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Glenmoriston

Glens of ScotlandNess basinValleys of Highland (council area)
Mistyglen
Mistyglen

Glenmoriston or Glen Moriston (Scottish Gaelic: Gleann Moireasdan) is a river glen in the Scottish Highlands, that runs from Loch Ness, at the village of Invermoriston, westwards to Loch Cluanie, where it meets with Glen Shiel. The A887 and A87 roads pass through Glenmoriston. The Glen is dominated by the River Moriston, which in Gaelic might mean "river of the waterfalls". The river is a big attraction for fishers, but also for birdwatchers who come to see osprey and eagles fishing on the river. The river crashes over waterfalls at Invermoriston into Loch Ness, passing under an original Thomas Telford bridge, built in 1813. About five miles along the glen from Invermoriston is Loch Dundreggan, "Dundreggan" being of Gaelic origin and meaning "Dragon Haugh". Here the natural force of the river is tapped through a hydro-electric dam, which supplies power to the area. Water is let out of the dam on Tuesdays, making it a popular attraction for white water rafting and canoeing. After a feasibility study in Glen Affric, wild boar were re-introduced by the charity Trees for Life to a large fenced area of the Dundreggan Estate in November 2009.

Excerpt from the Wikipedia article Glenmoriston (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N 57.173 ° E -4.813 °
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Mowri

A887
IV63 7YL
Scotland, United Kingdom
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Mistyglen
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Scottish Highlands
Scottish Highlands

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.

Caledonian Forest
Caledonian Forest

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.