Loch Mhòr

Loch Mhòr is a reservoir in the traditional county of Inverness-shire in the Scottish Highlands. Its name literally translates from Scottish Gaelic as "Big Loch". It occupies much of the wide floor of Stratherrick which runs roughly parallel to Loch Ness, around 3 mi (4.8 km) to its southeast. A generally shallow body of water 179 m (587 ft) above Loch Ness, Loch Mhòr achieves a depth in excess of 20 m (66 ft) towards its southern end. It is nearly 5 miles (8.0 km) in length, with a maximum breadth of 3⁄4 mile (1.2 km) and mean breadth around 1⁄3 mile (0.5 km). In its middle reaches, a broad and shallow embayment on its southeastern shore contains a scatter of islets. The loch is elongated with a very irregular form, the eastern shore broken up by multiple bays. Loch Mhòr was originally two separate lochs, Loch Garth in the southwest and Loch Farraline in the northeast. The reservoir was formed in 1896 by the construction of two dams, raising the water level by up to 20 feet (6.1 m) above the level of Loch Farraline and joining the two lochs into one. This was created for a hydro-electric scheme and associated aluminium smelter at Foyers, although the smelter closed in 1967. Loch Mhòr is divided in the middle by a causeway carrying a minor road. A masonry dam was constructed across the River Gourag, 230 m (750 ft) long and 9 m (30 ft) high. A longer embankment dam was constructed at Garthbeg, 325 m (1,066 ft) long and 5 m (16 ft) high. This only had a freeboard of 1 m (3 ft 3 in) and was known to leak. The main rivers flowing into Loch Mhòr are the Aberchalder Burn, originally a tributary of Loch Garth, and the River E, which was diverted for the original hydro scheme by construction of the Garthbeg dam. The waters of the loch empty as the River Gourag below the Loch Mhòr dam at its southwestern end. This short river becomes the Allt an Lòin downstream of the former confluence with the River E, then joins the River Foyers which empties into Loch Ness via the Falls…