denoted by the names Thebes, Carthage, Athens, and Rome, may be regarded as an unity.  The four nations represented by these names, after each of them had attained in a path of its own a peculiar and noble civilization, mingled with one another in the most varied relations of reciprocal intercourse, and skilfully elaborated and richly developed all the elements of human nature.  At length their cycle was accomplished.  New peoples who hitherto had only laved the territories of the states of the Mediterranean, as waves lave the beach, overflowed both its shores, severed the history of its south coast from that of the north, and transferred the centre of civilization from the Mediterranean to the Atlantic Ocean.  The distinction between ancient and modern history, therefore, is no mere accident, nor yet a mere matter of chronological convenience.  What is called modern history is in reality the formation of a new cycle of culture, connected in several stages of its development with the perishing or perished civilization of the Mediterranean states, as this was connected with the primitive civilization of the Indo-Germanic stock, but destined, like the earlier cycle, to traverse an orbit of its own.  It too is destined to experience in full measure the vicissitudes of national weal and woe, the periods of growth, of maturity, and of age, the blessedness of creative effort in religion, polity, and art, the comfort of enjoying the material and intellectual acquisitions which it has won, perhaps also, some day, the decay of productive power in the satiety of contentment with the goal attained.  And yet this goal will only be temporary:  the grandest system of civilization has its orbit, and may complete its course but not so the human race, to which, just when it seems to have reached its goal, the old task is ever set anew with a wider range and with a deeper meaning.

Italy

Our aim is to exhibit the last act of this great historical drama, to relate the ancient history of the central peninsula projecting from the northern continent into the Mediterranean.  It is formed by the mountain-system of the Apennines branching off in a southern direction from the western Alps.  The Apennines take in the first instance a south-eastern course between the broader gulf of the Mediterranean on the west, and the narrow one on the east; and in the close vicinity of the latter they attain their greatest elevation, which, however, scarce reaches the line of perpetual snow, in the Abruzzi.  From the Abruzzi the chain continues in a southern direction, at first undivided and of considerable height; after a depression which formsa hill-country, it splits into a somewhat flattened succession of heights towards the south-east and a more rugged chain towards the south, and in both directions terminates in the formation of narrow peninsulas.