Fort Augustus railway station

Kilchuimen Academy is a small secondary school located in Fort Augustus in Scotland. It shares its campus with neighbouring Kilchuimen Primary. The school has approximately 80 students enrolled. In 2009 the school saw the arrival of a new M.U.G.A (multi use games area) for the local community to use. In late 2010 the school received a grant of £18,000 to send its students to partnered schools in the Netherlands and Germany. The German partnered school is Gymnasium Querfurt.

Fort Augustus is a settlement in the parish of Boleskine and Abertarff, at the south-west end of Loch Ness, Scottish Highlands. The village has a population of around 646 (2001). Its economy is heavily reliant on tourism.

Fort Augustus Abbey, properly St. Benedict's Abbey, at Fort Augustus, Inverness-shire, Scotland, was a Benedictine monastery, from late in the nineteenth century to 1998 that also housed a school for boys until 1993.

Fort Augustus Pier was a railway station in Inverness-shire, Scotland, and served as the north terminus of the Invergarry and Fort Augustus Railway between 1903 and 1906.

The River Tarff is a river in Inverness-shire in the Scottish Highlands. It rises between the hills of Gairbeinn and Geal Charn and flows northwards then southwestwards and finally north-northwestwards into the Great Glen where it enters Loch Ness at Fort Augustus. The middle and lower reaches of the river are confined within the gorge of Glen Tarff. Its headwaters have been dammed to form the Glendoe Reservoir which forms the upper water storage basin for the Glendoe Hydro Scheme which began operation in 2009.

The Highlands (Scots: the Hielands; Scottish Gaelic: a' Ghàidhealtachd [ə ˈɣɛːəl̪ˠt̪ʰəxk], lit. 'the place of the Gaels') is a historical region of Scotland. Culturally, the Highlands and the Lowlands diverged from the Late Middle Ages into the modern period, when Lowland Scots language replaced Scottish Gaelic throughout most of the Lowlands. The term is also used for the area north and west of the Highland Boundary Fault, although the exact boundaries are not clearly defined, particularly to the east. The Great Glen divides the Grampian Mountains to the southeast from the Northwest Highlands. The Scottish Gaelic name of A' Ghàidhealtachd literally means "the place of the Gaels" and traditionally, from a Gaelic-speaking point of view, includes both the Western Isles and the Highlands. The area is very sparsely populated, with many mountain ranges dominating the region, and includes the highest mountain in the British Isles, Ben Nevis. During the 18th and early 19th centuries the population of the Highlands rose to around 300,000, but from c. 1841 and for the next 160 years, the natural increase in population was exceeded by emigration (mostly to Canada, the United States, Australia and New Zealand, and migration to the industrial cities of Scotland and England.): xxiii, 414 and passim  The area is now one of the most sparsely populated in Europe. At 9.1/km2 (24/sq mi) in 2012, the population density in the Highlands and Islands is less than one seventh of Scotland's as a whole. The Highland Council is the administrative body for much of the Highlands, with its administrative centre at Inverness. However, the Highlands also includes parts of the council areas of Aberdeenshire, Angus, Argyll and Bute, Moray, North Ayrshire, Perth and Kinross, Stirling and West Dunbartonshire. The Scottish Highlands is the only area in the British Isles to have the taiga biome as it features concentrated populations of Scots pine forest: see Caledonian Forest. It is the most mountainous part of the United Kingdom.

The Caledonian Forest is the ancient (old-growth) temperate forest of Scotland. The forest today is a reduced-extent version of the pre-human-settlement forest, existing in several dozen remnant areas. The Scots pines of the Caledonian Forest are directly descended from the first pines to arrive in Scotland following the Late Glacial; arriving about 7000 BC. The forest reached its maximum extent about 5000 BC, after which the Scottish climate became wetter and windier. This changed climate reduced the extent of the forest significantly by 2000 BC. From that date, human actions (including the grazing effects of sheep and deer) reduced it to its current extent. Today, that forest exists as 35 remnants, as authenticated by Steven & Carlisle (1959) (or 84 remnants, including later subjective subdivisions of the 35) covering about 180 square kilometres (69 sq mi) or 44,000 acres (18,000 ha). The Scots pines of these remnants are, by definition, directly descended from the first pines to arrive in Scotland following the ice age. These remnants have adapted genetically to different Scottish environments, and as such, are globally unique; their ecological characteristics form an unbroken, 9000-year chain of natural evolution with a distinct variety of soils, vegetation, and animals. To a great extent the remnants survived on land that was either too steep, too rocky, or too remote to be agriculturally useful. The largest remnants are in Strathspey and Strath Dee on highly acidic, freely drained glacial deposits that are of little value for cultivation and domestic stock. An examination of the earliest maps of Scotland suggests that the extent of the Caledonian Forest remnants has changed little since 1600.

The Caledonian Canal connects the Scottish east coast at Inverness with the west coast at Corpach near Fort William in Scotland. The canal was constructed in the early nineteenth century by Scottish engineer Thomas Telford.

Aberchalder railway station served the village of Aberchalder, in the county of Inverness-shire in Scotland.

Loch a' Bhainne is a small, upland freshwater loch approximately 2 miles (3.2 km) north of the east end of Loch Garry and 3.5 miles (5.6 km) north-west of Invergarry in the Scottish Highlands. The loch is roughly triangular in shape with a perimeter of 0.6 km (0.37 mi). It is approximately 0.33 mi (0.53 km) long, has an average depth of 10 ft (3.0 m) and is 28 ft (8.5 m) at its deepest. The loch was surveyed in 1903 by James Murray as part of Sir John Murray's Bathymetrical Survey of Fresh-Water Lochs of Scotland 1897-1909.

Aberchalder (Gaelic: Obar Chaladair) is a small settlement and estate at the northern end of Loch Oich in the Scottish Highlands and is in the Highland council area of Scotland. It lies on the A82 road and is situated in two parishes, Boleskine and Kilmonivaig. Fort Augustus is within 5 mi (8.0 km).

The Bridge of Oich (also known as Victoria Bridge, Aberchalder) is a taper principle suspension bridge, designed by James Dredge, across the River Oich near Aberchalder in Highland, Scotland. The bridge opened in 1854 and was used to take the main road traffic over the river until 1932.