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Ordnance Gazetteer of Scotland .. - National Library of Scotland

Ordnance Gazetteer of Scotland .. - National Library of Scotland

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——OVERTOWNmiles ENE <strong>of</strong> Dumbarton. Its owner, John Campbell Jlerse away to the German Ocean. The southern"White, Esq. (b. 1843 ; sue. 1884), holds 910 acres in district, to the extent <strong>of</strong> one-third <strong>of</strong> all the area, isthe shire, valued at £1032 per annum. Ord. Sur., nearly filled with masses <strong>of</strong> the Cheviots, dome-likesh. 30, 1866.hills, smooth and green ; the northern is much diversifiedOvertown, a large village in Cambusnethan parish, in surface, including <strong>of</strong>fshoots <strong>of</strong> the Cheviots, andLanarkshire, near a station <strong>of</strong> its own name on the abounding in ravines, picturesque defiles, and romanticCaledonian railway, IJ mile SE <strong>of</strong> Wishaw, and 3J dells ; and the banks <strong>of</strong> Oxnam Water are beautifullymiles NW <strong>of</strong> Carluke. Lying amid a rich mineral undulated, and rise into various slopes <strong>of</strong> the adjoiningcountry, and inhabited chiefly by workers in the mineral heights. Limestone is found near the Jed, but cannotfield, it has a post <strong>of</strong>fice under AVishaw, a school <strong>of</strong> well be worked ; and sandstone, hard, white, andthe Coltness Iron Co., a Eoman Catholic school, St thought to belong to the Carboniferous formation,Patrick's Roman Catholic church (1873 ; 200 sittings), abounds in the S, intersected by a thick dyke <strong>of</strong> trap.and an Established church. The last,',built in 1874-75 Transition rocks prevail throughout the N. The soil <strong>of</strong>at a cost <strong>of</strong> over £2000, is an Early English edifice, with the arable lands is loamy, clayey, or gravelly. Lessa bold square tower 80 feet high, and 600 sittings. than one-sixth <strong>of</strong> the entire area is in tillage ;plantationscover some 600 acres ; and the rest <strong>of</strong> the land isPop. (1861) 364, (1871) 1517, (1881) 1293.— Ord. Sur.,sh. 23, 1865.pastoral or waste. The Cheviot breed <strong>of</strong> sheep is inOxenfoord Castle, a seat <strong>of</strong> the Earl <strong>of</strong> Stair, in Cranstonparish, Edinburghshire, near the left bank <strong>of</strong> the high excellence. A weak chalybeate spring near Fair-great favour, and has been brought to a condition <strong>of</strong>river Tyne, IJ mile N <strong>of</strong> Ford, and 4 miles ESE <strong>of</strong> Dalkeith.Kemodelled towards the close <strong>of</strong> last century by went eventually into neglect. The Roman AVatlingloans enjoyed once some medicinal repute, butRobert Adam, and subsequently much enlarged by Street from Yorkshire to the Lothians, running 7^William Burn, it is a magnificent edifice, with extensive miles along the eastern and north-eastern boundary,and beautiful grounds. It contains a fine library, and remains throughout much <strong>of</strong> its length in good preservation; is still used as a drove road ; and once was aportraits and paintings by Jameson, Angelica Kauffmann,Thomson <strong>of</strong> Duddingston, etc. The estate, called favourite camping-ground <strong>of</strong> Border Gypsies. Otherformerly Oxfurd, from 1661 till 1706 gave the title <strong>of</strong> antiquities are a fairly entire Caledonian stone circle,Viscount Oxfurd, in the peerage <strong>of</strong> <strong>Scotland</strong>, to the remains <strong>of</strong> another stone circle, several circular camps,family <strong>of</strong> Macgill, whose heiress, Elizabeth, in 1760 vestiges <strong>of</strong> Dolphiston and two other mediaeval fortalices,and remains <strong>of</strong> a pre-Pieformation chapel. Themarried her cousin, Sir John Dalrymple, Bart, <strong>of</strong> Cousland,a great-great-grandson <strong>of</strong> the first Viscount Stair. Rev. Thomas Boston, one <strong>of</strong> the founders <strong>of</strong> the ReliefTheir son. Sir John, in 1853 succeeded as eighth Earl Church, was minister for some time prior to 1757.<strong>of</strong> Stair.— Ore?. S^cr., sh. 33, 1863. See Lochinch, and Four proprietors hold each an annual value <strong>of</strong> more, andJohn Small's Castles and Maiisio'ns <strong>of</strong> tlie Lothians three <strong>of</strong> less, than £500. Giving <strong>of</strong>f a portion to(Edinb. 1883).Edgerston quoad saera parish, Oxnam is in the presbytery<strong>of</strong> Jedburgh and the .synod <strong>of</strong> Merse and Teviot-Oxenham. See Oxnam.Oxfurd. See Oxenfoord Castle.dale ;the living is worth £350. The parish church,Oxna, an island in Tingwall parish, Shetland, 3i miles built in 1738, and enlarged and restored in 1880, contains280 sittings. A specimen <strong>of</strong> the old jougs is fixedSW <strong>of</strong> Scalloway. It has an utmost length <strong>of</strong> 6J and5j furlongs, and rises at Muckle Ward to 115 feet above outside the S wall. Oxnam public and Towford Dukesea-level. Pop. (1871) 29, (1881) 30.<strong>of</strong> Roxburghe's school, with respective accommodationOxnam (anc. Oxenham), a hamlet and a parish <strong>of</strong> for 110 and 56 children, had (1883) an average attendance<strong>of</strong> 69 and 32, and grants <strong>of</strong> £66, 4s. 6d. andSE Roxburghshire. The hamlet lies upon OxnamWater, 4J miles SE <strong>of</strong> Jedburgh, under which it has a £40, 8s. Valuation (1864) £10,526, Os. 8d., (18S4)post <strong>of</strong>fice.£11,750, 19s. Pop. (1801) 688, (1831) 676, (1861)The parish is bounded NE by the main body <strong>of</strong> 627, (1871) 695, (1881) 683, <strong>of</strong> whom 638 were in theJedburgh, E by Hounara, SE and S by Northumberland, ecclesiastical parish. Ord. Sur., sh. 17, 1864.and SW by the Edgerston or detached section <strong>of</strong> Jed-Ox Rocks. See Aires.burgh and by Southdean. Its utmost length, fromKNW to SSE, is 10| miles ; its utmost breadth is 5imiles ; and its area is 33 square miles or 21,193 acres,<strong>of</strong> which 33J are water. Oxnam Water, rising at analtitude cf 695 feet, runs 5J miles north-by-westwardthrough the interior, then 6J furlongs along the Jedburghboundary ; and, after quitting this parish, itwinds 3| miles north-by-westward through or along theborders <strong>of</strong> Jedburgh and Ceailing, till, after a totalcourse <strong>of</strong> 9| miles and a total descent <strong>of</strong> 455 feet, itfalls into the Teviot at a point i mile NNE <strong>of</strong> Crailingvillage. From J mile below its source. Kale Water(here Long Burn) runs 5J miles north-north-eastward,mainly across the south-eastern interior, but partlyalong the Edgerston and Hounam boundaries. TheCoquet, a stream belonging almost wholly to England,flows along the Northumberland border for the first jmile <strong>of</strong> its course ; a tributary <strong>of</strong> Jed Water traces 3miles <strong>of</strong> the south-western border ; and the Jed itself,after receiving that tributary, runs 2§miles north -northwestwardalong the same boundary. The surface ishilly, sinking in the extreme N to 340 feet above sealevel,and rising southward thence to the roundedpastoral Cheviots. Chief elevations, from N to S, areBloodylaws Hill (809 feet), Cunzierton (1100), Birkenside(763), Peg Law (932), Lawsuit Law (825), DodHill (977), Plenderleith (1198), Hindhope Hill (1349),Brownhart Law (1664), Grindstone Law (1535), andHungry Law (1643), <strong>of</strong> which the three last rise on orclose to the Englisli Border. Several oi these heightscommand a magnificent view <strong>of</strong> Teviotdale and the146CYNEOxton or Agston, a post-<strong>of</strong>fice village in Channelkirkparish, Berwickshire, near the right bank <strong>of</strong> LeaderWater, 5 miles NNW <strong>of</strong> Lauder.Oykell. See Oikell.Oyne, a parish in Garioch district, centi-al Aberdeenshire,with a post <strong>of</strong>fice under Insch and a station on theGreat North <strong>of</strong> <strong>Scotland</strong> railway,4 miles W by N <strong>of</strong>Inveramsay Junction and 24J NW <strong>of</strong> Aberdeen. It isbounded N by Culsalmond, NE by Rayne, E by Chapel<strong>of</strong> Garioch, S by Monymusk, W by Eeig and Premnay,and NW by Insch. Its utmost length, from N to S, is6J miles ;its breadth varies between 1^ and 3^ miles;and its area is 10,151i'3^ acres, <strong>of</strong> which lOf are water.The Don flows 2j miles east-south-eastward along thesouthern, the Uey 3 miles south-eastward along thenorth-eastern, boundary ; and to the Ury run the Burn<strong>of</strong> Shevock along the Culsalmond border, and GadieBurn across the interior. The surface sinks along theDon to 300, along the Ury to 283, feet ; and thence itrises to 415 feet at the parish church, 558 at Ardoyne,1698 at the Mither Tap <strong>of</strong> Bennochib, and 1340 atMillstone Hill. Bennochie, parting the Gadie's valleyfrom the Don's, and occupying close upon half <strong>of</strong> theentire area, forms a stupendous barrier between thenorthern and the southern district, the former <strong>of</strong> whichhas the richest soil, and contains four-fifths <strong>of</strong> the population.Granite is the predominant rock, and has beenquarried ; trap <strong>of</strong> hard texture and a deep blue hue isused for dykes and ordinary masonry ; and rock crystal,topaz, jasper, and shorl are found. The soil <strong>of</strong> the lowgrounds is mostly friable and fertile ; on the slopes <strong>of</strong>

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