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.
The flat country on the north, extending between the Alps and the Apennines as far down as the Abruzzi, does not belong geographically, nor until a very late period even historically, to the southern land of mountain and hill, the Italy whose history is here to engage our attention. It was not till the seventh century of the city that the coast-district from Sinigaglia to Rimini, and not till the eighth that the basin of the Po, became incorporated with Italy. The ancient boundary of Italy on the north was not the Alps but the Apennines. This mountain-system nowhere rises abruptly into a precipitous chain, but, spreading broadly over the land and enclosing many