It appears certain that there were ironworks in the following different places in Gairloch parish,-- 1. Glen Dochartie; three places. 2. Fasagh. 3. Furnace, Letterewe. 4. Talladale. 5. Garavaig, on Slatadale farm. 6. Red Smiddy, near Poolewe. 1. GLEN DOCHARTIE. The traveller proceeding from Loch Maree to Achnasheen may notice, to the right of the road, about four hundred yards before the head of Glen Dochartie is gained, and on the seven hundred feet contour line of the ordnance survey, a scattered heap of small pieces of the slag No. 1. The burn runs past not many yards below. No site of a furnace can be identified. On the other side of the road, about three hundred yards up the hill, on the thousand feet contour, are more extensive similar remains, with the same kind of slag. Mr Macadam finds that this slag contains 66 per cent. of metallic iron, and no lime as silicate. There is red earth in the neighbourhood resembling what is found with "pans" of bog iron. The burn runs past, but is now in a deep gully. At the foot of the glen, more than a mile nearer Kenlochewe, and a little to the west of the bridge over the burn, are fragments of similar slag, and traces of charcoal burnings. The place is on the ancient beach, about twenty feet above the level of the road. No doubt all these remains are of considerable antiquity; they may perhaps have been parts of the same undertaking. 2. FASAGH. The most extensive remains of ironworks on Loch Maree are on the south side of the Fasagh burn, close to where it runs into the loch. This burn comes from Loch Fada, a considerable sheet of water to the north of Slioch. There are remains of a sluice or dam where the burn leaves Loch Fada, evidently used long ago to regulate the water supply. The burn flows into Loch Maree at its south-east corner, close to the head of the loch. There are indications of a large artificial bank, probably the remains of a dam, formed at right angles to the burn, near the site of the ironworks; but the burn has of late years been subject to great floods, that have to some extent varied its course, and altered the surrounding features.