The Great Glen follows a large geological fault known as the Great Glen Fault. It bisects the Scottish Highlands into the Grampian Mountains to the southeast and the Northwest Highlands to the northwest.
The Glen is a natural travelling route in the Highlands of Scotland, which is used by both the Caledonian Canal and A82 road, which link the city of Inverness on the east coast with Fort William on the West.
Geography and Social history[change | edit source]
It was important in controlling the Highland Scottish clans, particularly in the Jacobite uprisings of the 18th century. This is recognised by the towns of Fort William (population ~10,000) in the south, Fort Augustus (popln. 600+) in the middle of the Glen, and Fort George (to this day an army barracks), just to the north of Inverness. These settlements were built by the British Army to control the Highlands in the 17th/18th centuries.
Fort William is now a significant town. Despite the difficult terrain, Fort William has rail connection with Glasgow in the south and Mallaig on the north-west coast. It is a tourism centre. The Caledonian Canal connects it with Inverness.
Much of the Glen is taken up with a series of lochs, with rivers connecting them. The Caledonian Canal also uses the lochs as part of the route, but the rivers are not navigable.
From northeast to southwest, the natural water features along the Great Glen are:
- River Ness
- Loch Dochfour
- Loch Ness
- River Oich
- Loch Oich
- Loch Lochy
- River Lochy
- Loch Linnhe
The watershed, or water-divide, lies between Loch Oich and Loch Lochy. Loch Linnhe to the south of Fort William is a sea-loch into which both the River Lochy and Caledonian Canal emerge. At the north end, the River Ness empties into the Moray Firth.
Great Glen Fault[change | edit source]
The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland. The fault is actually much longer, and over 400 million years old. It extends in both directions beyond mainland Scotland.
Position[change | edit source]
The fault continues on the North American side of the North Atlantic Ocean, but is no longer part of a continuous fault. The complete fault was broken when the Mid-Atlantic Ridge formed 200 million years ago.
History[change | edit source]
The Great Glen Fault has a long history of movements. It formed towards the end of the Caledonian orogeny (mountain building) associated with the collision of tectonic plates at the end of the Silurian period, and continued into the early Devonian. The likely age range of the fault is 430–390 million years ago.
The second main phase of movement was during the Carboniferous. The exact timing is uncertain but associated folds within the Devonian are cut by members of the Upper Carboniferous to Lower Permian dyke swarm. The Great Glen Fault had its final phase of movement during the Upper Cretaceous to early Tertiary. The displacement is estimated to be 64 miles (104 km).
The fault is mostly inactive today, but occasional moderate tremors have been recorded over the past 150 years.
Notes[change | edit source]
- Scottish Gaelic: An Gleann Mòr, also known as Glen Albyn (Gleann Albainn - the Glen of Scotland) or Glen More
- Glen = valley
- Loch = lake, or a sea inlet.
- Redfern, Ron 2001. Origins: the evolution of continents, oceans and life. University of Oklahoma Press. pp. 82–3. ISBN 0806133597.
- "Overview of Great Glen Fault". http://www.scottish-places.info/features/featurefirst10625.html.