquires an appearance of greater elevation than it really attains: the summit is flat, and on it is a lake of considerable extent. The granite of this mountain, particularly that procured near the summit, is frequently used for mill-stones, being extremely hard and fine-grained, and composed of quartz, feldspar, mica, and hornblende. This, indeed, is here the common composition of this primitive rock, the feldspar being grey and the mica black. Sometimes the hornblende is absent, in which case the rock is found to be a pure granite; and at others it graduates into a beautiful sienite composed of flesh-coloured feldspar and hornblende. Flesh-coloured veins of quartz are also found to variegate the granite, in a beautiful manner, in several places. On the south, towards Jonesborough, the sienite succeeds to the granite, and afterwards passes into porphyry, which is succeeded by silicious slate. The Newry mountains and the Fathom hills are composed of granite. Around Camlough mica slate is found in vast beds. Westward the granite district of Slieve Gullion extends to the hill above Larkin-mill, on the western declivity of which the granite basis is covered by almost vertical strata, composed first of an aggregation of quartz and mica with steatite, which in the distance of about a quarter of a mile is occasionally interstratified with greenish grey clay-slate, of which the strata still further west are wholly composed. Several slate quarries have here been opened and partially worked, but none with spirit or skill: the principal are at Dorcy, Newtown-Hanilton, Cregan-Duff, and in the vicinity of Crossmeglan. Further distant this becomes grauwacke slate, by being interstratified with grauwacke. In the neighbourhood of Market-hill the strata comprise also hornblende slate and greenstone porphyry. Sandstone is also connected with this district; there is a quarry of remarkably fine freestone at Grange; and on the surface of the southern confines is seen the intermixture of grit and limestone rocks above noticed. Trap rocks, forming a hard stone varying in hue between dark green and blue, here called whin, are found in various places in huge blocks and boulders, or long narrow stones. The substratum of the eastern portion of the county varies between a silicious schistus and an argillaceous deposit, forming a grauwacke district, which extends across to the western confines of the county. The west and middle of the county is limestone, which is generally white, except in the vicinity of the city of Armagh, where it assumes a red tinge, exhibiting that colour more distinctly as it approaches the town, improving also in quality, and increasing in the varieties of its shades. The minerals, as connected with metallurgy, are so few as scarcely to deserve notice, lead only excepted, a mine of which was worked in the vicinity of Keady, on a property held by the Earl of Farnham, under Dublin College; but after much expenditure the operations were discontinued in consequence of the loss incurred, which, however, has been attributed to the want of skilful or honest superintendence. Lead ore has also been found near Market-hill, in several places near Newtown-Hamilton, on the demesne of Ballymoyer, near Hockley, in Slieve Cross, near Forkhill, and in the parish of Middleton. Some indications of iron, imperfect lead, regulus of manganese, and antimony, have been found in a few spots. The other mineral substances found here are potters' clay and a variety of ochres. Various kinds of timber, particularly oak, pine and yew, have been raised out of the bogs; petrified wood is found on the shores of Lough Neagh; and fern, spleenwort, and mosses have been discovered in the heart of slaty stones.
The woollen trade flourished extensively in this county until interrupted by the legislative measures enacted by William III., and cloth of every description was manufactured. The linen manufacture is now pursued in all its branches, the finest goods being produced in the northern parts. The extent of the manufacture cannot easily be ascertained, because much comes in from the outskirts of the neighbouring counties, though the excess thus arising is most probably counterbalanced by the goods sent out of Armagh to the markets in the adjoining counties. At the commencement of the present century, the value of its produce annually was estimated at £300,000, and at present exceeds £500,000. Large capitals are employed by bleachers, who purchase linen and bleach it on their own account; the principal district is on the river Callan, at Keady. Considerable sums are also employed in the purchase of yarn, which is given out to the weaver to manufacture. Woollen goods are made solely for home consumption, and in only small quantities. Manufactories for the necessaries of life in greatest demand, such as candles, leather, soap, beer, &c. are numerous; and there are mills for dressing flax and spinning linen yarn, and numerous large flour-mills.
The two principal rivers are the Blackwater and the Bann, which chiefly flow along the north-eastern and north-western boundaries of the county, the former discharging itself into the western side of Lough Neagh, and the latter into the souther part of the same lake, at Bann-foot ferry. The Newry water, after flowing through a narrow valley between the counties of Down and Armagh, empties itself into the bay of Carlingford, below Newry. The Callan joins the Blackwater below Charlemont: the Cusheir falls into the Bann at its junction with the Newry canal; and the Camlough, flowing from the lake of the same name, discharges itself into the Newry water. This last named river, during its short course of five miles, supplies numerous bleach-works, and corn, flour, and flax mills: its falls are so rapid that the tail race of the higher mill forms the head water of the next lower. The Newtown-Hamilton river is joined by the Tara, and flows into Dundalk bay, into which also the Flurry or Fleury, and the Fane, empty themselves. The total number of main and branch streams is eighteen, and the combined lengths of all are 165 miles. The mouths of those which flow into Lough Neagh have a fine kind of salmon trout, frequently 30lb. in weight: the common trout is abundant and large, as are also pike, eels, bream, and roach. An inland navigation along the border of the counties of Armagh and Down, from Newry to Lough Neagh, by the aid of the Bann and Newry water, was the first line of canal executed in Ireland. Commencing at the tideway at Fathom, it proceeds to Newry, and admits vessels drawing nine or ten feet of water, having at each end a sea lock. From Newry to the point where the Bann is navigable, a distance of fifteen miles, is a canal for barges of from 40 to 60 tons, chiefly fed from Lough Brickland and Lough Shark, in the county of Down. The river Bann, from its junction with the canal to Lough Neagh, a distance of eleven miles and a half, completes the navigation, opening a communication with Belfast by the Lagan navigation, and with the Tyrone collieries by the Coal Island or Blackwater navigation. The chief trade on this canal arises from the import of bleaching materials, flax-seed, iron, timber, coal, and foreign produce from Newry; and from the export of agricultural produce, yarn linen, fire-bricks, pottery, &c. The canal form Lough Erne to Lough Neagh, now in progress, enters this county near Tynan, and passes by Caledon, Blackwatertown, and Charlemont to its junction with the river Blackwater above Verner's bridge, and finally with Lough Neagh. A line of railway from Dublin to Armag, and thence to Belfast, and another from Armagh to Coleraine, have been projected. The roads are generally well laid out, and many of them of late have been much improved.
Among the relics of antiquity are the remains of the fortress of Eamania, near Armagh, once the royal seat of the kings of Ulster. The Danes' Cast is an extensive line of fortification in the south eastern part of the county, and stretching into the county of Down. The tumulus said to mark the burial-place of "Nial of the hundred battles" is still visible on the banks of the Callan. The Vicar's Cairn, or Cairn-na-Managhan, is situated near the city of Armagh. Cairn Bann is in Orior barony, near Newry. A tumulus in Killery parish contains an artificial cavern. Two ancient brazen weapons were found in a bog near Carrick, where a battle is said to have been fought in 941. Spears, battle-axes, skeyns, swords, the golden torques, and collars, rings, amulets, and medals of gold, also various ornaments of silver, jet, amber, &c., have been found in different places, and are mostly preserved. Near Hamilton's Bawn, in 1816, was found the entire skeleton of an elk, of which the head and horns were placed in the hall of the Infirmary at Armagh; and in the same year also the body of a trooper was discovered in a bog near Charlemont, of which the dress and armour appeared to be of the reign of Elizabeth. The religious houses, besides those of the city of Armagh, of which any memorial has been handed down to use were Clonfeacle, Killevey or Kilsleve, Kilmore, Stradhailloyse, and Tahellen. The most remarkable military remains are Tyrone's ditches, near Poyntz Pass, Navan fort, the castles of Criff-Keirn and Argonell, the castle in the pass of Moyrath, and Castle Roe.
The peasantry are in possession of superior comforts in their habitations as well as in food and clothing, which cannot be attributed solely to the linen manufacture, as their neighbours of the same trade in the adjoining counties of Cavan and Monaghan are far behind them in this respect. The county possesses sufficient fuel for domestic consumption; but coal is imported from England by the Newry canal, and from the county of Tyrone by the Blackwater. In no other county do the working classes consume so much animal food. The general diffusion of the population is neither the result of a pre-determined plan, nor of mere accident: it arises from the nature of the linen manufacture, which does not require those employed in it to be collected into over-grown cities, or congregated in crowded factories. Engaged alternately at their loom and in their farm, they derive both health and recreation from the alternation. Green lawns, clear streams, pure springs, and the oper atmosphere, are necessary for bleaching: hence it is that so many eminent bleachers reside in the country, and hence also the towns are small, and every hill and valley abounds with rural and comfortable habitations.
In the mountainous districts are several springs slightly impregnated with sulphur and iron. The borders of the bogs sometimes also exhibit ferruginous oozings, one of which in the Fews mountains is said to be useful in scrofulous complaints. The same effect was also formerly attributed to the waters of Lough Neagh, in the north-western limits of this county. Boate states, in addition to this, that the temperature of the sand at the bottom of the bay in which this sanative quality is perceived, alternates frequently between cold and warmth. A petrifying quality, such as that said to exist in some parts of Lough Neagh, has been discovered at Rosebrook, near Armagh, the mansion-house of which was built, in a great measure, of petrifactions raised from a small lake there. Petrified branches of hawthorn have been found near the city of Armagh; and fossil remains of several animals have also been discovered in the limestone rocks in the same vicinity. Petrifactions of the muscle, oyster, leech, together with dendrites, belemnites, and madreporites, are also found; and in the mountain streams are pure quartz crystals, of which a valuable specimen, found near Keady, is in the possession of Dr. Colvan, of Armagh.