Parish of Lochrutton

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.

This edition is copyright © The Editors of the Gazetteer for Scotland, 2002-2022.

It has taken much time and money to make the six-volumes of Groome's text freely accessible. Please help us continue and develop by making a donation. If only one out of every ten people who view this page gave £5 or $10, the project would be self-sustaining. Sadly less than one in thirty-thousand contribute, so please give what you can.

Use the tabs on the right of this page to see other parts of this entry Arrow

Links to the Historical Statistical Accounts of Scotland are also available:
(Click on the link to the right, scroll to the bottom of the page and click "Browse scanned pages")

1791-99: Lochrutton
1834-45: Lochrutton

Lochrutton, a parish of E Kirkcudbrightshire, containing at its south-eastern border the station of Lochanhead, 6 miles SW of Dumfries, and 13¾ NE of Castle-Douglas; as also Lochfoot village, 1¾ mile NNW of that station, and 5½ miles WSW of Dumfries, under which it has a post office. It is bounded NW and N by Kirkpatrick-Irongray, NE by Terregles and Troqueer, SE by Troqueer and Newabbey, and SW by Kirkgunzeon and Urr. Its utmost length, from E to W, is 5½ miles; its utmost breadth, from N to S, is 37/8 miles; and its area is 7561 acres, of which 150 are water. Lochrutton Loch (7 x 3½ furl.; 325 feet) extends south-bywestward from Lochfoot village, and contains the tiny islet of Dulton's Cairn and the larger Big Island, which, partly at least, is an artificial crannoge. Half-adozen rivulets flow eastward, north-eastward, or westward to this lake, which sends off Cargen Water towards the Nith. Kirkgunzeon or Dalbeattie Burn, a feeder of Urr Water, traces all the Newabbey boundary; and Merkland Well, near the head of Lochrutton Loch, is a strong chalybeate spring, which was formerly very celebrated for the cure of agues and of dyspeptic and nervous disorders. The surface undulates, sinking along the northern and south-eastern boundaries to less than 300 feet above sea-level, and rising thence to 637 feet near the manse, 550 near Carswadda, and 604 near Slack. The predominant rocks are eruptive and Silurian, and the soil is mostly a light shallow loam. Nearly six-sevenths of the entire area are in tillage or in meadow; about 250 acres are under wood; and the rest is either pastoral, moss, or waste. An ancient Caledonian stone circle, called the `Seven Grey Stones,' but really comprising nine, with a diameter of 70 feet, is on the eminence near the manse, which commands a very extensive and brilliant view. Old baronial fortalices, or peel towers, were in various places; and the most perfect, Hills Tower, has been noticed separately. Henry Duncan, D.D. (1774-1846), the founder of savings' banks in Scotland, was the son of a former minister. Four proprietors hold each an annual value of £500 and upwards, 8 of between £100 and £500, and 6 of from £50 to £100. Lochrutton is in the presbytery and synod of Dumfries; the living is worth £221. The church, 1 mile E by S of Lochfoot, was built in 1819, and contains upwards of 300 sittings. The public school, with accommodation for 119 children, had (1882) an average attendance of 68, and a grant of £60. Valuation (1860) £5810, (1884) £9076, 17s. 6d. Pop. (1801) 514, (1831) 650, (1861) 677, (1871) 656, (1881) 614.—Ord. Sur., sh. 9, 1863.

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

If you have found this information useful please consider making
a donation to help maintain and improve this resource. More info...

By using our site you agree to accept cookies, which help us serve you better