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er of the rock is most distinctly seen; the effect being increased in many limestones by the interposition of two or three thinner beds between the large strata of which the block has been a part; these thin laminae breaking easily, and supplying a number of fissures and lines at the edge of the detached mass. Thus, as a general principle, if a rock have character anywhere, it will be on the angle, and however even and smooth its great planes may be, it will usually break into variety where it turns a corner. In one of the most exquisite pieces of rock truth ever put on canvas, the foreground of the Napoleon in the Academy, 1842, this principle was beautifully exemplified in the complicated fractures of the upper angle just where it turned from the light, while the planes of the rock were varied only by the modulation they owed to the waves. It follows from this structure that the edges of all rock being partially truncated, first by large fractures, and then by the rounding of the fine edges of these by the weather, perpetually present _convex_ transitions from the light to the dark side, the planes of the rock almost always swelling a little _from_ the angle. Sec. 3. Salvator's acute angles caused by the meeting of concave curves. Now it will be found throughout the works of Salvator, that his most usual practice was to give a _concave_ sweep of the brush for his first expression of the dark side, leaving the paint darkest towards the light; by which daring and original method of procedure he has succeeded in covering his foregrounds with forms which approximate to those of drapery, of ribbons, of crushed cocked hats, of locks of hair, of waves, leaves, or anything, in short, flexible or tough, but which of course are not only unlike, but directly contrary to the forms which nature has impressed on rocks.[58] Sec. 4. Peculiar distinctness of light and shade in the rocks of nature. Sec. 5. Peculiar confusion of both in the rocks of Salvator. And the circular and sweeping strokes or stains which are dashed at random over their surfaces, only fail of destroying all resemblance whatever to rock structure from their frequent want of any meaning at all, and from the impossibility of our supposing any of them to be representative of shade. Now, if there be any part of landscape in which nature develops her principles of light and shade more clearly than another, it is rock; for the dark sides of fractured stone
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