Upon the steep slope of a certain “bald” among the Great Smoky Mountains there lie, just at the verge of the strange stunted woods from which the treeless dome emerges to touch the clouds, two great tilted blocks of sandstone. They are of marked regularity of shape, as square as if hewn with a chisel. Both are splintered and fissured; one is broken in twain. No other rock is near. The earth in which they are embedded is the rich black soil not unfrequently found upon the summits. Nevertheless no great significance might seem to attach to their isolation--an outcropping of ledges, perhaps; a fracture of the freeze; a trace of ancient denudation by the waters of the spring in the gap, flowing …
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