Parish of Loth

A historical perspective, drawn from the Ordnance Gazetteer of Scotland: A Survey of Scottish Topography, Statistical, Biographical and Historical, edited by Francis H. Groome and originally published in parts by Thomas C. Jack, Grange Publishing Works, Edinburgh between 1882 and 1885.

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1791-99: Loth
1834-45: Loth

Loth, a coast parish of E Sutherland, with a station of its own name on the Duke of Sutherland's railway (1871), 5¾ miles SW of Helmsdale. Containing also the fishing village of Portgower, 2 miles SW of Helmsdale, and much curtailed by the annexation of its Helmsdale portion to Kildonan prior to 1851, it is bounded N by Kildonan, SE by the Moray Firth, and SW by Clyne. Its utmost length, from NE to SW, is 7½ miles; its utmost breadth, from NW to SE, is 5 3/8 miles; and its area is 28 1/5 square miles or 18,042 acres, of which 430 1/7 are foreshore and 4½ water. The coast-line, closely followed by the railway for 7¾ miles, is chiefly a low, level beach of sand, indented by several baylets, and projecting some low rocky headlands. The impetuous Loth, rising on Beinn na Meilich at an altitude of 1510 feet, winds 5¾ miles southward to the sea near Loth station, 2¾ miles above its mouth being joined by Sletdale Burn, which rises on Meall an Liath Mor at an altitude of 1495 feet, and, thence curving 5 ¼ miles east-by-southward, has a total descent of 1132 feet. Of seven other streamlets the chief is one running 4 miles south-south-eastward to the sea near Kintradwell. In 1818 a new channel was cut for the Loth through a solid rock 20 feet high, whereby a largish swamp or loch- the river's expansion-was drained, and its bed converted into rich arable carse-land. The surface rises rapidly north-westward to 1000 feet at Cregan Mor, 970 at Cnoc na h-Iolaire, 1294 at Creag a Chrionaich, 1346 at Creag a' Mheasgain, 1311 at Culgower Hill, 1767 at Beinn Chol, 1608 at Meallan Liath Mor, 1581 at Creag Mhor, 2068 at Beinn Dobhrain, 2046 at Beinn na h-Urrachd, and 1940 at Beinn na Meilich, the six last of which culminate on the confines of the parish. The rocks along the coast are oolitic, comprising limestone, conglomerate, variously-coloured shales, and white and red sandstone; but the prevailing rock of the uplands is a species of large-grained porphyry, unusually frangible, and easily denudated by running water. At most one-seventh of the entire area is in tillage, but what arable land there is has a fertile soil, and the farm of Crakaig is one of the best in the county. Pennant describes an ancient flag-built ` hunting house '-one of three-in Glen Loth; and near Kintradwell there still are remains of a Pictish tower. The mansion of Kintradwell was burnt by the Jacobite Earl of Cromarty in 1746. Hereabout stood a chapel dedicated to St Trullo; and another pre-Reformation place of worship was standing at Garty ;towards the close of last century. The Duke of Sutherland is sole proprietor. Loth is in the presbytery of Dornoch and the synod of Sutherland and Caithness; the living is worth £233. The parish church, 1½ mile NE of Loth station, is a handsome edifice of 1838. The public school, with accommodation for 60 children, had (1882) an average attendance of 37, and a grant of £35, 19s. 6d. Valuation (1860) £2223, (1884) £2681, 10s., plus £795 for railway. Pop. (1801) l374, (1831) 2214, (1861) 610, (1871) 583, (1881) 584.—Ord. Sur., sh. 10, 1878.

An accompanying 19th C. Ordnance Survey map is available, or use the map tab to the right of this page.

Note: This text has been made available using a process of scanning and optical character recognition. Despite manual checking, some typographical errors may remain. Please remember this description dates from the 1880s; names may have changed, administrative divisions will certainly be different and there are known to be occasional errors of fact in the original text, which we have not corrected because we wish to maintain its integrity. This information is provided subject to our standard disclaimer

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