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Have we not here a perfect case of what logicians call "reasoning in a circle," or "begging the question?" What, in view of this situation, becomes of the evolutionist's argument from fossils? And what becomes of the "ages" of speculative geology?

"It is really strange that vast numbers of perfectly similar specimens should be found, the chances against their perpetuation as fossils are so great; but it is also very strange that the specimens should be so exactly alike as they are, if, in fact, they came and vanished by a gradual change." Mr.

He therefore, as well as M. Alcide d'Orbigny, who had carefully studied the fossils, came to the opinion that it was an upper member of the Cretaceous group. It is usually in the form of a coarse yellowish or whitish limestone, and the total thickness of the series of beds already known is about 100 feet.

The coat and waistcoat which Forester wore at the ball were crammed in at the top; and underneath appeared unfolded linen, books, boots, maps, shoes, cravats, fossils, and heaps of little rumpled bits of paper, in which the fossils had once been contained. Dr. Campbell opened every one of these. The paper he wanted was not amongst them.

Over considerable areas the Chemung sandstones bear little or no trace of the action of the sea. The Catskill Mountains, for example, have as their summit layers some three thousand feet of coarse red sandstones of this series, whose structure is that of river deposits, and whose few fossils are chiefly of fresh-water types.

Marble, sea-shells, the chalk-cliffs of Dover, the limestone fossils which preserve for us animal forms of species long since extinct, the coral formations that are stretching out in dangerous reefs in so many seas of the tropics, are all identical in their chief ingredient, and, as we see, are by natural processes and various accidents constantly interchanging their positions.

"'Perhaps, said the professor, cautiously, 'you might wish to aid me in a little research that is to say, if you have an inclination for fossils. The double-entendre was not lost upon me. "'I have read all your books so eagerly, said I, 'that to join you, to be of service to you in any research, however difficult and trying, would be an honor and a privilege that I never dared to hope for.

Although the generic character of the Quiriquina fossils naturally led M. d'Orbigny to conceive that they were of tertiary origin, yet as we now find them associated with the Baculites vagina and with an Ammonite, we must, in the opinion of M. d'Orbigny, and if we are guided by the analogy of the northern hemisphere, rank them in the Cretaceous system.

Detached broken fossils of pre-adamite whales, fragments of their bones and skeletons, have within thirty years past, at various intervals, been found at the base of the Alps, in Lombardy, in France, in England, in Scotland, and in the States of Louisiana, Mississippi, and Alabama.

I am delighted with the bright results of your comparison of the Sheppy fossils with recent forms. You appear to have opened out an entirely new field of investigation, likely to be productive of most brilliant results.