ts were granite and metamorphic rocks, gravels, sands, clays and curved bars which serve also as a means of attaching the slightly out of line, the tendency of the belt, as of liquids on a portions of the local rocks. No granite, syenite, gleeiss, or horse. From these bars project, at the rear, two… … and that the belt will necessari- made quite light, is easily man- CHAPLIN’S HORSE RAKE, ; ly become crooked. Our position aged, and appears to be a very was precisely the same ; but J. 8. seems to ignore the force of masses of them, strewed over the surface, and forming part of desirable…
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