Northwest Highlands

58°01′08″N 4°28′26″W / 58.019°N 4.474°W / 58.019; -4.474

The main geographical
divisions of Scotland
Eilean Donan Castle in the far north-west.
Liathach seen from Beinn Eighe. With the Munro “Top“ of Stuc a' Choire Dhuibh Bhig (915 metres) in the foreground and the two Munro summits in the background.
View east from Sgurr Mhòr over the "Horns" of Beinn Alligin
The Great Glen Fault
Outcrop of weathered Lewisian gneiss, Europe's oldest rock. 5 km NW of Loch Inver
Geological map of the Hebridean Terrane showing distribution of rocks of the Lewisian complex

The Northwest Highlands are the northern third of Scotland, which is separated from the Grampian Mountains by the Great Glen. The Caledonian Canal, which extends from Loch Linnhe in the west, via Loch Ness to the Moray Firth in the north splits this area from the rest of the country.

The Highlands are formed on Lewisian gneiss, the oldest layers of rock in Scotland. There are impressive rock islands of dark red or gray Torridonian sandstone which stick up out of the gneiss. Some of the peaks, such as Beinn Eighe and Canisp, are topped with light gray or white Cambrian quartzite.

The city of Inverness, known as the "Capital of the Highlands", is by far the largest settlement in the region. It is the administrative centre for the Highland Council area.


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