The Northwest Highlands are the northern third of Scotland that is separated from the Grampian Mountains by the Great Glen (Glen More). The Caledonian Canal, which extends from Loch Linnhe in the west, 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. Suilven, Cùl Mòr, Cùl Beag, and Quinag are just some of the impressive rock islands o...
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The Northwest Highlands are the northern third of Scotland that is separated from the Grampian Mountains by the Great Glen (Glen More). The Caledonian Canal, which extends from Loch Linnhe in the west, 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. Suilven, Cùl Mòr, Cùl Beag, and Quinag are just some of the impressive rock islands of dark red or gray Torridonian sandstone which project 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.
This area's climate varies with altitude, altogether having wet, warm summers of average under 17C. The winters are mild at low altitude but become snowier and colder with higher elevation,...
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