;;—;MONTEITH, PORT OFfrom E to W <strong>of</strong> IJ mile, an utmost breadth from Nto S <strong>of</strong> 1 mile, and a depth in places <strong>of</strong> 80 feetand it sends <strong>of</strong>f Goodie Water 8| miles east-southeastwardto the Forth. Its shores display none <strong>of</strong> therude magnificence and grandeur that is characteristic<strong>of</strong> Highland scenery ; but, on the other hand, theypresent an aspect <strong>of</strong> s<strong>of</strong>t pastoral beauty which soothesthe soul, and fills the contemplative mind with thoughtscalm and quiet as its own transparent waters. Thenorthern shore is beautifully adorned with oak, Spanishchestnut, and plane trees <strong>of</strong> ancient growth—survivors<strong>of</strong> those which adorned the park <strong>of</strong> the Earls <strong>of</strong> Monteith.On the same side, the manse and church <strong>of</strong>Port <strong>of</strong> Monteith, mth the elegant mausoleum <strong>of</strong> theGartmore family, seated close on the margin <strong>of</strong> the lake,increase the interest <strong>of</strong> the scene. The lake containsthree islands, two <strong>of</strong> which, from the noble wood thatadorns them, add greatly to the beauty <strong>of</strong> its expanse ;whilst a long, narrow, wooded promontory running farinto the water diversifies the southern shore. Thelargest island, called Inchmahome, has been noticedseparately ; that immediately to the W bears the name<strong>of</strong> Inch talla or Earl's Isle. Here, from 1427, the Earls<strong>of</strong> Monteith had their feudal stronghold, the ruins <strong>of</strong>which still exist, comprising an ancient tower and somedomiciliary buildings. The smallest island is called theDog Isle, where the earls had their dog-kennel while•the stables were situated on the western shore <strong>of</strong> thelake. Twice in Sept. 1869 Queen Victoria drovehere from Invertrossachs. The trout-fishing is ruinedby the pike.— Or(^. Sur., sh. 38, 1S71. See P. Dun'sSummer at tlie Lake <strong>of</strong> Monteith (Glasg. 1866); chap,xxv. <strong>of</strong> Thos. Hunter's Woods and Estates <strong>of</strong> Perthshire(Edinb. 1883) ; and other works cited underInchmahome.Monteith, Port <strong>of</strong>, a hamlet and a parish <strong>of</strong> SWPerthshire. The hamlet lies on the NE shore <strong>of</strong> theLake <strong>of</strong> Monteith, 6 miles SSW <strong>of</strong> Callander, 4* E byN <strong>of</strong> Aberfoyle, and 4 NNW <strong>of</strong> Port <strong>of</strong> Monteith station,in Kippen parish, on the Forth and Clyde junctionsection <strong>of</strong> the North British railway, this being 13miles W by N <strong>of</strong> Stirling, and 17i NE <strong>of</strong> Balloch.Erected into a burgh <strong>of</strong> barony by James III. in 1467,it long was called simply Port, as being the landing-placefrom Inch Talla and Inchmahome ;* andhas a little pier, a good hotel, and a post <strong>of</strong>lSce underStirling.The parish, containing also the village and station <strong>of</strong>Gartmore, since 1615 has comprehended the ancientparish <strong>of</strong> Port and a portion <strong>of</strong> that <strong>of</strong> Lany. It isbounded N by Callander, NE by Callander and Kilmadock,E by Kincardine (detached), S by Kippen andDrymen in Stirlingshire, SW by Drymen, and W byAberfoyle. Its utmost length, from E to W, is 7Jmiles ; its utmost breadth, from N to S, is 5 miles ; andits area is 36J miles or 23,599J acres, <strong>of</strong> which 1S61Jare water. The Forth has here a winding course <strong>of</strong> 13Jmiles—viz., 7 furlongs southward along the westernborder, 2| miles south-eastward across the south-westerninterior, and lOJ miles eastward along all the southernborder—though the point which it first touches andthat where it quits the parj.sh are but 7§ miles distantas the crow flies. Kelty Water flows 2J miles east-bynorthwardalong part <strong>of</strong> Ihe Drymen boundary to theForth, another <strong>of</strong> whose affluents. Goodie Water, goes4 miles eastward from the Lake <strong>of</strong> Monteith (IJ x 1 mile55 feet) till it passes <strong>of</strong>f into Kincardine. Loch Deunkie(9 X 7J furl. ; 450 feet) lies on the boundary with Aberfoyle,and Loch Venxaohae (3| miles x 5 furl. ;270feet) on that -nith Callander ;whUst in the NE interiorare Loch Ruskie (2 x 2f furl. ; 400 feet) and LochanBalloch (2J x 1 furl. ; 1180 feet). The surface <strong>of</strong> thesouthern district is low and flat, sinking to 45, andrarely much exceeding 100, feet above sea-level ; but N<strong>of</strong> the Lake <strong>of</strong> Monteith rise the Monteith Hills (1289feet), Ben Dearg (1401), Ben GuUipen (1344), and Meall* Tlie present minister, however, inclines to refer Port to theLatin poHu, 'a gate, pass, or de&le,' this parish being indeed agate <strong>of</strong> the Higlilands.50MONTEVIOTnan Gohhar (812). This upland dLstrict, comprisingone-third <strong>of</strong> the whole area <strong>of</strong> the parish, consists <strong>of</strong> acongeries <strong>of</strong> rocky and mountainous elevations, chieflycovered with heath, and admitting cultivation only insome confined hollows and along some narrow skirts.The SE corner comprises part <strong>of</strong> Flanders Moss, in allrespects similar in character to the famous one <strong>of</strong> Kincardine.The rest <strong>of</strong> the parish, including the districtalong the Forth, consists <strong>of</strong> rich carse land towards theriver, <strong>of</strong> ' dryfield ' towards the hills, and presents anappearance <strong>of</strong> much fertility and high culture. Thetrausition from the uplands to the lowlands <strong>of</strong> the parishis sudden and perfect. In the mountains is limestone <strong>of</strong>the quality <strong>of</strong> marble, having a blue ground streakedwith white, which, when calcined, affords a quicklime<strong>of</strong> the purest white. A bluish grey sandstone occurs inthe champaign district, close in texture, and very suitablefor pavements and staircases. The soU <strong>of</strong> the carselands is rich argillaceous alluvium ;on most other lands<strong>of</strong> the champaign district is either a very fertile shallowloam, a stiff, intractable, tilly clay, a ferruginous andcomparatively barren gravel, or a more or less fertilereclaimed swamp or meadow ; on Flanders Moss and ontwo other smaller tracts is moss ; and on the cultivablepart <strong>of</strong> the uplands is chiefly reclaimed moor. Anisland in Loch Ruskie is the traditional site<strong>of</strong> a castlebelonging to Sir John Menteith, Wallace's gaoler atDumbarton. Other antiquities are traces <strong>of</strong> a Romanroad, deflecting from the great Roman road to Brechin ;vestiges <strong>of</strong> a Roman castellum at the north-westernextremity <strong>of</strong> Flanders Moss ; traces <strong>of</strong> an ancientmilitary post on Keirhead, 1 mile NE <strong>of</strong> the castellum ;and the ecclesiastical and baronial ruins on the islandsin the Lake <strong>of</strong> Monteith. Tuliimoss, to the NW <strong>of</strong>the Lake <strong>of</strong> Monteith, was the scene <strong>of</strong> a skirmish in1489 between James IV. and the Earl <strong>of</strong> Lennox ; anda spot called Suir, near Gartmore House, was the placewhere Rob Roy is said to have taken from the factor <strong>of</strong>the Duke <strong>of</strong> Montrose his collection <strong>of</strong> rents. From 1to 10 Sept. 1869, the Queen, with the Princesses Louiseand Beatrice, stayed at Invertrossachs, ' the recollection<strong>of</strong> the ten days at which — quiet and cozy—and <strong>of</strong> thebeautiful country and scenery I saw in the neighbourhood,wUl ever be a very plea.sant one ' (pp. 116-147 <strong>of</strong>More Leaves from the Journal <strong>of</strong> a Life in the Highlands,1884). Mansions are Blairhoyle, Caedeoss,Gaetmoee, Inveeteossachs, Lochend (1715), andRednock ; and 6 proprietors hold each an annualvalue <strong>of</strong> £500 and upwards, 8 <strong>of</strong> between £100 and£500, 1 <strong>of</strong> from £50 to £100, and 5 <strong>of</strong> from £20 to £50.Giving <strong>of</strong>f portions to the quoad sacra parishes <strong>of</strong> Gartmore,Norriston, and Trossachs, this parish is in the presbytery<strong>of</strong> Dunblane and the synod <strong>of</strong> Perth and Stirlingthe stipend and communion elements have a value <strong>of</strong> £330.The parish church, at Port <strong>of</strong> Monteith hamlet, was builtin 1878 in the Gothic style <strong>of</strong> the 13th century, and hasa stained E window. Three public schools—Dykehead,I'ort <strong>of</strong> Monteith, and Ruskie—with respective accommodationfor 66, 47, and 66 children, had (1883) anaverage attendance <strong>of</strong> 20, 26, and 33, and grants <strong>of</strong>£25, 17s., £32, 4s., and £38, 2s. 6d. Valuation (1860)£10,906, (1884) £12,649, 3s. 6d. Pop. (1801) 1569,(1831) 1664, (1861) 1375, (1871) 1243, (1881) 1175, <strong>of</strong>whom 60 were Gaelic-speaking, and 654 were in theecclesiastical parish. Ord. Sur., shs. 38, 39, 1871-69.Monteviot, a seat <strong>of</strong> the Marquis <strong>of</strong> Lothian, in Crailingparish, Roxburghshire, 2 miles E by N <strong>of</strong> Ancrumand 3 N by W <strong>of</strong> Jedburgh. It stands near the leftbank <strong>of</strong> the winding Tweed, at the southern base <strong>of</strong>Peniel Heugh (774 feet), in a park <strong>of</strong> singular beauty,and is itself an imposing Gothic edifice, rebuilt in thecourse <strong>of</strong> the present century. At Monteviot died MissJean Elliot (1727-1805), author <strong>of</strong> the Flowers <strong>of</strong> theForest, it then being occupied by her brother. AdmiralElliot. At Harestanes, within the park but in Ancrumparish, were remains <strong>of</strong> a stone circle till towards theclose <strong>of</strong> last century ; and a neighbouring serpentmound,'being explored by Mr J. S. Phene, F.S.A., ' in
MONTGOMEEIE1872, was found to entomb two skeletons. See New-BATTLE and Ckaimng.— Ord. Sur., sh. 17, 1864.Montgomerie. See Coilsfield.Montgreenan, an estate, with a mansion and a railwaystation, in Kilwinning parish, Ayrshire, 3^ milesENE <strong>of</strong> Kilwinning town. Its owner, Robert BruceEobertson-Glasgow, Esq. (b. 1842 ; sue. 1860), holds2645 acres in the shire, valued at £2576 per annum.— Ord. Sur., sh. 22, 1865.Mont-Quhanie. See Mount- Quhanie.Montrave, a mansion <strong>of</strong> 1836 in Scoonie parish, Fife,4 miles N <strong>of</strong> Leven. Its owner, John Gilmour, Esq.,jun., <strong>of</strong> Lundinand Montrave, holds 2728 acres in theshire, valued at £5244 per annum. In 1877 a metalpot was found on the estate, containing 9615 silvercoins—8675 <strong>of</strong> them English, <strong>of</strong> Edward I. and III.See Laego.— Or(i. Sur., sh. 40, 1867.Montrose, a parish containing a royal burgh <strong>of</strong> thesame name, on the coast, at the NE corner <strong>of</strong> Forfarshire.It is bounded N by Logie-Pert parish and byKincardineshire, E by the North Sea, S by Craigparish, and SW by Dun parish. The boundary withKincardineshire has evidently followed the course <strong>of</strong> theNorth Esk river, but now, both above and below thebridge by which the coast road from Dundee to Aberdeencrosses the river, the line follows an old channel,in the former case to the S, and in the latter to the N,<strong>of</strong> the modern one. The boundary on the S is the riverSouth Esk, and on the S"W the eastern foreshore <strong>of</strong> theMontrose Basin, along the track <strong>of</strong> Tayock Burn, whichenters it W <strong>of</strong> Newmanswalls House, and then it followsthe course <strong>of</strong> this stream for almost a mile to a point E<strong>of</strong> Newbigging. Elsewhere it is artificial. In shapethe parish is, roughly speaking, a triangle mth bluntedcorners, the sides being on the N, E, and SW. Thegreatest breadth across the N end, from the point onthe "W where Dun, Logie-Pert, and Montrose parishesmeet to that on the E at the old mouth <strong>of</strong> the NorthEsk river, is 3J miles ; the breadth, from the North Eskopposite Stone <strong>of</strong> Morphie (Kincardineshire) on the Nto the South Esk at Montrose harbour on the S, is 3|miles; and the area is 4722'415 acres, <strong>of</strong> which 95'855are water, 492 '172 foreshore, and the rest land. Allalong the coast, between the rivers, a flat sandy beachis bounded by a line <strong>of</strong> sandhills from 20 to 30 feet high,covered with bent. Immediately within these is a belt<strong>of</strong> sandy undulating ground, with close short herbage,known to the N as Charleton and Kinnaber Links, andto the S as Montrose Links. From this the ground rises,at first gradually, but afterwards more steeply, to the W,the greatest height (317 feet) being reached near the Wcorner, to the W <strong>of</strong> Hillhead <strong>of</strong> Hedderwick. Fromthis rising ground, sometimes known as Montrose Hill,along the lower slopes <strong>of</strong> which are the numerous villasand houses forming the village <strong>of</strong> Hillside, there is anexcellent view <strong>of</strong> the Forfarshire and KincardineshireGrampians ;<strong>of</strong> the end <strong>of</strong> the vale <strong>of</strong> Strathmore, withits mansions and woodland ; <strong>of</strong> the round tower andspires <strong>of</strong> Brechin, and the windings <strong>of</strong> the South Esk,down past the basin and on to the mouth below thetown <strong>of</strong> Montrose. In the N, along part <strong>of</strong> the course<strong>of</strong> the North Esk, there are high wooded banks, whilethriving plantations extend along the AV side <strong>of</strong> theLinks <strong>of</strong> Charleton and Kinnaber The soil all over thelinks is sandy, and the shells show that the deposit is amodern one, so that within the recent period MontroseBasin must have been a bay. On the W side <strong>of</strong> the linksis a raised beach <strong>of</strong> shingle, and to the W <strong>of</strong> this the soilis very fertile, being a strong clayey loam. A stiffunderlying clay <strong>of</strong> marine origin, and containing remains<strong>of</strong> starfishes, is worked for the manufacture <strong>of</strong> bricks andtiles at Dryleys and Puggieston. The imderlying rocksbelong to the Lower Old Eed sandstone formation. Thedrainage <strong>of</strong> the parish is carried <strong>of</strong>f by the North Eskand the South Esk. The north-western part <strong>of</strong> theparish is traversed for over 2J mUes by the Perth andAberdeen section <strong>of</strong> the Caledonian railway system,and from Dubton Junction station a branch line, 3miles in length, communicates with the town <strong>of</strong> MontroseMONTROSEthrough the STV part <strong>of</strong> the parish. The Montrose andArbroath section <strong>of</strong> the North British system, crossingthe South Esk by a viaduct over J mile long, passesby the NW side <strong>of</strong> the town, and, after a course <strong>of</strong> 2^miles, unites with the Caledonian system at KinnaberJunction to the N. From this the Jlontrose and Bervierailway, also belonging to the North British system,bi'anches <strong>of</strong>f and runs parallel to the coast along theW edge <strong>of</strong> Montrose and Kinnaber Links, for a distance<strong>of</strong> 2 mUes, till it crosses the North Esk.The parish isalso traversed by the main road along the coast fromDundee to Aberdeen, which, entering at the SW corner<strong>of</strong> Montrose, passes through the town, and then alongthe W edge <strong>of</strong> Montrose and Kinnaber Links, parallel tothe Montrose and Bervie railway, till it reaches Kincardineshireat the North Esk, which it crosses by agood .
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