ingly "bald" spot. Over it are scattered white and yellow chips, and, for anything that the eye can itself distinguish, these could easily be the chips left in the path of work of a recently passing woodsman. The deception is absolute, and it belongs to the stump as well. The knots and gnarls and annular rings are perfectly preserved; the bark stands in prominent relief both by ruggedness and color, and all this not in wood, but in the monumental substance of stone. The precise manner in which the substitution of silica for wood was effected can not now be learned, but, in a general way, we know it to have been brought about as the result of a slow infiltration into the tree trunks of heated waters containing silica in solution.
The remains are fairly numerous, but what strikes one with special astonishment is the giant size which some of them attain. Diameters of six, seven, and eight feet are by no means uncommon,
high, and at that distance above the roots it measures forty-five feet in girth—a colossus that would hardly be shamed by its more gigantic brethren of the existing redwood forests of California. This, so far as I have been able to ascertain, is the facile princeps