ally painted than those where Scott drew from the vivid recollections of his journeys among the dales and moors of the Southern Uplands.
III. For the purposes of our present inquiry, I would class together as Highlands all the higher, more rugged, and mountainous ground, which differs on the whole from the uplands, not only in its greater elevation, but in the more irregular form of its surface, the narrower crests of its ridges, and the more peaked shapes of its summits. The geological structure of these tracts of country is generally so complicated that it gives rise to much greater variety of outline than is to be found in either of the other types of scenery. Each kind of rock yields to the weather in its own characteristic way, and as the rainfall is heavier and the slopes steeper than elsewhere, the influence of the weather upon the topography is more especially prominent.
In the northern parts of Wales where a group of ancient volcanic rocks has been laid bare by the stupendous denudation of the surface, a small tract of truly highland scenery has been carved out in Cader Idris, Arenig, Snowdon, and the surrounding heights in Caernarvonshire and Merionethshire. Another isolated area of volcanic hills forms the picturesque district of the Lakes. But it is in Scotland that this type is displayed on the largest scale and in the most varied diversity. The Scottish Highlands are built up of the most ancient rocks of the British Islands, and possess a geological structure of extraordinary complexity. They include a vast variety of materials which, rising
