It is not my inclination—to say the truth, it is not my forte—to describe the lions of Amsterdam—or of any of the other dams in this hybrid offspring of land and water. It was quite enough for me to see the shows—their pictorial delineation I leave to those of my tourist brethren who have studied under that inimitable painter, and hero of the hammer, Geo. Robins, Esq. They can readily transmute a varnished treckschuyt into a Cleopatra’s barge—a buggerlugg into a bust of bronze—a Flanders mare into a prancing Bucephalus—a brick trottoir into a tesselated pavement—or a Belgian flat into a garden of the Hesperides. The worst of this is, that, by the time they have ascended the Rhine, or entered Switzerland, their stock of the picturesque is expended, and they have only the sublime to draw upon for the remainder of the tour. To see the sights of Amsterdam, the gilders and stivers must be in perpetual motion. Even at the doors of the churches, the padré’s demand your money for admittance into their cold, damp, and dreary tabernacles—a most unusual practice on the Continent. In order to vary the journey, we returned by Utrecht to Rotterdam:—but although the route was _alter_, the scene was _idem_—and I will not detain the reader with any account of it. BATAVIAN CHARACTERISTICS. Of all the geological ups and downs which the surface of this globe presents, none is more remarkable, or less remarked, than that which the land of Holland has undergone. Every particle of its soil must once have occupied some higher land or even mountain of the Continent, before it travelled down to take its bath in the ocean—ultimately to rise to nearly the level of the sea—then to be rescued from the waters, partly by the operations of Nature, and partly by the industry of man. Even now the mighty Alps are daily crumbling down, and every shower of rain, and mountain torrent washes down its quota of soil to the Mediterranean or the German Ocean.[5] Should no volcanic revolution interrupt these watery changes, a period must come—ten thousand years are but a dot in the stream of time—when the high lands will be worn down into alluvial deposits which, rising from their oceanic beds, will become annexations to the existing plains. The lower heights will of course shew the effects of this “wear and tear” sooner than the snow-clad Alps; but even these last must one day undergo that transmutation and transplantation to which all sublunary things are destined. This is no imaginary speculation. It is not in Holland alone that we see vast tracts of land carried down from the hills—buried in the deep, for a time—and afterwards rescued from their watery beds. The Delta of the Nile was once among the mountains of Abyssinia—the Sunderbunds have spread far and wide to the south of Calcutta, dividing the Ganges into a hundred mouths—extending the land into the bay of Bengal, and sustaining myriads of animals, and even man himself—the Mississippi and the St.