Online Encyclopedia

WESTMEATH

Online Encyclopedia
Originally appearing in Volume V28, Page 549 of the 1911 Encyclopedia Britannica.
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WESTMEATH  , a

county of Ireland in the province of
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Leinster, bounded N.W. by
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Longford, N. by
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Cavan, N.E. and E. by Meath, S. by King's county, and W. by Roscommon . The
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area is 454,104 acres, or about 709 sq. m . The Shannon forms the western boundary . The
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average height of the
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surface of the county is over 250 ft. above sea-level . The highest summits are Knocklayde (795 ft.), Hill of Ben (710 ft.) and Knockayon (707 ft.) . A large surface is occupied by bog . A
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special feature of Westmeath is the number of large loughs, which have a combined area of nearly 17,000 acres . In the north, on the
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borders of Cavan, is Lough Sheelin, with a length of 5 m., and an average breadth of between 2 and 3 m., and adjoining it is the smaller Lough Kinale . In the centre of the county there is a
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group of large loughs, of which Lough Dereveragh is 6 m. long by 3 broad at its widest
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part . To the north of it are Loughs Lene, Glore, Hawn and others, and to 4e south Loughs Iron and Owel . Farther south is Lough Ennell or
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Belvidere, and in the south-west Lough Ree, a
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great expansion of the
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river Shan-non, forming part of the boundary with Roscommon . The river Inny, which rises in Co .

Cavan, enters Westmeath from Lough Sheelin, and, forming for parts of its course the boundary with Longford, falls into Lough Ree . The Inny has as one of its tributaries the Glore, flowing from Lough Lene through Lough Glore, a considerable part of its course being under-ground . From Lough Lene the

Dale also flows southwards to the
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Boyne and so to the Irish Sea, and thus this lake sends its waters to the opposite shores of the island . The Brosna flows from Lough Ennell southwards by King's county into the Shannon . The Westmeath loughs have a
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peculiar fame among anglers for the excellence of their trout-fishing . Westmeath is essentially a county of the great Carboniferous
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Limestone plain, with numerous lakes occupying the hollows . Two or three little inliers of Old Red
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Sandstone, as at Killucan and Moate, form distinctive hills, about 500 ft. in height . At Sron Hill near Killucan, a core of
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Silurian strata appears within the sandstone dome . A considerable
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system of eskers, notably north of
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Tullamore, diversifies the surface of the limestone plain . The
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soil is generally a rich loam of great
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depth resting on limestone, and is well adapted both for tillage and pasturage . The occupations are almost wholly agricultural,
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dairy farming predominating .
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Flour and
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meal are largely produced .

The only textile manufactures are those of friezes, flannels, and coarse linens for

home use . The only
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mineral of any value is limestone . The main
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line of the Midland Great Western railway enters the county from E. and passes W. by
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Mullingar and
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Athlone . From Mullingar a branch runs N.W. to Inny Junction, where lines diverge N. to Cavan (county Cavan), and W.N.W. to Longford (county Longford) and
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Sligo . A branch of the Great
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Southern Western railway runs from
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Portarlington (Queen's county) to Athlone, and this and the Midland Great Western main line are connected by a short line between Clare and Streamstown, worked by the latter
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company .
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Water communication with
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Dublin is furnished by the Royal Canal, traversing the centre of the county . A branch of the
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Grand Canal reaches Kilbeggan in the south . The population (68,611 in 1891; 61,629 in 1901) decreases in excess of the average shown by the Irish counties, and emigration is considerable . About 92% of the
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total are
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Roman Catholics, and about 86% constitute the rural population . The
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principal towns are Athlone (pop . 6617), of which the part formerly in Roscommon was added to Westmeath by the
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Local Government (Ireland) Act of 1898, and Mullingar (4500), the county
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town . Castlepollard and Moate are lesser market towns .

By the Redistribution Act of 1885 Westmeath was formed into two

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parliamentary divisions, North and South, each returning one member, Athlone being included in the county representation . The county is divided into twelve baronies . Assizes are held at Mullingar and quarter sessions at Mullingar and Moate . The county is in the
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Protestant dioceses of Dublin,
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Killaloe and Ossory, and in the Roman Catholic dioceses of
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Kildare and Leighlin, Killaloe and Ossory . Westmeath was severed from Meath (q.v.) in 1543 . The plan for the insurrection of 1641 was concerted in the abbey of Multifarnham, and both in the
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wars of this period and those of 1688 the gentry of the county were so deeply implicated that the majority of the estates were confiscated . There are a considerable number of raths or encampments: one at Rathconrath is of great extent; another at Bally-more was fortified during the wars of the Cromwellian period and those of 1688, and was afterwards the headquarters of General Ginkell, when preparing to besiege Athlone; and there is a third of considerable
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size near Lough Lene . The ruins of the Franciscan abbey of Multifarnham, founded in 1236 by William
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Delaware, picturesquely situated near Lough Dereveragh, include a tower 93 ft. in height .

End of Article: WESTMEATH
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